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Advances

Forensic Taphonomy in

Method, Theory, and Archaeological Perspectives

© 2002 by CRC Press LLC

Advances

Forensic Taphonomy in

Method, Theory, and Archaeological Perspectives Edited by

William D. Haglund Marcella H. Sorg

CRC Press Boca Raton London New York Washington, D.C.

Library of Congress Cataloging-in-Publication Data Advances in forensic taphonomy : method, theory, and archaeological perspectives / edited by William D. Haglund and Marcella Sorg. p. cm. Includes bibliographical references and index. ISBN 0-8493-1189-6 (alk. paper) 1. Forensic taphonomy. I. Haglund, William D. II. Sorg, Marcella H. RA1063.47 .A37 2001 614'.1--dc21 2001029514 This book contains information obtained from authentic and highly regarded sources. Reprinted material is quoted with permission, and sources are indicated. A wide variety of references are listed. Reasonable efforts have been made to publish reliable data and information, but the author and the publisher cannot assume responsibility for the validity of all materials or for the consequences of their use. Neither this book nor any part may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, microfilming, and recording, or by any information storage or retrieval system, without prior permission in writing from the publisher. All rights reserved. Authorization to photocopy items for internal or personal use, or the personal or internal use of specific clients, may be granted by CRC Press LLC, provided that $.50 per page photocopied is paid directly to Copyright Clearance Center, 222 Rosewood Drive, Danvers, MA 01923 USA. The fee code for users of the Transactional Reporting Service is ISBN 0-8493-1189-6/02/$0.00+$1.50. The fee is subject to change without notice. For organizations that have been granted a photocopy license by the CCC, a separate system of payment has been arranged. The consent of CRC Press LLC does not extend to copying for general distribution, for promotion, for creating new works, or for resale. Specific permission must be obtained in writing from CRC Press LLC for such copying. Direct all inquiries to CRC Press LLC, 2000 N.W. Corporate Blvd., Boca Raton, Florida 33431. Trademark Notice: Product or corporate names may be trademarks or registered trademarks, and are used only for identification and explanation, without intent to infringe.

© 2002 by CRC Press LLC No claim to original U.S. Government works International Standard Book Number 0-8493-1189-6 Library of Congress Card Number 2001029514 Printed in the United States of America 1 2 3 4 5 6 7 8 9 0 Printed on acid-free paper

Table of Contents

Preface The Editors The Contributors Acknowledgments Multidisciplinary Forewords Foreword from Pathology Donald T. Reay

Foreword from Paleontology R. Lee Lyman

Foreword from Archaeology: A Pilgrim in Forensic Archaeology — A Personal View J.R. Hunter

Section 1: Theoretical Perspectives

1

Advancing Forensic Taphonomy: Purpose, Theory, and Practice Marcella H. Sorg and William D. Haglund

2

Is Forensic Taphonomy Scientific? Jon J. Nordby

Section 2: The Biogeographic Context

3

An Autopsy of the Grave: Recognizing, Collecting, and Preserving Forensic Geotaphonomic Evidence Michael J. Hochrein

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4

Forensics, Archaeology, and Taphonomy: The Symbiotic Relationship Julie Mather Saul and Frank P. Saul

5

Position of Skeletal Remains as a Key to Understanding Mortuary Behavior Mirjana Roksandic

6

Taphonomic and Forensic Aspects of Bog Bodies Don Brothwell and Heather Gill-Robinson

7

The Effect of Cultivation on Buried Human Remains William D. Haglund, Melissa Connor, and Douglas D. Scott

8

Detection and Recovery of Abducted and Murdered Children: Behavioral and Taphonomic Influences Robert J. Morton and Wayne D. Lord

9

Insects Associated with the Body: Their Use and Analyses Gail S. Anderson and Valerie J. Cervenka

10

Human Remains in Water Environments William D. Haglund and Marcella H. Sorg

11

Floating Remains on Pacific Northwest Waters Curtis C. Ebbesmeyer and William D. Haglund

Section 3: Mass Fatalities and Mass Graves

12

Recent Mass Graves, An Introduction William D. Haglund

13

Taphonomy of a Karstic Cave Execution Site at Hrgar, Bosnia-Herzegovina Tal Simmons

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14

Mass Graves and the Collection of Forensic Evidence: Genocide, War Crimes, and Crimes Against Humanity Stefan Schmitt

15

Postburial Disturbance of Graves in Bosnia-Herzegovina Mark Skinner, Heather P. York, and Melissa A. Connor

16

Cannibalism or Violent Death Alone? Human Remains at a Small Anasazi Site Sally Graver, Kristin D. Sobolik, and John Whittaker

17

Damnum Fatale: The Taphonomic Fate of Human Remains in Mass Disasters Paul S. Sledzik and William C. Rodriguez III

18

Approaches to the Study of Commingling in Human Skeletal Biology Doublas H. Ubelaker

Section 4: Modification of Bone, Soft Tissue, and Associated Materials

19

Detecting the Postburial Fragmentation of Carpals, Tarsals, and Phalanges Christyann M. Darwent and R. Lee Lyman

20

Degradation of Clothing and Other Dress Materials Associated with Buried Bodies of Both Archaeological and Forensic Interest R.C. Janaway

21

Taphonomic Context of Sharp-Force Trauma in Suspected Cases of Human Mutilation and Dismemberment Steven A. Symes, John A. Williams, Elizabeth A. Murray, J. Michael Hoffman, Thomas D. Holland, Julie Mather Saul, Frank P. Saul, and Elayne J. Pope

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22

A Critical Look at Methods for Recovering, Evaluating, and Interpreting Cremated Human Remains Pamela Mayne Correia and Owen Beattie

23

Recovery and Interpretation of the Fatal Fire Victim: The Role of Forensic Anthropology Dennis C. Dirkmaat

24

The Use of DNA in the Identification of Postmortem Remains Michele Harvey and Mary-Claire King

25

Disarticulation Pattern and Tooth Mark Artifacts Associated with Pig Scavenging of Human Remains: A Case Study Hugh E. Berryman

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Preface

It is only when viewed through the interdisciplinary lens that the full value of forensic taphonomy can be realized. Thus, we began the volume with a tri-partite foreword that is meant to be an integral part of this volume. These three contributions convey the perspectives of eminent spokespersons from pathology, anthropology/archaeology, and paleontology: the primary disciplines upon which taphonomy is based. Each author underscores the interdisciplinary nature of the field and, in the case of Hunter, presents a timely international perspective. Forensic pathologist Donald Reay speaks to the compatibility of collecting taphonomic data in the context of contemporary death investigations, its non-intrusiveness to the investigation process, and its potential contribution of broader-based data sets. He spreads a welcome mat to taphonomic approaches that is founded on personal experience and an enlightened vision. Lee Lyman, archaeologist and a leader in articulating taphonomic theory, points to what we believe is the seminal contribution that contemporary death investigation can repay to archaeology and paleontology. That is, a high-resolution perspective provided by actualistic experience in the time period spanning the “realms of flesh,” from the time of death through decomposition, and the flesh’s disappearance. Lyman further suggests a deeper, theoretical contribution of forensic taphonomy: its emphasis on positive findings (taphonomic data as evidence) as opposed to the more usual approach in paleontology of viewing taphonomic characteristics as a bias one must strip away to get to the truth. John Hunter offers a refreshing historical view of the recognition and growing pains of “forensic archaeology” in Great Britain. He also touches on the paradigm difference between the United Kingdom and the United States in the teaching of archaeology/anthropology. We would hope this makes more salient our sometimes provincial tendencies, characteristics we must confront more and more as we meet on the international stage to ply our professions. In addition to the bedrock disciplines of taphonomy, contributions to these pages also come from molecular biology, entomology, oceanography, criminal investigation, and philosophy — and from several authors outside the United States. Thus, it is in the spirit of interdisciplinary and international collaboration that we offer this volume. William D. Haglund, Ph.D. Marcella H. Sorg, Ph.D., D.A.B.F.A.

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The Editors

William D. Haglund, Ph.D., received his B.A. degree in biology from the University of California, Irvine, and his Ph.D. in physical anthropology from the University of Washington, Seattle. He served as Chief Medical Investigator of the King County Medical Examiner’s Office, Seattle, Washington, for 14 years. In December 1995 he became the United Nations’ Senior Forensic Advisor for the International Criminal Tribunals for Rwanda and the former Yugoslavia. He is presently Director of the International forensic Program for Physicians for Human Rights, a Boston-based non-governmental organization. He has conducted forensic missions in numerous countries, including Guatemala, Honduras, Rwanda, Somaliland, Georgia/Abkhazia, the former Yugoslavia, Cyprus, Sri Lanka, Indonesia and East Timor. Dr. Haglund teaches medicolegal death investigation through the Washington State Criminal Justice Training Commission. He also conducts international workshops, seminars and training in international forensic investigations. Dr. Haglund’s numerous publications have addressed issues such as outdoor scene processing for human remains, taphonomy, and human identification. Among these are two books, Taphonomy: the Postmortem Fate of Human Remains and the Medicolegal Death Investigator Training Manual. He has been an affiliate member of the Board of Directors of the National Association of Medical Examiners, is a past, three-time president of the Washington State Coroner/Medical Examiner’s Association, and is a fellow of the American Academy of Forensic Sciences. Marcella Harnish Sorg, Ph.D., D.A.B.F.A., is the consulting forensic anthropologist for the states of Maine and New Hampshire and an associated faculty member of the Department of Anthropology, University of Maine, since 1977. She served at the University of Maine as Associate Director of the Center for the Study of the First Americans, Institute for Quaternary Studies, from 1983 to 1988, and in private business from 1988 to 1996. She is currently Research Associate at the Margaret Chase Smith Center for Public Policy and on the faculty of both the School of Nursing and Department of Anthropology. Dr. Sorg received her R.N. from Fairview Park General Hospital in 1969, her B.A. in psychology from Bowling Green State University in 1972, and her Ph.D. in physical anthropology from The Ohio State University in 1979, and she was certified by the American Board of Forensic Anthropology in 1984. She has served as Secretary and as President of the American Board of Forensic Anthropology, and has returned recently to serve as a Director. Dr. Sorg is a Fellow of the American Academy of Forensic Sciences, a Member of the American Association of Physical Anthropologists, and the Maine Medico-Legal Society, and co-founder of the Northeast Forensic Anthropology Association.

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Dr. Sorg has authored many publications in forensic anthropology, taphonomy, and genetic demography. She was co-editor of the book Bone Modification in 1987, of Forensic Taphonomy in 1997, and co-authored The Cadaver Dog Handbook in 2000. She has done forensic research on scavenger modification of human remains as well as on the timing of epiphyseal union in the female medial clavicle. Her current forensic research focuses on taphonomic approaches to remains exposed in both marine and terrestrial environments, the estimation of postmortem interval, and the use of cadaver dogs, particularly for scattered remains.

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The Contributors

Gail S. Anderson, Ph.D.

Curtis C. Ebbesmeyer, Ph.D.

School of Criminology Simon Fraser University Burnaby, British Columbia Canada

Evans-Hamilton, Inc. Seattle, Washington

Owen B. Beattie, Ph.D. Department of Anthropology University of Alberta Edmonton, Alberta Canada

Hugh E. Berryman, Ph.D. Berryman Consulting 228 Bluegrass Circle Lebanon, Tennessee

D. R. Brothwell, Ph.D. Department of Archaeology University of York York, England United Kingdom

Valerie J. Cervenka, M.Sc. Department of Entomology University of Minnesota St. Paul, Minnesota

Melissa Connor, M.A. Forensic and Archaeological Services Lincoln, Nebraska

Pamela M. Mayne Correia, M.A. Department of Anthropology University of Alberta Edmonton, Alberta Canada

Heather Gill-Robinson, M.A. Department of Archaeology University of York York, England United Kingdom

Sally Graver, B.A. Smithsonian Institution Washington, D.C.

William D. Haglund, Ph.D. International Forensic Program Physicians for Human Rights Seattle, Washington

Michele Harvey, Ph.D. Division of Medical Genetics School of Medicine University of Washington Seattle, Washington

Michael J. Hochrein, B.A. Federal Bureau of Investigation St. Louis, Missouri

Michael J. Hoffman, Ph.D. Department of Anthropology Colorado College Colorado Springs, Colorado

Thomas D. Holland, Ph.D. U.S. Army Central Identification Laboratory Hickam AFB, Hawaii

Christyann M. Darwent, M.A.

J.R. Hunter, Ph.D.

Department of Anthropology University of Missouri Columbia, Missouri

University of Birmingham Birmingham, England United Kingdom

Dennis C. Dirkmaat, Ph.D.

R.C. Janaway, M.Sc.

Department of Anthropology Mercyhurst Archaeological Institute Mercyhurst College Erie, Pennsylvania

Department of Archaeological Sciences University of Bradford Bradford, England United Kingdom

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Mary-Claire King, Ph.D.

Stefan Schmitt, M.S.

Division of Medical Genetics School of Medicine University of Washington Seattle, Washington

School of Criminology and Criminal Justice Florida State University, and Florida Department of Law Enforcement Tallahassee, Florida

Wayne D. Lord, Ph.D.

Douglas D. Scott, Ph.D.

National Center for the Analysis of Violent Crime FBI Academy Quantico, Virginia

Midwest Archaeological Center National Park Service Lincoln, Nebraska

R. Lee Lyman, Ph.D.

Tal Simmons, Ph.D.

Department of Anthropology University of Missouri Columbia, Missouri

Department of Anthropology Western Michigan University Kalamazoo, Michigan

Robert J. Morton, B.A. National Center for the Analysis of Violent Crime FBI Academy Quantico, Virginia

Elizabeth A. Murray, Ph.D. Department of Biology College of Mount St. Joseph Cincinnati, Ohio

Jon J. Nordby, Ph.D. Final Analysis Forensics Tacoma, Washington

Elayne J. Pope, M.A. Department of Anthropology University of Tennessee Knoxville, Tennessee

Donald T. Reay, M.D. Oak Harbor, Washington

William C. Rodriguez III, Ph.D. Office of the Armed Forces Medical Examiner Armed Forces Institute of Pathology Washington, D.C.

Mirjana Roksandic, Ph.D. Max Planck Institute for Demographic Research Rostock, Germany

Frank P. Saul, Ph.D.

Mark Skinner, Ph.D. Department of Archaeology Simon Fraser University Burnaby, British Columbia Canada

Paul Sledzik, M.S. National Museum of Health and Medicine Armed Forces Institute of Pathology Washington, D.C.

Kristin O. Sobolik, Ph.D. Department of Anthropology, and Institute of Quaternary and Climate Studies University of Maine Orono, Maine

Marcella H. Sorg, Ph.D. Margaret Chase Smith Center of Public Policy, School of Nursing, and Department of Anthropology University of Maine Orono, Maine

Steven A. Symes, Ph.D. Department of Pathology University of Tennessee, and Regional Forensic Center Memphis, Tennessee

Douglas H. Ubelaker, Ph.D.

DMORT V Regional Command Lucas County Coroner's Office Toledo, Ohio

Department of Anthropology National Museum of Natural History Smithsonian Institution Washington, D.C.

Julie Mather Saul, B.A.

John Whittaker, Ph.D.

Forensic Anthropology Laboratory Lucas County Coroner's Office Toledo, Ohio

Department of Anthropology Grinnell College Grinnell, Iowa

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John A. Williams, Ph.D.

Heather P. York, M.A.

Department of Anthropology University of North Dakota Grand Forks, North Dakota

Department of Anthropology Kent State University Kent, Ohio

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Acknowledgments

As always in our endeavors, we thank those closest to us for their support and patience, especially Claudia and Ed. We also thank Joy Sorg, Noah Haglund, C.J. Bidwell, Juliet Fernandez, Boyd Brown III, Judith Cooper, Karen Turnmire, Bill and Kathy Cook, Amy Clifford, and Barbara Harrity. And, we offer our eternal gratitude to Becky McEldowney of CRC Press for her saintly forbearance during the birthing of this volume. We extend our gratitude to the Physicians for Human Rights of Boston, whose commitment to forensic issues in international human rights is an inspiration. We also thank colleagues at the Margaret Chase Smith Center for Public Policy and the School of Nursing, University of Maine, for their encouragement.

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Foreword

R. LEE LYMAN Russian paleontologist I.A. Efremov (1940) coined the term taphonomy and defined it as the study of the transition, in all its details, of organic remains from the biosphere to the lithosphere. My dictionary defines forensic as pertaining to argument, debate, or public discussion suitable for courts of justice. Contributors to this volume and its precursor (Haglund and Sorg, 1997) would define forensic taphonomy as the study of the transition of humans from living organisms to mortal remains, including causes of death, for judicial or legal purposes. I find the extension of taphonomic research into forensics to be critical for one simple reason. What can readily be categorized as taphonomic research has a deep history in paleontology, one of my two personal choices for the most exciting field of scientific inquiry, the other being archaeology. In the early nineteenth century, William Buckland (1823) observed how a hyena gnawed and thereby destroyed animal bones. Buckland used his observations to conclude that ancient bones with similar damage recovered from ancient cave deposits had been chewed by ancient hyenas. Archaeologist Edouard Lartet (1860) used precisely the same sort of reasoning to conclude that prehistoric humans had butchered extinct animals and, thus, humans and those beasts had been contemporaries. What Buckland, Lartet, and others in the nineteenth century were doing was actualistic research in an effort to gain insight to the processes that created particular taphonomic patterns among modern bones. Actualistic research — documentation of modern processes and the visible effects and patterns they produce — formed the basis for their inferences that the same processes had created the patterns among both the modern and the prehistoric materials. More than a century later, taphonomists have microscopes, including scanning electronic microscopes, instead of magnifying glasses, and they have computers to crunch all kinds of data of which Buckland and Lartet never dreamed. They also have radiocarbon dating laboratories to tell them exactly how old the bones are; biologists who can tell them the most intimate details about the physiology and life ways of the animals whose remains they are studying; chemists and geneticists to study dietary and genetic variation, respectively, as reflected in preserved tissues; and a host of other specialists, laboratories, and machines to help them decipher the fossil and subfossil records and thereby write taphonomic histories. Books and journal articles abound on each topic, indicating we know a great deal more about taphonomy than our intellectual predecessors of the nineteenth century. Yet the fundamental epistemology of actualism pioneered by Buckland, Lartet, and others remains the centerpiece of taphonomic and forensic research. Taphonomy and forensics are identical fields of investigation. Both seek an answer to the question “What are these bones doing here?” as taphonomist Pat Shipman put it 20

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years ago. True, forensic scientists want an answer they can take to court, whereas a taphonomist’s answer is usually judged only by other taphonomists and perhaps a few paleontologists or zooarchaeologists. Otherwise, there is absolutely no reason why the methods and techniques of one field of inquiry cannot overlap virtually completely those of the other, and this brings us to the point of my brief history of taphonomy, the reason I find the extension of the definition of taphonomy to include forensics and human remains to be significant. That point is simply this. Forensic scientists, on the one hand, are always looking for evidence that tells them what I think of as something positive about the bones and teeth they examine. Who was the represented individual? How and why did he or she die? Why are the mortal remains of the individual in the condition they are when found? Does anything about that condition imply a felonious act or help identify a perpetrator of the act? On the other hand, paleontologists and, particularly, zooarchaeologists are typically looking for what I think of as negative evidence, which I do not mean is the notion captured by the phrase “the absence of evidence is not necessarily evidence of absence,” sometimes referred to with the shorthand “negative evidence.” Rather, what I mean is that taphonomy is too often construed by taphonomists to merely comprise biasing processes. Most of the time in the zooarchaeological literature of the 1980s and 1990s we find the phrase “strip away the taphonomy cover print” or some variant thereof (see Lyman [1994] for an introduction to the relevant literature). Much less frequently do we see the evidence a taphonomist examines construed as somehow contributing in a positive way to our understanding of and knowledge about the past. And that, I think, is an important lesson that taphonomists can learn from forensic scientists. What do those gnawing marks apparently generated by carnivores represent with respect to the paleoecological setting in which the bones were deposited? Certainly more than that some bones or bone parts might be missing not because ancient hominids didn’t deposit them in the site sediments but because carnivores removed them. Those gnawing marks clearly mean that carnivores were part of the paleoecological setting, just as butchering marks on other bones in the collection signify that hominids were another part of the setting, had tools, and were extracting resources from animal carcasses; this was Lartet’s inference of 1860 and that same inference can be made today. Perhaps I am a bit too pessimistic with respect to my taphonomically inclined colleagues. Regardless of that, I think it is clear that we need to think about taphonomic histories in the same way that forensic scientists think about the human remains that they study — as revealing aspects of those histories that could be important for both analysis and interpretation. But by the same token, forensic scientists need to think, at least sometimes, like taphonomists; that is, to think of the negative aspects of taphonomic histories, the possible biases. For example, they need to be able to distinguish damage to bones that resulted from rodent gnawing from damage that resulted from felonious assault on the individual. They also must recognize that the former, if sufficiently extensive, may well remove all traces of the latter; that is, taphonomic history can bias — be negative — forensic evidence. I have argued that taphonomy and forensic science are, in a very practical way, sister disciplines. But they are also a bit different and some of us occasionally forget that fact. That these disciplines are different can be made clear by posing a question and telling a brief story to answer. Why are human feet sometimes so much better preserved than other parts of the body? A taphonomist would argue that it may be the result of the greater

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structural density of foot bones than other bones of the human skeleton. But as my colleague Sam Stout, who oversees the Human Skeletal Identification Laboratory at the University of Missouri, Columbia, pointed out to me, humans wear shoes, and footwear protects and shields human feet from the ravages of various sorts of taphonomic agents. On one occasion, Stout was out of town and two deputy sheriffs seeking his counsel showed up at my office near the forensic lab. They handed me a tightly sealed plastic bag and asked that I make sure that Dr. Stout be given the bag as its contents comprised important forensic evidence for a legal case. I glanced at the bag and asked the deputies why Stout would want the wing tip shoe the bag contained. The deputies replied, “Because of the foot inside the shoe.” Stout was glad to have such a complete portion of the human anatomy; I nearly lost my lunch. Looking back at that example, I did learn something from the forensic perspective. Forensic scientists can no doubt learn similar lessons from taphonomists, and probably without any feeling of nausea. The chapters in this volume are important contributions. In my view they reveal many of the parallels between taphonomy and forensic science, and in many ways other than the most fundamental shared aspect — actualism. Those of us in the taphonomy business can learn much about the earliest stages of taphonomic histories by reading this book. Forensic scientists can learn an equal amount by close study of the research undertaken by taphonomists that is described here. There is no shortage of paleontologically and archaeologically related studies focusing on single and multiple body or carcass sets of remains. Taphonomists often perform various types of actualistic research that forensic scientists would no doubt find of some utility were they to examine it. Recently, I’ve heard more and more regarding the benefits of interdisciplinary research — more funding, more solidly founded results, more relevant and pertinent conclusions, more marketable graduate students with interdisciplinary training. Forensic scientists and taphonomists would be well advised to pay heed and to interact much more frequently. This book is an important step in that direction.

References Buckland, W. 1823 Reliquiae Diluvianae, or Observations on the Organic Remains Contained in Caves, Fissures and Diluvial Gravel and on Other Phenomena, Attesting to the Action of a Universal Deluge. Murray, London. Efremov, I.A. 1940 Taphonomy: a new branch of paleontology, Pan-American Geologist 74:81–93. Haglund, W.D. and M.H. Sorg, Editors 1997 Forensic Taphonomy: The Postmortem Fate of Human Remains, CRC Press, Boca Raton, FL. Lartet, E. 1860 On the coexistence of man with certain extinct quadrupeds proved by fossil bones, from various Pleistocene deposits bearing incisions made by sharp instruments, M.G.S. Quarterly Journal of the Geological Society of London 16:471–479. Lyman, R.L. 1994 Vertebrate Taphonomy, Cambridge University Press, Cambridge, U.K.

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Foreword

DONALD T. REAY This second volume on forensic taphonomy adds to the available information about the postmortem fate of human remains. It is necessary to review the objectives first laid out by the editors in their first volume, Forensic Taphonomy: the Postmortem Fate of Human Remains (1997). In its introduction, the editors stated, “Data can be collected routinely in the normal course of the forensic investigation without interfering with the medical legal process. And if data collection strategies are shared among practitioners, the data sets will be more comparable and broader-based.” In their first volume, the editors made a major contribution to our understanding of how bodies decompose in different environmental conditions, the effects on the body of human and non-human activities including animal scavenging, the effects of aqueous dispersion of bodies and body parts, and the effects of immediate postmortem transfer. Although the first volume is multi-authored, each chapter provides the reader with new data and observations, frequently about individual cases, but nicely synthesized and discussed for the reader to ponder their significance. This second volume brings new data and observations extending from the initial volume, and again gives us insight into the discipline of forensic taphonomy. I would be remiss not to comment on what I consider the major achievement that the editors have attained by publishing on this subject. In 1991, I had the distinct privilege of reviewing the doctoral thesis of Dr. Haglund (Haglund, 1991). This was my first exposure to an organized body of information which dealt with the subject of taphonomy. Much of this work was the result of some 10 years of investigation into the deaths of a number of women who were the composite of the Green River murder investigation. During that investigation the bodies of young women were discovered in varying states of decomposition including skeletonization. At that time, our emphasis was on establishing identity and cause of death, the typical obligation and expectation of any agency responsible for examining human remains in a death investigation. Through the efforts of Dr. Haglund other information began to emerge. The manner and sequence of the disarticulation of the skeleton were noted and the way in which bodies were scavenged by predators was observed. Additionally, the environmental milieu in which human remains were found took on new significance. Although the ambient conditions have always been recognized as playing a major role in establishing time of death, as it unfolds and manifests itself in decomposition, assessing these observations for answers took on considerable urgency because of the nature of this serial murder investigation. In attempting to answer some questions concerning the nature of the decomposition and the dispersal of skeletal remains by predators, standard references in anthropology and forensic pathology were consulted. Sources from both these fields were found wanting in providing specific useful information. It was clear that anthropology and forensic pathol-

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ogy had not progressed to the point where useful information and observations had been recorded to aid our investigation. It was also clear that archeologists and paleontologists had much to say regarding the handling and processing of a scene where ancient human remains had been discovered. Recognizing the limitations of the information that was available, we attempted to answer questions about the postmortem fate of human remains during our death investigation. This was a new and exciting area of exploration which stimulated Dr. Haglund to organize the observations that later formed the central theme of his doctoral thesis. In my view, a new discipline of forensic taphonomy emerged for use by the forensic community. Why “taphonomy?” The use of the word has been generally restricted to the archeological recovery of burial sites and, to some authors (Olsen, 1980), the study of dead organisms from the biosphere to the lithosphere, i.e., fossilized organisms and their death assemblages. Taphonomy comes from the Greek taphe, which means grave. Since it has an archeological meaning for the study of gravesites, the subject material under examination from a forensic point of view is the study of the site of discovery of a body, which can be a shallow or deep grave or a surface deposit. The immediate concerns of the death investigator are the disintegration of flesh and bone in different environmental conditions and how it relates to the time of death. Other concerns include the modifications and disbursement of body parts caused by animal scavengers and the effects of standing and running water on a body; and the effects on a body of postmortem trauma whether inflicted by another human, animal, or the environment. It is fitting to make available whatever information exists on the subject of forensic taphonomy to enhance any death investigation where a body has been exposed to a variety of forces of man and nature. Volume 1 succeeded in accomplishing its goal of presenting data and information from a variety of sources in a very readable and scholarly fashion. This second volume amplifies the success of the first. The editors are to be commended for assembling the contributors to present information for use by the forensic community.

References Haglund, W.D. 1991 Applications of Taphonomic Models to Forensic Investigations. Ph.D. dissertation, Department of Anthropology, University of Washington, Seattle, University Microfilms, Ann Arbor, MI. Haglund W.D. and M.H. Sorg, Editors 1997 Forensic Taphonomy: The Postmortem Fate of Human Remains, CRC Press, Boca Raton, FL. Olsen, E.C. 1980 Taphonomy: its history and role in community evolution. In Fossils in the Making: Vertebrate Taphonomy and Paleoecology, edited by A.K. Behrensmeyer and A.P. Hill, pp. 5–19. University of Chicago Press, Chicago, IL.

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Foreword: A Pilgrim in Forensic Archaeology — A Personal View

J.R. HUNTER Forensic archaeology is a relatively well-recognized area of study in the United States where it is a component of physical anthropology in medico-legal matters. However, in the United Kingdom, where archaeology evolved as an independent discipline concerned purely with excavation and field skills, and in which human skeletal analysis was incidental rather than focal, forensic archaeology developed somewhat later and with a different character. Differences between the two “archaeologies” become compounded at scenes of crime: in Britain, for example, post-mortem study is normally the legal responsibility of the forensic pathologist, the role of the forensic archaeologist being one of providing supporting data through fieldwork. Forensic archaeology probably took its first public bow on a U.K. stage in 1988 with the discovery and excavation of a 3-year-old boy called Stephen Jennings, murdered by his father some 26 years earlier. There may have been instances of archaeologists assisting in other cases before then, but there are no informal, or even folk records of such, nor are there any more formal reports of archaeologists being called upon to give evidence in court. For this archaeologist, one of those involved in the recovery of Stephen Jennings, the event set in motion an unwitting divergence from an otherwise innocent career in historical archaeology. Since that time the smooth and predictable cycle of academic life has been disrupted by visits to distant parts of the country at short notice, by lengthy briefing meetings about hitherto unknown nefarious individuals and their activities, and by unpredictable late night telephone calls. The number of homicide cases involved over the years has never been counted; some merely reared their heads as requests for advice, or as visits by officers bearing a bag of bones, but every year a consistent number developed into scene visits and into deeper, practical involvement. These have occurred as complete burials, dismemberments and cremations; they have involved adults, children, ex-lovers, and spouses, and prostitutes; they have been brought about by drugs, accident, cultural incompatibility, or by sheer hatred; and the victims have been buried deeply, shallowly, or simply dumped on the surface and concealed. Taphonomically, some have decayed beyond recognition, some show differential decay, some still hung together articulately thanks to the resilience of synthetic fibers, and others had been scavenged by creatures of the wild. No two cases have ever been the same, or even remotely similar. They testify to unpleasant sub-cultures normally concealed from the gaze of much of society, and are viewed uncomfortably by many middle-class undergraduates who wrongly considered forensic archaeology to be a more glamorous subject for study.

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Forensic archaeology has evolved rather than flourished, and this somewhat personal view touches upon, inter alia, matters of professional and ethical responsibility encountered by its practitioners working in a novel arena. Conveniently, it follows an earlier paper that sought to market forensic archaeology to an unwary U.K. archaeological community (Hunter 1994).

Background There used to be the naive view, certainly held by this practitioner, that to trot across a suspect’s garden with a twin-probe geophysics array would undoubtedly detect the buried remains of some unfaithful spouse allegedly buried there and, equally, that to apply skilled archaeological methodology at a scene of crime was all that was necessary to ensure recovery in the best professional way. Such simplicity was soon dashed. It became manifestly apparent that forensic archaeology would never be a straightforward transference of methodology, but rather the application of archaeological theory to forensic circumstance. The time frame, the protocols, the processes, the chains of evidence, the working parameters, the ancillary disciplines, and the judicial constraints were all distinctive. More pertinently, the way in which the buried data were interrogated was different, and this alone effectively created a divergence between forensic archaeology and research-driven archaeology. In a recent paper entitled “The Excavation of Modern Murder” there was an attempt to flag some of the questioning that guided the excavation of a homicide victim; it also highlighted the differences between those questions and those designs which underlie the research-driven excavation of, for example, a Romano-British burial (Hunter, 1999). Pathological examination of a murder victim normally requires responses on at least three fronts: identity, interval since death, and cause/manner of death. Archaeological intervention can, directly or indirectly, aid all three, but the questions are already diverging from those normally asked under typical archaeological circumstances. Most significant is the issue of individuality: the homicide remains become personalized, they have a name, and they may have a grieving family. The life, activities, and last movement of the victim become a focus of necessary interest, and thus the ethical issues and professional responsibilities take on a different character from those of the traditional archaeological norm. Ultimately the forensic inquiry is geared to resolving the question, “Who killed this person?” In helping to achieve that answer the forensic archaeologist asks questions not normally voiced under purely archaeological conditions, and these questions frame the methodology of inquiry accordingly. Recovery is not simply the recording of buried evidence. It involves an understanding of how a grave might have been dug, the transfer of material between offender and grave, the nature of that material, how it can be sampled, how it can be contaminated, and often the degree of conclusiveness it can offer as evidence within the strict definitions imposed by forensic science. The archaeologist not only needs to be sure of his or her role within the investigating team, but must also be confident about how other members of the team operate, the nature of their evidence, and their respective methodologies. Other team members — the forensic scientist, entomologist, pathologist, and scene of crime examiners, etc. — have different evidentiary requirements based on diverse knowledge, background, and training. There are also new areas of study, including taphonomy, which lie in no-man’s land. Taphonomy covers more than simple decay process. Often perceived incorrectly as the exclusive remit

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of the forensic pathologist, it requires a diversity of knowledge from animal behavior and bacteriological activity to climatic and botanical effects (see Haglund and Sorg, 1997).

Mission and Morality Forensic archaeology requires team playing within a broad panorama of the different groups and disciplines involved. The archaeologist needs not only to understand the respective roles, but also to ensure that the different groups understand the nature of archaeological inquiry. Sigler Eisenberg’s early (1985) identification of a mission factor was especially perspicacious in this respect, but mission also seems equally relevant within the archaeological community itself. In a well-worded article, Cox (1998) criticized a number of operators for calling themselves forensic archaeologists when they were unlikely to appreciate the nature of criminal inquiry, the archaeologist’s role within it, or the extent of subject areas involved from psychology to taphonomy. There are also, sadly, archaeological purists who have failed to grasp what forensic archaeology is really about simply because they have been unable to recognize that the questioning of the buried data and the goals are distinctive from traditional archaeology. The end point of the forensic process is the conviction of the offender. In the recovery and autopsy of the victim, there is a strong argument to suggest that the end justifies whatever means are necessary to achieve it. In human terms, the recovered buried remains possess a name, a history, and a set of familial relationships. In cold, clinical, terms, they constitute potential evidence that requires investigation, analysis, or dissection to answer specific questions. It may be that the need to achieve those answers requires the dominance of one technique over another, that the need to collect one type of evidence overrules the loss of other evidence. Decisions are made through collaboration between scene specialists, not through a process of ethical and moral dilemmas, nor through the exactitudes of archaeological purism. What matters most are the underlying principles of the various techniques involved and the ability of all concerned to understand them. This is a process in which the archaeologist has to respond to a given situation: what may be professional best practice in one archaeological context is not necessarily best practice in a forensic one, and vice versa. It is perhaps opportune that the levels of competence and ability required in a forensic archaeologist are now being defined more precisely. The U.K. is moving inexorably toward the registration of forensic practitioners in all fields, from archaeologists to entomologists and from fingerprint specialists to toxicologists. Experience suggests that key requirements for a forensic archaeologist will be a long and varied experience in archaeological fieldwork, a working knowledge of skeletal remains, and the ability to operate independently within a crime scene, to make rapid decisions, and to be confident. Over-arching, however, is the need to understand crime scene protocols and the evidentiary requirements of others involved at the scene itself. The fragmented police structure in Britain means that disseminating information of any type or spreading mission is extremely difficult. The evidence from the relatively low number of burials in the U.K. each year (there is no precise figure but information suggests probably less than around 15 per year out of a total of some 700 homicides), based on word of mouth and anecdote, suggests that around half of these utilize proper archaeological techniques. Most involve instances where the burial site is known, the operation is fully briefed, and the forensic archaeologist is brought in at an early stage. The others

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(again, based on word of mouth and anecdote) are dug up rapidly without archaeological support through the necessity for speed (custody law in Scotland, for example, is only 6 hours), because they were found in an existing operation, or because of the perceived costs of bringing in specialists when the case is already cut and dried (i.e., when the necessary questions had already been answered without specialist support). Some police forces are more than happy to use archaeologists, and draw them in frequently at the earliest opportunity, whereas others are clearly not interested. Ignorance is no longer an excuse: several archaeologists have expended much energy and effort over the last decade in presentations on search and recovery to various groups involved, e.g., detectives, scene of crime officers, forensic scientists, coroners, etc. Homicide convictions have used archaeological evidence, and hence exhumation without archaeological assistance now lays itself open to more exacting cross-examination in court. One recent case was based entirely on taphonomic criteria. Was the victim’s state of decay commensurate with the interval since death and with active local carnivore activity, or had the body been moved? And who is competent to give opinion? To what extent is this “archaeology” by either U.K. or U.S. definitions? In retrospect, some 12 years since Stephen Jennings was excavated by archaeologists, there has been substantial progress, but not wholesale practical acceptance by either police forces or even archaeologists themselves. Stephen Jennings was a landmark. Whatever brutality and abuse he suffered in his 3.5 years of life are in some small way balanced by a growing string of life sentences that have occurred since, for which the recovery of his body was an archaeological precedent. However, even after these same 12 years, those few archaeologists who practiced forensic archaeology on their own time then, as some form of conviction, are still doing it today, still on their own time as an extra to their “day” jobs. More significant progress might perhaps have been made from a single high-profile case with national media interest.

Breadth At a conference in 1995 I made the throwaway comment that forensic investigation was one of the most frightening exercises for an archaeologist to undertake (see Cox, 1995). It was, however, a comment restricted to an experience of the occasional scene of crime, of helping to resolve some clandestine event by pitting wits against an unknown adversary. The rewards lie in achieving a sense of altruism from applying skills to society’s darker side, while being protected from the full reality by a cushion of scene protocols and a buffer of judicial machinery. These mixed sensations will be familiar to those who have undertaken the same or something similar, but the experience did not embrace the horrors of genocide and mass graves, where the motivation of inquiry and the questioning of evidence differ even further from research-led archaeology. Nor was it anticipated that Mant’s early work on taphonomic processes might be called upon to explain or predict the state of decay in multiple burials (see Mant, 1987). Those archaeologists who have gone to the killing fields of Rwanda, Bosnia, or Kosovo will be more acutely aware of these various issues as well as the emotional factors involved. The word “forensic” is not to be taken lightly. Unlike other specialist archaeological epithets — “environmental,” “underwater,” or “Aegean” — it involves a gravitas and a more distinctive knowledge base than is generally recognized by many other archaeologists. Like

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its research parent, forensic archaeology has no well-defined limits: it branches into fairly obvious areas such as biological anthropology; and it covers other taphonomic phenomena, although both the timescales and the materials are novel (cardboard, paper, cigarette butts, plastics and synthetic fibers, and human decay in the short term). Forensic archaeology also feeds off other intelligences of which the pure archaeologist might be better aware, notably offender profiling and dump site analysis. It also merges, uncomfortably, into matters of human rights. Until about 5 years ago, the concept of human rights had no place in the emerging forensic archaeology of Europe, or even in its vocabulary. From the United States physical anthropologists spread their expertise into South and Central America, and then into Africa, initially to recover and assess the mass graves of victims of genocide and political killings, and subsequently to recognize evidence of torture and human rights violations on human remains. Belief that such atrocity could never occur within the civilized western world was overly optimistic. Bosnia put an end to that, as later did Kosovo. Pessimism suggests that it is in human nature for there to be more killings, and that there is some urgency to improve on our expertise for the next time. Forensic archaeology’s first 12 years in the U.K., if nothing else, have been a learning curve; no two scenes of crime, big or small are ever the same and the emergence of human rights issues has become a fact of life in forensic archaeology whether we like it or not. Torture, for example, both psychological and physical, can occur in many ways: beatings, suspension, electric shock, burns, asphyxiation, nail torture, dental torture, pressure, strapping, forced positions, sexual abuse, etc., and any of these can leave traces on the hard as well as the soft tissue (Henneberg, 1999). It is important that the archaeologist knows about them during the recovery process, and that the anthropologist knows what to look for in the autopsy. Once again it is the nature of the questions that drives the method of recovery, not the direct application of field archaeology. The excavation of mass graves in Bosnia and Kosovo has also provided a much needed focus for the energies and convictions of forensic archaeologists and forensic anthropologists from many parts of Europe, notably Scandinavia and the United Kingdom. This is understandable given that the skills and knowledge these people learn (many of them students) from a growing range of university courses are largely unpracticed in what we might call normal criminal circumstances, and are likely to remain so. For some this is probably the only way of getting forensic archaeology experience. Archaeologists tend to be noted for the values they hold, their concern for the environment, and for their contribution to society’s knowledge base. To many archaeologists, working within mass graves is to exercise archaeological skills in an unusually meaningful way, and one more suited to satisfying personal missions under the disguise of altruism. It fits well, too, with a profession based on short-term employment contracts, and which in the United Kingdom at least has seen the prescriptive processing of developer-led archaeology sap much of the creative spirit from the discipline. Bosnia also gives some scope for physical anthropologists to practice in a real scenario, not just with the bones from an Iron Age cemetery and the odd Romano-British family. This is particularly relevant for those practitioners from countries where, unlike the United States, physical anthropologists have no traditional role in the forensic process. These may be some of the reasons why Bosnia and Kosovo seem so attractive. Forensic archaeology can also act as a postbox to a rich variety of skills that may be used on an occasional basis — zoological and botanical reference sets, total station recording or

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conservation skills, palynology, soils science etc. — all of which supplement the existing bread-and-butter techniques of the established forensic science service. This is a new and largely untapped forensic science resource. Sadly, it can become embarrassing when the archaeological proponents of these skills profess minimal or nil interest in support. They are reluctant to drop everything at a few hours’ notice, to be distracted, or be inconvenienced after hours. While quite content to bask in the heat of being an expert in beetles, grasses, teeth, cremations, or snails, they are not prepared to be inconvenienced where their contribution might matter most. Forensic archaeology feeds off other intelligences of which the traditional archaeologist might be aware, notably offender profiling, site disposal statistics, witness veracity, etc. All these have to be slotted into an equation in a forensic search before site targeting can take place. Not only does the archaeologist begin to know the victim, but there is also a real need to know about the offender, because knowing about the offender helps to locate the grave. How can objectivity possibly be retained under such circumstances? How is it possible to balance the need to remain clinical, and at a mental distance? And what happens when, despite all efforts to prevent it, there is involvement with the family of a victim, a victim who has not been found, and whose case the police may have wound down? Is it still possible to remain detached from the event? The longer and more detailed the case, the more familiar the victim becomes to the searcher. There are some victims I have never met, but I know them better than I know some of my friends. Where do ethics and responsibility fit into that context, and is it something that should now be reflected in our archaeology degree programs?

Search Recovery is only one part of the forensic archaeological spectrum. Another important aspect, and probably the one used most frequently is search. Several archaeologists, working independently for any of the 40 or so separate police forces which constitute the United Kingdom’s law enforcement system, noticed the lack of awareness among police forces regarding the range of search techniques available (technical, human, and canine) for finding clandestine graves. They also noted that the advantages and limitations of the respective techniques were largely unrecognized, and the extent to which the decay processes of the individual were being ignored in the detection equation. There was little conception, for example, of using complementary methods, or even sequences, depending on the situation. There was, by contrast, a tendency for police forces to use ground-penetrating radar (GPR) irrespective of whether it would work within the environment in question, its cost, and whether the operator was familiar with the responses given by GRP to human remains as opposed to the more customary civil engineering application. There was a similar tendency to consider geological search techniques with little in the way of regard for the scale of the task in hand, the nature of the local environment, or of the required sensitivity of response. The clear need for a central advice forum was eventually satisfied by the setting up in 1996 of the Forensic Search Advisory Group (FSAG) which incorporated personnel in academic life, commerce, police, and the military, covering a range of skills including geophysics, aerial interpretation, archaeology, decay chemistry, and body-scent dog training. Although the group has no formal status, it enjoys the recognition of ACPO (Association of Chief Police Officers) and is used frequently by the Home Office and the National Crime

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Faculty to put any police force requiring support in touch with the group by means of a 24-hour pager system. The group receives requests approximately 30 times per year on average, of which about two thirds result in operational support. The FSAG is broadly modeled on NecroSearch International, a similar but larger group in the United States. Elsewhere in Europe a similar organization has emerged in Sweden and a new group is forming in The Netherlands. There are embryonic noises emanating from other countries, but in general there is little awareness elsewhere of the opportunities and potential available from harnessing and centralizing resources in this way. Experience of this centralized search facility suggests that search usually follows one of two broadly defined routes (although there are always exceptions): (1) cases where a person is missing and a homicide and disposal are thought to have occurred, and where a number of locations need identifying and targeting; and (2) instances where information is received that an alleged clandestine burial has occurred in a particular vicinity, usually in a place that can be closely defined. The first of these involves a protracted analysis, initially desktop, of landscape, geology, and photographic evidence, together with psychological profiling, dump analysis, and the use of other intelligence. This includes targeting possible locations and utilizing certain techniques and sequences of techniques in order to maximize recovery potential. In these investigations the body of a known victim is being actively pursued. The second, and undoubtedly the more common, requires the elimination of sites. The information that promotes them is often hearsay, nostalgic, and warped through passage of time and drug or alcohol abuse. Despite this, the information often seems to contain some elements of truth and has to be verified, but in these investigations the onus is on eliminating the site from a potential inquiry and the methodology differs accordingly. These two broad types constitute the majority of scenarios. It could be argued that the methods for determining that a burial is not there are not necessarily the same as those implemented for proving that it is there. The importance of the archaeological pedigree in forensic search, and in forensic geophysics in particular, is simply that the requirements of archaeology bear much closer resemblance to those of operational taphonomic phenomena, etc. Many of us would also like to see a situation in which some practitioners are able to operate in a manner that is more than a hurried addition to their own livelihoods and careers. Highest on the list, however, is the need to fund, coordinate and develop the discipline to a level of more universal respectability, not just in the United Kingdom but also throughout Europe. Forensic archaeology, a victim of structure and perception, still has a long, long way to go.

References Cox, M. 1995 Crime scene archaeology is one of the most frightening areas of archaeology in which to operate, The Field Archaeologist 23:14–16. 1998

Criminal concerns: a plethora of forensic archaeologists, The Archaeologist 33:21–22.

Haglund, W.D. and M.H. Sorg, Editors 1997 Forensic Taphonomy: The Postmortem Fate of Human Remains, CRC Press, Boca Raton, FL. Henneberg, M. 1999 Forensic Evidence of Torture: Investigations into Human Rights Violations, unpublished M.Phil. thesis, University of Birmingham.

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Hunter, J.R. 1994 Forensic archaeology in Britain, Antiquity 68:758–69. 1999 The excavation of modern murder. In The Loved Body’s Corruption: Archaeological Contributions to the Study of Human Mortality, edited by J. Downes and T. Pollard, pp. 209–223. Cruithne Press, Glasgow. Mant, A.K. 1987 Knowledge acquired from post-war exhumations. In Death, Decay and Reconstruction: Approaches to Archaeology and Forensic Science, edited by A. Boddington, A.N. Garland, and R.C. Janaway, pp. 65–78. Manchester University Press, Manchester, U.K. Sigler Eisenberg, B. 1985 Forensic research: expanding the concept of applied archaeology, American Antiquity 50(3):650–655.

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Section 1

Theoretical Perspectives

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Advancing Forensic Taphonomy: Purpose, Theory, and Process MARCELLA H. SORG WILLIAM D. HAGLUND

1

Contents Background Conceptual Framework of Forensic Taphonomy The Unit of Analysis Taphonomic Time and Context A Brief History of Taphonomic Data Collection in Forensic Anthropology The Perimortem Problem Humans Are Taphonomic Agents Building Models and Data Sets Taphonomic Observations and Terminology Biogeographic Context Bogs and Aquatic Contexts Mass Fatalities and Mass Graves Mass Graves and Human Rights Scattered or Commingled Remains Reconstructing Taphonomic Context vs. Taphonomic History of the Remains Ethics and Standards of Practice Recommended Forensic Taphonomy Report Protocol Broader Professional Issues References

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Background Since work began on the first volume Forensic Taphonomy in 1993 (Haglund and Sorg, 1997a), traditional taphonomy and forensic research has undergone significant change. Additionally, despite the wide range of topics covered in the first volume, there remained significant topics not covered and those that should be covered in more depth. This volume attempts to extend coverage to include recent advances in the allied taphonomic and forensic fields as well as to explore a number of topics more fully or from a different perspective. The continuing effort is to articulate the interface among the paleontological, archaeological, and forensic sciences, placing it under one interdisciplinary umbrella (Haglund, 1991; Haglund and Sorg, 1997b,c). In many ways forensic taphonomy contrasts with and complements paleotaphonomy. Martin (1999) describes the purview of paleotaphonomy as an environmental and historical science, along with paleontology and geology. He argues that it is this very long timescale that is uniquely valuable in terms of its suitability for studying global environmental problems. With this long, time-averaged view, “The surface mixed layer or taphonomically active zone (TAZ) of sediment acts as a low pass filter, primarily through bioturbation and dissolution, that dumps high frequency signals before their incorporation into the historical record… (and) short-term noise is damped” (Martin, 1999b:vii). In fact, forensic taphonomy has just the opposite focus on the recent time frame (including the TAZ so contaminated by bioturbation) and particularly upon the anthropogenic ‘noise’ that Martin would seek to silence. In our own evaluation of the first volume, we felt that, although we had brought many disparate topics together and had focused a taphonomic perspective on forensic work, there were shortcomings that we continue to face. The relevance of forensic case material and research to paleontology and archaeology needs to be demonstrated. More effort needs to be given to a systematic approach to forensic recovery and interpretation which incorporates archaeological methods, and some attention needs to be focused on understanding (and precisely describing) the early decomposition process and its consequences for diagenesis and paleontological or archaeological interpretation. In this volume, we have chosen an explicitly bioenvironmental and idioecological approach. By bioenvironmental, we mean the incorporation of biological and environmental data using interpretive frameworks, models, and theory from allied disciplines. By idioecological, we mean the explicit focus on the idiosyncratic synchronic and diachronic (so-called context-specific) features of the case microenvironment, including the ecology and the particular historic sequence of taphonomic events. This is not new within archaeology and paleontology (Donovan, 1991; Gifford-Gonzolez, 1981; Haynes, 1980; Klein and Cruz-Uribe, 1984; Lyman, 1994; Martin, 1999a; Morse et al., 1983; Schafer, 1972; Shipman, 1981; Voorhies, 1969). But forensic efforts suffer from either too narrow disciplinary efforts or, conversely, models that are too general to offer much explanatory value for forensic practice. There is much progress to be made along these lines; this is only a beginning. The practice of forensic taphonomy is often an international endeavor. Although our closest connections have been with the Canada and the United Kingdom, recent work with mass fatalities, mass graves, and human rights offenses has involved problems worldwide with international teams of pathologists, archaeologists, and physical anthropologists (Haglund et al., 2001; Scott, 2001; Stover and Ryan, 2001). In fact, anthropologists have had to come to terms with human rights issues that rise to a level that dwarfs cultural

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relativism (An-Naím, 1992; Cohen, 1989; Fluehr-Lobban, 1995; Messer, 1993; Washburn, 1987). It is our purpose to increase visibility and understanding of the emerging issues, not only in terms of taphonomy and site interpretation, but also of variations across cultures and nations in how forensic taphonomy is practiced and how professionals are qualified (see, for example, Steyn and Meiring, 1997). To that end we have devoted a major section of the book to these topics.

Conceptual Framework of Forensic Taphonomy The Unit of Analysis From both taphonomic and ecological perspectives, the carcass can be considered the centerpiece of a newly emerging microenvironment (Kormondy and Brown, 1998; Krebs, 1994). It provides a serendipitous food source, setting off a complex set of trophic phases of consumption, decomposition, assimilation, and dispersal (Haglund, 1988a; Haynes, 1982; Hill, 1979; Mann et al., 1990). It also initiates particular changes in the chemistry and temperature of the immediate surroundings (Coe, 1978). Many of these changes are themselves catalytic, initiating or facilitating further processes. These processes are dependent on whatever unique patterns or sequences characterized the environment prior to deposition of the body: local features of the biosphere, lithosphere, and atmosphere (Behrensmeyer and Hill, 1980; Lyman, 1994). These factors continually interact and impact whatever taphonomic activity is occurring, having a differential effect depending on their own cycles of variation (e.g., ecological community, geological processes, weather/season), the interplay of those cycles, and the phases of decomposition of the index set of remains. As time passes and the body decomposes (in many outdoor settings), body and context tend to merge. The boundaries of the body diverge as decomposing materials penetrate the ground, are carried away by moving water, are digested by insect, mammalian, crustacean, or fish scavengers, or are volatilized to the air or water. Likewise, the environment penetrates the body as minerals from groundwater or sediment are incorporated into bone, plant roots and soil microbes penetrate soft tissue and bone, and sediment accumulates to surround and potentially bury the body. The particular decomposing human body becomes our unit of analysis at some point in its postmortem processes (Table 1.1). This is an extremely arbitrary aspect of taphonomic analysis, i.e., that this particular decomposing organism should be singled out for our analytical attention from the myriad other organisms whose remains are currently present and also decomposing at a given location. This bias persists as we select pertinent models for understanding the index organism. The shorter postmortem timeframe of a forensic taphonomy investigation (compared with traditional paleotaphonomy) dictates that particular attention be paid to data accumulating from periodic changes (e.g., seasonal, diurnal) with a cycle wavelength shorter than the postmortem interval (Martin, 1999); these data constitute the relevant diachronic context. All other data can be grouped as the background, the synchronic context, for the purpose of a particular analysis. Diachronic context data about other currently operating biotic process in the microenvironment, i.e., processes with a relevant periodicity (e.g., necrophagous insect succession associated with the body under consideration) provide useable taphonomic data. But diachronic data at the macroenvironmental level, such as faunal extinctions, probably

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Table 1.1

Environmental Frameworks and Relevant Contexts

Macroenvironment [Synchronic Context]

Macroenvironment Periodicity, within the Postmortem Interval [Diachronic Context]

Microenvironment, Site Specific, at the Point of Recovery (Actual) or Point of Death (Reconstructed) [Synchronic Context]

Microenvironment Periodicity, Site Specific, within the Postmortem Interval [Diachronic Context]

Atmosphere

• Point within longterm climate change cycles

• Current temperature • Current precipitation • Current distribution of water • Oxygenation

• Accumulated degree days • Precipitation pattern

Lithosphere

• Point within longterm geological change, such as continental drift, rising sea levels

• • • • •

Surface relief, terrain Minerals present Salinity Alkalinity Water vs. land distribution • Soil type

• Recent changes in landscape • Seasonal changes in landscape at that location

Biosphere

• Point within longterm faunal and floral changes, extinctions

• Producer, consumer, and decomposer presence • Primary productivity • Scavenger home ranges and territories

• Seasonal changes in plant and animal presence, activity • Necrophagous insect succession • Necrotic bacteria and fungal succession • Nitrogen cycle associated with remains

would not. Thus, the necessary interdisciplinary mix, the relevant biological models, and the data collection methods will differ somewhat between paleo- and forensic taphonomy, and will depend on the problem to be solved and the postmortem interval involved. Taphonomic data may provide clues to an ancient environment or may be extraneous or artifactual to the temporal or topical research focus (see Lyman Foreword, this volume). Nevertheless, as the body makes its way from the biosphere to the lithosphere, both earlier and later diachronic data are potentially relevant no matter whether the postmortem interval is centuries or days. The consequences of local scavenger activity, for example, or deposition during a dry spell, or flash flood, while the remains are still articulated, or while the skeleton is still fresh, or some other set of variables, will theoretically affect any subsequent analysis. The time during which soft tissue persists is a critical period taphonomically. The probability is enhanced for a wide range of dramatic alterations prior to decomposition, consumption, or preservation by, e.g., mummification, freezing, or adipocere formation (Haglund and Sorg, 1997a; Micozzi, 1991). The speed and attendant consequences of the taphonomic processes are great during this early period. From a forensic point of view, correct interpretation of the events surrounding a death is dependent on knowing both the sequence and character of the taphonomic processes.

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Taphonomic artifact may need to be stripped away to reveal forensic information, e.g., to discriminate scavenger modification from perimortem trauma. Conversely, taphonomic data may itself constitute forensic evidence, e.g., of the original place of death and transport, the behavior of the perpetrator (humans may be taphonomic agents), or the postmortem interval (cf. Lyman, 1994; Foreword this volume). No longer is skeletal morphology the only primary data derived directly from the skeleton itself. DNA extraction and analysis have rapidly risen to assume a partnership role, even when remains are decomposed or skeletonized. Harvey and King (Chapter 24, this volume) provide an update on DNA techniques along with a number of case examples. The body’s interface with its surroundings is not entirely discrete; it does not stop at the skeleton or the skin. Cells are lost constantly to the environment; some sources estimate thousands of dead or dying skin cells are lost each minute by a living individual. As our technical capacity increases, these tiny data sources will increase as well. Olfactory cues are used in forensic work (Hunt, 1999; Rebmann et al., 2000; Sorg et al., 1998) and may be a future potential source of taphonomic data. It is known that olfactory cues attract scavengers, including insects (see Hall, 1995); thus olfaction is an important aspect of scavenger patterning. As more is learned about decomposition, chemical signatures (Voss et al., 1992) and bacterial signatures (Pfeiffer et al., 1998) may become more important. Taphonomic Time and Context From the point of view of the forensic investigator, there are at least three events in taphonomic time: (1) the time of death; (2) the time of deposition in the recovery location; and (3) the time of recovery. But usually these events are not chronologically precise or even discoverable as actual points in time. Viewed in a more processual way, the taphonomic reconstruction is concerned with the ecological, biological, and physical context and processes impacting a particular set of remains during four temporal contexts: (1) the antemortem taphonomic period just prior to death and/or deposition; (2) the perimortem taphonomic period around the time of death and deposition; (3) the postmortem taphonomic period from deposition to recovery; and (4) the postrecovery taphonomic period from recovery to analysis. In some cases, there is also an archival period following analysis. Additionally, there may be a multiple, sequential taphonomic contexts due to transport or sequential modification agents. We have added the qualifier taphonomic to the temporal context designations for several reasons. First, the taphonomic perspective differs, although not completely, from the traditional medical usage, which generally focuses on fleshed remains with a rather short postmortem interval and on chronological reconstructions. Taphonomic time is a form of the archaeological concept relative time as opposed to time expressed in hours, days, and years, i.e., chronological time. It may be expressed as a function of the condition of the remains, for example, a stage of decomposition or stage of disarticulation. In medical parlance antemortem (sensu stricto, before death) can refer to the entirety of an individual’s biological and medical history prior to the relatively precise moment of brain death (see also Symes et al., Chapter 21, this volume), although it is usually used more narrowly. Perimortem generally refers to a fairly narrow time interval encompassing the death event. By contrast, the antemortem taphonomic period is characterized by the condition of the organism just prior to death (location, position, covering, size, shape, stage of development, presence of non-fatal wounding), inferred from or based on characteristics

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that can be discovered at recovery or analysis. The perimortem taphonomic period is not an actual time period, but a designation that infers the investigator’s inability to discriminate ante- and postmortem modifications, i.e., the remains have characteristics of being antemortem, but could possibly also be early postmortem. These determinations cannot be based on vital/non-vital reactions but rather must be based on biochemical and/or biomechanical conditions that are only indirectly related to the passage of time. Thus, to the extent that remains are decomposed, fragmented, or skeletonized, taphonomic time designations (of wounding, for example) usually cannot be precise à propos the medically defined moment of death. By way of illustration, impacts upon living or freshly postmortem long bone shafts tend to create defects that are curvilinear or spiraled, so long as the bone tissue retains sufficient fat and moisture; these are related to the taphonomic perimortem period. Such fractures might have happened while the person was living, but died before healing took place, or they might have happened after death, while the bone was still behaving biomechanically as if it were fresh. The same impacts applied to more decomposed or dried bone tissue tend to be more rectilinear, may be frayed, or may expose unstained fracture margins; these occur in the taphonomic postmortem period. Similarly, concepts and terms of taphonomic time may be applied to the scene or deposition site. This is conceptually useful in understanding and reconstructing the microenvironment that comes to house the remains, and in differentiating agents of modification. Predepositional period refers to the nature of the microenvironment just prior to deposition of the remains. Depositional period refers to the time in which alterations in the microenvironment were connected with the depositional event. Postdepositional period comprises the time after deposition and before recovery and refers to the characteristics and changes in the microenvironment due to the presence of the remains. Recovery period is the time during which the remains identifiable as such are removed from the context. Postrecovery period is the time following removal of the remains and refers to changes in the microenvironment due to removal of the remains. Table 1.1 outlines these taphonomic periods with respect to the data sets and analytical foci potentially involved in handling a forensic case. The efforts itemized in individual cells may, however, be combined, abbreviated, or eliminated altogether depending on unique aspects of the case, budget, and time constraints. For conceptual clarity, a generic and simple forensic model is used to create Table 1.2: a homicide at one location and transported to a single outdoor deposition site where the remains are deposited and ultimately recovered. It assumes that both the death and the deposition at the place recovered occur in the perimortem time frame; obviously, this is not always so. Additionally, it assumes that recovery is done at the place of deposition; in reality, remains are sometimes moved more than once in the postmortem period. A Brief History of Taphonomic Data Collection in Forensic Anthropology Early comments regarding taphonomic data-gathering by physical anthropologists in forensic investigations are found in Krogman (1962:7) when discussing estimation of time since death, although he does not use the term taphonomy: The problem of time-elapse since death is so complex that I’m not attempting to tackle it in this book. There are often too many unknowns, not the least of which may be careless or inexperienced exhumation. The soil may tell of primary or secondary inhumation; it

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Table 1.2 Taphonomic Time Periods, Analytical Foci, and Datasets for an Exemplar Homicide Victim Transported after Death to an Outdoor Site and Recovered after Skeletonization and Significant Weathering of the Remains Analytical Foci Reconstruction of Taphonomic Context: (Sequences, and Nonhuman Taphonomic Agents)

Taphonomic Periods Being Reconstructed Scene: Predepositional

Context prior to arrival of human remains (learned through research):

Remains: Antemortem

• • • •

Scene: Depositional

Context at the time of deposition (inferred or extrapolated):

Remains: Perimortem

• Time of day • Season • Presence of scavenger species

Scene: Postdepositional

Context changes between deposition and recovery (inferred or extrapolated):

Remains: Postmortem

• Effect of remains on environment • Taphonomic agents of modification, both the processes and sequences

Scene: Postrecovery

Context at time of recovery (observed): • Ecological characteristics • Evidence of scavenger species

Remains: Postrecovery

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Geological Biological Ecological Climatological

Reconstruction of Taphonomic Events: (Particularly Human Perpetrator as Taphonomic Agent) Events leading up to deposition (due to human as taphonomic agent): • Antemortem trauma (with vital response) • Trace evidence connected with a previous location or with perpetrator identity • Human as taphonomic transport agent

Reconstruction of Victim Discriminate taphonomic changes from indicators of: • Antemortem history • Biological profile • Individual identity

Events at the time of deposition:

Identify modifications which suggest:

• Perimortem trauma • Postmortem modification of remains by perpetrator • Trace evidence of trauma (e.g., weapon) or deposition process (e.g., shovel marks)

• Cause of death • Manner of death

Events after deposition and before recovery: • Intentional postdepositional disturbance by perpetrator or other humans • Accidental disturbance by humans • Modifications or transport by humans at the time of discovery

Analyze condition of remains to indicate:

Events following recovery: • Modifications due to recovery, examination, or storage

Document process of data collection to ensure: • Associations at the scene • Chain of custody

• Postmortem interval • Transport history • Postmortem modification by nonhuman agents • Postmortem modification by humans at recovery or at autopsy

may yield chemical (acid or base) evidence of rate of decomposition; it may tell of flora and fauna (vegetation and insect action); it may tell of the mechanical factors of movement of [sic] water-seepage (a homogeneous tightly-packed soil as in clays or glacial tills, or a heterogeneous soil as in gravels); depth of interment is very important; the swing of seasons and the amplitude of temperature change play their roles (in water deaths temperature and factors of stasis vs. current-movement are basic). The bones themselves give an idea of time-elapse in the presence or absence of ligamentous attachments and the rates of leaching out of fats and other organic content; surface erosions on bones are important, as well as changes in inner architecture (changes in cancellous tissue, in trabeculation seen radiographically). I don’t think the physical anthropologist should tackle cause of death.

Although they do not address taphonomic issues in any systematic fashion, El-Najjar and McWilliams (1978) do recommend graves be excavated by an archaeologist with a physical anthropologist there to excavate the remains themselves.* We underscore the value. El-Najjar and McWilliams also propose a standard narrative report format (1978:9–11) to be used by the physical anthropologist in forensic investigations. Included in the format is a section for Condition in which patterns of decomposition are described. In a section proposed for Time of Death, they discuss the necessity of knowing circumstances of deposition, and their sample report mentions scavenger modification. The report format also includes sections for Trauma and one for Death in which possible evidence of the cause of death is discussed. Stewart (1981) agrees that the physical anthropologist should assess evidence of the cause of death, i.e., the presence of trauma. He also devotes an entire chapter to “Judging Time and Cause of Death,” and proposes a list of attributes regarding time of death to be scored, he says, as present or absent: (1) odor, and its intensity; (2) soft parts, and their location; (3) adherent earth (clay, loam, or sand); (4) adherent vegetation (twigs, leaves, grass, or moss); (5) adherent insects, living or dead, including immature stages; (6) tooth marks; (7) stains and/or bleaching; and (8) adipocere. In the subsequent pages he devotes complete sections to necrophagous insects, minimum time of skeltonization, varying frequency of carnivores, shielded remains, adipocere formation, effect of a shallow burial, residual bone nitrogen, root penetration, and staining and bleaching. Stewart (1981:74) provides strong cautions against estimating time of death on the basis of skeletal appearance, citing the possible fresh appearance of long but deeply buried bone. He notes that the skeletons from the Korean war recovered “from the shallow graves of the American soldiers who had been held for varying lengths of time in prisoner-ofwar camps were virtually indistinguishable in appearance from prehistoric skeletons recovered archeologically; that is, they gave little if any visible evidence of containing organic matter and were beginning to show breakdown of the cortical surfaces.” Buikstra and Ubelaker (1994) include a chapter “Postmortem Changes: Human Taphonomy” in their handbook of data collection standards for human skeletons. This contribution systematizes observations of archaeological bone with regard to basic alterations of color, surface, and shape. They recommend routinely collecting data on weathering, discoloration, polish, cutmarks, evidence of rodent and carnivore gnawing, and * This issue has been a topic of conversation in recent meetings of the American Academy of Forensic Science, Physical Anthropology Section, and is a theme in a special, upcoming volume of the Historical Archaeology (Crist, 2001; Haglund, 2001; Haglund et al., 2001; Owsley, 2001; Scott and Connor, 2001; Stover and Ryan, 2001).

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other forms of cultural modification including creation of artifacts. These characteristics are also applicable in forensic taphonomy. In contrast to our approach here, Buikstra and Ubelaker place “premortem and perimortem fractures, wounds, and abrasions” (p. 106) in the chapter on paleopathology, thus separating perimortem trauma from taphonomy. However, cutmarks and burning remain in the taphonomy chapter because they are assumed to be connected with mortuary ritual. The taphonomic data collection protocols recommended in Buikstra and Ubelaker (1994) are fairly straightforward. All modifications are noted with the element and location. Munsell Color Charts are to be used for color observations; they offer a nominal scale for surface texture of burned bone. Weathering changes are to be recorded using Behrensmeyer’s (1978) categories. Other taphonomic changes (rodent gnawing, carnivore chewing, artifact creation) are recorded with drawings and/or photographs. Cutmarks are described by the number, length (mean and range), and a cast of a representative example (optional). The Perimortem Problem Forensic reconstructions frequently focus on discriminating trauma that occurred at or immediately prior to the time of death (and which, therefore, provide evidence about cause and manner of death) from those occurring after that. But the definition of death is a medicolegal one, based on medical soft tissue observations of the absence of heart and brain activity. Aside from the vital reaction of bleeding or bone remodeling with healing, we have no proxy for demonstrating that a traumatic event preceded death. The morphology of perimortem wounding to bone cannot, by that alone, be differentiated from postmortem damage to fresh or nearly fresh bone. As mentioned above, during the early postmortem period, before bone loses its moisture and organic components, it tends to respond to modification agents as if it were fresh. However, these patterns are not invariable or always diagnostic. The loss of organics and water is gradual and dependent on the microenvironment. As bone elements are exposed to their surroundings, their composition changes. There may be staining of outer layers, or weathering, or mineral uptake/loss into soil or water. Once bone surface color is altered, or significant weathering has occurred, it becomes easier to differentiate perimortem from postmortem modifications, as the latter will tend to disrupt the outer layer and expose unstained or unweathered bone. Certainly, more research is needed to establish descriptive standards of bone condition using chemical and physical properties in addition to visual characteristics to measure ‘freshness’. Sauer (1998) has offered a brief protocol for assessing the timing of a particular element or defect. Humans Are Taphonomic Agents One topic that has been an important issue in both forensic and archaeological investigation is that of humans as modifiers of remains, human or nonhuman. We believe the identification of common patterns of human modification of humans, whether due to homicide, dismemberment, warfare, scavenging, cannibalism, or burial ritual, should be included as an essential dimension of taphonomy. The differentiation of human from other agents causing long bone breakage has been debated for early hominid sites, in the controversy surrounding the peopling of the Americas (Bonnichsen and Sorg, 1987), and with respect to cannibalism (Graver et al., Chapter 16, this volume; Turner and Turner, 1999; White, 1992).

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A key concept here is the equifinality of some taphonomic processes (Bunn, 1991), i.e., more than one agent producing the same or similar taphonomic signature. Is it possible, for example, to identify diagnostic features or signatures of particular taphonomic agents (e.g., see Haglund et al. (1988a,b) regarding canids)? In a useful review of literature, Bunn points to the need for more research, but comments on the importance of looking at complete patterns, and in context, as well as the importance (echoed by many others) of microscopic observation. He particularly notes the need for more research on cutmarks, bone fracture biomechanics, carnivore modification patterns, faunal ecology, and actualistic studies of site formation. During the last decade these topics have indeed received more attention. Not only is human agency an issue, but the discrimination of peri- and postmortem can become the key issue in identifying human agency. Diez et al. (1999) describe the Atapuerca site in Spain, which dates to the Lower and Middle Pleistocene. They conclude that the array of butchered mammalian food includes humans, and they group humans with other mammals of similar weight. They list characteristics of the butchered bones, focusing on the identification of perimortem defects. The butchered remains are highly fragmented with few elements intact apart from teeth and articular bones. The fragments have a mixed representation of right-angled breaks (attributed to diagenesis) and oblique breaks (interpreted as perimortem). They note “curved, V-shaped fractures” as a “good discriminatory trait between fresh and old fractures” (1999:631). They find that smooth fracture edges, proposed by many as a characteristic of fresh breaks, do not discriminate; these are attributed more to a dynamic (vs. static) force impacting the bone. Jagged edges, they assert, are more likely related to the porosity due to loss of organic matter, low crystallinity, and non-mineralized tissue. Smooth edges are related to “compact structures, such as green bones with organic material still preserved in the Haversian and osteon canals, or fossil bones where mineralization and crystallization have occurred in the Haversian and osteon canals” (1999:631–632). They comment that a high frequency of bone fragments in which bone circumference is only half represented is more characteristic of scavenging or butchering; many complete shaft diameters, on the other hand, more likely represent postdepositional breaks. They also include observations of surface modifications related to fracture by humans, including impact points, flakes or notched fractures (conchoidal scars), commenting that most have associated hackle and rib marks which characterize green bone breaks according to Johnson (1985). Finally, they identify and extensively describe the cutmarks differentiating sawing from scraping, as well as skinning, viscera/periosteum extraction, dismembering, and filleting. Human agency is critical in the resolution of human rights abuses, including mass fatalities or mass burials as addressed by many in this volume. Haglund provides a conceptual framework for mass graves and Schmitt discusses some of the taphonomic implications of human rights abuses. Skinner addresses a frequently overlooked human taphonomic activity, postmortem alteration of burials, sometimes long after the original event. In a parallel, but prehistorically focused, analysis, Darwent and Lyman address the discrimination of postdepositional modification of nonhuman bones (limited to small, dense tarsals, carpals, and phalanges). Darwent and Lyman seek to quantify the rather complex relationships among shape, size, food value, and diagenesis pertaining to these selected elements. They test hypotheses proposed by Marean regarding the detection of postdepositional damage using small, dense faunal remains which are less likely to be broken (see discussion below), as opposed to the patterns of human food utilization patterns.

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Of course, modern forensic cases incorporate a varied array of human tool use, and tend to include relatively deviant behaviors. The forensic research is perhaps the clearest record of human conspecific predation. Symes et al. (Chapter 21, this volume) focus attention on several cases illustrating particular types of sharp trauma from tools. And Saul and Saul demonstrate the use of very small or subtle modifications to identify sharp trauma evidence. A parallel archaeological study described the patterning of ritual Mayan decapitation. The differentiation of human-induced trauma from nonhuman predation or scavenging is based on familiarity with taxon-specific patterns of bone and soft tissue modification. Berryman (Chapter 25, this volume), for example, provides an unusual case of pig scavenging of human remains, documenting and illustrating the modifications due to dental morphology, mastication, and feeding patterns (see also, Kerbis et al., 1993, for examples involving chimpanzee remains). Taxon-specific patterns have been shown to have a large range of variability, however (Saavedra and Simonetti, 1998), and much more research needs to be done to document and analyze such signatures. In an important example of the potential crossover between forensic and archaeological research, Gargett (1999) addresses the issue of identifying human agency in buried human remains (intentional burials), particularly for a number of so-called Middle Palaeoloithic burials. He concerns himself with the decomposition process, citing research by Haglund (1997), Micozzi (1997), and Galloway (1989), discussing the possible impact of decomposition sequence, rigor mortis, and rapid drying on evaluating burial position. The issue for these archaeological sites is whether burial (e.g., due to rapid sedimentation or cave roof falls) might occur prior to decomposition and disarticulation, thus imitating intentional burial. Another issue is the extent of disarticulation. For this author bones can remain “articulated”* following loss of flesh, assuming burial protects them from movement; it is important, therefore, to assess how close they are (at recovery) to anatomical position. He suggests focusing on three key processes: decomposition, disarticulation, and likelihood of disturbance. Gargett concludes with a set of factors to assess in evaluating whether a burial was purposeful; these include stratification, completeness of remains, articulation pattern, unequal preservation of parts, peri- vs. postmortem fragmentation patterns, position of remains, evidence of disturbance, characteristics of associated bedrock or cave, sedimentation pattern, and evidence of bioturbation. A related debate about human agency is going on regarding the Klasies River Mouth site in South Africa, dating to the Last Interglacial. These hominids are anatomically nearmodern, but did not use Upper Paleolithic tools. The question regarding their associated faunal remains is whether the hominids had hunted them or merely scavenged them, and much of the debate centers on which body parts are represented (scavenging should result in disproportionately more limb bones) (Binford, 1984; Blumenschine, 1986). Milo (1998) uses a wide range of analytical techniques to evaluate the array of faunal bones and the butchering marks, including assessment of minimum numbers, large carnivore scavenging signatures, and experimental butchering. In research very much applicable to the types of case studies in Symes et al., (Chapter 21, this volume) he outlines the morphology of cuts vs. stabs, the absolute necessity of microscopic examination (only 32% of marks he made in his experiments were macroscopically visible on fresh bone), and the mediation by * The terms disarticulation and articulation will be discussed more fully in the section Taphonomic Observations and Terminology.

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postdepositional deterioration (he estimates 30% of marks become undetectable). The conclusion is that the hominids were hunting, not scavenging. In a related article about this site, Bartram and Marean (1999) examine the importance of recovering, identifying, and analyzing midshaft bone fragments in the differentiation of hunting and scavenging. They also discuss the ongoing debate in archaezoological and taphonomic research regarding the applicability of actualistic studies and uniformatarian theory. Their conclusion, aided by ethnographic examples, is that scavengers raid human sites after hunted animal bones have been processed for marrow (with heavy fragmentation of midshafts), differentially removing the epiphyseal portions. Bias is introduced when archaeozoologists subsequently exclude these midshaft fragments from their analysis because they are coded as nonidentifiable during the analysis. Building Models and Data Sets Experimental taphonomic research, also called actualistic research, is an important common ground between traditional, paleontological taphonomy and forensic taphonomy (Gifford-Gonzolez, 1981). In actualistic experiments a particular taphonomic process is the focus for model building; key independent variables are controlled, and observation of the dependent variables can be systematized, e.g., the now-classic studies of fluvial transport of human remains in the paleoanthropological literature (Behrensmeyer, 1982; Boaz and Behrensmeyer, 1976; Hanson, 1980) or of the decomposition process by human cadavers in the forensic literature (Bass, 1984, 1997). In other actualistic approaches, the investigator studies a process seen in the fossil (or forensic) record by observing the same process in a natural setting, e.g., the studies of mammalian scavenging in the archaeological literature (Haynes, 1980, 1982; Brain, 1981; Hill, 1979). The forensic counterpart of these studies is the systematic analysis of a series of cases that bear certain structural similarities, such as the study of cases of canid scavenging of human remains by Haglund et al. (1988a,b) in order to construct a stage model of this process, or the study of cases of terrestrial decomposition (Galloway, 1997; Rhine and Dawson, 1998; Sorg et al., 1998) or marine decomposition (Boyle et al., 1997; Haglund, 1993; Sorg et al., 1997) in order to model the decomposition process regionally. The control in these case series is that time since death is known and a single investigator with a consistent and systematic approach to his or her cases is present. Data collection must be comparable across cases and, ideally, the data themselves are reported as part of the presentation of the model, enhancing the opportunity of replication or comparison by other scientists. A third type of actualistic research is the case study. Although some forensic cases are never solved with respect to victim identity, time, or cause and manner of death, many are. Thus, investigators have a luxury (or challenge) not afforded to colleagues doing traditional archaeology or paleontology: to learn whether hypotheses about the case were correct. That is, inferences and estimates proposed in the analysis are tested as further details of the case are revealed. It is this aspect of forensic taphonomy that offers a new type of data to the field of taphonomy generally. The variables are not under investigator control, as they are in experimental design or even systematic naturalistic observation. Case studies offer the opportunity to enrich explanation through enhanced observation and analysis, particularly in terms of learning about the range of variation. In Symes et al. (Chapter 21, this volume) two of the cases presented include confessional statements

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by perpetrators describing the sharp force trauma they used, corroborating the hypotheses of the investigators Forensic scientists have been constructing actualistic models of taphonomic change using nonhuman animal proxies for decades, with pigs being the most common choice due to their comparable mass, lack of fur, and availability (Anderson and Cervenka, Chapter 9, this volume; France et al., 1992, 1997; Haskell, 1989; Janaway, Chapter 20, this volume; Komar, 1999; Morton and Lord, Chapter 8, this volume; Payne, 1965; Payne and King, 1972). Others have done longitudinal studies with donated human cadavers under very controlled conditions (Bass, 1984, 1997; Rodriguez and Bass, 1985; Voss et al., 1992). A naturalistic study of rainforest taphonomy has recently been published utilizing the recovery of the remains of chimpanzees who died of natural causes, predation, or poaching (Peterhans et al., 1993). The purpose was to test the hypothesis that the primate fossil gap around the Pliocene might be due to the bone-destroying taphonomy of tropical forests. Chimpanzees are also potential models of human remains in forest settings. They conclude that some remains are undamaged even after several years, as long as the soil is not acid, permitting the accumulation of remains. Taphonomic Observations and Terminology The use of terms differs from one discipline to another. While a term may be well understood and functionally adequate, when it is applied in a new disciplinary context, its use may lead to misunderstanding or dwindle to meaninglessness. The lack of interdisciplinary term conventions may exacerbate misunderstanding, create error of assumption, and alter the inferences themselves. For example, the use of the terms articulated and disarticulated has different meanings when applied by forensic pathologists than by some forensic anthropologists. Articulation is the state of having parts connected by joints. The word is derived from the Latin term for joint: articulus. Variations of the definition of articulate are (1) to join together so as to allow motion between the parts, or (2) united by means of a joint, or (3) to make of parts united (Webster’s Collegiate Dictionary). With regard to anatomy specifically, an articulation is a place of union or junction between two or more bones of the skeleton (Dorland’s Illustrated Medical Dictionary). Contrarily, disarticulation is defined as the separation or amputation of a bone at a joint; to disarticulate is to become disjoined by flexible joints (Webster’s Collegiate Dictionary, Stedman’s Medical Dictionary). With these definitions in mind, the medical use of articulation is generally related to anatomical relationships or associations between bones maintained by soft tissue connections at joints. When soft tissue is absent at the joint, bones are in fact disarticulated, even though they remain in relative anatomical position. Occasionally, remains may actually be held in complete anatomical relationship by the soil matrix, but generally elements will have moved slightly out of position. Hence, the forensic pathologist describing a fully skeletonized remains, arrayed carefully in anatomical position (but not joined by soft tissue), would characterize such a skeleton as disarticulated and in anatomical relationship. This same set of skeletal remains might be described as articulated by some forensic anthropologists (Bass, 1962; Ubelaker, 1974, 1989; and numerous others), a usage connoting soft tissue presence with which we disagree. Such terminology confuses connectedness with relative anatomical relationship or approximation of bones at a joint. A more precise application

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would separate descriptions of anatomical relationship in situ from inferences of the condition of remains when buried. The foregoing misapplication of “articulation” has a range of consequences. First is the potential to introduce an erroneous assumption. When bones are connected at the joint by soft tissue, one can correctly assume they belong to a single individual. When bones rest in anatomical relationship, but are not physically connected, they may likely but not necessarily belong to the same individual (see Saul and Saul, Chapter 4, this volume). One must look to other contextual factors, such as the number of individuals and their relative positions. A second problem introduced by misapplying this or other terms is the potential loss of that term’s inferential power. For example, an important inference that can be drawn from the proper use of the term disarticulation is that the bone elements are now independent units, and are likely to be moved independently. This is of utmost significance in a taphonomic context, when dealing with issues of scavenged or otherwise transported remains. Transport units can be inferred to be (or to have been) joined and moved as a single entity, and therefore articulated. In Chapter 5, this volume, Roksandic pays particular attention to the interaction of decomposition processes and burial contexts. She builds on research by Duday (1978, 1981, 1987a,b and Duday et al. (1990) that considers types of articular anatomy, their behavior during the postmortem period when buried, and inferences regarding burial practices. She shows that with careful excavation in certain context types, one can infer the condition of the remains when buried. Saul and Saul explore the mutual benefits of archaeological and forensic case experience in differentiating taphonomic agents and contexts. In one archaeological case inferences about articulation become critical in the sorting of commingled remains.

Biogeographic Context To more fully understand issues, dynamics, and consequences of taphonomic processes, it is vital to collect higher resolution data on the ecological context from which individual cases are recovered. The goal of gathering these data, not generally part of forensic investigations, is to make forensic taphonomic research more systematic, comparative, and empirically based. This is a similar approach to that suggested by Potts (1998) in his treatment of an environmental hypothesis of hominin evolution. Conventionally, even when taphonomic issues are broached in the pursuit of death investigation data, environmental variables are poorly observed and little examined. The corpse becomes part of an ecological setting (see Behrensmeyer, 1975, and Behrensmeyer et al., 1979, for early examples linking paleoanthropology, taphonomy, and paleoecology), in some sense even creating a new ecological community delimited by physical and biotic parameters, and having a particular history. (Complications may be introduced if the place of death, place of deposition, and the place the modifications occurred are different.) For each location, questions must be asked about the emerging ecological community centered on the remains, and about the climatological, physical, and biological parameters that may have influenced the modification process. Then, based on a knowledge of generalized taphonomic processes combined with information about the specific location, decisions should be made concerning at what levels these should be documented (Haglund, 1998). Following these decisions regarding context, choices should be made about methods and approaches to data gathering and analysis of the

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remains themselves. This two-step process will lend power to the theory building that may result. For example, a variable as elemental as temperature, in routine death investigations, is usually documented by recording ambient atmospheric temperatures at the scene, including known maximum/minimum temperatures for the area along with seasonal and diurnal fluctuations. However, when considering putrefaction processes, air temperature is less important than temperatures on or near the surface. Coe (1978) pointed this out in his study of decomposition in elephant carcasses. In any local setting there are a host of temperature-driven microenvironments dependent on absorption of radiant energy. For a 3-day period, Coe found temperatures on open ground and scrub were between 25 and 28°C, but maximum surface open-ground temperature was 45 to 50°C in mid-afternoon. On rock surfaces, temperature approached 60°C, and for forest-shaded areas, the maximum surface temperature was only 28°C with a daily range of only 8°C. Among forensic entomologists, for example, the critical nature of temperature is already realized. Hence, more refined temperature observations are being demanded and more routinely made, increasing the resolution of their interpretations. In this volume, Anderson and Cervenka (Chapter 9) explore regional intra-species variation in the interpretation particularly of time since death for the Canadian northwest. Speciesspecific regional variation has been implicated in several taxas, including, for example, predation by owls (Fernandez-Janvo et al., 1999; Saavedra and Simonetti, 1998) and distribution of plant pollens (Horrocks et al., 1998). It is critical to take such potential variation into account by developing regional databases and comparing them. Marine settings offer an important testing ground for taphonomic studies. The literature on marine taphonomy is rich (Donovan, 1991; Martin, 1999; Parsons and Brett, 1991). Research on mollusks and foraminifera provides interesting models for the decomposition and dissolution of the (also calcium-based) human skeleton (Walker and Goldstein, 1999) within the Taphonomically Active Zone (TAZ) or bioturbation zone (Davies, et al., 1989). Walker and Goldstein (1999) propose a model for preservation of hardparts which may be applicable to skeletal remains. They comment that, for mollusks, time spent on the surface prior to burial is much more likely to drive the condition of the remains than is time since death. They have also concluded that burial may not be so much of a preservative as has been thought. They use a concept which may be useful in guiding recoveries in forensic settings: dominant taphonomic processes, which may be regionally specific, but discoverable, in terms of their applicability to common forensic problems. Bogs and Aquatic Contexts Human bodies have been recovered from an enormous variety of climatological, geographic, and physical contexts. Many forensic cases, with little archaeological comparison, are recovered from marine, riverine, or lacustrine environments. These cases tend to create considerable taphonomic difficulties due to the effects of extensive transport and/or the problems identifying and describing a meaningful, essentially 3-dimensional, taphonomic context. Haglund and Sorg provide in Chapter 10 in this volume a brief overview of taphonomic issues in aquatic settings. Ebbesmeyer and Haglund (Chapter 11) expand on particular circumstances and contextual issues: shipwrecks and ocean currents. In some contexts such as bogs, long-term preservation of human remains is possible. Brothwell and Gill-Robinson (Chapter 6) compare the condition and contexts of an impressive series of bodies found in bog settings. A number of these cases are suspicious

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deaths. The bog microenvironment is a highly acid, moist, and anaerobic environment with well-known characteristics. Yet the variation is remarkable.

Mass Fatalities and Mass Graves Mass Graves and Human Rights The reach of forensic inquiry and research has recently been extended in a prominent way beyond the purview of state and federal legal systems to international and pan-national contexts. That death investigations are done in international circumstances is certainly not new, but the explicit application of taphonomic approaches in these contexts is. In particular, this includes the exhumation and interpretation of traumatic deaths and mass graves due to war crimes and human rights violations, as well as the recovery of remains and the investigation of deaths in mass disasters. Haglund’s introduction (Chapter 12) in this volume to some of the terminology and conceptual issues regarding mass graves leads a series of chapters focused on case examples of larger-scale human death due to disasters and human rights abuses (see also, Burns, 1998). Simmons (Chapter 13) describes a cave context, comparing it to a similar karstic cave australopithecine site, and discusses the recovery and interpretation issues. Sledzik and Rodriquez (Chapter 17) discuss mass fatalities such as plane crashes and the effects of these events on remains: burning, fragmentation, and scattering, in particular, and the resulting taphonomic implications (see Lyman, 1987, for a faunal analysis of a mass disaster, the Mount St. Helens volcanic eruption). Schmitt (Chapter 14) focuses on some of the legal issues and the resulting taphonomic implications for search and recovery methods for clandestine graves. Skinner et al. (Chapter 15) review instances of postburial disturbance by humans, a problem that frequently impacts interpretations in these cases. Scattered or Commingled Remains Many taphonomic agents scatter remains. Some situations provide significant challenges for archaeological techniques and interpretation. Haglund et al. (Chapter 7) provide a discussion of plow-zone contexts and the recovery of human remains, describing modern equipment and its effects on buried remains. Ubelaker (Chapter 18), on the other hand, provides a comprehensive review of the types of issues that emerge in identifying and sorting commingled remains; he provides a literature review as well as case studies to illustrate several common situations. Reconstructing Taphonomic Context vs. Taphonomic History of the Remains One advantage of this interdisciplinary field is the possibility for independent observations of the same data sets by different investigators. This can become more important when considering the problem of analytical focus. On the one hand, the condition of the remains constitutes evidence for a particular taphonomic context. On the other hand, one needs to reconstruct the taphonomic history of the remains using data about the taphonomic context. To minimize circularity, it is best to focus first on the context, using the perspective of several disciplines if possible, then focus attention on the condition of the remains as dependent variables.

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Ethics and Standards of Practice Important ethical questions arise when the processes of forensic case investigation and data collection for research overlap, not only with regard to actualistic studies but also data collection incidental to case investigation. A delicate balance must be struck between potential benefit to the public and potential costs regarding how bodies are treated. The use of donated human bodies requires care and sensitivity. States, nations, and cultures differ in their tolerances, restrictions, and laws with regard to the treatment of human corpses for educational or research purposes. In most U.S. states, the collection and retention of any body part for study must be done only for legitimate inquiries in the case, unless the body has been donated for research. The use of nonhuman animal proxies also raises issues concerning humane treatment as well as levels of necessity for the research use. Since most forensic investigations are funded by public (governmental) or quasi-public (nonprofit organization) dollars, and since these investigations are by their nature conducted in a humanitarian or judicial role, resources are generally limited and investigator conduct is in the public domain. Regardless, the sensitive nature of the situation demands discretion. Thus, for example, resources must be appropriated on the basis of the needs of the particular case rather than any research agenda, minimizing damage to the body, and maximizing investigative potential. Nevertheless, investigatory quality (precision, thoroughness, accuracy, effectiveness) is enhanced by the use of basic standards and protocols, the use of which leads to routine collection of comparable sets of data (Buikstra and Ubelaker, 1994; Moore-Jansen et al., 1994). Whereas not all of these data may be seen as critical or even necessary in a particular case, the process of systematic coverage tends to reduce omissions and makes it more likely that data will be available in the event there are subsequent investigations. Although forensic taphonomy has emerged as a significant focus for research since our earlier efforts to link the two fields (Haglund, 1991; Haglund and Sorg, 1997a; Sorg, 1985), there is still much to do. The challenge continues in constructing well-documented series of cases, and in making the data available across investigators for comparative research. Additionally, we feel it is time for setting some standards in forensic taphonomic data collection, particularly for outdoor scenes, including systematic collection of minimal region-specific and site-specific, comparative information about temperature (current, nearest weather station, seasonality; see Anderson and Cervenka, Chapter 9, this volume), climate (particularly humidity and precipitation), soil, scavengers (mammalian, crustacean, avian, and arthropod), plants, and site history, as well as case-specific details about the condition of the remains and details of the deposition. Recommended Forensic Taphonomy Report Protocol Most forensic anthropologists use some variation of the report format recommended by ElNajjar and McWilliams (1978). During the last decade, however, the scope of practice has broadened somewhat to include scene visits and the recovery of remains, mass fatality incidents, and human rights investigations involving excavation. Although the use of archaeological techniques in forensic recoveries was pioneered much earlier (Brooks, 1975; Morse et al., 1983), it is only recently that anthropologists have been asked routinely to recover remains (Haglund, 1993; Reichs, 1998). This signals a broadening of the scope of practice for forensic anthropology in the United States to more closely resemble forensic archaeology practice in the United Kingdom (see Hunter’s Foreword, this volume). There has been a parallel

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Table 1.3

Updated Forensic Anthropology Report Format

Part 1: Introduction

• Background and chain of custody

Part 2: Taphonomy

• • • • •

Part 3: Biological Profile

Develop biological profile (individual and population characteristics) • Age • Sex • Stature • Discrete traits and anomalies (inherited and acquired) • Population ancestry • Pathology and evidence of medical history

Part 4: Individuation and Identification

• Combined pattern of anomalies, pathological conditions, or other traits known or documented for this individual • Compare remains and antemortem records of possible matches • Dental records • Radiographs • Medical history • Photographs • Facial imaging • DNA analysis

Part 5: Reconstruction of Death Event

• Trauma: types, location and patterning, trajectories, sequences, potential weapon classes • Document process of differentiating perimortem trauma from postmortem changes • Apply additional specialty analyses from other sources, e.g., tool marks, fracture biomechanics, trace evidence, histology, radiography

Document microenvironment at scene Document remains in situ Document recovery process Inventory remains Describe condition, including an assessment of taphonomic modifications due to transport, burial, decomposition, scavenging, weathering • Incorporate reports from other disciplines such as entomology, botany, and geology • Estimate postmortem interval

development of forensic taphonomy as a theoretical umbrella for interpreting postmortem processes in context. As a result, we recommend altering the basic forensic anthropology report format to include four parts, one of which focuses explicitly on taphonomy (see Table 1.3). Even when the formal report format must be abbreviated by request of the jurisdiction or function, the data collection and analysis that lie behind it should be thorough.

Broader Professional Issues The forensic sciences are a fast-evolving cluster of applied disciplines that operate independently as well as in interdisciplinary teams. As these forensic fields mature and develop, they expand to incorporate new methods and theories (often borrowed or adapted from

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allied fields) and contract to exclude outmoded ones. As a result, the boundaries between disciplines can become blurred and even changed. A distinction sometimes made in health care practice between the terms “interdisciplinary” and “multidisciplinary” highlights this complication. Multidisciplinary teams operate by applying multiple fields of learning to a problem in a parallel fashion, each discipline offering its own paradigm. Interdisciplinary teams operate by joining at the edges, often purposefully overlapping fields of knowledge and sharing competencies. The distinction between multidisciplinary and interdisciplinary is usually, however, not very clear in practice. The reality is that, at least within any group of allied fields, there is some shared knowledge or skills as a result of either common origins or shared experience. For example, many physical anthropologists have training and experience in archaeological techniques and many archaeologists have training and experience in the analysis of human remains. This is due to the structures in the United States, Canada, and elsewhere of degree-granting programs in anthropology. Yet these structures are not universal (either in the United States and Canada or internationally) and the auxiliary skills are not always present in a given individual. The consequence is that coverage of these competencies will differ for a particular jurisdiction or case. Similarly, training and skills in gathering forensic entomological evidence may be present in non-entomologists, and forensic entomologists may possess skills in excavation techniques. Nevertheless, the competencies for both archaeological techniques and forensic entomology data collection should be present within the team. The careful, 3-dimensional documentation of artifact provenience in a surface recovery or excavation of a clandestine burial is a skill and role often shared by criminalists, police, physical anthropologists, and occasionally medical examiner/coroners or death investigators, although it is probably best done by a forensic archaeologist. Thus, the case manager of a particular jurisdiction must evaluate both expertise and auxiliary competencies in team members. Budgets and circumstances limit both. It is not always possible to know, in advance, which knowledge bases will be critical for a particular case. First, in general and at a minimum, competencies for all basic areas of data collection should be represented on the team (for outdoor scenes in the northeast United States, for example, these would include scene context data, human remains collection, archaeological excavation or surface recovery, entomology, plant and fiber, DNA, and trace evidence). The development and maintenance of the knowledge base regarding data collection should be encouraged and ideally managed at an administrative level. Second, to the extent it is anticipated to be critical in a particular case, expertise (as opposed to just competence) should be present at the recovery and for the analysis. Teams comprised of individuals with basic competencies and frequently used expertise should be maintained and mobilizable. The bar has been raised in the United States during the last decade due to increased public awareness; unfortunately, budgets have not always followed. Forensic taphonomy, introduced within the past 15 years or so (Haglund et al., 1988a,b; Haglund, 1991; Haglund and Sorg, 1997; Micozzi, 1991; Sorg, 1985, 1986; Ubelaker, 1989), and mirroring paleotaphonomy, has been explicitly interdisciplinary. The result is increased ambiguity regarding professional or disciplinary roles. With its focus on postmortem changes and the incorporation of contextual data associated with human remains, forensic taphonomy embraces all disciplines charged with collecting and interpreting death and/or crime scene evidence. Competencies or skills in evidence collection and interpretation are partly shared, interdisciplinary, and may vary across jurisdictions according to expertise, local statutes, budgets, and customs.

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As in health care, procedural and knowledge-based skills in forensic sciences often cross-cut professional status, competence, certification, and/or licensure. Each jurisdiction is faced with the task of assembling a competent interdisciplinary team, utilizing the disciplines and skills (i.e., people) available for an often-limited set of resources. At another level, certification or licensing bodies are faced with continual pressures to evaluate incorporating more competencies or different types. Occasional turf battles are unavoidable. Potentially desirable consequences of the focus on interdisciplinary teams and shared competencies in forensic sciences include (paradoxically) a compensatory sharpening of professional distinctions through the adoption of certification processes and practice standards, lower (often public) cost of operation, or better articulation and clarification of the relationship between the knowledge base and the skills. Potentially undesirable consequences or costs include the weakening or extinction of certain disciplines, and/or the loss of quality. The challenge is to keep costs low and quality high. The value of taphonomic data is undeniable, but the cost of involving multiple disciplines is potentially high. A full range of taphonomic experts will normally not be on the staff. Pragmatic solutions will, we believe, include (1) cross-training of team members across disciplines in best practices for systematically collecting a multidisciplinary range of datasets; (2) avoiding attempts at cross-training or using less qualified persons for the interpretation of those data; (3) identifying within each jurisdiction one or more competent case managers or team leaders who can coordinate multidisciplinary data collections and make decisions about requesting expert consult for difficult data collections and for all interpretations; (4) cultivating a strong relationship with a basic team of experts, regularly requesting their interpretive input in both medium and high level cases (thus developing expertise for forensic applications through regular experience); (5) working in a team structure outside of the pressure of a particular case to set data collection standards and protocols for the group; and (6) encouraging team members to develop professional associations with forensic colleagues and to conduct research in their areas of expertise.

References An-Naím, A.A. 1992 Human Rights in Cross-Cultural Perspective: A Quest for Consensus, University of Pennsylvania Press, Philadelphia, PA. Bartram, L.E., Jr. and C.W. Marean 1999 Explaining the “Klasies Pattern”: Kua Ethnoarchaeology, the Die Kelders Middle Stone Age archaeofauna, long bone fragmentation and carnivore ravaging, Journal of Archaeological Science 26:9–29. Bass, W.M. 1962 The excavation of human skeletal remains. In Field Handbook on Human Skeleton, R.F. G. Spier, pp. 39–51. Missouri Archaeological Society, Colombia. 1984 Time interval since death. In Human Identification: Case Studies in Forensic Anthropology, edited by T.A. Rathbun and J.E. Buikstra, pp. 136–147. Charles C Thomas, Springfield, IL.

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1997 Outdoor decomposition rates in Tennessee. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp 181–186. CRC Press, Boca Raton, FL. Behrensmeyer, A.K. 1975 Taphonomy and paleoecology of the Plio-Pleistocene vertebrate assemblages east of Lake Rudolf, Kenya, Museum of Comparative Zoology Bulletin 146:473–578. 1978 Taphonomic and ecologic information from bone weathering, Paleobiology 4:150–162. 1982 Time resolution in fluvial vertebrate assemblages, Paleobiology 8:211–227. Behrensmeyer, A.K. and A. Hill 1980 Fossils in the Making: Vertebrate Taphonomy and Paleoecology, University of Chicago Press, Chicago, IL. Behrensmeyer, A.K. and S.M. Kidwell 1985 Taphonomy’s contributions to paleobiology, Paleobiology 11:105–119. Behrensmeyer, A.K., D. Western, and D. Dechant-Boaz 1979 New perspectives in vertebrate Paleoecology from a recent bone assemblage, Paleobiology 5:12–21. Binford, L. R. 1984 Faunal Remains from Klasies River Mouth, Academic Press, New York. Blumenschine, R.J. 1986 Carcass consumption and the archaeological distinction of scavenging and hunting, Journal of Human Evolution 15:639–59. Boaz, N.J. and A.K. Behrensmeyer 1976 Hominid taphonomy: Transport of human skeletal parts in an artificial fluvial environment, American Journal of Physical Anthropology 45:53–60. Bonnichsen, R. and M.H. Sorg 1987 Bone Modification, Center for the Study of the First Americans, Orono, ME. Boyle, S., A. Galloway, and R.T. Mason 1997 Human aquatic taphonomy in the Monterey Bay area. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 605–614. CRC Press, Boca Raton, FL. Brain, C.K 1981 The Hunters or the Hunted? An Introduction to African Cave Taphonomy, University of Chicago Press, Chicago, IL. Brooks, S.T. 1975 Human or not? A problem in skeletal identification, Journal of Forensic Sciences 20:149–153. Buikstra, J. and D. Ubelaker 1994 Standards for Data Collection from Human Skeletal Remains, Arkansas Archeological Survey Research Series No. 44. Bunn, H.T. 1991 A taphonomic perspective on the archaeology of human origins, Annual Review of Anthropology 20:433–467. Burns, K.R. 1998 Forensic anthropology and human rights issues. In Forensic Osteology: Advances in the Identification of Human Remains, 2nd edition, edited by K.J. Reichs, pp. 63–85. Charles C Thomas, Springfield, IL.

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Coe, M. 1978 The decomposition of elephant carcasses in the Tsavo (East) National Park, Kenya, Journal of the Arid Environments 1:71–86. Cohen, R. 1989 Human rights and cultural relativism: The need for a new approach, American Anthropologist 91:1014–1017. Connor, M. and D.D. Scott 2001 Paradigms and perpetrators, Historical Archaeology 35(1):1–6. Crist, T.A. 2001 Bad to the bone?: Historical archaeologists in the practice of forensic science, Historic Archaeology 35(1):39–56. Davies, D.J., F.N. Powell, and R.J. Stanton, Jr. 1989 Relative rates of shell dissolution and net sediment accumulation — a commentary: Can shell beds form by the gradual accumulation of biogenic debris on the sea floor? Lethaia 22:207–212. Diez, J.D., Y. Fernandez-Janvo, J. Rosell, and I. Caceres 1999 Zooarchaeology and taphonomy of Aurora Stratus (Gran Dolina, Sierra de Atapuerca, Spain), Journal of Human Evolution 37:623–652. Donovan, S.K. 1991 The Processes of Fossilization, Columbia University Press, New York. Duday, H. 1978 Archaeologie funeraire et anthroplogie, Cahiers d’Anthropologie, 1: 55–101. 1981 Le place de l’anthropologie dans l’etude des sepultures anciennes, Cahiers d’Anthropologie, (1):27–42. 1985 Nouvelles observations sur la décomposition des corps dans un espace libre. In Méthode d’étude des sépultures, pp. 6–13. Saint-Germain en Laye: Saint-Germain en Laye, France. 1987a Contribution des observations osteologiques a la chronologie interne des sepultures collectives. In Anthropologie Physique et Archéologie, edited by H. Duday and C. Masset, pp. 51–61, C.N.R.S., Paris. 1987b Organisation et fonctionnement d’une sepulture collective neolithique. L’aven de la Boucle a Corconne (Gard). In Anthropologie Physique et Archaéologie, edited by H. Duday and C. Masset, pp. 105–111. C.N.R.S., Paris. Duday, H., P. Courtaud, E. Crubezy, P. Sellier, and A.M. Tillier 1990 L’anthropologie de “terrain”: reconnaissance et interpretation des gestes funeraires, Bulletins et Memoires de la Societe d’Anthropologie de Paris 2(3–4):26–49. Duday, H., and Masset, C. 1987 Anthropologie Physique et Archaéologie, C.N.R.S., Paris. El-Najjar, M.Y. and K.R. McWilliams 1978 Forensic Anthropology: The Structure, Morphology, and Variation of Human Bone and Dentition, Charles C Thomas, Springfield, IL. Fernandez-Jalvo, Y., L. Scott, and C. Denys 1999 Taphonomy of pollen associated with predation, Paleogeography, Paleoclimatology, Paleoecology 149:271–282. Fluehr-Lobban, C. 1995 Cultural relativism and universal rights, The Chronicle of Higher Education June 9:B1–B2.

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France, D.L. et al. 1992 A multidisciplinary approach to the detection of clandestine graves, Journal of Forensic Sciences 37:1445–1458. 1997 NecroSearch revisited: Further multidisciplinary approaches to the detection of clandestine graves. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 497–510. CRC Press, Boca Raton, FL. Galloway, A. 1989 Decay rates of human remains in an arid environment. Journal of Forensic Sciences 34:607–616. 1997 The process of decomposition: A model from the Arizona-Sonoran Desert. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 139–150. CRC Press, Boca Raton, FL. Gargett, R.H. 1999 Middle Palaeolithic burial is not a dead issue: The view from Qafzeh, Saint-Césaire, Kebara, Amud, and Dederiyeh, Journal of Human Evolution 37:27–90. Gifford-Gonzolez, D.P. 1981 Taphonomy and paleoecology: A critical review of archaeology’s sister disciplines. In Advances in Archaeological Method and Theory, edited by M.B. Schiffer, pp. 365–438. Academic Press, New York. 1987 Modern analogues: Developing an interpretive framework. In Bone Modification, edited by R. Bonnichsen and M.H. Sorg, pp. 43–52. Center for the Study of the First Americans, Orono, ME. Haglund, W.D. 1991 Applications of Taphonomic Models to Forensic Investigations, Ph.D. dissertation, Department of Anthropology, University of Washington, Seattle, University Microfilms, Ann Arbor, MI. 1993a Disappearance of soft tissue and the disarticulation of human remains from aqueous environments, Journal of Forensic Sciences 38(4):806–815. 1993b Beyond bare bones: From consultation to authority, Practicing Anthropology 15(3):17–19. 1998 The scene and context: Contributions of the forensic anthropologist, In Forensic Osteology: Advances in the Identification of Human Remains, 2nd edition, edited by K.J. Reichs, pp. 41–62. Charles C Thomas, Springfield, IL 2001 Archeology and forensic death investigations, Historic Archaeology 35(1):26–34. Haglund, W.D. and D.T. Reay 1993 Problems of recovering partial human remains at different times and locations: Concerns for death investigators, Journal of Forensic Sciences 38:69–80. Haglund, W.D., M. Connor, and D.D. Scott 2001 The archeology of contemporary mass graves, Historic Archaeology 35(1):57–69. Haglund, W.D., D.T. Reay, and D.R. Swindler 1988a Canid scavenging/disarticulation sequence of human remains in the Pacific northwest, Journal of Forensic Sciences 34:587–606. 1988b Tooth artifacts and survival of bones in animal-scavenged human skeletons, Journal of Forensic Sciences 33(4):985–997. Haglund, W.D. and M.H. Sorg 1997a Forensic Taphonomy: The Postmortem Fate of Human Remains, CRC Press, Boca Raton, FL.

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1997b Introduction. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 1–9. CRC Press, Boca Raton, FL. 1997c Method and theory of forensic taphonomy research. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 13–26. CRC Press, Boca Raton, FL. Hall, M.J.R. 1995 Trapping the flies that cause myiasis: Their reponses to host-stimuli, Annals of Tropical Medicine and Parisitology 89(4):333–357. Hanson, B.C. 1980 Fluvial taphonomic processes: Models and experiments. In Fossils in the Making: Vertebrate Taphonomy and Paleoecology, edited by A.K. Behrensmeyer and A. Hill, University of Chicago Press, Chicago, IL. Haskell, N.H. 1989 Calliphoridae of Pig Carrion in Northwest Indiana: A Seasonal Comparative Study, Master’s thesis, Purdue University, West Lafayette, IN. Haynes, G. 1980 Prey bones and predators: Potential ecologic information from analysis of bone sites, Ossa 7:75–97. 1982 Utilization and skeletal disturbances of North American prey carcasses, Arctic 35(2):226–281. Hill, A.P. 1979 Disarticulation and scattering of mammal skeletons, Paleobiology 5(3):261–274. Horrocks, M., S.A. Coulson, and K.A.J. Walsh 1998 Forensic palynology: Variation in the pollen content of soil surface samples, Journal of Forensic Sciences 43(2):320–323. Hunt, R. 1999 The benefits of scent evidence, FBI Law Enforcement Bulletin 68(11):15–19. Johnson, E. 1985 Current developments in bone technology. In Advances in Archaeological Method and Theory, edited by M.B. Schiffer, pp. 157–235. Academic Press, Orlando, FL. Klein, R.G. and K. Cruz-Uribe 1984 The Analysis of Animal Bones from Archaeological Sites, University of Chicago Press, Chicago, IL. Komar, D. 1999 The use of cadaver dogs in locating scattered, scavenged human remains: Preliminary field test results, Journal of Forensic Sciences 44(2):405–408. Kormondy, E.J. and D.E. Brown 1998 Fundamentals of Human Ecology, Prentice Hall, Upper Saddle River, NJ. Krebs, C.J. 1994 Ecology: The Experimental Analysis of Distribution and Abundance, Harper Collins, New York. Krogman, W.M. 1962 The Human Skeleton in Forensic Medicine, Charles C Thomas, Springfield, IL. Lyman, R.L. 1987 Taphonomy of cervids killed in the May 18, 1980 volcanic eruption of Mount St. Helens, Washington, U.S.A. In Bone Modification, edited by R. Bonnichsen and M.H. Sorg, pp. 149–168. Center for the Study of the First Americans, Orono, ME.

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1994 Vertebrate Taphonomy, Cambridge University Press, New York. Mann, R.W., W.M. Bass, and L. Meadows 1990 Time since death and decomposition of the human body: Variables and observations in case and experimental field studies, Journal of Forensic Sciences 35(11):103–111. Martin, R.E. 1999 Taphonomy: A Process Approach, Cambridge University Press, New York. Martin, R.E., S.T. Goldstein, R. Timothy Patterson 1999 Taphonomy as an environmental science, Paleogeography, Paleoclimatology, Paleoecology 149:vii–viii. Messer, E. 1993 Anthropology and human rights, Annual Review of Anthropology 22:221–49. Micozzi, M. 1991 Postmortem Change in Human and Animal Remains: A Systematic Approach, Charles C Thomas, Springfield, IL. 1997 Frozen environments and soft tissue preservation. In The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 171–180. CRC Press, Boca Raton, FL. Milo, R.G. 1998 Evidence for hominid predation at Klasies River mouth, South Africa, and its implications for the behaviour of early modern humans, Journal of Archaeological Science 25:99–133. Moore-Jansen, P., S. Ousley, and R. Jantz 1994 Data Collection Procedure for Forensic Skeletal Material Report, 3rd edition, Investigations No. 48, Department of Anthropology, The University of Tennessee, Knoxville. Morse, D., J. Duncan, and J. Stoutamire 1983 Handbook of Forensic Archaeology and Anthropology, Rose Printing, Tallahassee, FL. Owsley, D.W. 2001 Why the forensic anthropologist needs the archaeologist, Historic Archaeology 35(1):35–38. Parsons, K.M. and C.E. Brett 1991 Taphonomic processes and biases in modern marine environments: An actualistic perspective of fossil assemblage preservation. In The Processes of Fossilization, edited by S.K. Donovan, pp. 22–65. Columbia University Press, New York. Payne, J.A. 1965 A summer carrion study of the baby pig, Sus scrofa. Linnaeus, Ecology 46:592–602. Payne, J.A. and E.W. King 1972 Insect succession and decomposition of pig carcasses in water, Journal of the Georgia Entomological Society 7:153–162. Peterhans, J.C.K., R.W. Wrangham, M.L. Carter, and M.D. Hauser 1993 A contribution to tropical rain forest taphonomy: Retrieval and documentation of chimpanzee remains from Kibale Forest, Uganda, Journal of Human Evolution 25:485–514. Pfeiffer, S., S. Milne, and R. M. Stevenson 1998 The natural decomposition of adipocere, Journal of Forensic Science 43(2):368–370. Potts, R. 1998 Environmental hypotheses of hominin evolution, Yearbook of Physical Anthropology 41: 93–136. Rebmann, A.J., E. David, and M.H. Sorg 2000 Cadaver Dog Handbook: Forensic Training and Tactics for the Recovery of Human Remains, CRC Press, Boca Raton, FL.

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Reichs, K.J. 1998 A decade of forensic anthropology practice. In Forensic Osteology: Advances in the Identification of Human Remains, 2nd edition, edited by K.J. Reichs, Charles C Thomas, Springfield, IL. Rhine, S. and J.E. Dawson 1998 Estimation of time since death in the southwestern United States. In Forensic Osteology: Advances in the Identification of Human Remains, 2nd edition, edited by K.J. Reichs, pp. 145–160. Charles C Thomas, Springfield, IL. Rodriguez, W.C., III and W.M. Bass 1985 Decomposition of buried bodies and methods that may aid in their location, Journal of Forensic Sciences 30(3):836–852. Saavedra, B. and J.A. Simonetti 1998 Small mammal taphonomy: Intraspecific bone assemblage comparison between South and North American barn owl, Tyto alba, populations, Journal of Archaeological Science 25:165–170. Sauer, N.J. 1998 The timing of injuries and manner of death: Distinguishing among antemortem, perimortem and postmortem trauma. In Forensic Osteology: Advances in the Identification of Human Remains, 2nd edition, edited by K.J. Reichs, pp. 321–332. Charles C Thomas, Springfield, IL. Schäfer, W. 1972 Ecology and Paleoecology of Marine Environments, edited by G. Craig and translated by I. Ortel, University of Chicago Press, Chicago, IL. Scott, D.D. 2001 Firearms identification in support of identifying a mass execution at El Mosote, El Salvador, Historic Archaeology 35(1):79–86. Scott, D. D. and M. Connor 2001 The role and future of archaeology in forensic science, Historic Archaeology 35(1):101–104. Shipman, P. 1981 Life History of a Fossil: An Introduction to Taphonomy and Paleoecology, Harvard University Press, Boston, MA. Sonderman, R.C. 2001 Looking for a needle in a haystack: Developing closer relationships between law enforcement specialists and archaeology, Historic Archaeology 35(1):70–78. Sorg, M.H. 1985 Scavenger modification of human remains, Current Research in the Pleistocene 2:37–38. 1986 Scavenger modifications of human skeletal remains in forensic anthropology. Paper presented at the 38th Annual Meeting of the American Academy of Forensic Sciences, New Orleans, LA. Sorg, M.H., E. David, and A.J. Rebmann 1998 Cadaver dogs, taphonomy, and postmortem interval in the northeast. In Forensic Osteology: Advances in the Identification of Human Remains, 2nd edition, edited by K.J. Reichs, pp. 120–144. Charles C Thomas, Springfield, IL. Sorg, M.H., J.H. Dearborn, E.I. Monahan, H.F. Ryan, K.G. Sweeney, and E. David 1997 Forensic taphonomy in marine contexts. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 567–604, CRC Press, Boca Raton, FL.

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Stewart, T.D. 1981 Essentials of Forensic Anthropology: Especially as Developed in the United States, Charles C Thomas, Springfield, IL Steyn, M. and J.H. Meiring 1997 Forensic anthropology in South Africa: A profile of cases from 1993 to 1995 at the Department of Anatomy, University of Pretoria, South African Journal of Ethnology 20(1):23–27. Stover, E. and M. Ryan 2001 Breaking bread with the dead, Historic Archaeology 35(1):7–25. Turner, C.G., II and J.A. Turner 1999 Man Corn: Cannibalism and Violence in the Prehistoric American Southwest, The University of Utah Press, Salt Lake City, UT. Ubelaker, D.H. 1974 Reconstruction of Demographic Profiles from Ossuary Skeletal Samples: A Case Study from the Tidewater Potomac, Smithsonian Contributions to Anthropology 18, Smithsonian Institution Press, Washington, D.C. 1989 Human Skeletal Remains: Excavation, Analysis, Interpretation, Taraxacum, Washington, D.C. Voorhies, M. 1969 Taphonomy and Population Dynamics of an Early Pliocene Vertebrate Fauna. Knox County, Nebraska, Contributions in Geology: Special Paper, No. 1, University of Wyoming Press, Laramie, WY. Voss, A.A. et al. 1992 Time since death determination of human cadaver using soil solution, Journal of Forensic Sciences 37(5):1236–1252. Walker, S.E. and S.T. Goldstein 1999 Taphonomic tiering: Experimental field taphonomy of mollusks and Foraminifera above and below the sediment-water interface, Paleogeography, Paleoclimatology, Paleoecology 149:227–244. Washburn, W.E. 1987 Cultural relativism, human rights, and the AAA, American Anthropologist 89:939–943. White, T.D. 1992 Prehistoric Cannibalism at Mancos 5MTUMR-2346, Princeton University Press, Princeton, NJ.

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Is Forensic Taphonomy Scientific? Diagnosing death is more than accumulating evidence against the hypothesis that no one is dead.

JON J. NORDBY Contents Introduction Theories, Models, and Data Methodological Mischief? Unlikely Bedfellows Conclusion References

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2

Introduction Distinctions between real science and mere collections of technical artistry, today politely referred to as multidisciplinary efforts, often appear arbitrary and unprincipled (Nordby, 1995). Many theoretical physicists, for example, enjoy disparaging mere applications of science, much as many sequestered academics eschew applications of pure science to practical problems, dismissing such efforts as mere technology unworthy of scholarly assessment (Cartwright and Nordby, 1983). The forensic sciences along with medicine, squarely lumped within this merely applied camp, seem to provide paradigm examples of applied science (Nordby, 1995). It is difficult for traditional theoretical scientists, or classical philosophers of science, to appreciate just how such technical artistry, with its many case-specific correctives and seat-of the-pants techniques, may contribute to the development of robust general theories. Such theories must, after all, inform us about the physical nature of our universe, and allow supportable predictions from models wholly entailed by theory alone. Much like medicine, the forensic sciences unite diverse scientific disciplines to unearth, construct, and justify the best explanations allowed by science for specific, concrete processes and events. For example, forensic anthropologists strive to explain specific human death scenes rather than simply testing and confirming the results predicted by models derived from some general anthropological theory. As such, forensic anthropology, and its relatively recent spin off, forensic taphonomy, supply no neat way for localizing the cluster of sciences to produce and defend these specific, concrete explanations of complex multivariate processes. Multivariate contextual settings such as variations in location, climate, flora, and fauna, appear to make robust theory building in forensic taphonomy at best useless, and at worst, impossible. Without robust scientific theories and the theoretical models fully entailed by them, understanding the explanatory processes in forensic taphonomy appears to remain politely multidisciplinary and impolitely not science (Nordby, 1989). Forensic taphonomy may at this time exist as a collection of hodge-podge theories, pasted together from many sciences, mixed with archaeological practices, and loosely accumulated to defend case-specific explanations and guide the discovery, investigation, and eventual explanation of specific decomposing human (or other) remains. However, to establish a scientific gauntlet for forensic taphonomy as punishment for its currently undeveloped theoretical perspectives ignores the theoretical growth of gradually maturing natural sciences for the last 2000 years (Neugerbauer, 1957). To develop theoretical perspectives to “improve the interpretation of individual biology and history within the context of depositional environment” (Haglund and Sorg, 1997b:16–18) theoretical models, explanatory narratives of case-specific phenomena, and the relation of theory development with explanatory processes must be more clearly understood. To ask if forensic taphonomy is a science, however, is to ask the wrong question. Given this multidisciplinary concatenation of theory with practice from many different scientific disciplines, just as one sees in medical research, the more important prior question becomes: Is forensic taphonomy scientific? If its methods are currently unscientific and no theoretical foundations can be developed, then at the very least, forensic taphonomy must refine its methods to be considered a natural science in the distant future. Can forensic taphonomy develop beyond its alleged war-story status, which thus far supplies a rather limited base for theory building? (See

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Haglund and Sorg, 1997b.) Developing a theoretical basis for forensic taphonomy invokes the logical process of theory development familiar to students of the history, philosophy, and methodology of both theoretical science and research medicine. Paucity of theory building is not a phenomenon unique to forensic taphonomy; it’s one component in the long story of all scientific progress.

Theories, Models, and Data The practice of natural science involves recognizing, developing, and applying many different concepts collected under the same name. Scientific theory provides a well-discussed example (Cartwright, 1980a,b; Duhem, 1962; Hempel, 1965; and Van Frassen, 1980). Rather than seeing scientific theory as one distinct thing, it appears that “scientific theory” captures a whole family of different makes and models, much as “product of General Motors” encompasses many related, yet distinct, divisions and vehicles. While there may be many differences, certain similarities exist, otherwise the categories “scientific theory” and “product of General Motors” would lose their members completely (Weil and Nordby, 1989). The similarity rests with method (Nordby, 1995). “Scientific model” also involves a whole family of concepts with significant practical and conceptual differences (Hanson, 1971; Weil and Nordby, 1989). A typical model presents an analogy — a relation between or among objects, supporting inferences about one based on manipulations with the other. Systematic western studies of the logical root of analogy began with Aristotle (384–322 B.C.). Archimedes (287–212 B.C.) also explains and defends the use of models in crafting the systematic explanations presented by natural philosophers (natural philosophers were first called scientists by William Whewell in 1840). William Whewell (1794–1866) further refined the modern concept in The Philosophy of the Inductive Sciences (Whewell, 1847). In his account, Whewell conceived induction to be a logical pattern for discovery, rather than a dubious mode of justification through mere enumeration. [For the latter account, see Hume (1777) and Carnap (1950); against the notions developed by Hume and Carnap, Whewell’s ideas were refined and developed by the American Pragmatist Charles Sanders Pierce (1839–1914) (Tursman, 1987).] A model represents, describes, exemplifies, or predicts some underlying phenomenon or process in terms of some other — it does not suffice as an explanation. Some brief examples illustrate. Posing questions about the observed world in a mathematical way has been the scientific norm in the West at least since Galileo (1564–1642). This mathematical modeling process selects specific characteristics to be represented mathematically, usually at the expense of other characteristics not so captured, allowing predictions of the modeled phenomena from mathematical manipulations alone. Accordingly, such predictions are then either confirmed or refuted by observation or experiment with data made relevant by theory. A model’s accuracy and predictive power depend on the relevance of the abstraction it captures for the process under investigation. For example, using geometric figures like triangles as models to calculate the distance from the earth to the sun revolutionized both physics and cosmology. Atomic, pendulum, equilibrium, and countless other mathematical models infuse theories of physics (Nordby, 1989). In fact, in physics, merely calculating with these models has become almost synonymous with ‘doing physics.’

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Modeling, as an important element of scientific theory, is also evident in many examples from biology. William Harvey (1578–1657) pioneered the use of mathematics to resolve biological conundrums. The evidence supporting his theory of blood circulation included a quantitative analysis measuring the volume of blood the heart pumped in an hour. (In his experiment, he measured the amount of blood moved in each systole and multiplied by the number of heartbeats per hour). The amounts vary with the measured volume and the number of beats. The predictive power of his model rests with its generality and universality among differing organisms sharing relevantly similar physiological characteristics detailed in his theory. Predator–prey, pollution, evolution, and countless statistical models abound in biology and medicine. For example, Gregor Mendel (1822–1884) modeled relationships among parental properties, breeding, and the properties of successive generations by using garden peas. Selecting snow peas from among the many garden pea varieties in order to investigate a developing genetic theory occurred through trial and error, mixed with critical scientific assessments distinguishing relevant from coincidental properties in the process they model. Models of fundamental natural processes are chosen for many different reasons, including unashamedly practical considerations. Selecting humans as subjects, for example, to investigate dominant and recessive genes would pose insurmountable investigative problems — succeeding generations are too far apart in time. Mendel himself would not have lived long enough to make his observations and develop his conclusions. He chose snow peas over other pea varieties to model the relevant features of genes because they have a much faster generation turn-around time. Others then applied the power of what later became the genetic theory to predict the process in humans. Choices among laboratory animals for medical research are often based upon developing an analogy — a systemic isomorphism or homomorphism — with humans; monkeys, rats, dogs, etc. each models some human systems and processes better than others do. The famous Bohr model of the atom, using planet-like subatomic orbits to model atomic structure, still has great heuristic value, although the model does not literally or accurately represent the atom. Instead, as with some medical models, it captures specific relationships among the particles thought essential for prediction and useful for understanding. This universality and predictive power characterize both theoretical models and the developing theories supporting their application. Identifying the exact processes to model, however, requires the scientific sagacity, luck, and patience associated with scientific discoveries. According to Whewell’s inductive logic and later, Peirce’s abductive logic, these logical processes of discovery rest at the heart of scientific method (Tursman, 1987). No model captures every element in a complex process under investigation. In real phenomena such as disease processes, factors covered by different theories and their models interact in ways not covered by any general umbrella theory. We pay a price for standing on the shoulders of past scientists, applying and investigating their theoretical constructs in relatively novel situations. For example, individuals appear to react differently to the HIV virus as well as to various medications developed to combat full-blown AIDS. The identification and explanation of these differences, however, allow medical researchers to identify and test alternative components of the general disease process, searching for the mechanisms that account for the differences while finding relevant similarities. Our successes or failures are measured by developing predictive and explanatory power.

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Models in forensic taphonomy are not all based simply on mathematical equations, nor are they fully entailed by paleontological, paleoanthropological, or archeological theory alone. Taphonomy appears to focus on processes more like those of disease, with all their individuating circumstances embodied in seemingly unique investigative data. One obstacle to classifying a theory, or a model of the theory, as scientific involves the need to make case specific correctives when applying the model. The presence of apparently ad hoc corrective procedures, without some logical rules for their application, appears to exclude certain theories and their models from being scientific. Consider the early caloric theory of heat, which theoretically explained combustion through the release of a theoretical entity called phlogiston. [Compare explaining combustion theoretically with explaining the Chicago fire by citing Mrs. O’Leary’s cow.] Combustion logically entailed phlogiston’s release when objects such as human bodies transform by fire. According to a simple model of this theory, phlogiston, as an element in everything combustible, is physically released during combustion. This release explained the production of heat. This simple model appeared to be consistent with the observed combustion of many materials. Of course, when Lavoisier roasted sheets of copper, the mass of the copper before combustion was less than its mass after combustion. If phlogiston, as a substance, was released during combustion, as caloric theory predicted through its theoretical model, then the mass of pre-roasted copper [copper plus phlogiston] would be greater than the mass of post-roasted copper [copper minus phlogiston]. Lavoisier’s actual measurements of copper, however, showed just the opposite. Caloric theorists first attempted to save the theory and explain the apparently contradictory result for copper by making copper a special case not captured in the model, or covered by the theory. Caloric theorists hypothesized that phlogiston, when a substance in copper, had a negative mass. This bold stroke to save the caloric theory’s theoretical model and the phenomenon, if not dignified with the status of corrective procedure, was certainly ad hoc and ultimately contradictory: the concept of negative mass was incoherent. This represents scientific progress: developing and investigating the caloric theory cannot be called unscientific simply because its model collapsed, and the theory turned out to be false. Forensic taphonomists appear to make logically similar correctives when specific depositions of human remains seem to have absolutely unique properties, apparently inconsistent with empirically investigated decomposition models built with work from various chemical, physiological, and medical theories. Unique combinations of climate, location, weather, circumstance, etc., appear haphazardly to amend theoretically imprecise time interval-relating properties of the so-called stages of decomposition. The scientific challenge involves remodeling decomposition models that come up short by analyzing the specific mechanism at hand. This remodeling casts a scientific eye toward theoretically robust accounts of the decomposition process that move beyond case-specific explanations. Remodeling becomes a logical mechanism for scientific discovery. If forensic taphonomy is to build a genuine theoretical basis from apparently anecdotal origins, the logical relations among different kinds of theories, and their differing models, must be systematically clarified and developed. Certainly not every corrective applied to a scientific model derived from theory must resort to ad hoc amendments to save the phenomena. If it did, no confirmed predictions demonstrating increased scientific understanding would be possible.

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The relationship of anecdotal experiences with specific phenomena, the development of rather specific models, and the incorporation of corrective procedures to build, apply, and remodel them remains an essential part of theory-building in any maturing science. Persisting uniqueness, faced with overly general and contextually vague models from various scientific disciplines, need not defoliate the theoretical landscape of any natural science. In fact, they’re necessary for sound theoretical development.

Methodological Mischief? When a suspect was told that a witness had seen him commit murder, he calmly replied that he could bring forward a hundred witnesses who had not seen him commit it. G.K. Chesterton

One common argument against the methods of any forensic science being scientific involves the forensic focus on investigations of single, unique events, usually crimes, which do not lend themselves to generalizations on a par with those of the natural sciences (Nordby, 1995). For example, crime assessment or profiling appears at first blush, at best, to be on a par with forecasting the weather, or with predicting the financial behavior of Wall Street investors. When resident psychological, meteorological, or financial theories make inaccurate predictions through their models, particular amendments may appear to cover errant predictions, and to smooth over inconsistencies. Such additions appear to save both the fundamental theory and the actual phenomenon. Rather than admitting that the underlying theory has some defect, or that the model exhibits a fatal weakness, the theory and its model become particularized to account for the now-expected inaccuracy in this special case. Such moves lead many who wash cars, invest money, or explain crimes to conclude that these areas simply lack an adequate theoretical basis altogether, much as shown by the caloric theory’s collapse. But why theories collapse is critical for understanding their scientific status. The caloric theory was scientific, but stock market projections are not. Without defending crime assessment against such charges here, let’s ask, “Does a similar charge legitimately apply to the corrective methods of forensic taphonomy?” Are the forensic taphonomic cases before us so particular, with conditions so unique to specific circumstance that no general bodies of theory, or no specific theoretical models, can even apply?” Fortunately, taphonomy shares at least one legitimizing tool with caloric theory that stock market behavioral explanation lacks: the complex logic of scientific method. Challenging theory construction and model development as a necessary component of scientific method rests on the idea that independent investigators should be able to apply the same methods to the same data and get the same, or at least similar, results (Lynch, 1995). Individual stockbrokers, brokerage houses, and mutual fund managers market unique, individual abilities, like the psychic, rather than offering independently applicable principles open to community testing. Unfortunately, scientists seldom agree on relevant bodies of experience, the accuracy or scope of a proposed or developing theory, or the bias introduced by the presence or absence of specialized training. Real conflicts about the same operation occur in medicine, chemistry, and physics; they are certainly familiar in expert disagreements among forensic

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scientists in courtrooms (Nordby, 1992). The independent reproducibility of complex events or experiments may remain more myth than fact, but this is not due to an inherently fatal, investigator-dependent uniqueness blocking any possible objective demonstrations of fact. The difficulty arises from differences among general theories and applicable predictive models, in principle open to independent analysis and critical investigation (see Hempel, 1965). The particular details reported and developed from the specific work of various forensic anthropologists engaged in taphonomic research are often found among apparently subjective impressions, or sampling bias (Szibor, 1998). They appear to be both investigator and context dependent, seemingly in conflict with the development of well-rehearsed theories in the natural sciences (Cartwright, 1980a,b). Forensic taphonomy relies on investigator judgment, and investigator-dependent approximating procedures regarding sample recovery, collection methods, curation, and analysis (Haglund and Sorg, 1997b). Given this dependence upon individually ordered procedures, imprecise theoretical terms, and as yet absent general theories with associated predictive models, forensic taphonomy has been referred to as more art than science. This may, according to some, capture the current status of forensic taphonomy. However, the view reducing taphonomy to anecdote rests on a radically inadequate understanding of the nature and development of theoretical science, and on viciously misleading notions about the logics of discovery and explanation (Hanson, 1965; Nordby, 1992, 1995). Attributing mere artistry to forensic taphonomy rests specifically on a flawed view of the legitimate relations among theory, models, approximations, and investigatordependent observations, or biases introduced by observers to the particularizing details. In this artistic view, any variations from theoretically predicted results are explained by investigator bias, errors in measurement, flaws in practice, or shortcuts in procedure. Following this position, to say that forensic taphonomy is a science is to say that it rests on a foundation of fully developed, or at least developing, true theories and their models that cover all the processes involved in changing human remains from life to dust. This position carries all the arrogance of the politicians at the start of the 20th century who demanded that the U.S. Patent Office be eliminated “since everything has already been discovered.” On this assumption, when field determinations fail to match theoretical predictions, we conclude that either the theory needs refinement, or the theory remains true, while our application of it in practice falls short of theory. Just how a theory or its model falls short in a particular set of circumstances reveals more about the development of the theory and its models than about alleged flaws introduced by bias, measurement error, or shortcuts. It also suggests how theories and theoretical models are built in the first place.

Unlikely Bedfellows Theory discovery and theory development differ from unique-event reconstruction and case-specific explanation. The absence of any umbrella theories in forensic taphonomy does not mean that we have no idea how to approach questions concerning the postmortem interval in individual cases, or where to look for teeth to help identify a body (Haglund, 1997). We do. But so far, this ability depends upon compilations of anecdotal experiences shared among death investigators practicing in the field from many different scientific

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points of view [anthropologists, archeologists, pathologists, entomologists, botanists, geologists, meteorologists, and many others]. Unfortunately, precious few such anecdotes exist to be compiled. However, the logical status of this investigator-specific data, somehow relevant in forensic taphonomy, parallels the logical status of data from any developing natural science in its infancy (Cartwright, 1983). We may not yet be in a position to build the necessary theoretical bridges. Forensic taphonomy, after all, only recently became a subject for formal study (as compared with chemistry). We may be guilty of common contemporary impatience for rigorous theoretical development, or we may not all be equipped scientifically to develop existing data in more theoretical directions. We may even make quick, partisan decisions between ill-chosen alternatives: Is taphonomy a mature science, or is it a waste of scientific time? Patience gleaned from the history of medicine counsels that these options remain profoundly incomplete. The practical urgency to prevent patient deaths from “childbed fever” at Vienna General Hospital in 1844 supplies a useful lesson. The situation faced by Ignaz Semmelweis, a Hungarian physician, loosely parallels the practical urgency of taphonomic analysis when facing criminal cases. As a staff member of the First Maternity Division, Semmelweis noted that many patients who delivered babies contracted an often-fatal disease called puerperal fever, or childbed fever. About 260 of the 3157 mothers, or 8.2 %, died from the disease. In 1845, the rate in the First Division fell to 6.8%, but in 1846 it jumped to over 11% (Sinclair, 1909; Kruif, 1909). He also noted that the hospital’s Second Maternity Division, over the same period, enjoyed a much lower death rate from the disease — about 2 to 3%. Wellqualified physicians, who taught in the medical school, treated patients in the First Division. Those in the Second Division saw only midwives, adding further professional chagrin to the otherwise intolerable situation. Semmelweis followed and tested many avenues to solve the puzzle. In 1847, a colleague, nicked by a student scalpel during an instructional autopsy, died a similar death. Semmelweis supposed that cadaveric matter from the dead body, introduced into the professor’s blood through the nick, had caused the fatal illness. He reasoned that washing with chlorinated lime would destroy the cadaveric matter introduced to patients in the First Division by physicians and medical students who routinely performed cadaver dissections. In 1848, after this cleaning practice became routine, the death rate for the First Division fell to a little over 1%, about the same as the Second Division, which followed the same practice. Additional data presented a new puzzle. After washing with chlorinated lime, Semmelweis examined an expectant mother suffering from a festering cervical cancer. The following 12 healthy women he examined all developed childbed fever: 11 died. Semmelweis concluded that childbed fever was caused by both cadaveric matter and “putrid matter derived from living organisms” (Sinclair, 1909). While Semmelweis may have solved the practical puzzle, he did not even broach the theoretical puzzle. He developed no theory to explain why cadaveric or putrid matter caused childbed fever, nor why washing with chlorinated lime arrested its spread and development. His practical success remained unexplained until the germ theory of disease showcased just what it was in cadaveric and putrid matter that provided the mechanism for what we now know as infections.

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A similar paucity of theory exists among case-specific research in forensic taphonomy. We may successfully distinguish antemortem, perimortem, and postmortem intervals in a specific case without understanding the underlying explanatory mechanisms that serve to distinguish them. This leaves theoretical development outside the action. Many successful specific case analyses share the scientific status of a Viennese bath in chlorinated lime. Facing multivariate, apparently unique factors, familiar in death assemblages and disease processes alike, remains the rule rather than the exception in the development of a scientifically solid theoretical structure. Eventually, forensic taphonomy may develop a theory to parallel the germ theory of disease through a more formal approach to current case experience. We may not yet have firmly established the science of forensic taphonomy, but it does not follow that it is unscientific — its developing methods and history parallel those of now recognized and trivially accepted theories of disease. For inspiration, we may consider examining logical relations among theories of the HIV virus, the common effects of full-blown AIDS, and practical patient therapies. We see the logical interaction of each as a key to developing a scientific theory, with model application and revision, given apparently unique, concatenated phenomena. Theory development in forensic taphonomy (Haglund and Sorg, 1997b and Chapter 1, this volume) broadly parallels that in medicine. Somehow, like the scientific pioneers following Semmelweis, we learn to move from anecdote to theory by seeking and unraveling the common threads that unite apparently dissimilar phenomena.

Conclusion Recognizing how a developing explanation or a proposed model falls short in a particular set of circumstances supplies insight into needed theory and model development. In fact, the history of medicine suggests how to build theories and theoretical models from specific case experiences. Current case-specific research virtually ensures that forensic taphonomy will remain scientific as it develops and broadens its theoretical base (see Table 2.1). The nature of these insights may initially appear to be anecdotal, but in the discussion and analysis of anecdote rests the beginning of robust theory. After all, that’s where theories come from in the first place: from the need to explain the explanations (Achinstein, 1983). Such theories in forensic taphonomy, developed through making particular corrections and tinkering with tentative models borrowed from intersecting sciences, may eventually change the theoretical faces of sciences such as paleoanthropology, physical anthropology, entomology, ecology, as well as taphonomy, forever.

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Table 2.1 Characteristics of Scientific Theories • Natural scientists do not always work with theories; they work with unexpected data and struggle to explain it. Particular explanations of unexpected or surprising phenomena lead to the development of general theories. • Scientific theories are much more than simple generalizations — they capture law-like generalizations that are true anywhere their boundary conditions have been satisfied. Promising theories withstand specific challenge, and fit together with other developing theories, observations, and recognized law-like statements about natural processes. • Scientific theories are a special kind of generalizing explanation. They systematize specific relationships to the exclusion of others in order to understand a complex phenomenon. • Promising theories allow predictions that, at least in principle, can be confirmed or refuted. For example, in the developing theory of blood circulation, Harvey postulated minute channels between the arteries and veins. Such structures were logically necessary for the theory to work. This feature of his theory was not confirmed until 1661, when Marcello Malpighi observed capillaries microscopically. • Scientific theories do not function to explain every, one could argue, any, unique event falling under their umbrella. Most unique events of forensic or other scientific interest fall under more than one theoretical umbrella, e.g., decomposition processes include putrefaction, a microbial process, as well as autolysis, a chemical process. But in a unique gravesite, a body decomposes among many other independent conditions, that are in turn covered by other theories, e.g., environmental factors • Individually corrected explanatory stories must be consistent with scientific theories that cover the event, or the theory must supply good reasons why they are inconsistent. Otherwise the theory may be defective in its present form. • Theories in a discipline must capture systematic regularities. When generalizations merely coexist with recognized exceptions, the generalizations retain the status of “rules of thumb,” eschewing the status of scientific theory. • Scientific theories, unlike causal or explanatory narratives, must not contain unspecified ceteris paribus clauses (all things being equal, or more clearly, all things being right). In specific forensic events, nothing is equal, and nothing is right as far as the rigid application of an umbrella theory goes. • Scientific theories must logically comprise a well-defined set of counterfactual conditionals (what would happen if) when applied to hypothetical phenomena, e.g., What would happen to a human body which suffered blunt-force trauma to the head when it is buried in 10 feet of snow at 12,000 feet for 30 days? Theories of putrefaction, and autolysis as well as theories of thermal interaction, and environmental agency, may cover and yield predictions that would then give relevance to certain measured data in the event the hypothetical became actual. Any deviation from theoretical prediction then, would itself need explanation — ranging from charges of defective theory to modifications in materials, the presence or absence of specific features such as alcohol consumption, or disease processes, or other intervening events, etc. Note that these particularizing modifications would NOT involve modifications to scientific theory itself — they would involve modifications to developing explanations of specific, concrete events. This is a different intellectual task (Cartwright, 1980) • In the absence of robust scientific theories, their construction proceeds through distinguishing corrective procedures that merely work in a specific case from those that inherently take us toward a true explanation. Systematic general theory building can begin with the systematic analysis of these specific corrections, keeping in mind that scientific theories do not assume the role of explaining all features of uniquely particular concrete events, but must retain the logical features listed above. Note: “Theory” covers many differing conceptual structures, some unique to natural science, some not, but there are some general features that uniquely scientific theories of many different sorts must contain.

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References Achinstein, P. 1983 The Nature of Explanation, Oxford University Press, New York. Carnap, R. 1950 The Logical Foundations of Probability, University of Chicago Press, Chicago. Cartwright, N. 1980a The truth doesn’t explain much, American Philosophical Quarterly 17(2):184–189. 1980b Do the laws of physics state the facts? Pacific Philosophical Quarterly 61:216–227. 1983 Do the Laws of Physics Lie? Oxford University Press, New York. Cartwright, N. and J. Nordby 1983 How approximations take us from theory and toward truth, Pacific Philosophical Quarterly 64:273–280. de Kruif, P. 1932 Men Against Death, Harcourt Brace & World, New York. Duhem, P. 1962 The Aim and Structure of Physical Theory, trans. by Philip P. Wiener. Athenaeum, New York. Haglund, W.D. 1997 Scattered skeletal human remains: search strategy considerations for locating missing teeth. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 383–394. CRC Press, Boca Raton, FL. Haglund, W.D. and M.H. Sorg 1997a Forensic Taphonomy: The Postmortem Fate of Human Remains, CRC Press, Boca Raton, FL. 1997b Method and theory of forensic taphonomic research. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 13–26. CRC Press, Boca Raton, FL. Hanson, N.R. 1965 Patterns of Discovery: An Enquiry into the Conceptual Foundations of Science, Cambridge University Press, New York. 1971 Observation and Explanation: A Guide to Philosophy of Science, Harper & Row, New York. Hempel, C. G. 1965 Aspects of Scientific Explanation and other Essays in the Philosophy of Science, The Free Press, New York. Hume, D. 1777 Enquiries Concerning the Human Understanding and the Principles of Morals. Oxford University Press, Oxford, 1968. Lynch, J. 1995 The Race To Catch a Bucky Ball, WGBH TV Boston, BBC TV Service, WGBH video, Burlington, VT. Neugerbauer, O. 1957 The Exact Sciences in Antiquity, 2nd ed. Brown University Press, Providence. Nordby, J. 1989 Bootstrapping while barefoot [crime models vs. theoretical models in the hunt for serial killers], Synthese 81:373–389. 1992 Can we believe what we see if we see what we believe? Expert disagreement, Journal of Forensic Sciences 37(4):1115–1124. 1995 Science is as science does: the question of reliable methodologies in “real science,” Shepard’s Expert and Scientific Evidence Quarterly 2(3):701–710.

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Sinclair, W.J. 1909 Semmelweis: His Life and His Doctrine, Manchester University Press, Manchester, England. Szibor, R., C. Schubert, and V. Wendt 1998 Pollen analysis reveals murder season, Nature 395(6701):449. Tursman, R. 1987 Peirce’s Theory of Scientific Discovery: A System of Logic Conceived as Semiotic, Indiana University Press, Bloomington, IN. Van Frassen, B. 1980 The Scientific Image, Clarendon Press, Oxford. Weil, V. and J. Nordby 1989 Introduction. In Synthese: Philosophy of Applied Science, Vol. 81, Kluwer Academic Publishers, The Netherlands. Whewell, W. 1847 The Philosophical Foundations of the Inductive Sciences, Founded on Their History, Vol. I2, 2nd ed. Cambridge University Press, London.

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Section 2

The Biogeographic Context

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An Autopsy of the Grave: Recognizing, Collecting, and Preserving Forensic Geotaphonomic Evidence MICHAEL J. HOCHREIN Contents Introduction Stratification Case History #1 Case History #2 Case History #3 Tool Marks Case History #4 Bioturbation Case History #5 Sedimentation Compression/Depression Case History #6 Internal Compaction Excavation Techniques Conclusions Acknowledgments References

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3

Introduction The use of archaeological methods on buried body crime scenes is not new to forensic science. Boddington et al. (1987), Brothwell (1981), Heizer and Graham (1967), Morse et al. (1983), Roberts et al. (1989), Skinner and Lazenby (1983), Ubelaker (1989), and others have become standard references in crime scene training; however, the actual application of formal archaeological techniques is too often ignored or shortcut to the point of absence at many crime scenes. At other sites, archaeology may be used without considering the recent, and forensic, contexts of scenes and the artifacts they include. The ability to consult professional archaeologists is often not recognized by many police departments, or is thought to be outside their fiscal means. When archaeology consultants are called into crime scenes, investigators may be at the mercy of their expertise level. Not all archaeologists are trained with emphases in physical anthropology or osteology, nor do all physical anthropologists have adequate archaeological field experience to direct excavations for, and interpret, subtle subterranean clues left at burial sites. Very few anthropologists, in general, have any practical experience in processing forensically significant sites. From the homicide or death investigator’s perspective, the need has been recognized (Horvarth and Meesig, 1998) for additional and appropriate training of law enforcement personnel who constitute first responders in the discovery, documentation, and collection of physical evidence. This also applies to those investigators tasked with interpreting the context of such evidence. For the non-anthropologist investigator, training in forensic anthropology is one of the least common areas of police instruction. When courses are available in forensic anthropology, they may concentrate on search techniques or the laboratory analyses of recovered evidence rather than collection methods. The end result may be the well-intended processing of crime scenes that appear to have been systematically excavated, but where subtle, important clues have been overlooked. In worse case scenarios, the excavations damage or destroy evidence. Consider the following descriptions of archaeological excavations: He stuck a small shovel several inches into the muck and struck something solid. “I pulled it up and it’s a bone, a arm bone,” (He) endured a week of ten hour days digging his gloved hand through decomposing flesh into rib cages and finding his fingers stuck in eye sockets. Anonymous, 1994

or this account: While digging in freshly turned dirt at the southeast corner of the property, (he) turned up some items that looked like pieces of cloth and beef jerky… when a lot of “whacking” and “banging away” on something that looked like a tree root failed to dislodge it, (he) wrapped (his) hand around it, braced (his) feet and started pulling on it… (He) pulled so hard that it broke loose, and when (he) pulled it up (he) could see the joint. It was a bone! Wilson, 1993

To the formally trained contemporary archaeologist, these accounts might conjure images of an Indiana Jones episode, or early classical archaeology and its emphasis on

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gathering artifacts for personal and museum collections, taking little care of their archaeological contexts. Unfortunately, these excerpts are not from movie scripts or of earlier eras. They describe more recent accounts of the recoveries of homicide victims. Archaeological approaches to buried evidence crime scenes should be similar to that of a thorough forensic autopsy. The use of protocol in excavations must be combined with an understanding of the dynamics of the matrices (tissues) being excavated (dissected). Just as the forensic pathologist is well versed in postmortem changes to muscle, organs, and wounds, the forensic archaeologist is expected to be well versed in intrinsic characteristics and environmental factors which can affect soil horizons and interfaces through which clandestine pits are dug. The concept of geotaphonomy was proposed to address the recognition and collection of specific types of evidence, which can be recovered only via appropriate archaeological techniques. Geotaphonomy has been defined as “The study of the geophysical characteristics of, and changes in, subterranean features associated with the interment of buried evidence.” (Hochrein, 1997a). This study of the dynamics behind the creation, closing, and postdepositional history of burial features differs from taphonomy by recognizing, collecting, and interpreting cultural and environmental factors affecting the burial feature, including its contents. Where taphonomy broadly utilizes the condition of or modifications to, and context of deposited remains for interpretation of peri- and postburial environments, geotaphonomy focuses such forensic examinations on the grave context itself. The focus of geotaphonomy is on the pit, grave, or concealing matrices whether or not the evidence buried includes human remains. Geotaphonomy encompasses six areas or aspects of the burial environment: stratification; tool marks; bioturbation; sedimentation; compressiondepression and internal compaction.

Stratification The geological principles of stratification, including axioms of superposition, original horizontality, and original continuity, were conceptualized as early as the seventeenth century by individuals such as Nils Steensen (Steno), William Smith, and Sir Charles Lyell. Those principles have been further developed, or applied, in more recent works (Donovan, 1966; Drucker, 1972; Dunbar and Rodgers, 1957; Harris et al., 1993; Pydokke, 1961; Schiffer, 1987; Spennemann and Franke, 1995, and others) as tenets of archaeology and paleontology. Stratigraphy is the primary basis for understanding buried crime scene evidence. The excavation of graves or pits cannot take place without permanently interrupting and mixing soil horizons. These layers can be naturally or artificially formed. Since the digging of a feature is chronologically and spatially relative to the soil layers in which it intrudes, changes to the stratification of manmade fill are as apparent as those of natural horizons. In the search for clandestine burials, e.g., Case Histories 1 to 3, interruptions to stratification is one basis for intensifying pedestrian, geophysical, and remote search techniques. Pedestrian searchers look for surface indications that subsoil horizons have been displaced to the top and mixed with superseding and underlying layers during the process of digging and then infilling a pit. These indications may be as obvious as differences between the color of the pit fill, backdirt remnants, and surface layer; however, they are often subtle textural differences. Geophysical prospection uses technically refined measurements of

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naturally or induced signals to identify areas in which a site’s stratification has been disturbed (Davenport, 1996; Killam, 1990; and Wynn, 1986). Stratification is also evident in trash dump deposits. The archaeology of commercial landfills is well documented, and has been refined, through the research of Rathje et al. (1992). The systematic excavation of refuse underlying and covering primary evidence can provide some of the clearest means of dating that evidence. Layers of garbage above, below, and contemporaneous with the primary object being sought contain artifacts that may be dated by marks, serial numbers, or calendar dates. At a minimum, such associated items offer a terminus post quem for when the primary evidence could have been deposited (Noël Hüme, 1970). When dating evidence on the basis of associated debris, investigators must take care to rely on the chronology of depositional layers rather than relying on individual pieces of garbage. Individual items may be curated for varying lengths of time resulting in a manufacture-deposition lag (Hill, 1982). For example, resealable items such as jars typically demonstrate datable labels or maker’s marks but are more subject to reuse than non-collectable beverage cans. Disadvantages associated with landfill searches are logistical in nature and relate to the size of the dumpsite and the length of time since the evidence was disposed. Laska (1996) describes the extent and cost such problems posed in the search for remains of a missing child. In that case, approximately three weeks and $100,000 were expended before the search concluded without the discovery of a body. Stratigraphy is even more forensically significant when applied within the burial feature. Often, a subject’s intent toward further concealment of buried evidence is reflected in introduced additives, which constitute layers of the clandestine pit’s stratification. It is not uncommon to discover graves into which lime, or related chemicals, were poured to mask the odor of decomposition or hasten the process. Subjects often confuse the properties of calcium oxide with similarly named but less caustic products such as calcium carbonate or calcium hydroxide. Inadvertently, their mistakes help to preserve the remains. Whatever the intent or outcome (Figure 3.1), the continuity of that stratum can be utilized to clearly document postburial tampering. Once an anomaly is identified as a burial feature, its examination is limited to the contents or stratification within the grave or pit. Internal interruption to the strata may represent a subject’s return to remove or alter grave contents. Likewise, multiple burials separated by time will be reflected by interruptions visible in horizontal and vertical stratifications. The forensic archaeologist must remember that each shovelful theoretically represents a separate stratigraphic event. To ignore stratification is to ignore some of the most direct information of how the evidence came to be interred. Case History #1 During a homicide investigation in which the author assisted, the establishment and maintenance of a vertical profile or section within a clandestine grave allowed the interpretation of grave construction and later intrusion. The case involved the sudden disappearance of an elderly couple. Foul play was immediately suspected and an investigation was initiated. Approximately 1 year later, accomplices confessed and told investigators where both victims were interred in a common grave. Evidence team members were able to document the sequence of deposits (Hochrein, 1997a) within the grave beginning with the wrapped bodies of both victims, followed by a layer of soil, a thin layer of concrete, additional soil, and finally horse manure. During excavation, a series of profiles or sections

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(a)

(b)

Figure 3.1 (a) Bisection and partial excavation of a burial feature.

(b) Stratum of calcium carbonate exposed in a vertical profile during archaeological excavation.

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were established across the grave and perpendicular to the buried remains. The profiles revealed that stratification was interrupted by a pit dug through layers in the southern half of the grave. This confirmed witness accounts of an abandoned attempt to remove and relocate the bodies. Archaeological techniques also allowed the discovery and precise recording of trace evidence, single synthetic fibers recovered in situ. The trace, associated, and stratigraphic evidence ultimately supported witness accounts of the double homicide, burial, and attempt to remove the bodies. These geotaphonomic clues would have gone unrecognized had large tools or heavy machinery been used in the exhumation. Case History #2 In a second case, the victim, murdered by a business associate, lay concealed for 9 months until an accomplice led investigators to a farm on which the remains were buried. Cadaver dogs pinpointed the location. The subject, familiar with a particular sinkhole historically used as the farm’s dump, disposed of the body in the sinkhole and covered it with layers of hay, trash, and lime (calcium hydroxide). During the exhumation, investigators asked if it appeared as if the lime-like substance was poured into the sinkhole prior to the deposition of the body. Such evidence might suggest additional planning and preparation for the homicide. The sandwiching of the remains between layers of lime would have called for some preparation of the burial site and procurement of a large quantity of lime. The information also would be valuable in future interrogations of subjects and witnesses. Excavation first required the establishment of a 3-dimensional grid system. Following the systematic documentation and removal of debris from above the sinkhole, the grid was projected down into it. Evidence and geotaphonomic artifacts of postdeposition environmental events were documented. The excavation revealed that heavy rains during the 9-month burial caused the northwestern edge of the sinkhole to erode down and over a portion of the remains. Attention to stratigraphy allowed the archaeologist to identify this depositional event as natural and not the result of dirt being shoveled onto the remains. To answer the investigator’s initial question, what appeared to be a thin layer of lime beneath the victim’s remains was, again, an artifact of natural erosion. The geotaphonomic examination demonstrated that the lime had washed down the southern facing side of the body and seeped beneath the victim’s right side. It did not constitute a pre-deposited layer on which the remains were placed. Case History #3 The principles of landfill archaeology were put in practice in a case in which the forensic archaeologist was asked to search for the neonate remains allegedly taken from an incest victim and disposed of in the family’s garbage. Approximately 20 months after the incident, the mother told authorities. She recollected being taken by her father, the morning after a forced delivery, to a gully that had been historically used as the farm’s refuse site. Because she was asked to pay her last respects at the site, she suspected the baby’s remains were buried within the dump. The forensic search of the site began with the use of cadaver dogs to narrow the focus of the search. The dogs identified multiple sites (not unexpected in a dump context) requiring the entire dump be searched. With the assistance of anthropology students, a physical anthropologist, and a vertebrate taphonomist, the evidence team systematically dismantled the site. After the establishment of a 10 ¥ 10 m grid system suspended over

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the gully, and the collection of topographic readings, a parallel grid was established on either side of the drainage. The grid was set so that its center line, or transect, bisected the dump lengthwise. Debris, including appliances, newspaper, cans, bottles, food items, etc., were then removed per grid square and placed in paralleling units in reverse stratification. In this manner, the human remains, if discovered, could be dated on the basis of datable debris situated above, below, and around them. Although the search uncovered numerous nonhuman bones, none of a human neonate were revealed.

Tool Marks Tool mark evidence at crime scenes is a primary consideration in burglaries, home invasions, and other crimes involving mechanical means of prying or cutting. At scenes of buried evidence, however, there is often a misconception that tool marks do not survive the elements. Invalid assumptions may be made that all holes are dug with shovels, or that identifying the digging implement used by the subject is not important. Whatever the rationale, marks left during the construction of clandestine graves are routinely overlooked even though they may be preserved below and above ground surface. If tool marks are preserved in buried settings, recognition and collection depends on a systematic removal of the pit’s fill from the original walls of the feature. The author has found one technique, known as profiling, sectioning, or partexing, the most expedient. Understanding how a grave was dug may offer insight into the amount of planning and intent a subject had in dispatching a victim. Tool marks from atypical implements like tree branches or cups may be more consistent with hurried, unplanned disposals. On the other hand, deep pits exhibiting marks from one or more types of shovels may imply a more planned crime and the involvement of an accomplice. Geotaphonomic experiments (Hochrein, 1997b), as well as case experience, have demonstrated how the use of various digging implements introduces unique marks to the walls of burials. Media accounts of buried body cases have documented subjects’ uses of a variety of digging implements from tire irons to clam shells (Anon., 1981a,b, 1984; Ross, 1994). Curwen and Curwen (1926), in discussing the use of a scapula as a tool, imply an even more interesting relationship between taphonomic and geotaphonomic agents. The geotaphonomic experiments mentioned above showed that the act of backfilling, compressing, or stomping the fill and exposing each test feature to approximately 2 weeks of ambient weather did not impede the clear recognition of tool marks upon archaeological excavation.* Subterranean tool marks have been observed in empirical studies, training exercises, and crime scene settings ranging in age from 2 days (Figure 3.2) to 4 years (Figure 3.3). In two experiments (Hochrein, 1997b; Hochrein, [in preparation]), multiple heavy rainfalls in excess of 2.54 cm were recorded at test sites; the buried tool marks remained intact in spite of the precipitation. These findings support assumptions that ambient conditions do not completely obliterate tool marks. Not all soil matrices are conducive to retaining the compression and friction details of digging marks. More plastic soils, with higher percentages of clays or silts, better hold * An ongoing review of media accounts of buried body cases (Hochrein et al., 1999) supports the applicability of such short-duration empirical experiments. To date, of 881 victims, the remains of 607 (68.9%) were found within a year of their disappearances or abductions. Of the same 881, 328 (37.2%) were found within a month of their disappearances.

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Figure 3.2 Claw hammer marks revealed in the walls of a burial (postdeposition period, 2 days).

Figure 3.3 Round-point shovel tool marks revealed in the walls of a burial (postdeposition period, 4 years).

striae and impression details. The least conducive matrices are those consisting of gravels or dry, sandy soils. The dynamics of digging a pit in rocky soil usually necessitate two digging implements: one, such as a pick or mattock to loosen soil and rock; and a shovel to removed the loosened matrix. Although compression-friction marks from the shovel may not be visible, the occurrence of large quantities of cracked or spalled rock in the remaining backdirt, or halo around a pit, can be the first indication of damage caused by a pick type tool. As with soils adhering to shovels, particles of rock impressed into the pick or mattock blade, as well as marks left on rock fragments and tool, might match when

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scrutinized under magnification. Hochrein (1997b) mentions specific characteristics associated with particular types of digging implements. These extend beyond the friction and compression details left by their blades, to the degree to which excavation with certain tools sever root networks, or require the excavator to stand or kneel in certain positions. When examining subterranean features for tool marks, it is important to avoid contamination of forensically significant marks. The excavator may be aided by textural differences between the fill and the more compact sides of a pit. As the fill is archaeologically sectioned, it tends to spall from tool-marked surfaces. The void created between the arbitrary wall constituting an established vertical profile and the original wall of the grave can be filled with dental gypsum to produce a cast of the mark. At deeper depths, the same void can be created by inserting a rigid board in place of the archaeological profile excavated within the feature. The instruments used examining tool mark evidence should include only small, handheld tools. Less refined instruments (such as spades) could allow the excavation to cause marks misattributed to the subject’s excavation. There is also less tactile sensation and control when using larger tools. The author recommends a combination of handheld tools and a vacuum to remove fill from tool marks. The vacuum removes the excavated material without touching the tool marks and their striae. In several experimental and training incidents, casts made after such preparation demonstrated detailed striae. Preserving this level of detail could result in positive identification of specific digging implements, although it is more often only possible to determine the class of tool. Knowing at least the tool class can confirm witness accounts, as well as pertinent information for search warrants. At, or near, the surface of a hand-dug pit, tool marks may be represented by handle impressions along the edge of the grave. As a feature is dug to greater depths using a shovel or long handled implement like a posthole digger, more of the handle, with greater force, is impressed into the top edge of the pit to lever dirt out of the hole; the pit’s edge being used as the fulcrum. A concentration of handle marks, together with the position of the backdirt around the feature, may indicate position while digging. The backdirt should also be examined for potential tool marks (Figure 3.4). The process of digging a hole repeatedly creates tool marks in the last surface receiving the impression of the tool. As a result, each shovelful, or clod, of dirt removed from the pit potentially contains a compression-friction mark. This is particularly apparent in clods, or clumps of sod, where the root network tends to hold the dirt and mark together until destroyed by erosion or crushing actions. Case History #4 In a missing person’s investigation, information was provided to investigators, 2 years after the victim’s disappearance, that a subject had been observed digging in his backyard. The subject lived near the victim and was known to have threatened him. Within days of the victim’s disappearance, the subject was observed digging in a grave previously constructed for one of his pets buried 2 years before. The subject then sold his property and moved from the area. Investigators thought the subject might have used the pet grave to hide the victim’s remains. During a search of the property, examination of the pet grave first delineated its boundaries. Then, its fill was systematically removed in 10-cm levels. The original walls of the grave were preserved behind vertical profiles. When exposed, those walls demonstrated

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Figure 3.4 Clods of soil, among backdirt from a burial feature, bearing shovel tool marks and striae.

pristine curvilinear tool marks with striae contemporaneous with the buried pet, approximately 4 years old. The excavation, removal of the animal remains, and soil core sampling at the base of the pit revealed no additional burials. The profiles did, however, offer an explanation of the subject’s digging activities. The stratification above the original ground surface, and observations of plant growth over the burial indicated the subject was merely tending his pet’s grave by planting grass.

Bioturbation Micozzi (1991) mentions a number of environmental factors which can turbate, or naturally churn, mix, displace, or otherwise modify, the position and nature of remains. Those same agents act upon the grave or pit created to conceal the remains. Plant (floral turbation) and animal (faunal turbation) activities, in particular, are very recognizable. For example, experienced field archaeologists have spent many seasons excavating and distinguishing prehistoric, or historic, post molds from rodent burrows. Searches for clandestine burials may entail a spectrum of techniques ranging from low tech uses of probes or soil core samplers, (Imaizumi, 1974; Owsley, 1995; Whalen, 1990), to state-ofthe-art techniques as sophisticated as infrared thermography (Weil and Graf, 1992) or ground penetrating radar (Conyers and Goodman, 1997), but there is no technique that can, in effect, X-ray soil matrices and conclusively determine the contents of a feature. Furthermore, subterranean anomalies may be produced by faunal turbation rather than burials. Burrowing animals will create chambers or networks of tunnels, open and infilled (krotovinas [Paton et al., 1995]), which appear as anomalies. If an experienced operator is unable to exclude such faunal-turbated areas as natural, limited test excavations may be required. Burrows may also confound, or facilitate, searches using cadaver dogs. Their tunnels act as routes through which scents can travel. Search teams may be led to a grave through

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which, or near which, burrowing fauna have traveled. The author has also found that small burrowing animals, in taking paths of least resistance, tend to follow the upper edge of backfilled test pits. This could aid in identifying original grave outlines. The age of the internment might also be narrowed by determining the season(s) during which particular species of burrowing animals could have made runs. Recognizing faunal turbation also reveals possible routes taken by scavenging fauna, which may have carried off skeletal elements, associated evidence, or trace evidence. In experiments conducted by the author (Hochrein, 1997b) the condition of root networks within some test excavations offered indications of the type of instruments used to dig the pits. Thin profile instruments such as crowbars, pitchforks, and screwdrivers were found to preserve root networks which appear as lattice across the interior of the burial feature but predominately beneath the remains. Broad-bladed instruments such as shovels tended to slice, or tear, roots at the interface of the pit fill and pit wall leaving root segments in the fill and a larger percentage of severed roots at the interface. As discussed in Bock and Norris (1997), Hall (1988, 1997), and Willey and Heilman (1997), this botanical evidence is collected for further interpretation of the crime scene environment. Case History #5 In a case that demonstrated the degree to which burrowing animals could interfere in geotaphonomic interpretation, the victim was hurriedly interred in a shallow grave after his relationship with a friend turned deadly. The homicide and burial occurred in January. In March of the same year, a walker discovered the partially uncovered and scavenged body. Authorities carefully processed the scene in a conventional manner. Five months later, a forensic archaeologist was asked to examine the scene for geotaphonomic indications of how the grave was constructed. Investigators explained how the body was exhumed by clearing soil from above the remains and lifting the corpse out of the shallow grave. The soils around the upper torso and head were dug out and screened for bullets and other evidence. The site was then backfilled. In the reexamination, the remnant of the foot end of the grave was relocated using archaeological techniques. Although the orientation and horizontal dimensions of the pit could be reconstructed, the identification of 3-dimensional tool marks was hindered by numerous krotovinas created during and after the depositional period. The faunal turbation destroyed diagnostic portions of the feature (Figure 3.5) that could have allowed a class determination of the tool used to dig the grave. Burrowing pocket gophers (Geomys burarius) eliminated the areas of the grave edge where the appearance of acute or nearly acute corners would have indicated that a flat-sided digging implement was used; the geotaphonomic examination was inconclusive. When the scene was originally processed, a qualified archaeologist might have been able to recover forensically significant tool marks.

Sedimentation A third agent affecting geotaphonomic interpretations of burial features involves the effects of water within and on the feature. The pooling, evaporation, and drying of water and fine sediments within an open pit, as well as on the surface of an infilled pit, create patterns of cracking. These patterns offer information about the pit’s spatial and temporal characteristics.

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Figure 3.5 Close-up of the foot end of a grave (F5) and undisturbed soils (F3) at a depth of approximately 10 cm below ground surface. Note the intrusion of krotovinas, marked a–d.

McLaughlin (1974) and Morse et al. (1983) mention the identification of surface cracks as a means of locating the grave’s edge during exhumation. Experiments designed to examine the effects of sedimentation on buried crime scenes (Hochrein, in preparation) have included the observation and monitoring of cracks that form along the infilled surface edge of test and control pits (Figure 3.6). In experimental and field school practical exercises, cracks formed as a result of desiccation and settling within 24 hours after rainfall. (Cracks will also form without rainfall, if the ambient moisture content of the fill and surrounding soils is sufficient.) The cracks reappeared after subsequent rainfalls obliterated those previously formed. The cracking will reoccur as long as the fill in the test and control features continues to settle. The cycle of moisture, reconstitution, and desiccation may continue for months after the interment. It has been observed to consistently reoccur along the same margins or boundary of the infilled feature. By comparison, sedimentation over very shallow or relatively flat surfaces, (i.e., puddles), will tend to crack in irregular, spider web-like fashion as the sediments dry. Geotaphonomic research on surface sedimentation and cracking must examine the regularity of the desiccation cycle. In the aforementioned experiments, the width of surface cracks were measured daily for a period of 1 month, monitoring weather conditions. When plotted in relation to each other, an obvious correlation between the amount of precipitation and the width of surface cracks appeared. Moistening of the surface by minor rain showers caused the surface area to expand, closing previously formed cracks. More significant rainfall caused sediment to flow in the cracks in addition to swelling surface areas. In either case, the cracks returned in the same positions within 24 hours following the last rainfall. This pattern continued for the entire 30 days of the experiment. When reexamined 2 months after the end of the experiment, the test pits could still be distinguished by the position of surface cracks.

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Figure 3.6 Surface desiccation and cracks formed around the edge of an infilled test pit.

The second pattern observed was crack width compared to the length of periods without precipitation. It appeared that the cracks would reach maximum widths during lengthy dry periods at a rate of approximately 1 mm per day. Closure during heavy rainfalls, however, could be rapid, going from as much as 7 mm to 0 mm within minutes. The preliminary implications of these observations are that it might be possible, through surface crack widths, to determine the time between the infilling of a clandestine pit and its discovery. With knowledge of the soil types and historical weather information, it may be feasible to determine the post-deposition interval to the last rainfall. In recent cases when that rainfall occurred on or as the only rainfall since the burial date, it might be possible to determine the date of the burial. Surface cracking around the edges of the clandestine graves is often observed but rarely recorded in a standardized manner. Obviously, further experimentation and study are needed in this area. Subsurface cracks, because they form within sedimentation at the bottom of the grave or pit, have an irregular spider’s web appearance. As described above, this occurs because of the shallow, relatively uniform, nature of the underlying surface. The abovementioned experiments, as well as field school observations, demonstrated that it was possible to excavate this desiccated stratum. The subterranean stratum formed from the settlement of sediments in water that accumulated and then drained at the base of the pit. (As with surface desiccation, cracks will form in exposed subsurfaces, without rainfall, when the ambient moisture in the soils evaporates, causing the surface area to shrink [Figure 3.7].) In the case of rainfall events, surface and subsurface sedimentation occurs primarily as the result of sediment going into solution with raindrops and pooling water. Little of the sediment comes from the erosion of backdirt piled near the pit. The experiments were conducted in two phases, wet and dry. The wet phase involved the accumulation of 4.36 cm of rainfall in a test pit followed by its drainage/evaporation. Once cracks formed in the remaining sediments the pit was infilled. The dry phase of the experiment repeated the wet phase protocol but allowed the sediment layer to dry more thoroughly before the pit was infilled. In both the wet- and dry-phase experiments archaeological excavation

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Figure 3.7 Subsurface desiccation and cracks formed in the walls of an open pit 1 day after

excavation.

of the test pits 23 to 30 days after they were backfilled revealed evidence of the desiccated strata’s surfaces including the original cracks (Figures 3.8a and 3.8b). Another indication of the interface between the buried strata and pit fill included vegetation, which settled upon the layer’s surface when the water drained from the pit. In actual case situations, the longer the post-deposition interval, the more likely subsurface cracks will be affected by decompositus, or purge. In areas where the remains are buried below high water-table levels the marks may be obliterated. The sedimentation experiments began with a hypothesis: Subsurface cracks that formed, and were covered after the sediments dried thoroughly, would be easier to identify through archaeological excavation than those covered while the sediments were still saturated. The hypothesis was based on observations that cracks reached a maximum width when lenses of sediment were allowed to dry more completely. Cracks that formed in, and were backfilled while the sediments were semisolid, almost gelatinous, tended to be less numerous and exhibited smaller widths. The experiments did not support the hypothesis, however. Wet sediment cracks, although less numerous, were easier to identify. They retained their widths and depths because the sediments were already saturated. The sediments were apparently less able to absorb additional moisture from rainfall or the backfilled dirt. As a result, the saturated stratum could not swell and close the cracks. In sediment lenses allowed to dry more thoroughly, the subsurface cracks tended to close after the pit was backfilled. Even though the cracks were wider and deeper in dried sediments, the lenses in which they occurred apparently absorbed moisture after backfilling. Like a sponge, the layer of dried sediment swelled, leaving some cracks to begin to, or completely, close. In both the wet and dry phases of the experiment, it was extremely difficult, and in some areas not possible, to distinguish the subsurface stratum, or lenses, by color. This was partially due to the shallow nature of the test pits and subtle color differences between the naturally occurring soil horizons. Another reason for the lack of color difference lies in the dynamics of sediment formation. Since most of the sediment formed from raindrops pulverizing soils at the

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(a)

(b)

Figure 3.8 Subsurface cracks (arrowed) formed at the base of a test pit prior to backfilling (a) and upon partial excavation (b), or sectioning, 30 days after the pit was backfilled. © 2002 by CRC Press LLC

base of the pit, throwing them into suspension in pooled water, the color remained uniform. The ability to recognize and record geotaphonomic artifacts of subsurface sedimentation may aid in determining whether a pit was dug and laid open in anticipation of a burial or a more spontaneous event occurring contemporaneously with the homicide. Several reference cases include subject or witness accounts of how clandestine graves were dug in preparation for homicides (Hays, 1995; Jackman, 1996; and Stuckey, 1981), but no research has been published identifying geotaphonomic characteristics of prepared graves. From the homicide investigator’s standpoint, indications of intent and planning may be reflected in the physical circumstances of the burial and types of tools used. Evidence that a grave was dug a day or more before the homicide would have significant investigative and prosecutorial impact, e.g., for those who had been told that the crime was not planned.

Compression/Depression Changes to surface contours in and around burial features fall into one of two categories: compression or depression. These geotaphonomic artifacts include the more traditional observations of primary and secondary depressions over clandestine inhumations as discussed in Hunter et al. (1996), Killam (1990), McLaughlin (1974), and Morse et al. (1983). Alternatively, they may include impressions left during the intentional compression of fill in a pit, or combinations of shoe and fabric impressions left in and around the burial feature during its excavation. Geotaphonomic evidence of compression or depression may be detected with aerial and pedestrian searches for the grave. The abovementioned sources as well as Avery (1977), Bewley (1993), Riley (1987), Stanjek and Fassbinder (1995), and others address the use of aerial photography in archaeology. Of key importance is the time of day during which such surveys are conducted. Multiple fly-overs in the morning and late afternoon take advantage of shadows created by low angle, i.e., oblique, sunlight across typically depressed graves. Every advantage may be needed in spotting a single 2 m ¥ 0.8 m depression among acres of undulating terrain. Primary depressions occur as freshly dug fill settles into a grave; secondary depression, when distinguishable, occurs as a result of the bloating from putrefaction followed by the release of gases and collapse of the cadaver’s abdominal region. Although primary depressions may be discovered during pedestrian reconnaissance, observation of a secondary depression requires more specific conditions. These include a faceup corpse position, shallow burial, and a postdeposition interval sufficient for bloating and collapse of the abdomen. Secondary depressions may occur after containers holding human remains deteriorate. Geotaphonomic artifacts may be misinterpreted as secondary depressions. The eroded remnants of holes dug into a grave by scavenging animals take on the appearance of secondary depressions. In most cases, a cross section of the feature, as well as documentation of the orientation of the body, will support or discount such an interpretation. Both primary and secondary surface depressions become subtler as time passes. Sedimentation, bioturbation, and cultural modifications to the landscape may obliterate compression and depression evidence over time. McLaughlin (1974) presents what might be considered early examples of empirical work in forensic geotaphonomy. In addition to offering a table of (estimated or observed) widths

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of disturbed areas associated with burials, McLaughlin (1974) contains a chart entitled “Depression Depth In Inches.” This chart presented depression depths in relation to soil types and burial feature depths. The ratios presented showed a precise association between depression depth and hole depth,* suggesting continued research on depression patterns is justified. Unfortunately, McLaughlin did not give the sources of his data. If based on experimentation, compression/depression studies should be replicated in a variety of soil, climate, and vegetation settings. The ability to predict or gauge clandestine pit depths from the measurement of surface depressions would be of obvious logistical value; for example, it might provide early information useful to confirm or deny subject or witness statements. Criminalists routinely recognize, preserve, and collect tire, shoe, or foot impressions left at crime scenes (Bodziak, 1986, 1995; Brennan, 1993; Hildebrand, 1995; Jasvja, 1993; and McDonald, 1993). These types of evidence constitute compressed soils within and around burial features. Hochrein (1997b, and subsequent unpublished experiments) documents the unavoidable creation of shoeprints and knee impressions as a result of the digger’s attempts to pack fill into the pit by stomping or tamping. Smaller, handheld digging implements require subjects to kneel or sit around the feature. Morse et al. (1983) note the recovery of a footprint at the base of a mock grave after 1 year of burial. As with subsurface sedimentation and desiccation, shoeprints and tool marks beneath remains may be blurred or destroyed as decomposition fluids and/or groundwater tables fill the interface between the burial feature and underlying substrate. Occasionally, compression evidence in the form of shoe heel prints may become commingled with tool marks, and may be confusing. In shovel use, one foot is used to force the tool’s blade into the soil. During such an operation, the heel of the shoe protrudes beyond the blade. If the shovel slips, the heel might slide down the newly exposed area of the grave wall leaving a curvilinear mark to the left or right of the shovel blade mark. In such instances, what might appear as two tools used in the construction of a burial feature would, in fact, be a combination of shoe print and tool mark. There are aspects of tool marks that consist solely of compression detail. Handle impressions left along the surface edge of pits result from that point on the handle used against the pit’s edge as a fulcrum to lever dirt out of the hole. Tools such as posthole diggers will tend to leave similar compression detail in deeper, straight-walled pits. Less apparent compression detail is impressed on the surface of the infilled pit if the shovel blade was slapped against the surface in an attempt to compress fill into the feature. Case History #6 A case that included the discovery of perhaps the most fragile example of compression detail involved the search of a victim’s basement. Four years after the reported disappearance of the victim, tenants happened upon some suspicious items in a basement once shared with the victim. The tenant’s cat, while scratching in an area it adopted as its litter area, unearthed bedding, bones, tape, and miscellaneous debris thought to be associated with the victim. With this discovery local authorities were summoned. The site was a half-walled, bin area in one corner of the basement. The area behind the wall was filled with landfill, and may once have been used to store coal. Large pieces * 14 mm of settlement were noted for each foot that holes were dug in packed sand or gravel. Holes dug into adobe clay exhibited 16 mm settlement for each foot in depth. Holes in loam soils settled at a rate of 33 mm for every foot of depth.

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Figure 3.9 Close-up of fabric impression detail left in a dirt floor.

of metal, building material, and other debris were first systematically removed from the surface of the site. An examination of the exposed surface revealed fabric impressions consistent with an individual kneeling near the spot at which the cat had unearthed the artifacts. Debris removed from above this compression detail suggested the marks were not created by the tenants. Since the soil holding the impressions was reasonably hard, the impressions were removed en bloc, packaged so they would not shift during transport, and taken to the laboratory for further examination (Figure 3.9). Excavation of the area continued with the creation of a 50 cm ¥ 50 cm ¥ 60 cm test pit and 90-cm deep soil cores sampled at 30-cm intervals across the adjacent area. The consistent, uninterrupted stratification of the fill outside the test area established there were no other burials. Bioturbation was limited to one corner exhibiting a rodent burrow. The skeletal elements unearthed by the tenant’s cat were determined by a forensic anthropologist to be nonhuman. To date, the victim has not been located. The processing of that scene did not resolve the case but did demonstrate the existence and resilience of fabric impressions in a sheltered environment.

Internal Compaction The sixth area of geotaphonomy involves internal compaction, or compressed areas of grave fill caused by movement of victims buried alive. Wood (1994) describes the possibility of such evidence in the Sacramento Boarding House Murders of the late 1980s:

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… he and the anthropologist saw an unusual compaction of dirt on either side of the victim’s wrapped legs, and a mound-like effect above the knees, as if the soil had been forced upward. A tunnel had been created between the victim’s wrapped legs, caused by the packing of the dirt on either side … it was possible, that (the victim) had awakened from her drugged stupor and begun jerking her wrapped legs… .

Unfortunately, the subterranean clues were not noticed until crime scene photographs were being reviewed after the exhumation of the bodies. Empirical studies of archaeological techniques for uncovering evidence of internal compaction are needed. Often victims are wrapped and/or exhibit such advanced decomposition that it is impossible to determine whether soil may have been inhaled. In cases where the potential exists that a victim was buried alive, the excavation methodology should involve the creation of sections perpendicular to the direction of any potential movement (side to side and bottom to top in the areas of the shoulders and knees, or back to front at the heel of the foot). This may reveal and define compaction indicative of post-deposition movement.

Excavation Techniques A wide variety of texts and empirical research on archaeological field techniques have been published (Barker, 1993; Connah, 1984; Dillon, 1993; Dirkmaat and Adovasio, 1997; Fladmark, 1978; Joukowsky, 1980; and others). Few, however, address forensically significant settings and none address the examination routines for all six types of geotaphonomic evidence. Given the unique nature of each buried crime scene, it would be impossible to assign one particular protocol to the excavation of all sites. Archaeology is a science that must be applied, not forced, upon sites (Hoshower, 1998). Forensic archaeology does, however, have two immutable requirements: excavations must be systematic and must consider the environment or context of the burial. Much like an autopsy, the body, or in this case the grave, must first be examined for superficial defects as well as trace and transfer evidence. The immediate establishment of a coordinate-based grid tied to a primary datum and elevation is one method to reconstruct the position and context of those defects and evidence. This 3-dimensional system of recording points throughout a site also assists in documenting the position of the body in relation to the site’s immediate topography. This may be crucial information for pathologists explaining the taphonomy of remains otherwise assumed to have been recovered from a level and unobstructed situation. Groundwater flow, surface erosion, and biota are all influenced by topography and, in turn, are part of the taphonomic process. The initial examination of the grave should include documentation of surface evidence of sedimentation and cracking, compression/depression artifacts, bioturbation, and tool marks. It is also at this phase that botanical and entomological sampling takes place in concert with defoliation across the grave, collecting and cataloging representative plant samples over and near the burial. Much like the pathologist cleans the areas around wounds to better see and document the underlying trauma, the removal of vegetation over a gravesite reveals the color, texture, and contour of the ground surface. This also provides a view of the ground surface more similar to that affected by the subject and victim. All environmental samples including core and column samples, as well as thermometer positions, associated evidence, and the remains themselves, are photographed and mapped

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in relation to the grid system and in relation to a primary or secondary datum situated outside the burial feature. To begin the systematic excavation of the grave, a technique found most expeditious by the author involves the creation of the archaeologist’s Y-incision, a small rectangular window near the center of the burial. The window is excavated down to the top of the remains. It allows a quick assessment of the burial depth and preliminary view of stratification. The clean, plumb sides of the box are then incrementally expanded toward the margins of the pit, leaving one or two sides of the box intact to maintain a section or profile above and across the remains (Figure 3.1a and b). In effect, this method of excavation, known as partial excavation or partexing results in a series of photographic and diagrammatic thin sections across the grave. As evidence or stratigraphic changes are encountered in the exposed profiles, they are photographed and mapped. Alexandrowicz (1985) offers an expeditious method of mapping profiles by placing transparent plastic sheets against the sections and tracing artifacts and strata onto individual sheets. Although the partexing method does not allow for the complete horizontal exposure of individual stratum as preferred by most archaeologists in traditional excavations, the same information can be diagrammed because both methods record data in 3 dimensions. Partexing does not involve the pedestaling of artifacts within the grave, i.e., preserving in situ on columns of fill. Pedestaling allows for dynamic photographs but is very time consuming. Pedestaled artifacts are also prone to be knocked off their columns during excavation. This inconvenience in traditional excavations has far greater implications in forensic examinations; the appearance of repositioned evidence, albeit slight or innocent should be questioned during deposition or trial. Archaeological excavation is so much a tactile experience that anything less precise than small hand tools reduces the excavator’s ability to sense horizontal and vertical changes in texture; however, specific archaeological protocols will be dictated by the nature of the crime scene or deposit site (Hoshower, 1998; Levine et al., 1984). Some scenes will require machinery or shovels to remove overburden to the original surface into which a pit or grave was dug (Bass, 1963). When utilizing heavy equipment, the investigator must consider whether the method will alter the appearance of the site from that which a subject might remember. The simple act of peeling off thin layers of soil with a backhoe or bulldozer in search of a grave outline may tear and drag root systems or uproot adjacent trees and rocks. Those same features may have been landmarks a subject or witness needs to remember the location of a burial. The use of heavy equipment must be a last resort, applied with surgical precision, and always involve the pulling of dirt toward a stationary machine with a smooth-edged blade or bucket. The forensic excavator should not use tools that might typically be used by a subject to create the clandestine grave (i.e., spades or military style entrenchment tools), and the forensic excavator’s tools must be clean and honed. Once the burial feature is located and defined, there is no excuse for continued use of large mechanical excavators. The clandestine pit or grave is the focus of the excavation. The undisturbed subsoils into which the pit was dug need not be excavated since they were not altered by the subject’s actions. To excavate the undisturbed areas may confound the interpretation of the site and creates unnecessary work for scene investigators. Vacuum equipment is appropriate and necessary to evacuate fill from the burial feature (Figure 3.10). The use of a wet/dry vacuum should not constitute excavation. The vacuum is employed in a cleaning technique to remove excavated fill which otherwise might be

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Figure 3.10 The application of crime scene vacuuming to aid in the archaeological excavation.

scraped or brushed into fine detail like desiccation cracks or tool mark striae. As with all excavated fill, vacuumed material must be screened. Most commercially available wet/dry vacuums do not have blades or other internal workings which might damage inadvertently suctioned evidence; however, care should still be taken in its use and it must be treated with the same attention to security and avoidance of cross-contamination as traditional evidence vacuums, and avoid decompositus or purge as well as heavy ground water. In such examinations, use of the vacuum is generally limited to debris from the walls of the grave. Another advantage in utilizing vacuums is to avoid arguments that the forensic investigator’s tool created tool marks attributed to the subject. The systematic and clean excavation of burial features includes the establishment and maintenance of a clean, vertical, and plumb profile, (or section) within the pit. This method most clearly reveals depositional and intrusive episodes above and below the primary evidence (Figure 3.1) and has the following advantages: 1. 2. 3. 4.

The excavation is forced to proceed in a controlled, systematic manner and pace. Contamination between strata is less likely. The excavator is constantly presented with a clear picture of stratigraphic events. At any time in the process, the excavator can compare stratification within the burial feature to that of undisturbed soils. 5. Stratification within the feature is more easily mapped and photographed as a series of slices, or thin sections. 6. Documents the in situ position of associated evidence, relationships between artifacts and the interfaces between depositional layers.

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7. Postburial intrusions into the feature, as well as bioturbation, are efficiently depicted. 8. Soil samples and soil columns are easily obtained and recorded.

Conclusions For forensic scientists, profilers, jurists, and jurors, the ideal crime scene evidence is submitted in as pristine a state as possible with its context recorded in as much detail as available. The integrity of forensic evidence and the conclusions drawn from that evidence remain contingent upon the manner in which the evidence was handled at its source. In cases of buried evidence, greater emphasis needs to be placed on recognizing and recording the burial environments. All too often forensic first responders recognize the value of the primary piece of evidence, the body, and direct their efforts at its extraction. In fact, the grave itself represents a second body of evidence, which deserves equal consideration because it was created or affected by witnesses to the burial. The application of the techniques briefly described above will inevitably extend the amount of time required to process crime scenes. The author would argue, from personal experience, that such investments of time are cost effective and necessary given the nature of the crimes under investigation. At a minimum, it is incumbent upon law enforcement to liaison with departments of anthropology or agencies which maintain qualified archaeologists versed in geotaphonomy and the special requirements of crime scene management, i.e., logistical constraints and procedures for handling evidence. Forensic anthropology courses for the investigator and criminalist need to concentrate more on aspects of archaeological photography, 3-dimensional mapping, basic principles of stratigraphy, botanical and entomological collection procedures and exhumation–conservation techniques. Law enforcement’s first responders frequently also have or share responsibility for the collection, documentation, and preservation of primary, associated, and trace evidence. The common denominator between the crime scene technician, forensic anthropologist, and forensic pathologist should be their systematic and holistic approaches toward the recovery and documentation of artifacts via methodologies, which are inherently site destructive.

Acknowledgments The author extends special thanks to the FBI’s St. Louis Evidence Response Team, Lincoln Police Department, Iowa Division of Criminal Investigation, and local Missouri law enforcement for their assistance in conducting training exercises which have proven invaluable toward empirical observations and the application of methodologies.

References Alexandrowicz, J.S. 1985 Rapid projected mapping: an alternative mapping technique for the Archaeologist, Historical Archaeology 19:79–85. Anon. 1981a Regional News, Texas. United Press International, Dateline: Galveston, TX, January 30.

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1981b Regional News, New York. United Press International, Dateline: Johnston, NY, February 18. 1984 Court Upholds Murder Convictions. United Press International, Dateline: Austin, TX, February 29. 1994 John Wayne Gacy runs out of time 15 years after bodies discovered, Rocky Mountain News, May 10, Section F:26A. Avery, T.E. 1977 Interpretation of Aerial Photographs, Burgess, Minneapolis, MN. Barker, P. 1993 Techniques of Archaeological Excavation, B.T. Batsford, London. Bass, W.H. 1963 The use of heavy power equipment in the excavation of human skeletal material, Plains Anthropologist 8(20):122–123. Bevan, B.W. 1991 The search for graves, Geophysics 56(9): 1310–1319. Bewley, R.H. 1993 Aerial photography for archaeology. In Archaeological Resource Management in the U.K.: An Introduction, edited by J.R. Hunter and I.B.M. Ralston, pp. 197–204. Stroud, Sutton Pub., Gloustershire, U.K. Bock, J.H. and D.O. Norris 1997 Forensic botany: an under-utilized resource. Journal of Forensic Sciences 42(3):364–367. Boddington, A., A.N. Garland, and R.C. Janaway 1987 Death, Decay, and Reconstruction: Approaches to Archaeology and Forensic Science, Manchester University Press, Manchester, U.K. Bodziak, W.J. 1986 Shoe and tire impression evidence, FBI Law Enforcement Bulletin July. 1995 Footwear Impression Evidence, CRC Press, Boca Raton, FL. Brennan, J.S. 1993 Dental stone for casting depressed shoemarks and tyremarks, Journal of the Forensic Science Society 23:275–286. Brothwell, D.R. 1981 Digging up Bones: The Excavation, Treatment, and Study of Human Skeletal Remains, Cornell University Press, Ithaca, NY. Connah, G. 1984 Australian Field Archaeology: A Guide to Techniques, Humanities Press, Atlantic Highlands, NJ. Conyers, L.B. and D. Goodman 1997 Ground Penetrating Radar: An Introduction for Archaeologists, Altamira Press, Thousand Oaks, CA. Curwen, E. and E.C. Curwen 1926 The efficiency of the scapula as a shovel, Sussex Archaeological Collections 67:139–145. Davenport, G.C. 1996 Geophysical Surveying, A Handbook for Criminal Investigators, NecroSearch International, Lakewood, CO. Dillon, B.D. 1993 Practical Archaeology: Field and Laboratory Techniques and Archaeological Logistics, University Museum Publications, Philadelphia, PA.

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Dirkmaat, D.C. and J.M. Adovasio 1997 The role of archaeology in the recovery and interpretation of human remains from an outdoor setting. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 39–64. CRC Press, Boca Raton, FL. Donovan, D.T. 1966 Stratigraphy: An Introduction to Principles, George Allen and Unwin, London, U.K. Drucker, P. 1972 Stratigraphy in Archaeology: An Introduction, Modules in Anthropology 30, Addison-Wesley, Reading, MA. Dunbar, C.O. and J. Rodgers 1957 Principles in Stratigraphy, John Wiley, London, U.K. Fladmark, K.R. 1978 A Guide to Basic Archaeological Field Methods, Simon Fraser University, Burnaby, B.C., Canada. Hall, D.W. 1988 Contribution of the forensic botanist in crime scene investigations, The Prosecutor, Summer: 35–38. 1997 Forensic botany. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 353–366. CRC Press, Boca Raton, FL. Harris, E.C., M.R. Brown III, and G.J. Brown (editors) 1993 Practices of Archaeological Stratigraphy, Academic Press, San Diego, CA. Hays, T. 1995 Man Charged with Murder, Mutilation of Robbery Witness. The Associated Press, Dateline: New York, February 2. Heizer, R.F. and J.A. Graham 1967 A Guide to Field Methods in Archaeology: Approaches to the Anthropology of the Dead, National Press, Palo Alto, CA. Hildebrand, D.S. 1995 Footwear, the missing evidence, Minutiae, November–December: 2–11. Hill, S.H. 1982 An examination of manufacture-deposition lag for glass bottles from late historic sites. In Archaeology of Urban America The Search for Pattern and Process, edited by R.S. Dickens, Jr., pp. 291–327. Academic Press, New York. Hochrein, M.J. In preparation. Sedimentation as a Geotaphonomic Agent (unpublished manuscript). 1997a Buried crime scene evidence: the application of geotaphonomy in forensic archaeology. In Forensic Dentistry, edited by P. Stimson and C. Mertz, pp. 83–99. CRC Press, Boca Raton, FL. 1997b The dirty dozen: the recognition and collection of toolmarks in the forensic geotaphonomic record, Journal of Forensic Identification 47(2):171–198. 1998 An Autopsy of the Grave: The Preservation of Forensic Geotaphonomic Evidence. A Paper Presented at the 50th Annual Meeting of the American Academy of Forensic Sciences, February 14, 1998, San Francisco, CA. Hochrein, M.J., J. Gabra, and S. Nawrocki 1999 The Buried Body Cases Content Analyses Project: Patterns in Buried Body Investigations. A Paper Presented at the 51st Annual Meeting of the American Academy of Forensic Sciences, February 18, 1999, Orlando, FL.

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Horvath, F. and R. Meesig 1998 A content analysis of textbooks on criminal investigation: an evaluative comparison to empirical research findings on the investigative process and the role of forensic evidence, Journal of Forensic Sciences 43(1):133–140. Hoshower, L.M. 1998 Forensic archaeology and the need for flexible excavation strategies: a case study, Journal of Forensic Sciences 43(1):53–56. Hunter, J., C. Roberts, and A. Martin 1996 Studies in Crime: An Introduction to Forensic Archaeology, B.T. Batsford, London. Imaizumi, M. 1974 Locating buried bodies, FBI Law Enforcement Bulletin 43(8):2–5. Jackman, T. 1996 Brother Admits Guilt in Deaths; James Vest Agrees to Testify on Slaying of Two Cocaine Couriers, The Kansas City Star, January 3, C1. Jasvja, M. 1993 Estimation of stature from footstep length, Forensic Science International 61(1):1–5. Joukowsky, M. 1980 A Complete Manual of Field Archaeology, Prentice-Hall, Englewood Cliffs, NJ. Killam, E.W. 1990 The Detection of Human Remains, Charles C Thomas, Springfield, IL. Laska, P.R. 1996 Forensic search of a landfill, Journal of Forensic Identification 46(1):7–12. Levine, L.J., H. Campbell, Jr., and S. Rhine 1984 Perpendicular forensic archaeology. In Human Identification: Case Studies in Forensic Anthropology, edited by T.A. Rathbun and J.E. Buikstra, pp. 87–95. Charles C Thomas, Springfield, IL. McDonald, P. 1993 Tire Imprint Evidence, CRC Press, Boca Raton, FL. McLaughlin, J.E. 1974 The Detection of Buried Bodies, Andermac, Yuba City, CA. Micozzi, M.S. 1991 Postmortem Change in Human and Animal Remains, A Systematic Approach, Charles C Thomas, Springfield, IL. Morse, D., J. Duncan, and J.W. Stoutamire (editors) 1983 Handbook of Forensic Archaeology and Anthropology, Rose Printing, Tallahassee, FL. Noël Hüme, I. 1970 A Guide to Artifacts of Colonial America, Knopf, New York. Owsley, D.W. 1995 Techniques for locating burials with emphasis on the probe, Journal of Forensic Sciences 40(5):735–740. Paton, T.R., G.S. Humphreys, and P.B. Mitchell 1995 Soils: A New Global View, Yale University Press, New Haven, CT. Pydokke, E. 1961 Stratification for the Archaeologist, Phoenix House, London, U.K. Rathje, W.L. et al. 1992 The archaeology of contemporary landfills, American Antiquity 57(3):437–447.

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Riley, D.N. 1987 Aerial Photos and Their Applications, University of Pennsylvania Press, Philadelphia, PA. Roberts, C.A., F. Lee, and J. Bintliff 1989 Burial Archaeology: Current Research, Methods, and Developments, British Archaeological Series International Reports 211, Oxford, U.K. Ross, B. 1994 Two Pairs of Sneakers Found Near Bodies: Overpass Searched Slowly, The Times-Picayune, May 29:B1. Schiffer, M.B. 1987 Formation Processes of the Archaeological Record, University of New Mexico Press, Albuquerque, NM. Skinner, M. and R.A. Lazenby 1983 Found! Human Remains: A Field Manual for the Recovery of the Recent Human Skeleton, Archaeology Press, Simon Fraser University, Burnaby, B.C., Canada. Spennemann, D.H.R. and B. Franke 1995 Archaeological techniques for exhumation: a unique data source for crime scene investigators, Forensic Science International 74(1, 2):5–15. Stanjek, H. and J.W.E. Fassbinder 1995 Soil aspects affecting archaeological details in aerial photographs, Archaeological Prospection 2:91–101. Stuckey, T. 1981 White Teenager Sentenced to 10 Years in Killing of Black Classmate. The Associated Press, Dateline: Denton, MD, September 9. Ubelaker, D.H. 1989 Human Skeletal Remains: Excavation, Analysis, Interpretation, Taraxacum, Washington, D.C. Weil, G.J. and R.J. Graf 1992 Infrared Thermographic Detection of Buried Grave Sites. Manuscript on File, Entech Engineering, St. Louis, MO. Whalen, M.E. 1990 Defining buried features before excavation: a case from the American southwest, Journal of Field Archaeology 17:323–331. Willey, P., and A. Heilman 1987 Estimating time since death using plant roots and stems, Journal of Forensic Sciences 32(5):1264–1270. Wilson, W. 1993 Puente “Acted Shocked” by First Body. Sacramento Bee, February 25, B:1. Wood, W.P. 1994 The Bone Garden, Pocket Books, New York. Wynn, J.C. 1986 Review of geophysical methods used in archaeology, Geoarchaeology 1(3):245–257.

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Forensics, Archaeology, and Taphonomy: The Symbiotic Relationship

4

JULIE MATHER SAUL FRANK P. SAUL Contents Introduction The Recreation of Past Events Maya Mountains: Decapitation and Dismemberment? Cuello: What Happened Here? Where Is the Rest of the Body? Chan Chich Tomb: Just a Scatter of Fragments, Offerings, or a Primary Burial? Forensic Applications Taphonomy, Pseudopathology, and Pseudotrauma: Roots vs. Blood Vessels Roots vs. Cannibalism Roots vs. Projectiles Roots vs. Incised Defects Other Possible Sources of Confusion Blood Vessel Impressions Misinterpreted as Cut Marks Trauma Assessment Based on Known Trauma Sharp-Force Injury Examples Turnpike Case A Known Sharp-Force Injury Case A Probable Sharp-Force Injury Case Conclusion Acknowledgments References

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Introduction Physical anthropologists who work only with ancient remains may be lulled into a sense of false security regarding their ability to designate individual skeletal remains as being of a certain sex and a specific age and perhaps to diagnose a lesion and associate it with a degree of disability. Such pronouncements on ancient remains are unlikely to be questioned, except rarely by rising graduate students or rival colleagues in need of a controversy. Unfortunately, the pronouncer cannot be proven right or wrong, as the next of kin are long dead. Forensic anthropologists, however, quickly learn that an error in assigning sex or a too narrow or inaccurate assessment of age will be discovered when the unknown remains are identified, unless, of course, the error results in non-identification. Access to identified cases as well as known individuals on our autopsy tables provides forensic anthropologists with continuing education and testing in regard to sex determination, age estimation, evaluation of ancestry, functional health status assessment, indications of skeletal trauma, etc. They also give us an opportunity to check the standards themselves. Metric sex and ancestry formulae based on ancient populations (therefore unidentified individuals) are potentially inaccurate, and formulae based on dissecting room populations are potentially out of date. Even modern forensic case-based formulae can result in misclassifications. In short, the data forming the basis of decision-making require continuing refinement. In essence, forensic anthropology practice serves as a “reality check” for academic assumptions and all physical anthropologists need to proceed with caution (Saul and Saul, 1994). The interaction between studies of ancient and modern skeletal remains should be a two-way street. Working with the poorly preserved remains of the ancient Maya has enhanced our ability to recognize, interpret and reconstruct very fragmentary forensic remains (Hammond et al., 1975; Saul, 1972, 1973, 1975, 1977, 1982; Saul and Saul, 1989, 1991, 1997a,b; Saul et al., 1995). This has been helpful in both identification analyses and interpretation of trauma and “weapon signatures” in support of determining cause of death. The latter activity in turn provides perspective for the interpretation of trauma in ancient remains. We also have the opportunity to see what happens in ancient cases of injury or disease in the absence of modern medical intervention. Familiarity with modern clinical cases then cautions us not to over-interpret or over-emphasize the physical disability that might have resulted. Finally, modern taphonomic research concerning decomposition, disarticulation, and postmortem disposition of remains in general supplies a basic framework for the recovery and interpretation of the human remains encountered in both ancient and modern contexts (Haglund and Sorg, 1997). Working in both areas is symbiotic and even synergistic, as we hope to demonstrate in the following examples.

The Recreation of Past Events “Forensic Science is used to predict not the future but the past.” Henry Lee, 1998

An archaeologic excavation and a crime scene are similar in many ways. The goal of investigators working at each is to recreate a past event — in the case of archaeology, many past events going back over hundreds, even thousands, of years. Each endeavor can reach

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its goal only through preserving the scene by limiting access and then documenting, gathering, preserving, and interpreting physical evidence. In both cases, this is best done by a team of specialists. Techniques used to excavate archaeologic burials (Ubelaker, 1978), with careful measurements and documentation (photos, sketches, and written notes) of the exact location of all items in situ, can provide the basis for recreating the scene whether it be a recent crime scene (Lee, 1994, Dirkmaat and Adovasio, 1997) or an ancient one (Scott and Connor, 1997). In the former, of course, law enforcement personnel — evidence specialists in particular — should be present to maintain the chain of custody. Physical evidence from any burial is best gathered by a team that includes physical anthropologists and archaeologists. Although these two areas of expertise may overlap, each has specialized skills and knowledge. Experience in the Maya area has shown that much more information can be gathered if a physical anthropologist is present for burial removal. Typically, ancient Maya skeletal remains are extremely poorly preserved and incomplete due to the tropical climate with its intense rainy and dry seasons and rapidly growing vegetation. In many instances, basic information regarding who the individual was (sex, age, stature, cultural modification, pathology, etc.) may be lost upon removal unless the fragmentary bones can be examined and measured while still in the ground. Sorting out what happened to the individual during life, at death (perimortem trauma), and postmortem (taphonomic events) can be difficult if clues are lost. Inasmuch as subsequent analysis is based on the in situ diagram, accurate determinations should be made as to what bone is present in a specific location and whether or not it is in appropriate anatomic position.

Maya Mountains: Decapitation and Dismemberment? As indicated above, both forensic and archaeologic scenes mandate knowing the exact orientation of bones in order to differentiate death events from postmortem events, and to interpret these events. A rock shelter excavation in the Maya Mountains of Belize illustrates this point. Unlike most Maya burial sites, preservation in the rock shelters seems to be excellent. The soil in rock shelters remains fairly dry, and due to locations near the tops of steep hillsides and cliffs, remains free of flooding from run-off. Additionally, there are few intrusions of the plant roots that in most other Maya burials produce major bone damage. In this case, what at first appeared to be two separate burials became a confusing, intimate arrangement of three individuals. Uppermost was a fully articulated adult female (based on pelvic characteristics) in a tightly flexed, knee-to-chest position, face down, with her head to the north and her arms crossed at her waist (left forearm closest to the body). Her left cheek rested on large stones that had been placed on the chest of an articulated adult male (also based on pelvic characteristics). He lay in an extended supine position (head to south) with his right arm at his side and the left arm bent slightly at the elbow, allowing his left hand to rest near his right hand. His upper torso was covered by the flexed or kneeling female. Across the knees and upper legs of the male were arranged the postcranial bones of a child approximately 9 to 11 years old (Figure 4.1). (The child’s age was determined using standard dental development and bone growth parameters.) Removal of the female’s torso revealed the articulated skull and mandible of the child resting on the right shoulder of the male, beside the male’s own skull and mandible. The right knee of

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Figure 4.1 Possible family burial in the Maya Mountains, Belize, rock shelter. Fragments of the flexed female’s skull (arrow) rest on rocks and dirt over the thorax of the adult male, whose lower body extends to the south. Bones of the child are scattered over the legs of the adult male.

the female rested directly on the skull of the child. Her left knee rested directly on the skull of the male. Attempts to figure out the position of the child could not reconcile what appeared to be articulated portions with any conceivable body position. The child’s pelvic bones were against the male’s right femur and ribs were scattered over both femora and tibiae (especially the right), with lumbar vertebrae tumbled between. The left scapula and humerus were lying, anterior surface upward, beside the male’s left femur. They appeared to be articulated and in a north–south orientation. The right humerus and scapula were east of this arrangement. However, the distal end of the humerus was closest to the glenoid cavity. The first two cervical vertebrae were tucked in under the left ilium of the male, with what appeared to be the rest of the cervical and thoracic vertebrae roughly lined up (north–south) about 2 in. north of C1 and C2. Whether these remaining vertebrae were

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Figure 4.2 Cervical vertebrae of child in the rock shelter. Placement of C1 (upside down) on top of C2 (also upside down) indicates vertebrae were defleshed when interred.

in exact anatomic order could not be determined. Had the child been decapitated and dismembered before being placed in the ground? We closely examined the child’s left radius and ulna in situ, lying in a north-south orientation east of the male’s right leg, some distance from the left humerus. They were lying close together, parallel, as one would expect in fleshed remains — except one of them had been flipped end for end, distal radius pointing south and distal ulna pointing north. An impossible situation if held together by soft tissue when buried. We turned our attention to the first two cervical vertebrae. C1 was sitting on top of C2, as one might expect in life; however, each individual vertebra was turned upside down (Figure 4.2). Again, impossible if fleshed. Upon closer examination we saw none of the incised or chopping marks indicative of possible decapitation, dismemberment, or defleshing. No signs of carnivore or rodent feeding or other such manipulation were evident. The separation of skull and mandible could have taken place early on, as these two skeletal elements are generally the first to become disarticulated during decomposition, an event that should have taken place fairly quickly in the extreme heat and humidity of the tropics. The disarticulation of cervical vertebrae will also occur well before complete skeletonization of the rest of the body. However, the disarticulation of shoulder, elbow, wrist, ribs, lower back, and pelvis suggest that the child was probably skeletonized and disarticulated when placed in the grave with the male as a secondary burial (Bass, 1997; Micozzi, 1991; Rodriguez and Bass, 1983, 1985). We conjectured that the child was probably the first to die. We have no way of knowing whether or not the child was initially buried following its death. Some time later, after the child had become skeletonized and disarticulated, the male died. When he was buried, the child was removed from his/her original resting place and interred with the male (the father?). The child’s skull and mandible were put on the right shoulder of the male, beside the male’s own head. The careful arrangement of the rest of the child’s bones told us that an attempt had been made to maintain the relationships in which these bones had been

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originally found. When the female (the mother?) died, either at the same time or some time later, she was placed in the same grave, kneeling over them, perhaps in a protective manner. We hope to determine whether the three are indeed related through DNA studies. This was a far cry from the decapitation and dismemberment that a less careful examination in situ might have suggested. Additionally, forensic experience and research reported in forensic literature enabled better understanding of the postmortem events involved.

Cuello: What Happened Here? Where Is the Rest of the Body? Not only is good visual and written documentation important to interpreting burial information, but continuity of investigators can also play a part. A full year passed, until the next excavation season, before we understood the taphonomy of the following burial. The skeleton that we were excavating at the Preclassic Maya site of Cuello (Saul and Saul, 1991, 1997b) in northern Belize appeared at first to be a simple extended supine burial. The pelvis and lower extremities were present and articulated, although poorly preserved. The position of the skull (face turned to the right) and clavicles seemed normal enough. But there was no sign of arm bones where they should have been, and no ribs or vertebrae. Eventually, we discovered the right arm was indeed present, positioned with a slight bend at the elbow, hand and wrist missing, laid along the long axis of the burial to the right of center. The distal radius had an unusual clubbed shape. A few ribs were stacked on the humerus, forming a semicircle opening to the right (laterally). At the upper end of the curve formed by the ribs were the first two cervical vertebrae, one atop the other, with the odontoid process of C2 pointing to the sky. The left arm, scapulae, vertebrae, and remaining ribs were absent (Figure 4.3). The skull appeared to be that of a female. There were no obvious signs of decapitation, defleshing, or disarticulation on the skull, mandible, cervical vertebrae, or left arm, although poor preservation could have masked them. We examined the pelvis in situ, as it seemed to be too fragile to survive excavation in good enough condition to yield information later in the lab. Pelvis morphology was definitely that of a female. Bone fragments from the right wrist and hand were near the right hipbone and those of the left at the left hipbone. This suggested that she had originally been buried with her arms extended at her sides. But where was the rest of her skeleton, and why had it been removed? And why the odd arrangement of right arm, ribs, and cervical vertebrae? The Maya, when engaged in remodeling and construction projects or in digging graves, often accidentally cut into and through previously existing burials. (We have excavated one individual whose grave cut passed through and disrupted five earlier burials.) Bones thus encountered were apparently usually tossed into the fill or put in with the subsequent burial. Bones and teeth of others were also often used as grave goods — placed in with the dead as offerings. But the arrangement here was unusual. Perhaps the burial was inadvertently disturbed by a later grave cut, removing thorax and arms. This would have to have been after decomposition had progressed to disarticulation and skeletonization, and perhaps after the grave location, and even its existence, had been forgotten. For unknown reasons some of her bones were laid back into her resting place and the intruding grave cut, unused, was filled in. Possibly the unique placement of the bones had some significance to the Maya. But where were the rest of her bones? The excavation season soon ended with that question still unanswered. © 2002 by CRC Press LLC

Figure 4.3 Disturbed and then rearranged extended burial, Cuello, Belize. Although skull, pelvis, and legs are in appropriate positions, only the right arm is present, laid out along the midline of the torso. Several stacked ribs (wide arrow) form a “C” on top of the humerus and cervical vertebrae (narrow arrow) are piled at the top of the “C.”

Next season, we were excavating another confusing arrangement of bone, trying to figure out if it was a secondary or primary burial, and if primary, how the body was positioned. (The ancient Maya buried their dead in many positions, including flexed, seated, face down, prone, supine, and with various arrangements of head, arms, and legs. One of the challenges of Maya burials is trying to figure all this out for each burial.) What we were uncovering appeared to be pieces of humerus, radius, ulna, ribs, scapulae, and vertebrae all jumbled together, in the same part of the excavation site that had produced the incomplete female, but at a lower level. Further excavation revealed bones of a left arm, with the distinctive clubbed shape of the left distal radius matching that of the right radius from the year before. The other bone fragments filled in the gaps — completing her skeleton with no duplications. Examination

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of excavation maps from the previous season revealed that this cluster of bone was located near where her left shoulder would have been and several inches deeper. Perhaps after intruding on her grave some bone was retrieved and replaced with care while the rest of it was dumped in with the fill. Careful excavation beneath and around a primary grave may uncover important information that might otherwise be missed and proper documentation can demonstrate relationships.

Chan Chich Tomb: Just a Scatter of Fragments, Offerings, or a Primary Burial? We could not be present during the excavation of a tomb at Chan Chich (Robichaux, 1998), a Maya site in northern Belize. Small fragments of bone were found scattered around and within 11 vessels found on the tomb floor. There were two separate groups of teeth. Perhaps this represented a secondary burial? Or was it a primary burial? In any event, the bone fragments within the vessels could be offerings, as could the teeth — neither possibility uncommon in the Maya area. The excavators were careful and followed our guidelines for recording the locations of bone fragments and teeth. They did this by measuring and recording the positions of bone fragments relative to individual vessels, after mapping in the vessels. With a diagram of the tomb and its vessels, we recreated the original relationships between vessels, bones, and teeth. Then we examined the fragments. Cranial fragments were at the south end, vertebral and rib fragments scattered down the middle to the north, fragments of arm bones on each side, pelvic fragments lay north of the vertebrae and leg fragments further north and to the sides. There were no apparent duplications. The fragments represented a large male with his head to the south. Locations of two identifiable scapula fragments indicated a supine position. The group of teeth furthest south, found among cranial fragments, were all maxillary teeth, while the group of teeth north of them, found mixed in with cervical vertebra fragments, were all mandibular teeth. These are logical locations for the dentition of a single individual, with the mandible dropping toward the chest during decomposition. The fragments of bone found within the vessels were from the bones found nearest these vessels on the tomb floor. Some fragments from within the vessels could even be joined to fragments from outside the vessels. This suggested that the body of the individual was placed on some sort of organic platform, and at least some of the vessels were placed beneath this platform. When the platform decayed and disintegrated, the skeletal remains dropped down onto and into the vessels. A small fragment of what is thought to be wood was found on the tomb floor. Without careful recording and documentation during excavation, this information would never have been obtained. However, even this detailed recording might have been insufficient for understanding the subtleties of the individually flipped cervical vertebrae in the previously discussed rock shelter burials. It is still important to have a physical anthropologist participate in the excavation, if possible.

Forensic Applications These and other excavations of ancient Maya skeletal remains provide lessons that apply to the forensic arena. Receiving an inadequately documented bag of bones in the lab, whether forensic or ancient, means that we have already lost information. This information loss is © 2002 by CRC Press LLC

most critical in forensic cases, where a small detail can be crucial in the resolution of a case and thereby can profoundly affect the lives of others. Having a physical anthropologist experienced in excavation involved in recovery/excavation of remains is also crucial. As seen in the Maya examples above, knowing the exact location and orientation of bones and bone fragments relative to each other and objects in the ground, and being able to retrieve information from the bones while still in the ground, may make all the difference in distinguishing trauma from postmortem process and in understanding what the sequence of events may have been. Knowledge of the normal decomposition and disarticulation process, based on our own forensic work and the forensic literature, helps to make this understanding possible (Bass, 1997; Micozzi, 1991; Rodriguez and Bass, 1983, 1985). Taphonomy, Pseudopathology, and Pseudotrauma: Roots vs. Blood Vessels In 1954 the junior author was asked to evaluate skeletal remains encountered at a construction site. The coroner had announced to the media that the remains were those of several individuals who had come to a violent end (indicated by multiple fractures) in recent times (indicated by the presence of blood vessels). Unfortunately, the multiple fractures were postmortem and probably due to the excavation process (broken edges were rough, jagged, and unstained by soil), and the blood vessels were plant roots. Skeletal and dental features indicated that the individuals were of ancient Native American origin. We have subsequently encountered many instances of misinterpretation of pathology and trauma, both in person and in the literature. Our presentations to forensic and academic groups stress the importance of ruling out taphonomy and normal variation as explanations before judging a lesion or defect to be pathologic or traumatic in origin. As a consequence of working in the Maya area where thirsty living roots extend to depths of at least 4.7 m below the surface of the ground, we have developed great respect for the ability of acid-secreting roots to modify bone and even dental enamel, thereby mimicking abnormality. Roots vs. Cannibalism Pencil-sized roots may travel through medullary canals and split sturdy long bone shafts while various size roots disintegrate the spongy articulations (Figure 4.4). The unwary might wonder if they were dealing with the aftermath of cannibalism or some aspect of secondary burial procedures if they had not seen the roots in situ. When seen in context, fragments of long bones split lengthwise by roots traversing the medullary canal will generally remain in proper relation to each other (Figure 4.5). Occasionally, roots can be seen on the external surface as they pass through the cortex, but often they are inside the medullary canal, producing the fractures by expansion from within. Such fractures may not even be visible initially, but the bone may come apart when recovery is attempted. Sometimes the bone will be tied down by rootlets passing on into the soil. If not seen in context, cannibalism can still be ruled out. Long bone fragments produced by root action will not show those characteristics suggested by White (1992) and Turner and Turner (1999) as indicative of cannibalism. These include cut marks at muscle attachments (defleshing) and near articulations (disarticulation/dismemberment), percussion marks produced by tools used to break shafts open to get at marrow, and pot polish on bone ends from cooking and burning, seen preferably, although not always, in combination. © 2002 by CRC Press LLC

Figure 4.4 Root-damaged proximal tibia with roots still in place (Ancient Maya, Belize).

Figure 4.5 Flexed burial (Ancient Maya, Belize). Long bone shafts have been split by small

roots that can be seen in and around the burial. Articular ends have been completely destroyed.

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Figure 4.6 Occipital bone penetrated by root visible within opening. Note lace-like pattern on cortex due to fine root action. Edge of foramen magnum can be seen at bottom of photo (Ancient Maya, Belize).

Roots vs. Projectiles Roots may also create openings that might be misinterpreted as due to a bullet or some other kind of projectile or piercing device (Figure 4.6). Entrance openings produced by projectiles during the perimortem interval will normally bevel inward (inner dimensions of the defect will be larger than the outer dimensions) while the exit will show some outward beveling. Such openings often are accompanied by radiating and sometimes concentric fractures. Openings caused by roots will show none of these characteristics, although bone weakened by root intrusions is more likely to fracture. These fractures, however, will be more jagged and random and not show the characteristics of perimortem fractures (curved or straight lines, beveling, tapering, radiating and concentric fractures). Roots vs. Incised Defects Changes to bone surfaces due to root erosion might be misinterpreted as incised defects or the caries sicca of treponemal infection and the scouring of dental enamel might confuse those interested in dental pathology. Incised defects, however, are usually straight and often involve multiple parallel grooves (see Symes, this volume). In cross section they are often V-shaped, whereas grooves caused by roots will have rounded floors (Figures 4.6, 4.8, 4.9). Roots also tend to meander over the surface, creating wavy lines or even a lace-like pattern (Figure 4.6). Other Possible Sources of Confusion Animals and insects also help create some pseudopathology and pseudotrauma (Haglund, 1997a,b; Haskell et al., 1997; Merbs, 1997; Murad, 1997; Rodriguez, 1997; Symes, this volume; Ubelaker, 1997). In addition, roots may displace bones, teeth, and artifacts, as do animals, insects, and other processes of bioturbation. These processes should always be considered when analyzing

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body orientation, possible dismemberment, etc. within the grave. The common Maya practice of burying their dead within rubble fill, often below floors, adds another factor. These burials are literally floating in the rubble (made up of cobbles and other stones of various sizes plus ceramic fragments and other bits and pieces). As the rubble shifts over time the bones are broken up and teeth, in particular, disappear downward into crevices between the stones.

Blood Vessel Impressions Misinterpreted as Cut Marks Although forensic anthropology was not initially involved, the approaches and materials we used to clarify the origin of certain temporal region grooves overlap those of forensic anthropology. In 1981, Zimmerman et al., describing the paleopathology of a Peruvian mummy, listed the presence on the mummy’s skull cap of “…a slightly curved, incised wound 20 mm long, 2 mm wide and less than 1 mm deep” (p. 498) and also referred to it as “an old incised wound” (p. 499). The location and configuration of the “curving incised wound” as shown in their Figure 1 suggested to us that it was actually the impression that is sometimes produced by the pulsation of the frontal (or anterior) branch of the superficial temporal artery. This artery, which is a terminal branch of the external carotid artery, is used by anesthetists and others when they check the temporal pulse (Goss, 1973). Illustrations from several anatomy texts show how the placement of the superficial temporal artery may vary in regard to its superimposition on bone or frontalis muscle. Goss (1973), for instance shows the artery upon frontalis whereas Lockhart et al. (1959) show a portion of it lying lateral to frontalis. We assume that the groove on bone is created when the frontalis muscle does not intervene. We had previously seen similar impressions and assumed that they were vascular impressions of the sort that T. Dale Stewart had long ago indicated had been “erroneously interpreted as results of cauterizations of long bones” (1937, 1966). Wells (1963a,b) reviewed some of the same materials (without referencing Stewart) together with several other instances that were previously attributed to tight bandaging or healed wounds associated with cuts, fractures, postmortem root erosion, or worm action. Wells, like Stewart, ascribed these grooves to vascular impressions based on their anatomical context, together with some insights from surgical practices. Campillo (1977) also suggested a vascular origin for temporal area frontal bone grooves. Campillo’s work noted that this groove was listed earlier by Testut (1911) who considered it a non-constant, but frequently found (20–25%) vascular groove related to the superficial temporal artery. It is obvious that the vascular origin of this feature has been accepted for some time, but the feature continues to be misinterpreted in both paleopathologic and forensic contexts (personal communications from Suchey and many others). In 1983, in response to the Zimmerman et al. article, we began to gather information on this apparently controversial subject. We were able to demonstrate the vascular relationship using a cadaver from the Medical College of Ohio dissecting room that shows the scalp (which is loosely attached in this area) peeled back to demonstrate a direct relationship on both sides between the frontal branch of the superficial temporal artery (embedded in the scalp) and the groove in the frontal bone (Figure 4.7).

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Figure 4.7 Left frontotemporal region of adult white male cadaver. The scalp has been peeled

superiorly to demonstrate the direct relationship between the superficial temporal artery embedded in the scalp tissue (above) and its groove in the frontal bone (below). (The temporalis muscle is to the right of the groove.)

We also surveyed a small sample (the first 10 males and first 10 females) from the Hamann-Todd Collection, a well-documented and studied dissecting room population obtained by the former Western Reserve University Medical School (now located at the Cleveland Museum of Natural History). The frequency is even higher (50%) than that previously indicated by Testut and it occurs in different frequencies in males (40%) and females (60%) in this sample. Our sample included 14 white individuals, of whom 5 (36%) exhibited the groove, with its presence noted in 2 of the 8 males (25%) and 3 of the 6 females (50%). Of the 6 black individuals, 5 manifest the groove (83%). It was present in both of the males (100%) and 3 of the 4 females (75%). Only 2 out of the 10 who show the feature also demonstrate pathology (of uncertain origin) in the vicinity of the marking and the listed cause of death offers no obvious association with presence of the marking. These blood vessel impressions do not appear to be age related inasmuch as they are present in both the oldest (age 70) and the youngest (age 19) of the individuals in this sample, and we have also found them in a commercially prepared neonate skull. The Hamann-Todd specimens and other modern and ancient specimens show grooves that vary in size, shape, and number of branches and often show marked variation from the left to the right side in the same individual. In 1984, with Dr. Delmas J. Allen (electron microscopist) and Dr. R.A. Burns (oral pathologist), we conducted a scanning electron microscopic evaluation of the previously mentioned Peruvian specimen. The scanning electron micrographs revealed the smooth channels and pores for branching vessels that are associated with blood vessel morphology rather than the straiae associated with incised defects (Shipman and Rose, 1984). In fact, when we presented our findings at the 1984 Paleopathology Association meetings in Philadelphia (Allen et al., 1984; Saul and Saul, 1984), the late Dr. Walter Putschar called our attention to the presence of smooth muscle impressions.

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Examination of the unprepared specimen with lower magnification or even the naked eye is usually sufficient to make the diagnosis. Knowledge of normal anatomical variation is the key (Saul and Saul, 1993). Similar blood vessel impressions may be found on other bones.

Trauma Assessment Based on Known Trauma Archaeologists and bioarchaeologists delight in theorizing violent and bloody deaths when describing ancient remains. Skulls crushed by blunt force, decapitations, dismemberments, and human sacrifices make for much more interesting reading. Familiarity with coroner/medical examiner cases of known trauma can be essential to interpreting and indeed recognizing perimortem trauma, and differentiating it from taphonomic processes. Lack of bony signs of a violent end, however, do not necessarily prove that the individual died a natural death. People may be murdered by sharp force and gunshot as well as with other equally lethal means (e.g., poison, suffocation, hanging) with no apparent bone defects (Saul and Saul, 1999). Nonetheless, with archaeological remains it is best to follow the old adage that the simplest answer is usually the best, and violence and mayhem should not be suggested until taphonomic changes have been ruled out and specific signs of perimortem trauma are present. In forensic cases we also rule out taphonomic changes and then recognize conclusive indications of perimortem trauma. But then we must go one step further by demonstrating to the coroner/medical examiner, and eventually the court, that recognition and interpretation of such trauma are based on known cases (Saul, 1998; Saul and ScalaBarnett, 1992). In trauma assessment and in development of the biographic profile, each forensic case teaches something. What we learn from each case enables us to do a better job with each succeeding case — whether archaeologic or forensic.

Sharp-Force Injury Examples The subtleties of sharp-force injury illustrate the above concerns — in particular, the defects produced on cervical vertebrae by sharp-force injury to the neck. These defects are such that many would be overlooked and/or misinterpreted without having seen them in known situations. We have found that some defense cuts can also be exceedingly subtle. Turnpike Case Our interest in sharp-force injury to the neck began with skeletonized and mummified remains found by hunters in early November, 1992 in a ditch beside an overpass for a major interstate in rural Ohio (Saul et al., 1997). The soft tissue on the upper surface of the body (where the sun could shine on it) had mummified and was dark brown to black, while the underside of the body (more shaded and damp) had become skeletonized. Some dark blonde hair was present on the preserved partial scalp. The remains brought to us at the Lucas County Coroner’s Office were essentially complete, lacking only 6 teeth, the right cornu of the unfused hyoid, and several phalanges from the right foot. Our examination indicated that the deceased was definitely a white male, based on pelvic and cranial morphology. We suggested that this young man was in his mid to late

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Figure 4.8 Dorsal view, proximal phalanx of the fifth digit of right hand. Two fine intersecting cuts forming a “V” on the medial edge (arrow) plus probable puncture near proximal end are defense wounds. (Photograph courtesy of Bud Weaver.)

teens, basing our age estimation on dental and skeletal developmental findings. We estimated a living stature range of between 6 ft and 6 ft 2 in. based on maximum lengths of femora and tibiae. He was eventually identified as a 6 ft 1 in., 18-year-old white male whose physical description matched our person. Mummified fingers from the left hand yielded usable prints and he was identified by fingerprint comparison. (The right hand was almost completely skeletonized, with only a small amount of very dry mummified skin remaining at the tips of the fingers.) He had been missing for about 2.5 months, since late August. The next question was cause and manner of death. The remains were too far (65 feet) from the interstate overpass for him to have jumped, or been thrown, from above. In the absence of appropriate soft tissue and obvious cause of death, we began the task of examining his bones using direct and cross lighting, the naked eye, and magnification. The only sign of possible carnivore or rodent damage was a puncture on the dorsal surface of the proximal phalanx of the right fifth finger (Figure 4.8). Although the coneshaped puncture was similar to carnivore tooth marks, there was none of the typical crushing of bone around it and no signs of carnivore activity on any other bones. We found no sign of rodent activity anywhere. On the medial edge of the same phalanx, and distal to the puncture, were two fine intersecting cut marks (Figure 4.8). The dorsal surface of the proximal phalanx of the right fourth finger bore two fine parallel cuts (Figure 4.9). These defects were so subtle that we discovered them by touch as we ran a fingernail gently along the shaft. Then, knowing that they were indeed there, we saw them with cross lighting and magnification. These were probable defense cuts. Due to the lack of any other signs

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Figure 4.9 Two parallel defense cuts (arrows) across the dorsal surface of proximal phalanx, fourth digit of right hand. (Photograph courtesy of Bud Weaver.)

Figure 4.10 First cervical vertebra, inferior aspect upward. Sharp-force defect on interior sur-

face of posterior arch (arrow) angles upward from right to left, originating from the right side of the space between the neural arches of C1 and C2. No defects are present on the second vertebra. (Photograph courtesy of Bud Weaver.)

of animal manipulation and the presence of these defense cuts, we suspected that the puncture might actually be another defense wound, perhaps from the point of a knife. We examined the rest of his skeleton and found small defects on two cervical vertebrae. The location of the first was surprising. It was a 4-mm cut on the interior and inferior aspect of the right side of the posterior arch of the first cervical vertebra (Figure 4.10). The cut angled into the bone in such a way as to lift up a sliver of bone at the edge, a sign of perimortem injury (Ubelaker, 1978). This small cut angled upward from the right, thus

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Figure 4.11 Anterior body of seventh cervical vertebra. Hinged flake (2.5 mm) of bone lifted

from the left on the anterior/superior border of vertebral body. Small cut (7 mm) on anterior aspect of body with inward bending edges indicating an anterior-posterior direction. (Photograph courtesy of Bud Weaver.)

originating from the right side of the space between the neural arches of C1 and C2. The second cervical vertebra showed no damage, leading to the hypothesis that the sharp instrument involved had a fairly long, thin blade. On the seventh cervical vertebra a hinged flake of bone (2.5 mm) was lifted from the left on the anterior/superior border of the vertebral body. A 7-mm cut on the anterior aspect of the body had edges that bent into the vertebral body, indicating an anterior-toposterior thrust. The hinged aspect of both defects suggested that they also occurred during the perimortem interval (Figure 4.11). The defect on the first cervical vertebra suggested the immediate cause of death was injury to the spinal cord and/or brain stem. Anecdotal information from military colleagues also confirmed this; such techniques may be taught in hand-to-hand combat. A sharp instrument, whether from the left or from the front, would also probably need to pass through other vital structures to arrive at the anterior surface of the seventh cervical body. We did a literature search in an attempt to base our analysis on known cases. The search indicated an absence of information on the impact of sharp-force trauma on cervical vertebrae. This is understandable, inasmuch as autopsy evaluation of sharp-force injury to the neck focuses on tracking wounds through soft tissue and documenting damage to vital structures. The impact on cervical vertebrae is a peripheral issue. In addition, the cervical region of the spine is difficult to visualize radiographically and such minute defects cannot be seen easily.

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Although the available literature failed to provide information about the recognition and interpretation of these defects, we felt certain that we were on the right track. In our opinion, the young man had suffered sharp-force injury to the neck originating from his left, right, and front. During the struggle, he had sustained defense cuts to his right hand. The perpetrator was arrested for a second murder, and at that time confessed to the above killing. He used a “kris,” an Oriental knife with a wavy blade. Surprisingly, the blade of the knife used reached a width of 1.5 cm just 4 cm from the tip and was 2.25 cm at the widest point, making it wider than hypothesized. In his confession he told of the struggle and said that he stabbed him in the neck “…three times … first in the left side, then in the right side, then through the middle.” We were surprised that the kris could create the incised defect on the interior of the posterior arch of C1 without damaging C2. Later, we were able to hold C1 and C2 in normal anatomic position and attempt to insert the kris between them from the right, lining the edge up with the incised defect. We found that if the knife angle is just right, it can be done with no difficulty. In fact, the width of the blade would probably have resulted in the severing of the right vertebral artery. This experience convinced us that we needed to know more about sharp force and cervical vertebrae. We began to work with the pathologists in our office to learn more, by tracking wounds through soft tissue to locate the site of impact on bone, and then examining the bone itself. The two cases that follow illustrate this process. In the first case, stab wounds to the neck were tracked through the soft tissue to the cervical vertebrae, which were then cleaned, examined, and the resultant bony defects noted. In the second case, cervical vertebrae were examined in the absence of soft tissue and the recognition and interpretation of defects were based on the previous known case. A Known Sharp-Force Injury Case A young woman was stabbed multiple times in the neck. One stab wound was visible just below and behind her left ear. This was tracked back to the first cervical vertebra, where we could see that a small oval of periosteum had been lifted on the exterior surface of the left side of the posterior arch. Another stab wound entered the front of the neck just to the right of center, traveling back to impact on the right transverse process of the seventh cervical vertebra. All cervical vertebrae were cleaned and examined for defects. Defects were found only on C1 and C7. First cervical vertebra: At the spot noted at autopsy, a small thin oval flake of bone, 6 mm ¥ 2 mm, had been shaved from the outer cortex just medial to the groove for the vertebral artery (Figure 4.12). The flake of bone was not recovered. This defect was so subtle that we might have overlooked or ignored it if we hadn’t known that the blade of the knife had hit that spot. Seventh cervical vertebra: The tip of the transverse process had been broken off and the cancellous bone within was exposed. Edges of this break were rough (almost scalloped), with no straight edges or other signs of having been cut (Figure 4.13). A small fragment (7 mm ¥ 4 mm) that had been broken from the tip, however, bore one straight edge, more consistent with sharp force (Figure 4.14). A fragment as tiny as this one would probably not be recovered if the remains had not been “fresh.” This defect intrigued us. If we had been confronted earlier with such a defect (minus the fragment) in skeletal or decomposed remains, we would have been unlikely to think of sharp force as the origin, and more apt to postulate the possibility of blunt force or strangulation as the cause. © 2002 by CRC Press LLC

Figure 4.12 Left side of posterior arch of C1. Small oval defect (arrow) marks location where

flake of bone was shaved off when individual was stabbed behind and below the left ear. Vertical cut to the left of oval was produced accidentally during removal of vertebra during autopsy. (Photograph courtesy of M.J. Naujock.)

Figure 4.13 Superior view of C7. Tip of right transverse process was broken off by stab to front

of neck just right of victim's midline. Note (far left of photo) the irregularity of edges and barely visible cancellous bone within. (Photograph courtesy of M.J. Naujock.)

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Figure 4.14 Broken tip of right transverse process of C7 plus fragment of bone broken from the tip. Note straight edge on fragment. (Photograph courtesy of M.J. Naujock.)

This case then provided a known case on which to base recognition and interpretation of perimortem trauma in the following unknown case. A Probable Sharp-Force Injury Case The body of a woman was discovered by a bulldozer (and its operator) in a quarry in midAugust. It was identified as a woman who had last been seen 2 weeks earlier. The body was generally in good condition, although the bulldozer had inflicted several postmortem soft tissue gashes and long bone fractures. There was no bleeding or bruising at the site of these injuries. There were no signs of carnivore or rodent activity. Decomposition had progressed only slightly, except for the left side of her neck. This region contained a large quantity of insect remains and other signs of heavy insect activity and advanced decomposition and virtually all of the soft tissue was gone. Since this is not the usual progression of decomposition (Rodriguez and Bass, 1983, 1985; Micozzi, 1991; Bass, 1997), we suspected that this was the site of perimortem injury that had breached the protective covering of skin, allowing early entry to insects and bacteria. The examining pathologist found no evidence of cause of death or perimortem trauma at autopsy, other than a cracked thyroid cartilage. We agreed that the cervical vertebrae, hyoid, and left clavicle should be removed, cleaned, and examined for possible defects, based on the disproportionately advanced amount of decomposition and insect activity in that area. We found defects on only the first and seventh cervical vertebrae. (Interestingly, in our limited experience so far we have found C1 and C7 to be the cervical vertebrae most often involved in perimortem sharp-force trauma.) First cervical vertebra: An approximately 6-mm long, thin, elongated fragment (sliver) of bone was separated from the left posterior arch at the medial edge of the groove for the left vertebral artery. This fragment was still attached by its medial end to the posterior arch. The edges of this defect were fairly straight (Figure 4.15).

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Figure 4.15 Left side of posterior arch of C1. Note cut extending medially from medial edge

of the groove for the vertebral artery, producing a separate thin sliver of bone attached to C1 at its medial end.

Figure 4.16 Left transverse process of C7. Cancellous bone is visible where tip has been broken off (slightly to right and below center of photo).

Seventh cervical vertebra: (1) The tip of the left transverse process was broken off, revealing the cancellous bone within (Figure 4.16). The fragment was not recovered. (2) An approximately 4-mm long, narrow portion (again a sliver) of the inferior edge of the left costal process was separated from the rest of the process, but still attached to it at the lateral end. The edges of this defect were straight (see Figure 4.17). The location and nature of two of these defects were surprisingly similar to those of the defects in the known case described earlier. Although the specifics of the defects on the first cervical vertebra differed (a sliver of detached bone vs. an oval flake shaved off), the location was essentially the same. Both of these defects were typical of sharp-force injury to bone. The broken tips of the transverse processes of the seventh cervical vertebrae

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Figure 4.17 Inferior view of C7. Note sliver of bone separated from inferior edge of left costal process (far left).

were virtually identical. The straight-edged sliver of bone raised from the inferior edge of the costal process, close to the broken tip of the transverse process, suggested the possibility of an additional stab or other movement of the sharp instrument responsible. These vertebral defects were too delicate to have been produced by the bulldozer. Based on experience with known cases of sharp-force injury to the neck, and especially the case described above, the defects were strongly suggestive of perimortem sharp-force injury to the neck. Although the woman’s estranged husband was the prime suspect, there were no witnesses and no weapon had been found. Only circumstantial evidence linked him to the crime. Although they were not living together and he said that he had not seen her for some time, the clothes she had worn to work on the last day she was seen were found in his house. Her stomach contents at autopsy were foods that were in his refrigerator when she was first reported to be missing. Bath mats and several towels had just been laundered and luminol revealed minute traces of blood in the bathroom (too little for DNA or other testing). In spite of the lack of direct evidence or witnesses, the estranged husband was charged. A video deposition was scheduled due to non-availability of the anthropologist at the proposed date of the trial. The deposition was taken in the courtroom, with the defendant present. It was conducted as expert witness testimony would be during a trial, but without judge and jury. The defects were demonstrated using photographs, diagrams, and the bones themselves to explain the difference between perimortem and postmortem injury and the similarities in this case to known cases of perimortem sharp-force injury to the neck. The interpretation was linked in particular to the case described above which was judged to be the result of sharp-force trauma to the neck. The defendant listened and watched with apparent great interest. When the deposition was over and the defendant was leaving the room, he stopped and quietly told the anthropologist, “You done good.”

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Unfortunately, his comment confirming the trauma analysis could not be used in the trial. The case depended heavily on circumstantial evidence, and he was subsequently acquitted. A day or two later, the forewoman of the jury asked the prosecuting attorney if they could “do it over again” as she felt that they “didn’t do the right thing.” In spite of the acquittal, we felt confident that our interpretation of the skeletal trauma, based on known cases, had been confirmed informally by the alleged perpetrator (Saul, 1994).

Conclusion Although we strongly encourage physical anthropologists who work in the archaeologic arena and those who work in the forensic arena to learn from each other, the ramifications of forensic work are such that we worry about occasional dabbling by the academic physical anthropologist who has no real experience in forensics and does not keep up with the literature or the exchange of ideas and techniques that takes place at professional forensic meetings. There is too much at stake. Errors in the excavation and recovery of forensic remains may mean the loss of evidence vital to the solution of the case, as well as damage to the human remains themselves. Damage to the remains may result in non-identification or misidentification of the individual and confounds perimortem trauma analysis. Each case is a new and different puzzle to solve as well as an opportunity to learn. Solved puzzles (or known cases) help us to solve the new puzzles that come our way. Our academic techniques for determining sex and ancestry, and estimating age and stature are tested in each forensic case that we do. If our analysis is wrong we fail, and the individual may go unidentified. If the individual is identified in spite of our error, our credibility suffers, but we can re-examine our work and learn from the error. If our analysis is right and the individual is identified, our credibility is intact, proper techniques are reinforced, and we know we are on the right track. Knowledge of known cases comes from our own cases, the forensic literature, case and technique presentations at professional meetings, and informal discussions as well as from working with and/or observing the work of our colleagues, including those in other areas of specialization. Perimortem trauma recognition and analysis also need to be based on a working knowledge of known forensic cases for interpretation. In addition, knowledge of the skeletal consequences of taphonomic forces is essential to recognition and interpretation of perimortem skeletal trauma. The time frames may differ, but the goals (and some of the techniques) of forensic science and archaeology are similar — to recreate past events. Forensic science itself encompasses many specializations, as does archaeology. However, we are basically, each one of us, intrigued by the challenge of solving a puzzle. We will solve more puzzles correctly by collaboration, sharing and learning from each other than by isolation. And solving the puzzle is our goal.

Acknowledgments We thank James R. Patrick, M.D., Lucas County Coroner; Diane Scala-Barnett, M.D., Deputy Lucas County Coroner; and Cynthia Beisser, M.D., Deputy Lucas County Coroner

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for their continuing support in the forensic arena. We are indebted to archaeologists R.E.W. Adams, Ph.D.; Norman Hammond, Ph.D.; Fred Valdez, Ph.D.; and Peter Dunham, Ph.D. for their continuing support in Maya bioarchaeology. Thanks also to M.J. Naujock and the late Bud Weaver for their technical and photographic assistance.

References Allen, D.J. et al. 1984 Old incised wound or vascular impression? Diagnosis by scanning electron microscopy. In Abstracts of the Eleventh Annual Meeting of the Paleopathology Society, Philadelphia, PA. Bass, W.M. 1997 Outdoor decomposition rates in Tennessee. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp 181–186. CRC Press, Boca Raton, FL. Campillo, D. 1977 Paleopatología del Craneo en Cataluña, Valencia y Baleares. Editorial Montblanc-Martín, Barcelona, Spain. Dirkmaat, D.D. and J.M. Adovasio 1997 The role of archaeology in the recovery and interpretation of human remains from an outdoor forensic setting. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 39–64. CRC Press, Boca Raton, FL. Goss, C.M. 1973 Gray’s Anatomy of the Human Body, Lea & Febiger, Philadelphia, PA. Haglund, W.D. 1997a Dogs and coyotes: postmortem involvement with human remains. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 367–381. CRC Press, Boca Raton, FL. 1997b Rodents and human remains. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 405–414. CRC Press, Boca Raton, FL. Haglund, W.D. and M.H. Sorg (editors) 1997 Forensic Taphonomy: The Postmortem Fate of Human Remains, CRC Press, Boca Raton, FL. Hammond, N., K. Pretty, and F.P. Saul 1975 A classic Maya family tomb, World Archaeology 7(1):57–78 Haskell, N.H. et al. 1997 On the body: insects’ life stage presence, their postmortem artifacts. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 415–448. CRC Press, Boca Raton, FL. Lee, H.C. 1994 Crime Scene Investigation, Central Police University Press, Republic of China. 1998 Quotation. In Forensic Radiology, B.G. Brogdon, p. 280, CRC Press, Boca Raton, FL. Lockhart, R.D., G.F. Hamilton, and F.W. Fyfe 1959 Anatomy of the Human Body, J.B. Lippincott Company, Philadelphia. Merbs, C.F. 1997 Eskimo skeleton taphonomy with identification of possible polar bear victims, In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 249–262. CRC Press, Boca Raton, FL.

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Micozzi, M.S. 1991 Postmortem Change in Human and Animal Remains: A Systematic Approach, Charles C Thomas, Springfield, IL. Murad, T.A. 1997 The utilization of faunal evidence in the recovery of human remains. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 395–404. CRC Press, Boca Raton, FL. Robichaux, H.R. 1998 Excavations at the Upper Plaza. In The 1997 Season of the Chan Chich Archaeological Project, edited by B.A. Houk, Papers of the Chan Chich Archaeological Project, Number 3, pp. 31–52. Center for Maya Studies, San Antonio, TX. Rodriguez, W.C., III 1997 Decomposition of buried and submerged bodies. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 459–467. CRC Press, Boca Raton, FL. Rodriguez, W.C., III and W.M. Bass 1983 Insect activity and its relationship to decay rates of human cadavers in east Tennessee, Journal of Forensic Sciences 28:423–432. 1985 Decomposition of buried bodies and methods that may aid in their location, Journal of Forensic Sciences 30:836–852. Saul, F.P. 1972 The Human Skeletal Remains from Altar de Sacrificios, Guatemala: An Osteobiographic Analysis, Papers of the Peabody Museum, Harvard 63:2:1–123, Peabody Museum of Harvard Press, Cambridge. 1973 Disease in the Maya Area: the pre-Columbian evidence. In The Classic Maya Collapse, edited by T.P. Culbert, pp. 301–324. University of New Mexico Press, Albuquerque. 1975 The human remains from Lubaantun. In Lubaantun, by N. Hammond, Appendix 8:389–410. Cambridge, Peabody Museum Monographs, Harvard No. 2. 1977 The paleopathology of anemia in Mexico and Guatemala. In Porotic Hyperostosis: An Enquiry, edited by E. Cockburn, Paleopathology Association Monograph, No. 2:10–15, 18 (plus cover photo), Detroit. 1982 The human skeletal remains from Tancah, Mexico. In On the Edge of the Sea: Mural Painting at Tancah-Tulum, by Arthur G. Miller, Dumbarton Oaks Trustees for Harvard University, Washington, D.C., Appendix II, pp. 115–128. Saul, F.P. and J.M. Saul 1984 Pseudopathology and Vascular Impressions: Clues from Anatomy. Abstracts of the Eleventh Annual Meeting of the Paleopathology Society, Philadelphia, PA. 1989 Osteobiography: a Maya example. In Reconstruction of Life from the Skeleton, edited by M.Y. Iscan and K.A.R. Kennedy, pp. 287–302. A.R. Liss, New York. 1991 The preclassic population of Cuello. In Cuello: An Early Maya Community in Belize, edited by N. Hammond, pp.134–158. Cambridge University Press, Cambridge, England. 1993 Cut marks or vascular impressions? Clues from paleopathology and anatomy (poster). In Abstracts of the 45th Annual Meeting of the Academy of Forensic Sciences, Boston, MA. 1994 Forensic anthropology: a “reality check” for physical anthropology. In Abstracts of the 1st Annual Midwest Bioarchaeology and Forensic Anthropology Conference, Madison, WI.

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Saul, J.M. 1994 “You done good”: cervical nicks and an unusual confirmation of probable cause of death. In Abstracts of the 1st Annual Midwest Bioarcharchaeology and Forensic Anthropology Conference, Madison, WI. 1998 “This is what happened to me:” allowing the dead to speak for themselves in court. In Proceedings of the American Academy of Forensic Sciences, 4:184, San Francisco, CA. Saul, J.M. and F.P. Saul 1997a The skeletal remains from a Maya royal tomb at La Milpa, northwest Belize. In Abstracts of the 62nd Annual Meeting of the Society for American Archaeology, Nashville, TN. 1997b The preclassic skeletons from Cuello. In Bones of the Maya: Recent Studies of Ancient Skeletons, edited by S.L. Whittington and D.M. Reed, pp. 28–50. Smithsonian Press, Washington, D.C. 1999 Biker’s bones: an avocational syndrome. In Forensic Osteological Analysis: A Book of Case studies, edited by S.I. Fairgrieve, pp. 237–250. Charles C Thomas, Springfield, IL. Saul, J.M. and D. Scala-Barnett 1992 A good fit: skull reconstruction fits the weapon to the wound (poster). In Abstracts of the 44th Annual Meeting of the American Academy of Forensic Sciences, New Orleans, LA. Saul, J.M., C.S. Beisser, and F.P. Saul 1997 The unkindest cuts of all: sharp-force injury to the neck and its impact on underlying bone (a case study) (poster). In Proceedings of the American Academy of Forensic Sciences, 3:149. Saul, J.M., F.P. Saul, and A.R. Muñoz 1995 Osteological analysis of burials from a small, non-elite site (RB-11, Programme for Belize). In Abstracts of the 60th Annual Meeting of the Society for American Archaeology, Minneapolis, MN. Scott, D.D. and M. Connor 1997 Context delicti: archaeological context in forensic work. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 27–38. CRC Press, Boca Raton, FL. Shipman, P. and J.J. Rose 1984 Cutmark mimics on modern and fossil bovid bones, Current Anthropology 23(1):116–117. Stewart, T.D 1937 Did the American Indians use the cautery in bone surgery? American Journal of Physical Anthropology 23(1)(O.S.):83–89. 1966 Some problems in human paleopathology. In Human Paleopathology, edited by S. Jarco, Yale University Press, New Haven, CT. Testut, L. 1911 Traite d’Anatomie Humaine, 6th ed., Octave Doin et Fils, Paris. Turner, C.G. and J.A. Turner 1999 Man Corn: Cannibalism and Violence in the Prehistoric American Southwest, University of Utah Press, Salt Lake City, UT. Ubelaker, D.H. 1978 Human Skeletal Remains: Excavation, Analysis, Interpretation, Taraxacom, Washington, D.C. 1997 Taphonomic applications in forensic anthropology. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 77–90. CRC Press, Boca Raton, FL.

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Wells, C. 1963a Cortical grooves on the tibia, MAN July, pp. 112–114. 1963b Cortical grooves on the tibia, MAN Nov., p. 180. White, T.D. 1992 Prehistoric Cannibalism at Mancos 5MTUMR-2346, Princeton University Press, Princeton, NJ Zimmerman, M.R. et al. 1981 Trauma and trephination in a Peruvian mummy, American Journal of Physical Anthropology 55:497–501.

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Position of Skeletal Remains as a Key to Understanding Mortuary Behavior

5

MIRJANA ROKSANDIC Contents Introduction Taphonomy in Human Remains Research Utilizing Taphonomy to Understand Mortuary Practice General Consequences of Soft Tissue Decomposition and Disarticulation Consequences of Decomposition Sequences of Disarticulation or Disintegration of Connective Tissue between Joints Potential Amplitude of Postdepositional Movement of Skeletal Elements Influence of Gravity and the Space in Which Decomposition Takes Place Inference about Ritual: Primary vs. Secondary Disposition Group Burials: The Study of Function Conclusions Acknowledgments References

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Introduction The key to understanding archeological mortuary behavior is to reconstruct the ritual context in which burial data are created. It is this intention that represents the greatest problem for the interpretation, but is also an opportunity to infer elements of conceptual life. In order to infer intentional behaviors related to understanding ideologies of past populations, it is necessary to incorporate information that pertains to periburial mortuary activity as well as mortuary and ancestral ritual (sensu Kinnes, 1975). At times this can be deduced from the relative position of the skeletal elements in the grave. However, simple correlation of the position of skeletal elements may not only prove insufficient but may also be misleading. Research methods and approaches borrowed from forensic anthropology can contribute to this analysis. Hence, the goals of this chapter are (1) to show that disposition of skeletal elements is a relevant source of information about mortuary behavior; (2) to argue that skeletons, as bearers of this information, must be excavated by experts trained in human osteology; (3) to call for a systematic investigation of taphonomic phenomena that affect disposition of remains; and (4) to suggest ways in which forensic experts can contribute to advancing this type of analysis.

Taphonomy in Human Remains Research Because human skeletal remains — with the exclusion of early hominid material — are found in archaeological contexts primarily as a consequence of human cultural, and more specifically, ritual activity, both natural and cultural agents should be regarded as taphonomic (Bonnichsen and Sorg, 1987). Human behavior involved in mortuary practices can leave potentially recognizable taphonomic signatures (Boddington et al., 1987; Duday and Masset, 1987). Modeling of the processes of decomposition and decay of the cadaver has been recognized as a relevant source of information on periburial activity. In France the interest arose from methodological approaches to excavating Neolithic group burials first developed by Andre Leroi-Gourhan et al. (1962), and promoted further in studies by Masset (1972a,b, 1973, 1987) and Duday (1978, 1987a,b; Duday et al., 1990). In French literature, concern for interpretation of mortuary ritual is evidenced by the focus on the disposition of skeletal elements as a primary goal of taphonomic studies. In England, studies such as those by Mant (1987) on war dead, although forensic in nature and scope, were recognized as relevant to the archaeological community. Regardless of their differences, Boddington et al. (1987) and Duday and Masset (1987) attempted to systematize current knowledge on the sequence of decomposition and the influence of the burial environment and other cultural factors on the position of bones within a grave. These texts are key for this type of archaeological inference. In the North American literature, most of the research on decomposition and decay centers on questions of exclusive interest to forensic anthropology in the medicolegal context. It should be emphasized that the forensic context offers potential resolution of taphonomic issues relevant to the sequence of decomposition and position of individual bones and bone fragments within burials that have to be deduced in archaeological contexts (Haglund and Sorg, 1997a). The subsequent systematization and publication of such data

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greatly advance our understanding and provide well-grounded explanations of some of these phenomena for the field of archaeology (Haglund and Sorg, 1997b). The taphonomic behavior of a cadaver is influenced by a large number of factors. Factors internal to the body include cause of death, state of the body at death, age, sex, body mass, and pathology. External factors such as the time elapsed between death and burial, the treatment of the body prior to burial, and the burial environment (Garland and Janaway, 1987) are all primarily cultural. Noncultural taphonomic factors are important in determining disturbance (bias) that in turn can be relevant for differentiation of culturally determined activity. For example, the extent of damage by burrowing animals can be relevant in inferring the presence and type of burial architecture (Mordant, 1987). Human skeletal remains found in archeological contexts are most often the consequence of human cultural activity. From the perspective of understanding mortuary patterns, nonhuman taphonomic agents need to be identified and understood in order to eliminate their effect and the possible misinterpretations they can cause. For this reason, to pursue an understanding of mortuary ritual, physical anthropologists must be actively involved in the excavation and documentation of the site. Duday (1978) rightfully insists that knowledge of human osteology and anatomy should be an imperative for anyone excavating human burials. Knowledge of forensic contexts can also be critical (Haglund and Sorg, 1997b).

Utilizing Taphonomy To Understand Mortuary Practice The original intent of human cultural activity in archeological contexts can be masked by the dynamics of decomposition and possible disturbance. Two phenomena of primary significance for funerary archaeology are the differential preservation of individual bones and differential disposition of human skeletal remains. Preservation is mitigated by cultural modes of disposal and by postdispositional agents. Understanding this interplay can assist in inferring burial circumstances. Cultural factors affecting preservation are numerous: Humans through their cultural norms decide who gets buried, where, when, and how the burial takes place. The place and mode of disposition will not only influence the position of the skeleton in the grave, but ultimately its preservation. General Consequences of Soft Tissue Decomposition and Disarticulation To understand the post-dispositional movements of bones, it is necessary to understand: (1) consequences of soft tissue decomposition, (2) the sequences of disarticulation or disintegration of connective tissue between bones, and (3) the potential amplitude of movement of skeletal elements. Consequences of Decomposition Decomposition is the general term used to refer to its two major processes, putrefaction (involving bacteria) and autolysis (involving autolytic enzymes). Disarticulation is defined as complete reduction of the soft tissues that hold bones together within a joint in living organisms. Therefore, even if every bone is in its correct anatomical position relative to the other bones, the skeleton is considered disarticulated as long as no soft tissue connects them.

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Sequences of Disarticulation or Disintegration of Connective Tissue between Joints Most research on skeletonization deals with exposed human remains from forensic contexts, or are experimental studies based on nonhuman carcasses (Toots, 1965; Hill, 1979; Haynes, 1982; Weigelt, 1989). Forensic experience with buried remains is relatively limited (Rodriguez and Bass, 1985; Manhein, 1997) and more information is needed to come to meaningful conclusions about the rate and sequence of skeletonization. The time it takes a carcass to skeletonize is highly variable and context (microenvironment) specific. When a body is exposed to scavengers and insects on the surface, or in shallow burials, decay is more rapid (Micozzi, 1986, 1991; Janssen, 1984; Polson et al., 1985; Haglund et al., 1989; Garland and Janaway, 1987; Janaway, 1997). Dirkmaat and Sienicki’s 1995 skeletonization sequence based on observations of human remains decomposed in open space is presented here for illustration, rather than a set of generally applicable rules: 1. The cranium is first to skeletonize primarily due to the accessibility of facial cavities to flies. If exposed to sun it will desiccate rather than decompose, and preserve skin and hair tissue for longer periods. 2. Clavicles and sternum are exposed early in the sequence. 3. Cervical vertebrae, even when exposed, will remain articulated for longer periods due to strong ligaments and complex interlocking bony surfaces. 4. Arms are usually at an enhanced state of decomposition compared to lower limbs. As with the cranium, limb surfaces exposed to the sunlight desiccate rather than decompose. 5. Pelvis is reduced later than the thoracic/abdominal region, while the vertebral column remains intact and articulated, and ribs present differing degrees of disarticulation. 6. Legs, especially if clothed, are preserved much longer than arms. Feet, often protected by socks and shoes, will preserve their shape longer than any other part of the body. Clothing in general seems to postpone decomposition significantly (Dirkmaat and Sienicki, 1995:7). Other disarticulation sequences suggested for human remains, such as Haglund’s (1993) for water environments and for canid-assisted surface remains (Haglund et al., 1989) underscore departures in disarticulation sequences that are due to different environments and circumstances. Comparison with archaeological observation demonstrates that disarticulation of the first and second cervical vertebrae is observed early in the sequence in both animals (Micozzi, 1991) and humans (Masset, 1987). This may have as much to do with the weight and shape of the cranium, allowing it to roll or rock, as with the joint. Mandible and cranium are frequently the first to separate from the rest of the skeleton. Hands and unprotected feet are also early to disarticulate, sometimes prior to disarticulation of head from the neck. Ubelaker (1974) suggests that the lower leg articulations can persist over longer periods of time. In archaeological contexts, the hip joint and the knee joint can become dislocated, whereas the foot retains perfect anatomical connections. The observed differences between forensic and experimental findings further underline the need to gather and systemize data

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on disarticulation rate and sequence in different burial environments. Some of the apparent differences may be due to the fact that the forensic cases Dirkmaat and Sienicki studied decomposed above ground. Forensic cases in which the deceased are interred might clarify these issues, provided relevant data are collected on a regular basis. The project by Rodriguez and Bass (1983, 1985) that deals with inhumated rather than exposed individuals over longer periods of time, although centered on forensic questions, could be an excellent source of information on sequence and pace of disarticulation not influenced by animal activity and weathering. Potential Amplitude of Postdepositional Movement of Skeletal Elements The potential for postdepositional position changes in human remains must be kept in mind. Empty space around the body leaves the potential for slight changes of body position due to buildup of gases during the decomposition process or collapse of joint connections. Examples of this type of movement might involve fingers spreading within the abdomen or splaying arms or legs. Postdepositional movement of remains buried with soft tissue depends on the shape of the joint and its associated degree of freedom (Duday, personal communication) coupled with the amplitude of possible movement in any of the given directions and the strength of associated ligaments. Amplitude of movement, i.e., displacement in situ from the original position, will depend upon the position of the remains, as deposited, and the available space in which the movement takes place. Potential for postdepositional movement of individual skeletal elements will differ for burials of fleshed, decomposing, and fully skeletonized remains. The amplitude of movement, or mobility, represents the extent to which a bone can move in any of the possible directions. Movement is, for example, only theoretical in adult cranial sutures, whereas it can be pronounced in the adult shoulder articulation. Potential for mobility and amplitude of mobility are crucial concepts, as they describe movement of any of the bones in the living individual. In the context of skeletonized remains, they serve to distinguish movements of bone that cannot be regarded as expected and thus require alternative explanations. The presence of an anatomically correct position of bones in the skeleton as a whole, which is referred to as anatomical relationship, should be regarded in light of the resistance of certain articulations to decomposition and disarticulation. In that respect, the table that Ubelaker (1974:31) presents for Ossuary II from Tidewater Potomac on the relative frequencies of anatomical relationships in secondary burials is most instructive. However, in order to develop a set of rules, we need more comparative data from both forensic cases and other archaeological contexts. Dastugue (referenced in Duday and Masset, 1987:129) pointed out that classifying ligaments as strong or weak is not consistent with anatomical knowledge. Masset (1987:131) argues that in cases where archaeological experiences conflict with medical explanations, archaeological observations should be regarded as more relevant. For example, the fact that costo-vertebral ligaments are difficult to separate in medical praxis does not put them in the category of persistent articulations, as the costovertebral joints are rarely found preserved in archaeological context. Duday (Duday, 1985:12) draws attention to variation in the volume of soft tissue that is attached to joints as a possible explanation for these inconsistencies. He notes three types of articulations: weak articulations with a small volume of soft tissue attached to them (extremities), weak

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with an important volume of soft tissue attached (trunk), and persistent articulations. However, it has been argued that although the articulations might be weak, the ligaments accompanying them can be numerous or strong, which in turn affects the disarticulation sequence. Furthermore, not only the soft tissue of the joint, but also the mass of soft tissue surrounding the joint will substantially influence the sequence of disarticulation. No simplistic scheme can be envisaged for ligament resistance as it depends on a number of factors. One cannot talk only of ligament strength; the relationship of joints to portals of entry for insects, accessibility and feeding behavior of scavengers, the position of the body and types of surfaces the remains rest on (inclines for example) have to be included as well. Again, as with decomposition rate, disarticulation sequences are highly environmentally and micro environmentally specific (Haglund, pers. commun.). Influence of Gravity and the Space in Which Decomposition Takes Place The principles of gravity and space provide the basis for interpreting the disposal space allocated to the individual, type of disposition, perishable grave architecture, and internal chronology of the necropolis (Crubezy and Helas, 1989:34–42; Duday, 1987b). Gravity and space also affect interpretations of different ritual functions served by the grave (sensu Kinnes, 1975). Most often, primary dispositions (especially burials) involve bodies and not skeletons (Garland and Janaway, 1987; Haglund and Sorg, 1997a). Given time, buried remains are usually reduced to a skeleton. If the mode of deposition puts bones in a stable position, little or no movement of bone will ensue following loss of soft tissue (other than collapsing). If disposition places bones in an unstable position, once soft tissue disappears, they will move in accordance with gravity and the architecture of the burial space. Clothing and wrappings will also affect potential movement. Additional space in a grave can be created from space previously occupied by the body volume. For example, if a hand is positioned flat on the substrate no movement will ensue, whereas, if it is positioned over the abdomen, as soft tissue of the abdomen disappears, disarticulated bones of the hand are subject to collapse into the pelvic area. Thus, bones of hands positioned in other than anterior palmer presentation are subject to relatively more displacement with decomposition. Interpretation of such postdispositional movement is dependent on the original position of the hand and requires expert knowledge of osteology and anatomy. Duday (1978:97) makes an excellent argument to illustrate this. By observing an uncommon in situ position of finger elements he was able to infer the paralysis of left ulna as a consequence of trauma. Had the position of the fingers not been noted during the excavation, even though the trauma was recorded, paralysis could not have been inferred. The space assigned to the deposition of the body is an integral part of the ritual. The changes through which a cadaver goes in the disposition context, while following general rules of decomposition, will have a significantly different outcome if the individual is deposited on “plain earth” and covered with sediment compared with a grave which (sensu lato) forms empty space around the body that eventually fills with earth (Duday, 1985:6). Archaeological observation can be sufficient when the architecture is made of non-perishable materials (Figure 5.1). However, when the architectural elements are no longer preserved, the position of skeletal elements (Figures 5.2 and 5.3) carries important information (Mordant, 1987; Brothwell, 1987).

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Figure 5.1 Non-perishable architectural elements (large rocks) account for (a) constriction at the level of left shoulder and lack of splaying of the left part of the rib cage. However, (b) shows that the other ribs on the same side tend to move in a predictable manner, as in (c), where there is no architecture limit. Normal movement (splaying) of the right side of the rib cage is shown at (c). (Photograph courtesy of B. Jovanovic, © STARINAR, Arheloˇski, Institut, Beograd.)

Figure 5.2 Perishable architecture elements (wrappings) are evidenced by constriction at the

shoulder girdle (a–c) and wall effect (a–b). Slumping of the thoracic cage is only toward the coxal and not lateral (i.e., not splayed). The left radius and ulna migrated within the initial volume of the body itself. (Photograph courtesy of B. Jovanovic, © STARINAR, Arheloˇski, Institut, Beograd.)

The manner of burial can provide insight into chronology and function of the gravesite as well as the associated ritual (Duday, 1985). The type of articulation (strong or weak) and the decomposition environment (covered vs. empty) influence the sequence of events and amplitude of movement. The original position of bones with weak articulations and a small volume of surrounding soft tissue will be preserved in the case of progressive infilling even in an unstable position because the soft tissue is immediately replaced by sediment. If the infilling is differential, weak articulations will be preserved only if the part

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Figure 5.3 The same wall effect that acts to preserve the position of the scapula and humerus in Figure 5.1a can be recognized here at (a). The right radius-ulna articulation persists (b), while the left radius migrates into the abdomen together with the hand (that had been displaced during excavation). At the same time, the unstable position of the left coxal and femur persists (c). (Photograph courtesy of B. Jovanovic, © STARINAR, Arheloˇski, Institut, Beograd.)

of the body is in a stable position, otherwise bones migrate within the initial volume of the cadaver. Persistent connections can be preserved in their anatomical position, on the other hand, even if the burial is secondary, depending on the time lapse between initial and secondary burial. The value any of these factors will have in determining the mode of disposition will depend upon site formation processes, disposition-specific parameters and the quality of excavation and the extent of documentation. Each case presents a set of specific problems, and because we often are dealing with equifinality, there are no simple space parameters; rather, a number of relevant observations have to be taken into consideration. Duday (1978:61–62, 1985:10) insists on the importance of discerning and documenting the amplitude of the displacement of bones relative to their expected anatomical position following decomposition. The following special terms are essential to understanding these issues. • Empty space, in the context of this discussion, refers to airspace between the body and surrounding sediment at the time or shortly after burial. Such space could be created by architectural elements of the burial, or by decomposition and disappearance of soft tissue. Empty space would allow limited movement of disarticulated skeletal elements, and might subsequently be vulnerable to infilling by sediment. • Wall effect results from architectural limits that enclose the remains and may prevent movement that would otherwise be expected. An example would be constriction of the shoulder or pelvic girdle if a body is placed in a confined space (Figures 5.2 and 5.3). Alignment of bones where there is no anatomical necessity for it is a good indicator of wall effects (Masset, 1993:125). • Nondelineated empty space refers to architectural or natural environments that do not involve burial, such as crypts, caves (Masset, 1993), and Bella-bella burial houses

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Figure 5.4 Decomposition in an empty space includes (a) slumping and splaying of the rib

cage, (b) severing of the costo-transverse joints, and (c) splaying and flattening of the pelvic girdle. (Photograph courtesy of B. Jovanovic, © STARINAR, Arheloˇski, Institut, Beograd.)

(Hester and Nelson, 1978). If the remains are not disturbed by external agents, such as scavengers, the processes of decomposition and disarticulation will result in slumping of various elements. Dislocations of skeletal elements that might result are collapse of the thoracic cage (Figure 5.4a), rotation of vertebral segments relative to each other, or disjunction of the coxo-sacral articulation (Figure 5.4c). • Empty space with later infilling presents a complex situation where it is necessary to demonstrate that infilling occurred long after cadaver decomposition and disarticulation. While decomposition occurred in a delineated empty space without any sediment, indicated by rearrangements of skulls, handfuls of ribs, and long bones, the sediment that covered them was brought in long after the last skeleton decomposed as a final event in the series of ritual actions (Leclerc, 1987). Duday (1978, 1987a,b) proposes a number of indicators of group burials within an empty space at the sites of Corconne and Villedubert: rearrangement of bones against walls, regrouping of long bones in a nonanatomical position, etc. Deposition in empty space was proposed for skeletons from Villedubert on the basis of following disposition: the left arm (elbow joint) of an adult (no. 1) lying against the fourth and fifth lumbar vertebrae of another (no. 2). The lumber vertebrae were rotated by 90 degrees with respect to sacrum, which itself was not in the anatomical position with coxal bones. The fact that the elbow (no. 1) was in correct anatomical relationship, although it is a far less persistent connection than the sacro-iliac joint, suggests that when subject no. 1 was deposited, disarticulation of subject no. 2 was already advanced and the individual was not covered with sediment. • Delineated empty space refers to architectural elements that create space around the decomposing body and prevent direct contact between sediment and individuals, such as a coffin, sarcophagus, planks over the top of the burial pit, skins, etc. Architecture can maintain a very delimited empty space around the corpse, which cannot always be distinguished from the initial volume of the body (wrapping in

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textile, skins, very narrow coffin). A good indicator of this constricted architecture is the wall effect, easily recognized in the perseverance of very unstable anatomical relationships and the rigid, unnatural position of the skeleton. Constriction of pelvic and shoulder girdle (Figures 5.2a–c and 5.3a–c), because it is in contradiction with the initial volume of the cadaver, is a very good indicator. The ability to determine these instances will depend on the relative rate of decomposition between the body and its associated architecture. If the architecture decomposes prior to the body, the effect will be the same as in covered space. Some damage to the bones from collapsing sediment is to be expected in the pubic region or at the sternal ends of the ribs, but only if there is a lapse of time between the decomposition of the body and the perishable architecture in which it is buried. If the two happen simultaneously, it is impossible to distinguish the interment “in plain ground” from interment in a coffin of very poor quality. If it decomposes well after the decomposition of the body, as in the case of wooden coffins, some displacement will occur outside the initial volume of the cadaver. The movements that ensue could be due to gravity, collapse of architectural elements, or human reintervention, such as reopening the grave to take out skulls or long bones. Note that these skeletons have to retain enough anatomical connections to group them into primary and not secondary burials. Other, nonritual factors of possible disturbance, such as burrowing animals, roots, movements of the terrain, grave robbers, etc. should always be considered. • Covered space refers to immediate contact of the body with sediments throughout the process of decomposition. Decomposition in a covered space corresponds to inhumation sensu stricto: the grave is dug in the ground and the fossa is immediately refilled, the body is posed in the soil and covered by the earth (Duday, 1985:8). The filling of body cavities by sediment in a simple burial pit can be progressive or differential (Duday, 1985). When the body is surrounded by sediment, as soon as decomposition sets in the sediment may fill body cavities. However, depending on the integrity, compaction, and moisture of the sediment, a different effect may be produced. For example, some clays can leave the original space that was occupied by the body as empty space rather than infilling it (Haglund, pers. comm.). Some movement of bones is expected within the initial volume of the cadaver. Variability is caused by the volume of soft tissue that each individual has. A person with greater volume of the abdominal and pelvic region will create more initial space than a slim individual. In extreme cases, it can produce the same effect as architecture. However, examination of the skeletal parts subject to movement can provide reliable information. • Progressive infilling occurs when the sediment is dry or fine-grained (sand or loess), and the filling of body cavities proceeds with decomposition and disappearance of soft tissue. No movement of bones is observable. However, the perseverance of the proper anatomical position of articulations is indicative only in those situations where the part of the body in question is in an unstable position. The left hand of the granolithic skeleton from Boniface (Corsica) was found on its side, positioned against the left hip, which makes the preservation of anatomical connection unlikely except in the case of continual filling (Duday, 1985:9). As was noted earlier, the hand articulations can be retained even when the body has not been covered with sediment, if they are in a stable position against the floor of the burial. However, proper anatomical position of the hyoid bone can be taken as a tell-tale sign of progressive sedimentation.

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• Differential filling refers to covered space where sediments are less fine grained. The space created by the decomposition of the thorax and abdomen will allow bones to move within that initial volume of the cadaver for a short time before the sediment collapses and fills in the remaining cavity. Slumping* (Figure 5.1) of the thoracic cage with disjunction of costotransverse articulation, dislocation of sternum, rotation of the segments of the vertebral column relative to each other, and splaying (Figure 5.4) of the pelvic girdle with minor displacement of the femoral head in the case of dorsal decubitus (when the individual is laid on the back) are all very common. Movements of the hand ensue (Figure 5.3), if placed on either abdomen or thorax. The fact that bones never migrate outside the initial volume of the cadaver is important in arguing against architectural elements.

Inference about Ritual: Primary vs. Secondary Disposition Disposition refers to the mode of disposing of the dead. Primary disposition concerns the initial location in which the body is placed. If the initial location is the same as final disposition, it is a primary burial. Secondary dispositions occur when remains are removed from the primary disposition; they are implied when the locus of soft tissue decomposition (or destruction in case of cremations) is different from the place of the final disposition. Inference that recovered remains are a primary or secondary disposition is not necessarily straightforward (Masset, 1987). For example, one cannot necessarily infer primary disposition just because all skeletal elements are present in relative anatomical order. Bodies may be removed while still fleshed and in stages of decomposition without disarticulation. Bodies may also be moved from a primary disposition enveloped in wrappings or some sort of enclosure such as a coffin or casket. When most of the articulations, even the least persistent, are present at the site, and virtually all bones present, we can infer primary disposition. While small carpal and tarsal bones preserve remarkably well, in secondary burials they may not be collected and placed in the ultimate burial area (Duday, 1978). If the initial position of the deceased is stable with respect to gravity, reconstruction of the original position in which the individual was buried is relatively straightforward. However, with positions that contribute to instability of skeletal elements, as for example in the case of seated individuals (Audouze, 1987), the inference becomes more complicated and demands more detailed and expert analysis. Caution should be used in deducing a secondary disposition simply because skeletal elements are in disarray or when complete skeletons are not present. Such disturbances can be caused by a variety of agents. Although secondary dispositions are traditionally described as containing complete skeletons, or having elements in anatomic disarray, such generalizations are useful only in cases of good preservation. A valuable indicator of secondary dispositions is the underrepresentation of normally well-preserved elements (see Darwent and Lyman, Chapter 19, this volume). When analyzing osteological collections, careful comparison of the found percentage of bones to the expected percentage is necessary (Mays, 1992). In case of good preservation where ribs, vertebral bodies, and sternum (for example) are present, lack of bones that preserve well can be indicative of secondary disposal. However, if skeletal material was collected earlier in the century, excavation and collection bias cannot be excluded. * T. Rogers helped translate the term “mis à plât” used by French authors (Masset and Duday, 1987).

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Secondary dispositions resulting from relocation of partly decomposing, relatively articulated cadavers allow for the most complete skeletal representation (Ubelaker, 1974; Duday, 1985). When remains are skeletonized, even if a full skeleton is represented, often not all the bones will be collected to be removed to a secondary disposition site. In some incinerations, representation of the body can be anywhere between 2 and 3000 grams (Antunovic, 1991). Completeness of dentition recovery has been discussed by Haglund as an indication of transport (1997a). If the number of teeth — especially incisors — is much smaller than expected, it can indicate secondary disposition, since teeth are susceptible to falling out of the alveoli after decay of the peridontal ligament, and thus may be overlooked when the individual is reburied. If the cranium is the object of an ancestral cult and is removed from the necropolis after decomposition, this argument is even more valid: the teeth will remain with the skeleton (primary disposition) while the cranium (or its fragments) will be missing. If the anatomical connections are lost due to successive rearrangements within the necropolis, the number of teeth in comparison with the number of skull fragments becomes a crucial argument (Gallay, 1987). Quality excavation and documentation are necessary to provide insights into secondary dispositions (Duday, 1978). At the site of Saint-Michael-du Touch (Toulouse, France), Simmone was able to show irrefutably that a body of an adult had been schematically reassembled from bone pieces but with obvious anatomical errors: an arm was reconstructed by placing two humeri so that their distal ends met at the “elbow”. In this case, if the position of bone fragments had not been noted during the excavation, the secondary disposition would have escaped the attention of the researchers (Duday, 1978:65–66). Sellier (1985) notes that while certain partial skeletons are secondary dispositions, others are definitively primary dispositions from which certain bones have been removed. Removal of the skull or its displacement is well-known at a number of sites in epochs as different as PPNA and PPNB in Jericho, the Mesolithic of the Lepenski Vir culture, and the Late Iron Age of the La Tene type (Srejovic, 1969; Rozoy, 1987). In the abovementioned site of Benon, by plotting the teeth Jousseaume was able to determine the exact position of the skulls that had been removed from the skeleton after decomposition (referenced in Masset, 1993:110). Implications of this practice go beyond mere funerary act; ancestral rituals can be implied. In rare instances it is even possible to suggest the original corpse position from its array in the secondary grave. Ambroise and Perlès (1972) were able to suggest, after detailed analyses of the preserved anatomical position and the presence of bones in a pile excavated at Chaussee-Tirancourt (Neolithic, France), that the individual was primarily buried in a seated position. A similar, although somewhat easier to discern, situation is presented in Figure 5.5: vertical position of the humeri, inferior rather than lateral slumping of the rib cage, and migration of the mandible within the initial volume of the thorax, all point toward a burial in a seated position within a delineated empty space.

Group Burials: The Study of Function Group burials are found in a number of cultural contexts. Depending on time of interment of individuals within the burial, group burials can be categorized as synchronous and diachronous. Synchronous burials can further be divided into primary, as in the case of mass burials, or secondary, as in the case of ossuaries. In the case of undisturbed tombs containing a number of buried individuals, we can presume catastrophic events: epidemics,

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Figure 5.5 Probable burial in a seated position within a delineated empty space suggested by vertical position of humeri, inferior slumping of the rib cage, and migration of the mandible within the initial volume of the thorax. (Photograph courtesy of B. Jovanovic, © STARINAR, Arheloˇski, Institut, Beograd.)

massacre, or ritual suicides of the household at the death of the master or mistress (Masset, 1993:13). Synchronous dispositions in ossuaries require that all the decedents decomposed elsewhere and were redeposited at the same prescribed time regardless of the state of decomposition. This would cause quite a variety of patterns: some of the bones may be neatly, but artificially, arranged while others may exhibit fully preserved anatomical connections as in primary burials (Ubelaker, 1974). Diachronic group burials are much more common and can be divided into primary and secondary as well. In the case of successive inhumations, it is necessary to have open access to the grave. These burials can be termed collective burials. In the case of secondary burials, the synchrony of the final interment does not imply the synchrony of death (Ubelaker, 1974, 1981; Masset, 1993), as the individuals interred might be brought in after a prescribed interval, rather than at a prescribed date. The diachronous ossuaries would differ from synchronous ones by greater uniformity of the degree of decomposition, as the skeleton would be brought in after a prescribed interval in the luminal phase of putrefaction (Metcalf and Huntington, 1991). Various aspects of mortuary ritual and functioning of the cemetery can be discerned from different accumulations of bones: space for the deposition of the corpse, evidence of rearranging, space assigned (or used) for later circulation of the members of the group. (Duday, 1981; Duday et al., 1990; Sauzade and Duday, 1979). Duday notes that at Villedubert only 40 assemblages displaying anatomical connections were found in over 53,000 recorded human bones and bone fragments. Some of the articulations, being of a very persistent nature, did not provide insight into the functions of the cemetery; others, nonpersistent in nature (interphalangial, cervical spine, vertebral), were found in place as a positive indicator of primary burials. Although animal activities could be inferred in a number of cases of nonarticulated fragments, they could not explain excessive fragmentation and disturbance. There is a strong likelihood that prehistoric humans themselves

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were the source of disturbance by rearranging graves for successive burials. This was shown through careful examination of the data: ribs gathered together as in a handful, whole skulls regrouped in limited spaces within the tomb in contrast to the presence of cervical vertebrae that were distributed over the extent of the burial, etc. Further, the fact that the atlas usually accompanied the skull points toward the rearrangement of the skulls after decomposition. Other indices discussed above also show that the bodies were deposited at different times (Duday, 1987a:53). If the totality of the information human bones carry is recorded, a number of inferences can be made. Excessive fragmentation and lack of complete bones at certain areas indicate post-burial disturbance by humans creating new burials or ancestral cults. Careful examination of skeletal elements helped determine the time and the mode of abandonment of a burial site in Corconne (Leclerc, 1987).

Conclusions Understanding taphonomic processes such as decomposition and disarticulation is crucial to understanding the function of a burial site in both its funerary and its ancestral ritual context. Ideally, presence, orientation, and association (levels of observation not traditionally documented) are crucial to such understanding. Needless to say, such observations should be made by experts knowledgeable about human osteology and anatomy. This requirement can be met only if the excavations of the burial are conducted by either a physical anthropologist or an archaeologist with extensive knowledge of anatomy and osteology. While it might be impossible to record every bone and bone fragment in the Cartesian system according to its anatomical position within the burial, the decision about the most efficient and relevant documentation should be made by an anthropologist well acquainted with the archaeological issues. In cases where efficiency is a must, photographic documentation has to be abundant. A number of careful, in situ observations are possible if the excavator is fully acquainted with osteology and can in certain cases substitute for excessive documentation. Further, taphonomy should not remain limited to the study of natural postdepositional processes affecting individual bones, although their thorough understanding is essential in avoiding misinterpretation. As taphonomy incorporates the study of the evolution of a cadaver within a burial, it has to place stronger emphasis on the context of the skeleton, the disposition of its elements, and possible explanations for the observed phenomena. All of this has to be done from the perspective of understanding cultural agents affecting the dead body. All of the inferences taken together, accompanied by data about grave architecture, bone element mobility, and temporal trends can provide insight into the ritual meaning of the burial structures. Such detailed knowledge can make possible comparisons between sites and insight about between-site similarities and variations that can be applied cross-culturally. By the nature of their study subjects, forensic experts often excavate human remains in different stages of decomposition and in different decomposition environments. These are, aside from conditions of exceptional preservation, unlikely occurrences in the archaeological record. By recording the stages of decomposition of individuals in different micro- and macrodecomposition environments and (even more importantly) sequences of disarticulation of joints, and systematizing this kind of information, forensic anthropologists can provide invaluable information that can be used to refine the interpretation of mortuary ritual.

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Acknowledgments My gratitude goes to Prof. Duday (University of Bordeaux I) whose course in taphonomy made this chapter possible, to Prof. Driver and Dr. Rogers (Simon Fraser University) for struggling through the first draft, Profs. Boyd (Radford University) and La Mota (University of Arizona) for their excellent criticism and encouragement, and to Dr. Sorg and Dr. Haglund for reviewing innumerable versions.

References Ambroise, D. and C. Perlès 1972 Étude de la position des ossements d’un squelette néolithique (sépulture collective de la Chausée-Tirancourt, Somme), L’Anthropologie 76(5–6):535–544. Andrews, P. and J. Cook 1985 Natural modifications to bones in a temperate setting, Man 20:675–691. Antunovic, M. 1991 Recherches preliminaires sur les restes humains incineres du site archaeologique de Konopiste (Mala Vrbica, Kladovo, Yugoslavie). D.E.A., Bordeaux I. Audouze, F. 1987 La sépulture d’enfant du Buisson Campin à Verberie (Oise). In Anthropologie Physique et Archaeologie, edited by H. Duday and C. Masset, pp. 147–155. C.N.R.S., Paris. Baden, M.M. 1982 Medical-Legal Aspects of Microbiology, New York Academy of Sciences, Section on Microbiology (February 17). Baud, C.A. and M. Gossi 1980 Degree of mineralization of bone tissue as determined by quantitative microradiography: effect of age, sex and pathological conditions. In Proceedings of the Fourth International Conference on Bone Measurement, pp. 345–351. U.S. Dept. of Health, Washington, D.C. Boddington, A. 1987 Chaos, disturbance and decay in an Anglo-Saxon cemetery. In Death, Decay and Reconstruction. Approaches to Archaeology and Forensic Science, edited by A. Boddington, A.N. Garland, and R.C. Janaway, pp. 27–42. Manchester University Press, Manchester. Boddington, A., A.N. Garland, and R.C. Janaway (Eds.) 1987 Death, Decay and Reconstruction. Approaches to Archaeology and Forensic Science. Manchester University Press, Manchester. Bonnichsen, R. and M.H. Sorg (Eds.) 1987 Bone Modification, Center for the Study of the First Americans, Orono, ME. Boyd, D.C. 1996 Skeletal correlates of human behavior in the Americas, Journal of Archaeological Method and Theory 3(3):189–251. Brothwell, D. 1987 Decay and disorder in the York Jewbury skeletons. In Death, Decay and Reconstruction. Approaches to Archaeology and Forensic Science, edited by A. Boddington, N.A. Garland, and R.C. Janaway, pp. 22–26. Manchester University Press, Manchester.

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Crubezy, E. and J.-C. Helas 1989 Archéologie funéraire et anthropologie: application de l’étude ostéologique in situ a l’interprétation de tombs rupestres adjacentes du cimetière médiéval de Saint-Come et Damien (Montpellier, Hérault). In La Matériel Anthropologique Provenant des Édifices Religieux, edited by L. Buchet, C.N.R.S., Paris. Dirkmaat, D.C. and L.A. Sienicki 1995 Taphonomy in the northeast woodlands: four cases from western Pennsylvania. Proceedings of the 47th Annual Meeting of the American Academy of Forensic Sciences 1:10. Seattle. Duday, H. 1978 Archaeologie funeraire et anthropologie, Cahiers d’Anthropologie 1:55–101. 1981 Le place de l’anthropologie dans l’etude des sépultures anciennes, Cahiers d’Anthropologie (1):27–42. 1985 Nouvelles observations sur la décomposition des corps dans un espace libre. In Méthode d’Étude des Sépultures, pp. 6–13. Saint-Germain en Laye, Saint-Germain en Laye, France. 1987a Contribution des observations osteologiques a la chronologie interne des sépultures collectives. In Anthropologie Physique et Archaeologie, edited by H. Duday and C. Masset, pp. 51–61. C.N.R.S., Paris. 1987b Organisation et fonctionnement d’une sépulture collective néolithique. L’aven de la Boucle a Corconne (Gard). In Anthropologie Physique et Archaéologie, edited by H. Duday and C. Masset, pp. 105–111. C.N.R.S., Paris. Duday, H. and C. Masset (Eds.) 1987 Anthropologie Physique et Archaeologie, C.N.R.S., Paris. Duday, H. et al. 1990 L’anthropologie de “terrain”: reconnaissance et interpretation des gestes funeraires, Bulletins et Memoires de la Societe d’Anthropologie de Paris, t.2(3–4):26–49. Gallay, A. 1987 Analyse de la necropole néolithique du Petit-Chasseur (Valais, Suisse). Vers un bilan méthodologique. In Anthropologie Physique et Archaeologie, edited by H. Duday and C. Masset, pp. 19–47. C.N.R.S., Paris. Garland, A.N. and R.C. Janaway 1987 The taphonomy of inhumation burials. In Burial Archaeology Current Research, Methods and Developments, edited by C.A. Roberts, F. Lee, and J. Bintliff, pp. 14–38. University of London, British Archaeological Reports International, Series 211, Oxford. Haglund, W.D. 1991 Applications of Taphonomic Models to Forensic Investigation, Ph.D. dissertation, University of Washington, Seattle. 1993 Disappearance of soft tissue and the disarticulation of human remains from aqueous environments, Journal of Forensic Sciences 38(4):806–815. 1997 Method and theory in forensic taphonomy research. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 13–26. CRC Press, Boca Raton, FL. Haglund, W.D. and M.H. Sorg 1997 Introduction to forensic taphonomy. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 1–9. CRC Press, Boca Raton, FL. Haglund, W.D., D.T. Reay, and D.R. Swindler 1989 Canid scavenging/disarticulation sequence of humans in the Pacific Northwest, Journal Forensic Sciences 34(3):587–606.

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Härke, H. 1997 The nature of burial data. In Burial and Society. The Chronological and Social Analysis of Archaeological Burial Data, edited by C.K. Jensen and K.H. Nielsen, pp. 19–29. Aarhus University Press, Aarhus. Haynes, G. 1982 Utilization and skeletal disturbances of North American prey carcasses, Arctic 35(2):226–281. Henderson, J. 1987 Factors determining the state of preservation of human remains. In Death, Decay and Reconstruction. Approaches to Archaeology and Forensic Science, edited by A. Boddington, A.N. Garland and R.C. Janaway, pp. 43–54. Manchester University Press, Manchester. Hester, J.J. and S.M. Nelson (Eds.) 1978 Studies in Bella Bella Prehistory, Department of Archaeology, Simon Fraser University, Burnaby, B.C. Hill, A.P. 1979 Disarticulation and scattering of mammal skeletons, Paleobiology 5(3):261–274. Janaway, R.C. 1997 The decay of buried human remains and their associated materials. In Studies in Crime: An Introduction to Forensic Archaeology, edited by J. Hunter, C. Roberts, and A. Martin, pp. 58–85. Routledge, London. Janssen, W. 1984 Forensic Histopathology, Springer–Verlag, Berlin. Kinnes, I. 1975 Monumental function in British neolithic burial practices, World Archaeology 7:16–29. Leclerc, J. 1987 Procedures de condamnation dans les sepultures collectives Sein-Oise-Marne. In Anthropologie Physique et Archaeologie, edited by H. Duday and C. Masset, pp. 73–88. C.N.R.S., Paris. Leroi-Gourhan, A. et al. 1962 L’hypogée II des Mournouards (Mesnil-sur-Oger, Marne), Gallia Prehistoire, 5(1):23–133. Lyman, R. L. 1994 Vertebrate Taphonomy, Cambridge University Press, Cambridge, U.K. Manhein, M.H. 1997 Decomposition rates of deliberate burials: a case study of preservation. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 469–482. CRC Press, Boca Raton, FL. Mant, A.K. 1987 Knowledge acquired from post-war exhumations. In Death, Decay and Reconstruction. Approaches to Archaeology and Forensic Science, edited by A. Boddington, A.N. Garland, and R.C. Janaway, pp. 65–78. Manchester University Press, Manchester. Masset, C. 1972a Influence du sexe et de l’âge sur la conservation des os humains. In L’Homme hier et aujourd’hui, pp. 334–343. Cujas, Paris. 1972b The megalithic tomb of La Chassée Tirancourt, Antiquity 46:297–300 + pl. 47. 1973 La démographie des populations inhumées. Essai de paléodemographie. L’Homme 13(4):95–131. 1976 Sur des anomalies d’ordre demographique observees dans quelques sepultures neolithiques. IX Congress de l’UISPP (Nice) pretirages, vol. Themes Specializes, pp. 78–107.

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1987 Le “Recrutement” d’un ensamble funéraire. In Anthropologie Physique et Archaeologie, edited by H. Duday and C. Masset, pp. 111–134. C.N.R.S., Paris. 1993 Les Dolmens: Societes Neolithiques et Pratiques Funeraires: Les Sepultures Collectives d’Europe Occidentale, Editions Errance, Paris. Mays, S. 1992 Taphonomic factors in a human skeletal assemblage, Circaea 9(2):54–58. Metcalf, P. and R. Huntington 1991 Celebrations of Death: The Anthropology of Mortuary Ritual, 2nd ed., Cambridge University Press, Cambridge, U.K. Micozzi, M.S. 1986 Experimental study of postmortem change under field conditions: effects of freezing, thawing and mechanical injury, Journal of Forensic Sciences 31:953–961. 1991 Postmortem Change in Human and Animal Remains: A Systematic Approach, Charles C Thomas, Springfield, IL. Mordant, D. 1987 Des inhumations en “pleine terre”? L’example dela Petite-Seine. In Anthropologie Physique et Archaeologie, edited by H. Duday and C. Masset, pp. 155–166. C.N.R.S., Paris. Nawrocki, S.P. 1995 Taphonomic processes in historic cemeteries. In Bodies of Evidence: Reconstructing History through Skeletal Remains, edited by A.L. Grauer, pp. 49–68. Wiley-Liss, New York. Polson, C.J., D.J. Gee, and B. Knight 1985 The Essentials of Forensic Medicine, 4th ed., Pergamon Press, Oxford. Rodriguez, W.C. and W.M. Bass 1983 Insect activity and its relationship to decay rates of human cadavers in east Tennessee, Journal of Forensic Sciences 28:423–432. 1985 Decomposition of buried bodies and methods that may aid in their location, Journal of Forensic Sciences 30:836–852. Rozoy, J.G. 1987 Manipulations celtiques dans les tombs au La Tène I. In Méthode d’Étude des Sépultures, pp. 59–63. Saint-Germain en Laye, France. Sauzade, G. and H. Duday 1979 L’abri de Sanguinouse, tombe collective du Chalcolithique ancien (commune de la Roquesur-Pernes, Vaucluse), 280–297. Sellier, P. 1985 Observations sur la position des corps dans les cimetières de Mehrgarh (Pakistan). In Méthode d’Étude des Sépultures, pp. 39–43. Saint-Germain en Laye, France. Skinner, M. and R.A. Lazenby 1983 Found! Human Remains: A Field Manual for the Recovery of Recent Human Skeletons, Archaeology Press, Simon Fraser University, Burnaby, B.C. Srejovic, D. 1969 Lepenski Vir. Nova Praistorijska Kultura u Podunavlju, SKZ, Beograd. Toots, H. 1965 Sequence of disarticulation in mammalian skeletons, University of Wyoming Contributions in Geology 4(1):37–39.

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Ubelaker, D.H. 1974 Reconstruction of Demographic Profiles from Ossuary Skeletal Samples, Smithonian Institution Press, Washington, D.C. 1981 The Ayalán Cemetery: A Late Integration Period Burial Site on the South Coast of Ecuador, Smithsonian Institution Press, Washington D.C. Weigelt, J. 1989 Recent Vertebrate Carcasses and their Paleobiological Implications, translated by J. Schaefer, University of Chicago Press, Chicago, IL. Willey, P. and L.M. Snyder 1989 Canid modification of human remains: implications for time-since-death estimations, Journal of Forensic Sciences 34(4):894–910.

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Taphonomic and Forensic Aspects of Bog Bodies DON BROTHWELL HEATHER GILL-ROBINSON Contents Introduction History, Dating, and General Preservation of the Finds The Burial Environment The Body Surface The Digestive Tract The Nervous System Connective Tissue Preservation The Musculoskeletal System Other Soft Tissues Evidence of Trauma and Pathology References

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6

120

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1400- 14511450 1500

15011550

1551- 1601- 1651- 1701- 1751- 18011600 1650 1700 1750 1800 1850

1851- 1901- 19511900 1950 1997

No find date

Figure 6.1 Dates at which there are recorded discoveries of bog bodies.

Introduction During the conflicts this century in Ireland numerous deaths have resulted. Some of these bodies have been placed in bogs and are identifiable to recent events by their clothing or other associated objects, but many bodies from these wetland sites have origins further in the past. Some are even of prehistoric date and have relevance beyond archaeology, in that they provide further information on the long-term taphonomy of bodies in bogs, and of a range of trauma and pathology in a series of individuals showing much variation in preservation. In some cases, preservation looks remarkably good, yet survival of DNA in these acid wetlands is known to be very poor.

History, Dating, and General Preservation of the Finds Because peat has been cut for fuel for many centuries, it seems likely that human remains have appeared in bogs over a long period of time. But it is only in the past two centuries (Figure 6.1) that literacy and interest in such finds have resulted in a growing number of written records about them. The total number of recorded finds probably is now in the order of 2000, but many of these are brief references, and there are relatively few wellpreserved bodies. Radiocarbon dating and associated cultural objects have enabled many of the bodies to be placed in a time sequence. Few of the prehistoric finds are earlier than 1000 BC, although the 160 bodies (mainly skeletons) from Windover in Florida are 7000 years old. Most of the earlier European bodies are in the time range 800 BC to 100 AD, and there is still much debate as to the reason for the bodies in the bogs. Was it the result of ritual, murder, punishment, or accident? Most of the more recent bodies are of post-medieval date and tend to display a better state of preservation. This may be because many of the prehistoric bodies are unclothed (or were superficially covered), whereas the more recent

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70 60 50 40

lnfant (18) Unknown

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United Kingdom

Sweden

Poland

Norway

Netherlands

lreland

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Figure 6.2 Estimated ages of the bog bodies at death (by country). 59

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MALE FEMALE UNKNOWN

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Figure 6.3 Sexes of the bog bodies by country of origin.

group were usually clothed. Immature individuals, which are not numerous (Figure 6.2), are not as well preserved as adults. No significant difference occurs between males and females (Figure 6.3), although there may be more evidence of adipocere in the females. Overall, it was possible from the data available to tentatively score the degree of preservation of the bog bodies in Europe, and this is summarized in Table 6.1. The score was based on the degree of preservation (bone, flesh, skin, etc.) in different regions of the body. Where information was limited, it was recorded as “unknown”.

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Table 6.1 European Bog Body Preservation, Scored into Eight Divisions

1. 2. 3. 4. 5. 6. 7. 8. 9.

Score

Number of bodies (N = 369)

% Total Bodies

Very poor Poor Poor to fair Fair Fair to good Good Good to excellent Excellent Unknown

107 11 85 2 7 9 73 5 70

29.00 2.98 23.04 0.54 1.90 2.44 19.78 1.36 18.97

Note: Based on a simple point scoring system. Points for skin (1), flesh (1), and bone (1) were given separately for the head, torso, arms (L and R), hands (L and R), legs (L and R), feet (L and R), hair, heart, liver, lungs, brain, intestinal tract, etc. Very poor preservation rated a score of between 35 and 41.

The Burial Environment The term bog body usually refers to human remains found in wetland peat deposits, although other mammals have been discovered occasionally. Depth of peat may vary from 30 cm to over 5 m. Waterlogged peatlands are common environments, perhaps covering nearly 5% of the earth’s surface (Brown, 1995). Surprisingly, however, human remains have been found in only parts of northern Europe, especially Britain and Ireland, Denmark, northern Germany, and the north of The Netherlands. Peat is formed at varying rates by the compaction and accumulation of plant biomass. Depending on the underlying geology, nutrients available, topography, water table level, drainage, and precipitation, raised or blanket bogs may be formed. These may be restricted or extend over a considerable area. Although about 50% of wetlands in the world are concentrated in Canada, there have been no bog bodies found in this vast territory. This is not due to major vegetation contrasts between Canada and Europe, as typical bogs in both regions are likely to contain Sphagnum moss species in particular. The different species are influenced in their distribution by moisture levels and nutrient availability (Archibold, 1995). Bogs of the southern hemisphere also have Sphagnum species well represented. A stagnant water source is critical and will significantly affect the plant succession. Bacteria are also essential in the modification of plant debris, attacking cellulose and polyphenols. It also would seem likely that microbial activity plays an important part in the differential decay of human bog bodies. Surprisingly, microbial decay is not well understood in relation to human corpses in bogs. Indeed, there is an urgent need for experimentation in order to understand the effects of such organisms on bone derived from contrasting environments (Child and Pollard, 1990).

The Body Surface Although the epidermis appears to be shed from bodies in all wetland environments, there are in fact no good records of this outer layer of skin having been separately identified. In

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Figure 6.4 Blistering of the dermis of the lower back of Lindow Man (pseudopathology).

the careful extraction of the Lindow II body, nothing of the epidermis was identified, but the dermis was for the most part well preserved. In some peat environments, it is clear that the last identifiable part of the bog body is the dermis, nails, and hair. For instance, in the case of the two Weerdingerveen bodies from northern Holland (Landweer, 1906; van der Sanden, 1995) and the Damendorf body from north Germany (Glob, 1969), it is the outer integument and keratin structures which alone have survived to any noticeable extent. Even in this advanced state of decay, the body surface can still reveal evidence of trauma, especially perforations through the skin as in the Lindow II scalp. Potentially, it may be possible to detect body surface pathology, although the blistering on the surface of the Lindow II body was in fact pseudopathology (Figure 6.4), the result of postmortem changes. Fingerprints can occasionally be well preserved, as in the male Grauballe corpse from Denmark. In the case of this individual, it was concluded that the undamaged nature of the dermal surface of the hands suggested that the individual did not undertake hard manual labor. Similar evidence has also been gleaned from the fingernails, and in the case of Lindow II, the smooth nail ends argue against hard manual labor in the individual’s life for some time before death. Hair has been found to be well preserved. In males, facial hair may be shaved off, or stubble as in Tollund man, or form a beard. In the case of the Huldremose woman and Lindow II man, there is clear evidence of cut hair ends, and in the latter case, the stepped form of some of the ends suggested cutting by scissors. Head hair of the Huldremose woman had been cut off and thrown down near the body (Figure 6.5). Hair color is usually modified as a result of burial and early decomposition. In particular, the melanin appears to oxidize to a lighter color, and in archaeological hair in general, there is a tendency to change to more ginger-tinted shades. In some, but not all bodies, early changes within the hair follicle may significantly loosen the hair from the dermis, and this may cause conservation problems when attempting to clean away peat from the head region or body surface in general. The chemistry of skin from wetland sites has been considered to a limited extent. Variation may be found even within one site, and in the Lindow II and III bodies, 12 and 10 elements, respectively, were noted (Pyatt et al., 1991a). Tests were also carried out to check for body decoration. Indigotin, which is the color in woad, was found to be negative in Lindow II. However, further skin tests using electron probe X-ray microanalysis revealed

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Figure 6.5 Frontal view of the head and shoulders of the Huldremose woman, showing hair cut off close to the scalp.

significant aluminium, silica, and copper, plus traces of titanium and zinc, and these were interpreted as residues of clay-based copper and other pigments that had been applied to the body (Pyatt et al., 1991b).

The Digestive Tract Perhaps one of the most puzzling questions associated with the preservation of bog body tissues is concerned with the occasional survival of the gut. While the intestinal tract is formed of separate layers of varying thickness and of epithelial membrane, connective tissue, smooth muscle, and mucous membrane, its function and microbial ecology would argue against its chances of survival. Nevertheless, in the case of the Danish Tollund body, much of the intestinal tract remained (Figure 6.6), although the quality of the histology is not known. We can say, however, that in the case of the restricted preservation of the Lindow II gut, the segment of small intestine did not display the contrasting tissues, but simply residual collagen tissue.

The Nervous System Because of the soft and delicate nature of nervous tissue, it would seem even less likely that any of this would survive. As yet, there seems to be no good evidence of nerves in general being identified, but the ultimate enigma is that tissue of the brain may retain its shape and quantity, although changes at a chemical and histological level have yet to be assessed. The whole brain remained a relatively normal size and shape in the Windeby girl, and indeed, the convolutions could be clearly seen (Glob, 1969). In some contrast, radiographic detail showed that the brains of the Lindow II and Huldremose bodies were partly changed and reduced in size (Figure 6.7). But why did they preserve better than stronger tissue such as muscle, ligament, and tendon? Experience by one of us (DRB) of the autopsy detail of Bosnian mass grave victims, where the bodies had been placed in deep pits about 4 years prior to excavation, again revealed well-preserved brain tissue as the common

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Figure 6.6 Part of the intestinal tract of Tollund Man.

finding. Most of these individuals had been shot through the head, allowing direct microbial access to nervous tissue, yet the brain remained visibly intact. From this evidence, it clearly cannot be argued that the brain had the double sealing effect of the endocranial tissues surrounding it and rapid burial into anaerobic conditions. Clearly, other factors are involved, but what could they be?

Connective Tissue Preservation Of the various forms of connective tissue, collagen fibers are one of the most important tissues to remain in bog bodies, maintaining the form of decalcified bones, the general structure of any remaining part of the intestinal tract, and defining the body surface, deprived of the epidermal layer. Evidence of adipose tissue occurs less commonly and has not been well studied in bog bodies. Masses of adipocere were present on the thighs, trunk, arms, and face in the Irish Meenybraddan and Danish Huldremose bodies (Delaney and O’Floinn, 1995; Brothwell, Liversage, and Gottlieb, 1990). While not confirmed, it is likely that the Windeby girl and Borre Fen III female also had some adipocere, but it seems unlikely that any noticeable deposits were present in Lindow II or III, Rendswühren man, Borre Fen I, Grauballe man, or the Tollund body. In the case of Lindow II, while adipocere was not evident, Evershed and Connolly (1988:144) point out that the fatty acid composition of the muscle tissue “suggests that processes of microbial alteration, analogous to these involved in adipocere formation, were in evidence in Lindow Man at some stage of submergence and burial” (in the bog). Could it be that where brain tissue is preserved in a recognizable state, it is due to environmental factors (waterlogging or significant dampness in particular), which initiate the rapid degradation of brain lipids that are then responsible for the maintenance of brain form (even if there are significant histological changes)? There is clearly a need for experimental burial specifically to investigate the interesting enigma of brain preservation.

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Figure 6.7 Lateral head X-rays of the Huldremose woman (left) and Tollund Man, showing brain preservation toward the back of the skull.

The Musculoskeletal System The main frame of the body, the skeleton together with muscles and ligaments, is surprisingly variable in preservation. While soft tissues generally are most likely to be destroyed, bones may be relatively well preserved, as in the Zweeloo, Tollund, and Meenybraddan bodies (van der Sanden, 1995; Delaney and O’Floinn, 1995). In contrast, the Lindow II body had greatly reduced muscle and ligaments, modified cartilage, and bones which ranged from well-shaped (vertebrae) to collapsed and fragmenting (ulna and radius). In the majority of skeletons, bones and teeth are severely decalcified by the acid bog environment, and because most have been allowed to dry naturally, they display considerable shrinkage (as in the Zweeloo body and the Lindow I skull). Some, such as the Gallagh man (O’Floinn, 1995) and Huldremose woman (Brothwell, Liversage, and Gottlieb, 1990) appear to have retained much of their body size and proportions, or at least not display evidence of shrinkage. In a number of instances the musculoskeletal system has largely decomposed, as in the Damendorf male (Glob, 1969), where only skin remained. Destruction of bone was mainly in terms of decalcification and collapse of the collagen infrastructure. Thus, although it has been well argued that Sphagnum peat has important preservative powers due to the tanning and antibiotic qualities of the polysaccharide sphagnan (Painter, 1991, 1995), there is some evidence that microbial damage does occur at times. In particular, bones of the hand of Lindow III (Figure 6.8) and part of a femur of Lindow II show punched-out lesions (Brothwell and Bourke, 1995). This could be the sequel to invasive microbial tunneling as studied by Bell, Skinner, and Jones (1996), and indeed they describe experimental work which included bacterial damage to bone from a waterlogged muskeg bog in British Columbia. Clearly, there is a need for further studies on microbial attack of bone and collagen (Child and Pollard, 1990) in bog bodies.

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Figure 6.8 X-ray of Lindow III hand bones, showing the punched-out holes of postmortem origin.

Other Soft Tissues As very few bog bodies have been submitted to CT scanning, our current knowledge of the survival of the lungs, heart, liver, blood vessels, kidneys, and reproductive systems is extremely limited. In the case of the Lindow II body, little intrathoracic or intra-abdominal soft tissue could be identified (Reznek, Hallett, and Charlesworth, 1986). In some contrast, in the Meenybraddan body, although individual organs had collapsed, shrunk, or been squashed during burial, nevertheless liver, and possibly lung, heart, and blood vessels were tentatively identified (Delaney and O’Floinn, 1995). Within the trunk, the evidence so far suggests that the intestinal tract, or part of it, is the most likely to survive. In one respect, this is fortunate, because food debris may remain — especially as fecal material — thus enabling some reconstruction of the food eaten before death (Helbaek, 1958; Holden, 1986, 1995).

Evidence of Trauma and Pathology While establishing cause of death may be problematic in the case of recent deaths, it becomes far more so when the body has been immersed in water or buried for a substantial period of time. Nevertheless, there is, at times, evidence even in partially decomposed bodies of some trauma and pathology. Data available on peat-preserved bodies indicate that 20 males and 11 females display trauma (with 4 of unknown gender). This includes possible cuts and stab wounds, fractures, decapitation, furrows in the neck (linked to cords or rope for garroting or hanging), and other wounds. Much of the evidence is in the form of cuts or fractures, and in the case of the Huldremose woman, there are multiple wounds as well as an arm clearly cut off (Brothwell, Liversage, and Gottlieb, 1990). In contrast, the Grauballe male had his throat cut and the Borre Fen III (Figure 6.9) woman was severely beaten on the head and had a fractured right leg below the knee (Glob, 1969). Tollund man (Figure 6.10) and Borre Fen male were found with ropes still around their necks. The Lindow II man was struck twice on the head (Figure 6.11), had sinew twisted around the neck, received a deep cut on the right side of the neck, and suffered a fracture dislocation at the middle cervicals of the neck (West, 1986).

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Figure 6.9 The Borre Fen woman, displaying severe head injuries.

In the case of pathology in general, surprisingly few bog bodies in the sample of 369 have been reported as showing anomalies. Eighteen males and eleven females, plus one of unknown gender, have been reported with some form of anomaly. As in the case of trauma, the pathology is mainly associated with fully adult individuals. There is a need to be aware of the possibility of pseudopathology in these human remains. In the case of the Huldremose woman, anomalous curvature of the bones of the forearm and femur was caused postmortem by decalcification and the pressure of wood within the peat (Figure 6.12). Of the wide range of pathology that might potentially have been identified, it was only possible to divide the current evidence into five categories: Harris lines, arthropathy, oral pathology, miscellaneous, and congenital anomalies and endoparasites (helminths). The latter parasites were identified as worm eggs of the species Trichuris trichiura and

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Figure 6.10 The head region of Tollund Man, with the rope still tight around the neck.

Figure 6.11 Scalp and skull injuries to the apex of Lindow Man’s head.

Ascaris lumbricoides, one or both of which have been identified in seven peat bodies (Jones, 1986). Harris lines, an indication of some form of environmental stress, have been noted in only two individuals. Arthropathy, predominantly osteoarthritis, has been recorded so far in only six individuals, with Lindow II also displaying clear evidence of Schmorl’s nodes in the lumbar region. Because radiological techniques are unlikely to pick up subclinical levels of infection, especially early periostitis, the eight cases of miscellaneous skeletal pathology must be seen as a minimum estimate. In fact, this category includes a case of sacral spina bifida and polydactyly. Oral pathology is the most commonly reported category, with eighteen individuals affected. In total, but excluding trauma, the pathology provides no evidence of the cause of death. This does not mean more pathology was not present in some of the bodies at death, but that taphonomic factors have since obscured the original changes.

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(a)

(b)

Figure 6.12 X-rays of the postmortem deformities to the forearm (a) and femur (b) of the Huldremose Woman.

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References Archibold, O.W. 1995 Ecology of World Vegetation, Chapman & Hall, London. Bell, L. S., M.F. Skinner, and S.J. Jones 1996 The speed of post mortem change to the human skeleton and its taphonomic significance, Forensic Science International 82:129–140. Brothwell, D.R. 1996 European bog bodies: current state of research and preservation. In Human Mummies: A Global Survey of Their Status and Techniques of Conservation, edited by K. Spindler et al., pp. 161–172. Springer–Verlag, Vienna. Brothwell, D. and J.B. Bourke 1995 The human remains from Lindow Moss 1987–8. In Bog Bodies, New Discoveries and New Perspectives, edited by R. Turner and R. Scaife, pp. 52–58. British Museum Press, London. Brothwell, D., D. Liversage, and B. Gottlieb 1990 Radiographic and forensic aspects of the female Huldremose body. Journal of Danish Archaeology 9:157–178. Brown, D.A. 1995 Carbon cycling in peat and the implications for the rehabilitation of bogs. In Wetlands Archaeology and Nature Conservation, edited by M. Cox, V. Straker, and D. Taylor, pp. 99–107. HMSO, London. Child, A. and M. Pollard 1990 Microbial attack on collagen. Archaeometry 32:617–625. Delaney, M. and R. O’Floinn 1995 A bog body from Meenybraddan Bog, County Donegal, Ireland. In Bog Bodies, New Discoveries and New Perspectives, edited by R. Turner and R. Scaife, pp. 123–132. British Museum Press, London. Evershed, R. and R. Connolly 1988 Lipid preservation in Lindow Man. Naturwissenschaften 75:143–145. Glob, P.V. 1969 The Bog People. Iron-Age Man Preserved, Faber & Faber, London. Helbaek, H. 1958 Grauballemandens sidste måltid, Kuml, Aarhus, 83–116. Holden, T.G. 1986 Preliminary report on the detailed analysis of the macroscopic remains from the gut of Lindow Man. In Lindow Man, The Body in the Bog, edited by I. Stead, J. Bourke, and D. Brothwell, pp. 116–125. British Museum Press, London. 1995 The last meals of the Lindow bog men. In Bog Bodies, New Discoveries and New Perspectives, edited by R. Turner and R. Scaife, pp. 76–82. British Museum Press, London. Jones, A.K. 1986 Parasitological investigations on Lindow Man. In Lindow Man, The Body in the Bog, edited by I. Stead, J. Bourke, and D. Brothwell, pp. 136–139. British Museum Press, London. Landweer, G.J. 1906 Twee Oud-Germaansche lijken uit Let Weerdingerveen, Eigen Haard 597–600. O’Floinn, R. 1995 Recent research into Irish bog bodies. In Bog Bodies, New Discoveries and New Perspectives, edited by R. Turner and R. Scaife, pp. 137–145. British Museum Press, London.

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Painter, T.J. 1991 Lindow Man, Tollund Man and other peat-bog bodies: the preservative and antimicrobial action of Sphagnum, a reactive glycuronoglycan with tanning and sequestering properties, Carbohydrate Polymers 15:123–142. 1995 Chemical and microbiological aspects of the preservation process in Sphagnum peat. In Bog Bodies, New Discoveries and New Perspectives, edited by R. Turner and R. Scaife, pp. 88–99. British Museum Press, London. Pyatt, F., E. Beaumont, P. Buckland, D. Lacy, and D. Storey 1991a An examination of the mobilisation of elements from the skin and bone of the bog body Lindow II and a comparison with Lindow III, Environmental Geochemistry and Health 13:153–159. Pyatt, F., E. Beaumont, D. Lacy, J. Magilton, and F. Buckland 1991b Non isatis sed vitrum or, the color of Lindow Man Oxford Journal of Archaeology 10:61–73. Reznek, R., M. Hallett, and M. Charlesworth 1986 Computed tomography of Lindow Man. In Lindow Man, the Body in the Bog, edited by I.M. Stead, J. Bourke, and D. Brothwell, pp. 63–65. British Museum Press, London. van der Sanden, W.A.B. 1995 Bog bodies on the continent: developments since 1965, with special reference to The Netherlands. In Bog Bodies, New Discoveries and New Perspectives, edited by R. Turner and R. Scaife, pp. 146–165. British Museum Press, London. West, I.E. 1986 Forensic aspects of Lindow Man. In Lindow Man, the Body in the Bog, edited by I. M. Stead, J. Bourke, and D. Brothwell, pp. 77–80. British Museum Press, London.

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The Effect of Cultivation on Buried Human Remains WILLIAM D. HAGLUND MELISSA CONNOR DOUGLAS D. SCOTT

7

Contents Introduction Machines for Power Farming Primary Tillage Seedbed Refining Fertilizer Application Planting and Seeding Weed, Insect, and Pest Control Harvesting Impact of Cultivation on Buried Materials Chemical Changes Mechanical Changes Surface Collections and Their Relationship to Subsurface Materials Modification of Bone Impact of Cultivation on Recovering Buried or Surface Remains Case Example The Site Methods Osteological Examination Site Analysis Human Remains from Cultivated Areas: An Investigative Strategy Conclusion References

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Figure 7.1 Two-row moldboard plow.

Introduction Archaeologists deal with sites in cultivated areas on a regular basis (Ammerman, 1978, 1985; Frink, 1984; Lewarch and O’Brien, 1981; Odell and Cowan, 1987; Roper, 1976; Yorston et al., 1990). In fact, plowing exposes subsurface archaeological sites by bringing remains to the surface. Because of this, archaeologists study how far material in an agricultural field is moved by cultivation activities and how deep the material is affected. This chapter outlines crop planting and other agricultural activities that affect buried material, discusses the relevant archaeological studies, and then presents a case study.

Machines for Power Farming The tasks necessary to cultivate a field have been the same for millennia, although the technologies used to complete those tasks have grown increasingly powerful. The basic tasks are primary tillage (to aerate and loosen the soil), seedbed refining (breaking up lumps and clods), fertilizer application, planting and seeding, weed, insect and pest control, and harvesting (Stone and Gulvin, 1977). Some activities, such as primary tillage, affect subsurface remains more directly than others, such as harvesting. Other activities involve applying chemical substances to the soil, which may affect soil chemistry. Primary Tillage The purpose of primary tillage is to aerate and loosen the soil. This prepares a suitable seedbed, destroys competitive weeds, and improves the soil’s physical condition (Smith and Wilkes, 1976). The implement most commonly used for tillage is the plow. There are moldboard plows, disc plows, subsoil plows, disc tiller plows, and rotary tillers. The most common plow for primary tillage is the single moldboard plow (Figure 7.1), which comes in two main groups that are relevant for this discussion. One-way plows throw the soil in one direction at all times. On two-way plows, the bottoms can be replaced with a set that turns the soil the opposite way. So at the end of the field, the tractor turns around,

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Figure 7.2 Disc plow. When the plow is in use, the first set of discs (vertically oriented) come toward the viewer and align with discs on the bottom.

mechanically reverses the plow bottoms, and plows into the furrow made on the last traverse. Common furrows made by moldboard plows are 14 to 16 in. across, with a depth of less than half their width. A double moldboard plow, also called a lister or middlebuster, does not turn the soil to the side, and so only forms ridges and furrows. It does not till all the soil, as the area between furrows is not turned over. The advantage is that a larger area of land can be prepared more quickly. For our purposes, it is worth noting that not all the soil in the plow zone is moved using this type of plow. The disc plow (Figure 7.2) is becoming a competitor of the moldboard plow particularly in many areas of the United States. The blades on a disc plow are usually set at an angle, and it depends on the weight of the disc and the angle for soil penetration. The soil is cut and moved with a rolling action, mixing the soil. The disc plow can be used with scrapers which help to invert the soil, although seldom as well as with a moldboard plow. Disc plows, however, do work in adverse soil conditions where a moldboard plow may become bogged down. Soil cultivated regularly over a number of years becomes very compact from the heavy machinery running over it. This can make some soils impervious to water below the plow zone. In these cases, heavy subsoil plows are used to break up the soil at a deeper level than the normal plow. Subsurface plows are designed to penetrate the soil as much as 20 to 36 in. (Figure 7.3). There are even deeper plows, called giant plows, designed to bring up soil from depths of as much as 2 to 6 ft (Smith and Wilkes, 1976:146). These are used in areas where fill or flood deposits have covered better soil. Use of the giant plow is infrequent. Primary tillage is probably the major culprit in disturbing subsurface material. The common moldboard plow disturbs objects to a depth of 7 to 10 in. below the surface, inverting the soil, and moving it sideways from its original position. Subsurface plowing breaks up the soil at depths of 20 to 36 in. The plowing itself may not move material to the surface, but breaking up the soil makes objects in the soil subject to movement through the repeated freezing and thawing of moisture in the soil, as well as insect and rodent activity.

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Figure 7.3 Subsurface chisel plow. Man and dog on right for scale.

Seedbed Refining This is also called secondary tillage and basically consists of stirring the soil at shallow depths to further pulverize the soil, cut up crop residue, and destroy weeds on fallow lands. Harrows are a common implement for this step and can be divided into the descriptively named disc, spike-tooth, and spring-tooth harrows. The spike-tooth harrow has a series of teeth that resemble spikes and commonly stir the soil to a depth of about two in. Springtooth harrows have curved teeth that penetrate to a greater depth than spike-toothed harrows. The disc harrow is by far the most common. It cuts small furrows with the front edge of the concave disc cutting the soil and stalks with the back edge acting as a moldboard, throwing the soil to the side (Stone and Gulvin, 1977:192). Pulverizers add the finishing touch to the seedbed, crushing lumps and compacting the soil after plowing or harrowing. The common V-shaped roller pulverizer consists of a number of wheels strung on a shaft commonly pulled behind the tractor. The wheels may have plain, wavy, or serrated edges, or have sprockets attached. Fertilizer Application Fertilizers come in the form of liquid, gases, and solids, and application methods are even more diverse. The machinery for spreading solid fertilizer commonly simply rolls over the soil spreading the fertilizer on the top and depending on water to move the nutrients into the roots and seeds. Planting and Seeding Planters deposit seeds evenly over the ground surface and cover each seed with soil. They may have a furrow opener, a hopper and drop mechanism for the seeds, and a furrow coverer (Figure 7.4). There are multiple types of furrow openers, depending on the seed and soil type. They can either plant at a constant depth throughout the field or at a variable depth, depending on the soil and the crop. The same is true for furrow coverers that can cover the seed with a light soil cover or a deeper one, depending on the soil and crop. Seeders may also have a fertilizer attachment that will sow fertilizer along with the seed. Finally, another attachment that also moves soil and material in the soil is a bar marker.

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Figure 7.4 Planter. Note plastic hoppers for seeds and discs for furrow openers.

Figure 7.5 Cultivator. Arrow-shaped tillers followed by harrow teeth are moved between the crop rows to destroy the weeds.

These drop at the side of the seeder to mark the edge of the last row planted so that the tractor driver can easily follow the edge of the row back to the end of the field. Planting and seeding devices operate a much shallower depth than plows. Their impact on bone and evidence in the soil mainly will be to subject material near the surface to yet another yearly instance of being pulverized, dragged, and compacted by heavy equipment. Weed, Insect, and Pest Control The war on weeds is carried out by cultivators that stir the soil, burning, chemicals, or laying plastic strips between the rows. The mechanical cultivator can be at the front or rear of the tractor and tills the ground between the crop rows (Figure 7.5). As with the seeders, there are various types of cultivators for different soils and crops, but they operate at a shallow depth relative to the plows. Flame cultivators can also be mounted on a tractor, and consist of a fuel tank, feed lines, control valves, and burners. The concept is that the plants to be cultivated are larger and woodier than weeds, and the weeds will burn first. While this system doesn’t move

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the soil it, too, could be detrimental to surficial bone and evidence by charring or burning either or both. Chemical measures to control weeds, insects, and pests are frequently applied by sprayers or dusters and do not mechanically impact material in the soil. Harvesting Harvesting equipment can be very crop specific: mowing machines, rakes, and balers for hay; the combine (harvester-thresher) for grains; specialized corn harvesters; cotton strippers; cotton pickers; sugar-cane harvesters; tobacco harvesting machines; and root crop (potato, sweet potato, beet, peanut) harvesters. Root crop harvesters are the machines with the most impact to the soil, usually having a blade running deep enough to scoop up the crop. They differ from other machinery in that they merely separate the crop from the soil.

Impact of Cultivation on Buried Materials Soil in a cultivated field is plowed, pulverized, crushed, fertilized, aerated, compacted, burned, and thrown into a harvester. Overall, these activities have a high potential to be detrimental to the investigation of buried remains. Archaeologists have completed a number of studies on cultivation of archaeological sites and how it affects their ability to reconstruct past human activities at a site (Ammerman, 1978, 1985; Frink, 1984; Lewarch and O’Brien, 1981; Odell and Cowan, 1987; Roper, 1976; Yorston et al., 1990). As this is directly relevant to the ability to reconstruct the activities at a clandestine burial, these studies will be briefly summarized. Chemical Changes The local chemical environment is one of the major factors affecting the decomposition of human remains (Gill-King, 1997). Chemicals added to fields include fertilizers, pesticides, and herbicides. Commercial fertilizers are usually composed primarily of oxygen, nitrogen, and phosphorus with traces of a number of other elements. Organic fertilizers, such as manure, have high amounts of organic material and bacteria, as well. These are usually spread on, or near, the ground surface, and target the nutrients toward the level of the plant roots, where many are absorbed. The chemicals do penetrate further into the soil, usually as surface water moves through the soil into the groundwater. It is likely that many fertilizers accelerate the decomposition of soft tissue by providing nutrients for bacterial growth. The chemical composition of pesticides and herbicides is widely variable with over 30 companies producing over 150 brand names of herbicide applications (Smith and Wilkes, 1976). The variability of these compounds makes it impossible to give a blanket statement about their effects on buried human remains. If any chemical tests are planned on the remains, then soil samples, as described below, should be collected. Detailed chemical analyses of a number of these compounds, particularly pesticides, can be found on the Internet. The U.S. Department of Agriculture operates a web site (http://www.arsusda.gov/rsml/ppdb3) that lists pesticides and their molecular formulas, physical state (gas, solid, liquid), water solubility, and field dissipation half-life. Other web sites include ChemFinder (http://www.chemfinder.camsoft.cam/), EXTOXNET

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(http://www.ace.ace.orst.edu/info/extoxnet), and Spectrum (http://www.speclab.com/ compound/chemabc.htm). The interaction of soil and bone chemical constituents is a process called diagenesis. The chemical composition of bone reflects the diet of the individual; thus, archaeologists are interested in bone chemistry and the interaction of soil and bone chemistry. Much of this body of literature is summarized by Whitmore and others who include a summary table of postmortem impact on bone by various elements (Table 5.2, Whitmore et al., 1989:220–239). For forensic purposes, it is sufficient to note that, given a generally basic soil pH, bone can be found in soil after tens of thousands of years. Should the investigator wish to complete any chemical testing on the remains, samples of the soil adjacent to the body should be taken. These will give the chemists an idea of the postdepositional environment of the remains and potential diagenetic conflicts with the test results. The first step in taking a soil sample is rinsing the implement (usually a trowel) with which the sample will be taken in water, preferably distilled water, in order to prevent contamination of the sample with other elements or soil. The first several millimeters of soil on the exposed surface are then scraped away, again in order to avoid contamination, and about 1.5 cups of soil placed in a clean plastic Ziploc™ bag. This bag is closed and placed in a second, labeled Ziploc™ bag. A piece of paper labeled with the provenience information can also be placed between the two plastic bags and provides the needed information if the labeling on the bag becomes smeared or wiped off. The location of the sample should be placed on the scene map. Two or three of these samples from different areas around the body will normally be sufficient. The sample should be stored in a refrigerator to prevent growth of molds or fungi. Mechanical Changes Plow zone studies follow three general lines of inquiry: (1) interpretation of surface collections and their relationships to their original locations; (2) displacement of artifacts both horizontally (lateral) and vertically; and (3) damage to the material from cultivation activities. These studies have been pursued through actual archaeological sites, experimental models, and computer simulations. Some authors concluded that the effects of cultivation are minimal (Odell and Cowan, 1987; Roper, 1976), while others contend this is a rather sanguine and complacent stance (Yorston et al., 1990). Nevertheless, cultivation can affect the site at the feature, artifact, or attribute level. Surface Collections and Their Relationship to Subsurface Materials Surface collections have long been used as a guide to locating subsurface materials and as a sample of what materials are at a site (Redman and Watson, 1970). Surface assessments are less expensive than excavation to carry out and, relative to excavation, require much less time and resource investment. Additionally, surface assessment minimizes disturbance to the site. Although the dislocation of artifacts moved by the plow disrupts spatial relationships of artifacts within the plow zone, Roper (1976:374) claims, “Archaeologists working in areas of intensive agricultural activity should be able to use surface scatter as a reliable indicator of subsurface distributions.” The relationship between surface artifacts and subsurface feature or artifact distribution is rarely straightforward (Yorston et al., 1990). Surface representation is subject to

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change from one bout of tillage to another and artifacts or bones recovered from the surface represent only a fraction of the subsurface assemblage (Ammerman, 1985). Lewarch and O’Brien (1981) originally estimated surface-to-subsurface assemblage ratios to represent 1 in 20. They later adjusted this estimate to less than 10% (1981). An elegant study (Odell and Cowan, 1987) confirmed a mean surface representation of 6.63%, close to the 1 to 20 figure given by Lowarch. Other estimates have ranged up to 15–16% (Reynolds, 1982), and 15% (Frink, 1984) of artifacts in the plow zone are seen on the surface. However, Reynold’s experimental design has been criticized because of the lack of variability in the shape and size of artifacts collected. Additional findings suggest that artifacts within the plow zone have a probability of reappearing on the surface every 6 or 7 years. Both experimental studies and archaeological materials studies suggest that the greatest concentration of surface material will be near the original site (Odell and Cowan, 1987; Redman and Watson, 1970; Yorston et al., 1990). Based on these studies, a potential investigative strategy used to look for a specific subsurface feature, such as a grave, is to mark all surface remains with a pin flag. Rain washes surface artifacts, making them more visible. A similar effect might be expected from irrigation. Intense summer light increases surface reflection and visibility of surface artifacts; however, it is best first to look at horizontal displacement of materials and excavate the area where the concentration is greatest. More studies have been completed on the horizontal, rather than vertical, movement of artifacts in the plow zone. The dominant direction of displacement is in the direction of tillage activity (Nartov, 1979; Odell and Cowen, 1987). Movement is most prominent in first passes and artifacts are affected to a lesser degree with successive tillage; however, the directional change is cumulative. When the tillage pattern is reversed from year to year (i.e., the plow is used in the opposite direction), the artifact movement is reversed. There is relatively little transverse flow of materials across furrows (Nartov, 1979). Spurious clusters can be created by lifting the plow or disc, thus either skipping artifacts or dropping all the artifacts rather than spreading them out. Differences in the topography of the field can also cause artifacts to cluster as they may be harder to drag upslope and may travel downhill with soil erosion. Potential displacement is greatest on slopes, where the downhill movement of material is assisted by rain and drainage. In a cultivated field, it is likely that part of the year there will be vegetation on the slope and part of the year there will not. Vegetation does inhibit downslope movement (Rick, 1976). Vertical dislocation of material in the plow zone is less studied; however, it appears that larger artifacts are more abundantly represented at the surface relative to their proportion in the total population (Ammerman and Feldman, 1978). Over time, fragment size on the surface becomes more heterogeneous as the plow fractures breakable material. The distance that bones and artifacts are moved from the original location is influenced by the size of the element or artifact, the duration and direction of tillage, and the topography of the field. Modification of Bone As buried deposits are disrupted by tillage practices the material is subject to mechanical abrasion and breakage. Fresh bone breaks differently than older, dry bone and as bone dries out, it will be more subject to fracture. Compaction of the soil as heavy machinery rolls over subsurface, or surface, elements may lead to fracturing of elements. This will occur not only during the plowing, or primary field tillage, but any time that machinery

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is run over the field. After harvest, cows or other animals are frequently allowed to graze in fields, and this will subject the surficial elements to trampling as well as being run over by farm machinery. Bones in the plow zone are subject to sharp and blunt force modification by machinery, which can result in simple breaks or, in very dry bone, splintering. Abrasion can also occur on bones through direct contact with the agricultural machinery, or through contact with other cultural or natural inclusions in the surrounding soil matrix as movement initiated by the machinery occurs. Once exposed to the surface, the skeletal elements begin to weather; in other words, they are affected by the combination of sunlight, temperature differentials, and moisture. Exposure to the sun and heat from the sunlight will dry the bone and bleach it. As small fractures occur in the bone, moisture will seep into them and expand as the temperatures lower, causing weather “checking” or exfoliation of the material. These factors destabilize the bone and cause accelerated decomposition. Skeletal elements exposed to the surface for a greater period of time should have a lighter color, less grease (be dryer and lighter), and may show variations in, and exfoliation of, the periosteal material. Impact of Cultivation on Recovering Buried or Surface Remains Cultivation activities can displace skeletal elements and evidence vertically and horizontally from their original position. They can fracture bone into increasingly smaller pieces, hence increasing exposure that accelerates weathering and decomposition. Plowing, tilling, and other cultivation activities may disperse remains within the plow zone from their primary resting places, and through repeated tillage episodes redistribute previously displaced materials. The plowing process may break up and mar bones. The overall impact of cultivation will depend upon the depth of the burial, the soil type, the crops grown, the cultivation strategy, and the number of episodes of cultivation that the land has undergone. It is also dependent upon the length of the postmortem interval and the condition of the remains.

Case Example A four-person forensic team was deployed to Cyprus in 1997 to investigate a potential gravesite for the remains of an American of Greek-Cypriot ancestry. The man disappeared during the military events of August, 1974 when the Republic of Cyprus was torn by military conflict resulting in the partition of Cyprus into a Greek southern portion and a Turkish northern portion. During the military activity, the Turkish Army and Turkish Cypriot Militia arrested many Greek males ages 15 to 50. Turkish Cypriot militia units were given the responsibility of guarding the prisoners. The missing person was a 17-year old American citizen of Greek-Cypriot descent who was arrested by two Turkish militiamen at his home August 20, 1974. Also arrested was his sister’s 23-year-old fiancé, a Greek Cypriot. According to information gathered by investigators, the two men were taken to a detention camp situated near agricultural fields several kilometers from the nearest town. No trace of either man has been found since they were last seen at the camp. On a humanitarian basis, the United States government, in 1981, supported the formation of a tripartite Committee on Missing Persons (CMP) under the auspices of the

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Figure 7.6 View of site area to east. Excavations are over the area of the bone concentration. Trees on the right side of the photograph mark the small rise with the well in the center.

United Nations. The CMP, comprised of a Greek Cypriot, a Turkish Cypriot, and an international member, accumulated a great deal of information about the missing of 1974. United States Public Law 103-372 was passed October 1994 mandating “the investigation of the whereabouts of the United States citizens and others missing from Cyprus since 1974.” Pursuant to the law, an investigative team under the direction of Ambassador Robert S. Dillon (retired) and Investigator Edward L. Lee II began work in 1995. Their report concluded that five Americans were missing from 1974. Four were elderly and probably dead (Dillon and Lee, 1995). The fifth man, the subject of this discussion, was 17 years old in 1974 and was considered missing and probably dead. During the recent investigation, informants were interviewed. They were able to describe the location of the detention camp, the last place the missing man was known to be alive. Comparing this statement with previous interviews of two soldiers and other corroborating evidence, Ambassador Dillon’s team felt the story was credible and recommended an effort to recover the remains. In 1997, the Turkish Cypriot Member of the CMP requested technical assistance from the U.S. government to locate the remains. The mission described here was the result. The Site When the technical team arrived they were told the site was purportedly near two wells and large bushes. The team was taken to the general area located in a microenvironment that matched the description. A large mound, built around a limestone cut-block well shaft and an island of vegetation which included a eucalyptus tree, very large yucca-type plants and large fern-type plants, marked the site area (Figure 7.6). A smaller mound between the well and the road consisted of straw-filled mud and probably marked the site of a former mud brick structure. A second well was approximately 100 m west of the first. Eucalyptus trees lined the road to the west of the well and a stand of approximately five olive trees lined the north side of the road to the west. Clothing, water bottles, and aluminum cans were hanging or placed in the trees, apparently by the field workers. A

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general scatter of trash had accumulated around the tree area. A variety of ceramics in the immediate area around the well and the tree area suggested that a relatively recent archaeological site was present as well. The fields on either side of the road were planted in barley at the time of the investigation. The barley was in its early growth stage, and ground visibility in the fields was approximately 80%. The edges of the fields and the mound around the well were covered in a dense stand of clover and ground visibility was closer to 10% in those areas. The team gained better visibility by working on their hands and knees and either pulling the clover up or cutting it off at ground level. Methods The initial method of investigation was a visual observation of the site surface. The fourmember forensic team lined up at approximately 1.5-m intervals and walked successive parallel transects in a north and south direction covering an area approximately 100 m north to south by 65 m east. As bones or other potential evidence were identified, each location was marked with a surveyor pin flag. The visual inventory identified human tarsals on the surface in the first pass across the relatively flat agricultural field. Unassociated fragments of cloth and foot apparel were also found. The area immediately surrounding the well contained a moderately dense surface concentration of modern domestic trash, including ceramic shards, tin cans, aluminum foil, and other metallic debris. These items were undoubtedly associated with agricultural and pastoral activities conducted on the site. The open well was examined by lowering team leader Haglund to the bottom on a stout rope. The well was dry and approximately 10 m deep. Skeletal remains of a domestic sheep were found as were tree branches and decomposing vegetation, but no human remains were observed. After completing the visual inventory of the field, a metal detecting inventory was begun. The metal detecting effort, using a White’s Classic SL with an 11.5-in. coil, was concentrated in an area measuring 25 m north to south by 30 m east to west and around the area where human bones were found. Sweeps were made in an east to west direction with overlapping transects to insure as complete a coverage as possible. The soils and rocks proved to contain minerals that affected the detector’s sensitivity. The detector was tuned to eliminate the mineralized soil and rocks. The metal detecting identified approximately 30 additional surface and buried targets in the search area. Each target was flagged as it was identified. After completing the initial metal detector search the targets were excavated and examined. The same metal detector was used to examine the targets. A smaller coil (4-in. diameter) was used to pinpoint the metal targets. Each target was dug with a 4-in. mason’s pointing trowel by scraping away the earth until the object was encountered. Each target was examined and identified by an archaeologist. All metallic targets were domestic trash including tin cans, a large iron hook, and fragments of various metal containers. No bullets, cartridge cases, or other items potentially related to causes of death or identification were encountered. Following the metal detector inventory, the pin flags marking human bone, shoes, or pieces of cloth were individually numbered or lettered, and the associated remains mapped and collected. An east–west baseline was established to facilitate mapping using standard

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OLIVE TREE

WELL

BUSH/ TREE ∞ ∞ ∞ ∞∞

1M

HUMAN REMAIN MAPPING BASELINE

SCAPULA FRAGMENT

N505/E500

FOOT BONES FEMUR FRAGMENT

N500/E500

ROAD

MANDIBLE FRAGMENT

VERTEBRA

N500/E520

VERTEBRA

CRANIA FRAGMENT

Figure 7.7 Site map showing distribution of recovered bones and bone fragments. (The rectangle and the oval within it mark the mound of a former mud brick structure.)

triangulation techniques. All flagged items were entered on the site map (Figure 7.7) and placed in a bag or envelope with the corresponding number or letter. The surface distribution of skeletal elements suggested that it was most likely that the original grave was near the concentration of bone at the west side of the site (Figure 7.7). So, two team members established Excavation Unit 1 (initially 2 m wide and 4 m long) oriented along the axis of a concentrated distribution of human tarsals and metatarsals. The unit and all subsequent excavation units were excavated by hand using shovels, trowels, brushes, bamboo excavation tools, and other standard archaeological tools. All fill was screened through a 1.0 cm ¥ 0.5 cm wire mesh screen. The units were excavated down to undisturbed sterile subsoil to insure no human bone, grave features, or other cultural manifestations were missed. Approximately 11 m2 around the bone concentration was hand excavated in the manner described above. Excavation extended below the plow zone so that the excavator could identify any discontinuities in the soil. Such a discontinuity could have indicated a grave. An additional 4 m2, in two 2 m ¥ 1 m strips, was shoveled past the depth of the soil disturbed by the plow to look for further remains and examine the soil for discontinuities. None were found. At this point, the forensic team requested the use of a backhoe or front-end loader. The machine, a Massey-Ferguson tractor with backhoe and front-end loader, was provided. The entire area between the well and the road was graded well below the depth of soil disturbed by the plow. A cement floor, approximately 2 m ¥ 3 m, was encountered at a depth of approximately 30 cm below the surface of a low earth mound. A few pieces of cut limestone and numerous pieces of unshaped limestone were laid over the edges of the cement floor. These formed a rock foundation for mud brick walls that had nearly completely eroded away. The feature may have been a small house, a pump house, or a capped well. The backhoe was used to remove the cement floor in an effort to ascertain if anything

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Table 7.1

Inventory of Recovered Skeletal Remains

Skeletal Remains Collection Number

Element

Condition

1

Right calcaneus

2

Left 3rd metatarsal

Complete

6

Femoral shaft fragment

Fragment

7

Right navicular and right proximal; 2nd phalange

8

Right cuboid and right middle cuneiform

Complete

9

Right proximal 1st phalange

Bleached, surface erosion

Femoral shaft fragment

Fragment

11

Complete, stained

a

Parietal bone fragment

Fragment

12b

Mandibular condyle

Fragment

13

Partial upper thoracic vertebrate

Fragment

14

2nd cervical vertebrate

Bleached, weathered, complete

10

Femoral shaft fragmenta

Bleached, longitudinal cracks, spalled cortex

16

Left 4th metatarsal

Complete

17–20

Left middle phalanges 1–4 and left distal 1st phalanges Complete

21

Left 2nd metatarsal

Complete

22

Right 1st metatarsal

Complete

24

Left 1st metatarsal

Complete

25

Right talus

Complete

26

Right 2nd metatarsal

Complete

27

Left distal scapula fragment (inclusive of glenoid fossa, coracoid process, and distal inferior border)

Irregular fractured margins; bleached, longitudinal cracks; some spalling

Left 5th metatarsals

Distal ends missing

Left middle phalanges 2 through 5

Complete

16 and 23 17–20

Femoral fragments 6 and 10 conjoined to form 23-cm length of lateral femoral shaft. Note: Missing numbers were collected, nonskeletal materials. a

was present below the structural feature; only natural clay soil was present. The grading continued around the south, east, and west sides of the well. An area 12 m east to west and 15 m north to south (between the road and the well) was excavated to depths ranging from 1 m to 2 m. No evidence of cultural features was noted. The unexcavated plowed field was also reinventoried and one additional human bone, a fragment of the glenoid region of a left scapula, was located, mapped, and collected. In all, over two dozen human skeletal elements and fragmented bones were recovered (Table 7.1). Their distribution is shown in Figure 7.7. Except for undisturbed right and

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left foot elements found in situ, the majority of the bones and bone fragments were recovered from the surface. Elements of the upper body (crania, scapula, and vertebra) were furthest from undisturbed foot bones at the eastern extreme of the bone distribution. Osteological Examination Differential weathering of the skeletal elements collected from the surface suggests that they were exposed for varying lengths of time for intervening periods from 1974. The extremely weathered long bone shaft and scapular fragments lay exposed during several seasons, although, because of their small size and the irregularities of the ground surface, their exposure would not have been as total as complete bones. Elements of the right ankle were probably exposed during more recent cultivation activities. Other elements were found within the plow zone but were unexposed and probably most recently disturbed from a burial. Morphologically, these skeletal remains represented the remains of a minimum of one individual of undetermined sex. The maturity of the remains suggested an individual of at least late adolescent to young adult age at time of death. Based on the size, articulation, and other common factors, the left and right tarsals and metatarsals were definitely from the same individual. Identification was based on mitochondrial DNA analysis. However, the remainder of the bones (6, 10, 11, 12b, 13, 14, and 27) could represent one or more additional individuals of approximately the same age and build. Site Analysis No soil discontinuity indicative of a grave was discovered. The human remains were scattered a maximum distance of 32 m east to west and 14 m north to south. The left and right foot elements were in a cluster less than 4 m in diameter, and in association were several fragments of simulated brown leather foot apparel. These shoe fragments are of lightweight construction consistent with a house slipper, although they were too fragmentary for definitive identification. The remains were in, and adjacent to, a field sown in barley. The machines observed in the area cultivating the fields were medium-powered farm (60 to 75 horse power) tractors (Culpin, 1975:4–7). Some cultivation machinery was observed in operation and others were seen sitting at the edge of fields. No moldboard plows were observed, but harrows and discs were seen on several occasions. This was probably because the crop was past the stage of primary tillage. Six- to eight-row seed grain drills were observed that combined a small plow or subsoiler to cut the furrow, the device to drop the seed in the furrow, and harrows or discs to cover the seed to a uniform depth (Culpin, 1975:96). The machinery observed would turn the soil to a 7 to 10 in. depth, consistent with the depth of the plow zone observed in the excavations at the well site. The linear distribution of the skull, vertebrae, scapula, and femur fragments was consistent with cultivation activities over a number of seasons. The disarticulation and mixing of the right and left foot elements were also consistent with disturbance from the primary burial context due to plowing and related activities. The presence of the broken and disarticulated human bones across the field suggested the original burial location was nearby and probably relatively shallow. The burial site was probably somewhere within the low mound south of the rock-lined well, and subsequent agricultural activities over the ensuing 23 years dispersed the remains and obliterated the grave itself.

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UNPLOWED AREA

PLOWED FIELD

UNPLOWED AREA BONE FRAGMENTS B

PLOWED FIELD

B

UNPLOWED AREA

B B

B

PLOWED FIELD B

B

PLOWED FIELD BB BB BB B B

B

B

B

B

B

Figure 7.8 Model of burial destroyed by cultivation activities.

A model the authors propose for the distribution of the remains is described in Figure 7.8. The grave may originally have been shallow and outside the area then cultivated. Over time, possibly as the remnants of the deteriorated mud brick wall became plowable, the farmer expanded the area plowed and began to catch portions of the burial in the equipment. The larger bones were moved furthest and survived longest. The cranial vault was crushed into smaller pieces, one of which was pushed to the side of the field where we found it. Many of the smaller bones were probably pulverized in secondary tilling or cultivating. The feet were either deepest or furthest from the plowed area, but appear to have been the last elements brought to the surface.

Human Remains from Cultivated Areas: An Investigative Strategy The burial of human remains within the depth of soil disturbed by the plow and other agricultural activities is not conducive to long-term preservation, or to the preservation of evidence to determine cause of death and identification. In the case example, the decedent was buried approximately 23 years before the investigation, and it is likely that no remains would have been found in another few years. The remains collected were not enough to determine cause of death. It was only luck, and access to extremely good DNA specialists, that allowed the investigators to collect remains from which DNA could be extracted and the identification made. In this case example, due to political reasons, it was not possible to talk to the men who cultivated the land. However, a number of questions about the type of farming were relevant to the investigation. The type of crop grown, the type of plow and other field

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equipment and fertilizer used, and the typical plowing pattern were agricultural information helpful to the investigation. The investigators had to rely on their own observations, but it would have been much more informative to talk directly to the farmers. During the first few months after burial, a depression is the best indicator of a grave area, the sharpness of which may vary with the soil type. Postburial precipitation hastens the formation of the depression. Rain, or irrigation, sufficient to dampen soil 2 to 3 ft below the surface results in a depression. There should be visible cracks in the soil in the grave depression that are wide (1 to 2 in.) and fairly deep (up to 10 in.), depending on the soil type. Cultivation tends to mask the grave depression (Duncan, 1983:13). The best chance of visually recognizing a depression in a cultivated area is directly after the area has been plowed, disced, or harrowed. Subsoil may even have been inverted to the surface, visually marking the disturbed area. Talking to the field hands may determine whether they noticed a depression in the field, or remembered that the wheels of the tractor sank into the ground at a certain location (Duncan, 1983). Interviewing the field hands also would include outlining the agricultural strategy. Hence, the number of inversions of the soil is important in determining the amount of potential disturbance. The pattern and direction of plowing are also significant. Knowing the time since death and the cultivation usage the land has undergone will focus the direction of searches. The most successful search will be early in the growing season before the crop obscures visibility. Rain washes the dust from objects on the surface and makes them easier to see, so conducting the search directly after a rain also helps ensure success. Finally, the glare from the sun is worst when it is directly overhead, and pieces in the ground are easiest to see either early to mid-morning or mid-late afternoon. The initial search in a plowed field should be conducted by a series of investigators lined up shoulder-to-shoulder and walking the field in the direction of the furrows. Each should carry surveyor pin flags and place one next to any potential piece of human remains or evidence. Bone fragments are not easy to recognize in the dirt, and the search should include an anthropologist or others with experience in recognizing dirty, fragmented bone and determining whether it is human or animal. When the investigators are sure all visible material has been flagged, a metal detector should be used on the relevant area. This may lead to subsurface concentrations of material, as well as to metal objects that were on the surface, but not spotted. By this time, a pattern should be apparent in the placement of the pin flags. It will probably be linear. There may be a concentration on one end of the line, as there was in the case example. However, if the field has been plowed in different directions over the years, the material may be more dispersed. The area with the greatest concentration of materials should be hand excavated, as this suggests that it is the area closest to the original subsurface feature. In any case, the soil should be removed below the depth disturbed by the plow, in order to look for a soil disturbance consistent with a grave. Additional material can be found by dividing the entire area containing remains into square units and shoveling the soil, to the depth of the plow zone, through 1/4-in. hardware screen. Although extremely laborious, this method will collect pieces of bone in the plow zone, but not currently on the soil surface.

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Conclusion Recovery of human skeletal remains from areas that have been cultivated is enhanced by an understanding of cultivation practices and their potential impact on subsurface materials. Ideally, recovery strategy should involve interviews with those who participated in the cultivation activities. For disturbed graves, return site visits should be considered.

References Ammerman, A.J. 1985 Plow-zone experiments in Calabria, Italy, Journal of Field Archaeology 12:33–40. Ammerman, A.J. and M.W. Feldman 1978 Replicated collection of site surfaces, American Antiquity 43:734–740. Culpin, C. 1975 Farm Machinery, Granada Publishing, New York. Dillon, R.S. and E.L. Lee 1995 The President’s Report to Congress on the Investigation of the Whereabouts of the United States Citizens Who Have Been Missing from Cypress since 1974, Office of Southern European Affairs, Department of State, Washington, D.C. Duncan, J. 1983 Excavation and Recovery, In Handbook of Forensic Archaeology and Anthropology, edited by D. Morse, J. Duncan, and J. Stoutamire, pp. 13–14. Rose Printing, Tallahassee, FL. Frink, D.S. 1984 Artifact behavior within the plow zone, Journal of Field Archaeology 11:356–363. Gill-King, H. 1997 Chemical and ultrastructural aspects of decomposition. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 93–108. CRC Press, Boca Raton, FL. Lewarch, D.E. and M.J. O’Brien 1981 The expanding role of surface assemblages in archaeological research, Advances in Archaeological Method and Theory 4:297–342. Nartov, P.S. 1979 Movement of soil masses by working surfaces of spherical discs, National Tillage Machinery Laboratory Report NTML-WRG876, Auburn University, Alabama. Odell, G.H. and F. Cowan 1987 Estimating tillage effects on artifact distributions, American Antiquity 52:456–484. Redman, C.L. and P.J. Watson 1970 Systematic, intensive surface collection, American Antiquity 35:279–291. Reynolds, P.J. 1982 The plow zone, Festschrift zum 100 Jahrigen Jubitaun der Abtelung der Naturhistorischen Gesellschaft, Nürnberg. V. 315–341. Rick, J.W. 1976 Downslope movement and archaeological intrasite spatial analysis, American Antiquity 41:133–144. Roper, D. 1976 Lateral displacement of artifacts due to plowing, American Antiquity 41(3):372–375.

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Smith, H.P. and L.H. Wilkes 1976 Farm Machinery and Equipment, 6th ed., McGraw-Hill, New York. Stone, A.A. and H.E. Gulvin 1977 Machines for Power Farming, John Wiley & Sons, New York. Whitmore, A.M. et al. 1989 Stability or instability: the role of diffusion in trace element studies. In Archaeological Method and Theory, Vol. 1, edited by M.B. Schiffer, pp. 205–273. Academic Press, New York. Yorston, R.M., V.L. Gaffney, and P.J. Reynolds 1990 Simulation of artifact movement due to cultivation, Journal of Archaeological Science 17:67–83.

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Detection and Recovery of Abducted and Murdered Children: Behavioral and Taphonomic Influences ROBERT J. MORTON WAYNE D. LORD Contents Introduction Child Abduction Prevalence Child Abduction/Homicide Characteristics Child Remains: Disposal, Discovery, and Distances Issues of Decomposition and Child-Sized Remains Animal (Swine) Model Research Field Research Data Site #1 Site #2 Site #3 Site #4 Site #5 Child Abduction Case Histories and Disposal Scenarios Case Study #1 Case Study #2 Case Study #3 Case Study #4 Multidisciplinary Approaches to Search/Recovery Strategies References

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8

Introduction Although child abduction/homicides comprise less than 1% of all murders (Hanfland et al., 1997), these cases are extremely high profile. Public and media attention is often overwhelming and national in scope. The value placed on children by families, communities, and entire societies often results in a greatly heightened public focus during child abduction cases. The overwhelming attention and concern generated when a child is abducted produce intense internal and external scrutiny during law enforcement investigations. Law enforcement agencies are routinely faced with strained resources, an immediate and intense demand for answers, and the seemingly insurmountable task of attempting to locate and safely return victims. In child abduction cases, the ability to rapidly locate, recover, and return victims to loved ones becomes crucial for the law enforcement community.

Child Abduction Prevalence While the greatest number of child abduction cases (approximately 350,000) reported in the United States each year involve parental discord and custody disputes, approximately 100,000 attempted abductions by non-family members occur each year (Finkelhor et al., 1992). Most of these non-familial abductions are of short duration, are perpetrated by acquaintances, and involve varying degrees of sexual abuse. Fortunately, only about 200 to 300 non-family abductions involve the taking of the child for an extended period of time, the transportation of the child a significant distance from the place of contact, and the intent to keep, ransom, or kill the child. Annually within the United States, however, 40 to 150 children are abducted and killed by strangers (Hanfland et al., 1997). Homicide rates for infants and children (ages 0–4) have risen to their highest levels in 40 years. Finkelhor (1997) indicates that child homicides have risen 50% over the last 3 decades.

Child Abduction/Homicide Characteristics Recently, two major studies have examined the characteristics of victims, offenders, and offenses in cases of child abduction and child homicide. Both studies revealed commonalities in the behaviors and methods employed by predators and their motivations. In 1996, the FBI sponsored research into the epidemiology of child abduction and homicide, looking at 550 cases from 47 states, drawn from FBI files over a 10-year period (Boudreaux et al., 1999.) Cases in this study were drawn from the FBI’s Violent Criminal Apprehension Program (VICAP), and the National Center for the Analysis (NCAVC). VICAP is a national database utilized by police agencies to link unsolved violent crimes. The NCAVC serves as the FBI’s primary child abduction investigative and research entity. The parameters for case inclusion in the study were twofold. First, the victims were required to meet the federal definition of a child (0 to 17 years old). Second, cases were required to have been reported to the FBI as an abduction, suspected abduction, or murder with abduction originally suspected or reported. This study divided case data into four general categories: the offender, the victim, the offense, and remains disposal characteristics. The study categorized victims into seven age groups: neonates, infants, toddlers,

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preschool, elementary school, middle school, and high school. Offenses were divided into five motivations: sex, emotional, profit, infant replacement (maternal desire), and unknown motivation. In 1997, The Washington State Attorney General’s Office, working through a grant from the United States Department of Justice, Office of Juvenile Justice and Delinquency Prevention (OJJDP), published a Research Findings Report, titled “Case Management for Missing Children Homicide Investigation” (Hanfland et al.1997.) The study included 577 cases from 44 states, 621 victims, and 419 killers, including a mix of juvenile and adult victims. The study included cases involving adult victims only when they were part of serial crimes involving juvenile victims. Of the 621 victims, 562 were under 18 years of age. Cases were obtained through written requests sent to police departments nationwide. Case data were obtained through interviews conducted with police agencies having cases meeting the inclusion criteria. Case inclusion required the homicide of a victim (or victims) younger than 18 years old, that the case was worked by the police agency as an abduction, or that the case was a part of a homicide series in which at least one victim met the first two criteria. The study also compared features of all homicides to child abduction homicides.

Child Remains: Disposal, Discovery, and Distances The results of both the FBI and Washington State studies included body disposal data concerning when, where, and how remains were disposed; the distances between the victim’s residence, the abduction site, the murder site, and the body disposal site; and the degree and type of concealment. In the FBI study, remains were disposed of in different scenarios depending upon the motivation of the offender and the age of the victim. These motivations had specific operational definitions. Infant replacement was defined as the abduction of a child with the intent of keeping the child. Emotional motivation included child abuse fatalities, child abuse fatalities resulting in parents claiming abduction (false allegation), revenge, retribution, and rage-based crimes. Sexual motivation required physical evidence of a sexual act, including visible trauma, and serology/DNA. Profit motivation included drug, robbery, and extortion cases. Unknown motivation included cases where the motivation was unclear or undetermined. (See Table 8.1). In the neonate category (age 0–1 month), most of the victims were abducted for infant replacement reasons. This type of motivation comprised 79% of the cases. The offenders who were motivated by infant replacement were primarily female abductors. The victims were recovered alive in almost all the cases. The remaining victims in neonate cases were killed for emotional reasons by biological parents. These victims were usually killed in their residences. They were disposed of 1 to 5 miles from their residences in 67% of the cases. The remainder of these victims were disposed of at their residences. In the infant category (age 1–12 months), the victims were killed for emotional reasons in a majority of the cases. The offender was always a family member, usually the biological parents. The victims were typically killed in their residences and primarily disposed of within 5 miles (83%). The remaining victims were disposed of 5 to 10 miles from their residences (17%).

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Table 8.1

Distance Between Victim’s Residence and Body Disposal Site Distance

Age of Child 0–1 month 1–12 months 13–36 months 3–5 years 6–11 years 12–14 years 15–17 years

< 100 yards

< 1 mile

1–5 miles

6–10 miles

11–30 miles

> 30 miles

— — — 58% — — —

— — 56% — 23% 27% 36%

67% 83% — — 18% — 42%

— — 22% 17% — 6% —

— — — 25% 12% 29% 15%

— — — — 16% 15% —

In the toddler category (age 13–36 months), the offender motivation was again primarily emotional. This motivation comprised 90% of the cases. Family members were the primary offenders in 82% of the cases. Disposal of victims’ remains was similar to infants; they were disposed of within 1 mile in 56% of cases, and 22% within 1 to 5 miles. In the preschooler category (age 3–5 years), the motivations were divided among emotion based (54%), sex based (30%), and profit (16%). For all categories, victims were disposed of within 100 yards of the offense site in 58% of the cases, within 5 to 10 miles in 17% of the cases, and 10 to 30 miles in 25% of the cases. In elementary age (6–11 years) victims, sex was the primary motivation, comprising 89% of the cases. Victims were disposed of within 1 mile of the abduction site in 23% of the cases, 1 to 5 miles in 18% of the cases, and over 10 miles away in 28% of the cases, with more than half of these over 30 miles away. For emotion-based cases, victims were disposed of within 100 yards in 73% of the cases, within 1 to 5 miles in 9% of the cases, and 10 to 30 miles in 18% of the cases. In middle school age (12–14 years) victims, sex was the primary motivation (79%). Victims were disposed of within 1 mile in 27% of the cases, 5 to 10 miles in 6%, 10 to 30 miles in 29%, and over 30 miles in 15% of the cases. In high school age (15–17 years) victims, motivation for offenders was divided between sex (52%), emotion based (25%), and profit (23%). The increase in emotion-based crimes for this age is attributed to boyfriend, ex-boyfriend relationships. Profit motivation primarily involved males. For victims of sex-motivated crimes, remains were disposed of at or within 1 mile of the abduction site 36% of the time, 1 to 5 miles in 42%, and over 10 miles in 15% of cases. In the Washington State study, all the cases were homicides. The study revealed that in the disposal scenarios of victims, 52% were concealed to prevent discovery. Another 39% were deposited in a manner suggesting the offender was unconcerned as to discovery, and 9% were openly placed. Offenders in this study deliberately selected disposal sites in 49% of the cases, randomly chose sites in 37% of the cases, and were forced to dispose of the victim by circumstances in 14% of the cases. In 63% of the cases, the body recovery site was greater than 1.5 miles from the victim’s home (see Table 8.1). As a general rule, the younger the victim, the closer to the victim’s home the remains were found. This study also divided the stages of the crime into the initial contact site, the murder site and the disposal site (see Table 8.2). The distances from initial contact site to the murder site, were from 0 to 199 feet in 31% of the cases, 200 feet to .25 mile in 16% of

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Table 8.2

Distances Between Sites

Last known location Initial contact site Murder site

Initial Contact Site

Murder Site

Body Recovery Site

< 200 feet (65%) — —

> .25 mile (55%) > .25 mile (54%) —

> .25 mile (66%) > .25 mile (63%) < 200 feet (72%)

the cases, .25 mile to 1.50 miles in 10% of the cases, 1.50 miles to 12 miles in 25% of the cases, and greater than 12 miles in 18% of the cases. The distances from murder site to body recovery site were 0 to 199 feet in 72% of the cases, 200 feet to .25 mile in 6% of the cases, .25 mile to 1.50 miles in 4% of the cases, 1.50 miles to 12 miles in 10% of the cases, and greater than 12 miles in 8% of the cases. In classifying the types of geographic areas in which initial contact took place, 51% were urban areas, 33% were suburban areas, and 16% were rural areas. The person who discovered the body was found to be a passer-by in 58.4% of the cases, the police in 23.1% of the cases, search party in 6.5% of the cases, relative or acquaintance of victim in 4.5% of the cases, the offender in 2.7% of the cases, witness to the death in 1.8%, and fire department/rescue personnel in 1.6% of the cases. The FBI study revealed that several factors accounted for different disposal scenarios. These factors included the sex of the offender, sex of the victim, and the motivation for the abduction. Male offenders were the overwhelming perpetrators in the age groups from preschool through high school. Females were the primary victims of male offenders in 74% of all of the cases. Sex was the primary motivation for the abduction in 60% of all of the cases in the study, with emotion-based motives comprising 27%. Male offenders abducted their victims from inside the victim’s residence in 31% of the cases, and from public streets inside and outside the victim’s neighborhood in 37% of the cases. The male offenders were acquaintances of the victim in 41% and strangers in 40% of the cases. Male offenders lived at or within 1 mile of the abduction site in 46% of the cases. Victims were disposed of at the abduction site in 32% of the cases, transported less than a mile in 17% of the cases, 1 to 5 miles in 19% of the cases, 5 to 10 miles in 6% of the cases, and surprisingly, over 10 miles in 26% of the cases. The Washington State study revealed that in most of the abduction/homicide cases, the body was concealed to prevent discovery. In a majority of cases, disposal was located greater than 1.5 miles from the victim’s residence. The Washington State study also identified the importance of identifying the initial contact site, the murder site, and the disposal site. The murder site was the least found of the three sites identified in the study. Obviously, the murder site is very important in linking physical evidence between the offender and the victim. In this study, 75% of the murder sites are within 200 feet of the disposal sites. Search strategies should incorporate this fact, and it should be standard procedure to search in at least a 200-foot diameter around any child homicide crime scene. The discovery of the initial contact site is equally important. In this study, the case clearance rate dropped 40 percentage points below the average clearance rate if the initial contact site was not located. If the initial contact site was located, the clearance rate rose to 13 percentage points above the average clearance rate. In 80% of the cases in this study, the initial contact site was within .25 mile of the victim’s last known location.

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Figure 8.1 Diagrammatic summary of the major factors influencing taphonomic changes and decomposition rates in the remains of childhood victims of abduction and murder.

Issues of Decomposition and Child-Sized Remains There have been very few studies conducted regarding environmental and taphonomic effects on child-sized remains during decomposition. Based on the findings of the few existing studies that have employed child-sized decomposition models and on reports from actual cases, child-sized remains appear to be “returned to nature” much more quickly than those of adults (Crist, 1997). A variety of influences, including environmental, behavioral and zoological factors, contribute to the rate of childhood taphonomy (Figure 8.1). In warm weather total skeletonization has been observed to occur in as little as 6 days (Morton et al., 1999). The quick reduction to skeletal remains can present serious recognition problems for untrained searchers who are looking for a “whole” child. The differences in decomposition changes in child-sized remains vs. adult remains are quite logical. Child remains undergo decomposition processes in a shorter time interval than adult remains due, in part, to smaller size and greater surface-to-volume ratios. The smaller body size and lower weight of child remains contribute to the shorter interval. There is less flesh for arthropods to consume, and so the remains are reduced to skeletal elements more quickly. Size is also a factor in scavenging by feral animals. In larger remains, scavenging canids are forced to pull and tear at limbs and other extremities to remove them. Smaller size allows for easier disarticulation and removal of an entire corpse. Greater surface-to-volume ratios characteristic of child remains facilitate more rapid environmental degradation and arthropod consumption.

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This quick return to nature when coupled with the small size of child victims and the disposal methods employed by offenders help contribute to the poor success of organized searches.

Animal (Swine) Model Research In 1998, members of the FBI’s National Center for the Analysis of Violent Crime (NCAVC) conducted a research project looking at the decomposition changes of child-sized remains. During the time period from late May 1998 through July 1998, remains of small pigs (less than 30 lb.) were deposited in a wooded area adjacent to a dirt road in a suburban area of Virginia. The sites were located between 40 and 80 feet from the shoulder of the road. The pigs were placed in a variety of scenarios, including surface deposit, no covering; surface deposit, covered with tree branches and deadfall; surface deposit, enclosed in a rolled up carpet; shallow burial (less than 1 foot); and suspended by rope from a tree approximately 2.5 feet above the ground. All the pigs were deposited in late May, and were environmentally exposed and monitored for a total of 75 days. The pigs were secured with wire mesh for the first 8 days, which was then removed. Environmental temperatures averaged from the 60s (lows), to 80s and 90s°F (high) for the entire 75-day time period. The use of pigs as substitutes for human remains is an accepted standard in decomposition and taphonomic research, and has become routine in anthropological and entomological research. Although not a perfect substitute for human remains, pigs are an accepted comparative model. The decomposition process for pigs approximates decomposition for humans, and takes place in similar time frames (Payne, 1965; Haskell, 1989). The unique microenvironment created by the introduction of a pig carcass or human body into an existing habitat results in the attraction of a variety of scavengers and insects. Creation of a temporary food source, shelter, nursery, and the production of decomposition by-products alter normal flora and faunal communities, and produce observable and detectable changes. A broad, multidisciplinary approach was employed during the collection and subsequent analysis of study data. The five sites included in this study were observed regularly to record various decomposition stages and taphonomic changes. Observations included stages of the decomposition process, activity of necrophagous arthropods, and the extent of remains scavenging and scattering by birds and mammals. Remains were monitored weekly to chart disarticulation and skeletal disposal. Site surveillance was conducted prior to approach to minimize impact on scavenger activity. Scavenging effects were photographed and examined in an effort to identify species of vertebrate predators. At the conclusion of the study, an archeological approach was used to recover the remains. Loose vegetation was raked and removed, and various skeletal components were located and charted. Remains from each site were collected, sorted and tabulated to identify missing skeletal components. Carrion predators common to northern Virginia include the coyote (Canis latrans), stray domestic dogs (Canis familiaris), the red fox (Vulpes vulpes), both turkey (Cathartes aura) and black (Coragyps atratus) vultures, and a variety of scavenging rodents, including fox squirrels (Sciurus niger), gray squirrels (Sciurus carolinensis), deer mice (Peromyscus maniculatus), and voles (Microtus pennsylvanicus).

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Figure 8.2 Photographic depiction of the surface deposit study site (site #1) characterized as a mixed eastern deciduous forest with prominent leaf and plant litter. The study animal (swine) was placed directly on top of the existing leaf fall.

Field Research Data Five sites will be discussed individually and the observations will be described chronologically. Site #1 (Figure 8.2) This site was a surface deposit. The area was a mixed deciduous and evergreen forest. There was significant leaf and plant litter on the surface. The pig was deposited directly on the top of the leave litter. On the first day, adult necrophagous flies arrived within minutes and began laying eggs. Over the next 6 days the insect infestation continued unabated increasing in both species diversity and richness. By day 7, fly larvae (maggots) had consumed approximately 60% of the soft tissue. By day 12, the remains were totally skeletonized; the only tissues remaining were small bits of mummified integument. After 75 days, the skeletal elements were scattered in a small area approximately 14 feet long and 11 feet wide. There was very little carnivore/scavenger activity. A detailed search resulted in the recovery of all the skeletal elements from this site. Site #2 (Figure 8.3) This site contained a small pig placed within a rolled-up carpet, with the ends open. On the first day, necrophagous flies were very active and were laying eggs. The open carpet did little to inhibit access. The shelter produced by the carpet increased egg laying activity by adult flies, and consequently produced many more fly larvae (maggots). The increase in the numbers of maggots allowed for quicker consumption of the soft tissues. By day 6, fly larvae had invaded the entire carcass. After 12 days, the remains were completely skeletonized, and the maggots had migrated from the remains into the surrounding substrate to complete their development. After 75 days, approximately 60% of the skeletal elements

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Figure 8.3 Photographic depiction of the rolled-carpet study site (site #2). The study animal (swine) was placed within the rolled residential carpet, which was then deposited on the ground surface.

were recovered, found mostly within the carpet. The skull, mandible, a rib, and several vertebrate were found within 6 feet of the carpet. These elements were removed from the carpet by scavengers, primarily turkey vultures. Site #3 (Figure 8.4) This site was a shallow burial. A small pig was placed in a shallow depression, approximately 2 feet deep, and covered with dirt. On the first day, there was insect activity but the burial prevented adult fly access. After 6 days, however, there was significant adult and larval insect infestation. After 12 days, the pig had been removed from the shallow grave by vertebrate scavengers and dragged 46 feet away. The head was missing and there were obvious signs of canid scavenging. After another week, the carcass of the pig was devoid of soft tissue and had been disarticulated. An area of soil discoloration and some small pieces of tissue, revealed where the pig had lain during early decomposition prior to being disarticulated by scavenging canids. The skeletal elements of the pig were scattered around the site. Several skeletal elements (ribs and vertebrate) were dispersed in an area approximately 15 feet wide and 9 feet long. Numerous skeletal elements were missing, primarily the skull and long bones. After 75 days, the scattering was distributed over a wider area. The furthest element recovered was located 89 feet from the burial site. Site #4 (Figure 8.5) This site had a hanging pig. The pig was secured by a rope and suspended approximately 2.5 feet above the ground. On the first day, carrion insect activity was observed almost immediately, with adult female flies beginning to oviposit within minutes. After 6 days, there was heavy insect infestation. Fly larvae (maggots) had eaten most of the soft tissue, particularly within the abdominal cavity. Fly larval infestation became so heavy that maggots were seen falling out of the pig to the ground below. These maggots were unable

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Figure 8.4 Photographic depiction of the shallow burial study site (site #3). The pig carcass

was interred in a shallow depression, approximately 2 feet deep, and covered with dirt from the surrounding environment. This site displayed the most prominent vertebrate scavenger activity of all of the carrion study sites.

Figure 8.5 Photographic depiction of the suspended carrion study site (site #4). At this location a pig carcass was suspended by a small diameter rope at an approximate height of 2 feet above ground level. It should be noted that the study animal was deceased prior suspension.

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Figure 8.6 Photographic depiction of the carrion study site (site #5) containing a pig carcass covered with deadfall vegetation and branches. Dead vegetation from the surrounding deciduous forest habitat was utilized to completely cover the study carcass.

to re-infest the suspended carcass and thus a complex community of carrion insects developed in the fluid stained soil beneath the hanging carrion. After 12 days, dry, windy environmental conditions had mummified the skin, creating a hard protective shell. No soft tissue remained. Several teeth had dislodged, as well as one rib, which was on the ground beneath the carcass. After 75 days, the carcass was still intact, but several more ribs had dislodged. The carcass appeared to remain intact for such a long period because the suspension of the carcass precluded vertebrate scavenging, limited insect colonization, and allowed the wind to rapidly desiccate the integument. This mummification process formed a protective leathery shell, securing the majority of the skeletal elements within the carcass. Site #5 (Figure 8.6) This site contained the pig covered with deadfall and branches. The deadfall completely covered the carcass. On the first day, there was pronounced insect activity. Adult flies were observed to gain carrion access through gaps in the covering. Fly oviposition and maggot population development, however, were less intense than that observed on more exposed carrion. After 6 days, the carcass of the pig had been dragged out of the deadfall and was lying approximately 3 feet from the original deposition site. After 12 days, almost all of the soft tissue had been consumed. The skeletal elements were still in close proximity, the furthest less than 13 feet. After 75 days, the skeletal elements were still in the immediate area of the deadfall, the furthest element being located about 15 feet away. Almost all of the skeletal elements were recovered at this site. Observations conducted at the previously described study sites revealed that small pigs decompose within a short time interval. Each of the pigs, other than the hanging pig, was reduced to skeletal components (almost devoid of soft tissues) within 12 days. Skeletal components were most often recovered in the near vicinity of the original disposal site,

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Table 8.3 Animal (Swine) Model Research: Remains Recovered

Cranium Mandible Pelvis Scapula Humerus Radius Ulna Femur Fibula Patella Cervical vertebrae Thoracic vertebrae Lumbar vertebrae Sacrum Caudal Ribs Carpals Metacarpals Tarsals Metatarsals Phalanges

Pig #1

Pig #2

Pig #3

Pig #5

X X X X X X X X X X X X X X X X X X X X X

X X * 0 X X X * * 0 * * * * * * 0 * * * *

0 X * X 0 * 0 * * 0 0 * * 0 0 * 0 * 0 * 0

X X * X * X X X X * * * * * * * * * * * *

Note: X = all found, * = part found, 0 = none found.

with the majority located within 15 feet (Table 8.3). Disarticulated remains were scattered, and in some cases, difficult to see due to similarities in their appearance and the color of the environmental background on which they were located. The small size of many skeletal elements required careful and structured procedures to ensure recognition and recovery. Unexpectedly, remains interred in the shallow burial were subjected to greater vertebrate scattering than those that decomposed on the surface. In this study, the vertebrates involved in scavenging were mostly canids (coyotes and fox) and turkey vultures. Scavenging activities by small rodents was limited to skeletal element gnawing with little actual remains movement noted. Coyotes are generally predaceous, but will readily participate in carrion scavenging activities. They hunt both singularly and in cooperation with other coyotes, are largely nocturnal, but are also active at dusk and dawn. Coyote diets include carrion, birds, rodents, and larger animals. Red foxes are also efficient predators who participate in carrion scavenging activities, are solitary hunters, and are primarily nocturnal. Common food items include carrion, mice, voles, rabbits, bird’s eggs, large insects, and fruit. Turkey vultures are large raptors whose primary food source is carrion. They soar on wind currents and thermals and are able to detect dead animals at great distances. Squirrels, mice, and voles are primarily herbivores, but will scavenge bone for calcium. There are several explanations for the differences observed in the taphonomic process characteristic of each of the pig carcasses. At site #1, the pig was laying on the surface. This allowed easy access for a wide variety of necrophagous insects. The adult insects and their offspring were able to rapidly colonize and consume the carcass. This carcass had the least amount of scavenging activity by larger predators, and the least scattering of skeletal elements. At site #2, the pig carcass was contained within the rolled-up carpet. The open,

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but narrow carpet ends allow easy access for colonizing insects, which again devoured carcass soft tissues rapidly. However, there was very little vertebrate scavenging observed at this site, as the carpet presented a formidable barrier to both birds and canids. Again, skeletal scattering was almost non-existent at this site. Site #3 was the shallow burial. There were noticeable increases in vertebrate activity and remains scavenging at this site. Research has shown that burial of bodies retards the decomposition process. Burial slows down bacterial putrefaction via cooler, more uniform temperatures and reduced oxygen availability. Burial also provides a soil layer, which prevents easy carrion detection and access by insects and, with sufficient depth, acts as a barrier to larger scavengers. The carcass at site #3 was buried in a shallow grave that suppressed insect colonization, thus preserving the food source for larger scavengers. As a result, the carcass was dug out of the burial site, carried a greater distance, disarticulated more completely, and subsequently scattered to a greater extent than those at other sites. There was significant evidence (hair and scat) of scavenging by canids. Vultures also fed upon the remains after the carcass was disinterred. This was evidenced by the presence of beak injuries in the carrion and by fecal deposits and feathers in close proximity. This site had the most scavenging activity and the fewest number of skeletal elements recovered. Site #4 was the pig carcass that was suspended above the ground. This carcass had no evidence of bird or mammal scavenging activity. There was insect activity; however, the lack of access prevented re-infestation by maggots once they fell to the ground. The carcass exhibited drying by the wind. Mummification progressed until the skin became very hard and shell-like. This hardened skin allowed most of the skeletal components to remain in place. In the absence of insect infestation and vertebrate scavenging, less destructive decomposition processes (mummification) prevail. The last site was the deadfall covered carcass. This site allowed insect infestation, and the scavengers eventually dragged the carcass out of the deadfall. At this site, the scattering of skeletal elements was localized in a small area, and most of the skeletal elements were recovered. The deadfall covering resulted in both a moderation of insect infestation and vertebrate scavenging, perhaps indicating a more pronounced competition between vertebrate and invertebrate consumers. The different patterns of decomposition and scattering exhibited at the five sites were based primarily on the physical and climatic conditions to which the remains were exposed and the differential impacts of vertebrate and invertebrate activity. Each site was characterized by different factors that dictated which populations of consumers had the competitive edge in carrion exploitation. Competition exhibited between vertebrates and invertebrates for a highly prized food source, the length of time the food source was available, and prevailing climatic conditions, all contribute to differing rates of decomposition and scattering of remains by scavengers. An understanding of these influences is crucial to the successful detection and recovery of child-sized remains.

Child Abduction Case Histories and Disposal Scenarios Case Study #1 This case is presented because the offender transported the victim over 30 miles away from her residence and buried her in a remote area. The victim was a 6-year-old female, and the offender in this case was the victim’s biological father.

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This case first came to the attention of law enforcement after the father and stepmother reported the victim missing after she went out to play one morning. The police organized a large-scale search effort, continually expanding the boundaries to include numerous bodies of water. At one point, the search effort involved hundreds of police and volunteers. Police became suspicious of the parents when they learned the father had been previously investigated by child protective services for being physically abusive to his daughter on at least three occasions. He had temporary custody of his daughter at the time of the homicide. Case investigators were able to persuade the stepmother to cooperate during questioning. She eventually provided the details of the murder to the police. Additionally, she led police to the burial site. Once the body was discovered, the father confessed. The evening before the victim was reported missing, the father stated he became angry with his daughter and lost his temper. He repeatedly hit and threw the victim against a wall, killing her. After she was killed, he wrapped her in a blanket, and attempted to dispose of the body. He drove to several locations, even visiting a friend with the body of the victim lying in the back seat next to the father’s and stepmother’s infant. The offender finally drove to a recreational area the young victim enjoyed visiting. The father buried her there, in a secluded location. The facts in this case relate directly to the abduction research conducted by the FBI’s NCAVC. This case was an emotion-based crime. In this age group, female children who are murdered for emotional reasons are disposed 10 to 30 miles from their residences. The victim was buried 30 miles away. The offender also disposed of the victim in an area familiar to him. Ironically, the disposal site was also one of the victim’s favorite places to visit. The burial was unusual, and was used to conceal the victim to prevent discovery of her body. The victim was buried in a deep, clandestine grave, approximately 3 feet deep. The body was in a moderate stage of decomposition with skin slippage, and bloating. There was no insect or scavenging activity because of the depth of the grave (see Table 8.4). Case Study #2 This case is offered because of the unusual disposal scenario. This offender deposited the victim in a river, and the victim was transported several miles downstream before being discovered. The stream had a normal depth of less than 2 feet. The fluvial action of the river was possible because of several days of storms, which raised the water level well beyond normal. An 11-year-old female disappeared while riding her bike from her residence to her aunt’s apartment. The victim had been playing with friends at a nearby playground. The victim left the playground and went to her residence. No one was home, so a neighbor instructed the victim to go to her aunt’s residence. She rode her bicycle toward her aunt’s apartment. The victim was not seen alive again. After several hours, the family reported her missing. A search of the area was organized and the victim’s bicycle was located in the storage area of the aunt’s apartment. The offender lived with the aunt in her residence. He advised that he was at the apartment that afternoon and had seen the victim. According to the offender, the victim sat in his vehicle and he talked with her for a few minutes. The offender stated he went to work and left the victim. He advised that he last saw the victim riding away on her bicycle.

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Table 8.4

Case Characteristics and Disposal Method Case No.a

Locale Age in years Sex Height (inches) Weight (pounds) Cause of deathc Postmortem interval Disposal methodd Decomposition typee Month of death b

a b c

d

e

1

2

3

4a

4b

4c

4d

SE 6 F 45 55 BFT 1 wk

MW 11 F 66 140 MS 1 wk

W 7 F 48 38 MS 1 wk

NE 12 M 64 125 LS 1 mo.

NE 16 M 62 110 Unknown N/A

NE 10 F 54 60 Unknown 2 mo.

NE 12 F 60 68 BFT2 N/A

DB

W

DLF

SB, RT

N/A

SB, ES

N/A

P

S, P

P, M

P, M

Unknown

P

Unknown

Nov.

May

Aug.

Oct.

Nov.

Aug.

Aug.

Victims #1–3 had different offenders; #4a–4d had the same offender. All victims from continental United States. NE = northeast, etc. MS = manual strangulation, LS = ligature strangulation, BFT = blunt force trauma, BFT2 = blunt force trauma according to offender version only. S = surface, SB = shallow burial 2 feet, W = water deposit, DLF = body placed in trash bag in dumpster and buried in landfill, RT = rope around neck and attached to tree but not hanging, ES = skeletal elements scattered over 100 yards and many elements missing. P = putrefaction, S = saponification, M = mummification.

The offender related that after leaving the victim, he went to work and was there until the early evening hours. When the offender returned, he participated in the search for the victim. Police questioned the offender and during a subsequent interview, he requested an attorney. The next day, the offender contacted the police and told them he was having visions concerning the victim. The offender voluntarily related that in his visions the victim was wet, cold, and in the immediate area. The search broadened, but the victim was not located. After a week, the victim was discovered by a passerby in a small creek several miles away. The victim was clothed, and had duct tape around her mouth. The autopsy revealed the cause of death to be strangulation, although the victim had some water in her lungs. It is believed that she was strangled until unconsciousness by the offender, who thought she was dead. The victim was then dumped in the stream where she finally died. The location where she was found was .5 mile from the nearest road. A few miles upstream from this location was an area where the offender had spent a great deal of time several years earlier. This site was one of the few spots upstream from the recovery site that was readily accessible by a vehicle. The offender’s residence and vehicle were searched, and some of the victim’s blood was located on items in the back seat of the vehicle. A review of the offender’s action in this case revealed many characteristics common to the two abduction research studies discussed previously. The victim was taken from near her home, by an offender related to her. She was abducted from the site where she was last seen. The offender assaulted her in his vehicle. The offender disposed of the victim in an area with which he was very familiar. He concealed the victim by placing her in the shallow stream. The stream’s usual depth was very shallow, less than 2 feet in the deepest

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portions. The stream meandered, and was not navigable through its length by a floating object, unless the water level was high due to storm activity. The body could only reach the area where it was recovered through fluvial action. The weather conditions consisted of severe thunderstorms during the week the victim was missing. The victim was found on a bank of the stream, in a location where she would have been carried by the action of the stream. The elevated water levels allowed the transport of the victim to the recovery location. The remains were very decomposed and bloated, with evidence of saponification. There was evidence of scavenging by insects, but no evidence of activity by large scavengers (see Table 8.4). Case Study #3 This case involved the abduction of a 7-year-old female, who disappeared on her way home. The offender was acquainted with the victim; his daughter was a friend of the victim. The disposal scenario in this case was unusual in that the offender hid the victim in a garbage bag, which he placed in a dumpster near his residence. The victim left her residence and rode her scooter down the street to water her grandfather’s vegetable garden. She was observed leaving the garden and was last seen heading toward her residence. However, she never returned to her home. She was reported missing within the hour, and a massive search of the neighborhood was undertaken. The majority of the searchers were volunteers, and they combed the immediate area around the residence and the neighborhood. The searchers even opened the dumpsters, and looked in, but never opened the garbage bags themselves. The dumpsters were emptied the next day and transported to the landfill. The operator of the landfill isolated the garbage from the neighborhood from which the child had disappeared and stored it separately. He did this because he felt it might be helpful. A search of the garbage from the dumpsters was eventually conducted, and the victim and her scooter were located in garbage bags. The scooter had been taken apart and placed in separate bags. The offender came to the attention of the police because his daughter and the victim were playmates. A check of his criminal record revealed that he had been previously convicted of a sexual offense. He was home the afternoon the victim disappeared; he had been babysitting his children at his residence. He told police he was home and had fallen asleep. He claimed he woke up when searchers knocked on his door, looking for the victim. He also participated in the search. Once the victim was located, the offender admitted he had lured the victim into his residence, sexually assaulted her, and strangled her. He disposed of her in the dumpster because it was close and convenient. The victim was in an advanced state of decomposition. She was bloated and there was heavy insect infestation. The black plastic garbage bag she was placed in increased the temperatures to which the body was exposed. There was no evidence of scavenger activity. The lack of scavenging can be attributed to the placement of the victim in a dumpster, which was eventually deposited in a landfill. The victim was buried beneath numerous other bags of garbage. The recovery of the victim in this case was due to the initiative taken by the landfill operator who isolated the trash. This allowed for a more comprehensive search of trash taken from the immediate area of the abduction. The fact that the dumpsters in the area

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were searched by volunteers should not preclude a more detailed search of the contents of garbage bags at a later time by law enforcement professionals (see Table 8.4). Case Study #4 This case is offered because it involved a number of victims and disposal scenarios. There were five victims, one of whom was recovered alive. Of the four murdered victims, only two bodies were recovered. Two of the victims were killed in one state and disposed of in a different state. The victim recovered alive was the last victim in this series of abductions. This offender was a serial child abductor/murderer who operated in two separate states. The offender came to the attention of law enforcement after he was arrested for the attempted abduction of a 12-year-old female. His vehicle was seized and his kidnap kit was recovered from the vehicle. Subsequent to his arrest, the offender confessed to the attempted abduction, the abduction and murder of a 12-year-old male and a 12-year-old female. In the fall of early 1990, a 12-year-old male disappeared. He was last seen riding his bicycle in the parking lot of a strip mall adjacent to a major county road. A month later the victim’s body was discovered by deer hunters in a wooded area approximately 200 miles away. The body was recovered on top of the ground, face down, completely nude, with a 7-foot length of clothesline tied around the neck. The other end of the clothesline was tied to a tree 5 feet from the ground, but was not a hanging attempt. The body was found approximately 200 feet from the closest access roadway and no attempt was made to conceal the body. The findings indicated the victim’s arms and legs had been bound with tape but no bindings were found on the body. The tape bindings were recovered from the victim’s clothing. Investigation indicates the victim walked into the crime scene wearing his sneakers. The victim’s eyes and mouth were covered with duct tape, which was still in place when the body was found. The victim’s clothing was found 200 feet away from the body, further into the woods and away from the access road. The clothes included a tee shirt, a pair of jeans, underwear, sneakers, and socks. The tee shirt had been cut off in one piece to allow removal without removing the bindings. The Medical Examiner determined that the cause of death was ligature strangulation from the clothesline found around the victim’s neck. No semen was found at the scene and no evidence of sexual assault was found. The offender admitted that he was working near the strip mall where the victim was last seen. He lured the victim with the promise of money to help move furniture. The offender placed the victim and his bicycle in his van, drove to his apartment, and walked the victim into the residence. The offender attempted a sexual assault but could not perform sexually. At that point, the offender decided to kill the victim. The following morning, the offender drove to an adjacent state to an area he was familiar with from his childhood. The offender told the victim he was going to release him in the woods. He tied the clothesline around the victim’s neck and walked him into the woods. As they were walking, the offender tightened the ligature and the victim fell. He continued pulling the rope until the victim stopped struggling. The offender then tied the rope to a tree and kept pressure on the victim’s neck to insure he would die. He removed the victim’s clothing and cut his shirt off with his knife. The offender reported he removed the clothes to make it appear that a pedophile had killed the victim and to also insure the victim would die of hypothermia if the strangulation did not kill him. The offender removed all of the victim’s clothes and deposited them in a puddle of water, to remove

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any trace evidence. The offender then drove home back to his residence. He later disposed of the victim’s bicycle in a lake; police recovered it. The body had moderate decomposition because of the cool temperatures during the postmortem period. There was also extensive skin drying due to the position of the body. Several years after the previous abduction, a 16-year-old male disappeared from the area of his residence. The victim suffered from a mental disability and his mental age was less than his chronological age. He was small and slightly built and appeared to be approximately 12 years old. He, too, was last seen riding his bicycle along a major county highway. Less than a week later, the victim’s bicycle was found in a wooded area a short distance away. Crime scene investigation by police failed to locate any evidence on the bicycle. The victim’s body has never been found and the offender has denied any involvement in his abduction. Investigation by police after the offender’s arrest determined that offender was in the same general area where the victim was last seen. The next year, a 10-year-old female disappeared from a rural road in a neighboring area. A thorough search was conducted in the area where the victim was last known to be and her left sneaker was recovered along a secondary road. Two months later, the victim’s skeletal remains were found by hunters in a heavily wooded area, approximately 16 miles from the abduction site and a short distance from a major county highway. Examination of the scene determined the victim’s body decomposed on top of the ground and there was no attempt to conceal the body. The victim’s shorts, tee shirt, and right sneaker were recovered in the same general area as the body. The remains were completely skeletonized and had been widely scattered throughout the area by animals. The disposal area was frequented by numerous large scavengers including coyotes, dogs, and foxes. Due to the extensive decomposition involved, the cause or manner of death or sexual assault could not be determined. Two weeks after the previous abduction, a 12-year-old female disappeared from a country road in an adjacent state. Her bicycle was located on the side of the road but the victim’s body has never been recovered. After the offender’s arrest, he advised investigators that during the same time frame, he went for a ride along the same county highway previously mentioned, looking for vulnerable girls to kidnap. He turned off the county highway onto a rural road and he came upon a girl pushing a bicycle, and who was both vulnerable and sexually arousing to him. He pulled alongside the girl and jumped from his van with his knife. She tried to run but he grabbed her, threatened her with the knife, and forced her into the van. He duct-taped her hands and feet and quickly threw her bicycle and packages into the woods. The offender identified an unusual feature of the bicycle that had not been disclosed to the public prior to the confession. The offender advised he drove the victim to a very sparsely populated area. He found a dirt road in an extremely remote area and pulled over. He climbed into the back of the van, removed the victim’s clothes and vaginally raped her. He then forced her out of the van and instructed her to walk up a hill, away from the van. The offender claimed he then struck the victim in the back of the head with a large tree limb, killing her. He said that he buried the victim in a shallow grave, face down, digging the grave with a pick and shovel he had in the van. He then placed her clothes in a plastic bag and left the area. The offender disposed of the clothes in a dumpster, on his way back to his residence. He disposed of the pick and shovel the next morning near his residence.

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Table 8.5 Case #a

Distance from Residence to Various Sites in Case Studies Last Known Location (Verified Sighting)

1 2 3 4a 4b 4c 4d a

< 200 feet < 1 mile < 200 feet > 5 miles < 200 feet > 1 mile < 1 mile

Initial Contact (Verified Sighting)

Murder Site if Known

Body Recovery Site if Known

< 200 feet < 1 mile < 200 feet > 5 miles < 200 feet > 1 mile < 1 mile

< 200 feet > 5 miles < 200 feet < 200 feet Unknown Unknown > 50 miles

> 30 miles > 15 miles > 15 miles N/A < 200 feet > 15 miles N/A

Cases #1–3 had different offenders, #4a–4d had the same offender.

The offender provided investigators with a hand-drawn map indicating where the victim was supposedly buried. As a result of this information, a massive, methodical search was initiated by the police. The search continued throughout the winter in sub-zero temperatures and blizzard conditions. During the search, tons of snow and dirt were moved but the victim’s body was never found. A review of this offender’s crimes reveals that he would use separate murder and disposal locations when committing his crimes (Table 8.5). He was responsible for possibly five victims, one of whom lived. Of the four homicides, only two of the bodies were recovered. Both of these victims were located accidentally by citizens, and not by organized searches by law enforcement personnel. In the case of the fourth victim, the offender provided a map to a location where he supposedly buried the victim. After an exhaustive search, no remains were located. The burial, however, falls outside the offender’s usual pattern of surface disposal. The distance the suspect traveled to dispose of his victims varied greatly. One victim was located 16 miles from the abduction site, and the other 220 miles away, in a different state.

Multidisciplinary Approaches to Search/Recovery Strategies The failure of law enforcement to locate child-sized remains is not because of lack of resources or technology. The biggest issues are twofold: 1. Recognition of the behaviors exhibited by offenders who abduct and murder children and the patterns inherent in their selections of remains’ disposal methods and sites. 2. An understanding of the environmental influences that affect child-sized remains, the subsequent taphonomic changes that occur, and the impact that these have upon remains’ recognition, detection, and recovery. Taphonomic changes in child-sized remains present unique patterns and challenges to agencies and personnel involved in search and recovery operations. Judging from the literature available concerning child abduction/homicide scenarios, it is apparent that most search strategies employed by law enforcement in response to such cases are misdirected. Most law enforcement searches for missing children begin around the victim’s residence,

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and then expand outward, usually terminating less than a mile from the alleged abduction site. Available research, however, suggests that abducted victims are often transported much farther than the traditional search parameters encompass. Disposal methods and scenarios also appear to differ with victim age and gender. These differences appear to be rooted in the motivation for the abduction/homicide, the spontaneity of the offense, and the relationship between the victim and the offender. This frequently translates into considerable distance between the abductions and recovery site. Hanfland et al. (1997) provide an excellent review of the important sites associated with child abduction /homicide cases, and strategies for intensive investigative efforts to locate and process these sites. Because child-sized remains are rapidly recycled through the environment into which they are placed, and because of the lengthy time interval frequently preceding remains discovery, great care must be taken in the processing of child recovery sites. The cryptic and scattered nature of such remains requires a well-organized, pre-planned, team approach to both detection and recovery. A multidisciplinary team of experts including forensic pathologists, anthropologists, entomologists, botanists, soil scientists, geophysicists, serologists, trace evidence experts, canine search personnel, crime scene technicians, and behavioral scientists should be utilized to the fullest extent possible in cases of child abduction. Investigators must remain mindful of the fact that most child abduction/homicide cases are successfully resolved through thorough investigative efforts and the proper collection, preservation, documentation, and analysis of tiny items of trace evidence. Recognition of the role that invertebrate and vertebrate scavengers play in the recycling process, coupled with the ability to recognize and interpret signs of their activities is often crucial to successful detection and recovery. The development of a knowledgeable multidisciplinary team, prior to the onset of a child abduction case, will maximize the appropriate allocation of investigative resources early on in subsequent investigations and enhance the probability of successful case resolution. At the very least, law enforcement agencies should compile lists of qualified local experts who are willing to provide assistance in child abduction cases and establish and maintain continuing liaison with these individuals. Little people leave behind little things and special investigative insights and efforts are required to recognize and recover such evidence.

References Boudreaux, M.C., W.D. Lord, and R.L. Dutra 1999 Child abduction: aged-based analysis of offender, victim, and offense characteristics in 550 cases of alleged child disappearance, Journal of Forensic Sciences, 44(3):539–553. Crist, T. A. J., A. Washburn, H. Park, I. Hood, and M. Hickey 1997 Cranial bone displacement as a taphonomic process in potential child abuse cases. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 319–336. CRC Press, Boca Raton, FL. Finkelhor, D. 1997 The homicides of children and youth: a developmental perspective. In Out of the Darkness: Contemporary Perspectives on Family Violence, edited by G.K. Kantor and J.L. Jasinski, pp. 17–34. Sage Publications, Thousand Oaks, CA. pp. 17–34. Finkelhor, D., G.T. Hoatling, and A.J. Sedlak 1992 The abduction of children by strangers and non-family members, Journal of Interpersonal Violence 7(2):226–243.

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Haglund, W.D. 1991 Applications of Taphonomic Models to Forensic Investigations, Ph.D. dissertation, Department of Anthropology, University of Washington, Seattle. University Microfilms, Ann Arbor, MI. 1997 Dogs and coyotes: Postmortem involvement with human remains, In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 367–379. CRC Press, Boca Raton, FL. Hanfland, K., R. Keppel, and J. Weis 1997 Case Management for Missing Children Homicide Investigation: Executive Summary. Christine O. Gregorie, Attorney General of Washington and United States Department of Justice, Office of Juvenile Justice and Delinquency Prevention, Office of Justice Programs, pp. ii, 5–92. Haskell, N.H. 1989 Calliphoridae of Pig Carrion in Northwest Indiana: A Seasonal Comparative Study. Master’s thesis, Purdue University, West Lafayette, IN. Morton, R.J., W.D. Lord, and M.L. Goff 1999 Taphonomic effects on child sized remains located in surface deposit and shallow burial disposal sites, Proceedings of the American Academy of Forensic Sciences 51st Annual Meeting, American Academy of Forensic Sciences, Colorado Springs, CO. Payne, J.A. 1965 A summer carrion study of the baby pig, Sus scrofa Linnaeus, Ecology 46:592–602. Rodriguez, W.C. 1987 Postmortem Animal Activity: Recognition and Interpretation. Paper presented at the 39th Annual Meeting of the American Academy of Forensic Sciences, San Diego.

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Insects Associated with the Body: Their Use and Analyses GAIL S. ANDERSON VALERIE J. CERVENKA Contents Introduction Blow Fly Eggs Case Study #1 Collection and Handling of Eggs at a Crime Scene Blow Fly Larvae Case Study #2 Case Study #3 Collection of Blow Fly Larvae Blow Fly Pupae Case Study #4 Collection of Blow Fly Pupae Case Study #5 Empty Blow Fly Puparia and Newly Emerged Adult Flies Case Study #6 Collection of Puparia Successional Colonization of the Remains Case Study #7 Collection of Other Insect Evidence Conclusions References

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9

Introduction After death, a body, whether human or animal, goes through many rapid changes, the most noticeable of which is the decomposition of the soft tissue. Decomposition is driven by many factors, but among the most important are bacterial and insect action. Insects can be primarily responsible for the removal of most of the soft tissue. As such, they provide an extremely important ecological role, recycling the biomass of an animal so that it can be re-utilized in the food chain. A human body is a valuable food resource to a large number of insects and becomes attractive to insects immediately after death (Anderson and VanLaerhoven, 1996; Dillon, 1997; Dillon and Anderson, 1995; 1996; Nuorteva, 1997; Smith, 1986). The body changes biologically, physically, and chemically as it decomposes, so the composition of the food resource modifies over time. However, insects are extraordinarily good at exploiting just about all food niches possible, and a changing sequence of insects will be attracted to the remains after death, until there is no more utilizable nourishment left. Insects are, therefore, a very noticeable part of the decomposition process. Insects are not only of ecological importance in decomposition, but are extremely valuable in death investigations. Although used in Europe for nearly 150 years (Haskell et al., 1997; Smith, 1986) it is only in the last 30 years that insects have become commonly used in death investigations in North America (Catts and Haskell, 1990). Now, in most regions, the entomologist has become an accepted part of the death investigation team. Insect evidence is used to estimate time of death, as well as drug use before death, position and presence of wounds, and whether the body has been disturbed or moved since death (See Anderson, 1999a; Catts and Goff, 1992; Haskell et al., 1997 for reviews.) There are two fundamental ways to use insects to estimate time of death. The first method, blow fly developmental rates, is used when the body is relatively fresh, i.e., in the first few hours, days, or weeks after death. The second method relies on the fact that insects colonize remains in a predictable sequence, and is used when the victim has been dead from weeks to months to years in some cases. Blow flies are the large metallic-colored flies seen attracted to meat or food. They belong to the family Calliphoridae, in the order Diptera, or True Flies. They are the first arrivals, laying their eggs on the body very soon after death. Their development from egg to first, second, and third instar, to pupa, and to adult follows a predictable pattern and is most influenced by species and temperature. As the development rates are predictable, an analysis of the oldest insect stage on the body, together with the meteorological conditions and the micro-climatic conditions at the scene, can be used to estimate how long insects have been feeding on the body, and hence how long the victim has been dead. All stages of the blow fly developmental cycle can be used in the death investigation. In the late postmortem interval, species composition of insects present on the body at the time of discovery, with the species composition of those that have already left the remains, can be used to estimate time since death. However, caution must be taken when analyzing insect succession as it is strongly impacted by geographical region, habitat, and season (Anderson and VanLaerhoven, 1996; Dillon, 1997; Dillon and Anderson, 1995, 1996; Hobischak, 1997; Hobischak and Anderson (in press); MacDonell and Anderson, 1997; VanLaerhoven, 1997; VanLaerhoven and Anderson, 1996, 1999). The following briefly reviews how both of these techniques are used, emphasizing the use of each stage of blow fly development, and illustrates their use with a variety of case studies.

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Figure 9.1 Large egg mass on pig (Sus scrofa (L.)) carcass, resulting from several female blow

flies laying eggs. This egg mass was laid in under 5 min, as the carcass had previously been lying on the other side and had been turned over to collect insects from underneath the body. The wound is an exit wound from a .22 pistol. (Photograph taken by G.S. Anderson and S.L. VanLaerhoven. With permission.)

Blow Fly Eggs Blow flies are the first insects to colonize remains, although the species will vary with geographical region and season. Some individuals will obtain a protein meal from the remains in order to develop their ovaries and testes (Erzinclioglu, 1996), but the majority of females are attracted to the body to lay their eggs. When the eggs hatch into first instar (first stage larvae), they are very small and vulnerable. They require a liquid protein meal but are unable to break skin (Smith, 1986). The female, therefore, ensures that she lays her eggs close to a wound site or a natural orifice that provides blood, body fluids, or a mucosal layer upon which it is easy to feed. Therefore, eggs are usually first found around these areas. If the wound is very wet, eggs and early instars may drown, so the female often lays her eggs extremely close to, but not actually in, a wound (Figure 9.1). The eggs are usually laid in large batches, up to 180 eggs at a time (Erzinclioglu, 1996). If one female has laid her eggs, many others become attracted to the same area and lay their eggs at the same site. Therefore, an egg mass may be several square centimeters in size and may contain many thousands of eggs. Eggs hatch after a predictable period of time, dependent on temperature and species, ranging from hours to days (see Table 9.1). As time of death estimations using insect evidence are based on the age of the oldest insects on the body, eggs are only of value in the very early postmortem interval. In the later stages larvae or maggots are more important. Therefore, if the body already has maggots present, eggs are of little value. Blow flies will continue to lay their eggs on a body as long as it remains attractive to them. It is quite possible to find a body with extensive maggot activity from third instar, down through second and first instars, as well as freshly laid eggs; the third instars, then, would be of the most value. In fact, entomologists are usually involved in cases in which the decedent has been dead for 72 h or more. It is after

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Table 9.1 Developmental Time for Two Species of Blow Fly under Varying Temperature Regimes Time for Eggs To Hatch (h) Temp. (°C)

Phaenicia (=Lucilia) sericata

Phormia regina

15.0 17.8 20.6 23.4 26.1 28.9 31.7 34.5 37.3 40.0 42.8

42.37 29.42 20.89 15.78 12.63 10.25 8.82 8.10 8.09 None hatched None hatched

51.97 34.42 24.14 18.10 14.32 11.42 9.51 8.55 8.13 8.70 None hatched

Adapted from:

Melvin, R., Annals of the Entomological Society of America, 27:406–410, 1934.

this time that medical parameters are of less use in estimating postmortem interval (Henssge et al., 1995), and insects may be better. However, as there are a tremendous number of variables involved in using medical parameters to determine time since death (Henssge et al., 1995), we have found that pathologists are calling entomologists into more and more cases of early postmortem interval for a second opinion. Case Study #1 A young girl was found dead in late summer close to a riverbank in an urban area in western Canada. She was naked and face down. There were no wounds. The pathologist called to the scene called the entomologist (GSA). The victim had been found a few hours earlier, and had been rolled onto her back when examined. The only insect evidence on the remains consisted of unhatched insect eggs in the corners of the eyes and in one nostril. Half the eggs were preserved immediately for later court purposes, to prove that the exhibits had contained only eggs when collected. The remaining eggs were placed on a piece of fresh beef liver in a gallon glass jar and observed every hour until the majority had hatched. The eggs were received at 1030 h and the very first larva began to hatch at 1320 h later that day. Hatching in larger numbers began at 1750 h. The larvae were then reared through to adulthood in the forensic entomology lab at Simon Fraser University and identified as Calliphora vicina (Robineau-Desvoidy). The duration of insect development stages decreases in a linear manner with increasing temperature (Chapman, 1980). Once maggots reach the third instar, large numbers together can generate heat and raise the body temperature considerably (Anderson and VanLaerhoven, 1996; Catts and Haskell, 1990; Dillon, 1997; Dillon and Anderson, 1995, 1996; Early and Goff, 1986; Greenberg, 1991). However, at the egg and early instar stages, development rates are entirely dependent on the ambient temperatures. Temperature data are available through Environment Canada throughout Canada, but hourly data could be obtained from only two Environment Canada weather stations in the area, both several kilometers from the death scene. On bright sunny days, there could be a great deal of variation between weather stations several kilometers from each other; however, the days

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including and preceding the discovery were overcast, which flattens out temperature variation. Thus, both stations would probably differ little from the crime scene temperatures (Webster, 1999). The mean temperature for the preceding 2 days was 17.4/17.9°C depending on which weather station was used. Calliphora vicina takes a minimum of 41.4 h to hatch at 15.8°C (Anderson, 2000); however, the scene temperature was warmer and fluctuated. Temperatures were converted to a thermal measure, accumulated degree hours (ADH), to allow for the warmer conditions. ADH were calculated for C. vicina by multiplying the developmental duration (in hours) for the time to hatch, by the rearing temperature. C. vicina would require a minimum of 654.12 ADH for eggs to hatch. The date and time of oviposition or egg laying are calculated by a simple reverse summation process. Table 9.2 shows the meteorological data from both Environment Canada Weather Stations and the summation of ADH. The majority of larvae began to hatch at 1750 h on the day of collection (25th). As can be seen from Table 9.2, the weather stations indicated very similar temperatures and 654.12 ADH were accumulated by 0800 to 0900 h the previous day, whichever weather station is used. This means that at the temperatures the insects were exposed to, in order to hatch by 1750 h on the date of discovery, the eggs must have been laid by 0800 to 0900 h the previous day. Most blow flies do not oviposit at night. Although one study (Greenberg, 1990) indicated that some blow fly species will oviposit in small numbers on rat carcasses exposed at night near sodium vapor lamps in Chicago, it has never been observed in British Columbia (Anderson, unpublished data) nor was it observed in extensive studies in Indiana (Haskell et al., 1997). In fact, in a case in Manitoba, disemboweled and bloody bear cubs, shot at night at a garbage dump in the vicinity of large numbers of blow flies, were not colonized until the following morning (Anderson, 1999b). Therefore, the insect evidence indicated that the victim could have been killed any time during the evening of the 23rd or the night of 23/24th. The decedent could not have died during the day of the 23rd; otherwise, the eggs would already have hatched. Therefore, death occurred before 0800 to 0900 h the day prior to discovery and probably occurred the previous night. During the trial the defendant changed his plea and admitted to killing the victim in the night of 23/24th. Collection and Handling of Eggs at a Crime Scene Eggs should be carefully collected and observed in relatively fresh cases, in which no, or very little, maggot activity is present. 1. Look for egg masses in, or close to, wounds and natural orifices (e.g., inside nostrils and in and under eyelids). Eggs are usually laid in a mass, but more isolated eggs in eyelashes may look like insignificant cream-colored specks. Note position of egg masses. 2. Collect from each mass separately and keep each exhibit separate as site of oviposition may be of value later. 3. Collect using forceps and break a small piece of the egg mass away. The eggs appear glued together so breaking some off the main mass feels a bit like breaking a piece from a cookie. The forceps will invariably break some of the eggs but as such large numbers are usually collected, this is not a problem. The exhibit should be approximately a quarter the size of a dime (3 to 4 mm2). Do not collect from the very edge of the mass as eggs on the edge could well be desiccated and may not survive.

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Table 9.2

a

Temperature Records and Accumulated Degree Hours (ADH) in Case Study 1

Time

Temperature Weather Station 1 (°C)

Temperature Weather Station 2 (°C)

ADH Weather Station 1

ADH Weather Station 2

0700 0800 0900 1000 1100 1200 1300 1400 1500 1600 1700 1800 1900 2000 2100 2200 2300 0000 0100 0200 0300 0400 0500 0600 0700 0800 0900 1000 1100 1200 1300 1400 1500 1600 1700 1800

14 16 18 19 20 21 20 20 20 20 19 18 18 17 17 17 17 17 17 17 16 15 14 14 15 15 17 18 18 26a 24 24 24 24 24 24

15 16 17 18 18 17 18 18 18 18 18 18 18 17 17 17 17 17 17 17 17 17 16 16 17 16 17 17 18 26a 24 24 24 24 24 24

674 660 644 626 607 587 566 546 526 506 486 467 449 431 414 397 380 363 346 329 312 296 281 267 253 238 223 206 188 170 144 120 96 72 48 24

667 652 636 619 601 583 566 548 530 512 494 476 458 440 423 406 389 372 355 338 321 304 287 271 255 238 222 205 188 170 144 120 96 72 48 24

Oviposition began

1st hatch

Over 5% hatched

Temperatures from 1200 h August 25 are the temperatures at which the insects were maintained after collection and do not reflect temperatures from Environment Canada weather stations.

4. Each exhibit should be divided into two. One half should be immediately killed and preserved by placing in a vial with 75% alcohol (ETOH). The rest should be kept alive. 5. Place the live eggs in a vial with a piece of damp paper towel to prevent desiccation. Make a lid with dry paper towels, two layers thick, held in place with an elastic band to allow for air circulation. As soon as possible, a small piece of beef liver should be added.

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Figure 9.2 Small mass of first instar larvae on pig carcass. The mass is centered on a small wound in the skin, which is not visible under the maggots. Arrow indicates discarded chorions or egg shells. (Photograph taken by G.S. Anderson and S.L. VanLaerhoven. With permission.)

6. Place the vial with the live eggs in a protected area, out of direct sunlight. Observe the eggs every 30 to 60 minutes, noting any signs of hatch. Note also when first hatch occurs, then continue to monitor until all have hatched, approximating percentage hatch at each time. 7. Ensure that all vials are labeled with case number, collection site, date, time of collection/preservation, name, and phone number of collecting officer. Deliver to entomologist as soon as possible.

Blow Fly Larvae Blow fly eggs hatch into the first of three separate stages of larvae (maggot). The first stage, or first instar, is a very tiny animal, about 1 to 2 mm in length. Figure 9.2 shows a mass of first instars around a small wound site. The cast chorions or egg shells can also be seen. The first instar feeds for a period of time, then molts into a second instar, which again feeds, then molts into a third instar. At each of these molts, the insect sheds its outer layer, as well as its internal cephalopharyngeal skeleton or mouthparts, and the lining of its tracheal system. Therefore, each new stage has a new set of spiracular slits and a new set of mouthparts. It is the mouthparts that contain the most diagnostic features for identification. During the third instar, the maggots may form large masses which can greatly increase the temperature of the body (Anderson and VanLaerhoven, 1996; Catts and Haskell, 1990; Deonier, 1940; Dillon and Anderson, 1995, 1996; Early and Goff, 1986; Greenberg, 1991; Haskell et al., 1997; Payne, 1965; Shean et al., 1993). During these feeding stages a bright red or brown crop or food storage organ is clearly visible. After a period of time in the third instar, the maggots enter a prepupal or wandering stage, leaving the body and searching for a safe, protected area in which to pupate. They will frequently burrow into soil, clothing, hair, or carpet. If the remains are on a hard floor, linoleum or

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Table 9.3 Actual Temperatures Recorded at Environment Canada Weather Station and Scene Temperatures Predicted Using Regression Analysis, Case Study 2 Date

Environment Canada Weather Station (°C)

Predicted Scene Temperatures (°C)

13th 14th 15th 16th 17th

17.5 18.0 17.8 18.3 21.8

21.6 22.2 22.0 22.5 26.4

Victim last seen alive

Victim found in morning

concrete, for example, the larvae may travel great distances to find a suitable area, and may be found underneath boxes, flowerpots, etc. In extremely wet conditions, they have even been observed to climb the trunks of trees (Haskell et al., 1997). Some species such as Protophormia terraenovae (Robineau-Desvoidy) may stay close and pupate on the body (Erzinclioglu, 1996), but this is rare. Toward the end of this prepupal stage the maggots contract and broaden and become opaque. The time that the insect spends in each stage is dependent on temperature and species. When large numbers of larvae are present on remains, large quantities of flesh may be consumed. Great care must be taken to determine whether any of the insects have entered the pupal stage. Failure to locate pupae will result in an underestimate of elapsed time since death. Conversely, if a thorough search for pupae is made, and none are found, then it can be safely concluded that the larvae are the oldest insects on the remains. Case Study #2 Human remains with severe head trauma were found in a rural area of central Canada in summer. The head was colonized by larval blow flies. The victim was last seen alive on the 13th and was found on the 17th of the month. The remains were refrigerated overnight and the insects were sampled the following morning. The majority of insects collected from the remains were Lucilia illustris (Meigen) and the oldest specimens were in the third instar. Weather records from Environment Canada indicated that the mean temperature for the area for the previous few days was between 17.5 and 21.8°C. A portable data logger (SmartReader®) was placed at the scene to determine whether the temperature at the scene was in general warmer, cooler, or similar to that recorded at the Environment Canada weather station. The logger recorded temperatures at the scene for 3 weeks and these were compared with data recorded at the Environment Canada weather station for the same time period. The data were compared visually and statistically using a regression analysis, which showed a good correlation between the two sets of data, with an R 2 of 0.69. The regression equation was used to predict the temperature at the scene, based on the temperatures recorded at the Environment Canada weather station. The results confirmed that the mean temperatures at the scene were warmer than those recorded at the Environment Canada weather station (as shown in Table 9.3), with mean temperatures ranging around 21 to 22°C, and rising to 26.4°C on the date of discovery and removal. It is always preferable for a qualified forensic entomologist to attend both the crime scene and the autopsy to collect the insects. However, because Canada is an extremely large country, covering five time zones, this is often not possible. In these cases, identification

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(specialized crime scene police) officers (called Ident Officers) specifically trained in the collection of entomological evidence can be used. Entomologists frequently train police officers in insect collection, and a police training video has been developed for Canada (Royal Canadian Mounted Police “E” Division Training, 1997). The insects in this case were collected at the autopsy by a Royal Canadian Mounted Police (R.C.M.P.) Ident Officer. Half were killed and preserved immediately to stop the clock and the rest kept alive. If they are not killed, they will continue to develop and many more parameters, such as temperature during transit, will have to be taken into account. Moreover, such preserved specimens can be produced in court later if there is any question about their stage or identity. The rest of the specimens are kept alive to be reared to adulthood in the lab for identification. It is much easier to identify an adult fly than it is a maggot. The entomologist (GSA) examined both live and preserved specimens. The majority of the preserved specimens were immature Lucilia illustris in the third instar, with some molting from second to third instar. As the live insects then took a further 6 days to pupate in the lab, it is probable that they were in the early stages of the third instar when collected. L. illustris takes a minimum of 93 h or 3.9 days to reach the third instar at a mean temperature of 21.2°C (Anderson, 2000). This is extremely close to the temperature of the death scene. The remains were refrigerated for 11 h. Refrigeration of up to approximately 200 maggots at a time has been shown to stop development almost immediately (Johl and Anderson, 1996). However, as some maggot masses were present, the temperature in the remains probably will have dropped more slowly, possibly allowing some continued development. Maggot masses increase the temperature of the body, and when in large numbers and well advanced into the third instar, can maintain temperatures as high as 27 to 38°C for several hours within the refrigerator (Haskell et al., 1997). However, temperature does not rise significantly in a maggot mass until the maggots have entered the third instar. The insects in this case had only just entered this stage so it is probable that they did not have a major impact, although they may have increased the temperature of the remains slightly. It would have been far preferable had the body been available for insect collection before refrigeration; however, this was not possible. So, as the insects were at the beginning of the third instar when collected at 0910 h on the 18th, they had either entered this stage just before refrigeration at 2142 h on the 17th, or had continued to develop briefly during refrigeration and entered this stage after 2142 h on the 17th, but before 0910 h on the 18th. The maggots would have begun to cool after they were refrigerated and development would probably have been arrested sometime between being placed in refrigeration and being removed from refrigeration. The oldest insects were a minimum of 93 h old when collected. Counting back from the time of refrigeration and the time of collection, eggs would have been laid between midnight the 13th and noon the following day, the 14th. Blow flies do not usually lay eggs at night in dark, rural areas; therefore, it is probable that the eggs were laid in the early morning of 14th, and that death could have occurred in the previous evening, 13th or in the night of the 13 to 14th. The victim must have been dead by the morning of the 14th. She was last seen alive the previous evening.

Case Study #3 In some cases, blow flies will colonize a person in life. This is called myiasis or the infestation of living vertebrate animals with dipteran larvae which, at least for a certain

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period of time, feed on the host’s dead or living tissue, liquid body substances, or ingested food. This usually occurs in animals, when an injury or presence of excretory material makes the living animal attractive. It is a major problem in the sheep industry, resulting in blow fly strike and causing $100,000s of damage every year (Wall et al., 1992, 1995; Wardhaugh and Morton, 1990). When found in humans it is usually the result of neglect. There have been many reports worldwide of cases of accidental myiasis in humans (Bauch et al., 1984; Carpenter and Chastain, 1992; Deroo et al., 1990; Erzinclioglu and Whitmore, 1983; Fawzy, 1991; Fotedar et al., 1991; Greenberg, 1984; Hall et al., 1986; Kpea and Zywocinski, 1995; Lee and Yong, 1991; Miller et al., 1990; Morsy and Farrag, 1991; Nielsen, 1993; Richard and Gerrish, 1983). In most of these cases, the insects are colonizing a living person, and feeding on the dead organic matter, rather than on living tissue. In fact, this ability to remove dead tissue, cell for cell, while leaving the living tissue intact has been used in medical systems for centuries for debridement of wounds (Baer, 1931; Sherman and Pechter, 1988) and has recently been revisited as a viable option to surgery (King and Flynn, 1991; Kumar and Joshi, 1995; Pechter and Sherman, 1983; Sherman, 1998; Sherman and Pechter, 1988; Sherman et al., 1995, 1996). From a forensic perspective, myiasis may cause confusion. It is generally assumed that the blow flies have colonized shortly after death; so postmortem interval estimation is based on this. For instance, if larvae are determined to be a minimum of 7 days old, then it is usually accepted that the victim has been dead for a minimum of 7 days. However, if the victim was colonized when alive, the insect evidence is indicating time of neglect or injury, rather than time of death (Goff et al., 1991). If the victim subsequently dies prior to discovery, this can result in an error in postmortem interval estimation. In the following case, the victim was found prior to death. A man was found in spring in a major city in western Canada, unconscious with severe head injuries. He was lying down an embankment in partial shade. He was taken to hospital, but died 2 days later from his injuries. A large number of maggots were feeding in the head area, in the wounds, and in the mouth and throat. In fact, at the hospital, the victim appeared to be choking on the large numbers of maggots in his mouth and throat (Dillon, pers. comm.). The mean temperatures for the area ranged between 10.7 and 16.9°C, with highs ranging from 13.6 to 23.4°C. However, as the victim was alive and the insects were feeding in the wound, the temperature to which the maggots were exposed was probably considerably higher. Body temperature is 37°C, so the insects were probably at a temperature between the two. Larval Calliphora vomitoria (L.) and Phaenicia sericata (Meigen) were collected from the wounds. These species normally colonize dead material, but will feed on dead organic matter on a living person. C. vomitoria is normally considered a more rural species, and its presence at this urban site is unusual, although P. sericata is a common urban species (Anderson, 1995). At 29°C, Calliphora vomitoria takes a minimum of 45 h to reach the beginning of the third instar, and at 35°C, it takes a minimum of 42 h to reach the beginning of this stage (Greenberg and Tantawi, 1993). This is probably a reasonable temperature range as the insects would not have been at a temperature as high as body temperature, nor as low as ambient air temperature, but somewhere between. The oldest insects had already entered the 3rd instar, so were older than this, but had not yet reached the prepupal stage, which takes a further 88.8 h at 29°C and a further 44.4 h at 35°C (Greenberg and Tantawi, 1993). Therefore, these insects were probably at least 2 days old and could have been 3.6 or more days old. Phaenicia sericata takes a minimum of 50 h to reach the beginning of the third instar at 29°C, and spends a further 22 h in this stage before entering the prepupal stage

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(Greenberg, 1991). Therefore, insects from this species were probably at least 2 days old and could have been almost 3 days old. It is probable that the victim was injured but not colonized by insects for some days, especially if conscious. It is likely that the insects began to colonize the man when he started to lose consciousness. These species usually colonize dead victims or carrion animals; when found on living victims, they feed on the dead and infected tissue, not on the living tissue. Therefore, the insects would not have colonized until the wound reached a stage where infection and dead organic matter were present. This may have taken a few days. Therefore, the insects probably colonized the victim at least 2 to 3 days before discovery, but the injuries would have occurred some days before this. If the victim in this case had died before discovery, an overestimate of time since death could have been made, without attention to the colonization, wounds, and general scenario. In cases involving myiasis, the forensic entomologist is determining time since injury or neglect, rather than time since death.

Collection of Blow Fly Larvae 1. Blow fly larvae may be found as 1st, 2nd, 3rd or prepupal (post feeding) maggots. The 1st to 3rd stages will be found on the remains. They may be first found close to wound sites and/or natural orifices, but as decomposition progresses, they will be found throughout the body. They may be found in small groups or in large masses. Prepupal larvae will have begun to move away from the body and may be found in the hair, clothing or first 3 to 5 cm of soil. They may wander as far as 50 m from the body (Haskell et al., 1997), but are usually found quite close to the remains, if suitable media are found nearby. 2. There may be several sites of maggot activity on the body. If so, collect and keep separately, as the actual location of the maggots may be important in wound determination later (Rodriguez and Bass, 1987). Note whether maggot masses are present and how large. If possible, carefully take the temperature of each mass. Mass temperature fluctuates diurnally, dropping at night (Anderson and VanLaerhoven, 1996; Dillon, 1997; Dillon and Anderson, 1995, 1996), so a temperature taken during the day will probably give the maximum mass temperature. 3. For each exhibit, approximately 100 to 200 larvae should be collected (insects have a very high mortality rate so more, within limits, is usually better). An ideal vial size is a 250-mL urinalysis vial (Figure 9.3). 4. Collect the larvae with forceps (gently); 50% of each exhibit should be preserved immediately at the scene. The larvae should be placed first in hot water for 5 min then placed in preservative, preferably 75% or higher ethanol. This is the best method because it prevents shrinkage and preserves the larvae very well (Tantawi and Greenberg, 1993). However, if hot water is not available, the larvae should be placed directly in preservative. It is extremely important to preserve the insects in the quickest manner at the scene for later forensic analysis. The vial should be clearly labeled with the time and date of preservation, location of collection, collecting officer’s name, etc. 5. The other half of each exhibit should be kept alive for later rearing to adulthood, for identification purposes. The larvae should be placed in a vial (Figure 9.3) with no more than will cover the base in a single layer. In the past, samples have been sent to entomologists with the vial filled to the brim. Larvae are air breathers, and

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Figure 9.3 Vials used in insect collection. The screw lid (on the right) should be used for insects

in preservative, and the paper towels, held in place with an elastic band, used for live specimens. The paper towels allow the passage of air, but prevent insect escape. A piece of slightly damp paper towel prevents drowning or desiccation and increases surface area. A small piece of raw beef liver should be added as soon as possible. A full label should be placed on every vial. (Photograph taken by G.S. Anderson. With permission.)

when the vial is filled to the top, there is no air, and the majority, if not all, will die. So larvae should be placed in the vial no more than one layer deep. A piece of paper towel can be placed inside to increase the surface area. Care should also be taken to ensure that maggots collected from the remains do not drown. Maggots, particularly those in the third instar in masses, are often very wet from body fluids and the products of their own metabolism (Figure 9.4). When on the remains they are capable of moving away from very wet areas, but in a small vial, they can frequently drown. The paper towel helps prevent the insects from drowning. Conversely, if the larvae are very dry, perhaps from being in the soil, then the towel can be moistened slightly to prevent desiccation. The normal screw lid should be discarded and replaced by two layers of paper towel held in place by an elastic band, as shown in Figure 9.3. As soon as possible, the larvae should be fed a small piece of beef liver. Do not use the plastic lid pierced with holes. The holes will be either too small for adequate air circulation or large enough to allow escape. 6. Prepupal larvae should be treated in the same manner as above, but will be found away from the body. They do not require food, but a piece of damp paper towel will prevent desiccation. 7. See R.C.M.P. “E” Division Training (1997) for further details.

Blow Fly Pupae Once the prepupal maggot has contracted, it will begin to pupate. It does not shed its third instar cuticle as was done in its previous molts, but rather loosens itself from the cuticle, and secretes a number of substances into this cuticle which then hardens and darkens to form the puparium. The pupa is a living insect and the outside pupal case or puparium is the non-living structure that encloses it (Erzinclioglu, 1996; Fraenkel and Bhaskaran, 1973). However, for simplicity’s sake, the puparium, together with the internal, living pupa,

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Figure 9.4 Maggots on human remains at autopsy. Note how wet the maggots are. Caution should be taken when collecting maggots from masses such as this as they may drown if placed directly into a vial. The addition of a small piece of paper towel will prevent this. (Photograph taken by C. Newell, B.C. Coroners Forensic Unit. With permission.)

will be referred to as the pupa, and the puparium as the pupal case, as these are terms usually used at crime scenes. At the onset of pupation, the pupa is a pale cream color which darkens over a few hours (Smith, 1986). Therefore, if a very pale-colored pupa is found, then it has only just begun to pupate and its age can be determined very precisely. If such pupae are found, they should be kept separate from other samples and it should be noted on the label that they were pale in color when collected, as they will continue to darken in transit and will be fully tanned by the time the entomologist receives them. Once pupae are found at a scene, it is very important to continue to search to determine whether any have already reached the adult stage and left empty pupal cases behind. If such evidence is missed, then the determination of elapsed time since death will be an underestimate. Conversely, if a full search is made and only pupae are found, it is safe to assume that the pupae are the oldest stage.

Case Study #4 Human remains were found on large rocks beneath a cliff in western Canada in early summer. Insect evidence was collected from the remains and from the rocks beneath and below the body. Further evidence was collected at the autopsy. The remains were not skeletonized, and were dried in areas that were exposed to the sun. Weather records for the area from Environment Canada indicated that the mean temperature for the previous 3 weeks was 15.2°C, with highs reaching into the twenties on occasion and a low down to 6.5°C. Three species of blow fly were collected from the remains:

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Phormia regina (Meigen), Protophormia terraenovae, and Calliphora vomitoria. However, the vast majority were P. regina. The oldest specimens of P. regina were in the pupal stage, but few pupae were found, indicating that pupation probably had only just begun. This species takes a minimum of 18.4 days to reach the beginning of the pupal stage at 16.1°C or 296 accumulated degree days (ADD) (Anderson, 2000). These would have accumulated if eggs had been laid 20 days earlier. Other species collected were P. terraenovae, which develops at a similar rate to P. regina (Greenberg, 1996; Kamal, 1958) and C. vomitoria, which was in the third instar when collected and was younger. Therefore, the insects indicated that death had occurred 20 or more days prior to discovery. The victim was last seen alive late in the day, 21 days earlier.

Collection of Blow Fly Pupae 1. Search soil under and around body. Also search clothing, hair, and any other debris around scene. Prepupal larvae can migrate great distances, but usually stay within a meter or so of the body. Usually, the majority are found within the area that is gridded and screened. Therefore, no further work is being asked for, only that the investigator keep an eye out for pupae when looking for other evidence in soil as it is screened. 2. Pupae must NOT be put into preservative. They should be placed in a dry vial, with a piece of damp paper towel to cushion the insects and to prevent desiccation. If transport time will be less than 24 h and the vial is at least 250 mL, then the original screw lid can be used. Otherwise, a lid of paper towels should be used instead (Figure 9.3). 3. A small soil sample from close to, but not under, the body should also be placed in a separate container. Usually a coffee or paint can-type container is appropriate and should be half-filled with soil. The lid can then be placed securely on the can as the loose soil, together with the air space above, will allow enough air for any insects in the soil. Do not fill up to the top with soil, or use plastic bags, as this will not allow enough air. 4. See RCMP (Royal Canadian Mounted Police) “E” Division training video for further details. In some cases forensically important insects may themselves be parasitized by other insects. This can also aid in determining time since death.

Case Study #5 The remains of an unidentified female were discovered in the underbrush near a cornfield by a deer hunter in mid-November. The body was clothed and almost entirely decomposed, with the head and feet skeletonized and disarticulated. During the postmortem exam 2 days later, VJC collected insect evidence, including the larvae of Fannia canicularis (L.), F. manicata (Meigen), F. scalaris F., Piophila casei (L.) and Heleomyzidae. Fannia species, also known as latrine flies, occur on bodies in a state of protein fermentation, arriving later in the successional colonization of the body. The timing of their arrival depends on geographic region but is usually about 2 months after death (Dillon, 1997; Dillon and Anderson, 1995, 1996) or more (Smith, 1986), although they can be found on buried bodies much earlier (VanLaerhoven, 1997; VanLaerhoven and Anderson, 1996, 1999). More importantly, however, large numbers of Protophormia terraenovae and Phormia regina (Meigen) puparia were collected, many eclosed, and some containing parasitoid emergence holes. © 2002 by CRC Press LLC

Figure 9.5 Muscidifurax sp. ovipositing egg in fly puparium. (Photograph taken by V.J. Cervenka. With permission).

In this case parasitoid were tiny wasps (Hymenoptera) that lay their eggs in the eggs or pupae of other insects, causing the host insect’s death. The wasps belonged to the family Pteromalidae, which can lay single or multiple eggs. They sting or oviposit in the pupae of muscoid flies, including blow flies (Figure 9.5). The wasp eggs hatch, and the larvae feed on the fly developing within the puparium, or pupal case, killing it. The wasp larva pupates and emerges as an adult, still within the fly puparium. Once emerged, it chews a small, circular hole in the pupal case and climbs out, to repeat the process on another fly. Since the wasps will only oviposit on pupae of a certain age, they can be used to estimate postmortem interval. The wasp waits until the last larval skin has separated from the inside of the fly puperium before it deposits the egg. This generally occurs from 24 to 30 h of pupal age (Fraenkel and Bhaskeran, 1973). One of the Protophormia terraenovae pupae collected from the remains contained a parasitoid, Muscidifurax species. Muscidifurax sp. lay their eggs in puparia that are at least 24 h old (see Figure 9.5). Pupae continue to be attractive to parasitoids until several days later (Moon, pers. comm.). Muscidifurax has a developmental threshold or base temperature of 6°C (Moon, pers. comm.). At a constant temperature of 30.6°C, the wasp needs 344.4 ADD to reach adulthood. In order for Muscidifurax to complete its development, it would have had to lay its egg in the Protophormia terraenovae pupa around August 12, when the fly pupa would have been at least 24 h old. Since P. terraenovae needs 110 ADD to reach the pupal stage (Moon, pers. comm.), adding this amount to the 344 ADD that Muscidifurax needs brings the date of fly egg laying to sometime between August 2 and 3. Assuming flies had access to the remains soon after death, it is likely the woman was dead at the end of July at the earliest or around August 3 at the latest.

Empty Blow Fly Puparia and Newly Emerged Adult Flies When the insect has completed its metamorphosis inside the pupal case, or puparium, the adult fly emerges. The fly breaks open the puparium by expanding and contracting a haemolymph (blood)-filled sac, or ptilinum, on its head (Erzinclioglu, 1996). This ptilinum

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Figure 9.6 Empty puparia and ecdysial caps from Calliphora vicina left behind after the adult fly emerged. (Photograph taken by G.S. Anderson. With permission.)

forces the tip of the puparium, or operculum, off and the new adult emerges from the pupal case. As the operculum is broken off, it splits into two halves or caps (Figure 9.6). The upper cap still has the respiratory horns attached and the lower cap bears the mouthparts (Erzinclioglu, 1996). When the adult fly emerges, it is fairly unrecognizable as the bright, metallic-colored fly that it will become. The wings are crumpled, the legs spindly, and the body dull, dark, and puny. It cannot fly, but can run very fast, often leading investigators to mistake it for some other type of insect, or even a spider (Haskell et al., 1997). This can be likened to a butterfly emerging from the chrysalis, which also has crumpled wings and nothing of the splendor it will later achieve. The newly emerged blow fly crawls out of the soil or clothing in which it has secreted itself during the pupal period and orients itself toward the light, digging upward (Fraenkel, 1935). This positive phototropism is why adult flies often appear to be attracted to light bulbs later in life. The ptilinum is then withdrawn back into the head, and has no further use. During the following few hours, the adult pumps haemolymph into its wings and the rest of the body and the wings expand and the body begins to take on its usual metallic sheen. The fly may appear to be fully expanded and pigmented after a few hours, but it usually takes 24 h for the process to be completed (Erzinclioglu, 1996). Newly emerged flies are of great forensic significance as they indicate that a complete blow fly life cycle has been completed on the body. If they are the first flies to emerge and the majority of other forensic evidence consists of complete pupae, then they can be used to determine the postmortem interval very precisely. However, they are extremely delicate and can be crushed easily. They are also very mobile and prefer to hide, presumably because they are so vulnerable at this stage. If found, such flies should be placed in a dry vial and not preserved. If killed at this stage, even if they have begun to expand their wings and attain color, they immediately crumple and lose all color if placed in preservative. This can make it extremely difficult to identify the species. The appearance of the fly when collected should be clearly noted because once it reaches the entomologist, it will have completed its expansion and will look like any other adult fly of that species. Adult blow flies are normally of little forensic value as there is usually no way to determine whether the fly has emerged from the body or has just arrived to feed, lay eggs, or mate. However,

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when newly emerged, non-expanded specimens are found, they cannot fly and are clearly associated with the remains. It is quite rare to find newly emerged flies, but they leave behind the puparium or empty pupal case as evidence that this life cycle has taken place. These can be identified, but some species have few identifying characteristics. The scanning electron microscope has been used to identify more diagnostic criteria (Liu and Greenberg, 1989), but this is an expensive technique that is rarely available. Empty pupal cases are dark and fragile and are usually buried in a few centimeters of soil or hidden in the clothing seams, making them difficult to locate. They have also been confused with rat droppings (Haskell et al., 1997). In addition to the puparium, the two parts of the ecdysial caps are also left behind. The third instar mouthparts are the main features used to identify the species of the larva, and are left behind after the fly emerges. In most cases, the ecdysial cap is broken away from the rest of the pupal case and, as it is so small and delicate, it is invariably lost. However, in some cases, particularly when the body has been protected or sheltered, such as in a vehicle or closet, the ecdysial caps may also be recovered. They are usually separate from the main puparium, but may, in some cases, remain attached. These are particularly valuable, as the mouthparts can be used to identify the puparium. The presence of empty pupal cases indicates a minimum elapsed time since death. However, as the pupal case is made of chitin, it is very durable, and although an empty pupal case is fragile, in that it is easily crushed, in a protected environment it may last an extremely long time. In some cases they have been found in graves 130 to 160 years old (Gilbert and Bass, 1967). This usually occurs only in sheltered situations, as weathering from rain, wind, soil action, etc. usually breaks down the puparia. Most of the time it is possible to tell whether puparia are relatively fresh or have been exposed for a while from the level of deterioration, but it is not possible to tell whether a fly emerged a day, a week, a month, or more before discovery.

Case Study #6 The skeletonized and heavily scavenged remains of a young girl were found in summer in central Canada, in a forested area in complete shade. The victim had last been seen alive 38 days earlier, on June 5. The insect evidence collected included empty pupal cases which were identified as belonging to Phormia regina and Protophormia terraenovae, as well as pupae of P. regina and P. terraenovae, larval Hydrotaea dentipes and H. houghii (Diptera: Muscidae), larval Psychodidae, larval and adult Histeridae (Hister depurator; Coleoptera), larval Staphylinini (Coleoptera: Staphylinidae), larval Hydrophilidae (Coleoptera), and adult Geotrupes semiopacus (Coleoptera: Geotrupidae). The empty pupal cases of Phormia regina and Protophorma terraenovae indicated that both species had completed an entire life cycle of egg to adult on the remains. The mean temperature for the previous 38 days recorded from the nearest Environment Canada weather station was 15.7 ± 3.8°C. Other Environment Canada weather stations in the vicinity showed means of 15.2°C and 15.3°C for this time period, indicating that the overall temperatures in the area were similar. However, the remains were found in a forested region and were shaded so the conditions there may have been somewhat cooler. Therefore, a portable SmartReader® data logger was placed at the scene which recorded the temperature every 30 minutes for 6 wks. These data were then compared statistically using a regression analysis, with data recorded for the same time period by Environment Canada. The cor-

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Table 9.4 Comparison of Regression Analyses for Four Weather Stations in the Vicinity of the Crime Scene, Case Study 6 Weather Station

R2

1 2 3 4

0.84 0.82 0.91 0.90

Significance

Regression Equation (Scene Temperature =)

Predicted Scene Mean Temperature (°C)

1.65–18 4.44–17 2.61–23 3.11–22

Station 1 temp. ¥ 1.060172 – 1.97833 Station 2 temp. ¥ 0.974563 + 0.092445 Station 3 temp. ¥ 1.069499 – 1.55617 Station 4 temp. ¥ 0.996069 – 1.508

14.7 15.0 14.8 14.7

relation between the two sets of data was extremely high, with an R 2 of 0.84; the significance of the relationship was 1.65–18, extremely significant. The equation generated by this regression analysis was used to predict the temperature at the death scene, and was found to be a mean of 14.7°C for the 38 days that the victim had been missing, on average 1°C cooler than that at the weather station. Originally, the data used were those from the Environment Canada weather station that was closest to the crime scene and which also had the most similar habitat (station 1). However, defense counsel expressed concern that this station, despite being closest, might not actually be representative of the area. Therefore, the analysis was repeated using data for all four weather stations within a 100 km radius of the scene. Each weather station gave very similar results (Table 9.4). Overall, the temperature at the scene would have been slightly cooler than that at the weather stations, as would be expected in a forested, shaded region. Phormia regina takes a minimum of 29.8 days (716.3 h) and a maximum of 36 days to complete development and emerge as an adult fly at 16.1°C (Anderson, 2000). The scene temperatures were cooler than this so development would have taken longer. Protophormia terraenovae takes 13.9 days to complete development at 23°C and 90.7 days to complete development at 12.5°C (Greenberg, 1991). No published data are available for this species at temperatures close to the death scene, but P. terraenovae has been reported to develop at the same rate as P. regina (Greenberg, 1996; Kamal, 1958) so it can be assumed that it also would have taken 29.8 to 36 days to complete development. As the temperatures at the scene were slightly lower than 16.1°C, the data can be converted to accumulated degree days (ADD) to allow for the cooler temperatures. The use of ADD is based on the assumed linear relationship between temperature and development; however, although the relationship is linear over optimum temperature ranges and within small temperature ranges, it becomes more sigmoid at extremes of temperature. Therefore, ADD should only be used for situations in which developmental data are available that have been generated from temperatures close to those at which they will be applied. As the temperature gap becomes wider, the relationship between temperature and development rates becomes less linear. For instance, Protophormia terraenovae takes 13.9 days to complete development at 23°C or 319.7 ADD, and 10.9 days or 314.7 ADD at 29°C (Greenberg, 1991), showing that the relationship between development and temperature for these two temperatures is very close to linear, allowing for the accurate use of ADD to predict development times between these temperatures. However, at the much lower temperature of 12.5°C, this species takes 90.7 days or 1133.75 ADD to complete development; the relationship is more sigmoid than linear at this temperature.

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If data generated at 16.1°C, very close to that of the death scene, are converted to ADD, it would take Phormia regina (and presumably Protophormia terraenovae) a minimum of 480.5 ADD and a maximum of 580 ADD to reach the adult stage (Anderson, 2000). Using the temperatures predicted for the crime scene by the regression analysis, 480.5 ADD would have been accumulated by June 5 and 580 ADD by June 11. Other factors that must be considered include whether or not a maggot mass increased the temperature of the body, and so speeded up development. This is difficult to predict in most cases, when the insect colonization has gone beyond the maggot stage. However, in this case the entire scene was very carefully gridded, searched and screened and a total of only 20 puparia and 19 pupae were found. Even when exhaustive search methods such as this are used, it is quite possible that some pupae/puparia may have been missed, but even if only 10 to 20% were collected, there would still not have been nearly enough maggots to generate any significant increase in temperature. It could be argued that scavengers had moved the remains away from its original decomposition site, but this was not the case as decomposition had clearly occurred at the discovery site. Even when maggot masses are present, the lab data still appear to be representative of field data. This is possibly because the oldest prepupal maggots appear to leave before a maggot mass begins to generate heat when the remains are in shade (Dillon, 1997; Dillon and Anderson, 1996, 1998) or it may be because lab data still incorporate a measure of maggot mass activity as large numbers of maggots are raised together. Field experiments with pig carcasses (Sus scrofa (L.)) in the northern interior region of British Columbia showed very similar developmental data for Phormia regina (Dillon, 1997; Dillon and Anderson, 1996). A large number of carcasses were placed at the research site and were monitored throughout decomposition. Insects were regularly collected from them in order to observe development and insect succession in a natural environment (Dillon, 1997; Dillon and Anderson, 1996). The research site had very similar weather conditions to those found at the scene in this case, and as temperature is the main governing force in blow fly development, these data are probably representative of those from the crime scene. These similarities, of course, do not apply to successional data, as geographic differences have a great deal more influence on arrival times and species composition on later successional species. In the field research, the very first blow fly to emerge was observed 30 days after death (Dillon, 1997; Dillon and Anderson, 1996). After considerable searching of the remains and the soil nearby, only one empty pupal case was found, but within the next 5 days 200 pupal cases were found (Dillon, pers. comm.). This indicates that the very first flies emerged after 30 days and continued to emerge for several days. Phormia regina was the dominant species at this site, representing over 80% of the blow flies (Dillon, 1997; Dillon and Anderson, 1996). The mean temperature at the research site was 15.4°C, very similar to that at the crime scene, with the mean maximum temperature at 22.2°C, slightly above that at the weather stations near the scene, and the mean minimum temperature was 8.6°C, slightly lower than the mean minimum temperatures at the weather stations (Dillon, pers. comm.; Dillon, 1997; Dillon and Anderson, 1996). So the weather conditions at the research site in British Columbia were very similar to those indicated for the death scene, using any or all of the weather station data. Large maggot masses were present on the carcasses at the research site and they did raise the internal carcass temperature. The mean internal carcass temperature was 23.1°C,

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with a mean maximum of 27.6°C and a mean minimum of 18.7°C. The highest temperature reached was 44.8°C, and the lowest was 8.0°C. (Dillon, pers. comm.; Dillon, 1997; Dillon and Anderson, 1996). However, despite the increased heat generated by the maggots, the first insects still took 30 to 35 days to develop (Dillon, pers. comm.; Dillon, 1997; Dillon and Anderson, 1996), just the same as laboratory data indicated (Anderson, 2000). P. regina takes a minimum of 15.4 days to complete development at 23.0°C (Anderson, 2000). Had the mean carcass temperature of 23.1°C been used to determine developmental rates for the research carcasses, rather than ambient temperatures, death of the research pigs would have been predicted to have occurred 15.4 days postmortem, rather than the actual 30 days. Obviously, although maggot masses can raise the temperature of the carcass, development at these temperatures still appears to be very closely linked to ambient temperature, rather than maggot mass temperature. These field data (Dillon, pers. comm.; Dillon, 1997; Dillon and Anderson, 1996) completely support the laboratory data (Anderson, 2000). These data also answer questions about the potential effect of constant vs. fluctuating temperatures. Frequently, there is a question in court as to whether data generated in a lab, at constant temperatures, can be applied to a field situation in which the insects are exposed to fluctuating temperatures. The proper use of degree days should eliminate some of this concern; however, it is possible that fluctuating temperatures could retard or increase developmental rates as is seen in some insect groups (Bradshaw, 1980; Hagstrum and Leach, 1972; Messenger, 1964, 1969; Richards and Suanraksa, 1962; Yeargan, 1980). Research on blow flies has shown that in most species there is no significant difference between development rates of insects raised at constant temperatures and those raised at a temperature that fluctuated around the mean (Dallwitz, 1984; Greenberg, 1991). This is supported by field research (Dillon, 1997; Dillon and Anderson, 1996) and lab data (Anderson, 2000). In some blow fly species, fluctuation in temperature slightly delayed development rate (Erzinclioglu, 1996; Greenberg, 1991), which means that in these cases, because forensic entomologists usually estimate a minimum elapsed time since death, any error generated by using data developed at constant temperatures will be conservative. The estimate of 480.5 ADD, reached on June 5, is based on the minimum developmental time to reach the adult stage and assumes that the very first flies have only just emerged on the day of collection. The estimate of 580 ADD, reached on June 11, is based on the maximum time to reach the adult stage, and assumes that all the flies have eclosed. In this case, however, just over half the collected pupae and empty puparia consisted of puparia, indicating that approximately half the insects had already emerged. Therefore, these insects were probably oviposited midway between June 5 and 11, around June 8. Another factor to be taken into account is the fact that Phormia regina is a species that is often not attracted to the remains for the first few days after death (Anderson and VanLaerhoven, 1996; Denno and Cothran, 1976; Goddard and Lago, 1985; Hall and Doisy, 1993; Lord and Burger, 1984), with the majority attracted 2 to 3 days after death. So it is possible that death occurred 2 to 3 days before oviposition, indicating that death probably occurred on June 5, the day the victim went missing. Many other species of insects were associated with these remains, as well as blow flies, and were mostly those seen in later succession: days, weeks, or months after death. Blow flies are ubiquitous and most data used in their analyses are lab generated. Therefore, such data can be applied to any geographical area, as long as careful attention is made to local meteorological conditions, which are the main governing forces in blow fly development.

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However, the successional colonization of remains by carrion insects depends heavily on geographic region and biogeoclimatic zone. Different species will be present in various geographic areas, and their arrival times and tenure on the body may change greatly from region to region (Anderson and VanLaerhoven, 1996; Dillon, 1997; Dillon and Anderson, 1995, 1996). Therefore, data generated from one geographic region should only be applied to another geographic region with utmost caution. No successional database existed at the time of this case for any region of central Canada, so the timing of arrival of the other species in this case could not be used to back up the estimation based on blow fly development. We have, however, begun an extensive set of experiments to develop a database of insect succession on carrion for the southern Manitoba region in the future (Gill et al., 1998/2000).

Collection of Puparia 1. Empty pupal cases will be found hidden, usually a few centimeters deep in the soil, or within clothing pockets, folds, and seams — see Collection of Blow Fly Pupae for full details. 2. Empty pupal cases look very similar to pupae, but as if the top has been cut off, a bit like a boiled egg with the top removed (Figure 9.6). They will be hollow inside. See Haskell et al. (1997). 3. Search for puparia but also for the tiny caps that have been pushed off, as these can be very diagnostically useful. The caps are tiny and very fragile (Figure 9.6). 4. Place in a dry vial and add a piece of tissue paper to cushion them in transit. No preservation is required as they are not alive. 5. A small soil sample should also be collected — see Collection of Blow Fly Pupae for details.

Successional Colonization of the Remains Once blow flies have gone through an entire life cycle on the remains, they can be used only to indicate a minimum elapsed time since death. Additional analyses of the later colonizing species are useful in refining that estimate. This method usually is not as precise as using maggot development, but can estimate the postmortem interval up to a year or more after death. However, much more than blow fly development, the successional colonization of remains is very dependent on biogeoclimatic zone, habitat, and season. Therefore, databases of insect succession on carrion should be established for all areas, seasons, and habitats in which such analyses are being attempted.

Case Study #7 Human remains were found under the frame of a waterbed in northwestern Canada. The mattress was not present; the remains were completely enclosed by the frame, and the frame was covered with a plastic lining. The remains were partially mummified and fully clothed. The victim had last been seen alive the previous year, in March. The bed was in a basement bedroom of a house (the house had been continuously occupied). A number of different species were collected from the remains, including pupae and puparia from

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Figure 9.7 Cast larval skins of dermestid beetles (Dermestidae: Coleoptera). (Photograph taken by G.S. Anderson. With permission.)

the families Fanniidae and Sphaeroceridae (Diptera), and cast larval skins of Dermestidae (Coleoptera) (Figure 9.7), together with large quantities of dermestid frass (excreta) and peritrophic membrane. Peritrophic membrane lines the gut of insects and is passed out when the insect defecates. Normally, it is lost, together with the delicate cast larval skins of beetles, due to the action of environmental conditions such as rain and wind; however, in sheltered conditions, peritrophic membrane associated with dermestid beetles (Coleoptera: Dermestidae) may build up and survive for a long period of time. It is often found years after death (Haskell et al., 1997; Voigt, 1965), but has been observed as early as 4 months after death (Haskell et al., 1997). Although the remains would have been highly unattractive to blow flies at the stage they had reached when discovered, some evidence of blow fly presence, such as empty pupal cases, would have been expected had they been present earlier. No Calliphoridae were found at any developmental stage, nor was there any evidence of past colonization. In fact, peritrophic membrane is usually found in cases in which fly activity has been minimal. (Haskell et al., 1997) The remains were found in late May, a time when mean daily temperatures were in the single figures, and night time temperatures still commonly dropped below 0°C. It was too early for insects to have colonized the remains that season, so the remains must have been present the previous year. The large numbers of puparia and pupae of later colonizing insect species indicated the remains had been present in the room during an entire insect season. Since there was no reason blow flies could not have penetrated to the body, the complete lack of these first colonizers provided evidence that the victim did not die in the summer. A delay in colonization might have been expected due to the protected state of these remains, but no more than a matter of days. Clearly, the fact that the remains were under a waterbed frame did not prevent other insect families from colonizing. When the insect season began in June, the remains would no longer have been attractive to blow flies, but would have been to later colonizers, such as Fanniidae, Sphaeroceridae, and Dermestidae. Their presence indicated that the victim had died during the wintertime, over a year previous to discovery. The victim must have died, and had time to become mummified before the insect season began. The defendant later admitted strangling the victim the previous March, and placing the victim under the bed.

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Collection of Other Insect Evidence 1. Search the body, the clothing, and all the surrounding area for insects. They may be found on or under the body, above the body in the air, or in the soil or carpet. 2. Beetle adults and larvae move rapidly, so the collector must be ready to catch them. They can be placed in separate vials (evidence will eat evidence!) or in one vial filled with alcohol. 3. Small adult flies or larvae can be collected with a paint brush dampened with water. Adults can be placed in alcohol and larvae should be treated in a similar manner to blow fly larvae, with half preserved and half kept alive. 4. A sweep net can be used to collect flying insects, but care must be taken not to disturb other evidence. 5. Measure ambient and soil temperatures, and leave a data logger at the scene, if possible, for 3 to 4 weeks to record the temperatures. If the victim is buried, soil temperature at the depth of the victim should be recorded as this more approximates the body temperatures (VanLaerhoven, 1997; VanLaerhoven and Anderson, 1996, 1999). 6. The soil or area under and near the remains should be screened, and a small soil sample collected as before. See R.C.M.P. “E” Division Training (1997) for further details.

Conclusions Insects can be extremely valuable in a forensic investigation, and can be used to determine time of death, from days to years after death. However, accurate collection is vital. If the insects are not collected properly at the scene, then little or no analysis can be completed. It is, therefore, vital that a trained specialist, preferably a Board Certified Forensic Entomologist (American Board of Forensic Entomology), is called to the scene. If time does not permit the presence of the entomologist at the scene, then officers should contact the entomologist to receive advice over the phone. Above all, a qualified forensic entomologist should be located and contacted long before such a case occurs so that he or she can be quickly contacted when the need arises. Insects collected by investigators should be hand delivered or sent by courier to the entomologist as soon as possible. A good collection should include collection at the scene and at the autopsy, when a more detailed examination of the remains can be made.

References Anderson, G.S. 1995 The use of insects in death investigations: an analysis of forensic entomology cases in British Columbia over a five year period, Canadian Society Forensic Sciences Journal 28(4):277–292. 1999a Forensic entomology: the use of insects in death investigations. In Case Studies in Forensic Anthropology, edited by S. Fairgreave, pp. 303–325. Charles C Thomas, Toronto. 1999b Wildlife forensic entomology: determining time of death in two illegally killed black bear cubs, a case report, Journal of Forensic Sciences 44(4):856–859.

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2000 Minimum and maximum development rates of some forensically important Calliphoridae (Diptera), Journal of Forensic Sciences 45(4):824–832. Unpublished data, School of Criminology, Simon Fraser University, Burnaby, British Columbia. Anderson, G.S. and S.L. VanLaerhoven 1996 Initial studies on insect succession on carrion in southwestern British Columbia, Journal of Forensic Sciences 41(4):617–625. Baer, W.S. 1931 The treatment of chronic osteomyelitis with the maggot (larva of the blow fly), Journal of Bone and Joint Surgery 13:438–475. Bauch, R., K. Ziesenhenn, and C. Groskoppf 1984 Lucilia sericata myiasis (Diptera: Calliphoridae) on a gangrene of the foot, Angewandte Parasitologie 25(3):167–169. Bradshaw, W.E. 1980 Thermoperiodism and the thermal environment of the pitcher-plant mosquito, Wyeomyia smithii, Oecologia 46:13-1. Carpenter, T.L. and D.O. Chastain 1992 Facultative myiasis by Megaselia sp. (Diptera: Phoridae) in Texas: a case report, Journal of Medical Entomology 29(3):561–563. Catts, E.P. and M.L. Goff 1992 Forensic entomology in criminal investigations, Annual Review of Entomology 37:253–272. Catts, E.P. and N.H.E. Haskell 1990 Entomology and Death — A Procedural Guide, Joyce’s Print Shop, Inc., Clemson, SC. Chapman, R.F. 1980 The Insects, Structure and Function, Hodder and Stoughton, London. Dallwitz, R. 1984 The influence of constant and fluctuating temperatures on development and survival rate of pupae of the Australian sheep blow fly, Lucilia cuprina, Entomologie Experimentalis et Applicata 36:89–95. Denno, R.F. and W.R. Cothran 1976 Competitive interaction and ecological strategies of sarcophagid and calliphorid flies inhabiting rabbit carrion, Annals of the Entomological Society of America 69:109–113. Deonier, C.C. 1940 Carcass temperatures and their relation to winter blow fly activity in the Southwest, Journal of Economic Entomology 3:166–170. Deroo, H. et al. 1990 Human cutaneous parasitosis: two cases of furuncular and creeping myiasis, Dermatologica 180(3):199–200. Dillon, L.C. 1997 Insect succession on carrion in three biogeoclimatic zones in British Columbia, M.Sc. thesis, Simon Fraser University, Burnaby, B.C., p. 76. Personal communication, Dept. of Biological Sciences, Simon Fraser University, presently Coroner, B.C. Coroners Service, Burnaby, B.C. Dillon, L.C. and G.S. Anderson 1995 Forensic entomology: the use of insects in death investigations to determine elapsed time since death, Canadian Police Research Centre, Technical Report TR-05-95, Ottawa, Ontario.

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1996 Forensic entomology: a database for insect succession on carrion in Northern and Interior B.C., Canadian Police Research Centre, Technical Report TR-04-96, Ottawa, Ontario. 1998 Insect Succession on carrion in three biogeoclimatic zones of British Columbia, American Academy of Forensic Sciences, San Francisco. Early, M and M.L. Goff 1986 Arthropod succession patterns in exposed carrion on the island of Oahu, Hawaiian Islands, Journal of Medical Entomology 23:520–531. Erzinclioglu, Y.Z. and R.P. Whitmore 1983 Chrysomya albiceps (Wiedemann) (Diptera: Calliphoridae) in dung and causing myiasis in Oman, Entomologist’s Monthly Magazine 119:51–52. Erzinclioglu, Z. 1996 Blow Flies, Richmond Publ., Slough. Fawzy, A.F. 1991 Otitis media and aural myiasis, Journal of the Egyptian Society of Parasitology 21(3):883–885. Fotedar, R., U. Banerjee, and A.K. Verma 1991 Human cutaneous myiasis due to mixed infestation in a drug addict, Annals of Tropical Medicine and Parasitology 85(3):339–340. Fraenkel, G. 1935 Observations and experiments on the blow fly (Calliphora erythrocephala) during the first day after emergence, Proceedings of the Zoological Society of London 893–904. Fraenkel, G., and G. Bhaskaran 1973 Pupariation and pupation in cyclorraphous flies (Diptera): terminology and interpretation, Annals of the Entomological Society of America 66:418–422. Gilbert, B.M. and W.M. Bass 1967 Seasonal dating of burials from the presence of fly pupae, American Antiquity 32:534–535. Gill, G. et al. 1998/2000 Dept. of Entomology, University of Manitoba, and School of Criminology, M.Sci. thesis in progress, Simon Fraser University. Goddard, J. and P.K. Lago 1985 Notes on blow fly (Diptera: Calliphoridae) succession on carrion in Northern Mississippi, Journal of Entomology Sciences 20:312–317. Goff, M.L., S. Charbonneau, and W. Sullivan 1991 Presence of fecal matter in diapers as a potential source of error in estimations of postmortem intervals using arthropod development rates, Journal of Forensic Sciences 36(5):1603–1606. Greenberg, B. 1984 Two cases of human myiasis caused by Phaenicia sericata (Diptera: Calliphoridae) in Chicago area hospitals, Journal of Medical Entomology 21:615. 1990 Nocturnal oviposition behavior of blow flies (Diptera: Calliphoridae), Journal of Medical Entomology 27:807–810. 1991 Flies as forensic indicators, Journal of Medical Entomology 28:565–577. 1996 Personal communication, University of Illinois, Chicago, IL. Greenberg, B. and T.I. Tantawi 1993 Different developmental strategies in two boreal blow flies (Diptera: Calliphoridae), Journal of Medical Entomology 30(2):481–484.

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Hagstrum, D.W. and C.E. Leach 1972 Role of constant and fluctuating temperatures in determining developmental time and fecundity of three species of stored products Coleoptera. Annals of the Entomological Society of America 66:407–410. Hall, R.D., P.C. Anderson, and D.P. Clark 1986 A case of human myiasis caused by Phormia regina (Diptera: Calliphoridae) in Missouri, USA, Journal of Medical Entomology 23(5):578–579. Hall, R.D. and K.E. Doisy 1993 Length of time after death: effect on attraction and oviposition or larviposition of midsummer blow flies (Diptera: Calliphoridae) and Flesh Flies (Diptera: Sarcophagidae) of medicolegal importance in Missouri, Annals of the Entomological Society of America 86(5):589–593. Haskell, N.H. et al. 1997 On the body: insects’ life stage presence and their postmortem artifacts. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, CRC Press, Boca Raton, FL, pp. 415–448. Henssge, C. et al. 1995 The Estimation of the Time since Death in the Early Postmortem Period, Arnold, Seven Oaks, CA. Hobischak, N.R. 1997 Freshwater invertebrate succession and decompositional studies on carrion in British Columbia, M.P.M. thesis, Simon Fraser University, Burnaby, B.C., p. 54. Hobischak, N.R. and G.S. Anderson In press. Time of submergence using aquatic invertebrate succession and decompositional changes, Journal of Forensic Science. Johl, H.K. and G.S. Anderson 1996 Effects of chilling on development of the blow fly Calliphora vicina Robineau-Desvoidy (Diptera) and their relationship to time of death, Journal of the Entomological Society of British Columbia 93:93–98. Kamal, A.S. 1958 Comparative study of thirteen species of sarcosaprophagous Calliphoridae and Sarcophagidae (Diptera). I. Bionomics. Annals of the Entomological Society of America 51:261–270. King, A.B. and K.J. Flynn 1991 Maggot therapy revisited: a case study, Dermatology Nursing 3:100–102. Kpea, N. and C. Zywocinski 1995 Flies in the flesh: a case report and review of cutaneous myiasis, Cutis 55(1):47–48. Kumar, A. and B.P. Joshi 1995 Studies on the clinical efficacy of ivermectin against cutaneous myiasis in domestic animals, Indian Veterinary Journal 72(3):277–280. Lee, H.L. and Y.K. Yong 1991 Human aural myiasis, Southeast Asian Journal of Tropical Medicine and Public Health 22(2):274–275. Liu, D. and B. Greenberg 1989 Immature stages of some flies of forensic importance, Annals of the Entomological Society of America 82:90–93. Lord, W.D. and J.F. Burger 1984 Arthropods associated with Herring Gull (Larus argentatus) and Great Black-Backed Gulls (Larus marinus) carrion on islands in the gulf of Maine, Environmental Entomology 13:1261–1268.

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MacDonell, N.R. and G.S. Anderson 1997 Aquatic forensics: determination of time since submergence using aquatic invertebrates, Canadian Police Research Centre, Technical Report TR-01-97, Ottawa, Ontario. Melvin, R. 1934 Incubation period of eggs of certain muscoid flies at different constant temperatures, Annals of the Entomological Society of America 27:406–410. Messenger, P.S. 1964 The influence of rhythmically fluctuating temperatures on the development and reproduction of the spotted alfalfa aphid, Therioaphis maculata, Journal of Economic Entomology 57:71–76. 1969 Bioclimatic studies of the aphid parasite Praon exsoletum. 2. Thermal limits to development and occurrence of diapause, Annals of the Entomological Society of America 62:1026–1031. Miller, K.B., L.J. Hribar, and L.J. Sanders 1990 Human myiasis caused by Phormia regina in Pennsylvania, Journal of the American Podiatrical Medicine Association 80(11):600–602. Moon, R.D. Personal communication, University of Minnesota, St. Paul. Morsy, T.A. and A.M. Farrag 1991 Two cases of human ophthalmomyiasis, Journal of the Egyptian Society of Parasitology 21(3):853–855. Nielsen, B.O. 1993 Cases of human myiasis from Denmark, Entomologiske Meddelelser 61(3):81–82. Nuorteva, P. 1977 Sarcosaprophagous insects as forensic indicators. In Forensic Medicine: A Study in Trauma and Environmental Hazards, Vol. II, edited by C.G. Tedeschi, W.G. Eckert, and L.G. Tedeschi, pp. 1072–1095. W.B. Saunders, Philadelphia. Payne, J.A. 1965 A summer carrion study of the baby pig Sus scrofa Linnaeus, Ecology 46:592–602. Pechter, E.A. and R.A. Sherman 1983 Maggot therapy: surgical metamorphosis, Plastic and Reconstructive Surgery 72:567–570. Petersen, J.J. and B.M. Pawson 1988 Early season dispersal of Muscidifurax zaraptor (Hymenoptera: Pteromalidae) utilizing freeze-killed housefly pupae as hosts, Medical and Veterinary Entomology 2:137–140. Richard, R.D. and R.R. Gerrish 1983 The first confirmed field case of myiasis produced by Chrysomya sp., (Diptera: Calliphondae) in the continental United States, Journal of Medical Entomology 30:685. Richards, A.G. and S. Suanraksa 1962 Energy expenditure during embryonic development under constant versus variable temperatures (Oncopeltus fasciatus (Dallas)), Entomology Experimentalis et Applicata 5:167–178. Rodriguez, W.C. and W.M. Bass 1987 Examination of badly decomposed or skeletonized remains — overlooked evidence. Thirty-ninth annual meeting American Academy of Forensic Sciences, San Diego. Royal Canadian Mounted Police “E” Division Training 1997 Forensic Entomology, Vancouver, B.C. Shean, B.S., L. Messinger, and M. Papworth 1993 Observations of differential decomposition on sun exposed v. shaded pig carrion in coastal Washington State, Journal of Forensic Sciences 38(4):938–949.

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Sherman, R.A. 1998 Maggot debridement in modern medicine, Infections in Medicine 15(9):651–656. Sherman, R.A. and E.A. Pechter 1988 Maggot therapy: a review of the therapeutic applications of fly larvae in human medicine, especially for treating osteomyelitis, Medical and Veterinary Entomology 2(3):225–230. Sherman, R.A., J.M. Tran, and R. Sullivan 1996 Maggot therapy for venous stasis ulcers, Archives of Dermatology 132:254–256. Sherman, R.A., F.A. Wyle, and L. Thrupp 1995 Effects of seven antibiotics on the growth and development of Phaenicia sericata (Diptera: Calliphoridae) larvae, Journal of Medical Entomology 32(5):646–649. Smith, K.G.V. 1986 A Manual of Forensic Entomology, Trustees of The British Museum (Nat. Hist.) and Cornell University Press, London. Tantawi, T.I. and B. Greenberg 1993 The effect of killing and preservative solutions on estimates of maggot age in forensic cases, Journal of Forensic Sciences 38(3):702–707. VanLaerhoven, S.L. 1997 Successional Biodiversity in Insect Species on Buried Carrion in the Vancouver and Cariboo Regions of British Columbia, M.P.M. Thesis, Dept. of Biological Sciences, Simon Fraser University, Burnaby, B.C., 60 pp. VanLaerhoven, S.L. and G.S. Anderson 1996 Forensic entomology. Determining Time of Death in Buried Homicide Victims Using Insect Succession. Canadian Police Research Centre, Technical Report TR-02-96, Ottawa, Ontario. 1999 Insect succession on buried carrion in two biogeoclimatic zones of British Columbia, Journal of Forensic Sciences 44:31–41. Voigt, J. 1965 Specific postmortem changes produced by larder beetles, Journal of Forensic Medicine 12:76–80. Wall, R., N. French, and K. Morgan 1992 Blow fly species composition in sheep myiasis in Britain, Medical and Veterinary Entomology 6:177–178. 1995 Population suppression for control of the blow fly Lucilia sericata and sheep blow fly strike, Ecological Entomology 20:91–97. 1990 The incidence of flystrike in sheep in relation to weather conditions, sheep husbandry and the abundance of the Australian sheep blow fly Lucilia cuprina (Wiedmann) (Diptera: Calliphoridae), Australian Journal of Agricultural Research 41:1155–1167. Webster, A. 1999 Personal communication, Environment Canada, Pacific Region. Yeargan, K.V. 1980 Effects of temperature on developmental rate of Telenomus podisi (Hymenoptera: Scelionidae), Annals of the Entomological Society of America 73:339–342.

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Human Remains in Water Environments WILLIAM D. HAGLUND MARCELLA H. SORG

10

Contents Introduction Significance of Aqueous Environments to Fossil and Forensic Assemblages Behavior of Carcasses in Bodies of Water: Sink or Float? Behavior of Floating Carcasses: Position and Movement Decomposition of Carcasses in Water Disarticulation of Carcasses in Water Fluvial Transport Studies and the Behavior of Single Bones Bone Modifying Effects of Water Environments Recovery Issues Conclusion Acknowledgment References

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Table 10.1

Global Water Inventory

Reservoir Rivers Atmosphere Soil moisture Freshwater lakes Saline lakes and inland seas Groundwater (to 4-km depth) Glacial ice Oceans Total

Volume (thousand km) 1 13 67 125 104 8350 29,200 1,320,000 1,357,860

Volume (%) 0.0001 0.0010 0.0049 0.0092 0.0076 0.6149 2.1504 97.2118 100.0001

Source: Adapted from Skinner and Porter (1987).

Introduction Approximately 71% of the earth’s surface is hydrosphere, i.e., covered with water. More than 97% of the earth’s water resides in oceans and saltwater seas. Of the remaining 3%, 2% is distributed in snow and ice, and 1% is distributed in rivers, freshwater lakes and seas, groundwater, and water vapor (Table 10.1). The nature of these water accumulations varies tremendously in physical and chemical characteristics and biology. Variation between and within hydrospheric units depends on climate, depth and topography, underlying geochemistry, access to other bodies of water, and ecological relationship to the adjacent landforms. From a geological point of view, bodies of water and landforms are dynamic and interactive. Snow, ice, and water are part of a vast array of exogenous agents and processes constantly changing the earth’s surface, and being changed by it. Because humans are primarily terrestrial animals, from one taphonomic perspective they constitute allochthonous remains when found in water; that is, they are foreign remains derived from other biological communities. From another taphonomic perspective, however, because humans extend their activities near and into water, the natural distribution of their remains can be expected to extend there, too, particularly at the land–water interface. Human remains in water are subject to many potential actions, dependent upon the remains themselves and the type and characteristics of the water environment (Table 10.2) (Parsons and Brett, 1991; Sorg et al., 1997). Oceans, rivers, lakes, and ponds may differ radically with respect to temperature, depth, salinity, oxygenation, or current. Features of shores, bottoms, and life forms are also variable. Dependent upon these and other microenvironmental factors, bodies entering water may initially float or sink, possibly to surface later, or remain submerged, or even be buried by accumulating sediment. They may be carried by currents, cast upon shores, caught up in jams of debris, or rafted with floating objects. They may be disarticulated, or consumed by scavengers, or become abraded, dissolved, or otherwise decomposed. Bodies in aqueous environments may also be stationary, i.e., burial in snow or ice, or terrestrial burial where groundwater is abundant. Thus, bodies become modified due to their physical nature (an object that is transported), biochemical nature (a decomposing animal that becomes disarticulated and scattered), and biological nature (a source of food).

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Table 10.2 Factors of Environment and the Body Affecting the Postmortem Fate of Remains Exposed to Aqueous Environments Environment Factors

Body Factors

Temperature Depth Currents Fauna and flora Obstruction and debris Season Water chemistry Sedimentation and geology

Body covering Body habitus Submerged or floating Type of joint Position of joint Amount of tissue surrounding joint Trauma: position and character Adipocere presence

Significance of Aqueous Environments to Fossil and Forensic Assemblages In the fossil record, as in forensic practice, hydraulic factors have played a significant role in transport, modification, and burial. Western (1985) studied the waterside deposition of East African samples of Homo and noted that the record is skewed toward more watered, axial areas of basins associated with the Eastern Rift. According to White (1988), 70% of all hominid specimens whose sedimentary envelope could be established were derived from sand or gravel sediments deposited by moving water. The potential for rapid burial, and hence for preservation, is enhanced in such settings. Some of the most remarkably complete fossil assemblages in the hominid record were water depositions, including the “First Family” of Australopithecus afarensis which may have died in a flash flood, and the Nariokoteme Homo erectus boy whose body was preserved in the marshy floodplain associated with the Omo River (Walker and Leakey, 1993). Extremely waterlogged soils, such as bogs, allow preservation of soft parts, even at the expense of bone (Brothwell, this volume). Certain aqueous environmental settings (e.g., anoxia, rapid burying) associated with mass mortality have produced large concentrations of exceptionally preserved material, sometimes termed lagerstätten by taphonomists (Martin, 1999; Seilacher et al., 1985). Anoxia (usually associated with stagnation) inhibits necrolysis, scavenging, and disarticulation. When coupled with rapid burial (obrution), decaying carcasses will mineralize quite rapidly, sometimes even preserving soft parts (Martin, 1999); extremely alkaline environments in both fresh and saltwater will further enhance the likelihood of certain types of concretions (hence, preservation). Deep lacustrine environments are well-known to promote preservation of both soft tissue and skeletons (Allison and Briggs, 1991a,b). In stark contrast, the forensic literature has, until quite recently, paid scant attention to cases from aqueous environments. When human remains are recovered from water, unique questions are posed regarding their origin (Ebbesmeyer and Haglund, 1994, this volume; O’Brien, 1997), postmortem history (Boyle et al., 1997; Brooks and Brooks, 1997; Haglund, 1993; London et al., 1997; Nawrocki et al., 1997; Sorg et al., 1995; 1997), identity (Rathbun and Rathbun, 1984), and injuries (Brooks and Brooks, 1997). For example, drifting bodies sometimes move long distances from where they entered the water (Ebbesmeyer and Haglund, 1994, and this volume). Giertsen and Morild (1989) discuss two bodies that traveled in excess of 300 miles. Modification of soft tissue, including adipocere formation, can interfere

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with postmortem interval estimates (Cotton et al., 1987; O’Brien, 1997; Simonsen, 1977) and interpretation of injuries (Dix, 1987). Disarticulation, resulting in loss of body parts and their dispersal, can confound identification and the re-attribution of parts to a single person (Haglund, 1993; Symes et al., this volume ). Water environments can modify bones through encrustation, abrasion, bioerosion, and even dissolution (Sorg et al., 1997). Disasters such as floods (Charney and Wilber, 1980, 1984), ship tragedies (Berryman et al., 1988; Ebbesmeyer and Haglund, this volume; Timperman, 1991), and airplane disasters over water provide tremendous challenges to forensic investigators with regard to body recovery, identification, and scene reconstruction. Large losses of human life can be attributed to water. Pennsylvania’s Johnstown Flood of May 31, 1889, accounted for over 2000 fatalities (McCullough, 1968). Current interest in the sinking of the passenger liner Titanic has revived awareness of the large number of its victims (Ebbesmeyer and Haglund, this volume).

Behavior of Carcasses in Bodies of Water: Sink or Float? At the time a carcass enters the water it either sinks or floats. Archimedes’ Principle asserts that an object in water will experience a buoyant force equal to the weight of the water it displaces. Body fat content affects buoyancy, such that bodies with relatively higher fat content have a greater tendency to float, while bodies of lower fat proportion sink (Schäfer, 1978). For animals, hair and feathers trap air and increase carcass buoyancy (Haynes, 1980). Density and viscosity of the surrounding water may alter the speed of changes in position and depth (Martin, 1999). Four potential phases of movement have been suggested by Dilen (1984) for bodies in rivers. They may settle to the bottom, move along the bottom, ascend to the surface, or drift along the surface. These modes are generally applicable to non-riverine, currentdriven bodies of water. Standard forensic references have provided various opinions with regard to the initial behavior of human remains in bodies of water. Simpson (1965) asserts that dead, unclothed bodies are heavier than water and, therefore, sink when immersed. Adelson (1974:563) states that because “specific gravity of the lifeless human body, regardless of cause of death, exceeds the specific gravity of fresh or sea water, any recently dead person always sinks to the ocean floor, river bed, lake, or pool bottom.” Spitz (1980:360) points out that trapped air in clothing could cause a body to be buoyant. Buoyancy significantly increases with the build-up of decomposition gasses (Teather, 1994). Rafting on debris can also account for bodies floating (Haglund, 1993). Donoghue and Minnigerode (1977) calculated specific gravity for living, nude men at functional, residual, and total lung capacity. In both seawater and fresh water, at total lung capacity, all 98 subjects floated. At functional residual capacity, approximately the lung volume of a dead body, 69% floated in seawater and 7% in fresh water. This relationship can be altered by body size and composition, clothing, flotation devices, weights, and decomposition gas. As a body sinks, hydrostatic pressure increases 1 atm for every 10 m. This is a function of Boyle’s Law. Snyder (1972) suggests that once a body begins to sink it goes directly to the bottom. Dilen (1984) claims bodies sink in incremental steps. Because pressure increases with depth, gas in tissue and air in the lungs are compressed, which in turn causes further sinking. These forces alternate until the bottom is reached. Adelson (1974:563) states that, as a body approaches the bottom, it floats in a head down position because the head has a higher specific gravity than the feet. This conclusion is based on observations of accentuated cephalad hypostasis of recovered remains. Once it reaches the floor of an ocean, riverbed, lake, or pool bottom, a body may become encumbered by irregularities

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Figure 10.1 Floating position of fresh remains. (Adapted from Spitz and Fisher’s Medico Legal Investigation of Death, 2nd ed., Charles C Thomas, Springfield, IL, 1993.)

of the substrate, entangled by vegetation or moved by currents. When movement at the bottom occurs, it is because forces of drag and lift overcome forces of gravity and friction. Low temperatures may preclude or significantly inhibit decomposition gas build-up. Anaerobic waters of protected troughs are unfavorable for bacterial activity (Schäfer, 1978). If sufficient depth is reached, no amount of decomposition gas will overcome external water pressure. When temperature, depth pressure, and lack of encumbrance allow, decomposition gas may accumulate and expand the volume of body cavities to a point where internal pressure overcomes external water pressure, the body expands, and the body becomes buoyant. Some of the gas is trapped in body cavities, possibly contained by distention of the esophagus and anus (Schäfer, 1978). Interstitial spaces also confine significant gas build-up. Behavior of Floating Carcasses: Position and Movement If afloat, parts of a carcass are above the surface while others are submerged. This allows differential access to agents of destruction. Position of floating bodies relative to the water line may also affect the rate and sequence of soft tissue destruction and disarticulation of bones or body units. For instance, surfaced portions may be exposed to infestation by insects and devastation by other animals such as birds, while submerged portions are exposed to water life. Mammals with grossly different conformations float in different positions. Fetal pigs float belly-up (Payne and King 1972). Fresh, nude, adult human remains generally float with the back exposed, and the majority of the head and limbs dangling below the water line (Figure 10.1). Such a position in shallow environments exposes these dangling body parts to mechanical abrasion from dragging along the bottom. Especially vulnerable are the forehead, toes, and volar aspects of the hands (Spitz, 1993). Once remains have decomposed with accompanying gas build up in the abdomen they may float face up. The susceptibility of appendages to wave and current action is different from that of the torso. For example, extended appendages such as tails and limbs of terrestrial vertebrates are more vulnerable to being caught on obstructions. Marine mammals are protected from mechanical destruction by their barrel-shaped bodies (Schafer, 1978). This is no doubt enhanced by their diminutive limbs which do not protrude from the body in as exaggerated a fashion as those of terrestrial mammals.

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Schäfer (1978) has provided several comments regarding the behavior of marine carcasses in the closed basin marine environment of the North Sea, where carcasses may drift for weeks on the surface. In such enclosed ocean basins, carcasses generally reach a beach before disintegration, to subsequently be refloated by high tides, or set adrift by backwashing surf. This beaching and refloating may occur many times. Surf action separates, tumbles, and jumbles skeletal parts. Weigelt (1927:83–84) quotes Abel’s description of the action of waves and river currents upon carcasses: A large carcass rolls along the swell, closer to the shore. It is a dead manatee, whose abdomen, blown up like a balloon by gases of decomposition, rises now and then above the surface. Then breakers shove the carcass into the sandy beach. It is already in an advanced stage of decay: the head hangs loosely on the trunk, and the lower jaw has long since fallen to the bottom of the sea.

Shipwreck literature is a virtually untapped source of information regarding behavior of human remains in water (Ebbysmeyer and Haglund, 1994; and this volume). Hydraulic and other oceanographic models may be used to track or predict trajectories of remains in large bodies of water. Potential applications for forensic death investigators include (1) setting geographic and time limits for searches; (2) estimating the likely origin of remains found floating or beached; (3) confirming correlative information regarding entry into the water and sightings of remains; and (4) estimating postmortem interval.

Decomposition of Carcasses in Water For longitudinal observations of the rate and pattern of decomposing carcasses in water we must look to the experimental studies of Dodson (1973) and Payne and King (1972). Dodson examined decomposition of mouse (Mus) and frog (Bufo) in an aquarium of pond water. Deterioration of muscle was followed by skin, then tendon. Payne and King (1972) focused on decomposition and insect succession of previously frozen fetal pigs ( Sus scrofa). The specimens were thawed and placed in wire baskets, which were suspended in tanks of water. Specimens were weighed at 4-hour intervals up to 20 hours. Insect succession was monitored. The process of decomposition was divided into six stages: submerged fresh, early floating, floating decay, bloated deterioration, floating remains and sunken remains. In the initial fresh stage, the majority of pig carcasses sank. They bloated in 2 days in summer or 2 to 3 weeks in winter. In the early floating stage the distended abdomen was usually first to project above water. Eggs were laid on the exposed carcass surfaces by blowflies. Decomposition and insect scavenging took place in tandem. By the bloated deterioration stage most exposed flesh was gone. Maggots migrated from the body and many fed on the carcass below the water line with only spiracles extending above the surface. Head, shoulders, abdomen, and hindquarters had separated by this time. Thus, the body floated until it lost buoyancy and sank. Payne and King and Dodson considered their observations to be affected by a complex interplay of variables, which included pH, pO2, salinity, and temperature. They were critical of the artificiality of their decomposition experiments, particularly the agitation of the carcasses when the baskets in which they were suspended were removed for weighing and observation. Payne was of the opinion that moving the baskets was probably not unlike wave or surf action. His self-criticism included his use of previously frozen specimens. His use of fetal material might also have significantly affected his results. Protection from scavenger access is also an issue.

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Table 10.3 Observations of Taphonomic Changes in 15 Remains from a Sequestered Environment Over a Period of 433 Days Time since Death (Days)

Number of Bodies

2 25 38

2 3 1

68

2

109 433

3 4

Postmortem Changes Washerwoman hands Bloating, marbling, skin slippage Bloating, skin slippage, dark gray-brown discoloration, focal adipocere, purge fluid in body cavities Bloating, skin slippage, dark gray-brown discoloration, extensive subcutaneous adipocere, purge fluid in body cavities Total saponification covered by a thin friable crust Total saponification with thick friable crust and skeletonization

Source: Adapted from Kahana, T. et al., Journal of Forensic Sciences, 44(5), 897–901, 1999.

A recent comment on decomposition in water involves adipocere formation in a series of 15 bodies recovered from Belgian flag cargo ship, the Mineral Dampier, sunk in the East China Sea at a depth of 65 m in water that ranged from 10 to 12°C (Kahana et al., 1999). Thirteen of the remains were recovered over a period of 433 days from the same contained environment aboard the ship. A summary of taphonomic observations is shown in Table 10.3. The authors point to discrepancies between their data and other published accounts of the rate of adipocere formation, and conclude that the presence of adipocere formation is unreliable for estimating postmortem interval.

Disarticulation of Carcasses in Water Disarticulation sequences have important ramifications for differential skeletal element survival and accumulation. One would expect differences in disarticulation pattern between bodies floating in water vs. those supported by a firm substrate. For example, the dangling appendages of carcasses floating in water are subject to constant movement, agitation, and potential transport. Schäfer (1972) asserts that bones of drifting whale carcasses become largely separated prior to the skin rupturing. Once rupture of the hide occurs, bones fall one by one as if from a drifting sack. For seals, whales, and dolphins, the integument tears where tensile strength is particularly strong: above roof of skull, at outer rims of jaws, and above the shoulder, scapula, and tail section. He asserts that for drifting seals, drying of gum tissue results in teeth being pulled from gums. Phalanges and forelimbs are next to disarticulate. Commenting on disarticulation of cows from the Gulf Coast of the United States, Weigelt (1927) observed that the mandible separates first, then disarticulation proceeds from the extremities. Dodson (1973) noted the following disarticulation sequence: caudal vertebrate sections, femur from acetabulum, jaw from skull, and hand from arm. Eventually, disarticulated bony elements and carcass units separate from a carcass or the carcass loses buoyancy and settles to a new environment where it is subjected to different taphonomic circumstances. In one study of the disappearance of soft tissue and the disarticulation of human remains recovered from aqueous environments in the Puget Sound area, bodies were scored for regional presence of soft tissue, exposure of bone, and loss of body parts to determine the general pattern of soft tissue loss and loss of body parts (Haglund, 1993). The following regions were scored: cranium, mandible, neck, hands, forearms, upper arms, feet, legs, pelvic girdle, and

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trunk. Initial disappearance of soft tissue, exposing underlying bones, occurred in areas thinly covered by soft tissue beginning with the head, hands, and anterior lower legs. For this small sample (11 individuals) disappearance of body parts followed a general sequence: bones of the hands and wrists, bones of the feet and ankles, and mandible and cranium. The lower legs, forearms, and upper arms are the next units to separate from the body. Postmortem intervals for 6 of the 11 remains were known and ranged from 1.25 to 36 months. As seen from Table 10.4, when the cases were ordered using the above criteria, postmortem interval could not be reliably estimated based on the condition of the body and time of recovery. As parts drop away from a floating carcass in large or current-driven bodies of water, they are often separated from the major body unit. This complicates both the recovery and the interpretation. Knowledge of disarticulation sequences allows more informed assessment of skeletal elements expected vs. recovered in the forensic context, and assists in the interpretation of artifacts and events produced by different disarticulating environments (Figure 10.2).

Fluvial Transport Studies and the Behavior of Single Bones Nawrocki et al. (1997) point to three unit-phases of fluvial transport: (1) the body as a unit of transport, before significant disarticulation has occurred; (2) movement of disarticulated body parts; and (3) the movement of isolated bones. It is the third phase that has hitherto received most attention. Studies of bone sorting and movement in water have focused on single bones of animals (Behrensmeyer, 1982; Dechant-Boaz, 1982; Hanson, 1980; Voorhies, 1969). A major reason for the concentration on single bones is the assumption that fossil bone accumulations resulted from sheet-wash transport of previously disarticulated skeletal elements that had been deposited on flood plains. These experimental studies used artificial flumes (inclined channel with running water). Voorhies (1969), in a now classic report, attempted to determine the process of bone accumulation in the Valentine Formation of northeastern Nebraska. He tested whether the relative differences of skeletal elements represented in this early Pliocene bone concentration could be due to current sorting. He used coyote and sheep bone in “stream table” experiments to determine the effect of current sorting of various bony elements. Condition of the bones was not indicated. The general conclusions were that bones, which tend to move by rolling, will become oriented transverse to the current and those with one end markedly heavier than the other will tend to move by sliding with their long axis parallel to the current. Exceptions arose in very shallow water, where the bone was partially submerged. Voorhies classified bones as falling into highly transportable, intermediate, and lag groups. Boaz and Behrensmeyer (1976) provide the only direct observations of human bones in moving water. Using 35 human bone elements or parts and an artificial flume, different transport groups were achieved. Skeletal parts consisted of fragmentary and weathered material, as well as whole skulls. Behavior was characterized as (1) sliding, movement along the bed in which the bone material remains horizontal; (2) flipping, movement around the axis perpendicular to the current in which the piece turns over once; (3) rolling, successive tumbling of a skeletal part around an axis perpendicular to the current; (4) stable, where the piece lies flat on the bed and shows no movement; and (5) quasi-stable, where there is little or no component of longitudinal movement, but the piece is not flat on the bed or moves slightly in some direction. Orientation was defined as the relationship of

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Table 10.4 Disappearance of Soft Tissue and Bone for Bodies Subjected to Aqueous Environments (in order of increasing tissue and body part loss scores)

Case 1 2 3 4 5 6 7 8 9 10 11 Total Note:

Mandible 1 1 1 1 2 2 4 4 4 4 4 28

Cranium 1 1 1 1 2 2 2 4 4 4 4 28

Hand

Lower Leg

0 1 1 1 1 2 4 4 4 4 4 26

0 0 1 1 1 1 3 3 1 3 4 18

Neck

Forearm

0 0 0 0 1 2 1 3 2 4 4 17

0 0 0 0 0 0 1 3 4 4 4 16

Feet

Upper Arm

0 0 0 1 0 0 0 4 3 3 4 15

0 0 0 0 0 0 1 2 3 4 4 14

Trunk

Upper Leg

Pelvic Girdle

0 0 0 0 0 0 0 1 1 3 3 8

0 0 0 0 0 0 0 1 2 1 1 5

0 0 0 0 0 1 0 0 1 1 1 4

0 = soft tissue complete; 1 = partial exposure of bone; 2 = total exposure of bone; 3 = exposure of bone and partial absence of area; 4 = absence.

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Total

Postmortem Interval

2 3 4 5 6 9 16 29 29 35 37

1.25 26 9 31 — — 2.5 — — 36 —

Figure 10.2 Schematic representation of disarticulation and bone exposure of floating bodies in aqueous environments (in order of increasing tissue and body part loss).

the long axis to the current. Orientation can be influenced by water depth, initial orientation of bone, size and shape (Hanson, 1980; Hill, 1975; Toots, 1965; Voorhies, 1969). Dodson (1973) sought to determine the sequence of mouse bone movement. He reported the following sequence: large thoracic vertebrae, small thoracic vertebra, pelvis,

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caudal vertebrae, cervical vertebrae, tibia-fibula, femur, calcaneus, radius, ulna, jaw, incisor. Very low water velocities were sufficient to move any of these small bones. Each of these experiments has shown the behavior of bones in current-driven water to be idiosyncratic for particular skeletal parts (Boaz and Behrensmeyer, 1976; Dodson, 1973; Voorhies, 1969). Initial placement did not seem to affect behavior. Elongate pieces, circular in cross section, roll in an arc around the smaller end, resulting in a quasi-stable orientation with the larger end of the piece pointing downstream. Samples could be divided into transportable and non-transportable groups. Flat or small skeletal parts lacking processes maintain stable or quasi-stable positions. Individual cranial and mandibular parts do not move (lag group), whereas complete crania are the fastest moving of single elements. Table 10.5 summarizes skeletal elements and their respective transport groups from the studies of Voorhies (1969) and Boaz and Behrensmeyer (1976). Inconsistencies between these studies are explained, in part, by variations in experimental conditions (Table 10.6). Potts (1988) discusses commonalities in the experimental results: (1) mandibles in the lag category; (2) tibia and radius (proximal ends only for human bones) in the intermediate group; and (3) sacral vertebrae and sacrum in the highly transportable category. A major inconsistency was found for bones with high surface-to-volume ratios (e.g., ribs, sacrum, and scapula) placed in Voorhies group I, but in Boaz and Behrensmeyer’s group III. Hanson (1980) suggested that improvement is needed in attempts to define fluvial transport criteria. The experiments of Voorhies (1969) and Boaz and Behrensmeyer (1976) assumed ideal rather than natural conditions. Hanson suggested that further refinement needs to insure that (1) vertical distribution of fluid velocity is adequately described; (2) water depth is much greater than element height; (3) there is an insignificant amount of sediment in transport; (4) bones are not impeded, buried, or sheltered by bed features; and (5) the normal force between the bone and the bed is greater than zero and equal to the submerged weight of bone. He attempted to derive equations predictive of bone behavior in fluvial environments, pointing out that such schemes are applicable only if hydraulic transport is the only biasing agent and if three further conditions are addressed. First, skeletal elements should be completely disarticulated prior to the initial transport event. If this assumption is not met, the term unit rather than skeletal element should be used when referring to complete carcass or a physically connected portion of it. Second, predicted biases may not be apparent if the parent assemblage included only a narrow transportability spectrum of elements. Third, there should be no nonfluvial biases, for instance, a parent assemblage that is made up of bones that would be underrepresented in a fluvial transport assemblage. Todd and Frison (1986) analyzed mammoth bones deposited in an arroyo bottom at the Colby Site. Their observations and conclusions underscore the idiosyncrasies of natural conditions, which create fluvial biases and may dictate dispersal, orientation, and accumulation of bones. The arroyo was narrow, steep-sided, and composed of bentonite that becomes extremely slick when wet. Movement of bones was constrained at the narrow channel bottom. Although long bones were aligned roughly parallel to the channel, they were aligned without regard to polarity, i.e., with their heavier ends pointing upstream and lighter ends downstream. In the constricted channel they had equal opportunity of sliding to its bottom with polarity in either direction. The narrowness of the stream further restricted dispersal. For instance, when a mandible or innominate lodged crossways at the bottom of the channel, it served to trap smaller elements coming downstream later. As expected, bone density, size (weight), and morphology are major characteristics of bone invoked to explain flume study results. Factors that influence transport and accumu-

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Table 10.5 Hydraulic Transport Groups Comparing Voorhies and Boaz and Behrensmeyer Transport Group

Voorhies

Boas and Behrensmeyer

I (highly transportable)

Scapulaa Phalangesa Ulnaa Ribs Vertebrae Sacrum Sternum

Talus Metatarsals I and IV Proximal ulna Proximal humerus Vertebra T12 Acetabulum Calcaneus Cuboid Sacrum Cranium

II (intermediate)

Femur Tibia Humerus Metapodial Pelvis Radius Scapulaa Ramusa Phalangesa Ulnaa

Mandible with teeth Vertebra T1 Proximal tibia Proximal radius

III (lag)

Skull Mandible Ramusa

Cranial vault pieces Hemi-mandible Mandible without teeth Molar Incisor Patella Proximal radius Distal radius Rib Atlas Proximal femur Scapular fragment Clavicle

a

Appears in more than one category.

Sources: Data from Voorhies, M., Contributions to Geology, 1969; Boaz, N.T. and Behrensmeyer, A.K., American Journal of Physical Anthropology, 45(1), 53–60, 1976.

lation of bone by water include the following: shape, breakage, orientation relative to flow, and irregularities of the substrate including vegetation (Potts, 1988). The condition of a bone or body unit and its effect on buoyancy are significant variables affecting the dispersal of bones in moving water (Dodson, 1973). Throughout the postmortem interval the density spectrum of body units and bones is affected by loss of soft tissue, loss of grease and moisture content, as well as the weathering state of a bone. Flume experiments to date have assumed single bone transport, not the transport of whole carcasses or units of bones with varying amounts of soft tissue. Hence, they have little practical relevance for forensic cases with short postmortem intervals. The time of exposure between death and disarticulation plays a significant role in the fate of remains in water.

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Table 10.6 Elements

Comparison of Experimental Conditions in Fluvial Transport Studies of Skeletal

Experimental Conditions

Voorhies (1969)

Boaz and Behrensmeyer (1976)

Dodson (1973)

Stream table substrate Gradient Time of bone placement Taxon State of bone Number of trials

Fine sand 0.9 in./foot Before water Coyote, sheep ? 15/specimen

Coarse sand 31 cm/sec After water Human ? ?

Medium sand 6.35 in./sec Before water Mouse, toad, frog Fragmented, weathered 10/specimen

Sources: Data from Voorhies, M., Contributions to Geology, 1969; Boaz, N.T. and Behrensmeyer, A.K., American Journal of Physical Anthropology, 45(1), 53–60, 1976; Dodson, P., Contributions to Geology, 12(1), 15–19, 1973.

Bone Modifying Effects of Water Environments Taphonomic factors in water environments include abrasion, disarticulation, bioerosion, dissolution, encrustation, fragmentation, spatial orientation, decomposition, and scavenging (Table 10.7) (Parsons and Brett, 1991; Sorg et al., 1997). Current-driven, sediment-laden water tends to abrade, or round off, projections of bone (e.g., muscle markings and articular ends). Abrasive modification of bone can result when bones are exposed to particles suspended in moving water or when the skeletons themselves are moved relative to other particles or objects (Parsons and Brett, 1991). The ability of sediments in energetic water flow to abrade or round off articular ends and muscle markings has also been noted by Potts (1988). Such transport or positional abrasion can be generalized or focal. Abrasion can play a significant role in interpretation of taphonomic history as reported by Brooks and Brooks (1997). Generalized sediment abrasion can obscure signs of trauma, such as gunshot or stab wounds. High-energy currents or surf in conjunction with barriers, rocky bottoms, or rocky shores can cause bones to break apart along natural lines of weakness or produce defects from blunt or sharp force, possibly leading to fragmentation, dispersal, and loss (Brooks and Brooks, 1997; Nawrocki et al., 1997). When such damage occurs early in the postmortem period, the fracture or puncture margins may be impossible to differentiate from perimortem trauma. In both forensic and archaeological settings, marine organisms are commonly seen encrusting bones. In general, these creatures settle on hard surfaces above the water-sediment line. When properly identified in the early postmortem period, barnacles can suggest, or at least confirm, the postmortem interval and location (Skinner et al., 1988; Sorg et al., 1997). Caution must be used, however, due to environmentally dependent variations in growth patterns, even within species. Other encrusting epifauna are coralline algae, foraminifera, coelenterates, surpulid worms, bryozoans, barnacles, and some mollusks (Parsons and Brett, 1991). Corrosion or pitting of skeletal surfaces is termed dissolution. Such damage may occur in environments with high salinity, low temperature, or active bioturbation. These alterations have been observed in human remains recovered from near-coastal settings as early as during the first year after death (Sorg et al., 1997). Bioerosion results from boring, grazing, or shelterseeking organisms and often co-occurs with dissolution (Parsons and Brett, 1991). Grazing fish can leave telltale scrape marks from their mouth plates. Radula scrapes of gastropods (sea snails), which are carrion feeders, can create significant damage, particularly to long bone ends. Although some radula signatures can be identified microscopically, the majority of gazing organisms simply grind away substrate without leaving characteristic signatures.

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Table 10.7 Taphonomic Modification in Water Environments Modification

Implications

Abrasion

Wearing-down of bone due to sediment action, particularly in highenergy settings.

Encrustation

The overgrowth of hard skeletal elements by other organisms. Indicates exposure above the sediment–water interface, encrustation can specify environment and may be an indicator of time passage.

Bioerosion

Corrosive processes by organisms. The most pervasive causes of degradation are boring or grazing. Bioerosion erases surface features, but leaves traces made by the organism. Patterns and processes of bioerosion vary among environments due to the distribution of bioeroders, energy levels, and other habitat differences.

Dissolution

Skeletal remains are often in equilibrium with surrounding waters, but changes in chemical conditions can cause skeletons to dissolve. Dissolution represents fluctuations in temperature, pH or PCO2 in calcium carbonate skeletons.

Erosion

Broken edges of skeletons become rounded due to either dissolution or abrasion of the exposed surface. The processes that control edge erosion are not fully known, but are probably a combination of dissolution, abrasion, and bioerosion. Rounding may give a relative estimate of time since breaking.

Decomposition

Decomposition attracts scavengers in phases and increases the probability of soft tissue loss. Its presence generally signifies the presence of oxygen and above-freezing temperatures.

Disarticulation, fragmentation

Separation of body units increases the probability of transport and influences the type of transport possible. Dispersal resulting from disarticulation may change the accessibility of soft tissue or bone to other taphonomic processes.

Scavenging

Consumption by other organisms decreases the probability of preservation and may increase dispersal and fragmentation. The presence of some scavengers may attract others.

Spatial orientation

Position exposes particular surfaces to taphonomic agents and processes; it may enhance or impede transport by wave or current action.

Sources: Adapted from Parsons, K.M. and C.E. Brett, in The Processes of Fossilization, edited by S.K. Donovan, Columbia University Press, New York, 1991, pp. 22–65; Sorg, M.H. et al., in Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, CRC Press, Boca Raton, FL, pp. 1–9.

Recovery Issues Forensic remains from aqueous environments present significant challenges for both recovery and taphonomic interpretation. Most floating or beached remains are discovered by accident by people involved in fishing, boating, or shoreline activities (Boyle et al., 1997) and are frequently recovered by first responders, law enforcement, or forensic personnel. Many submerged remains, on the other hand, are discovered when they are recovered by accident in fishing nets (Sorg et al., 1995; 1997). When recovery is done purposefully as part of a forensic investigation, divers or other recovery personnel should be instructed to gather data about the immediate surrounding, including exact location and depth, bottom type, water currents and, whenever possible, temperature and water chemistry. Flora and fauna associated with the remains should be

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recovered. Knowledge about the taphonomic setting will be useful in interpreting modification of soft tissue and bone and understanding distribution pattern, attrition of elements, scavenger changes, and differentiation from trauma.

Conclusion The study of human remains in aqueous contexts offers enormous potential for exchange between forensic taphonomy and archaeology/paleontology. Water is perhaps the most ubiquitous taphonomic agent transporting, modifying, and accumulating remains. Yet, the hydrodynamics and chemistry of decomposing carcasses, carcass units, and bones in water are poorly understood for either archaeological or forensic assemblages. Actualistic observations of carcasses in water are rare. The majority of studies involving fluvial transport deal with behavior of single bones, studies which have sought to understand assemblages of fluvially accumulated skeletal elements. This represents an unfortunate lapse, because the depositional fate of the majority of forensic remains in water is inextricably bound to their hydraulic behavior as carcasses, their loss of soft tissue and subsequent disarticulation from the body, and the taphonomic environment in which these processes occur. Research gaps should be bridged not only by the use of animal proxies in experimental contexts, but also by careful documentation of data from forensic cases, particularly those in which details about the postmortem period become available.

Acknowledgment We acknowledge the assistance of graphics artist Megan Abbott-Moore.

References Adelson, L. 1974 The Pathology of Homicide, Charles C Thomas, Springfield, IL. Allison, P.A. and D.E.G. Briggs 1991a The taphonomy of soft-bodied animals. In The Processes of Fossilization, edited by S.K. Donovan, pp. 120–140. Belhaven Press, London. 1991b Taphonomy of nonmineralized tissues. In Taphonomy: Releasing the Data Locked in the Fossile Record, edited by P.A. Allison and D.E.G. Briggs, pp. 25–70. Plenum Press, New York. Behrensmeyer, A.K. 1982 Time resolution in fluvial vertebrate assemblages, Paleobiology 8:211–227. Berryman, H.E., J.O. Potter, and S. Oliver 1988 The ill-fated passenger steamer Sultana: an inland maritime mass disaster of unparalleled magnitude, Journal of Forensic Sciences 33(3):842–850. Boaz, N.T. and A.K. Behrensmeyer 1976 Hominid taphonomy: transport of human skeletal parts in an artificial fluviate environment, American Journal of Physical Anthropology 45(1):53–60. Boyle, S., A. Galloway, and R.T. Mason 1997 Human aquatic taphonomy in Monterey Bay Area. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, CRC Press, Boca Raton, FL, pp. 1–9.

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Brooks, S. and R.H. Brooks 1984 Effects on bone of abrasive contents in moving water. Abstract from the First International Conference on Bone Modification, Carson City, NV, August 1984. 1997 The taphonomic effects of flood waters on bone. In Forensic Taphonomy: The Postmorem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 553–558. CRC Press, Boca Raton, FL. Charney, M. and C.G. Wilber 1980 The Big Thompson flood. American Journal of Forensic Medicine and Pathology 1(2):139–1444. 1984 The Big Thompson flood. In Human Identification: Case Studies in Forensic Anthropology, edited by T.A. Rathbun and J.E. Buikstra, pp. 107–112. Charles C Thomas, Springfield, IL. Cotton, G.E, A.C. Aufderheide, and V.G. Golschmidt 1987 Preservation of human tissue immersed for five years in fresh water of known temperature. Journal of Forensic Sciences 32(4)1027–1037. Dechant-Boaz, D. 1982 Modern Riverine Taphonomy: Its Relevance to the Interpretation of Plio-Pleistocene Hominid Paleoecology in the Omo Basin. Ph.D. dissertation, University of California, Berkeley. Ann Arbor University Microfilms (no. 8312762) (unpublished). Dilen, D.R. 1984 The motion of floating and submerged objects in the Chattahoochee River, Atlanta, GA. Journal of Forensic Sciences 29(4):1027–1037. Dix, J.D, 1987 Missouri’s lakes and the disposal of homicide victims, Journal of Forensic Sciences 32(3):806–809. Dodson, P. 1973 The significance of small bones in paleontological interpretation, Contributions to Geology 12(1):15–19. Donoghue, E.R. and S.C. Minnigerode 1977 Human body buoyancy: a study of 98 men, Journal of Forensic Sciences 22(3):573–579. Ebbesmeyer, C.C., J.M. Cox, and B.R. Salem 1991 1875 Floatable wreckage driven inland through the Strait of Juan de Fuca. Proceedings of the Puget Sound Research Conference, 1:75–85. Puget Sound Water Control Authority, Washington. Ebbesmeyer, C.C. et al. 1991 Eddy induced beaching of floatable materials in the eastern Strait of Juan de Fuca. Proceedings of the Puget Sound Research Conference, 1:76–98. Puget Sound Water Control Authority, Washington. Ebbesmeyer. C.C. and W.D. Haglund 1994 Drift trajectories of a floating human body simulated in a hydraulic model of Puget Sound, Journal of Forensic Sciences 39(1):231–240. Giertsen, J.C. and I. Morild 1989 Seafaring bodies, American Journal of Forensic Medicine and Pathology 10(1):25–27. Haglund, W.D. 1993 Disappearance of soft tissue and the disarticulation of human remains from aqueous environments, Journal of Forensic Sciences 38(4):806–815. Hanson, B.C. 1980 Fluvial taphonomic processes: models and experiments. In Fossils in the Making: Vertebrate Taphonomy and Paleobiology, edited by A.K. Behrensmeyer and A. Hill, pp. 156-181. University of Chicago Press, Chicago, IL.

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Haynes, G. 1980 Prey bones and predators: potential ecologic information from analysis of bone sites, Ossa 7:75–97. Hill, A.P. 1975 Taphonomy of Contemporary and Late Cenozoic East African Vertebrates. Ph.D. dissertation, University of London, U.K. 1979 Disarticulation and scattering of mammal skeletons, Paleobiology 5(3):261–274. Kahana, T. et al. 1999 Marine taphonomy: adipocere formation in a series of bodies recovered from a single shipwreck, Journal of Forensic Sciences 44(5):897–901. London, M.R., F.J. Krolikowski, and J. H. Davis 1997 Burial at sea. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 615–622. CPR Press, Boca Raton, FL. Martin, R.E. 1999 Taphonomy: A Process Approach. Cambridge University, Cambridge, U.K. McCullough D. 1968 Johnstown Flood, Simon & Schuster, New York. Nawrocki, S.P., J.E. Pless, D.A., Hawley, and S.A. Wagner 1997 Fluvial transport of human crania. In Forensic Taphonomy: The Postmorem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 529–552. CRC Press, Boca Raton, FL. O’Brien, T. G. 1997 Movement of bodies in Lake Ontario. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W. D. Haglund and M.J. Sorg, pp. 559–565. CRC Press, Boca Raton, FL. Parsons, K.M. and C.E. Brett 1991 Taphonomic processes and biases in modern marine environments: an actualistic perspective of fossil assemblage preservation. In The Processes of Fossilization, edited by S.K. Donovan, pp. 22–65. Columbia University Press, New York. Payne, J.A. and E.W. King 1972 Insect succession and decomposition of pig carcasses in water, Journal of the Georgia Entomological Society 7:153–162. Potts, R. 1988 Early Hominid Activities at Olduvai, Aldine de Gruyter, New York. Rathbun, T.A. and B.C. Rathbun 1984 Human remains recovered from a shark’s stomach in South Carolina, Journal of Forensic Sciences 29(1):269–272. Schäfer, W. 1972 Ecology and Paleocology on Marine Environments, edited by G. Craig and translated by I. Ortel, p. 22. University of Chicago Press, Chicago, IL. Schafer, W. 1978 The Ecology and Paleoecology of Marine Environments. University of Chicago Press, Chicago, IL. Seilacher, A., W.E. Reit, and F. Westphal 1985 Sedimentalogical, ecological and temporal patterns of fossil lagerstatten. In Extraordinary fossil biotas: Their ecological and evolutionary significance. Philosophical Transactions of the Royal Scoeity of London 311:5–23. Simonsen, J. 1977 Early formation of adipocere in temperate climate, Medicine Science and Law 17(1):53–55.

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Simpson, K. 1965 Taylor’s Principles and Practices of Medical Jurisprudence, Vol. 1, 12th ed., Churchill Livingston, London, p. 379. Skinner, J.B. and S.C. Porter 1987 Physical Geology, p. 240. John Wiley & Sons, Inc., New York. Skinner, M.F., J. Duffy, and D.B. Symes 1988 Repeat identification of skeletonized human remains: A case study. Journal of the Canadian Society of Forensic Sciences 21(3): 138–141. Snyder, L. 1972 Homicide Investigation, 2nd ed., p. 218, Charles C Thomas, Springfield, IL. Sorg, M.H., J.H. Dearborn, K.G. Sweeney, H.F. Ryan, and W. C. Rodriguez 1995 Marine taphonomy of a case submerged for 32 years. Proceedings of the American Academy of Forensic Sciences 1:156–157. Sorg, M.H. et al. 1997 Forensic taphonomy in marine contexts. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 1–9. CRC Press, Boca Raton, FL. Spitz, W.U. (Ed.) 1993 Spitz and Fisher’s Medicolegal Investigation of Death: Guidelines for the Application of Pathology to Crime Investigation, 3rd ed. Charles C Thomas, Springfield, IL. Spitz, W.U. and R.S. Fisher 1980 Medicolegal Investigation of Death: Guidelines for the Application of Pathology to Crime, 2nd ed., p. 360, Charles C Thomas, Springfield, IL. Teather, R.G. 1994 Encyclopedia of Underwater Investigations, p. 6, Best Publishing, Flagstaff AZ. Timperman, J. 1991 How some medicolegal aspects of the Zeebrugge Ferry disaster apply to the investigation of mass disasters, American Journal of Forensic Medicine and Pathology 12(4):286–290. Todd, L.L. and G.C. Frison 1986 Taphonomic study of the Colby Site mammoth bones. In The Colby Site Mammoth Bones, pp. 27–90. Albuquerque, NM. Toots, H. 1965 Sequence of disarticulation in mammalian skeletons, Contributions in Geology 4(1) January: 37–39. University of Wyoming Press, WY. Walker, A. and R. Leakey (Eds.) 1993 The Nariokotome Homo Erectus Skeleton, Harvard University Press, Cambridge, MA. Weigelt, J, 1927 Recent Vertebrate Carcasses and their Paleobiological Implications, translated by Judith Schaefer, University of Chicago Press, Chicago, IL. Western, J. 1985 Discussions. In L’environment des Hominides au Plio-Pleistocene, pp. 402–405. Masson, Paris. White, T.D. 1988 The comparative biology of robust Australopithecus: clues from context. In Evolutionary History of the Robust Australopithecines, edited by F.E. Grine, pp. 449–483. Aldine de Gruyter, New York. Voorhies, M. 1969 Taphonomy and population dynamics of an early Pliocene vertebrae fauna, Knox County, Nebraska, Contributions to Geology, Spec. Paper, No. 1., pp. 1–69. University of Wyoming Press, WY.

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Floating Remains on Pacific Northwest Waters* CURTIS C. EBBESMEYER WILLIAM D. HAGLUND

11

The dust on the sea is the grave of a ship. It is only a temporary marker, but it is an indelible one to those who have seen it. Dust on the Sea Edward L. Beach (1972, p. 7)

Contents Introduction Tale of Two Ferries Case #1: Collision of the Pacific and the Orpheus Case #2: The Ill-Fated Clallam Storms Drive Debris Inland Tidal Eddies Concentrate Wreckage Three Puget Sound Cases Involving Individuals Case #3: An Accidental Fall from a Ferry in Georgia Strait Case #4: Jumper from the Narrows Bridge, Southern Puget Sound Case #5: Deception Pass: The Body in the Nylon Suitcase Discussion Acknowledgments References

* This chapter contains adaptations from three previously published papers: Ebbesmeyer et al. (1991a,b) and Ebbesmeyer and Haglund (1993).

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Figure 11.1 Map of the waters of Juan de Fuca Strait and locations mentioned in text (adapted from Ebbesmeyer et al., 1991a). Illustration by Megan Abbott-Moore. With permission.

Introduction A huge gap divides oceanography and forensics because specialists in these fields are rarely familiar with the other discipline. Consequently, little is known about where human bodies drift on the sea. This chapter seeks to bridge that gap and describes studies of the inland drift of bodies and debris after two maritime disasters in the vicinity of the Pacific Northwest’s Juan de Fuca Strait. The incidents are the 1875 sinking of the steamer Pacific after it collided with the clipper Orpheus, and the 1904 sinking of the ferry Clallam. Both tragedies involved vessels carrying a large number of passengers and resulted in great loss of life. For weeks afterward searches were made for bodies and debris. The last three cases illustrate patterns of movement on two other areas of Puget Sound. These five studies provide important scientific implications that deviate from traditional studies of floating objects for three reasons: (1) searches for objects floating at the sea surface are rarely done in oceanography because of the expense involved; (2) drifting objects tracked by satellite are tethered to underwater sails (drogues) usually placed at depth in the Strait, and thus do not necessarily represent the movement of water and bodies floating at the sea surface; and (3) recovery of drift bottles and cards may be influenced by population density along selected segments of the shoreline. The potential applications of this information for forensic death investigators include the ability to set geographic and time limits for searches; determine the potential origin of remains found floating or beached, and confirm and correlate information regarding entry into the water and sightings of remains. Turned on its side, a map of the Pacific Northwest waters resembles a tree with its roots in the coastal Pacific Ocean (Figure 11.1). Its trunk is Juan de Fuca Strait, Georgia Strait is the northern foliage, and Puget Sound is the southern overhang. The eastern Strait is a junction between several estuarine reaches (Haro Strait, Rosario Strait, Admiralty Inlet, western Strait of Juan de Fuca). Each of these regions has distinctly different current patterns. Strong tidal eddies are present in a number of other junctions [off Alki Point, near The Narrows (see discussion of case 4, Figure 11.7), and the five-way junction south of Dana Passage].

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Tale of Two Ferries Historical accounts of maritime disasters can provide valuable insights into the fate of floating debris and human remains. The first ferry account in this chapter relates the collision between the paddle wheeler Pacific and the clipper Orpheus off the Washington State coast. It took place during the evening November 4, 1875, and demonstrates how storm-related reversed surface currents in Juan de Fuca Strait transported bodies and wreckage as far as 100 miles inland. In the second account, tidal eddies dispersed the debris from the ferry Clallam, sunk on January 8, 1904, by a violent storm off Victoria, Canada, to specific shorelines around the head of Juan de Fuca Strait. Case #1: Collision of the Pacific and the Orpheus The illustrious career of the steam-powered paddle wheeler Pacific began with her launching on September 24, 1850 in Buffalo, New York (Figure 11.2a). On her maiden voyage, the 226-foot long, 876-ton vessel logged 360 miles in 24 hours, a record run for a steamer at that time. In her 5th year of service, on a run between Nicaragua and New York, a cholera outbreak killed 45 of 800 passengers. On July 18, 1861, on a trip down the Columbia River from Portland to Astoria, the notoriously strong winds in the Columbia Gorge area grounded and sank the side-paddle wheeler near Coffin Rock. No casualties resulted and soon she was raised and repaired. By 1872, after 22 years of service, she quietly decayed for 3 years on the mud flats in San Francisco Bay (Bailey, 1967). However, in 1875, the new owners unwisely pressed the aged vessel back into service in order to ferry miners to San Francisco from the lucrative Cassiar gold fields of British Columbia. November 4, 1875, found the Pacific southbound to San Francisco from Victoria with 250 to 300 passengers aboard. During the day the weather was moderate, although by evening, the wind had churned up the oncoming seas. Rounding Cape Flattery, at the northwestern corner of Washington Territory (now Washington State) the Pacific, in an apparently minor accident, collided with the northbound clipper ship Orpheus, and sank off the mouth of Juan de Fuca Strait. The clipper Orpheus (Figure 11.2b) was 6 years newer than the Pacific. The Rice and Mitchell Company launched the medium clipper at Chelsea, Massachusetts on March 1, 1856. With an overall length of 200 feet, the 1272-ton clipper ship sailed the Pacific Ocean, setting record times. It was on her second trip to Puget Sound from San Francisco that the Orpheus collided with the Pacific, losing her foretop mast and main top gallant mast, with all starboard rigging. Her Captain, Sawyer, made for land but mistook the newly installed light on Cape Beale for the older light at Tatoosh Island. The clipper went aground, becoming a total wreck. The magnificent vessel, once valued at $20,000 to $30,000, was scrapped for $380. Though the collision had damaged Orpheus only slightly, the Pacific sank within 20 minutes. Although carrying lifeboats for 160 persons, the ship sank so quickly that only one lifeboat with 15 women and 6 men could be launched. Unfortunately, it slammed against the steamer drowning most of those on board. The next day, a handful of survivors drifted on floating wreckage. Of these, passenger H.F. Jelly died of exposure a few days after being rescued. The other was quartermaster Neil Henley, a second survivor, a hardy Scotsman, who lived another 60 years, reaching the age of 85.

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(a)

(b)

(c)

Figure 11.2 (a) The steamship Pacific. (b) The clipper Orpheus from painting. (c) The Pacific seen listing against Yesler Wharf. (Courtesy of the Museum of Industry and History, Seattle, WA.)

The massive effect of the slight collision might be attributed to the fact that the Pacific received the blow on her Achilles heel, near the buff of her bow, where the bracings were too far apart (~18 in.). In steamers, frames were separated from 12 to 20 in., whereas, in sailing vessels of the day, it was usually never more than 3 to 6 in.; the timbers of steamers were also smaller and their whole construction lighter, from the water mark up. According

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to other speculation, this seemingly minor collision may have just been the last in a cascade of events that lead to the sinking. Despite intensive court trials, theories persist as to why the Pacific sank from a seemingly slight blow. One theory attributes the sinking to her instability in the water. In a photo taken in Seattle in the year of the collision, she can be seen listing against Yesler Wharf (Figure 11.2c). Shortly before departing Victoria on the day of the collision, water had been poured into the lifeboats in order to trim the overcrowded ship. This apparently occurred because more than 200 of the 600 tons of coal stored below deck had shifted. A few months before her last voyage, the Pacific was thoroughly overhauled and critically inspected. A few days prior to sailing, she was in dry-dock to be cleaned. The inspector of hulls carefully examined her bottom and did not hesitate to say that she was in perfectly seaworthy condition. However, suspicions surrounded the premature retirement of the Pacific prior to the Cassiar gold fever, when the vessel had lain for years in the company’s San Francisco “bone yard” (Bailey, 1967). According to carpenters who refurbished the ship in 1875, she had substantial dry rot and was structurally weak at the time of the collision. An explosion during her sinking, inferred by the scalded condition of one of the recovered bodies, coupled with dry-rotted wood, may explain the extensive debris. Parts of the Pacific’s frame that came ashore at Foul Bay were so decayed that beachcombers picked them to pieces with their fingers, the wood about bolt heads was gone and bolts played in their sockets. The most probable scenario for what happened after the collision is that water quickly poured in through the bow, destabilizing the Pacific. Afterward, she apparently broke in half, much like the RMS Titanic. Though a number of attempts have been made to salvage the estimated $178,000 in gold aboard the Pacific, accurate measures of the latitude and longitude of the collision remain speculative because oceanographic reconstructions of the winds and coastal currents have not yet been performed. Official inquiries found that the clipper Orpheus’ captain disregarded the universal rule of navigation in putting his helm to starboard, then to port, then to starboard again, and then again to port, repeatedly changing his course so that the steamer could not anticipate his movements and thereby avoid her. He countered, saying that the steamer had given, not received, a blow and no one aboard the clipper had any idea that damage had been done to the Pacific. The collision seemingly minor, the Orpheus’ crew occupied themselves with repair of her riggings, and then sailed on 2 hours after the collision. It has been rumored that the Orpheus’ Captain was the scapegoat in a cover-up that remains mysterious to this day. Some would lay the blame at the feet of the owners and inspectors of the Pacific. The condition of the recovered wreckage was at variance with the report of the Inspector of Hulls who stated that the Pacific “…was in perfectly seaworthy condition” (Annual Report of the Supervising Inspector of Hulls, 1876:39). The time of the collision was shortly after 9:30 p.m., according to testimony from Captain Sawyer of the Orpheus. At the time of the accident, Captain Jefferson D. Howell, brother-in-law to Jefferson Davis, former president of the Confederate States during the Civil War, reckoned that his ship lay 15 to 20 miles offshore. Other accounts place the collision closer to shore. Testimony of H. F. Jelly and Neil Henley, confirmed by the watches found on two bodies, indicated that the Pacific sank within 20 to 30 min after the collision, carrying down with her all aboard except a few persons who floated off on wreckage.

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Table 11.1 Chronological Order of Recoveries and Sightings of Survivors, Bodies, and Prominent Debris from the Steamship Pacific Date 1875 Description of Sighting or Victims

Location of Sighting or Recovery

Nov. 6

Rescued by vessel Awkright

Nov. 10

Survivor Jelly and great amount of wreckage sighted Body of unidentified womana and great quantity of debris Bodies of Keller,a Vining,a and an unidentified stewarda Large mass of debris

Nov. 11 Nov. 12 Nov. 13 Nov. 13 Nov. 13 Nov. 13 Nov. 13

Bucket rack Body of Jonesa recovered Body (unidentifieda) Bodies of Crowley and unidentified Negroa Part of a life boat Horse Body of Helmut

Nov. 14

Ceiling beam written on by passenger Moody and body (McIntyrea) Light wreckage

Found off Victoria Recovered near Neah Bay Sighted in the Eastern Strait Recovered Found near Victoria Found floating off Slip Point Recovered floating 12 miles west of Race Rock at mid-channel Recovered between Sooke and Becher Bay

Nov. 7 Nov. 8

Nov. 14 Nov. 18 Nov. 19 Nov. 22 Nov. 22 Nov. 25 Nov. 27 Nov. 29 Nov. 29 Dec. 10

Sighted off Neah Bay by vessel Awkright Recovered in the vicinity of Neah Bay Sighted near Race Rock by vessel Wolcott

Sighted floating from Point Wilson to Freshwater Bay Bodies of Sullivan,a Farrell Recovered Wreckage Floating off Elwah River Body of Hastings Recovered on Ediz Hook Rudder of SS Pacific Found on Bentinck Island Body of Palmer Recovered on San Juan Islands Some wreckage Sighted just south of Cape Flattery Piece of bucket Recovered at Fort Bellingham Body of (Chinese) and Timbers marked 30 and 41 Recovered at Neah Bay Wreckage Sighted off Hoko River Trunk belonging to passenger Palmer Found at Fort Dungeness

Presence of life preserver according to newspaper account. Note: Resulting from the November 4 collision between the SS Pacific and CS Orpheus. Locations are shown in Figure 11.3 by day of discovery in November of 1875 and December 10 (from reports published in the Daily British Colonist and supported by eight other Pacific Northwest newspapers of the time).

a

Source: Adapted from Ebbesmeyer, C.C. et al., Puget Sound Research ’91 Proceedings, Puget Sound Water Quality Authority, Olympia, Washington, 1991.

Whereas the Orpheus’ crew safely made it to land, all but one of those aboard the Pacific perished. She did not go down quietly, leaving an enormous floating debris field. Ironically, the currents carried the bodies and other debris back towards Victoria, her last port of call, strewing them along the shorelines for 100 miles as detailed in local newspaper accounts (Table 11.1 and Figure 11.3). The resulting debris field from the Pacific provides a dramatic example of bodies and debris driven inland by storms. Case #2: The Ill-Fated Clallam Whereas the Pacific wrecked in her third decade of service, the ferry Clallam perished in her maiden year (Figure 11.4a). In June 1903, at Tacoma, Washington, the 167-foot Clallam

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Figure 11.3 Location and date of recovery or sighting of the SS Pacific wreckage. Notation: hatching, offshore distance at time of collision between the SS Pacific and the clipper ship Orpheus (the north–south position of the wreck is considered to be speculative); dashed line, approximate track of the clipper ship Orpheus from the site of the collision to her grounding near Tzartus Island in Barkley Sound. Solid lines, approximate trajectories for the two survivors (Jelly and Henley). Parallel lines indicate sightings of the main mass of wreckage by the vessels Awkwright and Wolcott. Corkscrew indicates line of debris between Cape Flattery and Victoria reported by George Fox to George Davidson. Staircase pattern eastward from Port Angeles, scattered light wreckage. Dot, recovery of survivors or bodies; +, location of prominent debris; number with dot or +, date sighted or recovered in November 1875 (one sighting, December 10). (Illustration by Megan Abbott-Moore. With permission.)

slid broadside from Heath Shipyard’s gangways, an ill-fated omen according to mariners witnessing the ship builder’s daughter christening the new ferry. Just 6 months later, at noon on Friday, January 8, 1904, the Clallam departed Port Townsend (on the U.S. side of Juan de Fuca Strait) for a routine 3-hour, 20-mile-run to Victoria on Canada’s Vancouver Island. Shortly after departing, the Clallam encountered a 54-mile-per-hour gale. At mid-Strait, 10 miles from shore, she began taking on water through deadlights (portholes) located only 18 in. above the port-side waterline facing into the gale. Within 3 to 4 miles of journey’s end, the crew managed to staunch the inflow of water entering the deadlights. Nevertheless, enough water flooded in to reach fireman Maddock’s shoulders and snuff out the boilers. Without power, the pumps failed. At the mercy of currents, bucket brigades and hand pumps madly flailing, the Clallam drifted out of the sight of shore-bound onlookers who witnessed the mayhem. Captain Roberts, thinking the Clallam likely to sink at any moment, ordered all women and children overboard in three lifeboats manned by carefully picked men to row them the short distance to shore. It was impossible to lower the remaining three lifeboats on the weather side of the ship. Men watched in horror as a few hundred yards away gigantic waves swamped the lifeboats, drowning the women and children. Survivors told later of their heartbreak. S.E. Bolton, for example, who was returning home from his honeymoon after just 10 days of marriage, watched his wife drown. Thomas Sullins, a mine owner, lost his wife and three children. By this time, winds and tides had carried the Clallam east to a position off Trial Island near Clover Point, just 20 minutes from Victoria. Through the afternoon and evening, crew and passengers battled to keep the Clallam afloat by jettisoning 2 tons of coal, oilcakes,

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(a)

(b)

Figure 11.4 (a) The steamer Clallam. (b) Steamer Clallam’s top foredeck lying on the beach

at Sidney Spit, Vancouver Island, British Columbia. (Courtesy of the Museum of Industry and History, Seattle, WA.)

and cargo. Finally, midway between Smith and San Juan islands, the tug Holyoke got a tow line on the Clallam. Nevertheless, in the darkness, the Holyoke’s captain couldn’t discern the Clallam’s waterlogged condition. After 12 miles, the Holyoke, herself in peril, cut the towline. The Clallam’s bow rose out of the water; the men remaining on board ran forward, clinging to the railings. Among them was Captain Robert, who along with others was swept overboard by a monstrous wave. On sinking, the upper two decks detached. Of the 89 aboard, at least 55 passengers and crew perished. Over the next 13 days, searchers recovered 32 bodies (Table 11.2) and wreckage including the whole foredeck (Figure 11.4b). Storms Drive Debris Inland The great loss of human life resulting from the sinkings of the Pacific and Clallam motivated intensive searches on both occasions. Results of these searches provide two rare instances in which the destinations of floating objects were intensively traced in inland waters. The Pacific’s debris provides the only data on floatable objects driven inland by coastal storms through Juan de Fuca Strait. When combined, the Clallam’s and Pacific’s debris show that most of the bodies were found along only 10% of the 277 miles of the eastern Strait’s

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Table 11.2 Chronological Order of Sightings and Recovery of Clallum Passengers and Debris during January 1904 Date 1904

Victim No.

Jan. 9

1–5

Jan. 10

Description of Sighting or Victimsa

Location of Sighting or Recovery Recovered 1/2 mile from floating pilot house near site of sinking

6

Captain Livinston,b William Buchanan Gibbons,b W.H. Hicks,b unidentified elderly male,b unidentified male,b Louise Harrisb,c,d

Jan. 10

7

Mrs. Thomas Sullinsb,c

Jan. 10 Jan. 10 Jan. 10 Jan. 10

8 9 10, 11 12–15

Jan. 10

16

Jan. 10

17–21

Miss Galletlyb,c Ethel Diproseb Alex Harvey,b unidentified femaleb N. P. Shaw,b Miss Gill,b C. H. Joy,b Miss Minnie Murdockb Peter LaPlanteb

Jan. 17 Jan. 17 Jan. 19

29 30

Captain Thomson,b W.B. Gibbons,a,b Eugene Hicks,a,b Archie Hudson,a,b C.F. Johnsona,b Upper deck, and sacks of oilcakese Wreckagee William Cherretf Life boat no. 1g Wreckageg Col. Charles W. Thompsonh Harvey Searsh R. G. Campbellh E. Lockwood,h Guy L. Daniels,h A.K. Princei W. F. Rocklidgei Wreckagei Homer S. Swaneyj

Jan. 22 ??

31 32

Unidentified femalek Bruno Lehman

Jan. 12 Jan. 12 Jan. 13 Jan. 14 Jan. 13 Jan. 15 Jan. 15 Jan. 16

a b c d e f g h i j k

22

23 24 25 26–28

Recovered from lifeboat 2 miles east of Clove Point, off Victoria Recovered off Beacon Hill alongside life boat no. 1 Recovered, Clover Point Recovered, Beacon Hill Recovered off Williams Head Recovered 1/2 mile from floating pilot house between Race Rock and Brochie Ledge by Tug Mary Reynolds Recovered between Victoria and New Westminster Recovered near site of sinking (one body wedged between stanchions)

Sighted as far as San Juan Island Recovered off Clover Point Sighted, off Beacon Hill Sighted, along north side of San Juan Island Recovered off D’ Arcy Island Beach Recovered near Brochie Ledge Recovered near Albert Head Recovered, floated into Esquimalt Harbor Recovered at the end of Angeles spit Sighted, near Port Angeles Recovered 1 mile off Dungeness Light in the straits Recovered off Ediz Rock Recovered, location not stated

Presence of life preserver according to newspaper account. Seattle Post Intelligencer, January 10, 1904. Seattle Post Intelligencer, January 11, 1904. Seattle Times, January 12, 1904. Seattle Post Intelligencer, January 13, 1904. San Juan Islander, January 14, 1904. Seattle Times, January 14, 1904. Seattle Times, January 16, 1904. Seattle Times, January 18, 1904. Seattle Post Intelligencer, January 20, 1904. Seattle Post Intelligencer, January 23, 1904.

shoreline. By identifying the pattern of floating bodies on particular shores, medical investigators may substantially narrow their searches for bodies and other floating forensic evidence.

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Newspaper accounts provide most of what is known about the debris field and recovery of human remains from these two disasters. To ascertain the quantity and variety of wreckage from the Pacific, nine Pacific Northwest newspapers published between November 6 and December 10, 1875 were examined. According to their reports, the shores throughout Juan de Fuca Strait were thoroughly searched and hefty rewards were offered for the bodies of loved ones. Scant debris was reported outside the Strait, whereas extensive amounts were found inside. Despite diligent searches, only about 6% of the approximately 250 to 300 bodies were recovered. Judging from their well-preserved condition and that most of those who jumped from the ship wore life preservers, it is a fair assumption that they had been floating between the time of the collision and recovery. As they clung to floating pieces of wreckage, two Pacific survivors realized that they drifted inland to the east rather than the expected northward trajectory along the Vancouver Island coast. Jelly, the wreck’s survivor who died shortly after being recovered, drifted close to Cape Flattery, then within a mile of Vancouver Island, and was rescued off Port San Juan. Henley, the Scotsman, drifted within sight of the Cape Beale lighthouse, then close to Vancouver Island, and finally to mid-channel between Pillar Point and Sooke Inlet where he was rescued after 72 hours adrift in a wooden box (Lockley, 1926). Normally, because of river discharge from Georgia Strait and Puget Sound, the sea surface stands higher in the eastern Strait than at the Strait’s mouth to the Pacific Ocean. As a result, the surface water usually flows downhill from east to west. However, during winter storms, low atmospheric pressure and southerly winds along the Pacific Ocean coast often elevate the surface water at the mouth, effectively reversing the sea surface slope along the Strait, thereby pushing surface water counter to the usual direction. Statistical correlations with currents measured in the Strait revealed that coastal winds were of prime importance, with local winds in the Strait itself exerting small influence on the reversed currents (Holbrook et al., 1980). Because of the Earth’s rotation, the water intruding from the coast (known as current reversals and oceanic intrusions) tends to flow inland along the Strait’s southern shore. Oceanographic measurements in the Strait during 1977–1981 showed that reversals may occur in any month (Holbrook et al., 1980, 1983). In winter, 2 to 3 reversals, each lasting 2 to 7 days, typically occur each month (Holbrook et al., 1983). Although most frequent during winter, intrusions also occur in summer, e.g., movements of surface drifters were observed when a low pressure cell lay off the Washington coast during August 23–25, 1978, and trajectories of several drifters abruptly reversed in the western Strait (Cox et al., 1978; Ebbesmeyer et al., 1979; Holbrook et al., 1980; Frisch et al., 1981). The rate of intrusion (eastward surface current speed) was computed from Benjamin’s (1968) equation for the hydraulic flow of a lens of lighter water drawn by gravity inland over denser sea water (Holbrook and Halpern, 1982; Holbrook et al., 1983). Subtracting an assumed mean westward estuarine current of 15 to 20 cm/sec from the theoretical intrusion speed yielded an eastward speed of 25 to 30 cm/sec (12 to 14 nautical miles/day). Information reported in newspapers was sufficient to estimate the speed at which Pacific wreckage drifted inland. Wind drag on the wreckage was neglected because wind observations in the Strait were not available and windage on the wreckage could not be ascertained. Over an 11-day period the largest mass of wreckage drifted inland as reported at three places (Figure 11.3): (1) off Neah Bay during the afternoon of November 7 (vessel Awkwright); (2) north of Port Angeles in the afternoon of November 10 (vessel Wolcott); and (3) in the vicinity of Victoria during November 11 to 14 (many recoveries). These

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Oceanography of Juan de Fuca Strait

Distance (nautical miles)

60

City of Victoria

40

Vessel Wolcott

Survivor Henley

/s

19

20

cm

Survivor Jelly Vessel Awkwright

SS Pacific Collision

-20

4

5

6

7

8 9 10 11 November 1875

12

13

14

Figure 11.5 Distance in miles vs. time in days for sightings of selected wreckage and accounts

of the two survivors from the SS Pacific. The straight line represents a linear regression fit to the observations, where r equals the regression coefficient and speed (19 cm/sec) corresponds to the slope of the regression. Notation: SS Pacific COLLISION, collision of vessels Orpheus and Pacific; JELLY AND HENLEY, the two survivors, AWKWRIGHT & WOOLCOTT, sightings of the main mass of wreckage by the vessels Awkwright and Wolcott; and VICTORIA, frequent reports in the vicinity of Victoria (adapted from Ebbesmeyer et al., 1991a). (Illustration by Megan Abbott-Moore. With permission.)

data, in addition to those of the collision itself and the rescue of the two survivors, were entered on a graph of distance vs. time, and a linear regression was computed (Figure 11.5). The regression slope, equivalent to the wreckage’s average inland speed, explained 92% of the variance (19 cm/sec; 9 nautical miles/day). Some flotsam traveled inland more quickly than the average; on November 8, debris began appearing at Victoria, equivalent to 20 miles per day. If the observations of Pacific wreckage are reliable, the inland speed derived from them should be comparable to speeds derived from modern oceanographic measurements. Floatable oil spilled from the Nestucca barge off Grays Harbor in 1989 and floated inland through Juan de Fuca Strait at 9 miles per day (U.S. Coast Guard, 1989). Reversals transported Pacific wreckage inland at 9 to 20 miles per day and surface drifters, during the summer intrusion of 1978, at 18 miles per day. We see that the intrusion speed derived from the Pacific wreckage is comparable to that derived from a model, an oil spill, and oceanographic field measurements. Tidal Eddies Concentrate Wreckage Observers aboard search vessels on Juan de Fuca Strait reported the Pacific’s debris concentrated in well-defined trails and patches in open water and at specific locations along the shore. Survivor Henley had noticed a large patch as a current reversal carried him inland. George Fox (1910), in a letter to Professor George Davidson, wrote of a 60-milelong line of debris, aimed at the southern end of Vancouver Island, coinciding with the many recoveries of bodies and wreckage. Between 1875 and 1984, more than 16,000 drift objects were released in the waterways approaching eastern Juan de Fuca Strait, including the Pacific Coast, Georgia Strait, and

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Puget Sound. The drifters found within the eastern Strait showed two striking patterns: (1) 73% of the recoveries came from the northern shores vs. 27% from the southern shores; (2) 50% of the recoveries were made in three specific locations totaling about 10% of the eastern Strait’s shoreline (Victoria, San Juan Islands, Dungeness Spit) (Ebbesmeyer et al., 1991a,b). These results were insensitive to the type of drifter, or whether the drifters were actively sought out or were simply found by beach walkers happening upon them. The tidal water volumes feeding the eastern Strait between mean high water and mean lower water are comprised of 76% from Georgia Strait and 24% from Puget Sound. These percentages are within one standard error of those associated with the north–south asymmetry (73% of recoveries on northern shores; 27% on southern shores). This explains why the eddies in the northern areas of the eastern Strait are larger and more vigorous than those in the south. Overlaying the recoveries on maps of surface currents (derived from models and field studies) showed that the localized recovery areas coincided with tidal eddy currents directed onshore. Fourteen prominent tidal eddies in the eastern Strait have been documented with hydraulic and numerical models, as well as with oceanographic field observations (Figure 11.6). Each eddy was observed in the hydraulic model, and nine with field observations and the GF7 numerical model, Georgia Strait–Juan de Fuca version 7, numerical model utilizing 61 tidal constituents (Crean, pers. comm.) (Figure 11.6a). The eastern Strait wreckage reports can be explained by the strength and position of tidal eddies. In Figure 11.6b the ovals circumscribe the approximate extent of the net currents that circulate around the individual tidal eddies shown in Figure 11.6a. Explanations for the observed asymmetries in drifter recovery were found by comparing the recoveries with positions of the tidal eddies (Figure 11.6b). The highest frequency occurred between eddies #2 and #3 in the vicinity of Victoria. The second highest frequency occurred along the outer half of Dungeness Spit in the vicinity of eddy #10. Between eddies #11 and #10 there is a net along-shore flow that sweeps floating objects, or drifters, to Dungeness Spit (Ebbesmeyer et al., 1979). A third concentration occurred between eddies #4 and #5. This comparison suggests that tidal eddies gather drifters and send them ashore where the currents are perpendicular to the beach. Recoveries of individual releases are often said to be modified by winds. The releases reported herein represent a composite from many months, sites, and years. The agreement between recoveries and tidal characteristics further suggests that winds are of secondary importance to the recovery patterns in the eastern Strait.

Three Puget Sound Cases Involving Individuals The following cases involve additional areas of Puget Sound: (1) the Georgia Strait where a passenger fell overboard from a ferry; (2) southern Puget Sound between Tacoma and Seattle Washington which was traversed by a jumper from the Tacoma Narrows Bridge; and (3) Deception Pass, a narrow slot between Fidalgo and Whidbey islands and the alleged disposal site of a homicide victim. Case #3: An Accidental Fall from a Ferry in Georgia Strait Late on Sunday night, July 25, 1993, Robert Lord, aged 42 years, boarded a Canadian ferry to travel across the southern end of Georgia Strait from Tsawassen (a suburb of Vancouver)

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(a)

(b)

Figure 11.6 (a) Direction of net currents computed over a 30-day interval using Crean’s (1983)

numerical model. Dots indicate location of computation and sticks point in current direction without regard for speed. Outlines show tidal eddies. (b) Location and date of recovery or sighting of the steamer Clallam wreckage. Dashed lines connect last port of disembarkation at Port Townsend area of Clallam’s initial distress (+), launching of lifeboats (▫), and Clallam’s sinking ("). Dot, recovery of survivors or bodies; +, location of prominent debris. Number with dot or +: date sighted or recovered in January 1904, with the exception that three bodies were recovered near Victoria on January 10 and 12 as noted in parentheses. * next to ‘DECK’ = top foredeck recovered. Ovals, areas of thirteen tidal eddies, where arrows show the rotation of the eddy currents. Numbers refer to tidal eddies at the following approximate locations: (1) Becher Bay; (2) Race Rocks; (3) Victoria; (4) San Juan Islands; (5) Lopez Island; (6) Partridge Point; (7) Point Wilson; (8) Diamond Point; (9, 10) Dungeness Spit; (11, 12) Ediz Hook; (13, 14) Elwah R. Delta. (Illustrations by Megan Abbott-Moore.)

to Sydney, British Columbia (on Vancouver Island). Reeling from severe nausea, Lord leaned out from an upper-deck window so as not to make a mess. But he leaned too far, and pitched overboard 25 feet into the water. Without a life jacket or survival suit, Lord, 6′4′′ tall and weighing 240 lbs., survived adrift for the ensuing 8 hours. Georgia Strait is a large coastal waterway connected to the Pacific Ocean by Juan de Fuca Strait to the south and Discovery Passage to the north. The tide and the plume of Fraser River drainage, which spreads out over much of southern Georgia Strait, dominate surface currents. Winds can be important in surface drift, but happened to be particularly

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light during Lord’s ordeal. The combined effects of tides, rivers, winds, and ocean density were modeled by Jim Stronach, Sea Consult Marine Research Ltd., using GF9, a 3D hydrodynamic model implemented on a 2-km Cartesian grid for the entire Juan de Fuca–Georgia Strait-Puget Sound system. GF9 evolved from several decades of dedicated research and is summarized in a monograph by Crean (1983). Tides and ocean density conditions were specified at the Pacific Ocean entrances, and river flow was prescribed from daily discharge measurements. Winds from 13 coastal stations provided the necessary stress data at the sea surface. To eliminate the transients that develop when complex computer models first begin running, GF9 was initialized on July 1 and spun up for 25 days prior to coupling with the surface spill simulator program (SPILLSIM). Turbulence in the tidal waters was modeled at 10-minute intervals with the release of 10,000 particles dispersing with an eddy viscosity of 8 m 2/sec in Monte Carlo fashion. The modeled currents agreed satisfactorily with surface currents measured with a SeaSonde high frequency radar. The modeled drift also agreed well with the time and location where Lord was rescued. Throughout his grueling ordeal, Lord was conscious and aware of his position. After falling overboard at 11:15 p.m. Pacific Daylight Time (PDT used throughout this section) he drifted for 1.75 hours, coming within a few hundred meters of Galiano Island. After 3.5 hours (2:45 a.m. on July 26), a large southbound freighter passed close by Lord then floating a few miles offshore. By sunrise, near Orcas Island in the San Juan archipelago, Lord had drifted about 15 nautical miles (28 km). Finally, after 8 hours (7:15 a.m.) and 22 miles adrift (40 km), a vacationing police officer recovered him. At a hospital some hours after being rescued, Lord’s body temperature registered 93.2°F. Coast Guard officials told Lord that he survived the chilly waters longer than the expected 1 to 2 hours for two reasons. First, he drifted in an unusually warm current draining from the Fraser River. Second, Lord’s windbreaker jacket acted as a flotation device by holding air in its shoulders. How accurate was the computer simulation? The Monte Carlo simulation of tidal turbulence yields probabilities of target locations. In this case, Lord was rescued in the center of the high probability area spread over an elliptical region measuring approximately 10 × 20 nautical miles. A good simulation by oceanographic standards, it presents forensic investigators with the uncertainties associated with hundreds of square miles. Case #4: Jumper from the Narrows Bridge, Southern Puget Sound The case below represents a unique opportunity for high-resolution tracking with respect to the drift of human remains. The model showed that small changes in the time of a jump (± 30 min) from a high bridge made great differences in where the body drifted (± 30 miles; 48 km). On Friday February 5, 1988, a 22-year-old male leapt from midspan of the Tacoma Narrows bridge that connects the city of Tacoma and the Olympic Peninsula (Figure 11.7a). Two friends, who were also at the site of the jump, later told police the time of the jump was 3:00 a.m. (Pacific Standard Time used throughout this section). They then proceeded to a predestinated location on the eastern shore of the Tacoma Narrows (approximately 1 km away), where they were to meet their friend when he swam to onshore. The two friends waited until 7:20 a.m. before reporting their friend missing to local police. According to these friends, the missing man was an experienced bridge jumper and leapt for sport.

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(b)

(a)

(c)

(d)

Figure 11.7 Model predictions for the Narrows Bridge remains. (a) Overall map of Puget Sound.

(b) Using the Puget Sound hydraulic model, a trajectory of a bead released at approximately 0230 hours on February 5, 1988. Hour 1 corresponds to 0230 and numbers (bead counts) by dots thereafter are spaced at intervals of 2 hours. Note that after 48 hours (bead count = 25) the bead is still located south of the Tacoma Narrows Bridge. (c) A trajectory of a bead released at approximately 0300 hours on February 5, 1988. Hour 1 corresponds to 0300 and numbers (bead counts) by dots thereafter are spaced at intervals of two hours. Note that after two hours (bead count = 2) the bead is located off Fox Island, and that after 56 hours (bead count = 29) the bead is located near Alki Point. (d) A trajectory of a bead released at approximately 0330 hours on February 5, 1988. Hour 1 corresponds to 0330 and numbers (bead counts) by dots thereafter are spaced at intervals of two hours. Note that after a half hour (bead count = 1.5) the bead is located about a mile south of the Tacoma Narrows Bridge, and that after 48 hours (bead count = 25), the bead is located off the northern end of Vashon Island. (Illustrations by Megan Abbott-Moore.)

According to police reports, a fisherman sighted the body off Fox Island, approximately 6 km south of The Narrows, late in the afternoon of February 5 (Figure 11.7b). On February 7 at 11:25 a.m., after a higher high tide at 7:39 a.m., the deceased was recovered on the beach near Alki Point in Seattle approximately 20 miles north of the bridge (statute miles

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The Narrows

Tidal Currents - 5 February 1988

Current Speed (knots)

5 4 3 2 1 0

Slack Tide

-1 -2

Jump

-3 -4 -5 0 1 2 3 4 5 6 7 8 9 1011 12 13 1415 16 17 18 19 20 21 22 2324

Hour

Figure 11.8 Tidal currents predicted by the National Oceanic and Atmospheric Administration

at midstream in The Narrows during February 5, 1988. Straight line segments connect predictions given for times of slack water and maximum flood (negative) and ebb (positive) tidal currents. Dot and lines indicate ± 30 minutes before and after indicate jump from The Narrows Bridge.

used throughout this section; 32 km). At the time of recovery, the body was clad in a sweatshirt, sweat pants, boxer shorts, shoes, and socks. Autopsy revealed bilateral injuries to the lungs, liver, left kidney and spleen, as well as fractures of the right wrist and ribs. According to construction drawings, the distance from the mid-span of the Narrows Bridge to the water surface is approximately 221 feet (67 meters). Hydrographic charts indicate a water depth of approximately 209 feet (64 meters) at the point of entry (Chart No. 1874) and mid-channel tidal currents for February 5, 1988, predicted by standard tidal current tables, are shown in Figure 11.8. At the time of the jump, currents in The Narrows were flowing south at approximately 2.3 knots (1.2 m/sec) (U.S. Department of Commerce Tidal Current Tables, 1988). Winds at Alki Point recorded at 3-hour intervals during October 5–7 were calm except for a few brief intervals when they were from the north at 3 to 8 knots. According to historic records, water temperature at this time of year is near its annual minimum of approximately 8°C (46°F) (Collias et al., 1974). Fast tidal currents in The Narrows and Colvos Passage cause considerable turbulence and homogenize the water such that temperatures and densities near the sea floor are nearly the same as those of the sea surface. If the deceased were neutrally buoyant, his depth could have varied substantially. The fact that the body was clad and its movement, as shown later, agrees with that of surface currents in the hydraulic model, suggests that the body was at the sea surface most of the time between the jump and beaching. Clearly defined flow patterns and several other factors including the known time of entry into the water, the sighting south of the jump, and subsequent recovery of the body north of the bridge, make this case ideal for demonstrating the applicability of hydraulic models for correlation of oceanographic and forensic information. Hydraulic models have been used successfully since the 1880s to perform simulations of the tidal currents in estuaries (Rouce and Ince, 1957). Concrete is often used to simulate the seafloor, where the vertical and horizontal scales are selected based on fluid dynamic principles. Water level in the models is made to rise and fall through the use of plungers and water pumps that are usually placed at the entrance to the estuaries, where the rates of

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flow are also scaled from physical equations governing tidal currents. They vary in size from areas covering several hundred square feet to several acres. Experience gained over a century has shown these concrete tidal hydraulic models often to be of considerable accuracy. The hydraulic model of Puget Sound located at the School of Oceanography, University of Washington, was used to simulate the body’s drift. The model was constructed in the early 1950s to study currents in Puget Sound (Collias and Andreeva, 1977; Rattray and Lincoln, 1955). For more than 40 years it has been in active use as a teaching aid for students, as well as being used in numerous engineering and environmental studies (Collias and Andreeva, 1977). Experience from many studies has shown that the water currents near the sea surface of the subject area are accurately represented, except close to the shore. The design of the hydraulic model incorporates a number of physical characteristics, including simulation of tides that accurately reproduce predictions given in standard tidal (U.S. Department of Commerce Tide Tables, 1988) and current tables (U.S. Department of Commerce Tidal Current Tables, 1988) and approximate representation of the outflow of major rivers and the salinity in Puget Sound. For our purpose, simulation was simplified as wind effects could be neglected because local winds were mostly calm during the body’s drift. The model was programmed to simulate tidal currents at the reported time of the jump and was operated for 3 model-time days (a 24-hour day of model time equals approximately 70 seconds real time; 1 hour corresponds to approximately 2.9 seconds). To represent the body, a small floating bead with a diameter of 2 mm was used in three experimental runs. As the tidal and mean currents transported the bead, its location was videotaped and later mapped with a personal computer as shown in Figure 11.7. Preliminary model runs (not shown) indicated that the correct jump time within a small tolerance is crucial in determining where the body might have traveled, because the tidal currents were changing rapidly at the time of the jump. Therefore, three simulations, a jump a little earlier than 3:00 a.m. (approximately 2:30), one close to 3:00 a.m., and another a little later than 3:00 a.m. (approximately 3:30), were investigated (Figures 11.7b, c, and d), respectively). Positions of the bead in the three model runs are shown at 2-hour intervals, with positions numbered consecutively, beginning with “1” at the time of jump. By comparing the bead counts with times when the body was observed, the approximate time of the jump was judged to be a fraction of an hour earlier than given in the police reports. The first sighting of the body off Fox Island at approximately 4:00 p.m. on February 5 (about 13 hours after the jump) corresponds to a bead count of 7 to 8. The second sighting (i.e., recovery) at 11:25 a.m. on February 7 on Alki Point (about 56 hours after the jump) corresponds to a bead count of 29. However, as the winds were calm, it is likely that the body actually beached at high water prior to being discovered. For example, the body could have beached at approximately 6:53 p.m. during darkness on February 6, or at 7:39 a.m. on February 7. These times correspond to approximately 40 and 53 hours after the jump, or bead counts of 21 and 27 to 28, respectively. Therefore, the body could have beached at any time between bead counts 21 and 29. We determined that the jump occurred earlier than 3:00 a.m. in the following manner: In the model simulation, the body was off Fox Island at the reported location at bead counts of 15 and 2, corresponding to jump times of 2:30 and 3:00 a.m. (Figures 11.7b and 7c, respectively). For a jump occurring at 3:30 a.m. the body did not reach Fox Island (Figure 11.7d). A bead count of 8 for the sighting off Fox Island corresponds to a model

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time approximately mid-way between counts of 2 and 15 (Figures 11.7b and 7c), or approximately 15 minutes before 3:00 a.m. The effect of a jump a little earlier than 3:00 a.m., as shown in Figure 11.7b, is to increase the bead count off Fox Island by 6 and to decrease it by 6 to 23 off Alki Point. The count of 23 nearly corresponds with the high water of February 6 mentioned earlier (count = 21). This correlation suggests that the body was in the vicinity of Alki Point shortly after darkness on February 6. Given the uncertainties with the model, it is possible that the body actually beached at Alki Point during the evening of February 6, but was not discovered until the morning of February 7. Also, it is possible that the body beached during the night then floated away for a time before again washing ashore. In the three simulations (Figures 11.7b, c, and d) within 2 days after the jump, the beads were found as far south as 6 miles from The Narrows Bridge and as far north as 20 miles from The Narrows Bridge, off Alki Point. This wide dispersion occurred for jump times spanning 1 hour (2:30 to 3:30), thereby illustrating the sensitivity of the recovery to small changes in the jump time. Case #5: Deception Pass: The Body in the Nylon Suitcase The following case illustrates that currents sometimes display so much drift variability in time and space that where a body may float is not predictable. In the early morning hours of May 17, 1993, Petty Officer Mark Allen Eby, 38, strangled his wife Teresa S. Eby, 26, at the Naval Air Station, Whidbey Island, Washington. Afterward he stuffed her 5′2′′, 102-lb. body clad only in a nightshirt into a black nylon soft-sided suitcase measuring 33 × 24 × 10 inches. Shortly after the crime, Eby drove to the northernmost bridge span of the Deception Pass Bridge and dropped the suitcase into the tidal waters 180 feet below. At that time, which Naval investigators estimated to be 2:39 to 3:15 a.m., the tidal currents were flowing at 6.0 to 6.8 knots westward into Juan de Fuca Strait. Divers searched extensively for 48 hours without success in the 42°F waters. Meanwhile, a 14-person ground party searched the shoreline. For ideas of where the suitcase could have drifted, divers released a surface float that quickly exited Deception Pass and snagged on the shore a few miles to the north. Naval investigators also considered the historical oceanographic measurements collected nearby for siting a nuclear power plant, an oil pipeline, and a floating fish farm. Without exception, floating markers placed immediately east of the bridge drifted within a few days into Juan de Fuca Strait. Overall, the average water movement from the sea surface to the bottom exited Deception Pass into Juan de Fuca Strait. During one study in 1992, oceanographers dropped 250 postcard-sized wooden placards from a small aircraft flying at 500 feet altitude immediately east of the Deception Pass Bridge. Specifically, five drops of 50 cards each were made off Hoypus Point (48°24.75′N, 122°45.85′W) on the following dates: January 20, January 28, February 7, February 21, and February 29. The placards were painted with red nontoxic paint to aid beachcombers in finding them. Figure 11.9 shows the location where drift cards were recovered through March 27, 1992. With two exceptions, the recoveries were generally west of the drop site. The recovery pattern is as expected from the other oceanographic studies because drift markers, despite the tides, moved toward and into Deception Pass in a day or two. Eby’s body would be

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Figure 11.9 Locations where drift cards were recovered through March 27, 1992 are indicated

by dots. The victim’s body would be expected to drift out into Juan de Fuca Strait or beach within Deception Pass itself. (Illustrations by Megan Abbott-Moore.)

expected to drift out into Juan de Fuca Strait or beach within Deception Pass itself. Within about a month, beachcombers reported 35.2% (78) of the cards scattered along a thousand miles of shoreline westward to the Pacific Ocean over an area measuring roughly 50 by 100 miles. Naval investigators concluded that it was virtually impossible to determine where the suitcase drifted once it hit the water due to the many variables involved: water in the victim’s lungs, current speed and direction, water depth due to tide height variations, the condition of the body when it hit the water, whether the body remained in the suitcase after it hit the water, and the inability to determine exactly where the body was thrown off the bridge. Though the probability was high that Mrs. Eby’s body drifted into Juan de Fuca Strait, searching this large water body was virtually impossible. Not surprisingly, her body was never recovered. Nevertheless, based on his confession not long after the crime, in October 1993 a Naval court convicted Eby of first degree murder and sentenced him to life imprisonment.

Discussion The previous accounts illustrate that given accurate tidal, wind, and river inputs, computer simulations can provide reliable predictions over hour to day-long intervals even in areas of fast, complex currents and strong turbulence. Only a small number of observations are available with which to derive the inland movement of floatable materials. Conclusions from this study of the collision between the steamship Pacific and clipper Orpheus may be summarized as follows: (1) substantial amounts of floatable material can be transported from oceanic regimes through the Strait of Juan de Fuca to the entrances of Puget Sound and the Strait of Georgia (order of 100 miles inland); (2) the inland transport speed of the SS Pacific wreckage was comparable to that of surface drifters, an oil spill (Canadian Coast Guard Western Region Report, 1989) and a dynamic model; and (3) during episodes of reversed estuarine currents,

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extensive lines and patches of floatable material form, with significant amounts of the material tending to beach at specific locations in the eastern Strait. A variety of oceanographic models may be utilized to demonstrate trajectories of floating human remains and to obtain the time required to arrive at certain locations. Some are physical, being constructed mostly of concrete covering substantial areas, and some are numerical, being run on electronic computers. Examples of physical or hydraulic models include the one described in this chapter for Puget Sound and models on display at the U.S. Army Corps of Engineers Waterways Experiment Station at Vicksburg, Mississippi. Oceanographic models do not show with complete reliability where a floating object will travel under all environmental conditions for a number of reasons. Despite shortcomings, the models often predict probable trajectories the body could travel and indicate areas that the body is not likely to travel. By superposing oceanographic models with up-to-date field data, death investigators may set limits for searches, determine potential origins of floating or beached remains, and correlate information regarding points of water entry and sightings of remains.

Acknowledgments My thanks to Brian Gisborne, owner-operator of the water taxi Juan de Fuca Express, Victoria, British Columbia, for locating photos of the Pacific and Orpheus; to Nick Hanson and Carolyn Marr, Museum of History and Industry, for reproducing photos of the Pacific and Clallam; to Jim Stronach, SeaConsult Marine Research Ltd. for simulating Bob Lord’s drift; to Gary R. Miller, Trans Mountain Oil Pipe Line Corporation, for permission to use the drift card data for Deception Pass; and to Douglas A. Tomaso, Naval Criminal Investigative Service Field Office Puget Sound, for information regarding Mark Allen Eby.

References Annual Reports of the Supervising Inspector of Hulls, First District 1876 Annual Report of the Supervising Inspectors, San Francisco, CA. Bailey, R.G. 1967 British Columbians enraged at Pacific–Orpheus Disaster of 1875, Marine Notebook, 50:54–56. Beach, E. L. 1972 Dust on the Sea, Zebra Books, New York. Benjamin, T. B. 1968 Gravity currents and related phenomena, Journal of Fluid Mechanics 31(2):209–248. Chart No. 1874, National Oceanic and Atmospheric Administration. Collias, E.E. and S.I. Andreeva 1977 Puget Sound Marine Environment: An Annotated Bibliography, Washington Sea Grant Program Publication Seattle, WA, WSG 77-2, 392 pp. Collias, E.E., N. McGary, and C.A. Barnes, 1974 Atlas of Physical and Chemical Properties of Puget Sound and its Approaches, Washington Sea Grant Publication, University of Washington Press, Seattle 235 pp.

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Cox, J.M., C.C. Ebbesmeyer, and J.M. Helseth 1978 Surface drift sheet movements observed in the inner Strait of Juan de Fuca, August. National Oceanic and Atmospheric Administration Technical Memorandum ERL MESA-35, Washington, D.C. Crean, P.B. 1983 The development of rotating, nonlinear numerical models (GF2, GF3) simulating barotropic mixed tides in a complex coastal system located between Vancouver Island and the mainland. Institute of Ocean Sciences, Dept. of Fisheries and Oceans, Canadian Tech. Dept. of Hydrography and Ocean Sciences No. 31, p. 65. Ebbesmeyer, C.C. and W.J. Haglund 1993 Drift trajectories of a floating human body simulated in a hydraulic model of Puget Sound, Journal of Forensic Sciences 39(1):231–240. Ebbesmeyer, C.C. et al. 1979 Dynamics of Port Angeles Harbor and approaches. U.S. Environmental Protection Agency Research Report EPA600/7-79-252, Washington, D.C. 1991a 1875 Floatable wreckage driven inland through the Strait of San Juan de Fuca. Puget Sound Research ’91 Proceedings, Puget Sound Water Quality Authority, Olympia, Washington, pp. 75–85. 1991b Eddy induced beaching of floatable materials in the eastern Strait of Juan de Fuca. Puget Sound Research ’91 Proceedings, Puget Sound Water Quality Authority, Olympia, Washington, pp. 86–98. Fox, G.H. 1910 Personal letter dated 23 September to George Davidson. George Davidson Papers, University of California, Berkeley, California. Frisch, A.S., J. Holbrook, and A.B. Ages. 1981 Observations of a summertime reversal in circulation in the Strait of Juan de Fuca. Journal of Geophysical Research 86(C3):2044–2048. Holbrook, J.R. and D. Halpern 1982 Wintertime near-surface currents in the Strait of Juan de Fuca, Atmosphere–Ocean 20(4):327–339. Holbrook, J.R., G.A. Cannon, and D.G. Kachel 1983 Two-year observations of coastal–fjord interactions in the Strait of Juan de Fuca. In Coastal Oceanography, edited by H. Gade, A. Edwards, and H. Svendsen, pp. 411–426. Plenum, New York. Holbrook, J.R., R.D. Muench, and G.A. Cannon 1980 Seasonal observations of low-frequency atmospheric forcing in the Strait of Juan de Fuca. In Fjord Oceanography, edited by H.J. Freeland, D.M. Farmer, and C.D. Levings, pp. 305–317. Plenum, New York. Lockley, F. 1926 Impressions and observations of the Journal man, The Journal, Portland, OR, April 6–9. Rattray, M., Jr. and J.H. Lincoln 1955 Operating characteristics of an oceanographic model of Puget Sound, Transactions of the American Geophysical Union 36, 251–261. Rouse, H. and S. Ince 1957 History of Hydraulics, Iowa Institute of Hydraulic Research, State University of Iowa. U.S. Coast Guard 1989 Oil sample analysis report. Marine Safety Office Puget Sound Case Number MP89000186, Oil Identification Laboratory Case Number 89-117.

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U.S. Department of Commerce Tide Tables 1988: High and Low Water Predictions, West Coast of North and South America including the Hawaiian Islands, National Oceanic and Atmospheric Administration, National Ocean Service. Tidal Current Tables 1988: Pacific Coast of North America and Asia, National Oceanic and Atmospheric Administration, National Ocean Service. U.S. Signal Office 1875 Bulletin of international meteorological observations, November and December. Year Wind Observations, National Weather Service, personal communication, Robert Anderson, Chief, Seattle Ocean Service, Seattle, Washington.

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Section 3

Mass Fatalities and Mass Graves

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Recent Mass Graves, An Introduction WILLIAM D. HAGLUND Contents Introduction Defining Mass Grave Why Exhume Mass Graves? The Social Context Selected Accounts of Mass Grave Exhumations Anatomy of a Mass Grave: Concepts and Terminology Approaches to Exhumation Exposure and Delineation Extraction of Fleshed Remains Documentation and Removal Issues Involved in Mass Grave Investigations Expert Assessment Levels of Examination and Documentation Case Numbering and Removal Units Identification of Victims Conclusions References

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12

Introduction Under normal circumstances, burial of human remains is a common cultural means of disposal. Human burials also can result from natural phenomena such as animal caching, sheet wash, leaf fall, or various forms of mass wasting such as avalanches, slides, debris flows, and slumping (Skinner, 1987). As a criminal means of disposition of human remains, burial is relatively infrequent. Figures for U.S. State of Washington serve to illustrate. For the period 1981 through 1990, of the 1,960 murders for which deposition information is available, only 27 (1.38%) were recovered from burials (Homicide Information Tracking System (HITS)). Legally condoned, manmade mass burials occur only under extraordinary circumstances, when they are deemed necessary for humanitarian or sanitation purposes. Mass burials in the aftermath of the August 1999 earthquakes in Turkey are but one example (Thieren and Guitteau, 2000). Tragically, burial is a commonplace, extra-legal expedient to cover up both human rights abuses and war crimes. The victims in contemporary clashes, to a large extent, are not combatants, but civilians. Hostilities fueling these killings range broadly, including declared wars between nations, nondeclared border clashes, struggles between ethnic or political entities within a country, or “dirty” wars of repression (Geiger and Cook-Deegan, 1993). Although such mass graves are not necessarily a new phenomenon, it is only over the past two decades that their forensic investigation has been on the rise, beginning with Argentina, Guatemala, Iraqi Kurdistan, Ukraine, and El Salvador (Anderson, 1993; Bevan, 1994; Danner, 1993; Equipo de Anthropologia Forense de Guatemala, 1994; Joyce and Stover, 1991; Stover and Manuel, 1991). Rwanda, Croatia, Bosnia, Kosovo, and East Timor continue to supply the current surge of ongoing mass grave investigations (Ferllini, 1999; Jiménez, 1996; Koff, 1996; Stover, 1997; Stover and Peress, 1998). Less publicized mass grave investigations have been carried out in Somaliland, Indonesia, Sri Lanka, and Bangladesh in the past 5 years. These investigations add new dimensions to the knowledge base of forensic taphonomy with respect to buried remains and mass graves. This chapter considers the definition of mass grave, briefly recaps seminal mass grave investigations, and borrows from recent experience to discuss the dynamics of mass graves, approaches to their exhumations, and issues encountered in their forensic investigations.

Defining Mass Grave There is no agreement on the minimum number of individuals that comprise a mass grave (Haglund et al., 2000). Mant (1987) in his discussion of post-World War II exhumations defines a mass grave as containing two or more bodies that are in contact with each other. The UN Special Rapporteur interprets a mass grave as a location where three or more victims of extra-judicial, summary, or arbitrary executions, not having died in combat or armed confrontations are buried (International Criminal Tribunal for The Former Yugoslavia, 1996). Skinner (1987) suggests a mass grave contains at least half a dozen individuals. It should be noted that each of these definitions introduces a qualifier that incorporates the particular interests of its author. Mant’s stricture that the bodies must be in physical contact with each other incorporates his interest in variables that affect decomposition of buried remains. The burden of the Special Rapporteur’s definition (above) that the grave

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occupants must be victims of a particular type (International Criminal Tribunal for The Former Yugoslavia, 1996) serves the Tribunal’s legal concerns regarding how the grave occupants died (Haglund et al., 2000). Another qualifier, introduced by Skinner et al. (this volume), suggests a functional distinction between single graves, group graves in which bodies are laid out in parallel, and mass graves in which bodies are disordered. Although not meant as a precise definition, Skinner et al. (this volume) introduce the distinction of organized group graves, in which individuals lie parallel to one another, vs. mass graves in which placement of the dead is disorganized. Disorganization of buried victims, though not a strict rule for mass graves, reflects the lack of dignity given to disposal of mass grave occupants (Skinner, pers. comm.). Mant’s definition, while using the minimum number of individuals needed to comprise the mass grave, recognizes a salient taphonomic character of mass graves. A mass grave involves remains in contact with each other. It is this contact that creates the unique grave environment in which the rate and character of decomposition depart from patterns in graves containing a single individual. It is for that reason that this discussion revolves around graves containing a mass or aggregate of individuals, whether organized or disorganized.

Why Exhume Mass Graves? The Social Context There are multiple rationales for the exhumation and investigation of contemporary mass graves. First, in the human rights context, is to collect narrative and physical evidence that will assist in establishing accountability for those responsible and bring them to justice. Second is the process of collecting evidence to identify the victims in order for their remains to be returned to their survivors. Third, the investigative process creates a document that should stand up to historical revisionists. Fourth is to expose atrocities to world opinion and to establish an international standard to prevent such crimes from occurring in the future. A fifth inducement for investigation of mass graves involves a basic dignity for the victims and for human life. If victims remain buried along with the secrets of their deaths, their deaths will have been in vain, threatening a similar fate for future generations. Exhumation of a particular mass grave may or may not address all of these objectives. Some mass grave exhumations are performed for purely humanitarian reasons with no goal of prosecutions in mind.

Selected Accounts of Mass Grave Exhumations Even though experience with excavation of mass graves is on the ascent, little has appeared in peer-reviewed literature. Skinner’s thoughtful 1987 paper, “Planning the Archeological Recovery of Evidence from Recent Mass Graves,” reviewed relevant literature, considered logistical aspects, and advocated the use of archeologists. During the past 15 years much of the experience involving mass grave exhumations languishes in the respective reports of their investigations. Certainly, with the continued experience of the multitude of investigators now involved in international forensic investigations, we can expect more articles in the future dealing with issues of mass graves (Haglund, 2000; Haglund et al., 2000; Simmons, this volume; Skinner et al., this volume; Schmitt, this volume). A few historical examples of reporting on mass grave investigations are in order. One intriguing case is the 1943 forensic investigation into the massacre of over 11,000 Polish

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prisoners in the Katyn Forest near Smolensk, in modern-day Russia (Abarinov, 1993; FitzGibbon, 1979). The victims were Polish soldiers, primarily officers, who had been held as prisoners of war by the Soviets. The executions took place in 1941. The graves were first brought to the attention of the public by the Germans in April of 1943. Earlier, in February of that year, German troops advancing through the Katyn Forest near Smolensk had discovered suspicious earth mounds planted over with young pine trees. Preliminary excavations confirmed the existence of mass graves. A concern of the Nazi government was that they would be blamed for the deaths, which occurred at a time when the region was under Russian occupation. In May of 1943, strategizing to counter future allegations that they had carried out the massacres, the Germans established an international medical mission composed of professors of forensic medicine from nine German-occupied European nations, Italy, and neutral Switzerland. The commission was to report manner, cause, time of death, and probable culpability in the deaths. The report, edited and issued by German authorities, was released in April 1943. FitzGibbon (1977), citing from translations of the report, relates that 4143 bodies were exhumed and 2914 were identified on the basis of personal artifacts and documents recovered from the bodies. A majority of the victims had been shot in the head; 5% were found with their hands tied behind their backs with ropes. The report went on to comment that absence of insects, as well as the presence of documents, correspondence, diaries and newspapers in the grave, indicated that the deaths occurred in March, April, and May of 1940. The Soviets reoccupied the area of Smolensk in September of 1943. They vigorously denied charges that they were responsible for the Katyn atrocities and began their own investigations that in turn laid blame on the Nazi German government for the executions. At the insistence of the Soviets and over the reluctance of the French, British, and American prosecutors, allegations of the massacre were included in count three of the indictment at the Nuremberg War Crimes Trial. Although the falsity of these indictments was strongly suspected by many, they were allowed to stand though they were not mentioned in the verdict (Davidson, 1997; Taylor, 1992). It has become clear in recent years that the Soviets were responsible for these mass executions and popular accounts have since been published (Abarinov, 1993; FitzGibbon, 1977; Zawondy, 1962). It was not until Mant’s 1950 Doctoral Thesis in Medicine at London University that variables involved in the preservation of remains in mass graves were more systematically analyzed. He served in the British Army Royal Medical Corps as a pathologist during and after World War II. His primary mission was the identification of missing allied military personnel, especially fliers. The largest mass grave he reported held 40 bodies, and the total number of individual remains in his study was 150 (Mant, 1950). Other World War II-associated mass graves have been investigated in Saipan (Russell and Flemming, 1991) and in the Ukraine (Bevan, 1994). The latter investigation was carried out by an Australian forensic team in June of 1990. From one grave they performed examinations on selected skulls of 553 individuals. The dead were alleged to be Jewish men, women, and children who had been rounded up from the area around the town of Serniki. Limited examinations were carried out at the graveside, with the goal of estimating age and sex and determining cause of death. This was part of an investigation by the Australian government into the case of Nazi Officer Ivan Polyukhovich who was indicted for his involvement in a massacre outside the town of Serniki in the fall of 1942. Nineteen hundred ninety-six stands as a watershed year for launching large-scale mass grave exhumations. A primary influence was provided by the Boston-based organization,

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Physicians for Human Rights (PHR). They provided the forensic expertise for the International Criminal Tribunals for Rwanda (ICTR) and The Former Yugoslavia (ICTY), fielding international teams of experts to exhume nearly 1200 individuals from seven sites on two continents. The 1996 work was launched in Rwanda where massacres had taken place in 1994. Nearly 500 individuals were exhumed and examined from the site of the Roman Catholic Church in Kibuye, a western Rwandan province. A second Rwandan site in the capital, Kigali, was also examined. The Rwandan investigations were followed by exhumations in The Former Yugoslavia at the Bosnian sites of Cerska, Lazete, Nova Kasava, Pilica, and finally the Ovcara grave in eastern Croatia. As of this writing, the ICTY continues seasonal exhumations.

Anatomy of a Mass Grave: Concepts and Terminology Each mass grave is unique. A grave may consist of a simple trench in which bodies are arrayed with minimal contact with each other. In more complex graves, bodies may form a dense, contiguous aggregate known as a body mass (Figure 12.1). Within a body mass, individuals are in contact with each other, often extremely jumbled, contorted, and entangled (Figure 12.2). It is not unusual that individuals are in various stages of dress and undress. When exposed, such a body mass presents a jolting, chaotic vision that assaults all sensibilities. Some graves may contain more than one discrete body mass (Figure 12.1A and B). Not infrequently, there will be satellite remains that are not a part of the body mass. Multiple body masses within the same grave indicate their entry into the grave at different times. Another indication of multiple bouts of entry into a grave is the presence of layers of remains interrupted by intervening fill (Figure 12.1B and Figure 12.3). This is a result of groups of individuals being deposited in successive events, each group covered by fill and then the next group of individuals added. In this type of grave the intervening layers of fill allow increased drainage that can drastically alter the decomposition dynamics. Such a grave is described by the Germans investigating in the Ukrainian area of Vinnytsia where graves were found to contain groups of 100 to 120 bodies separated by a layer of clothing and earth, followed by another group of bodies (Eher, 1944). Regardless of its configuration, a large body mass presents a complex taphonomic environment affected by a multitude of variables (Table 12.1). Mant is truly the pioneer in systemizing observations affecting preservation of buried human remains including those in mass graves. Among his many contributions to the field of forensic investigation are his analyses of the various processes of body decomposition in different grave contexts and his demonstration that mass graves create their own micro-environment (Mant, 1950, 1957, 1987). Mant clearly showed that bodies decompose at different rates depending on their condition at burial, method of burial, and soil conditions in and around the grave. He also pointed out that bodies in the center of mass graves decompose more slowly than those on the outer edge of the body mass, thus creating a feather edge effect, which ran contrary to the general consensus of medical opinion at that time. A major factor in determining of the state of a particular individual in a mass grave is its relative position in relation to the body mass. Satellite remains are least preserved. Peripheral bodies of the body mass are less preserved (Figure 12.4) than individuals within the core of the assemblage (Figure 12.5). This dynamic was noted in the 1943 report of the International Medical Commission that investigated the Katyn Forest Massacre.

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Figure 12.1 Three mass grave configurations in cross section: (A) single, contiguous body mass;

(B) multiple discrete body masses in a single grave; and (C) multiple, layered configuration with intervening fill, indicative of separate bouts of entry. The body masses each consist of a core or inner taphonomic zone, an outer margin or peripheral taphonomic zone, and the outermost edge or the mass/fill taphonomic interface. ■ = core of the body mass or inner taphonomic zone; = margin of the body mass or peripheral taphonomic zone.

FitzGibbon (1977) relates the descriptions of the graves and the conditions of the remains as summarized by Dr. Buhtz, a professor of forensic medicine and criminology at Breslay (Wroclaw) University: Dr. Buhtz documents that the pits had been dug in stepped terraces in a hilly area and in sandy soil. In some places, they penetrated to underground water. He continues with observations on decomposition: The bodies were in various stages of decay. In a few cases mummification of the uncovered parts had taken place (bodies from the uppermost layers), but generally the formation of adipocere had started with the fat penetrating into the clothing. (p. 136) The stages of decay were found to vary in accordance with the position of the bodies in the pits. Whilst mummification had taken place on the top and at the sides of the mass of bodies, a humid process could be observed caused by the damp nearer the center. Adjacent bodies were stuck together with thick putrid liquid. The peculiar deformations due to pressure show that the bodies had remained in the position they had assumed when they were first thrown into the pits. (p. 142)

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Figure 12.2 Large body mass with complex positioning of individuals, viewed from above.

Postmortem interval is 1 year; same site as Figures 12.3 and 12.5. Note that portions of one individual may extend horizontally to be overlain by surrounding remains, or parts of an individual body may extend to higher or lower areas of the grave to be entrapped by other bodies. Decomposition and skeletonization are accelerated for individuals on the periphery. (Photograph courtesy of Gilles Peress.)

Figure 12.3 Portion of body mass viewed in cross section illustrating interrupted bouts of

entry with further deposition of remains. Note layering of bodies with sediment and plants. Postmortem interval is 1 year; same site as Figures 12.2 and 12.5. (Photograph courtesy of Gilles Peress.)

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Table 12.1 Major Taphonomic Factors Affecting the Condition of Remains in Mass Graves Grave Characteristics • Depth • Compaction • Inclusions • Intervening fill Temporal Factors • Postmortem interval prior to burial • Duration of burial • Season Body Characteristics • State of decomposition • Cause of death • Body habitus • Clothing or other wrapping Soil Characteristics • Ph • Drainage • Compaction • Coarseness and type of soil • Contaminants Body Assemblage Characteristics • Thickness and extent • Position relative to core and perimeter Other Characteristics • Temperature during pre-burial period • Moisture • Post-burial exposure of remains to atmosphere • Disturbance • Oxygen content

Buhtz added that the accumulation of the initial products of decomposition in the surrounding soil had caused chemical changes that in turn affected the subsequent decomposition process. Remains on the fringes of the body mass bridge two taphonomic interfaces: One is contact with other bodies, and the other is contact with fill or the surrounding matrix that forms the walls and floor of the grave. At the outer fringe they are affected by porosity and percolation characteristics of the surrounding substrate. Best preserved are remains within the interior of the body mass where they create their own synergistic environment, body on body. These remains, isolated from the grave substrate, trap moisture that originates from body fluids and the fluids of decomposition. For graves submerged beneath the water table or in areas susceptible to seasonal rains or flooding, additional moisture may be transported into the core of unsaturated body masses. Clothing may act as a wick. The weight of the overburden or its method of compaction can compress bodies in the grave and reduce pore spaces between sedimentary particles. The overburden of schist in the grave at Kibuye, Rwanda, resulted in severely flattened remains that were often pressed into each other. Compaction will vary with respect to the weight of different

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Figure 12.4 Three individuals in satellite position relative to larger body mass, illustrating

the effect of relative position within the grave on preservation. Least preservation, in this case full skeletonization, is encountered for satellite individuals and for individuals located at the periphery of the body mass, especially those interfacing with the fill. Postmortem interval is 5 years. (Photograph courtesy of Gilles Peress.)

Figure 12.5 Bound hands of an individual found within the core of a body mass, illustrating

the effect of relative position within the grave on preservation. Most preservation, in this case all of the soft tissue, is encountered for individuals located within the core of the body mass. Postmortem interval is 1 year; same site as Figures 12.2 and 12.3. (Photograph courtesy of Gilles Peress.)

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soil/rock types and the depth of the fill. Coarser-grained sediments are more resistant to compaction due to the supporting effect of the grains and the lower water content (Briggs, 1990). Reduced porosity decreases permeability, the capacity to transmit fluids. Driving heavy machinery over the grave contributes to compaction. The degree of compaction and depth of burial will allow or dissuade encroachment of the grave by mammalian scavengers or necrophilous insects (Haskell et al., 1997; Rodriguez and Bass, 1985). For skeletal remains, compaction may also account for distortion of bone that can both mimic pathology and throw off statistical measurement. Nawrocki (1995) points out that subtle warping of cranial fragments is often not detected unless all fragments are present and incorporated into a reconstruction. Under favorable conditions, a mass grave may yield partially to fully fleshed remains up to several years following the primary burial; for example, after 5 years of internment in the Ovcara Grave outside of Vukovar, Croatia, the majority of the 200 victims were fleshed remains, some retaining tattoos. On the other hand, the Bosnia-Herzegovina grave at Cerska, opened merely 12 months following burial, revealed 150 males in varying stages of advanced skeletonization.* The stark contrast of soft tissue preservation between these two examples can be attributed to several factors. The grave at Ovcara was relatively deep with clay soil that facilitated drainage from surrounding fields. The overburden had been firmly compacted. In locations of highest body density they had as many as eight bodies deep. Both the body mass and drainage conditions conspired to trap moisture. In contrast, bodies of the Cerska grave were deposited on a roadside embankment and had been covered by a relatively thin layer of loosely compacted gravel overburden. The lack of compaction and incline of the surface upon which the bodies rested did not allow moisture to be trapped. Drainage was transient and encouraged rinsing and draining of bodily fluids and products of decomposition from the area. Decomposition was accelerated further because the grave surface was fully exposed to the sun. This allowed warming of the overburden and the remains, some deposited as little as 50 cm below the surface. The moisture-trapping ability of the remains was lessened due to their low density. Throughout most of the grave, with the exception of the foot of the embankment where bodies had piled up against each other, the density of the remains tended to be only 1 to 3 bodies deep.

Approaches to Exhumation Table 12.2 presents an overview of the steps involved in the exhumation of a mass grave. It can readily be seen that investigations of these graves necessitate an interdisciplinary effort. Once authority is granted for access to the site, the first priority ideally should be an on-the-ground assessment. For purposes of this chapter, only the steps of exposure, delineation and extraction of the remains (steps 6 to 8 in Table 12.2) will be addressed in detail.

* Some would advocate that the Cerska “grave” is not technically a grave. The bodies were simply deposited on the ground surface and covered with borrowed soil. No excavation or hole was made in which to deposit the remains. Regardless, preservation dynamics hold and are relevant to this discussion.

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Table 12.2 1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11.

Overview of the Exhumation Process for a Mass Grave

Assessment Staging, equipment, supplies Site preparation, surface evidence, and clearing of ground cover Initial overview site mapping Establishment of grave boundaries Exposure and removal of overburden Delineation in preparation for removal Documentation: photography, mapping, completion of field forms Extraction Storage/transport to location of examination Clean-up

Exposure and Delineation The first step in actually preparing bodies for removal is their exposure. This requires removing fill that covers the topmost layer of the bodies and then cleaning the area so they can be clearly delineated. The presence of clothing can be beneficial on several counts. It provides protection to bodies from damage during excavation. Garments can be an asset in exposing remains as they can be very gently manipulated and shaken to dislodge soil. Done gently, this is less damaging to soft tissue and quicker than using tools. Clothing also serves as an envelope for the remains. As bodies are exposed, it is prudent to secure bags around unclothed hands, feet, and crania. This minimizes the potential for loss or displacement of teeth, bones, fingernails, and other remains or evidence (Haglund, 1988). If there is no clothing over exposed areas of soft tissue, often the hands and the face, great care is necessary so as not to damage the soft tissue of fleshed remains. Although soft materials, such as wooden chopsticks and brushes, are useful for many excavations, when one is working in damp soggy environments, brushes may prove next to useless. Soft adipose tissue, however, can be marred even by soft brushes. In these situations consideration should be given to more detailed cleaning at the time of postmortem examination. Extraction of Fleshed Remains Frequently, a single individual will not be completely exposed at the time the initial overburden is removed. Portions may extend horizontally to be overlain by surrounding remains or parts of the body may extend to lower areas of the grave to be entrapped by other bodies. This situation usually demands exposure of an area encompassing several surrounding individuals. Fortunately, in larger, more recent graves, especially where moisture content has been trapped, groundwater is prevalent, or drainage poor, the remains may be well preserved, fleshed, and pliable. This flexibility allows adjacent remains to be rolled or lifted in order to facilitate freeing trapped body parts from their surroundings. Extraction of a particular individual often requires manipulating several surrounding remains in order to remove the one that is potentially most free. When the majority of a body is visible, and perhaps a leg or an arm is still beneath surrounding remains, there is a tendency to want to pull it free. There is the danger that weakened articulations, especially the knee joint, ankles, wrists, or fingers, may separate, leaving the disarticulated body

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portion trapped beneath other remains. The level of the grave harboring the separated body part may not be reached for hours or days, thus increasing problems of reassociating body parts to appropriate individuals. Inability to reassociate such body parts can potentially confound the identification; for example, rings that could potentially lead to identification might stay on a finger that has been left behind. There is also the negative perception of not being able to repatriate the most complete remains once they have been identified. Prioritizing remains for removal requires a good spatial sense. Where bodies are partly covered by another body, experience assists in determining which bodies should be manipulated next so they may be extracted. Care needs to be taken, however, that parts do not become detached while being manipulated. This might necessitate sliding an excavator’s arm between bodies to the point where the end of the limb can be held and pushed gently back, freeing the limb from the mass. The excavator needs to ensure that all the digits at the end of the limb are held in place as this occurs, or those digits might be left behind when the limb is moved. Once hands or feet are exposed, if they are in any way disarticulated or vulnerable to disarticulation, they should be placed inside a bag tied to the nearest long bones, to ensure that the digits or phalanges do not detach when the body is moved. A bag might also be placed over the head, as the cervical vertebrae are frequently loose. This also ensures that hair and teeth are not lost during transport. Documentation and Removal Prior to removal, a case number is assigned and the documentation team can begin photographing, mapping, and describing the body. An overall photograph is taken showing the position of the body, as well as any detail shots deemed necessary. Close-ups might include tattoos, obvious trauma, or unusual clothing. The overall photograph is accompanied with a north arrow, scale and case number. The detail photograph also includes a scale, and the case number. All photographs are entered into a photograph log. At a minimum, the horizontal and vertical positions of the crania are plotted from a point usually taken from the top of the crania. The outlines of the body might also be plotted, depending on the detail of the map decided on by the investigator. The description of the body is brief. The purpose of the description is to gain enough information so that the remains will not be confused with others during transport to the morgue where a full description and postmortem are completed. Fleshed remains should be removed, as much as is possible, as intact units with minimal disturbance. This allows for proper inspection in the examination area and presents the remains in the best condition for postmortem examination. Once photography, mapping, and other documentation are complete, the body is ready for removal. Minimally, the case number and date of removal are written on both ends of the body bag. The bag is unzipped, opened, and moved adjacent to the body. If the body is face up, the arms are moved close to the body and placed on the chest. The legs are lifted together. One excavator is positioned at the head, one in the middle of the body, and one at the legs. As these people lift, an additional person holds open the body bag and helps to slide it beneath the body. Once the body is inside, the bag is placed to the side while the team examines the soil underneath the body to ensure that no body parts or associated evidence are left behind. Any loose disassociated portions of the remains are separately bagged and included in the body bag. Remains lying face down often can be

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simply supported and rolled into the body bag. Finally, the bag is zipped and removed to a storage area.

Issues Involved in Mass Grave Investigations Exhumation of mass graves is a complex process that requires the balancing of many simultaneous goals, issues, and activities. It also requires processing large numbers of bodies and volumes of evidence over a matter of days, weeks, or even months. This is a process that requires continual rechecking of procedures and data. Procedures of a field operation are frequently carried out in temporary or substandard facilities. Often, the exhumations and examinations are part of an evolutionary process and adaptation of procedures not only to address the goals of the mission, but also to generate pragmatic solutions to the many problems encountered, and to resource limitations. The following section explores some common issues encountered in the exhumation of mass graves and the examination of their victims. Expert Assessment Prior to exhumation, large graves should be assessed by personnel experienced in mass grave exhumations and attendant logistical needs. Such an on-site visit officially confirms the presence of human remains. Equipment and potential security concerns can be evaluated. Logical requirements of the work, such as transportation of remains, morgue facilities, and staff housing, are assessed at this time. The assessment phase typically entails notification of local authorities and determination of local cultural and religious sensitivities. Levels of Examination and Documentation A major question that arises in international investigations is what level of documentation and examination will satisfy both legal and professional standards? The United Nations Manual on the Effective Prevention and Investigation of Extra-Legal, Arbitrary and Summary Executions (1991) is often quoted as the benchmark by which investigations (including exhumations and examination of remains) should be judged. However, these are ideal standards and, as the guidelines caution, they may not be attainable for many reasons. For example, it is necessary to give recognition to the often-divergent perspectives of politics, religion and culture that pervade such investigations. Other impediments frequently encountered include lack of facilities, inadequate logistical support, limited financing, equipment and supplies, as well as inclement weather conditions, and security issues. Limitations and impediments leading to the relaxation of particular standards always should be disclosed in the final report. Case Numbering and Removal Units The term removal unit is used here to indicate remains or groups of remains that are packaged and numbered for removal from a particular site. Removal units may or may not bear a one-to-one correspondence to case numbers. A numbering system in which consecutive numbers are assigned to individuals is the most common approach when dealing with multiple fatality incidents such as mass graves. It would be ideal if each

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removal unit equated with a complete individual. Unfortunately, this frequently is not possible. What comprises a removal unit is dependent upon the condition of the remains. Under various circumstances a removal unit could consist of complete remains, partial remains or include the remains of more than one individual; for example, an infant hidden by its mother’s swaddling clothing might be collected as one removal unit. A removal unit may receive one case number but be packaged separately. A single set of remains may end up distributed among multiple body bags when remains in advanced stages of decomposition are removed from an extremely muddy environment. Partial individuals may have been placed in the primary grave originally, or partial individuals can result from tampering, such as attempts to rob the grave. Several operative concepts should be considered when assigning and numbering removal units. First among these is the need to enforce a uniform approach. This is critical when there is the potential of excavating multiple graves with parts of the same individuals distributed among them. It is necessary to be able to track removal units back to a relatively in situ location at particular sites. Attempts to allocate partial remains to a single individual should not be undertaken in the field, but are best accomplished under laboratory conditions with detailed supportive documentation regarding their recovery. This process may not be possible for weeks, months, or even years following the exhumations. In addition to the problems imposed by condition or completeness of the remains or the grave, false totals of the number of individuals can arise at one of several junctures during the numbering, removal, and storage of remains. Error can occur in the initial assignment of numbers; for example, duplicate numbers may be given out or numbers may be skipped. Clerical errors can happen in writing numbers on body bags. Oversights can occur when placing individuals into body bags. These include placing parts of more than one individual in one body bag or the wrong body into a particular body bag. One staff member should be charged with giving out numbers for removal units. In any situation, the more staff involved in numbering and extracting of bodies, the higher the potential for error. Another pitfall is to assign a number to a body or skeleton prematurely, before it is ready to be removed. This usually occurs when the availability of a body to be removed is misjudged. Inexperience is commonly at fault. A worker may request a number, assuming that a particular remains can be extracted, only to find upon trying to remove the remains that he or she cannot. This can happen when one misinterprets the position of one or more limbs, either assuming an unobservable limb would be no problem to extract or mistaking a freed and observable limb of a separate individual as belonging to the remains one wishes to remove. Such problems occur when a part of the body is trapped beneath other remains or debris. In these cases it is necessary to leave the “numbered” remains in the grave until additional bodies or overburden can be removed in order to free the trapped part. The final freeing of the remains may not occur for hours or days and result in reassigning a different number to the same remains at a later period. An illustration of misnumbering is noted in the Argentine forensic report of the investigation into the 1981 El Mazote Massacre (Danner, 1993). At the end of the exhumation the tally of individuals was 119. During the examination phase of the investigation it was found that three skeletons (23, 61, and 72) had been miss-numbered (no skeletons matched those numbers) and two skeletons had been assigned one number (81). Hence, the final individual count was 117. Similar numbering problems were encountered in the 1996 exhumations of graves investigated under the International Tribunals; for example,

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although 154 numbers for body bags were given out during the exhumation of the Cerska site, only 150 individuals were exhumed. This discrepancy was attributed to clerical errors, numbers (21, 55, and, 56) being requested by team members but not immediately assigned to bodies or body bags. A fourth number, 93, was assigned to a remains, and these remains proved impossible to remove at that time. When the body was finally freed the next day, it was inadvertently re-photographed with a new number, body number 100. These examples point out that when complicated graves are involved, it is imprudent to assume that the numbers allocated or number of body bags necessarily equates with the number of individuals. The calculation of the total number of individuals exhumed is best done after the postmortem examinations are completed and after commingling and reattribution of parts has been accomplished to the greatest extent possible. Prior to that point, comments about the numbers of bodies being removed should be presented as estimates only. This is especially germane in answering media demands regarding body counts. There are various means of guarding against potential numbering errors. Organization of the removal process is essential. It is crucial to have a specific team member in charge of giving out numbers. Another strategy is to limit the numbers of team members involved in the body extraction processes. Fundamental to proper extraction is a full understanding of the relationship of bodies to other remains or features of the grave. The ability to judge the accessibility for removal of a remains needs to be a prerequisite for granting a number for its removal. Identification of Victims Although personal identification is the traditional goal of the recovery of human remains, the identification process is carried out at several levels: biological, anatomical, sociocultural affiliation (or circumstantial), and personal. Most elemental is to distinguish human from nonhuman remains. Assessment of an individual’s biological characteristics (i.e., sex, age, stature, and ancestry) provides the groundwork for personal identification and constitutes the next level of identification. When multiple individuals are involved, their minimum number must be established. If body parts, individual bones or bone fragments are involved, efforts must be made to attribute them to the appropriate individual. Another level of identification is the assignment of an individual to a particular population segment such as a religious, cultural, or social affiliation. For example, associated artifacts or circumstances can aid in determination of individuals’ military vs. civilian status, whether they were hospital patients, membership in a particular religious group, or whether they were rendered helpless at the time they were killed. Individualizing traits, such as dental characteristics, tattoos, osteological evidence of past injuries or life stresses may lead to a more specific level of identification and offer the greatest hope of unique personal identification. Geberth (1990:192) points out that in traditional homicide investigations: The identification of the victim is critical because in order to prove a charge of homicide, it must be established that a named or described person is in fact dead...furthermore, from an investigative point of view, identification provides a starting point and direction for the inquiry.

In part, the rationale for this dictum is that most homicide victims are killed by someone they know; a personal motive is involved in the killing. In upward of 75% of solved homicides, the victims were murdered by someone they knew. Hence, much investigative

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effort is expended to confirm personal identification of the victim. Fortunately, the potential to achieve personal identification is high in developed countries with infrastructures that allow sophisticated tracking of citizens, a level of health care that documents identifying features and, as a last resort, recourse to DNA technology. Stranger-on-stranger killings are most problematic for homicide investigators to solve. By contrast, in the investigations of genocide and crimes against humanity involving mass graves there may be less emphasis placed on identifying the individuals who actually did the killing. Rather, the prosecutorial focus may be to identify those individuals in positions of authority who gave the commands to the killers. Actual killing may be carried out by anonymous persons remote from the chain of command. So with regard to mass graves and prosecutions involving war crimes, genocide, and crimes against humanity, personal identification of the victim(s) may not be a necessary starting point to the investigation. Particular persons became victims because of how they were perceived by the culture; for instance, they may have been singled out because of their religion or ethnicity. This categorization of the victim by the killers has consequences for the level of identification sought by investigators. It may be sufficient to be able to attribute categorical identification to the victims (such as ethnicity, religion, or political viewpoint) and to show that victims were killed because of attributes perceived by their killers. This is particularly true when indictments for killings are based on genocide: the deliberate intention to exterminate a national, ethnic, or religious group. For investigators, other categorical levels of identification could rest on whether or not the victims can be identified as civilians, women, children, or combatants. If military or civilians, for example, were they bound, blindfolded, or tortured? The foregoing does not imply that personal identification would not lend a deeper level of support to indictments or to a tribunal’s investigations, only that pursuit of positive personal identification of victims may not be a primary issue to the prosecution. Hence, there may be no resources allocated for that purpose. This legal aim does not necessarily satisfy the needs or desires of survivors to have their individual dead returned. But, in the context of current ad hoc tribunals, the efforts and funding for personal identification of victims often fall upon the shoulders of entities other than tribunal investigators. A sad reality is that positive, personal identifications are often neither pragmatic nor even possible in poor nations and areas suffering from recent conflicts, where the infrastructure has been severely compromised or is nonexistent. Out of nearly 500 individuals examined from exhumations at Kibuye, Rwanda, evidence for identification could be established for only 17 persons; 6 carried identifying documents and 11 more had clothing or personal effects recognizable to acquaintances, none had hospital X-rays or dental records. For only two of these victims could surviving blood relatives be located (Haglund and Kirshner, 1997). In Bosnia-Herzegovina, there are currently 4420 body bags being stored, and awaiting identification (Knight and Rhode, 2001). Notably, the ICTY-investigated Croatian grave at Ovcara, with 200 remains, currently has approximately 150 individuals identified; the majority confirmed via DNA. This relatively high success rate of identification can be attributed to a concerted government effort to identify these victims, combined with the fact that the war left the country’s infrastructure relatively unscathed, and there was a quality forensic community left to follow-up on identifications subsequent to tribunal examinations. Prior to the exhumations, however, 4 years were devoted to collection of antemortem data and there was local access to DNA technology.

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Conclusions Exhumation and examination of victims of a medium to large mass grave are huge undertakings in terms of resources for financing, staffing, expertise, logistical support, and often security. For both the exhumations and examinations, basic infrastructures that are taken for granted in industrialized countries, such as working facilities, storage for remains, water and electrical utilities, are often nonexistent. In areas plagued by war and civil disobedience, suitable equipment and supplies need to be ordered and shipped from other countries. Authority to carry out the work may depend upon changes of government or international will. These complexities translate into the necessity for careful and flexible planning. With the burgeoning amount of forensic experience in mass grave exhumation, we can expect more accounts of exhumations to appear in the peer-reviewed published literature. It is only through sharing of experience by mass grave investigators that we will learn how to better accomplish these investigations.

References Abarinov, V. 1993 The Murderers of Katyn, Hippocrene Books, New York. Anderson, K. 1993 The Anfal Campaign in Iraqi Kurdistan: The Destruction of Koreme, Human Rights Watch and Physicians for Human Rights, New York. Bevan, D. 1994 A Case to Answer: The Story of Australia’s First European War Crimes Prosecution, Wakefield Printing, Kent Town, South Australia. Briggs, D.E. G. 1990 Flattening. In Paleobiology: A Synthesis, edited by D.E.G. Briggs and P.R. Crowther, Blackwell Scientific, Oxford, U.K. Bulletin: International Criminal Tribunal for the Former Yugoslavia 1996 Twin Tribunals ICTY/R, No. 9/10 14-VIII. Danner, M. 1993 The Massacre at El Mazote, Vintage Books, New York. Davidson, E. 1997 The Trial of the Germans: An Account of the Twenty-Two Defendants before the International Military Tribunal at Nuremberg, University of Missouri Press, Columbia, MO. Eher, F. 1944 German Government Report on Vinnytsia, 1944. Based on translation from the Forensic Medical Report prepared by Prof. Dr. Gerhard Schrader, Director of the Institute of Forensic Medicine and Criminal Investigation of the University of Halle-Wittenberg, Germany. Equipo de Anthropologia Forense de Guatemala 1994 Las Massacres en Rbinal: Estudio Historico Anthropologico de las Massacres de Plan de Sanchez, Chichupak y Rio Negro. Ferllini, R 1999 The role of anthropology in human rights issues. In Forensic Osteological Analysis: A Book of Case Studies, edited by S.I. Fairgrieve, Charles C Thomas, Springfield, IL.

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FitzGibbon, L. 1977 Katyn Massacre, Corgi Books, London. Geberth, V.J. 1990 Practical Homicide Investigation: Tactics Procedures, and Forensic Techniques, 2nd ed., Elsevier, New York. Geiger, J. and R.M. Cook-Deegan 1993 The role of physicians in conflicts and humanitarian crises: case studies from field missions of Physicians for Human Rights, Journal of the American Medical Association 270(5):616–620. Haglund, W.D. 2000 Archeology and forensic death investigations, Historical Archeology 35(1):26–56. 1988 The scene and context: contributions of the forensic anthropologist. In Forensic Osteology II, edited by K. Reichs, Charles C Thomas, Springfield, IL. Haglund, W.D. and R.H. Kirschner 1997 Report: Investigations at Kibuye Roman Catholic Church: Kibuye, Rwanda. Prepared for the United Nation’s ad hoc International Criminal Tribunal for Rwanda. Haglund, W.D., M. Connor, and D. D. Scott, 2000 The archeology of contemporary mass graves, Historical Archeology 35(1):57–69. Haskell, N.H. et al. 1997 On the body: insects’ life stage presence, their postmortem artifacts. In Forensic Taphonomy: The Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 319–332. CRC Press, Boca Raton, FL. HITS (Homicide Information Tracking System), Computer Database, Office of the Washington State Attorney General. Courtesy of Robert D. Keppel, Ph.D. Jiménez, S. 1996 Forensic anthropology in Bosnia-Herzegovina: the assembly-line approach, The Connective Tissue 12:7–11. Joyce, C. and E. Stover 1991 Whiteness from and the Grave: Stories Bones Tell, Little, Brown, Boston, MA. Knight, G. and D. Rhode 2001 Warehouse of death, New York Times Magazine, March 11, 2001, pp. 46–47. Koff, C. 1996 Have trowel, will travel: scratching the surface layer, The Connective Tissue 12:8–11. Mant, A.K. 1950 A Study of Exhumation Data. M.D. Thesis. University of London. 1957 Adipocere: a review, Journal of Forensic Medicine. 4:18–35. 1987 Knowledge acquired from post-war exhumations. In Death Decay and Reconstruction: Approaches to Archeology and Forensic Science, edited by A. Boddington, A.N. Garland, and R.C. Janaway, Manchester University Press, London. Nawrocki, S.P. 1995 Cemetery taphonomy. In Bodies of Evidence: Reconstructing History through Skeletal Analysis, edited by A. Grauer, Wiley-Liss, New York. Rodriguez, W.C. and W.M. Bass 1985 Decomposition of buried bodies and methods that may aid in their location, Journal of Forensic Sciences 30(3):836–852.

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Russell, S. and M.A. Flemming 1991 A bulwark in the Pacific: an example of World War II archaeology on Saipan. In Archaeology Studies of World War II, edited by W.R. Wood, pp. 13–28. Department of Anthropology, University of Missouri, Columbia, MO. Scott, D.D. 2000 Firearms identification in support of identifying a mass execution at El Mosote, El Salvador, Historical Archaeology, 35(1):79–86. Skinner, M. 1987 Planning the archeological recovery of evidence from recent mass graves, Forensic Sciences International 34:267–287. Stover, E. 1997 The grave at Vukovar, Smithsonian 27(12):7–25. Stover, E. and A. Manuel 1991 Getting Away with Murder, Americas Watch and Physicians for Human Rights, Human Rights Watch, New York. Stover, E. and G. Peress 1998 The Graves: Srebrenica and Vukovar, Scalo, New York. Stover, E. and M. Ryan 2001 Breaking bread with the dead, Historical Archeology 35(1):7–25. Taylor, T. 1992 The Anatomy of the Nuremberg Trials, Alfred A. Knopf, New York. Thieren, M. and R. Guitteau 2000 Identifying cadavers following disasters: why, Disasters: Preparedness and Mitigation in the Americas 80:1. United Nations 1997 Manual on the Effective Prevention and Investigation of Extra-Legal, Arbitrary and Summary Executions. United Nations, New York. Washington State 1990 HITS (Homicide Information Tracking System), Office of the Washington State Attorney General. Courtesy of Robert D. Keppel, Ph.D. Zawodny, J. A. 1962 Death in the Forest: The Story of the Katyn Forest Massacre, University of Notre Dame Press, South Bend, IN.

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Taphonomy of a Karstic Cave Execution Site at Hrgar, Bosnia-Herzegovina TAL SIMMONS Contents Introduction Cave Formation Geology Site History and Description Logistics of the Exhumation Differentiation and Exhumation of the Remains Commingling Perimortem Trauma Identifications Conclusions Acknowledgments References

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13

Introduction Interpretation of postmortem, taphonomic processes in some outdoor scenes requires an understanding of geological processes and features. Geomorphologically induced microenvironments coupled with the taphonomic overprint of decomposition processes produce differential preservation, transport of body parts, and perimortem trauma. Remains deposited within vertical caves, in particular, are generally isolated from surface taphonomic processes such as weather and scavengers, but subjected to subsurface, geological taphonomy (Brain, 1975, 1981; Oliver, 1989). These variables provide limits and challenges to the interpretation of postmortem intervals, commingling, and evidence of the cause of death, as well as to the technical issues of scene processing and recovery of remains. In the summer of 1992, early in the Balkan War, a cave in the Hrgar region of northwest Bosnia was used to dispose of approximately 70 individuals who had been executed on the ground surface near the vertical entrance shaft. After they were killed, their bodies were thrown down into the cave where they decomposed and were subject to taphonomic processes unique to this environment. The remains were discovered and exhumed 5 years later in 1997. In 1996, just prior to the Hrgar region exhumation, the State Commission for Missing Persons (Bosniak Entity) had exhumed another vertical cave at Laniˇste. Nearly 200 individuals had been killed and deposited in two separate episodes, one of which was quite recent. Sand had been dumped on top of both sets of remains. The preservation of the bodies near the top (second deposition) was excellent, allowing visual identification of the victims by survivors in nearly all cases. The bodies lower in the cave (first deposition) were less well preserved and remain largely unidentified It was this experience that the State Commission personnel brought to the exhumations at the cave at Hrgar. Excavators expected the same type of preservation and the ultimate recovery of relatively whole bodies. Unfortunately, however, differences between the modes of deposition and geomorphology resulted in much less soft tissue preservation at Hrgar. It is likely that the excellent preservation at Laniˇste was maintained by both the sand covering the bodies and because the cave was an old one, dry and no longer actively forming. Neither of these conditions was met at Hrgar. Not only was the cave there deeper, but it was still in the active formation phase, bringing excessive amounts of water into contact with the remains for a period of 5 years. Further, no attempt was made to cover the bodies dumped there. The cave geology, including the cave type, the depth and width of the shaft, and the existence of the talus cone beneath the aven are key to understanding the taphonomy of the human remains deposited within it.

Cave Formation Geology Geological features of karstic or dolomitic caves and their formation are relevant to a discussion of the taphonomy of the human remains thrown into the cave at Hrgar. C.K. Brain (1975, 1981) provided an early description of accumulated hominid remains in the South African australopithecine cave sites, in one case relating them to the feeding habits of leopards in trees hanging over these karstic avens. Karstic cave systems are part of

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Figure 13.1 Stages of karstic cave formation, beginning from upper left: horizontal lines = dolomite; vertical lines = travertine; stippling = breccia. (Adapted from Brain, C.K., in Archaeological Studies, edited by A.T. Clason, North-Holland, Amsterdam; and Brain, C.K., The Hunters or the Hunted? An Introduction to African Cave Taphonomy, University of Chicago Press, Chicago, IL. With permission.)

limestone and/or dolomite rock formations. As Brain (1975, 1981) describes, their formations proceed in an ordered sequence. While Brain describes six separate stages of formation (see Figure 13.1), only the first four are relevant to the cave at Hrgar. In Stage 1, a solution cavity is formed inside the rock strata. During Stage 2, the water level drops and the cavern becomes filled with air, which may be ventilated to the surface by distant and indirect means. Stalactites and stalagmites may begin to form during this period. The development of the aven (or vertical shaft to the surface) is the hallmark of Stage 3 and is caused by rainwater enlarging fissures in the rock. Brain (1981:7) notes that the passage of this water is accelerated by the presence of the cavern, since the water can drip freely from the roof of the cavern as it percolates down through the joint. Stage 4 witnesses the break-through of the aven to the surface, thus opening the cavern to the external environment. It is during Stages 3 and 4 that a depression may develop in the ground above the forming aven. Trees are plentiful in and around these depressions due to the abundance of water. The Stage 4 cavern begins to fill with debris from the surface and accumulating deposits form a talus cone on the floor beneath the aven. Geologically, the northwest region of Bosnia is karstic with an abundance of both caves and actively forming sink-holes. If one travels along the north–south road connecting the cities of Klju´c and Biha´c (parallel to the border with Croatia), the area can be seen to exhibit wide expanses of grazing land where numerous shallow depressions mark the ground surface. These depressions are filled with trees. The site at Hrgar is located in a geologically similar, although more densely forested region.

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Figure 13.2 Cross section of cave at Hrgar.

Site History and Description In June 1997, in the city of Biha´c in northwestern Bosnia, preparations to exhume the remains of an unknown number of individuals from a karstic cave were begun. At this time, no site exploration had yet occurred, nor had local authorities defined with certainty which of three known cave shafts was the site identified by Serb informants as the mass grave. Local history asserts that on July 11, 1992 a number of prisoners from the nearby Ripa´c concentration camp were released by the Serbs. Those that remained interned, however, were never seen alive again. These individuals were believed to have been executed that same day at nearby Hrgar. There was compelling evidence on the ground surrounding one of the cave shaft entrances to suggest that a large number of people had been killed at this location. Grenade pins and .762 cartridge casings littered the area. This cave was explored in early August by a Criminal Inspector from the Biha´c police who is also an amateur speleologist. Descending into the shaft using a rope and harness, he photographed and videotaped the evidence within the cave. This visual record clearly documents the markings of explosives detonating along the length of the shaft itself as well as the presence of numerous human skeletal remains, remnants of clothing, and refuse on the cave floor. The cave was nicknamed JamaBezdan, or cave without daylight, because the shaft proved to be approximately 80 m in depth, and light adequate for exploration does not reach the cave floor (Figure 13.2). Trees and other vegetation surround the broad entrance and grow along the shaft walls to a depth of approximately 10 m. At this point the aven narrows to a width of 2 to 3 m. The shaft is not completely straight and takes a slight bend about one third of the way down. Its walls are relatively dry in the upper half, but water runs freely down one side of the shaft from this point. One wall of the cave itself is continuously running with water and water drips heavily and steadily from other points in the cave ceiling. The floor of the cave (Figure 13.3) is roughly rectangular, and approximately 4 ¥ 7 m in area, although one

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Figure 13.3 Plan view of cave at Hrgar.

narrow, tall crevice and one wide, low antechamber extend away from the main chamber. The ambient temperature inside the cave is a steady 3 to 4°C and the quality of the air is fresh and circulating. In addition to containing commingled human remains, the cave also held quantities of refuse; it had been in use prior to the war as a municipal and police garbage dump. Once thrown down the shaft, the rubbish formed a talus cone of deposits ranging from 2.0 to 2.5 m higher than the floor of the cave. The area directly under the opening contained the deepest deposits of garbage and was the highest point on the cave floor. These accumulations consisted largely of tires and inner tubes, shattered glass bottles, plastic containers, animal carcasses, unassociated clothing and footwear, leather police belts and web gear, a variety of rusted firearms, old personal identity cards, and a vast quantity of vehicle license plates. The latter proved to be important in the taphonomy of the human remains. The recently deposited corpses had, when thrown into the cave, dropped onto this talus cone and its coating of flat metal license plates (Figure 13.4). The license plates acted like sleds on the slope of the deposits to disperse the bodies, many of which were transported to the far edges of the cave floor with a layer of license plates often accompanying them. In addition, many bodies simply rolled down the slope and became lodged at its junction with the walls of the cave; bodies were frequently layered 4 to 5 deep in these areas as well as at the base of the talus cone. The cave floor topography and differential moisture, along with the accumulating bodies themselves, acted to produce variable microenvironments (Figure 13.5). Bodies

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Figure 13.4 License plates removed from the cave at Hrgar. They contributed to dispersion of remains.

exposed on the surface were less well preserved. Almost no articulated remains were found in the top layers. In several articulated bodies found on the slope, clothing and the skeletal remains within appeared stretched to an abnormal length from the effects of decomposition on the steep slope. As decomposition continued in some individuals, the crania and other extremities separated from the trunk and subsequently rolled down the slope. This taphonomic progression was evidenced by the presence of scattered extremity elements in the lower and flatter portions of the cave floor. This area contained many crania that were clearly supernumerary to the complement of skeletonized individuals. Nearly all the remains were completely skeletonized. It is likely that soft tissue decomposition was enhanced by the high moisture levels and dripping water within the cave during the 5 years since their deposition. The contributions of mammalian scavengers to the decomposition process were minimal as the depth of the shaft provided a protected environment. Although several mice and one frog were noted living in the cave shaft at the time of excavation, no evidence of rodent gnawing or carnivore chewing was noted on any of the remains. The activity of nematodes and other insects, however, clearly contributed greatly to the decomposition process. During the exhumation, the earthworm population of the cave was abundant and manifested robust health. A few bodies contained significant amounts of dry adipocere and, in some cases, recognizable muscle and skin tissue. Bodies exhibiting the best preservation were found in the shallow antechamber (see Figure 13.3) of the cave, where because of its greater distance from the aven it was a drier even more protected environment. Only one individual retained a desiccated brain while

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Figure 13.5 The lower, flat portion of the cave floor during the first few days of the exhumation.

another retained some discernible organ structure (the diaphragm and intestinal mesentery). No detectable odor of decomposition was present during the exhumation.

Logistics of the Exhumation During the course of 14 days in the second half of August, the site of Hrgar Jama-Bezdan was prepared for exhumation by the 5th Corps of the Bosnia-Herzegovina Army (Figure 13.6a). The area surrounding the cave entrance was assessed for de-mining; no mines were detected. All of the trees surrounding the shaft were bulldozed and an extensive, covered wooden platform was constructed over the opening in order to support and shelter the machinery necessary for descending into the cave (Figure 13.6b). The logging road which gave access to the site was regraded and new gravel roads were constructed in the site area itself. Canvas army tents were pitched and designated for specific purposes: housing the generators, storage for recovered remains, an autopsy area, changing areas, meeting areas, storage for identified remains, etc. Latrines were dug. A campfire kitchen and eating area was established. An ambulance and crew were always on site. An army and police checkpoint was established at the site entrance off the logging road. The exhumation began on September 1 and remains were recovered through September 12, 1997. Descent into and ascent out of the cave were accomplished by means of an electrically driven winch and pulley system which raised and lowered a covered metal mining cage

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(a)

(b)

Figure 13.6 (a) Hrgar cave opening prior to logistical preparations and removal of remains. (b)

Entrance to Hrgar cave following logistical preparations. The wooden platform was constructed over the opening in order to support and shelter the machinery necessary for descending into the cave.

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by means of a steel cable. This system was operated by a career army engineer who was in radio contact with members of the exhumation team during transport and as they worked in the cave. Other police officers, members of the exhumation team, were also in radio contact with the workers below. The geology often interfered with radio transmissions, however, but in these instances shouting would attract the attention of those on the platform above. The process of getting into and out of the cave took between 6 and 10 minutes in each direction. Four adults could squeeze into the mining cage at a time, and one of these was always the speleologist. His job was to maneuver the cage past the bend in the cave shaft by physically pushing it away from the walls. All exhumation team members were equipped with warm clothing, rubber boots, Tyvek™ suits, rubber or latex gloves, hard hats, and battery packs connected to headlamps. Additional light was provided by one stationary and one mobile reflector lamp; however, the lighting was usually inadequate to the task. Any area of the cave not illuminated directly by the reflector lamps was extremely dark. The excavation of remains was accomplished using trowels and buckets to remove surrounding soil and debris. The garbage and dirt were placed into body bags which were rolled into a canvas tarpaulin. The tarp was then secured to the outside of the mining cage with ropes and taken to the surface with the speleologist inside the cage. All such material was sorted on the surface by other members of the exhumation team. Once remains were excavated, they reached the surface in the same manner. Between 1 and 14 body bags containing human remains were brought to the surface daily. Due to logistical constraints and level of documentation decisions made by the State Commission team (for example, lack of both mapping and body part inventories), subsequent resolution of issues relating to minimal numbers of individuals and the ability to re-attribute remains to particular individuals was severely hampered.

Differentiation and Exhumation of the Remains Due to spatial constraints and the poor lighting quality, only a maximum of five or six members of the team could work in the cave at one time. Effective work time for any individual was also reduced by the cold temperatures and wet conditions to about 3 to 5 hours a day; for example, working along certain walls of the cave caused the Tyvek suits to become saturated with water in a matter of a few hours. Returning to the cave after a period of absence, with or without the work of another team having taken place between visits, was very disorienting. The poor light and pervasive mud made it very difficult to relocate and redefine characteristics of the work area, including individual bodies, clothing, and the relationships among them. Work thus proceeded slowly at the beginning of each group’s shift. A large quantity of cow and goat bones, as well as several decomposing animal hides, were present in the cave. All parts of the animals were represented, but terminal phalanges and hooves, caudal vertebrae, and horn cores (waste elements in food production) dominated the assemblage. The first tasks of the exhumation team were to delimit individuals and to clear refuse away from the remains. Much of the garbage consisted of loose clothing, inner tubes, and leather belts, all of which had become entangled with the remains during deposition and decomposition. Defining and differentiating individuals were difficult due to poor light, water-saturated and mud-coated clothing, and the entangling garbage.

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Commingling The sliding and rolling taphonomic processes described above also contributed to the excavation complexity. Because most of the crania were shattered (see discussion below), cranial fragments could not be associated reliably with particular individuals. When skeletal remains with associated clothing were superimposed on one another, it was troublesome to distinguish where one body began and another ended. Similarly, when remains lacking clothing were overlain in this manner, the decomposition process had caused the bones of one individual to sink into the remains of the one below and become commingled. For example, bodies H-J 58 and H-J 59 found in the lower, antechamber part of the cave were both subadults of approximately the same epiphyseal age; separating these two individuals was difficult. The positions that the bodies had assumed during decomposition made excavation problematic. Several individuals were thoroughly entangled with other bodies and webbing gear. In one instance the skeleton was supine with the knees bent upward. The entire individual from the proximal femora to the skull was free of surrounding mud, but the lower legs and feet were still covered by mud and the bodies of other individuals. The excavator had to choose either to slide a hand down the tibiae and fibulae in order to locate the feet, or to try to excavate the other bodies from over them first. In this instance, the excavator was able to determine that the bones of the feet were encased in socks and shoes, thus ensuring that all the elements would be recovered. She, therefore, opted to pry the legs and feet out from under the other bodies. Isolated skeletal elements could not be reliably associated with a specific individual skeleton during the exhumation process. These elements, including isolated crania and halves of bodies that had decomposed on the slope, were collected in separate body bags. Positions and associations of remains were not mapped. During examination and analysis in the morgue, a few matching element pairs were identified. The majority of isolated elements, however, could not be reassociated with a particular body. A total of 83 body bags (containing the remains of approximately 70 individuals) were recovered from the cave at Hrgar. The remains were examined on site by forensic anthropologists and pathologists during the 2.5 weeks following the exhumation. All the individuals were male and ranged in age from 16 to 65 years. In addition, a few fragmentary cranial and foot bones of a 3- to 5-year-old child of indeterminate sex were found associated with two small rubber boots and a red sock.

Perimortem Trauma Although only one bullet was recovered from a body (H-J 56, lodged between the clothing and the sternum), perimortem injuries at Hrgar consisted primarily of gunshot wounds which were easily distinguished from taphonomic modifications. This finding is consistent with the presence cartridge casings on the surface of the site surrounding the entrance to the cave shaft. Forty-nine sets of remains exhibited gunshot wounds and the cause of death was attributed to either single or multiple gunshot wounds in 45 cases. Five bodies exhibited a combination of perimortem trauma, including gunshot wounds and blunt-force trauma, the latter always inflicted to the cranium. Three cases exhibited only blunt-force trauma

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Figure 13.7 Blunt-force trauma to the frontal bone. The arrow indicates a piece of the instrument, a rock, still embedded in the cranium.

to the cranium. One case (H-J 52) exhibited penetrating sharp-force trauma to the cranium with an implement consistent with the size and shape of a screw driver. Ligatures of varied types (rope, wire, portions of a leather belt, etc.) were present on several, but not all of the bodies. One of the greatest difficulties during autopsy was distinguishing deliberate, perimortem blunt-force trauma from injuries the corpse might have sustained from being thrown down the cave shaft; for example, there was a reasonably large portion of a jagged rock embedded in the frontal bone of one victim (Figure 13.7). It was determined that this was an example of deliberate blunt-force trauma; while many loose rocks of that type exist on the surface of the ground, none are to be found within the cave shaft, which is smoothwalled limestone. It was also difficult to reconstruct circumstances where a glancing impact with the cave shaft walls would have produced this type of focal trauma. Most crania were fragmentary. Discriminating gunshot trauma from that due to impact with the walls and/or bottom of the cave required that the crania be reconstructed. This process revealed that most, if not all, of the trauma seen in the crania and other skeletal elements was patterned and had resulted from bullet impact. Likewise, the examiners found no evidence (such as impact or compression fractures to the legs or vertebrae) to support the contention that some of the victims had been thrown into the cave alive.

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Identifications Family members of the missing viewed the remains and identified their relatives primarily based on recognition of unique items of preserved clothing, in some cases a waistband mended in red thread, the pattern of a hand knit sweater, etc. In all, names were associated with 45 of the bodies recovered at the site of Hrgar, Jama-Bezdan. All the named individuals were males between the ages of 18 and 55 years at the time of their deaths in 1992. These individuals, as well as the remains of the unidentified, were buried on October 5, 1997.

Conclusions Understanding the karstic cave formation processes, the role of flowing, seeping, and dripping water, and the constant temperatures deep in the ground are integral to the taphonomy of the human remains within the Hrgar, Jama Bezdan, cave. The transport and dispersal effects of the talus cone and the layer of license plates played a major role in the ultimate positioning of the bodies and separated elements. Taphonomic differences were produced by microenvironmental variation: whether the body lay nearer or farther from one of the wet walls; whether it was nearer the top or the bottom layer of bodies; or whether it decomposed on a flat surface or the talus slope. Remains on the talus slope and on the lower surface were completely skeletonized, while remains underneath these others often contained some adipocere. Bodies in the main cave chamber, exposed to constant moisture, were predominantly skeletonized. Bodies that had been deposited in the drier antechamber exhibited greater preservation, including some mummified skin and muscle, dry adipocere, and occasionally recognizable soft tissue structure. Distinguishing deliberate perimortem trauma from circumstantial injury sustained by bodies in the depositional phase necessitated careful reconstruction of all fragmentary remains. Through this process at autopsy, the forensic anthropologists and pathologists were able to conclude that none of the perimortem fracture injuries could be clearly attributed to the depositional process itself, but resulted from gunshot wounds and/or deliberate blunt force trauma.

Acknowledgments The exhumations at Hrgar were logistically challenging, physically taxing, and emotionally draining for all personnel involved. I would, therefore, like to express my appreciation to the members of the Bihac Expert Team, in particular to Kriminalni Inspektor Ermin ˇ Lipovi´c, the amateur speleologist of the Biha´c police. Thanks also to Dr. Samira Mesic, Mr. Amor Ma´covi´c , Mr. Esad Bajramovi´c , and Judge Adem Jakupovi´c for fulfilling their roles at Hrgar. I am very grateful for the assistance of a rapidly and temporarily assembled Physicians for Human Rights team (Dr. Page Hudson, Dr. Onder Ozkalipci, and Ms. Ann ˇ Ross) during the autopsy phase. Finally, my gratitude is expressed to Mr. Zlaya Sabanovi´ c and Ms. Elvira Taluroviˇc of Physicians for Human Rights in Tuzla, who ostensibly acted as my translators, but who, in reality, provided invaluable assistance throughout the exhumation and identification processes, respectively.

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References Brain, C.K. 1975 An introduction to the South African australopithecine bone accumulations. In Archaeological Studies, edited by A.T. Clason, pp. 109–119. North-Holland, Amsterdam. 1976 A reinterpretation of the Swartkrans site and its remains, South African Journal of Science 72:141–146. 1981 The Hunters or the Hunted? An Introduction to African Cave Taphonomy, University of Chicago Press, Chicago, IL. Oliver, J.S. 1989 Analogues and site context: bone damages from Shield Trap Cave (24CB91), Carbon County, Montana, U.S.A. In Bone Modification, edited by R. Bonnichsen and M.H. Sorg, pp. 73–98. Center for the Study of the First Americans, Orono, ME.

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Mass Graves and the Collection of Forensic Evidence: Genocide, War Crimes, and Crimes against Humanity

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STEFAN SCHMITT Contents Introduction Defining “Mass Graves” Witness Testimony — Cornerstone of Mass Grave Forensic Analysis Approaches to Mass Grave Location and Evidence Collection Location of Mass Graves by Trenching Example of Trenching: El Maguelar, Honduras Location of Mass Grave by Sniff Probe Method Example of Sniff Probe Burial Location Method: Pakracka Poljana, Croatia Surface Evidence Example of Surface Evidence Collection: Koreme, Iraq Approaches to Documentation Labeling, Inventory, and Determining Minimum Number of Individuals Minimum Number of Individuals: Examples from Plan de Sanchez, Guatemala, and Kibuye, Rwanda Identification Issues: Examples from Chichupac, Guatemala, and Koreme, Iraq Mass Graves and Taphonomic Evidence: Illustration from Chichupac, Guatemala Conclusions References

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Introduction Individual responsibility is one of the cornerstones of international criminal law. Genocide, war crimes, or crimes against humanity, are all crimes for which an individual can be prosecuted. Legally, the concepts of war crimes and crimes against humanity had been established by the time the Nuremberg International Military Tribunal took up its work prosecuting Nazi war criminals in 1945 (Neier, 1998). The crime of genocide was first adopted by the United Nations General Assembly on December 9, 1948, in its Resolution 260 (III) (U.N.T.S., 1951). Articles II and III of the Convention on the Prevention and Punishment of the Crime of Genocide present a definition for genocide and which acts are punishable under this definition. Since this time, war crimes and crimes against humanity have been further elaborated in the Geneva Conventions of 1949, which were expanded in 1977, adding among other things the phenomena of internal armed conflicts. These conventions are today generally accepted as customary international law (Neier, 1998). Crimes against humanity encompass a broader spectrum than war crimes, which are restricted to crimes against combatants or nationals of a hostile power or an occupied territory. As Neier (1998:17) describes: In contrast, the concept of crimes against humanity applies only to crimes committed on a large scale. A defendant charged with crimes against humanity may be convicted only if the prosecution establishes the connection between the particular crime and a broad pattern and practice of the commission of such crimes for reasons of political, ethnic, or religious persecution. Accordingly the evidentiary burden on prosecutors is far greater when they prosecute a defendant for crimes against humanity than when they must demonstrate to a court the commission of a war crime.

These factors also apply to the crime of genocide, where the “intent to destroy, in whole or in part, a national, ethnical, racial or religious group…” (U.N.T.S., 1951) has to be demonstrated in order to support the accusation of genocide. Such an accusation implies organization on a higher level, such as would be provided by a government. The concept of a “broad pattern and practice of the commission of such crimes for reasons of political, ethnic, or religious persecution” (Neier, 1998:17) also applies to the documentation and collection of evidence of what is generally termed as human rights violations. To prove the violation of human rights, which generally are committed by a government against its citizens, a pattern of such practices has to be documented. Since civilians are often the ones who commit such crimes, establishing a direct link to a government order might be difficult.

Defining “Mass Graves” Before discussing how mass graves can provide evidence for war crimes and/or genocide, the term should be defined (also see Haglund, this volume). Some authors define it by the number of individuals; for example, Skinner (1987) suggests that a mass grave must contain at least six individuals. Mant (1987) limits the term to sites where two or more bodies physically touch each other. These definitions depend on the technical and physical characteristics of the grave itself. A more holistic definition is needed, however, which includes

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the anthropological context. It is this context that focuses and defines what evidence should be collected and which methods should be used to excavate. From this perspective, a mass grave can be defined as one that contains the remains of more than one victim who share some common trait connected with the cause and manner of death. Using this definition emphasizes the importance of social context along with the forensic determination of manner of death. Some mass graves are the result of homicide; others, including many mass disasters, for example, are the result of an accident. Deaths from either may be examined forensically. In homicide-related mass graves the forensic investigation involves criminal wrongdoing. In some accident-related mass graves the forensic investigation may involve civil litigation, such as issues with insurance. Both are medicolegal, forensic types of scene investigation. In other, non-forensic, accident-related mass graves, the investigation may be purely archaeological; for example, the excavation of the volcano victims from Pompeii or the australopithecine “first family” group from the African Pliocene who may have been flash flood victims. The putative manner of death and its social determinants form the core of the investigation and drive choices about the techniques and approaches to the excavation, including the types of evidence sought and methods for finding it. The forensic anthropologist, trained in linking cultural behavior, human biology, and archaeology, brings a holistic perspective to mass grave examination and analysis. This chapter treats mass graves concerned with criminal or homicide-related mass murders due to war crimes or genocide. In these situations the victims share, or are perceived to share, some kind of common trait which justifies the homicides in the minds of the assassins. Therefore, a mass grave of this type is not so much defined by the number of individuals buried, but rather by the sharing of a common trait that led to their deaths. Such criminal mass graves are frequently not secret. In Guatemala, for instance, mass graves of the 1980s military’s anti-insurgency campaign are referred to as clandestine graves, implying that their locations are secret or unknown. The secrecy, however, lies not in their locations but in the repression of any acts that might commemorate the event that led to the mass fatality. That is, survivors often know very well where their loved ones lie; they are just not allowed to acknowledge the event that led to the death by performing religious ceremonies or decorating the grave site. The trauma caused by this proscription enhances the terror under which survivors live. They are constantly reminded of their subjugation by the fact that they cannot mourn their dead and openly acknowledge the injustice done to them. Because of ongoing repression, perpetrators initially do not need to cover up their deed by burying the evidence. In fact, mass graves are often created by others, nonperpetrators, doing the clean-up work, rather than trying to hide the evidence of a crime. The reasoning behind this lies in the justification the perpetrators feel they have in killing the victims: in other words, “Why hide what is right?” As time passes and circumstances change, efforts may then be made to hide evidence, but generally not at the time the crime is committed. To summarize then, criminal mass graves contain the remains of a group of individuals who share some common trait that justified their assassinations in the eyes of the perpetrators. Additionally, mass graves often are not secret in the sense that knowledge about them exists, even though the exact geographical location might still need to be determined scientifically. This two-point definition has methodological consequences when investigating what is assumed to be such a grave.

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From a taphonomic standpoint it introduces the human as an agent of perimortem and postmortem changes. That is, the process from the selection of the victims to their killings and interments becomes evident taphonomically when exhuming such a mass grave with a holistic anthropological approach. Forensic anthropology then has to go beyond the mere investigation of the grave itself and also has to include the context in which the grave was produced. The following discussion and presentation of case examples elaborate this point.

Witness Testimony — Cornerstone of Mass Grave Forensic Analysis The cornerstone of mass grave forensic investigation is witness testimony. As described above, a mass grave is seldom a secret. All of the mass graves in the present study were located with witness information. The witnesses were generally survivors of the massacres themselves who had managed to get away, or people who had helped bury the remains. An example of the importance of witnesses is the mass grave discovered by forensic anthropologist Clyde Snow at the Ovcara farm which contained the victims from the Vukovar Hospital. He found the grave after listening to the story of one of the intended victims who managed to jump off the truck that was taking him and others from a farm equipment building, where they had been taken after being removed from the Vukovar Hospital to what was later confirmed to be a mass gravesite. The grave was exhumed by a forensic team from Physicians for Human Rights who were under contract to the United Nations International Tribunal for the former Yugoslavia in 1996 (Stover and Peress, 1998). Witness testimony frequently leads investigators to the grave location, and may provide collaborative evidence about the circumstances that led to the fatality incident. Witness testimony also may provide the basis for the accusation that the massacre was part of an organized effort to eradicate, in whole or in part, such a group of people. The corroboration (and speaking in the objective language of science, the negation) of such testimony becomes the goal of the exhumation.

Approaches to Mass Grave Location and Evidence Collection The exhumation of human remains from a mass grave uses archaeological techniques to test witness testimony. Such efforts occur in 5 phases: (1) the grave location and survey; (2) excavation; (3) collection and documentation of evidence; (4) analysis; and (5) reporting. This chapter focuses particularly on phases 1 and 3, including approaches to grave location, locating circumstantial evidence, labeling, estimating minimum numbers, and associating artifacts. Location of Mass Graves by Trenching The first step lies in determining if a mass grave actually exists at the suggested location. Eyewitnesses very rarely remember the exact location of a grave. In the best case, the grave may have been marked by people who buried the victims, but often this has not happened. Trenching can be used to find a grave, define its boundaries, and confirm that it contains human remains. Use of a probe is another method utilized to confirm the presence of decomposing tissue. All other methods, such as ground penetrating radar or cadaver dogs

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Figure 14.1 Site diagram for El Maguelar, Honduras (not to scale).

(trained to alert to the scent of buried, decomposing material) may indicate the presence of human remains, but they cannot rule out their absence. That is, one might use them, not get positive results, but still not be able to clear the site with a measurable degree of certainty. Trenching is the most reliable method of locating a mass grave because it allows confirmation of the presence or absence of human remains in a specific area without a complete excavation. Trenches can be dug using either human or mechanical power, such as a backhoe in some cases. Traditional archaeologists may be reluctant to utilize untrained human power or a backhoe because of the risk of damaging evidence. However, due to limited resources and time, which are often extreme, this possibility has to be balanced against the risk of not undertaking or completing the excavation. The remedy is to document damage if it occurs. Postmortem trauma is usually distinguishable from perimortem trauma, particularly if the excavator notes that it occurred. The responsibility then lies with the forensic investigator to make sure that every step of the process of discovery is documented meticulously. Example of Trenching: El Maguelar, Honduras A good example of the use of trenching and untrained manual labor is the 1995 excavation at El Maguelar in Honduras. The investigation was carried out to determine whether two bodies found alongside the road leading to El Maguelar on April 18, 1988, were union leader Rolando Vindel and former vice president of the National Lottery, Gustavo Morales. Both reportedly had been kidnapped by the military on March 18, 1988 (Anon., 1995). The discovery of the bodies in 1988 led to a semi-judicial inquiry with a minimal postmortem examination taking place beside the road where they were found. The judge decided to re-bury the bodies in the same location, a rather common practice in Honduras at the time. Witness testimony pointed to the presence of this grave in an area of approximately 25 ¥ 50 m (Figure 14.1). Since this constitutes an area of approximately half a football field, the task of trenching and clearing it of underbrush was considerable (Figures 14.2, 14.3, and 14.4). For this purpose the Special Human Rights Attorney of Honduras, Sonia

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Figure 14.2 Beginning excavation utilizing trenching methods at El Maguelar, Honduras.

Figure 14.3 Completed excavation showing trenches at El Maguelar, Honduras.

Figure 14.4 Overview of banana grove including area ‘e’ trenches (covered with tarpaulin). © 2002 by CRC Press LLC

Dubón was asked to hire 30 people. They were hired from the surrounding area; most of them were farmers and thus used to hard, physical labor. Reliable eyewitnesses did not become available for 3 days, during which excavation had commenced. It was decided to trench across the entire area pointed out by several villagers who claimed to have witnessed the burial of the bodies under supervision of the then Justice of the Peace. Each trench was separated by no more than 1.5 m, assuming this would not likely exceed the length of the disturbed area of the grave. The trenches were parallel and dug to a depth of 1.2 m where water was encountered and digging was impossible. Over the next 3 days, 5 major trenches were dug 30 m long, with 1.5 m separation between them (Figure 14.1, Area A) along with four minor trenches 9 m long with 1.0 m separation (Figure 14.1, Area B). Before taking the next step of perpendicular trenches, dug in a checkerboard fashion, and thus definitely ruling out or finding the grave in the berms between the original trenches, early in the morning of the fourth day one of the workers uncovered one of two crania in one of the trenches of Area C (Figure 14.1). This area had been pointed out by the man who had actually buried the remains, a witness that appeared on the third day the dig was in progress. The crania were located at a depth of 2.20 m. As it turned out, an access road had been built and approximately 1 m of fill had been placed over the gravesite. The grave was located, outlined, and the skeletal remains of two individuals were exhumed (E.A.F.G./P.H.R., 1995). Location of Mass Grave by Sniff Probe Method Metal probes that are equipped with a T-bar on one end, measuring approximately 0.6 cm in diameter and 1 m in length, can be inserted into the ground in an area where one suspects the presence of a grave. The differences in subsurface resistance (i.e., the probe can be inserted easier in one area than in another, indicating disturbed soil) or the presence of the odor of decomposing flesh on the end of the probe when it is withdrawn might indicate the presence of buried human remains (Killam, 1990). Trenches are still necessary in order to confirm or rule out burials. Example of Sniff Probe Burial Location Method: Pakracka Poljana, Croatia Probes were used during the forensic exhumation in 1993 of several bodies near the town of Pakracka Poljana, Croatia. The area to be investigated consisted of several hundred meters of grassy field along a road. A backhoe was utilized to dig several trenches at intervals along the road. Probing was an additional technique utilized in locating the graves. The bodies were suspected to have been buried in this area between August, 1991 and March, 1992. Considering they had been buried for a little over a year, one could assume that soft tissue was still likely to be present. The probe proved very successful in this case. A total of 19 individuals (16 males and 3 females) were exhumed from 9 separate graves, which were located this way (Report, Physicians for Human Rights, 1994). Surface Evidence Although the perpetrators may have left the scene of the crime quite some time ago, the grave is probably the best snapshot of what happened. That moment in time is in some way preserved, because the bodies have been isolated from further human manipulation by burial.

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Some evidence may be located outside of the grave. This evidence is circumstantial, i.e., not directly associated with that evidence encountered in the grave; however, its location and the pattern it presents in conjunction with supporting witness testimony might indicate its relationship to the contents of the grave, and be critical to the reconstruction of events. Example of Surface Evidence Collection: Koreme, Iraq A good example of the pattern of evidence located outside of the grave proving to substantiate witness testimony is the incident investigated by the forensic team organized by Physicians for Human Rights and Human Rights Watch in 1992 at the village of Koreme in Kurdistan, northern Iraq. It involved the exhumation of two mass graves containing the skeletal remains of 27 men executed by the Iraqi military on August 28, 1988. Careful documentation and analysis of the spatial distribution of cartridge cases collected near the alleged execution site as well as an analysis of the firing pin patterns on each cartridge brass allowed reconstruction of the minimum number of weapons used, minimum number of shots fired, and the spatial relationship between the shooters and the victims (Scott and Connor, 1997). These details could then be compared with witness testimony.

Approaches to Documentation Each grave is unique, and flexibility is essential to approaching an exhumation. Unlike a historical archaeological excavation, time and resources are usually more limited, having direct consequences as to which techniques are selected. In this way forensic mass grave excavation bears a strong resemblance to survey archaeology. Features of the grave itself influence the techniques utilized to exhume them, particularly the extent of decomposition. It is important to ascertain the progress of disarticulation, as well as the preservation of outside coverings or clothing that may hold skeletal elements together. Preservation of soft tissue translates into the state of articulation of the remains, and, in turn, how recovery units need to be defined; for example, soft tissue preservation limits commingling. Labeling, Inventory, and Determining Minimum Number of Individuals The archaeological identification of remains and artifacts, as well as their labeling and inventory, are the first steps in determining what a mass grave contains. They are essential in determining the minimum number of individuals (MNI) present, especially if they are anatomically disassociated or commingled. What the excavation team recovers, labels, and inventories ends up being analyzed as a unit by the team that carries out the postmortem examinations. The postmortem examination team frequently must revise the initial findings once the autopsy has been completed. A numbering system is needed which is flexible enough to allow revisions to be made without major complications, i.e., without having to relabel remains, containers, documentary photographs, and evidence lists. With this in mind, the following labeling system seems to be the most appropriate. Each item bears a label including (1) a short acronym for the site, such as RN for Río Negro; (2) a roman numeral for each mass grave at the site; and (3) an Arabic number for each anatomically articulated or associated set of remains.

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Figure 14.5 Grave III at Chichupac. Disturbed grave site with evidence of re-depositing of remains as can be seen from the long bone assembly.

Anatomically disassociated or partially associated remains present a problem. Although the emphasis at the excavation site is on keeping anatomic assemblages together, the setof-remains number may not be correct in the final analysis. It is an arbitrary label based on the excavator’s decision of association in the field. Anatomically disassociated remains are numbered individually, but in such a way as to convey associative information. If the site is divided into arbitrary levels and quadrants, the disassociated skeletal remains can be labeled according to the quadrant and level from which they were extracted. This is more efficient than numbering each bone and then trying to document associations through photography alone. Individual element numbering, if necessary, can be reinstated later under laboratory conditions. For example, see Figure 14.5. This photograph of Grave III located close to the village of Chichupac in Guatemala shows one of the disturbed graves. It is apparent from the long bone assemblages that some type of re-depositing has occurred, something corroborated by the owner of the cornfield in which the graves were located. Utilizing the principle of numbering crania first, the skeletal assemblages and artifacts were numbered according to the crania they were closest to or according to the sector in which they were found. It is recommended that any artifacts encountered in association with labeled remains be kept with them until the postmortem examination. Labeling of artifacts and remains must be done in the grave, prior to the actual exhumation. This is documented thoroughly by photographs and, if time permits, sketching and mapping. The labeling has to be backed by an inventory. An inventory form is created for each label given, and these are filled out as the remains are extracted from the grave, requiring a preliminary determination of what is present. The remains then should be individually packaged and the bag marked with the appropriate label. At the end of an exhumation, one then should have a set of inventory forms to match each individual bag. The inventory forms can be revised by the team carrying out the postmortem examinations, initially serving to confirm that a labeled bag contains no less than what it says it does. This is important for the exhumation team to keep in mind. Analysis of what is

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found is to be kept to a minimum by them, and items labeled only when reasonably sure of the finding. If a bag contains less than what it says it should, by virtue of a graveside identification error, it might suggest to the examination team or to the court that evidence was lost. Obviously, a bag might very well contain more than what was initially inventoried by the exhumation team. This might simply happen due to breakage during transport, or because remains were not clearly visible at extraction. An example of discrepancies between the exhumation team inventory and the examination team analysis is the many, partially decomposed and disassociated infant remains recovered by the forensic team for the International Criminal Tribunal for Rwanda at the mass grave in Kibuye, Rwanda, in 1996. They were so small, often enveloped in the mother’s clothing, and encased in adipocere that often they were packaged with the remains of an adult without being inventoried. It was not realized until the postmortem examination. The inventory form should not only provide insurance that no mistakes were made during the exhumation process, but also allow the possibility of revision by the postmortem team. Revision presents two possibilities: (1) there is less content in the bag than documented on the inventory form, or (2) there is more content in the bag than documented on the inventory form. In the first case, an investigation has to be launched to determine what error occurred along the line and then rectify and document it according to what is found. The second possibility often requires a change in labeling in order to adjust the inventory. If an extra set of remains, undocumented in the initial inventory is found, this can simply be corrected by creating a second identifier, based on the original one, such as adding a letter to the end of the original one and adding another inventory form to the records. Minimum Number of Individuals: Examples from Plan de Sanchez, Guatemala, and Kibuye, Rwanda The case of several mass graves in the village of Plan de Sanchez, Guatemala, investigated by the Guatemalan Forensic Anthropology Team/Equipo de Antropología Forense de Guatemala (E.A.F.G.) in 1994 demonstrates the importance of inventory keeping. Testimonial accounts stated that on Sunday, June 18, 1982, the military came to the small village of Plan de Sanchez where they blocked off the road. All the people who were returning from the market in the town of Rabinal, some 9 km away, were detained in a house alongside the road. Later in the day the military opened fire on the house and several grenade detonations were heard. Shots were also heard from 5:00 to 9:00 p.m., at which point the house with the bodies in it was set on fire. The next day surviving family members put the fire out. Permission was asked of the military to bury the bodies. The charred remains were buried in several shallow graves. Several women who had been raped and then shot, but had not been burned, were buried separately. Based on interviews with surviving family members who were willing to come forward, at least 99 people lost their lives during this incident (E.A.F.G., 1995a). At the time of exhumation, the remains ranged from complete to partial skeletons, commingled, charred, and fragmented. In order to determine the minimum number of individuals, an inventory was kept of all long bones, maxillae, and mandibles. Once the remains reached the laboratory for analysis, it became clear that a simple counting of bones was not sufficient. Many bones encountered were fragmented. This meant that potentially one might count the distal fragment and proximal fragment of the same right femur as

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two individuals. Hence, each long bone was divided into three units, each representing 33% of the bone. Over 50% of that third had to be present in order to be counted. A femoral head or a distal epiphysis of a long bone by itself was not counted, because most of the bone itself was missing and possibly could turn up somewhere else. The cranial vault, maxilla, and mandible were divided into the left and right halves, and the innominate was divided into its three components: left and right ilium, ischium, and pubis. At Plan de Sanchez the element recorded with the highest frequency was the proximal third of the right femur, which appeared 84 times, suggesting a minimum of 84 people exhumed (E.A.F.G., 1995a). This example demonstrates that an inventory starts out in the grave with the archaeological team and then is revised during the postmortem examination. The inventory depends very much on the condition of the remains. In the case of Plan de Sanchez, due to the burning, it was necessary to divide individual bones into separate analytical units in order to avoid duplication. When recognition and identification of individual body parts or bones during exhumation are difficult due to commingling, partial decomposition, and presence of adipocere tissue, such as it was in the case in the mass grave in Kibuye, Rwanda, the inventory becomes even less precise. In this situation, we reverted to counting what appeared to be the most easily recognized feature (the cranium) to determine the minimum number exhumed.

Identification Issues: Examples from Chichupac, Guatemala, and Koreme, Iraq Artifacts such as clothing, jewelry, and identification cards potentially shed light upon the identity of the human remains with which they are found. As indicated above, it is best to package these along with the associated human remains. At a later point their documentation can be completed through photography and inventory. They can be itemized separately from the remains by adding a distinguishing letter or number to the original identifier. For example, artifacts associated with remains XYZ-II-1, could be labeled as AXYZ-II-1-a, b, c, etc. It must be underscored that just because an identifying artifact is found associated with a particular individual’s remains, it does not necessarily mean it belongs to that individual or confirms their identity. An example that points this out occurred in the case of the three mass graves exhumed in the small town of Chichupac in Guatemala by the Guatemalan Forensic Anthropology Team in 1993. During exhumations in Guatemala, it is customary for family members to watch the work in progress. Sometimes a family member might recognize a piece of clothing or other identifying artifact that is believed to belong to the loved one. In Chichupac this happened on several occasion. On one of these, the remains of CH-II-5 were identified by a family member as Francisco de Paz on the basis of clothing. As it turned out, Francisco was reported to be left-handed and a nonsmoker. Skeleton CH-II-5, however, appeared to be a right-handed individual with sufficient stains on his teeth to assume that he was a smoker. The identification based on the artifact was thus incorrect (E.A.F.G., 1993). There are several possible reasons for this mistake. One is that the family member’s memory failed her as to the identification of clothing articles that had spent 11 years in the ground. Another might be that the clothing at some point was switched from one victim to another. This illustrates that associated artifacts are only circumstantial evidence.

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For identification in a population lacking dental records, radiographs, and capacity for DNA testing, it is necessary that a pattern be found which elevates circumstantial evidence to the level of compelling circumstantial evidence. Group patterns may also offer compelling evidence useful for forensic identification. The clothing worn by all 27 victims exhumed from the mass graves at Koreme were the traditional shirt and pants worn by Kurdish men (Middle East Watch and Physicians for Human Rights, 1993), distinguishing them as a distinct ethnic, religious, and in this case possibly even distinct political group from their executioners. This pattern can be considered compelling circumstantial evidence, even if no identifications of the remains themselves were made.

Mass Graves and Taphonomic Evidence: Illustration from Chichupac, Guatemala Taphonomic evidence documented in the excavation and analysis of mass graves can be critical in the corroboration of witness testimony. This can be particularly useful in cases with a complex taphonomic history, including a sequence of events. The massacre at Chichupac, Guatemala is an excellent example. On January 8, 1982, 32 men were pointed out to the military as subversives by 15 men of a neighboring village. They were then detained and taken to the small town hall where they were tortured. Later on they were led up a hill, executed, and buried in two shallow graves (E.A.F.G., 1993). Witness testimony reported that severed fingers, noses, and ears were found later by the villagers in the town hall. One of the surviving widows reported that she and several other women went to the graves a week to 10 days later. Due to their shallow burial, many of the bodies were exposed and the smell was described as being unbearable. They decided to dig another pit into which they dragged several bodies with the help of their hoes. Eleven years later, in May of 1993, the E.A.F.G. was asked to exhume the remains. At the time of the incident the area was forested. During the intervening years the hill had been deforested by slash and burn agriculture; the land had been under cultivation for 5 years. This traditional practice disturbs the top layer to a depth of about 1 m. Trenching revealed the location of three graves on the sloping hillside. These were designated Sites I, II, and III (see Table 14.1). Numerous fragments of clothing were recovered from the surface throughout the cultivated area, suggesting that farming had disturbed the graves. Excavation of the top 90 cm revealed that all three sites contained some partial skeletal remains in approximate anatomical order, some disassociated but arbitrarily grouped elements, and clothing. Between 90 and 125 cm in Site II 10 skeletons in anatomical order were also found, although in unnatural positions, with scavenger damage and one arm missing postmortem. Also found at this level were artifacts and personal effects such as machetes, carrying bags, wallets, and documents. Sites I and III had no remains below about 90 cm. The three sites were arranged on a hillside, with Sites I and III about 1.5 m above Site II. Site I was disturbed by the cultivation in progress, which in Guatemala is done using large hoes with which the soil is aired and made to form mounds in which the corn is

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Table 14.1

Comparison of three sites at Chichupac, Guatemala

Surface Upper excavated layer

Site I

Site II (Secondary)

Site III

Clothing fragments

Clothing fragments

Clothing fragments

1. Partial skeletal remains of three individuals in approx. anatomical order 2. Disassociated remains but belonging to the anatomically arranged individuals found in arbitrary groups, including few small bones 3. Clothing 4. Condition: some burned, most unburned

1. Partial skeletal remains in approx. anatomical order 2. Disassociated remains 3. Clothing

1. Partial skeletal remains not in anatomical order, including 14 crania concentrated in two areas 2. Disassociated remains found in arbitrary groups 3. Clothing

Below 90 cm

1. Ten skeletons in anatomical position, but some flexions not possible in life; one missing left arm postmortem; several with scavenger damage 2. Artifacts and personal effects

Burial pit Disturbance by cultivation in progress

Yes

2.70 ¥ 1.35 cm

Approx. 1.30 ¥ 1.80 m

No

No

planted. The mounds are occasionally reformed and secured to provide the necessary support for the corn to grow. The condition of the remains suggested many bodies must have been interred superficially, i.e., within the top 90 cm, susceptible to damage by the agricultural processes. Even after the reburial and grave reinforcement by the widows, cultivation of the land had caused the fragmentation and disassociation of the remains and clothing found in all three sites. Several of the skeletal elements were found to have been burned, leading to the conclusion that they were on the surface when the land was made agriculturally useable by the slash and burn method used by Guatemalan peasants. In addition, the arbitrary groupings of mainly larger bones suggested they had been exposed during agriculture, recollected by the peasants (who may have easily missed or ignored the smaller bones), and reburied in the general area known to contain the original graves. The condition of the remains in the deeper layer of Site II suggests they had minimal disturbance, but that burial had taken place after decomposition had loosened the articulations. The remains were in anatomical association, but in positions impossible prior to

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decomposition. Evidence of scavenger damage, including a missing left arm, supports the interpretation that this burial took place following a period of decomposition and exposure, especially in view of the fact that the body with the missing arm also was the one lowest in the grave, i.e., it must have been one of the first ones to be redeposited into Site II. It, therefore, must have come from a top layer of either Site I or Site III and, thus, was the one most exposed to any scavenging. All of these factors combine to corroborate the witness testimony of initial shallow burial, exposure, and reburial of some of the partially decomposing remains 7 to 10 days later. This was followed by agricultural disturbance and reburial of the (by then) skeletonized remains. Site III presented the highest number of long bones grouped in arbitrary assemblages, along with a total of 14 crania found concentrated in two areas. It is probable that the peasants used this site more often than the one in which they would rebury remains they found on the surface while tilling the soil. Another detail reported in a witness statement was the aftermath of torture in the town hall. Evidence of amputation of fingers was observed in skeletons CH-II-4 and CHII-9, including perimortem fractures of several metacarpals and absence of phalanges. In the latter skeleton, several cut marks were observed on the fourth right metacarpal (E.A.F.G., 1993). The taphonomic processes documented at Chichupac were essential in providing compelling circumstantial evidence to corroborate witness testimony. It also suggested that the farmer using the field did not attempt to erase the evidence, but made an effort to consolidate it.

Conclusions The objective of exhuming mass graves is to provide evidence of war crimes, crimes against humanity, and genocide. The intent to destroy a particular group has to be demonstrated in order to prosecute these cases. Forensic investigation focuses on collecting data to reconstruct events in question. The examples presented here show that archaeological techniques and taphonomic interpretation can provide evidence of such patterns. Witness testimony often provides critical information for grave location, identification of victims, and interpretation of perimortem trauma and postmortem sequences. Likewise, the forensic taphonomy analysis can corroborate witness reports. Data about time since death, scavenger modification of remains, disarticulation, and postmortem sequences can play a critical role in building a case. Forensic anthropology and taphonomy of mass graves in this context are more than technical and isolated approaches to evidence collection and remains recovery. Anthropology in all of its facets, including law, cultural patterns, biological diversity, and archaeological interpretation of cultural patterns can and should be brought to bear in the investigation of genocide, war crimes, crimes against humanity, and human rights violations. The combination of taphonomic and anthropological expertise in the recovery and examination of forensic evidence provides the most effective approach.

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References Andino, L. 1995 Encontraron la primera osamenta en El Maguelar, El Heraldo, Tegucigalpa, Honduras, October 24. Anonymous 1995 Los antropólogos iniciaron la busqueda de tres desaparecidos, El Heraldo, Tegucigalpa, Honduras, October 23. Equipo de Antropología Forense de Guatemala 1993 Informe de Investigaciones Antropológico Forenses. Aldea Chichupac, Rabinal, Baja Verapaz. E.A.F.G., Guatemala City. 1995a Informe de Investigaciones Antropológico Forenses. Aldea Plan de Sánchez, Rabinal, Baja Verapaz. E.A.F.G., Guatemala City. Equipo de Antropología Forense de Guatemala/Physicians for Human Rights 1995 Report to the Special Human Rights Prosecutor of Honduras on the Forensic Investigations Carried Out in October of 1995 at El Maguelar, Honduras. E.A.F.G., Guatemala City. Haglund, W.D. 1997 Report of the Exhumation and Examination of Remains from the Kibuye, Physicians for Human Rights, Boston. Killam, E.W. 1990 The Detection of Human Remains, Charles C Thomas, Springfield, IL. Mant, A.K. 1987 Knowledge acquired from post-war exhumations. In Death Decay and Reconstruction: Approaches to Archeology and Forensic Science, edited by A. Boddington, A.N. Garland, and R.C. Janaway, Manchester University Press, London. Middle East Watch and Physicians for Human Rights 1993 The Anfal Campaign in Iraqi Kurdistan: The Destruction of Koreme, Human Rights Watch, New York. Neier, A. 1998 War Crimes. Brutality, Genocide, Terror, and the Struggle for Justice, Random House, New York. Physicians for Human Rights 1994 Report of a Preliminary Medicolegal Investigation of a Series of Clandestine Graves near Pakracka Poljana, Former Yugoslavia, Physicians for Human Rights, Boston. Scott, D.D. and M. Connor 1997 The Koreme execution site: a modern crime scene investigation using archaeological techniques. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 34–38. CRC Press, Boca Raton, FL. Skinner, M. 1987 Planning the archeological recovery of evidence from recent mass graves, Forensic Sciences International 34:267–287. Stover, E. and G. Peress 1998 The Graves: Srebrenica and Vukovar, Scalo, New York.

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United Nations 1997 Manual on the Effective Prevention and Investigation of Extra-Legal, Arbitrary and Summary Executions, United Nations, New York. U.N.T.S. 1951 Convention on the Prevention and Punishment of the Crime of Genocide, Vol. 78, No. 1021, United Nations, New York.

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Postburial Disturbance of Graves in Bosnia-Herzegovina MARK F. SKINNER HEATHER P. YORK MELISSA A. CONNOR

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Contents Introduction Background Historical Propaganda and Mass Graves Varieties of Postburial Disturbance Body Trading during the War Mandated Exhumations with Reburial during the War Body Relocations Unmonitored Intra-Entity Exhumations Unmonitored Inter-Entity Exhumation Removal of Grave fill with Continued Interment in Same Grave Case Studies of Sites in Bosnia-Herzegovina Where Clandestine Removal of Bodies Is Inferred Tasovcici Observations at the Site Prior Site Disturbance at Tasovcici Vojno Prior Site Disturbance at Vojno Bijelo Polje Prior Site Disturbance at Bijelo Polje Zaklopaca Prior Site Disturbance at Zaklopaca Discussion Conclusion Acknowledgments References

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Introduction* Much forensic taphonomic analysis is undertaken to elucidate the decay of evidence. In the case of clandestine removal of bodies from mass graves** the taphonomic data are the evidence (cf. Holland et al., 1997). Recent investigations undertaken by Physicians for Human Rights (PHR)*** and International Criminal Tribunal for the Former Yugoslavia (ICTY) suggest strongly that in the aftermath of hostilities in the former Yugoslavia, several mass graves were emptied and the remains disposed elsewhere. For example, on November 4, 1996, Newsweek quoted Dr. R. Kirschner, Director, International Forensic Program, PHR, as observing about the Lazete Site: “We have several bags of extra limbs and other body parts [which] indicates there has been tampering” (Sullivan, 1996). Similarly, a UN team found only 146 bodies along with miscellaneous unmatched limbs and appendages at the site of Pilica where up to 1200 Muslims died on July 6, 1995, according to Drazen Erdemovic, a confessed Serb executioner testifying at the Hague. Significantly, satellite photographs taken 3 months after interment showed heavy equipment returned to the site (Stover and Peress 1998). By contrast there was no evidence of tampering at the site of Nova Kosaba which yielded only 33 bodies when more than 600 were expected (Sullivan, 1996). This report describes four additional sites in Bosnia-Herzegovina where tampering is suspected and compares them with other monitored sites in which prior, proper removal of bodies took place.

Background Christian unity was sundered in 1054 AD by a schism between Rome and Constantinople. Historical interactions between the Catholic West and Orthodox Christian East have centered on the Balkans. Turkish occupation commencing in the 14th century converted many of the area’s Slavic inhabitants to Islam. Three ethnicities based on religious differences coexisted more or less successfully as colonial subjects at the boundary between the Austro-Hungarian and Ottoman empires (Kaplan, 1996). Serbian nationalism emerged in the early part of the 20th century, contributing to the conflict that resulted in the First World War. Out of this conflict arose the nation of Yugoslavia (southern Slavs) dominated by Serbs. At the outbreak of hostilities in the Second World War, a Nazi-dominated faction of disaffected Catholic Croats called Ustashe participated in barbaric acts of genocide directed at Jews, Gypsies, and Partisan Serbs, termed Chetniks, who fought a long guerrilla war of resistance (Kinzer, 1996). Memories of this conflict, particularly the infamous mass grave * The views expressed here are those of the authors and should not be construed to reflect those of Physicians for Human Rights. ** This chapter is not concerned with the precise definition of a mass grave. Functionally, one may distinguish between single graves, group graves in which bodies are laid out in parallel, and mass graves in which bodies are disordered. All three site types were monitored in Bosnia-Herzegovina. *** Physicians for Human Rights (PHR) is an organization of health professionals, scientists, and concerned citizens that use the knowledge and skills of the medical and forensic sciences to investigate and prevent violations of international human rights and humanitarian law. One component of PHR Bosnia Projects is the Forensic Monitoring Project, which monitors the exhumation of human remains, dating from the 1992–1995 conflict in the former Yugoslavia, by members of the State Commissions within and between entities. PHR issues Findings Reports, which provide a neutral source of information about the contents of such graves and their manner of formation and exhumation.

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Figure 15.1 Map of Bosnia-Herzegovina within the boundaries of the former Yugoslavia showing location of four sites where clandestine removal of bodies is inferred.

of Serb dead at the Jasenovac death camp smoldered through the peaceful decades of communist rule under Tito and fueled the outbreak of ethnic violence in 1992. The main conflict in post-communist Yugoslavia developed between Serbians in the east led by Slobodan Milosevic and Croats in the west led by Franjo Tudjman (Cohen, 1993). Both areas contained significant enclaves of Orthodox, Catholic, and Islamic communities. According to the 1991 census, of some 4.35 million inhabitants from the BosniaHerzegovina area, 48.0% were Muslim, 33.6% Serb, and 12.7% Croat (Tokaca, 1996). The term Bosniak, meaning people from Bosnia, is increasingly accepted as an alternate for designating a Muslim from Bosnia. Bosniaks fared worst during the 1992–1995 war because they lacked large weaponry and geographical access to supportive European and Warsaw Pact nations (Dydynski, 1997). With the imposition of peace created by the Dayton Agreement in November 1995, there were approximately 16,806 missing Bosniak Muslims, 2503 missing Bosnian Serbs, and 704 missing Bosnian Croats registered with the International Committee for the Red Cross* (figures released January 9, 1998). Most of them are believed to be in mass graves scattered throughout Bosnia-Herzegovina. The war in Bosnia ended officially in December 1996 with the Dayton Accord in Paris. Bosnia-Herzegovina currently comprises the Serb Republic entity, covering 49% of the territory, and a more or less cooperating political body called the Croat-Bosniak Federation comprising 51% (Cohen, 1998) (Figure 15.1). Hence, there are two states (Federation and Republic) encompassing Bosnia-Herzegovina and three functional entities (Croat, Bosniak, Serb).** An ICTY team sponsored by Physicians for Human Rights exhumed the mass grave of Ovcara near the Croatian city of Vukovar in December, 1992, leading to the indictment of three members of the Yugoslav People’s Army in November of 1995. Commencing in * Government sources in Sarajevo put the number of missing persons at 25,000 (Tokaca, 1996). ** Inter-entity exhumations require monitoring while intra-entity exhumations do not.

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late 1996, Physicians for Human Rights, supported by the Office of the High Representative and the Stabilization Force organized by NATO to preserve the peace created by the Dayton Accord, have monitored the efforts of the local entities to locate and excavate many mass graves. Initially, efforts in 1997 were restricted primarily to intra-entity exhumations resulting in the monitored exhumations of approximately 99 bodies from 5 sites. In late 1997, PHR monitored inter-entity exhumations at 2 sites containing approximately 94 bodies. Commencing in 1998, inter-entity activities resulted in the exhumation of 1653 bodies from 374 sites (PHR, 1999), the majority of these being Bosniaks recovered from the Serb Republic.

Historical Propaganda and Mass Graves It is an extreme irony that political manipulation of the historical existence of mass graves results in another generation of such graves. Bax (1997) concludes from an investigation of memorials created in Bosnia-Herzegovina to commemorate mass graves from the Second World War that such memorials functioned ritually to preserve and engender animosity and thus help explain the local sources of renewed conflict. During the appalling Serb–Croat combat last year, it [Jasenovac Memorial] was occupied for a while by Croatian forces. They methodically trashed the museum and the exhibits, and left only the huge, ominous mounds that mark the mass graves. (Hitchens cited in Denich, 1994).

In a remarkably prescient article, conceived before the outbreak of hostilities in the former Yugoslavia, Denich (1991) reasons that rival exhumations of Second World War dead were publicized to advance extreme nationalist political agendas. In order to offset the victim status of Serbs created by Ustashe-led events at Jasenovac, Croats deliberately publicized the existence of mass executions perpetrated in the immediate aftermath of the Second World War by Communist-led Partisan troops. The publication of these revelations led to the discovery of actual burial sites. In June, 1990, word reached the Zagreb media of a cave called Jazovka. Like the pigeon-caves of massacred Serbs, its existence had been known to nearby villagers, who now revealed the secret. The media in Croatia published pictures of the 40-m-deep cavern, piled with killing field relics. A Croatian emigrant publication described the cave as “full of bones of innocent Croat postwar victims of Communist savagery” (Denich, 1994:378). The Serbian media in turn emphasized the repatriation of Serbian World War II genocide victims from Croatia and Bosnia-Herzegovina: the exhumation of their collective graves, recovery of bones, and reinterment in village cemeteries with Orthodox burial rites. Such ceremonies increased in scale. In 1991, caves in Bosnia-Herzegovina were exhumed, and mass public burials were shown over television throughout Serbia. At one of these ceremonies, Radio Belgrade described the line of coffins as extending for 1.5 km (Denich, 1994:382).

Political and ethnic conflicts persist in Bosnia-Herzegovina. Even within political entities, there is an essential tension between those who wish to forget the past and only look forward vs. those who seek to right historical wrongs through analysis of what happened.

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The internationally monitored exhumation of mass graves is potentially destabilizing. In the wake of national media reports of exhumations, there are frequent allegations of manipulated coverage ranging from misreporting of age and sex of victims to site names. Nevertheless, it is generally accepted by the local entities and the international community that documentation of mass graves and their contents is necessary for a lasting peace. Exhumations lend themselves to propaganda. Hence, the international forensic community has a significant responsibility to treat this problem as both a sociopolitical and forensic science issue with historical roots.

Varieties of Postburial Disturbance In addition to the obvious political use to which mass graves can be put, there are other less obvious ploys. For example, there is the oft-voiced suspicion expressed at monitored exhumations that the continued removal of bodies, single or massed, from known cemeteries is a form of ongoing ethnic cleansing. This act has been characterized as killing the dead — the ultimate form of ethnic cleansing (Bax, 1997). In the Bosnian countryside the deceased continue to be part of their kinship group. Via them, their progeny can lay claim to the use of land and water and to the produce of fruit and olive trees. It is not until all the traces of their lives have been wiped out that these claims cease to exist (Bax, 1997:17).

A war-time Muslim burial in an orchard near Carakovo-Zeger appeared, from grave architecture and the widow’s account, to have been a formally conducted affair; nevertheless, it contained the partial remains of a pig inserted under the traditional sloped wooden plank cover within the grave which serves to protect a body from the grave fill; these anomalous inclusions could be construed as having been added as a form of religious insult (field observation by MFS, 1998). According to a Serb forensic pathologist, rubbish had been heaped on a mass grave at Carevo Polje (nr. Jajce) (Savic, 1998). The rubbish consisted of small pile of dirt and bricks on a small area of the mass grave (field observation by MFS, 1998). Evidence is presented below to substantiate the conclusion that some gravesites in Bosnia-Herzegovina have experienced the clandestine removal of bodies prior to monitored exhumations. However, there are several other situations that include the prior removal of bodies; these have to be differentiated forensically from improper activities. Clearly, one defense to the charge of clandestine removal of bodies from a mass grave would be to allege prior undocumented exhumation, which would affect the evidentiary properties of forensic observations made at a mandated exhumation. Body Trading during the War This is commonly alleged in Bosnia-Herzegovina and is a familiar practice in war. The first 16 bodies recovered in 1998 at the Muslim graveyard site of Balinovac in West Mostar were each contained in two body bags, rather than one. These bodies are alleged by representatives of the State Commission to be exhumed Bosniaks, from an unnamed site, returned in 1993 by Serbs to the Croat entity, in an apparent three-way trade (Skinner, 1999).

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Similarly, 70 bodies from undesignated sites in the Mostar area were handed over by the Croatian Council for Defense (HVO) to the Bosniaks on March 29, 1994 after the local cessation of hostilities (pers. comm. April 9, 1998, President, State Commission on Missing Persons). One of these bodies was buried at Sarica Podharem designated as NN61; at autopsy an accompanying note sealed in plastic attested to the date the body trade occurred (Skinner, 1999). Also, unmonitored body trading took place in the immediate aftermath of cessation of hostilities in November 1995 (Silber, 1996). Mandated Exhumations with Reburial during the War Nine small graves in the vicinity of the execution site of Pakracka Poljana, Croatia suspected to contain Serb bodies were excavated in November, 1993 by personnel from Physicians for Human Rights. The remains of 19 exhumed individuals were re-interred in body bags with formaldehyde preservative at an UNPROFOR observation post (Physicians for Human Rights, 1996) pending full forensic examination which took place in late 1995; the bodies were re-buried as originally (Haglund, pers. comm. April 28, 1999). Body Relocations On the north side of the formal cemetery site of Medine, near Mostar, were some 20 or so numbered wooden T-shaped grave tablets plus 12 or so tablets strewn about dating primarily from 1993 which are alleged to mark remains of Bosnian Croat individuals who were previously autopsied at the Clinical Hospital in Split, Croatia (Skinner, 1999). Where they were previously interred/stored and why they were transferred to Medine is not known. Similarly, it is alleged by the President of the State Commission on Missing Persons that Bosniak civilians were used by HVO forces as a human shield to protect defense lines in battles over Makljen and Crni Vrh on July 31, 1993 (Tokaca, 1996). Those who died were buried, but disinterred later, possibly in 1995, and jointly reinterred at Lapsunj Village after the signing of the Dayton Agreement (ONASA, September 25, 1998). Twenty-one bodies were removed in a monitored exhumation of this site September 23–24, 1998 (Connor, 1998c). Members of a Serbian family abandoning Sarajevo at the end of hostilities privately removed the body of a family member who died during the war (New York Times, February 16, 1996). This scene was probably repeated many times over throughout Bosnia-Herzegovina as families permanently relocated. Unmonitored Intra-Entity Exhumations The site of Miljkovici, south of Mostar, was alleged to have been excavated by unspecified persons 7 to 8 months prior to a monitored exhumation by the State Commission (Bosniak side) in April 1998 (pers. comm. to MFS, August 4, 1998, Police Representative, Federal Commission on Missing Persons). This site is mentioned as the burial place of individuals from the Heliodrome Concentration Camp (run by the HVO) who were allegedly taken out for forced labor and to act as human shields (Tokaca, 1996). The monitored exhumation yielded partial remains of two individuals plus four identity cards (Skinner, 1999).

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Unmonitored Inter-Entity Exhumation Allegedly, on August 4, 1997, 16 Serb bodies (civilians and soldiers) were exhumed at the cemetery site of Caprazlije by Bosnian Croat diggers in the presence of a Serb Republic crime technician; monitored exhumations of 36 remaining bodies occurred at this site in 1998 (Connor et al., 1998). Similarly, at the nearby site of Donja Rujani beside an Orthodox church, 82 bodies of soldiers were allegedly removed prior to monitored exhumations of the same ground in 1998 that yielded only fragments of clothing (Connor and York, 1998). Removal of Grave fill with Continued Interment in Same Grave This unusual situation observed in a Croatian cemetery developed during the war on the west side of a Catholic Seminary at Humac near Prozor. There are several east–west oriented rows of single, marked graves arrayed among a plum tree orchard. These bodies were buried in 1993 by the Army without family members present and without formal rites. The Humac priest stated that there had been a problem with vandalism of temporary grave markers in 1993, 1994, and 1997. There were numerous family members present at the exhumation on August 4, 1998. Some of them volunteered the information that they had previously opened particular graves to view the remains and confirm identification to their satisfaction. Several stated that they had placed objects in the graves to ensure proper identification in the future. Excavation revealed that Grave 5 contained a shallowly buried metal washbasin that an attending family member stated she had placed in the grave to mark it with certainty. Similarly, jars and plastic bags containing names written on pieces of paper were discovered at shallow depths in Graves 14, 18, and 19. Surgical gloves were observed in the grave fill from Graves 11, 12, 13, 14, 17, and 18. These observations are consistent with claims that these graves had been previously opened for examination of the remains (Skinner, 1998a).

Case Studies of Sites in Bosnia-Herzegovina Where Clandestine Removal of Bodies Is Inferred Tasovcici Tasovcici is located 2 km east of Capljina, Bosnia-Herzegovina. The site is on a hill called Modric, the location of a damaged memorial cemetery for Second World War Partisan soldiers (Figure 15.2). The State Commission on Missing Persons (Bosniak) investigated the site from April 24–27, 1998. Exhumations were monitored by Physicians for Human Rights. Exposure of the bodies was accomplished by backhoe supplemented by shovels. Trowel work was undertaken by autopsy assistants supported by the pathologists and various members of the State Commission. Excavation revealed an unmarked, mass grave of 30 bodies arranged in 2 discontinuous east–west rows (Figure 15.3); bones on the surface represented 2 individuals (Skinner, 1998b). About 75% of the bodies were in body bags; the remainder were lying on remnants of canvas sheets. Of the entire series, most were clothed and, judging from the clothing, civilian. There were 12 males and 11 females, the remainder indeterminate. Virtually all individuals were skeletonized. Skeletally and dentally, the adults were relatively elderly with an average age of 66 years. Two of the Tasovcici

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Figure 15.2 Sketch map of Tasovcici site.

remains were children who came from a cluster burial of several related women and children. The forensic pathologists determined that 20 of 22 sets of fairly complete remains showed hard tissue trauma. Nine individuals had experienced two or more wounding events. Most traumata were confined to the head and trunk; arms and legs were little affected. In nine instances, there was unequivocal evidence of gunshot wounds in the form of bullet holes or actual bullets. Deaths are said to have occurred in 1993. The total number of identifications obtained at Tasovcici was not stated. Observations at the Site Although, 30 bodies were exhumed, 9 were incomplete (TAS 6, 7, 8, 9, 12, 17, 19, 20, 30); also, there were obvious gaps in the rows of bodies. This is shown in Figure 15.3. There is a clear pattern in which bodies adjacent to gaps in the body row were damaged and incomplete. Five incomplete bodies bordered on four gaps in the southerly row of bodies. Also, at the west end of the southerly row and the east end of the northerly row, the bodies were incomplete suggesting prior removal of bodies in these areas, both of which were excavated in their entirety by the team. The average distance between adjacent bodies was 0.75 m; thus the estimated number of missing bodies in the measured gaps is as follows: between TAS 5 and 6 — 1; between TAS 8 and 9 — 5; between TAS 11 and 12 — 4; between TAS 17 and 18 — 2; to east of TAS 30 at end of row — minimum of 1. In total, a minimum of 13 bodies may have been previously removed from this site. In other words, there is evidence of at least 43 bodies having been present at the Tasovcici site, which is still considerably less than the figure of 80 bodies alleged by the State Commission’s investigators to have existed. There is other evidence consistent with the allegation that prior removal of bodies has occurred at this site:

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Figure 15.3 Distribution of bodies from Tasovcici site.

• During the grass removal, a number of pieces of clothing were encountered including a pair of running shoes, one of which had foot bones in it. These items were not found associated with other remains. • Two fused neck vertebrae were found on the surface. • Several rubber gloves were found on or close to the surface. • A military document bearing an individual’s name was found in the grave fill. It is not known whether this came from one of the identified individuals. • In the gap between bodies 5 and 6 there were remnants of another body bag. • At the west side of body 21, there was a shallowly buried blanket like those found wrapped around bodies at many other sites. • In the dirt above bodies 21 and 22 (that is, at the west end of the row), two pieces of crumpled sheet metal from a coffin were encountered by the backhoe. One of the sheet metal pieces had remnants of a glass viewing window. These metal sheets can be accounted for in two ways: either they were used separately to carry bodies or they represent the remnants of a coffin from a disinterred body to the west of 21.

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• Fragments of coffin wood with impressed design, unassociated with any observed body, were found in the excavated earth immediately west of the northerly row of bodies. The observations summarized above are strong evidence that a prior exhumation occurred at this site. However, body parts can be scattered at the time of burial if the bodies are badly decomposing. Similarly, secondary burial may leave clothing and body parts on the surface. Also, it could be argued that evidence on or close to the surface (foot and neck bones, rubber gloves) could simply have been surface remains. However, it was possible to show at autopsy that the buried shoe from TAS 26 matched a shoe found on the surface (Skinner, 1999). Prior Site Disturbance at Tasovcici Before the start of exhumation, the President of the State Commission stated that 80 bodies were to be expected. This is consistent with the description of this site provided by Tokaca (1996:153): Already in June 1993, information on the existence of mass grave on the Modric hill near Tasovcici was known. That was the place of the Partisan Cemetery where from July 15, 1993, in evening hours, the bodies of killed persons were taken to the place in trucks (this is according to the witness statements). As the action of ethnic cleansing was in process in the region of this municipality between July 13/14 and 15, 1993, and the torture against population of the village in Dubrave and Stolac also was performed, and having in mind many cases of murders and taking of persons from Capljina concentration camps in unknown directions, the conclusion could be made that many persons from the area finished in that mass grave. Namely, eyewitnesses state that 60 corpses were driven on trucks on July 15, 1993 and that two days after that, on July 17 and 18, 1993, the mass grave was excavated with a dredging machine and the corpses were thrown in. The mass grave was not covered and that meant new corpses would be taken in. That was true and it lasted for another 20 days.

However, one wonders whether the full complement of 80 bodies was truly to be expected since a newspaper account dated March 28, 1996 claimed prior removal of 26 bodies: Disputed delivery of victim’s bodies from Modric Pit. IFOR blocks death site After the recent delivery of 26 disputed bodies of Bosniaks from the Capljina and Stolac area removed from the Modric pit by the HVO entity, of which 15 are already identified and re-buried, it seems that disentanglement of this tragic story is in sight. Namely, after simultaneous public condemnation by several specific institutions of the delivery of these bodies without proper legal representatives plus information supplied by forensic pathology experts that remnant soil from four different, successive burial sites was found on the bodies, there is an unconfirmed report that IFOR used its strong influence to close the Modric burial pit for Bosniaks, located near Capljina beside the coast road to Stolac. After this demonstration of power by IFOR, chances are increased that international and legal institutions of Bosnia-Herzegovina will go to the site. With reference to the unidentified bodies from the above-mentioned delivery, these will be buried as NN assuming the approval of representatives of the State Commission

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for Missing and Tracing Persons including the involvement of Mr. Amor Masovic. We should remember that there are 44 reported missing persons from the Capljina commune and 32 from Stolac. (G. Smajic, 1996)

In addition, part way through the monitored exhumation commencing on April 24, 1998 the Forensic Monitor was shown a video by the President of the State Commission alleged to have been taken in April 1997 at the Tasovcici site showing it recently dug over with bare earth, rocks and surgical gloves on the earth. He alleged that 26 bodies had already been removed from this site, taken to the Mostar Bridge in November 1996 and given without explanation to the Bosniaks. He insisted that there were still some 24 bodies missing and that these were improperly removed either prior to November 1996 or later in April 1997 as attested by the alleged date of the video. Clearly, these are complex matters.* Nevertheless, it can be concluded that there is obvious postburial disturbance at this site. Vojno This area included a prison organized by HVO members at which numerous deaths are alleged to have occurred in the fall of 1993 with the victims being buried in nearby fields (Tokaca, 1996). A witness led the President of the State Commission to this site, claiming that several Bosniaks had been buried there and that at least some of the bodies had been subsequently removed (York, 1998). The site is on a raised plateau, northwest of the highway that parallels the Neretva River. The exhumation team processed this site on May 21, 1998. After the laborers cleared thick, uniform vegetation from an area of approximately 25 ¥ 8 m, 8 depressions of about 60 cm in depth became evident (Figure 15.4). There were approximately 40 cm between adjacent depressions. No surface remains were visible. A backhoe was brought in to determine whether there were any graves outside of the area of the visible depressions. Finding nothing, the decision was made to use the backhoe to break up the soil in each of the depressions to search for remains. Prior Site Disturbance at Vojno The first depression (Figure 15.4A) yielded a large piece of blanket with a sheet of plastic beneath it. Some pieces of soft tissue were stuck to one side of the plastic. One laborer shoveled into the bottom of the depression while others sifted through the backdirt by * Conceivably, these 26 bodies, given to the Bosniaks, were re-interred at Miljkovici, since, as noted, at the latter site there were 26 discarded blank T-shaped markers. It is known that at the Miljkovici Site, which yielded no intact bodies, a Red Cross document was exhumed in 1998 bearing the name of an individual (A…C…) registered on March 18, 1993 (Skinner, 1999). Interestingly, an individual, with the same surname (C…) and purportedly part of a body exchange, was disinterred from Sarica Podharem (NN96) on May 6 or 7, 1998 in an unmonitored exhumation and autopsied that same day; significantly perhaps, as part of the Tasovcici series (field observation by MFS, 1998). He had some broken bones. Furthermore, a body known as Balinovac 104 exhumed on May 5, 1998 had the same surname but different first name (D...C…). At autopsy the next day it was determined that he had been shot in the head. Two individuals (brothers) with the same names as noted above (A…C… and D…C…) were allegedly taken from the town of Capljina in early July 1993 to Rastanje Hill, used as a human shield and killed and buried in an unspecified mass grave, possibly the Tasovcici site (Tokaca, 1996). Thus, there may be a link between the missing bodies at Tasovcici and those removed from Miljkovici.

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Figure 15.4 Distribution of pit features at Vojno.

hand and trowel, but no other remains were found. Shoveling in the depression to the west (Figure 15.4D) revealed a right mandibular ramus and an open and empty silvercolored body bag. A backhoe trench through the northeasternmost depression (Figure 15.4E) yielded a piece of clear plastic and an orange and white print blanket. A backhoe trench through a depression in the northwest corner of the site (Figure 15.4G) revealed a silver body bag but no human remains. Another trench through the adjacent depression at the northwestern limit of the plateau (Figure 15.4H) exposed another torn piece of a body bag. A small trench dug between these two depressions yielded one torn, short white sock. Other backhoe trenches approximately 50 cm wide and 60 cm deep were dug around the perimeter and between some of the adjacent depressions (Figure 15.4, shaded areas), but no further remains or body bags were found. Behind a rock approximately 15 m to the west northwest and upslope of the depressions, crime technicians found a pair of military pants with cigarettes in the pocket, and a camouflage vest with a knife sheath and holster in another pocket. Bijelo Polje This site is located a few kilometers north of Mostar between the Neretva River and the highway to Sarajevo. The area to the north had been mined and unexploded ordinance was found throughout the site area (Connor, 1998b). The State Commission conducted monitored exhumations at this site on June 15, 1998. The site is in the vineyard and orchard of a destroyed house. Large areas of the site were trenched; however, evidence was recovered only from an obvious pit feature in the de-mined path. Prior Site Disturbance at Bijelo Polje The laborers found two hand bones and a bullet. A blanket was present at the bottom of the depression. The laborers unfolded the blanket and found two buttons stuck to the

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inside. One was a four-hole shirt button and the second a loop-back jacket button. The remains and evidence found were consistent with one set of remains previously removed from this location (Connor, 1998a). Zaklopaca The State Commission on Missing Persons conducted exhumations on June 22–24, 1998 at Zaklopaca, east of Vlasenica in the Srebrenica region. The grave was said to be that of the Bosniak residents of the village killed in their homes in 1992 and brought to the grave area on tractors. A witness said the grave was dug with a mechanical excavator and was so deep that only the scoop of the backhoe, rising out of the ground, could be seen from the informant’s vantage point. The witness said the bodies of children were placed in the grave first, those of women and young boys next, and the adult males last. There were said to be 58 people of known identity in the grave. Attempts to locate the grave began around a pile of earth about 50 m long, 2 m wide, and less than 1 m high. The exhumations continued for 3 days with a small, and then much larger, backhoe (Connor, 1998a). Prior Site Disturbance at Zaklopaca Near the initial trench, a sock containing foot bones, ankle bones, and some cloth were found. The digging unearthed a tire rim; a portion of a child’s cranium was found in the rim. Hair and clothing were also collected from the backdirt. Digging with the backhoe was stopped when a shoe, an adult cranial fragment, and several hand bones were seen in the profile of the trench. The deepest human material was about 2 m below the original ground surface. The shoe was bent back on itself. The partial remains found were isolated and no additional materials were found adjacent to them. The Forensic Monitor calculated that the area of disturbed soil was roughly 20 m in diameter. It was concluded that there had been two episodes of soil disturbance; first, the actual digging of the grave, and second, the soil disturbance reflecting the digging to remove the bodies that resulted in the partial remains scattered in the disturbed soil.

Discussion At two sites (Tasovcici and Vojno) informants stated that bodies had been taken away. Monitored exhumations suggest that a minimum of 13 individuals had been removed from Tasovcici and 8 from Vojno. It is not clear how many had been removed from the other two sites. There is a variety of surface, grave fill, and buried evidence indicative, in these instances, of site disturbance. At all four sites incomplete remains represented by flesh and/or bone remnants were observed. Clothing fragments were observed at all four sites. Empty body containers, in the form of blankets, plastic, wood, and body bag fragments were observed at three sites (excluding Zaklopaca). Various artifacts supported the prior presence of human remains (bullet, plastic gloves, military document in grave fill). In one instance (Tasovcici) an association between surface and buried evidence could be shown. At two sites (Tasovcici and Vojno) military clothing was observed to one side of the site. At two of the sites (Vojno and Bijelo Polje) surface depressions containing partial human remains were observed. At one site (Tasovcici) spatial anomalies in the form of gaps in the row of bodies were observed. Also, at this site there was a clear association between gaps and

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damage to bodies on either side of the gap suggestive of crude body removal techniques. At Vojno, the digging appeared to have been selective and circumscribed; that is, there were no random trenches or holes and all holes were grave sized and no larger.

Conclusion The women of Srebrenica seek to understand the whereabouts of their husbands and sons who disappeared in 1995; thousands disappeared — they ask, “Where are their graves?” (Stover and Peress, 1998). As we have seen, there are many reasons why bodies are removed from mass graves prior to monitored exhumations. Only one of these may be clandestine. The others include body trading, mandated wartime exhumations, post-war body removals and transport, and unmonitored post-war exhumations within and between geopolitical entities. Distinguishing among these will be difficult unless steps are taken to obtain the following: • • • • •

Informant accounts (full disclosure by various state commissions) Site topography, including artifact distribution, prior to excavation Mapping of all features Careful attention to stratigraphy especially grave cuts Screening or at least examination of grave fill

In order to remove bodies from a grave a hole has to be dug, usually with a backhoe. Consequently, it may be that apart from informants’ accounts, the only way to differentiate between secret and public exhumation is the relative care given the exhumation. It is the careful integration of statements from local eyewitnesses and taphonomic experts which provides sufficient evidence to determine that a clandestine exhumation has occurred. In our opinion, it is essential that potentially disturbed site topography be recorded by neutral personnel with expertise in the processes of site formation. While it is important to substantiate clandestine exhumations intended to hide evidence of war crimes, it is equally essential to keep in mind that mass graves can be used for a variety of political ends by competing entities. Both parties have vested interests, depending on site history, in the accurate determination of why bodies have been previously removed from a site. Most important for international organizations involved in the monitoring of exhumations is a means of keeping track of sites exhumed in the past including unmonitored, monitored, and what are ultimately determined to have been clandestine exhumations. Where clandestine removal of bodies and other evidence from mass graves is substantiated, it should be viewed as a serious breach of international humanitarian law as is inhuman treatment of protected persons (Physicians for Human Rights, 1996). Mass graves are more than repositories of the dead. Unexcavated, they can function as political tools to intimidate survivors; scientifically excavated they are threats to the perpetrators. Clandestine efforts to remove the bodies inevitably leave taphonomic clues behind for forensic archaeologists and anthropologists to discover and interpret.

Acknowledgments We thank the following organizations and key personnel for their support: PHR Boston (Len Rubenstein); PHR Bosnia Projects (Laurie Vollen, Brenda Kennedy); Office of the

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High Representative (Agneta Johansson); International Commission on Missing Persons (Laura Bowman); State Commission on Missing Persons Bosniak Side (Amor Masovic); Federal Commission on Missing Persons Croat Side (Jerko Radic); and Republika Srpska State Commission on Missing Persons (Berislav Pusic and Jovo Rosic). The authors also wish to thank particular individuals for their professional and personal kindnesses during our work in Bosnia-Herzegovina: Sime Andelinovic, Mujo Azic, Berislav Cvitanovic, Marija Definis-Gojanovic, Ilias Dobraca, Kemal Dragonovic, Doug Ford, Saudin Hrnjic, Page Hudson, Zeljko Karon, Roy Lausecker, Halil Maksumic, Huso Mehrimic, Muhamed Mujkic, Adnan Music, Jerko Radic, Adnan Rizvic, Elvira Tarhovic, Miroslav Tomic, Ismet Trebinjac, Werner Zofal, Gordana Zovko, and Hamza Zujo.

References Bax, M. 1997 Mass graves, stagnating identification, and violence: a case study in the local sources of “The War” in Bosnia Herzegovina. Anthropological Quarterly 70(1):11–19. Cohen, L.J. 1993. Broken Bonds. The Disintegration of Yugoslavia, Westview Press, Boulder, CO. 1998 Whose Bosnia? The politics of nation building, Current History 97(617):103–112. Connor, M.A. 1998a Forensic Monitoring Project Findings Report, Physicians for Human Rights, Exhumation Conducted by State Commission on Missing Persons at Zaklopaca, Bosnia I Herzegovina, June 22–24, 1998, Report Date: July, 1998. 1998b Forensic Monitoring Project Findings Report, Physicians for Human Rights, Exhumation Conducted by State Commission on Missing Persons at Bijelo Polje, Bosnia I Herzegovina, June 15, 1998, Report Date: August, 1998. 1998c Forensic Monitoring Project Findings Report, Physicians for Human Rights, Exhumation Conducted by State Commission on Missing Persons at Lapsunj, Bosnia I Herzegovina, September 23–24, 1998, Report Date: November, 1998. Connor, M.A. and H.P. York 1998 Forensic Monitoring Project Findings Report, Physicians for Human Rights, Exhumation Conducted by Republika Srpska State Commission on Missing Persons at Donja Rujani, Bosnia I Herzegovina, June 11, 1998, Report Date: November, 1998. Connor, M.A., H.P. York, and M. Skinner 1998 Forensic Monitoring Project Findings Report, Physicians for Human Rights, Exhumation Conducted by Republika Srpska State Commission on Missing Persons at Caprazlije Cemetery and Provo Surface Collection, Bosnia I Herzegovina, June 11, 1998, Report Date: November, 1998. Denich, B. 1991 Unbury the victims: rival exhumations and nationalist revivals in Yugoslavia. Paper for the American Anthropological Association Annual Meeting, Chicago. 1994 Dismembering Yugoslavia: nationalist ideologies and the symbolic revival of genocide, American Ethnologist 21:367–390. Dydynski, K. 1997 Eastern Europe, 4th ed., Lonely Planet Publications, Oakland, CA.

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Holland, T.D., B.E. Anderson, and R.W. Mann 1997 Human variables in the postmortem alteration of human bone: examples from U.S. war casualties. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 263–274. CRC Press, Boca Raton, FL. Kaplan, R.D. 1996 Balkan Ghosts, Random House, New York. Kinzer, S. 1996 When did the war begin? Atlas of War and Peace, Macmillan, New York. New York Times 1996 Photo Agence France Presse, February 16, 1996. Physicians for Human Rights 1996 War Crimes in the Balkans. Medicine under Siege in the Former Yugoslavia 1991–1995. Boston. 1999 Forensic Monitoring Project 1998 Joint Exhumation Process. Summary, March 23, 1999, PHR Bosnia Projects, Tuzla, Bosnia-Herzegovina. Savic, V. 1998 Their crosses were touching, Reporter May 21, 1998. Silber, L. 1996 Reconciliation means finding where the bodies lie, The Financial Times, October 14. Skinner, M.F. 1998a Forensic Monitoring Project Findings Report, Physicians for Human Rights, Bugojno Area Exhumations (Vucipolje, Rosulje, Causlije, Sultanovici, Humac), of Federal Commission on Missing Persons Croat Side, August 3–4, 1998, Report Date: November, 1998. 1998b Forensic Monitoring Project Findings Report, Physicians for Human Rights, Capljina Area Exhumations (Tasovcici and Kapica) of State Commission on Missing Persons Bosniak Side, April 24–27, 1998, Report Date: November, 1998. 1999 Forensic Monitoring Project Findings Report, Physicians for Human Rights, Mostar Area Exhumations (Balinovac, Bijeli Brijeg, Bijelo Polje, Blagajtusa, Donja Jasenica, Liska Park, Medine, Miljkovici, Podhum Mosque, Sarica Harem, Sipad, Soinovac, Zahum-Pijesak) of State Commission on Missing Persons, Bosniak Side, March 16–May 18, 1998, Draft Report Date: February 1999. Smajic, G 1996 IFOR blokirao stratiste. Newspaper report March 28, 1996. Stover, E. and G. Peress 1998 The Graves. Srebrenica and Vukovar, Scalo, Zurich. Sullivan, S. 1996 Genocide without corpses, Newsweek Nov. 4, p. 37. Tokaca, M. 1996 Missing Persons — Analysis of Causes and Circumstances in Territory of Bosnia and Herzegovina April 1992–December 1995, State Commission for Gathering Facts on War Crimes, Presidency Bosnia and Herzegovina, Sarajevo. York, H.P. 1998 Forensic Monitoring Project Findings Report, Physicians for Human Rights, Capljina Area Exhumations (Rastani and Vojno) of State Commission on Missing Persons, Bosniak Side, May 21–22, 1998, Report date: September, 1999.

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Cannibalism or Violent Death Alone? Human Remains at a Small Anasazi Site SALLY GRAVER KRISTIN D. SOBOLIK JOHN WHITTAKER Contents Introduction The Grinnell Site Methods Results and Discussion Depositional Pattern Breakage Pattern Burning Cut Marks Pot Polish Conclusions Acknowledgment References

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16

Introduction It has been proposed that cannibalism was practiced by prehistoric populations in the southwestern United States for about 4 centuries, beginning around AD 900 (Turner and Turner, 1999). Evidence for cannibalism has centered along the Little Colorado River and in the Four Corners region at the Anasazi sites during the Pueblo III phase, approximately AD 1075 to 1300, although evidence for cannibalism is also claimed at a small number of sites dated earlier in time and located outside this region (Billman et al., 2000; Fagan, 1995; Turner and Turner, 1999; White, 1992). Although the existence of Anasazi cannibalism in the Southwest is widely accepted by many archaeologists (Billman et al., 2000; Preston, 1998; White, 1992), the issue is still highly controversial (Arens, 1979; Darling, 1999; Dongoske et al., 2000). The human assemblage at the Grinnell Site, a small Anasazi ceremonial center dated to the late Pueblo II and early Pueblo III time periods (Luebben, 1983), has been considered by other researchers as evidence of cannibalized remains (Billman et al., 2000; LeBlanc, 2000; Turner and Turner, 1999; White, 1992). Although the human remains have been described previously (Luebben and Nickens, 1982), they have not been analyzed for many of the traits currently used to characterize cannibalized assemblages. This chapter reports results of a comprehensive reanalysis of the Grinnell Site human remains to assess the validity of claims made about the evidence of prehistoric cannibalism at the site, using criteria for recognizing cannibalism developed by Turner (1983) and Turner and Turner (1999).

The Grinnell Site The Grinnell Site is situated 1.66 km southwest of Yucca House National Monument in southwestern Colorado (Figure 16.1). Structures there included a low ceremonial mound with steps and a ramp that overlays a small trapezoidal structure, a Mesa Verde type kiva (Kiva 1), an elaborate tunnel complex which linked Kiva 1 to a completely subterranean room and a circular tower, and a larger and older Mancos type kiva (Kiva 2) that underlay the eastern end of the passages and part of the tower (Figure 16.2). The mound was flanked along its north side by a masonry retaining wall that held back alluvium. Kiva 1 had burned completely and contained a large number of artifacts indicating habitation use of the kiva. Tree-ring dates obtained from Kiva 1 indicated that the timber was cut in 1244 A.D. No other living accommodation existed at the site. In contrast, Kiva 2 contained few artifacts but yielded a mass burial. Bones of eight individuals were deposited in Cist 2, situated on the southern recess of Kiva 2. Some bones were in a corrugated pot that sat on top of and was surrounded by other bones. Outside the cist, additional bones were found on the recess surface adjacent to the cist and on the kiva floor between the kiva wall and deflector (Figure 16.2). The latter may have been dropped accidentally when bones were brought into the kiva and deposited in the cist. The human remains pre-date 1244 A.D., the date of an overlying Kiva 1 timber. While the report by Luebben and Nickens (1982) claimed the mass burial provided evidence of brutality, it stopped short of suggesting cannibalism. In an earlier unpublished paper, however, Nickens (1979) concluded that the data indicated cannibalism. For the current authors, the nagging question persists. Had the individuals whose remains were found in the mass burial been both traumatized and cannibalized? To find a more definitive answer, the osteological assemblage from Kiva 2 was reexamined.

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Figure 16.1 Location of the Grinnell Site (13) and other southwestern sites considered to

provide evidence of cannibalism. 1 = Canyon Butte Ruin 3; 2 = La Plata 23; 3 = La Plata 41; 4 = Big Hawk Valley NA-682; 5 = Yellow Jacket Porter Pueblo 5MT-1; 6 = Sambrito Village LA4195; 7 = Bluff; 8 = Polacca Wash NA-8502; 9 = Burnt Mesa LA-4528; 10 = Monument Valley; 11 = Mancos 5MTUMR-2346; 12 = Leroux Wash NA-12854; 13 = The Grinnell Site; 14 = Marshview Hamlet 5MT-2235; 15 = Ash Creek AZ:U:3:49; 16 = Yellow Jacket 5MT-3; 17 = Cottonwood Canyon; 18 = Fence Lake Area; and 19 = Verdure Canyon. (Modified from White, T.D., Prehistoric Cannibalism at Mancos 5MTUMR-2346, Princeton University Press, Princeton, 1992, p. 37. With permission.)

Methods The criteria for cannibalism developed by Turner and Turner (1999) were applied to our data (Table 16.1). The first step of the reanalysis was to prepare an inventory to compare with that of Luebben and Nickens (1982) (Table 16.2). Initially, the bones were counted and recorded by element to determine a minimum number of individuals (MNI), and age and sex were evaluated where possible from skull, teeth, innominates, bone size, and epiphyseal fusion (Bass, 1987; Buikstra and Ubelaker, 1994).

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Figure 16.2 Site plan of the Grinnell Site, illustrating location of human bone deposition. Table 16.1

Taphonomic Signature of Cannibalism

1. Single, short-term depositional episode (discerned from stratigraphy and bone quality), preventing bone weathering and animal scavenging. 2. Bone preservation good to excellent. 3. Animal gnawing occurs on fewer than 5% of all elements. 4. Vertebrae are usually missing.a 5. Most body parts are “disarticulated.”b 6. Perimortem breakage occurs in 40 to 100% of skeletal elements. 7. Head, face, and long bone breakage is universal.a 8. Total bone fragment counts range between 400 and 3500 elements in a given episode. Body reconstruction is difficult due to a high rate of unaccounted for bone loss. 9. Breakage is by percussion hammering against some form of anvil, with spiral and compression fracturing very common.a 10. Burning after butchering and breaking is present in 2 to 35% of all elements.a 11. Butchering and skinning cut marks occur on 1 to 5% of bone elements, usually in appropriate locations for muscle tissue or scalp removal.a 12. Taphonomic sequence includes: (a) cutting; (b) breaking, and (c) burning (or, if evident, gnawing). 13. Pseudo-tools or accidentals made of human bone may occur in the frequency range of 1 per 10,000+ pieces. 14. The frequency of alteration in cannibalized bone lots is 95% for perimortem breakage, 20% for burning, 3% for cut marks, and 2% for possible gnawing or chewing. 15. Evidence of pot polish — the smooth polish that appears on the ends of bone that were cooked in prehistoric vessels — should be present.a a b

Denotes Turner’s six key, minimal taphonomic features of cannibalism. Term used by Turner to refer to bones out of anatomical order.

Source: Modified from Turner, C.G., II, in Carnivores, Human Scavengers, and Human Predators: A Question of Bone Technology, edited by G.M. LeMoine and A.S. MacEachern, 1983, pp. 233–244. With permission.

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Table 16.2 Human Skeletal Fragmentation at the Grinnell Site Element Frontal Temporal Parietal Occipital Maxilla Zygoma Mandible Tooth Unclassified vault fragment Unclassified facial fragment Vertebra Clavicle Scapula Humerus Radius Ulna Rib Pelvis Femur Tibia Fibula Metacarpal Phalange Navicular Unclassified long bone fragment Unknown Total

Whole

Fragments 8 8 3 3 10 6

1 2 4 29

136 34 9

4 1

2 4 4 2 1 7 4 2 11 1 68 10 374

Next, each bone was thoroughly examined with a 10-power hand lens for human or animal modification and for antemortem, perimortem, and postmortem alteration using the taphonomic criteria listed in Table 16.1.

Results and Discussion Most evidence for Anasazi cannibalism correlates with periods of environmental stress, the result of a severe drought that started in the area at about AD 1145 and continued to the end of the 12th century. During the Pueblo III phase, these environmental problems may have led to widespread agricultural failure and famine. Tree-ring records show severe drought co-occurring with depopulation of Chaco Canyon from AD 1145 to 1193 (Billman et al., 2000). A number of Anasazi sites, including Chaco Canyon and the Cowboy Wash areas, were abandoned. Some archaeologists propose that the resulting competition for resources may have triggered violence and cannibalism among the Anasazi (Billman et al., 2000; White, 1992). The existence of cannibalism in the Southwest has been argued by a number of scholars for decades. The earliest published claim for cannibalism was made in 1902 by Hough, an anthropologist from the Smithsonian Institution. Hough based his conclusion on an

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assemblage of burnt and broken human bones that were uncovered at a small pueblo in northeastern Arizona, Canyon Butte 3 (Turner and Turner, 1999). However, when Morris first presented her hypothesized findings of cannibalized remains at Polacca Wash at the 1969 meeting of the Society for American Archaeology in Santa Fe, her views were not accepted by many participants (Turner and Turner, 1999). Opposition to Anasazi violence and cannibalism in the Southwest was strong due to popularly held conceptions of peaceful puebloan Native Americans. The controversy surrounding cannibalism still exists today (Dongoske et al., 2000). While we believe that White and the Turners have made a convincing argument for the presence of cannibalism in the Southwest, the evidence is not equally good in all of the instances proposed. In his report on prehistoric cannibalism at Mancos 5MTUMR2346, White (1992:37) cited 19 other sites where cannibalism occurred in the Southwest (Figure 16.1). In a more recent publication (Turner and Turner, 1999:55), they identify evidence of cannibalism based on the remains of 286 individuals in 38 sites. However, Billman et al. (2000:169) propose that there are only 18 well-documented and dated sites that exhibit cannibalism. The strength of these claims of cannibalism in the Southwest rely on their shared taphonomic and osteological features, including abundant evidence that these human remains were processed like game animals prepared for consumption. Cannibalized human remains show a number of defining characteristics. Turner (1983) published a list of 15 taphonomic traits that he believed typified cannibalism in southwestern sites (Table 16.1). More recently, Turner and Turner (1999) have proposed that a minimum of six critical perimortem effects must be present. These taphonomic signatures include breakage, cut marks, anvil abrasions, burning, many missing vertebrae, and pot polishing (Table 16.1). The mass inhumation at the Grinnell Site included 374 bone fragments (Table 16.2) and contained remains of at least eight individuals, including three pre-teen children, two subadults 16 to 21 years old, and three adults: one female aged 21–25, a male aged 21–25, and a female aged 26+. These results differ from Nickens’ previous study (Luebben and Nickens, 1982) by six bones and one individual. Our age assessments also differed. Depositional Pattern The most obvious taphonomic indicator of cannibalism in the archaeological record is the presence of a non-considerate burial. Non-considerate burials, specifically those of cannibalized remains, consist of one or more individuals with evidence of trauma and disarticulation usually deposited in a nonstandard and presumably discourteous manner. Sometimes type of burial is difficult to determine because many Anasazi considerate burials are bodies disposed of in trash middens and on the floors of abandoned rooms. Considerate burials, however, usually contain one or more complete skeletons in correct anatomical position, and may be associated with grave goods. At sites with evidence of cannibalism, the osteological record demonstrates an absence of animal scavenging or bone weathering, indicating rapid interment of the remains. Similarly, bone preservation at these sites, with few exceptions, is unusually good, despite fragmentation of many of the bones. Weathering and animal gnawing are minimal, occurring on fewer than 5% of the bones. Turner and Turner (1999) attribute excellent preservation to a single, short-term disposal episode. The above characteristics closely resemble both damage patterns and depositional characteristics of the remains of large and small game animals taken for food.

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Another important taphonomic signature of cannibalism is the absence of vertebrae in bone assemblages. Those that are present are out of order anatomically. Turner postulates the underrepresentation of vertebrae may be because they were broken and boiled to extract oily contents. However, human vertebrae may be missing in burials for the same reason animal vertebrae are at archaeological sites; namely, vertebrae are left behind at the kill site. The commingled remains of eight individuals from the mass interment in Cist 2 and other parts of Kiva 2 are disorganized and highly fragmented, but well preserved. Most were deposited in Cist 2, inside, below, and around a corrugated jar. The presumably hasty manner in which this burial was prepared, including scattered remains, suggests that it is a non-considerate burial, a taphonomic indicator of violence and possibly of cannibalism. Bones found in the kiva fill may be attributed to later rodent activity (Luebben and Nickens, 1982). The entire assemblage from Kiva 2 contains only four complete and nine fragmentary vertebrae. For a sample of eight individuals, these numbers are especially small. In addition, only two bones in the previous study were interpreted as having been gnawed (Luebben and Nickens, 1982:74); the present study recorded no gnawed bone. How much time elapsed between the death and mass burial of remains in Kiva 2 is not known. Evidence suggests that the humans were processed outside the kiva. Soon afterward, they were buried inside and abandoned, either carelessly deposited by the perpetrators, or hastily cleaned up by others. Breakage Pattern An important characteristic of cannibalized remains is the prevalence and character of bone breakage. The latter suggests a perimortem timeframe just before or fairly soon after the time of death in dry climates. Peri- and postmortem damage patterns can be distinct, particularly if the former occurs on “green” or “fresh” bones, and the latter occurs on dry bones. Postmortem, dry-bone damage due to impacts with dynamic loading often includes shatter with multiple, rectangular pieces of bone. Antemortem fractures, by contrast, are more likely to show bone reaction or healing, or signs of infection. Human bones from cannibalized assemblages appear to have been processed like game animals. It is rare to find any whole bone, including the skull. Bones tend to be recovered in many small fragments with numerous pieces either missing or unidentifiable. Of the 374 human bone specimens from the Grinnell Site, only 24 are whole (most from crania), 321 are fragments, and 29 are teeth. The large proportion of fragments (93% of the sample) is indicative of perimortem bone processing (Table 16.3). Spiral fractures appear on most long bone fragments (Table 16.3; Figure 16.3). Spiral or compression fractures can result from percussion hammering against some form of anvil, although anvil abrasions, common at Anazasi cannibalism sites (Turner and Turner, 1999), were not observed in this sample. Overall, skeletal indicators of blunt trauma and perimortem damage occur on 20% of all cranial elements (Table 16.3; Figure 16.4). First, the crania have been broken apart into many fragments; however, assessment of the number of individuals present in the assemblage was possible as a result of cranial reconstruction (Figure 16.5). Cranial injuries are more ambiguous than long bone anvil fractures and could result from opening the cranium to remove the brain, death by bludgeoning, or postmortem mutilation. Empty and damaged anterior sockets suggest the front teeth of most individuals have been knocked out (Figure 16.6).

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Table 16.3

Taphonomic Factors Present on Human Remains (Number of Occurrences)

Element Maxilla Mandible Frontal Parietal Occipital Temporal Zygoma Teeth Cranial fragments Cervical vertebrae Lumbar vertebrae Miscellaneous vertebrae Scapula Clavicle Ribs Radius Ulna Phalange Navicular Pelvis Femur Tibia Fibula Long bone fragments Unidentified Total = 374

Whole 2 4

1

Fragments / Side 5L, 5R 4L, 1R, 3 3L 2R, 1 4R, 3L, 1 6

Blunt Impact Depression or Other Defect

Spiral Fractures

Cutmarks

7 4 8 4 2 2

23 10 23 2 2 4

18 1

17

Burning

29 170 4 2 7

21

1

2L 1L

1 2 1LD, 1LP, 2RP 2LP, 2RP

11 1

53

2 4

1

1 2

4

2

6

7

7

13 23

126

1R 4+ 1D, 1DR, 1LP 3 + 1D 2 68

1

3 2 61

10 321

62

80

21

Note: L = left; R = right; D = distal; P = proximal.

Figure 16.3 Photograph of spirally fractured long bone fragments from the Grinnell Site.

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Figure 16.4 Photograph of the right maxilla of a subadult approximately 16 years of age, illustrating blunt trauma on the zygomatic process (a) and cut marks near the nasal bone (b).

Figure 16.5 Photograph of the reconstructed cranium of a male aged 21 to 25 years illustrating perimortem breakage.

Burning According to Turner and Turner (1999), the presence of burned bone is another indicator of human remains being cannibalized (Table 16.1). Following butchering of animals for food, bone is often burnt during the cooking process when exposed directly to fire or not covered by a sufficient amount of flesh. Burning on human remains, Turner believes, is evidence of prehistoric cooking. He hypothesizes that burning should be evident in 2 to 35% of all elements in the cannibalized assemblage. Remains from the Grinnell Site yielded very little evidence for burning: 10 burnt and 11 slightly charred cranial fragments, comprising 5.6% of the total sample, were burnt only on the exterior surface. Although this frequency falls within the range stipulated by Turner, it is significantly lower than that observed at other southwestern sites with evidence of cannibalism.

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(a)

(b)

Figure 16.6 Photographs of the right maxilla of a subadult approximately 16 years of age illustrating cut marks near the alveolar ridge and incisors that have been evulsed.

Cut Marks Cut marks constitute a ubiquitous signature on bones that have been processed for food. On game animals, cut marks usually appear either near joints from dismemberment, or on bone surfaces where defleshing took place. Cut marks around the joints indicate that bones were disarticulated prior to final deposition. A number of sites in the Southwest contain human skeletal remains with cut marks on both crania and long bones. Cut marks on the crania probably indicate scalping or facial flaying (Allen et al., 1985). Cranial elements from the Grinnell Site exhibited 126 cut marks. Most of them were on the maxilla in the nasal area and above the teeth (Figures 16.4 and 16.6), on mandibles, and on the frontal bone above the orbits. Occasionally, cut marks were even observed inside the orbits, and one cut mark and one scrape were noted on the interior of a skull. Post-cranial elements exhibited 45 cut marks, including 7 chopper marks on a tibia fragment. All cut marks occurring on long bone fragments were near the proximal and distal ends of bones, suggesting disarticulation and butchering of meat. Pot Polish The last taphonomic signature in Turner’s criteria is the presence of pot polish. Although not widely accepted (Bahn, 1992), pot polish is one of the main taphonomic indicators

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of cannibalism at Anasazi archaeological sites (Turner and Turner, 1999). “Pot polish” is a term used to describe a smooth polish that appears on the ends of bones that were cooked in prehistoric vessels to extract grease or oil. When cooked and stirred in a pot tempered with coarse sand, the gritty inner surface of the vessel causes the edges of bone to become smooth and polished. This polish is visible to the naked eye, and striations are clearly visible with a scanning electron microscope. The presence of polish on human bones cannot be attributed to deliberate polishing; no evidence for this practice exists on animal bones or elsewhere in the Southwest (Turner and Turner, 1999). Bone remains from the Grinnell Site do not exhibit evidence of pot polishing. This absence does not necessarily rule out that human remains were cooked or eaten; however, Turner (1983) claims that the presence of pot polish is necessary to support an argument for cannibalism (Table 16.1).

Conclusions A reanalysis of the osteological data from the Grinnell Site provides evidence that eight individuals met a violent and traumatic end as indicated by extensive perimortem breakage patterns, including both blunt- and sharp-force trauma to crania and long bones. Although the Grinnell Site contains considerable evidence that Turner (1983), Turner and Turner (1999), and others have considered indicative of cannibalism, two main taphonomic criteria are missing: pot polishing and high frequency of burning. It is possible that cannibalism could have occurred without leaving these markers, but using Turner’s criteria, the Grinnell Site remains should not be considered evidence of cannibalism. A more conservative assessment nevertheless still indicates perimortem trauma. There is no evidence for the use of projectile or stabbing weapons, but such evidence could have perished with the soft parts and missing bones. Facial crushing and cranial fractures suggest that these individuals were beaten to death. While the bones were still high in fat and moisture, they were dismembered with stone tools. Their heads were mutilated or flayed, and probably broken up further. The limbs were defleshed enough that long bones could be extensively fragmented. Whether the Grinnell Site people were eaten or not, they were probably victims of the endemic violence and warfare for which evidence is accumulating in the prehistoric Southwest (Haas and Creamer, 1993; LeBlanc, 2000).

Acknowledgment We would like to acknowledge Steve Bicknell for figures and photographs.

References Allen, W.H., C.F. Merbs, and W.H. Birkby 1985 Evidence for prehistoric scalping at Nuv Akwewtaqa (Chavez pass) and Grasshopper Ruin, Arizona. In Health and Disease in the Prehistoric Southwest, edited by C.F. Merbs and R.J. Miller, Anthropological Research Papers No. 34, Arizona State University, Tempe, AZ. Arens, W. 1979 The Man-Eating Myth: Anthropology and Anthropophagy, Oxford University Press, New York.

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Bahn, P. 1992 Ancestral cannibalism gives us food for thought, New Scientist 134(1816):40–41. Bass, W.M. 1987 Human Osteology: A Laboratory and Field Manual, 3rd ed., Special Publication No. 2, Missouri Archaeological Society, Columbia. Billman, B.R., P.M. Lambert, and B.L. Leonard 2000 Cannibalism, warfare, and drought in the Mesa Verde region during the twelfth century A.D., American Antiquity 65(1):145–178. Buikstra, J.E. and D.H. Ubelaker, Editors 1994 Standards for Data Collection from Human Skeletal Remains, Arkansas Archaeological Survey Research Series No. 44, Fayetteville. Darling, J.A. 1999 Mass inhumation and the execution of witches in the American southwest, American Anthropologist 100(3):732–752 Dongoske, K.E., D.L. Martin, and T.J. Ferguson 2000 Critique of the claim of cannibalism at Cowboy Wash, American Antiquity 65(1):179–190. Fagan, B.M. 1995 Ancient North America: The Archaeology of a Continent, Thames & Hudson, New York. Haas, J. and W. Creamer 1993 Stress and Warfare among the Kayenta Anasazi of the Thirteenth Century A.D., Fieldiana, Anthropology, Field Museum of Natural History, Chicago, IL. Hough, W. 1902 Ancient people of the petrified forest of Arizona, Harper’s Monthly, 105:897–901. LeBlanc, S.A. 2000 Prehistoric Warfare in the American Southwest, The University of Utah Press, Salt Lake City. Luebben, R.A 1983 The Grinnell Site: a small ceremonial center near Yucca House, Colorado, Journal of Intermountain Archaeology II:1–26. Luebben, R.A. and P.R. Nickens 1982 A mass interment in an early Pueblo III kiva in southwestern Colorado, Journal of Intermountain Archaeology I:66–79. Nickens, P. R. 1979 Osteological Analysis of Human Skeletal Material from the Grinnell and Ismay Sites, Montezuma County, Southwestern Colorado. Manuscript in author’s possession. Preston, D. 1998 Cannibals of the canyon, The New Yorker 74:76–89. Turner, C.G., II 1983 Taphonomic reconstructions of human violence and cannibalism based on mass burials in the American southwest. In Carnivores, Human Scavengers, and Human Predators: A Question of Bone Technology, edited by G.M. LeMoine and A.S. MacEachern, pp. 219–240. Archaeological Association, University of Calgary, Calgary. Turner, C.G., II and J.A. Turner 1999 Man Corn: Cannibalism and Violence in the Prehistoric American Southwest, The University of Utah Press, Salt Lake City. White, T.D. 1992 Prehistoric Cannibalism at Mancos 5MTUMR-2346, Princeton University Press, Princeton.

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Damnum Fatale: The Taphonomic Fate of Human Remains in Mass Disasters PAUL S. SLEDZIK WILLIAM C. RODRIGUEZ, III Contents Introduction Literature Review Disaster-Specific Taphonomy Aircraft Accidents Bombing and Explosions Earthquakes Fires Floods Infectious Disease Outbreaks Landslides, Mudslides, and Avalanches Mass Suicides Tornadoes and Hurricanes War-Related Deaths and Weapons of Mass Destruction Conclusion References

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Table 17.1

Forensic Anthropological Skills for the Mass Fatality Incident (MFI) At the Scene

• • • •

Set up grid system for search and recovery of remains Locate, recognize, and recover human remains, especially those burned and fragmented Document location of remains within grid units Devise search criteria based on size and scope of disaster In the Morgue

• • • • • • • • • • •

Assist in triage of remains Describe incomplete/fragmentary remains and conditions of remains Conduct forensic analysis to determine sex, age, race, stature, and distinguishing characteristics Separate commingled remains Obtain radiographs for age estimation and unique skeletal features Reassociate body parts based on biological profile and descriptions of missing parts Determine minimum number of individuals based on remains recovered Assist in organizing identification exclusion/inclusion matrix Compare antemortem and postmortem data (e.g., radiographs, skeletal information) Assist in age determination of complete remains/bodies Analysis of trauma patterns/evidence and crash-related injuries

Introduction The public health and economic effects of natural and technological (manmade) disasters increased dramatically during this century. International public health agencies report that natural disasters disrupted the lives of 800 million people, caused more than $50 billion in property damage, and killed 3 million people in the past 2 decades (International Federation of Red Cross, 1993). With global population growth and the development of vulnerable areas, disasters will claim more lives and property in the future (Noji, 1994). Disaster planners and emergency managers call a mass disaster involving a large number of deaths a mass fatality incident (MFI). MFI management has undergone significant change in the past decade, as a greater focus is placed on the search for, recovery of, and identification of human remains. The forensic anthropologist plays a key role in these areas. Forensic archeology, skeletal analysis, and other skills are invaluable to the MFI response (Sledzik, 1996a,b; 1998). Table 17.1 enumerates these and other forensic anthropological skills used in an MFI. As the end result of the perimortem and postmortem factors affecting the human body during and after a disaster, disaster taphonomy can be viewed as a continuum, with survival and total disintegration of the body at opposite ends of the scale. Along the continuum, two groups of factors impact the human body: primary and secondary. Table 17.2 delineates these factors. Primary factors result directly from the disaster, and may be the cause of death. Secondary factors affect the body after death. For example, in an explosion, taphonomic changes may result from the actual blast (primary), the crushing effects of the collapsing structure, and burning from the ensuing fire. Primary and secondary effects may be indiscernible. Because disaster forces are more variable in duration and intensity than those encountered during normal decomposition and skeletonization, predicting the taphonomic outcomes of

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Table 17.2 Primary and Secondary Factors Affecting Human Preservation in Mass Disasters Primary

Secondary

Explosion fragmentation G-force impact fragmentation Burning Crushing (structure collapse) Dismemberment (e.g., from flying debris)

Burning Temperature and humidity effects Water effects (warm, cold, salt, fresh) Decomposition effects Crushing (e.g., building collapse) Carnivore/rodent actions Freefall injuries Ground impact injuries

a specific disaster is difficult. The forensic anthropologist should understand these forces, how they influence taphonomy, and how they affect search, recovery, analysis, and identification. For example, disasters involving high speed and flammable products (e.g., an aircraft accident) leave human remains burned and highly fragmented. In these cases, fragmentation occurs before burning, resulting in remains that are unassociated, fragmented, and burned. In house fires, remains may be extremely burned, but they generally are not unassociated.

Literature Review If disaster taphonomy is defined as the preservation of human remains in an MFI, few publications exist in the forensic anthropological literature. The paucity of published information is likely due to several factors: forensic anthropology’s recent focus on taphonomy, the relatively recent inclusion of the forensic anthropologist into the MFI team, the focus on identification rather than taphonomy during MFI work, and restrictions on the use of MFI victim data for publication. Some taphonomic information can be gleaned from forensic pathology or aerospace medicine publications. Aerospace pathology confines itself to the examination of injuries received in aircraft accidents, using the pattern of these injuries to help determine the cause of the accident. However, some of these publications mention taphonomic factors. Forensic pathology publications discuss taphonomic issues, but these are largely early postmortem changes or general discussions of fragmentation and burning. Taphonomic information can be extracted from the forensic reports of specific disasters (e.g., TWA 800 and KAL 801 reports on the National Transportation Safety Board web site, www.ntsb.gov). T. Dale Stewart’s edited volume Personal Identification in Mass Disasters (Stewart, 1970) is the earliest work examining forensic anthropology in disasters. One chapter in that volume, “Identification Involving Atrocities” by A. Keith Mant, discusses the appearance of remains from aircraft that “crashed, caught alight, and exploded.” The remains were a few inches in size and the author presents his methods for determining the minimum number of individuals. Because only a few publications by forensic anthropologists give insight into taphonomic issues in specific disaster situations, these publications will be referred to in the sections pertaining to specific disasters.

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Table 17.3 Characteristics of Decelerative Crash Forces Observation Vertebral body compression Fracture dislocation of C1/C2 Mandible fractures Skull fractures Pelvic fractures Total body fragmentation

G-force 20–30 20–40 40 50+ 100–200 350+

Disaster-Specific Taphonomy The cause and outcome of every disaster are unique. The preservation of human remains in a disaster is unique as well. Generalities about taphonomic changes related to specific disasters are extractable from the working knowledge in the literature by forensic anthropologists. These changes are grouped below into categories based on disaster type. The taphonomic categories reflect the forces acting during and after the disaster. Aircraft Accidents Aircraft accidents involve a variety of forces: forces, fire, freefall, impact, and environmental effects. Impact g-forces cause fragmentation — the greater the g-force at impact, the greater degree of fragmentation. After a crash, a fire often ensues. The intensity and duration of the fire determine the degree of burning to the remains. When fragmentation and burning are combined, the degree of preservation of body parts and bone decreases. Other factors, such as water and freezing temperatures, also alter decomposition. There are some consistencies in how remains are fragmented during a crash that are related to the forces experienced during the crash and anatomical structures (Hill, 1989; Wagner, 1990) (Table 17.3). Large joints (e.g., hip, knee, and ankle) are often recovered because numerous ligaments hold these joint areas together. The authors observed this preservation after several crashes, including the 1994 crashes of USAir 427 and American Eagle 4184. In addition, cranial bones fragment severely at impact, leaving little of the cranium intact because of the jelly-like actions of the brain within the cranial cavity (Hill, 1989). An estimate of the degree of fragmentation and tissue destruction can be made by comparing the total weight of recovered remains to the estimated total weight of passengers before the crash. Slower impact crashes, such as a controlled flight into terrain or a ditching, exhibit a greater range of preservation. In the controlled crash of a United Airlines jet in Sioux City, Iowa, in 1989, 17 people survived the crash, and the 110 dead showed fragmentation and burning (Randall, 1991). A wide range of preservation, from calcined bone to complete bodies was documented in the crash of KAL 801 on Guam in 1997 (Saul and Saul, 1999). The 1985 crash of Delta 191 at Dallas/Fort Worth International Airport was documented by Gilliland and co-workers (1986). The crash killed 137 people, including one on the ground. Intact bodies were flattened from front to back and incurred cranial damage at the level of the mouth. First-class passengers and the cabin crew suffered the most disruptive injuries; some were not recognizable as human. Most of the survivors were in the back of the plane, a finding mistakenly interpreted to mean that the safest seats on all aircraft are in the rear.

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The 1989 crash of a Norwegian aircraft into the ocean revealed a pattern of trauma (Gregersen et al., 1995). Of the 48 bodies recovered (most of which were in complete condition), the most frequently observed fractures were of the ribs (100% of the victims), skull (96%), pelvis (88%), face and spine (83%), sternum (71%), lower leg (63%), thigh (58%), and upper arm (56%). Few fractures of the hand (19%) and foot (17%) were observed. The authors report that a small percentage of the fractures resulted from the midair breakup of the aircraft; a majority were caused by the impact. Hinkes (1989) examined the role of forensic anthropology in resolving identification issues at the 1985 crash of a chartered DC-8 in Gander, Newfoundland, carrying 256 U.S. military personnel. She reported that the remains were incinerated and dismembered. Her work involved assessing age, sex, stature, and race, determining the minimum number of individuals, and reassociating remains, which were fragmented and shrunk due to postcrash burning. Of the 50 sets of remains she analyzed, four consisted of a lower torso (hip to mid-thigh), two were hemipelves with legs and feet, and one comprised a head and shoulders. Explosions and breakups of aircraft in midair pose other taphonomic challenges. The bombing of Pan Am 103 over Lockerbie, Scotland, and the explosion of TWA 800 off Long Island, New York, and other similar accidents have been examined (Eckert, 1990.) In the Pan Am 103 case, the remains were subjected to high winds, flying debris, and impact. Eckert (1990) reported that none of the remains overtly showed evidence of the explosion. Of the 264 passengers killed, more than 160 were bodies that landed individually or in clusters. If the conditions are right, the actions of humans may influence aircraft accident victim taphonomy. The U.S. Army Central Identification Laboratory, Hawaii (CILHI) recovers and identifies U.S. servicemen killed in Southeast Asia. CILHI’s experience in examining highly fragmented, skeletonized remains that have been in soil for nearly 40 years is unique and important (Holland, Anderson, and Mann, 1997; Holland and Mann, 1996; Webster, 1999). Of particular note are remains removed by Southeast Asian residents and modified for use in the “bone trade.” Bombing and Explosions An explosion creates direct and indirect forces that cause body fragmentation. A body impacted by a direct explosive force (e.g., landmine) is fragmented in large pieces. Indirect explosive forces impact the body after the initial explosion; for example, a body may be crushed in a building collapse caused by an explosion. Marshall (1993) divides the injurious effects of explosions into six categories: complete disruption, explosive injury, injury by separate fragments, injury by falling masonry, burns, and blast. Complete disruption occurs when the body is in close contact to a large explosive. As the location of a victim moves away from the explosion, the amount of trauma will decrease. Victims within a meter of the explosion will be severely mangled, while those farther away will incur less damage. Falling structures cause nonspecific traumatic injuries that can be discerned from blast-related injuries. Remains fragmented by an explosion can differ from fragmented remains from a highspeed plane crash. In a bombing, the fragmentation is a result of bomb construction, device detonation, and the presence of flying debris from the explosion. The explosive forces may not be applied in equal strength to the body as a whole. Severe fragmentation is often seen

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if the victim was near the detonation site. The farther the person is from the detonation site, the larger the body parts (e.g., foot and lower leg, entire arm, head) recovered. Kahana and co-workers (1997) describe the methods used to identify remains from suicide bombings in Israel from 1993 to 1996. Many of these bombings took place in public places and involved cars, buses, or metallic objects used in the bombs. Of the 136 bodies examined, 17.4% of the victims showed total disruption of the body, 69.7% showed explosive injuries, 10.4% showed injuries from flying debris, and 2.3% showed injuries directly related to the blast. Earthquakes A majority of earthquake deaths are due to falling buildings, masonry, or engineering structures (Alexander, 1985). Studying the mortality following a 1985 earthquake in Chile, Ortiz et al. (1986) reported that of 145 documented deaths, 53 (36.6%) were the result of injury to the skull. Other causes included multiple trauma (52 cases), thorax crush injuries (12 cases), and myocardial infarction (10 cases). Remains from earthquakes typically will be found crushed but complete inside collapsed structures. Although normal decomposition will occur, there may be some variation in the severity and extent of the trauma may occur. Fragmentation and burning of remains may not happen unless explosions and fires occur as a secondary effect of the earthquake. Earthquakes have left bioarcheological evidence. The New Madrid earthquakes of 1811–1812 devastated large areas of western Tennessee and Kentucky, northeast Arkansas, and southeast Missouri. Prehistoric Native American burials at the Campbell site in Missouri were impacted by the quakes, causing disruption of skeletal elements and creating fissures cutting through skeletons (Chapman et al., 1955). Fires Fires can be the primary cause of death or may cause secondary effects. Heat-related shrinkage of the muscles results in the pugilistic position, often preserving the fingertips, which are useful for identification. In more severe fires the ends of the protruding long bones may become burned, while the shafts of the bone are less affected by burning. Blowout fractures of skull result from vapor pressure within the heated cranial vault. Secondary effects of fire may be seen in aircraft accidents, bombings, and explosions and as a secondary effect can involve intact whole bodies or fragmented remains. The intensity of the fire may cause charring, burning, or calcination. Ubelaker et al. (1995) reported on the taphonomy of the victims of the Branch Davidian fire in 1993. The data collection procedure for bone inventory allowed the authors to reconstruct the preservation of bones in body regions (e.g., head/neck, arm/shoulder, chest, etc.) and the completeness of major bones. They report that the more massive and better protected bones were more frequently preserved. Pelvic bones were most often found complete. The mandible and maxilla was least often preserved. Bones of anthropological interest that were most often preserved were the os coxae and femora. Floods Flash floods and hurricane storm surges are the most common flood events. About 90% of flash flood deaths are attributable to drowning (French et al., 1983). Debris in the

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floodwaters results in trauma and dismemberment to bodies. Large body sections with multiple fractures are often observed. Severe fragmentation resulting in small body parts is infrequent. Charney and Wilber (1980) described their efforts to identify remains recovered from the 1976 Big Thompson flood in Colorado. They noted that all 139 bodies recovered after the flood were whole or partly fragmented. Bodies were difficult to locate because mud and silt camouflaged the remains. Many bodies showed evidence of multiple fractures, loss of extremities, bruises, abrasions, and avulsions, presumably from impact with stationary objects or floating debris. Sledzik and Hunt (1997) reported on the processing and identification of skeletal and fleshed remains from a cemetery washed away during the 1993 midwestern United States floods. Thousands of skeletal elements and several hundred bodies in various states of preservation were recovered. The search and recovery methods and the size of the search area (more than 34,000 acres) resulted in the recovery of recognizable human remains (e.g., crania) and large bones (e.g., femora). No discernible pattern of preservation based on the length of internment was noted in either the complete bodies or partial remains. To understand the taphonomy of a flood event, the anthropologist should examine the factors leading to the flood (e.g., flash flood, hurricane) and the location of the event (e.g., rural, urban). Knowledge of intervening factors such as the amount of debris the bodies may encounter aids in assessing taphonomic information. Infectious Disease Outbreaks Emerging and reemerging infectious diseases threaten public health worldwide. At present, deaths from these diseases that intersect with forensic identification are limited. Pathologists play an important role in identifying emerging diseases such as Hantavirus, but, at present, there has been no outbreak requiring identification of large numbers of fatalities. The taphonomic aspects of an MFI involving a disease outbreak are speculative. Since most infectious diseases take time to cause death, there is the opportunity for the exposed person to seek medical care. In a mass exposure situation, local health care facilities would be overwhelmed by a large number of deaths. People may also die at home or in a quarantine facility. Once decomposition begins, the way the disease affects the body may alter the normal decomposition pattern; for example, purging of blood, vomit, or urine/feces from the body may cause more rapid decomposition. Epidemiological issues are important in disease outbreaks. Forensic specialists should use typical crime scene documentation procedures in a disease-related MFI. Death scene documentation would supplement the pathological information to help understand disease etiology. In addition, information on the age, sex, and race of the individual is helpful in epidemiological analyses. Landslides, Mudslides, and Avalanches The effects of mudslides, landslides, and avalanches on the human body after death would presumably by similar to those seen in flood events — whole bodies showing some dismemberment. The degree of fragmentation would be a function of the force of the event, the distance traveled, and the amount of debris encountered during transport. The presence of a large amount of mud, earth, or snow may act to preserve bodies.

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Mass Suicides Mass suicide deaths caused by poison will not directly cause taphonomic changes of interest to the anthropologist. But, if the time from death to discovery is long, decomposition will occur. This happened after the mass suicide of over 900 members of a religious cult in Jonestown, Guyana, in 1978. The bodies were first examined 6 days after the event, and a range of decomposition was noted (Thompson, Manders, and Cowan, 1987). Tornadoes and Hurricanes Flash floods and the storm surges associated with hurricanes are the most common flood events. About 90% of hurricane deaths are due to drowning (Noji, 1993), and the same percentage is reported for flash floods (French et al., 1983). Bodies can be struck by debris, resulting in trauma and dismemberment. In general, large body sections are often seen and severe fragmentation resulting in small body parts is infrequent. War-Related Deaths and Weapons of Mass Destruction Wars can leave large numbers of combatants and noncombatants dead from a variety of causes. Bombs and gunfire are the common modern methods of wartime killing. The most recent wave of concern among disaster managers is the potential for a chemical or biological weapon used against a civilian population, a so-called weapon of mass destruction (WMD). Although these two terms are often linked, the effects of chemical and biological weapons differ greatly, and are mostly in the area of onset time of symptoms (or incubation period of the pathogen) and the biological effects on the victim. In a biological attack, days may pass before death occurs. Epidemiological tracking of disease symptoms and deaths is the only way to accurately assess if a biological weapon has been used (Franz et al., 1997). Most emergency managers and bioweapon experts believe that most bioweapon deaths will occur in hospitals. No resultant taphonomic effects will be observed in this situation. Conceivably, in the event of a large number of deaths or where the body is not recovered for a period of time, differential decomposition may occur, depending on the pathogen used. In some situations, certain animal “sentinels” may be the first to die. If the bioweapon kills carnivores, no dispersal of the body by this method would occur. Deaths from chemical weapons are more rapid. Many chemical weapons affect the skin and internal organs, which may lead to differential decomposition. The effects on skeletonization are unknown.

Conclusion Disasters are chaos in action. Taphonomy, like chaos, is characterized by being consistent only in its variability. The forensic anthropologist reassembles the human body after the chaos of a disaster takes it apart. In a sense, the forensic anthropologist continually fights the second law of thermodynamics. In the realm of disasters, one cannot help but be impressed by how difficult it is to predict how the human body will be deposited in the environment. We have attempted to document our experiences and those of others, and do some extrapolating to help understand the taphonomic effects of disasters.

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References Alexander, D. 1985 Death and injury in earthquakes, Disasters 9:57–60. Chapman, C.H., L.O. Anderson, and R.F. Spier 1955 The Campbell Site: a late Mississippi town site and cemetery in southeast Missouri, Missouri Archaeologist 17:3–140. Charney, M. and C.G. Wilber 1980 The Big Thompson flood, American Journal of Forensic Medicine and Pathology 1:139–144. Eckert, W.G. 1990 The Lockerbie disaster and other aircraft breakups in midair, American Journal of Forensic Medicine and Pathology 11:93–101. Franz, D.R. et al. 1997 Clinical recognition and management of patients exposed to biological warfare agents, Journal of the American Medical Association 278:399–411. French, J. et al. 1983 Mortality from flash floods: a review of national weather service reports, 1969–1981, Public Health Reports 98:584–588. Gilliland, M.G.F. et al. 1986 Disaster planning for air crashes: a retrospective analysis of Delta Airlines flight 191, American Journal of Forensic Medicine and Pathology 7:308–316. Gregersen, M., S. Jensen, and P.J.T. Knudsen 1995 The crash of the Partnair Convair 340/580 in the Skagerrak: traumatological aspects, Aviation, Space, and Environmental Medicine 66:152–157. Hill, I.R. 1989 Mechanism of injury in aircraft accidents — a theoretical approach, Aviation, Space, and Environmental Medicine 60(7, suppl.):A18–25. Hinkes, M.J. 1989 The role of forensic anthropology in mass disaster resolution, Aviation, Space, and Environmental Medicine 60(part 2):A60–A63. Holland, T.D. and R.W. Mann 1996 Forensic aviation archaeology: finding and recovering American MIA remains, Cultural Resource Management 19(10):29–31. Holland, T.D., B.E. Anderson, and R.W. Mann 1997 Human variables in the postmortem alteration of human bone: examples from U.S. war casualties. In Forensic Taphonomy: The Postmortem Fate of Human Remains, edited by W.D. Haglund and M.H. Sorg, pp. 263–274. CRC Press, Boca Raton, FL. International Federation of the Red Cross and Red Crescent Societies 1993 World Disasters Report. Martinus Nijhoff, Dordrecht, The Netherlands. Kahana, T., M. Fruend, and J. Hiss 1997 Suicidal terrorist bombings in Israel — identification of human remains, Journal of Forensic Sciences 42:260–264. Mant, A.K. 1970 Identification involving atrocities. In Personal Identification in Mass Disasters, edited by T.D. Stewart, pp. 11–18. Smithsonian Institution, Washington, D.C. Marshall, T.K. 1993 Violence and civil disturbances. In The Pathology of Trauma, 2nd ed., edited by J.K. Mason, pp. 71–85. Hodder and Stoughton, London.

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Noji, E.K. 1993 Analysis of medical needs during disasters caused by tropical cyclones: anticipated injury patterns, Journal of Tropical Medicine and Hygiene 96:370–376. 1994 Progress in disaster management, Lancet 343:1239–1240. Ortiz, M.R. et al. 1986 Brief description of the effects of the earthquake of 3rd March 1985, Chile, Disasters 10:125–140. Randall, B. 1991 Body retrieval and morgue operations at the crash of United flight 232, Journal of Forensic Sciences 36:403–409. Saul, F.P. and J.M. Saul 1999 The evolving role of the forensic anthropologist as seen in the identification of the victims of the Comair 7232 (Michigan) and KAL 801 (Guam) aircrashes, Proceedings of the American Academy of Forensic Sciences 5:222. Sledzik, P.S. 1996a Physical anthropology’s role in identification of disaster fatalities. In Proceedings of the Second National Symposium on Dentistry’s Role and Responsibility in Mass Disaster Identification, pp. 62–64. American Dental Association, Chicago, IL. 1996b Federal resources in mass disaster response, Cultural Resources Management 19(10):19–20. 1998 Anthropology and mass fatality response. In Proceedings of the International Symposium on Family and Victim Assistance for Transportation Disasters, National Transportation Safety Board, September 28–29, 1998, Arlington, VA. Sledzik, P.S. and D.R. Hunt 1997 Disaster and relief efforts at the Hardin Cemetery. In In Remembrance: Archaeology and Death, edited by D.A. Poirier and N.B. Bellantoni, pp. 185–198. Bergin and Garvey, Westport, CT. Stewart, T.D., Editor 1970 Personal Identification in Mass Disasters, Smithsonian Institution, Washington, D.C. Thompson, R.L., W.W. Manders, and W.R. Cowan 1987 Postmortem findings of the victims of the Jonestown tragedy, Journal of Forensic Sciences 32:433–443. Ubelaker, D.H. et al. 1995 The role of forensic anthropology in the recovery and analysis of Branch Davidian Compound victims: recovery procedures and characteristics of the victims, Journal of Forensic Sciences 40:335–340. Wagner, G.N. 1990 Aerospace pathology. In Handbook of Forensic Pathology, edited by R.C Froede, pp. 197–204. College of American Pathologists, Northfield, IL. Wagner, G.N. and R.C. Froede 1993 Medicolegal investigation of mass disasters. In Spitz and Fisher’s Medicolegal Investigation of Death: Guidelines for the Application of Pathology to Crime Investigation, edited by W.U. Spitz and R.S. Russell, pp. 567–584. Charles C Thomas, Springfield, IL. Webster, A.D. 1999 Human taphonomy and its impact on forensic recovery operations in Vietnam, Proceedings of the American Academy of Forensic Sciences 5:211–212.

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Approaches to the Study of Commingling in Human Skeletal Biology DOUGLAS H. UBELAKER Contents Introduction Morphological Techniques Fluorescence Trace Element Analysis An Ossuary Example Portuguese Medieval Battle of Aljubarrota The Crow Creek Massacre Site The Search for Father Bachelot Taphonomic Factors in Commingling Animal Chewing Bone Density Excavation Factors Curation Practices Number of Individuals Represented by Bone Counts Summary References

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Introduction In forensic anthropology, commingling refers to the mixing together of remains of different origins. Usually the term applies to situations in which remains of more than one individual have become mixed together. The scientific problem is to determine if this has occurred, and, if so, what parts and what different individuals are represented. In the most general terms, commingling refers to the mixing of evidence in a manner that may require scientific study to differentiate the various components. Although in recent years much has been written about many aspects of forensic anthropology, relatively little attention has been focused on issues of commingling. The topic is largely absent in a frequently cited text by Krogman (1962) and the revision by Krogman and Iscan (1986). Stewart’s classic Essentials of Forensic Anthropology (1979) devotes only 2 of its 300 pages to the topic. Yet increasingly, forensic anthropologists must apply their scientific skills to issues of commingling. As noted by Stewart (1979:38), commingling usually is not an issue in forensic anthropology analysis because many of the materials we examine are recovered in contexts suggesting the presence of a single, isolated individual. Even these, however, have to be screened for mixed-in nonhuman elements, including the remains of nonhuman animals that can closely resemble those of humans. This process is usually easy when whole bones are involved. Difficulties intensify when remains have been fragmented, burned, or otherwise altered. As noted by Stewart, this is largely a sorting problem. The criteria used to sort human remains are mostly morphological. The first step is usually a detailed inventory listing bones by type and side. The presence of multiple bones from the same type and side (e.g., two left tibiae) indicates clear evidence of commingling. Lack of such evidence by itself does not preclude the possibility of commingling; it just does not confirm it. For example, if 15 human bones are recovered without anatomical duplication, commingling is not proven, but it is possible that as many as 15 individuals could be represented. If duplication among the 15 bones was confined to only the presence of 2 left tibiae, the evidence would establish that at least 2 individuals are present (minimum number) but would not establish the actual number represented. The amount of detail recorded in the inventory should be guided by the problem, and the condition of the remains. Buikstra and Ubelaker (1994) provide an inventory system developed from input by practicing skeletal biologists. Because this system is widely utilized, it also offers the advantage of capturing data that can be compared broadly. This inventory is not exhaustive; rather, it captures information considered to be most important in comparative analysis. Bones of the skull are coded as complete (at least 75% present), partially complete (between 25% and 75% present), poorly preserved (present but less than 25%), or absent. The postcranial bones other than limb long bones are recorded in a similar manner, except that some components of these bones are recorded separately (e.g., the glenoid fossae of the scapulae). For limb long bones, the degree of preservation categories are applied to the proximal and distal epiphyses and three sections of the diaphyses. The advantage of this system over simpler systems for assessing commingling is the level of detail that can be used to detect part duplication. To determine the number of individuals represented by commingled remains beyond duplication of bone type and side, it is useful to consider age at death, sex, general bone size, and other information as applicable. For the next layer of detail beyond bone type and side, many investigators turn to age at death. A simple sort of immature and mature

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can yield useful results, although the criteria for such determinations become important. For long bones, if epiphyseal union is employed as a criterion, it must be remembered that union occurs earlier in females than in males, the timing and rate of union differ for the different bones and considerable time can elapse between beginning and complete epiphyseal fusion (Ubelaker, 1989). For example, because it unites early, the distal tibia from an adolescent might appear to be mature whereas the sternal clavicle (uniting relatively late) from the same individual might appear to be immature. Observations on the general morphology of bone fragments can be relevant in some situations. For example if some skeletal or dental evidence within fragmentary remains suggests that a young infant or fetus is present, then the additional presence of mature bone (as suggested by bone type, size, and/or shape) of a nature that could not be present in a younger individual would suggest commingling, even though the specific age of the more mature bone could not be determined. If relatively few individuals are involved, it might be useful to attempt to assemble the remains into likely individuals, in consideration of not only bone type, side, and age at death, but also overall bone size and shape. This exercise can be especially revealing with fragmentary remains in which, for example, several left tibia fragments all could have originated from one bone. It also may be possible to observe the morphological relationship of bones that articulate and determine if multiple individuals are represented. This process has been termed “positive articulation” by Kerley (1972:355) and may provide important information, depending upon the skills of the observer and the nature of the evidence. More sophisticated sorting approaches can involve chemical or radiographic techniques.

Morphological Techniques As early as 1972, Kerley emphasized the importance of experience in the ability to detect commingling and to sort out the respective individuals. He also emphasized the value of comparative morphology, with thoughtful evaluation of age at death, sex, and ancestry. He appropriately recommended caution in the interpretation of differences in coloration patterns because environmental factors that likely contribute to such differences frequently are not known in forensic analysis. Kerley also called attention to specific analytical techniques that offered some potential for analysis of commingling, namely, ultraviolet light analysis of fluorescence, radiographic approaches, blood-type study, and neutron activation analysis. Rösing and Pischtschan (1995) also offer a review of approaches to the assessment of commingling. They provide excellent discussion of mathematical approaches, but recommend (beyond inventory) the use of sex, robusticity, age at death, bone color, surface preservation, and bone density. Judgment and experience are usually required to assess the probabilities of articulating bones originating from the same individual. Such evaluations are best made in areas of the skeletal anatomy where the relationship between articulating bones is especially close. Examples are the vertebral articular facets (including the occipital condyles of the cranium) and femur/acetabulum articulation. London and Curran (1986) and London and Hunt (1998) have called attention to the value of the latter in contributing useful information for commingling evaluation. Their research suggests that a combination of observations and measurements facilitates evaluation of the femoral head and acetabulum relationship.

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Buikstra and Gordon (1980) document how evaluation of the articular surfaces and general morphology of the cervical vertebrae can be useful in assessing commingling. Their study of the Smithsonian’s Terry collection emphasizes the use of both measurements and observations of epiphyseal union in establishing the probabilities involved. In a later publication, Buikstra et al. (1984) provide more detail on how such an approach proved useful in a dispute regarding, in part, if cervical vertebrae found in one location originated from the same individual as other cervical vertebrae from another location. These two publications also present useful summaries of the literature (largely not duplicated here) relating to these issues. Bone weight represents another variable that could be relevant in some commingling assessments. Much of the relevant data here stems from an early interest in the relationship between bone weight and body weight. As noted by Baker and Newman (1957), this correlation is only very general; however, within individuals the correlation of the relative weight of individual bones is substantial. Using data gathered from 125 skeletons of war dead examined in Kokura, Japan, at Army Graves Registration Service Headquarters, they produced regression equations that enable dry weight of individual bones to be predicted from another bone. For example, using their regression equations, the approximate weight of a tibia could be predicted from a femur of the same individual. Baker and Newman (1957) offer a more detailed procedure for evaluating commingling using weight and other data. Stewart (1979) critically evaluated this approach: “Given the limitation of the method to fat-free bones, I feel compelled to express doubt that the separation of commingled remains by this untested metrical means can be done any better than, if as well as, by eye. Also, most certainly the eye can do the job faster” (Stewart, 1979:225–226). In spite of the difficulties of using bone weight as a specific indicator of body weight, extreme situations can support opinions in some circumstances. Murray and Rose (1993) describe a civil case involving the analysis of cremains, the residue of human cremation. In this case two sets of cremains were present. Both had been presented to a family as representing the cremains of a particular decedent. Analysis revealed differences between the two sets of cremains, indicating to the authors that they did not originate from the same individual. The combined weight of the two sets of cremains was larger than the weight expected by the authors from a single individual. The weight information contributed to the evaluation that more than one individual was represented. As discussed above, duplication of skeletal parts offers positive evidence of commingling; however, the lack of duplication, by itself, does not prove that commingling did not occur. As noted by Snow and Folk (1965), in most forensic contexts, in the absence of duplicated bones, the likelihood of commingling diminishes with the increasing size of the sample. They provide a statistical procedure to evaluate the probabilities involved. Snow and Luke (1970, 1984) further offer an example of how the statistical evaluation procedure (Snow and Folk, 1965) can be applied in an actual forensic case. In the 1960s two children disappeared from the Oklahoma City area. Skeletonized child remains were later recovered with no duplication of skeletal elements. The application of the mathematical approach to the recovered remains suggested a high likelihood that only one individual was present. This contributed to the case interpretation that only one individual had been recovered.

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Fluorescence McKern (1958) suggested that the fluorescence of human bone when viewed under short wave ultraviolet light can be useful in some situations to evaluate commingling. His test of this technique on a large sample of human remains suggested it might be useful at times for sorting remains of individuals. The problem is not only the natural variation within a skeleton for fluorescence, but also how it is influenced by postmortem effects that may have operated differentially on the different bones represented. Eyman (1965) experimented with human bones from individuals from an archeological context using a modification of this approach. Eyman found that ultraviolet fluorescence was useful in indicating which bones originated from the same individual, but it was less successful in separating individuals from different archeological sites.

Trace Element Analysis In 1970, Guinn called attention to the potential of trace element analysis, particularly neutron activation analysis, in forensic analysis. In short, this application assumes that if two specimens being tested share not only major-element components but also minor or trace element components, they likely originated from the same source. Guinn noted that the technique was then widely used on many materials recovered in a forensic context and had excellent potential when applied to hair or blood if contamination factors could be controlled. In a 1986 test on human bone, Fulton et al. found that ratios of trace metal provided some useful information in sorting out commingling problems. The data were not precise enough to sort out individuals from large commingled mass graves, but offered useful data in resolving some specific commingling problems when used in conjunction with other techniques. In this experimental study, 21 elements were sampled from 54 sites on 30 human bones from 5 skeletons. The ratio of magnesium to zinc was the most useful in addressing commingling problems. More recent research by Finnegan (1988) and Finnegan and Chaudhuri (1990) suggests that trace elements and especially measurements of isotopic strontium show promise for commingling analysis. Although chemical techniques continue to show great potential, contamination remains a critical problem. Most forensic cases originate not from museum anatomical collections but from environments that are closer to archeological contexts. In such situations, the opportunity for environmental chemical invasion of hard tissue is significant. Considerable attention has focused on this problem in the context of chemical dietary analysis from archeological bone and teeth (Ambrose and Norr, 1993; Katzenberg, 1992; Schwarcz and Schoeninger, 1991; Sillen and Kavanagh, 1982). For example, Klepinger et al. (1986) conducted chemical elemental analysis of archeologically recovered human bone from Sicily and experienced difficulty separating dietary indicators from the effects of diagenesis. In recent years, the ability to relate commingled remains, especially those including soft tissue, has been greatly aided by molecular approaches. When resources are available to allow molecular analysis of recovered samples, difficult cases show high potential for resolution. The molecular literature is too large to be summarized here, but coupled with

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Figure 18.1 Bone concentration within ossuary II, Maryland. (From Ubelaker, D.H., Recon-

struction of Demographic Profiles from Ossuary Skeletal Samples: A Case Study from the Tidewater Potomac, Smithsonian Contributions to Anthropology 18, 1974, p. 23. With permission.)

more traditional techniques, these new approaches offer powerful new tools. A logical use of molecular analysis involves first proceeding with sorting and identification using the techniques discussed above. Molecular techniques potentially could be applied to remaining problems.

An Ossuary Example Ossuaries represent communal deposits of skeletal remains from multiple individuals who were initially deposited elsewhere after death. Ossuaries from archeological contexts are well known from eastern North America, especially the areas of the mid-Atlantic and the Great Lakes. Here, ethnohistorical and archeological evidence suggests that Indian groups living in those areas went to great lengths to gather up all of their dead for communal burial. Archeological discovery of these ossuaries has revealed the expected large deposits of many individuals. In the mid-Atlantic area, the ossuaries that have been carefully excavated have produced individuals in various stages of articulation. Since the ossuary burial procedure calls for the mutual inclusion of all individuals who had died since the last burial ceremony, some individuals would have been included who had died relatively recently and were completely articulated. Others died earlier and were in more advanced stages of decomposition, allowing parts of the body to detach during the removal process. A final group died long before and were completely skeletonized. During ossuary burial the bones from this final group would completely disarticulate. Obviously, excavation and analysis of such an assemblage involve major assessment of commingling.

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Table 18.1 Number of Individuals Represented by Each Type of Subadult Bone in Ossuary II Bone Humerus Radius Ulna Femur Tibia Fibula Clavicle Scapula Temporal Maxilla Mandible Gladiolus Manubrium Ilium Ischium Pubis Patella Rib Vertebraeb Sacrum Coccyx Calcaneus Talus Other tarsals Carpals Metatarsals/metacarpals Phalanges a b

Left

Midline or Side Unknown

71 47 58 89 67 35 47 59 81 49 52

Right 68 45 54 82 75 35 49 52 84 49 49

10 13 71 43 41 0

58 48 22 1 19 (494)a 29 (775)a 10 1 (4)a

18

25 10 (20)a 3 (28)a 1 (10)a 16 (295)a 6 (271)a

Numbers in parentheses indicate actual number of bones. Cervicals, thoracics, lumbars.

Source: From Ubelaker, D.H., Reconstruction of Demographic Profiles from Ossuary Skeletal Samples: A Case Study from the Tidewater Potomac, Smithsonian Contributions to Anthropology 18, 1974, p. 33. With permission.

In 1971 and 1972, T. Dale Stewart and I excavated such an ossuary (Figure 18.1) from a site in southern Maryland (Ubelaker, 1974). The site had been visited previously by Stewart, who supervised the excavation of a first ossuary there in 1953 and 1955. Although my involvement with the excavation dates back nearly 30 years, the experience offers an excellent example of the analysis of commingling. Because most of the bone assemblage was secondary and lacked the articulations needed to relate bones to individuals, we conducted a skeletal inventory of bone and side, separated for immature and mature, to assess the minimum number of individuals. To examine cultural evidence of spatial variability within the ossuary, bones within artificially designated squares were first tabulated. These data then were merged to assess the overall representation. The inventory of immature remains was reported separately from that of mature individuals.

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Table 18.2 Order of Representation of Subadults in Ossuary II as Indicated by Bone Types Represented

Absent

Bone

No.

%

No.

%

Femur Temporal Tibia Ilium Humerus Scapula Ulna Mandible Maxilla Ischium Clavicle Radius Pubis Fibula Vertebrae Calcaneus Ribs Metatarsals/metacarpals Manubrium Gladiolus Talus Phalanges Other tarsals Sacrum Carpals Patella

89 84 75 72 71 60 58 52 49 49 49 47 41 35 29 25 24 16 13 10 10 6 3 3 1 1

100 94 84 81 80 67 65 58 55 55 55 53 46 39 33 28 27 18 15 11 11 7 3 3 1 1

0 5 14 17 18 29 31 37 40 40 40 42 48 54 60 65 66 73 76 79 79 83 86 86 88 88

0 6 16 19 20 33 35 42 45 45 45 48 54 61 67 72 73 82 85 89 89 93 97 97 99 99

Source: From Ubelaker, D.H., Reconstruction of Demographic Profiles from Ossuary Skeletal Samples: A Case Study from the Tidewater Potomac, Smithsonian Contributions to Anthropology 18, 1974, p. 37. With permission.

Results of the immature remains inventory are provided in Table 18.1. The table reveals the variability of immature bone representation: 89 individuals were represented by left femora; at the other extreme, only 1 immature right patella was found. Table 18.2 presents these data arranged by bone type in order of maximum representation with an indication of the percentage of bones of this type that are not present as well. Similar results were found for adults (Table 18.3). When these data are also arranged in order of greatest representation (Table 18.4), maximum counts come from the tibia, followed closely by the femur and humerus. At the other extreme, 96% of the second through the fifth distal foot phalanges was missing. The order of the bones present on both the adult and immature lists generally approximates their size. Since the ossuary was carefully excavated using fine hand tools, with backdirt screened, etc., and maximum care was provided after excavation in processing and storage, it seems likely that the differential representation results from events prior to excavation. Some small fragile bones that had been deposited in the ossuary possibly were not detected during excavation and analysis due to poor preservation. Because preservation of most bones was generally excellent,

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especially for the mature remains, loss due to this factor was likely minimal. Most of the variability in bone representation appeared to represent selection on the part of the Indians. Through either careful intentional selection of the parts buried or unintentional carelessness, not all of the remains had been transferred from their primary repository to the ossuary. Thus, as with many commingled bone assemblages found in archeological and forensic contexts, the final bone grouping represents the culmination of many factors, including human behavior. In regard to the Maryland ossuary, the number of individuals represented by immature bones (at least 89 left femora) combined with the number of individuals represented by mature bones (at least 99 right mandibles) suggests the combined presence of at least 188 individuals. This represents the minimum number of individuals determined by the bone inventories. Of course, the actual number represented could be larger if some subadults were represented by bones other than the left femur and some adults by bones other than the right mandible. The minimum number represented perhaps could be determined more precisely by attempting to match pairs of bones, or arranging the immature bones by approximate age. Such additional analysis was complicated by the large size of the assemblage, but would be a recommended addition to smaller studies.

Portuguese Medieval Battle of Aljubarrota Cunha and Silva (1997) chose a similar approach to examine the minimum number of individuals represented in their skeletal sample from a famous Medieval Period Portuguese battle. Victims of the 1385 battle had been commingled and placed in a communal ossuary. Careful inventory revealed that at least 400 individuals were represented by the right femur.

The Crow Creek Massacre Site Selection of techniques to assess commingling and evaluate the individuals represented must be chosen on a case-by-case basis. Each problem and context should be assessed on its own merits. P. Willey reports (1990) an interesting example from the Great Plains of the United States. His excavation and analysis focused on a large prehistoric communal burial of American Indian origin. Archeological and skeletal findings suggested the individuals buried there were massacre victims who probably died at the hands of another hostile Indian group. Because of political complications stemming from contemporary American Indians (Ubelaker and Grant, 1989), the remains were available for analysis only for a relatively short period of time. Each “bag” of bones resulting from the excavation was analyzed separately. The contents of each were inventoried and then the numbers were totaled to obtain the maximum counts. This procedure recognized the possibility of some duplication of counts in the case of fragmented remains but also considered articulation data and observations on archeological context. The frequencies of the bones recovered suggest that 486 individuals were represented by right temporals, 477 by left temporals, 367 by left and right femora, 269 by right tibiae, and only 91 by left radii. Willey felt that scavenging activity of animals between death and burial as well as cultural selection of the parts to be buried likely produced most of the reported variability in the counts.

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The Search for Father Bachelot Smaller samples offer greater opportunities for refined analysis. Pietrusewsky and Willacker (1997) report their careful study of remains which were thought perhaps to represent an early Catholic missionary to the Hawaiian Islands. Father Bachelot was the leader of the first Catholic missionary group to the Hawaiian Islands between 1827 and 1837. In a search for the remains of this prominent figure in Hawaiian history, six sets of commingled remains were recovered. Father Bachelot was a male of French ancestry and 41 years of age at the time of his death. Analysis involved sorting the remains by skeletal element, size and age at death. This procedure established that at least 10 individuals were present; 8 of the individuals could be eliminated from consideration as being those of the missionary because of their age at death, sex, and the likely presence of a disease (yaws) from which it was believed Father Bachelot did not suffer. The remaining two individuals showed evidence of Pohnpean ancestry rather than the French ancestry of the missionary. In addition, some artifacts of native (not French) manufacture were present with the remains. The authors concluded that the remains represented local inhabitants of the island and not the missionary. Theoretically, some of the bones present could have originated from the man and just happened to appear consistent with the other more identifiable remains. From the analysis conducted however, the probability of such commingling is low.

Taphonomic Factors in Commingling Taphonomic factors are always present in commingled skeletal assemblages. The list of such factors is long and varied. It begins with the death of the individual and can extend to the time of analysis. Extensive discussion of the complex taphonomic factors that affect bone assemblages is available in the published literature (e.g., Binford, 1981,1984; Haglund and Sorg, 1997; Lyman, 1994). Human behavior plays a very important role in the process that leads to commingling in archeological assemblages (Binford, 1978) and especially in those of forensic contexts (Haglund and Sorg, 1997). Although exotic explanations of commingled samples are not unexpected in forensic remains, they are less likely in most archeological assemblages. Brain (1976), for example, examined bone accumulations associated with Hottentot villages along the Kuiseb River in the Central Namib Desert. Bone refuse of goats was highly variable, reflecting human activity, animal chewing, and other preservation factors. Brain suggested that the bone distribution at the African Australopithecine site of Makapansgat could be explained by similar factors. This interpretation contrasted with more exotic explanations offered by others. Many human activities can lead to incomplete skeletal representation and commingling. Burning of remains can lead to fragmentation and differential skeletal representation (Buikstra and Swegle, 1989; Heglar, 1984). Criminal behavior and/or mortuary practices can add complexity. Willey (1997) studied human remains recovered from the Custer National Cemetery. The mixed preservation seemed to favor “larger, more proximal bones” over smaller distal ones (Willey, 1997:i). Such a preservation pattern reflected previous exhumation practice, in addition to other factors.

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Table 18.3 Number of Individuals Represented by Each Type of Adult Bone in Ossuary II Bone Long Humerus Radius Ulna Femur Tibia Fibula Clavicle Irregular Scapula Temporal Maxilla Mandible Gladiolus Manubrium Innominate Patella Rib Cervicals 1 2 3–7 Thoracics 1–9 10 11 12 10 or 11 11 or 12 10 or 11 Lumbars 1–5 Sacrum Coccyx Hand Navicular Lunate Triquetral Pisiform G. multangular L. multangular Capitate Hamate MC1 MC2 MC3 MC4 MC5 Hand phalanges Proximal 1 Proximal 2–5

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Left

? or Midline

Right

87 80 88 82 81 74 70

84 80 86 85 93 81 72

85 92 86 98

92 91 81 99 56 58

84 73

86 78 72 (1727)a 98 97 76 (389) 72 (645)a 63 80 59 37 1 11 77 (385)a 84 9 (33)a

59 54 41

63 46 24 18 (35)a

45 37 69 51 66 74 74 56 69

55 38 58 55 68 65 77 54 74 53 (106)a 66 (524)a

Table 18.3 Number of Individuals Represented by Each Type of Adult Bone in Ossuary II (cont.) Bone Middle Distal 1 Distal 2–5 Foot Calcaneus Talus Cuboid Navicular Cuneiform 1 Cuneiform 2 Cuneiform 3 MT1 MT2 MT3 MT4 MT5 Foot phalanages Proximal 1 Proximal 2–5 Middle Distal 1 Distal 2–5 a

Left

? or Midline

Right

44 (348)a 29 (57)a 23 (181)a 86 93 70 69 78 73 73 82 72 77 77 81

86 90 73 80 73 68 75 74 63 85 74 73 60 (125)a 46 (385)a 19 (118)a 45 (89)a 9 (55)a

Numbers in parentheses indicate actual number of bones.

Source: From Ubelaker, D.H., Reconstruction of Demographic Profiles from Ossuary Skeletal Samples: A Case Study from the Tidewater Potomac, Smithsonian Contributions to Anthropology 18, 1974, p. 34. With permission.

In their analysis of archeologically recovered burials at the Larson Site in South Dakota, Bass and Rucker (1976) discovered many graves with multiple individuals of varying completeness. They felt this pattern reflected the Arikara’s attempt to resolve the very practical problem of how to bury their dead during the winter. During the freezing winter months, the best site for burial was that of a previous burial in which the soil was less compact. Articulation patterns and pit outlines noted during excavation provided the keys to this interpretation. Animal Chewing Animal chewing is common on remains that are accessible. Animal activity can lead to destruction of remains, dispersal, and even commingling. Much has been learned about the effects of different animals on bone (Haglund and Sorg, 1997; Ubelaker, 1989). Animal activity can affect bone counts and estimates of the minimal number of individuals in bone assemblages. Marean and Spencer (1991) report an experiment with spotted hyenas suggesting that hyena activity is focused on the ends of the long bones. Thus, maximum bone counts would come from the diaphyseal midshaft rather than the proximal or distal ends. Hudson (1993) published a controlled study of faunal remains associated with the Aka of the Central African Republic. In this community, domestic dogs played a major role in dispersal of faunal remains. Hudson found that the smaller the animal, the greater the

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Table 18.4 Order of Representation of Adults in Ossuary II as Indicated by Bone Types Represented Bones

No.

Mandible 1st cervical 2nd cervical Tibia Talus Scapula Temporal Ulna Humerus Innominate Maxilla Calcaneus 3rd metatarsal Femur 10/11/12 thoracics Sacrum 1st metatarsal 5th metatarsal Fibula Radius Foot navicular Patella 1st cuneiform 4th metatarsal 3rd metatarsal Lumbars 3–7 cervicals 3rd cuneiform 5th metacarpal 2nd metacarpal Cuboid 2nd cuneiform 2nd metatarsal 1–9 thoracics Clavicle Rib Capitate 1st metacarpal Prox. 2–5 hand phalanges Hand navicular 1st prox. foot phalanx Manubrium Gladiolus 4th metacarpal Greater multangular Hamate Lunate 1st prox. hand phalanx 2–5 distal foot phalanges 1st distal foot phalanx

99 98 97 93 93 92 92 88 87 86 86 86 85 85 84 84 82 81 81 80 80 78 78 77 77 77 76 75 74 74 73 73 72 72 72 72 69 68 66 63 60 58 56 56 55 55 54 53 46 45

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% 100 99 98 94 94 93 93 89 88 87 87 87 86 86 85 85 83 82 82 81 81 79 79 78 78 78 77 76 75 75 74 74 73 73 73 73 70 69 67 64 61 59 57 57 56 56 55 54 46 45

Absent No.

%

0 1 2 6 6 7 7 11 12 13 13 13 14 14 15 15 17 18 18 19 19 21 21 22 22 22 23 24 25 25 26 26 27 27 27 27 30 31 33 36 39 41 43 43 44 44 45 46 53 54

0 1 2 6 6 7 7 11 12 13 13 13 14 14 15 15 17 18 18 19 19 21 21 22 22 22 23 24 25 25 26 26 27 27 27 27 30 31 33 36 39 41 43 43 44 44 45 46 54 55

Table 18.4 Order of Representation of Adults in Ossuary II as Indicated by Bone Types (cont.) Represented

Absent

Bones

No.

%

No.

%

Middle hand phalanges Triquetral Lesser multangular 1st distal hand phalanx 2–5 distal hand phalanges Middle foot phalanges Pisiform Coccygeal vertebrae 2–5 distal foot phalanges

44 41 38 29 23 19 18 9 9

44 41 38 29 23 19 18 9 9

55 58 61 70 76 80 81 90 90

56 59 62 71 77 81 82 91 91

Source: From Ubelaker, D.H., Reconstruction of Demographic Profiles from Ossuary Skeletal Samples: A Case Study from the Tidewater Potomac, Smithsonian Contributions to Anthropology 18, 1974, p. 36. With permission.

probability of loss. Resulting bone counts accurately measured the presence of larger species but poorly accounted for smaller ones. Bone Density As noted by Lyman (1993), bone density can be an important factor in the survival of skeletal parts although animal chewing is not always correlated with density. Galloway et al. (1997) used a single photon absorptiometer to measure bone density in a modern forensic sample. Like others, they noted that density is a factor in postmortem preservation, but they also found that variation due to sex, handedness, and age may be influencing factors. The same group (Willey et al., 1997) found that bone density correlated with bone survival in the Crow Creek assemblage discussed earlier. Age at death is closely linked with bone density in postmortem preservation issues. Guy et al. (1997) found that the low mineralization associated with infant bone contributes to poor preservation. Similar factors suggested to Walker et al. (1988) that age factors, especially the very young and very old, contribute to differential preservation. Again, low bone density in these age groups appears to be the key factor. Preservation also relates to the many variables that are properties of the environment (Haglund and Sorg, 1997; Ubelaker, 1989). Gordon and Buikstra (1981) have demonstrated how soil acidity can affect bone preservation. Excavation Factors Excavation techniques can further alter the preservation of remains and lead to commingling. Bones that have been weakened by human or environmental factors are especially vulnerable to fragmentation during recovery. A hasty or incomplete excavation can alter the bone assemblage. Casteel (1972) demonstrated how a recovery technique such as mesh size used in screening can influence faunal samples. Similarly, Payne (1975) water-screened the backdirt of an excavation and found many smaller bones and bones of smaller species. Thus, recovery technique can influence the representation of species in faunal studies and of individual bones and ages in human studies.

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Curation Practices The final limitation placed on skeletal samples relates to storage and processing protocols operating on samples prior to analysis. The analyst may not be aware of what practices others have employed regarding the samples studied. This is especially a problem with older museum collections and forensic cases in which the forensic anthropologist may follow a long line of previous examiners. Stewart (1937) describes an archeological project that sent 80 barrels of fragmentary human remains to the Smithsonian for curation. Stewart relates how lack of storage space forced curators to decide what aspects of the remains should be saved for analysis. Thus, storage facilities and curation policy can affect the final assemblage available for study. Number of Individuals Represented by Bone Counts As noted above, skeletal biologists and forensic anthropologists have utilized detailed bone inventories, coupled with observations on articulation, age at death, sex, joint congruence, and a variety of other factors to determine the minimum number of individuals represented by the assemblage. The related question of how many actual individuals are represented by the minimum number is rarely addressed. The mathematical approach advocated by Snow and associates (1970, 1984) reveals some information in this regard, but most anthropologists have been content to not estimate numbers beyond the minimum indicated, likely in recognition of the unknown variables involved. Paleontologists and archaeozoologists working with faunal assemblages have struggled with the larger question of total individual representation for some time. Issues include anatomical defects as potential sources of error in individual counts (Steele and Parama, 1981), statistical procedures for sampling (Chapman, 1951), and general issues of the relationship between individual counts and the total number of individuals present (Allen and Guy, 1984; Casteel, 1977; Chase and Hagaman, 1987; Fieller and Turner, 1982; Gilbert et al., 1981; Gilbert and Singer, 1982; Grayson, 1973, 1978, 1981, 1984; Klein and CruzUribe, 1984; Krantz, 1968; Lyman, 1987; Plug, 1984; Plug and Plug, 1990; Ringrose, 1993; Shotwell, 1995; Wild and Nichol, 1983; Winder, 1991). Specific techniques advocated include A computer procedure to assist matching bones by size (Nichol and Creak, 1979) Techniques modified from the mark-capture procedure in which a sample of a biological living population is captured, marked, and released, followed by the capturing of a new sample and observing the percentage that are marked (LeCren, 1965) A sorting procedure that considers bone counts along with the size and age of the animal (Bökönyi, 1970) The Lincoln Index based on matching pairs of bones (Winder, 1992) As noted by Badgely (1986), Holtzman (1979), and Horton (1984), the selection of which methods to use depends upon the nature of the assemblage, problem orientation, and other factors. All of the methods make assumptions but offer a variety of approaches to estimating the size of the total population. Although the issues discussed above have produced a voluminous and somewhat tedious discussion among archaeozoologists and paleontologists, physical anthropologists generally have remained on the sidelines. A notable exception is the work of Adams (1996)

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who reviewed this literature and used one of the techniques, the Lincoln/Peterson Index, to assess the number of individuals represented in an archeologically recovered assemblage of human bone from South Dakota. The Lincoln/Peterson Index involves estimating the total population size by multiplying the number of bones of one side by the number of bones of the opposite side and dividing the product by the number of matched pairs of that bone. Adams applied this technique to the Larson village sample from the area of Mobridge, South Dakota, a sample that had previously been studied by others (Owsley and Bass, 1979; Owsley et al., 1977). In particular, the Owsley et al. (1977) work had obtained the minimum number of individuals by a straightforward count of right and left major bones. Adams’ reanalysis of the material generally agreed with the Owsley et al. (1977) minimum number of individuals from the bone counts. His application of the Lincoln/Peterson Index then produced a slightly larger figure.

Summary Although forensic anthropologists only occasionally deal with issues of skeletal commingling in their work, such cases can be challenging. As anthropologists become increasingly involved in mass disasters and other events leading to fragmentation and mixing of individuals, this work likely will grow. Recent years have witnessed a gradual increase in the scientific tools available to study commingled cases. Although these developments are helpful, experience with skeletal morphology remains the principal requirement for skilled analysis.

References Adams, B.J. 1996 The use of the Lincoln/Peterson Index for quantification and interpretation of commingled human remains. Unpublished Master’s Thesis, Department of Anthropology, University of Tennessee, Knoxville. Allen, J. and J.B.M. Guy 1984 Optimal estimations of individuals in archaeological faunal assemblages: How minimal is the MNI?, Archaeology in Oceania 19:41–47. Ambrose, S.H. and L. Norr 1993 Experimental evidence for the relationship of the carbon isotope ratios of whole diet and dietary protein to those of bone collagen and carbonate. In Prehistoric Human Bone: Archeology at the Molecular Level, edited by J.B. Lamber and G. Grupe, pp. 1–38. Springer-Verlag, Berlin. Baker, P.T. and R.W. Newman 1957 The use of bone weights for human identification, American Journal of Physical Anthropology 15:601–618. Bass, W.M. and M.D. Rucker 1976 Preliminary investigation of artifact association in an Arikara cemetery (Larson Site), Walworth County, South Dakota, National Geographic Research Reports, 1968 Projects, pp. 33–48. Binford, L.R. 1978 Nunamiut Ethnoarchaeology, Academic Press, New York. 1981 Bones: Ancient Men and Modern Myths, Academic Press, New York. 1984 Faunal Remains from Klaises River Mouth, Academic Press, New York.

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Bladgley, C. 1986 Counting individuals in mammalian fossil assemblages from fluvial environments, Palaios 1:328–338. Bökönyi, S. 1970 A new method for the determination of the number of individuals in animal bone material, American Journal of Archaeology 74:291–292. Brain, C.K. 1976 Some principles in the interpretation of bone accumulations associated with man. In Human Origins: Louis Leakey and the East African Evidence, edited by G.L. Isaac and E.R. McGown, pp. 97–106. W.A. Benjamin, Menlo Park. Buikstra, J.E. and C.C. Gordon 1980 Individuation in forensic science study: decapitation, Journal of Forensic Sciences 25:246–259. Buikstra, J.E. and M. Swegle 1989 Bone modification due to burning: experimental evidence. In Bone Modification, edited by R. Bonnichsen and M. Sorg, pp. 247–258. Maine Center for the Study of the First Americans, Orono. Buikstra, J.E. and D.H. Ubelaker, Eds. 1994 Standards for Data Collection from Human Skeletal Remains, Proceedings of a Seminar at the Field Museum of Natural History. Arkansas Archaeological Survey Research Series No. 44, Arkansas Archaeological Survey, Fayetteville. Buikstra, J.E., C.C. Gordon, and L. St. Hoyme 1984 The case of the severed skull: Individuation in forensic anthropology. In Human Identification: Case Studies in Forensic Anthropology, edited by T.A. Rathbun and J.E. Buikstra, pp. 121–135. Charles C Thomas, Springfield, IL. Casteel, R.W. 1972 Some biases in the recovery of archaeological faunal remains, Proceedings of the Prehistoric Society 38:382–388. 1977 Characterization of faunal assemblages and the minimum number of individuals determined from paired elements: continuing problems in archaeology, Journal of Archaeological Science 4:125–134. Chapman, D.G. 1951 Some properties of the hypergeometric distribution with applications to zoological sample census, University of California Publications in Statistics 1:131–159. Chase, P.G. and R.M. Hagaman 1987 Minimum number of individuals and its alternatives: a probability theory perspective, OSSA 13:75–86. Cunha, E. and A.M. Silva 1997 War lesions from the famous Portuguese Medieval Battle of Aljubarrota, International Journal of Osteoarcheology 7:595–599. Eyman, C.E. 1965 Ultraviolet fluorescence as a means of skeletal identification, American Antiquity 31:109–112. Fieller, N.R.J. and A. Turner 1982 Number estimation in vertebrate samples, Journal of Archaeological Science 9:49–62. Finnegan, M. 1988 Variation of trace elements within and between skeletons using multiple sample sites. Paper presented at the 15th Annual Meeting of the Paleopathology Association, Kansas City, MO.

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Finnegan, M. and S. Chaudhuri 1990 Identification of commingled skeletal remains using isotopic strontium. Paper presented at the 42nd Annual Meeting of the American Academy of Forensic Sciences, Cincinnati. Fulton, B.A., C.E. Meloan, and M. Finnegan 1986 Reassembling scattered and mixed human bones by trace element ratios. Journal of Forensic Sciences, 31(4):1455–1462. Galloway, A., P. Willey, and L. Snyder 1997 Human bone mineral densities and survival of bone elements: a contemporary sample. In Forensic Taphonomy, edited by W.D. Haglund and M.H. Sorg, pp. 295-317. CRC Press, Boca Raton, FL. Gilbert, A.S. and B.H. Singer 1982 Reassessing zooarchaeological quantification, World Archaeology 14:21–40. Gilbert, A.S., B.H. Singer, and D. Perkins, Jr. 1981 Quantification experiments on computer-simulated faunal collections, OSSA 8:79–94. Gordon, C.G. and J.E. Buikstra 1981 Soil pH, bone preservation, and sampling bias at mortuary sites, American Antiquity 46:566–571. Grayson, D.K. 1973 On the methodology of faunal analysis, American Antiquity 38:432–439. 1978 Minimum numbers and sample size in vertebrate faunal analysis, American Antiquity 43:53–65. 1981 A critical view of the use of archaeological vertebrates in paleoenvironmental reconstruction, Journal of Ethnobiology 1:28–38. 1984 Quantatative Zooarchaeology, Academic Press, New York. Guinn, V.P. 1970 Forensic neutron activation analysis. In Personal Identification in Mass Disasters, edited by T.D. Stewart, pp. 25-35. Smithsonian Institution, Washington, D.C. Guy, H., C. Masset, and C.-A. Baud 1997 Infant taphonomy, International Journal of Osteoarcheology 7:221–229. Haglund, W.D. and M.H. Sorg, Editors 1997 Forensic Taphonomy: The Postmortem Fate of Human Remains, CRC Press, Boca Raton, FL. Heglar, R. 1984 Burned remains. In Human Identification: Case Studies in Forensic Anthropology, edited by T. Rathbun and J.E. Buikstra, pp. 148–158. Charles C Thomas, Springfield, IL. Holtzman, R.C. 1979 Maximum likelihood estimation of fossil assemblage composition, Paleobiology 5:77–89. Horton, D.R. 1984 Minimum numbers: a consideration, Journal of Archaeological Science 11:255–271. Hudson, J. 1993 The impacts of domestic dogs on bone in forager camps. In From Bones to Behavior: Ethnoarchaeological and Experimental Contributions to the Interpretations of Faunal Remains, edited by J. Hudson, pp. 301–323. Center for Archaeological Investigations, Carbondale. Katzenberg, M.A. 1992 Advances in stable isotope analysis of prehistoric bones. In The Skeletal Biology of Past Peoples: Research Methods, edited by S.R. Saunders and M.A. Katzenberg, pp. 105-120. WileyLiss, New York.

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Kerley, E.R. 1972 Special observations in skeletal identification, Journal of Forensic Sciences 17:349–357. Klein, R.G. and K. Cruz-Uribe 1984 The Analysis of Animal Bones from Archeological Sites, University of Chicago Press, Chicago, IL. Klepinger, L.L., J.K. Kuhn, and W.S. Williams 1986 An elemental analysis of archaeological bone from Sicily as a test of predictability of diagenetic change, American Journal of Physical Anthropology 70:325–331. Krantz, G.S. 1968 A new method of counting mammal bones, American Journal of Archaeology 72:286–288. Krogman, W.M. 1962 The Human Skeleton in Forensic Medicine, Charles C Thomas, Springfield, IL. Krogman, W.M. and M.Y. Iscan 1986 The Human Skeleton in Forensic Medicine, 2nd ed., Charles C. Thomas, Springfield, IL. LeCren, E.D. 1965 A note on the history of mark-recapture population estimates, Journal of Animal Ecology 34:453–454. London, M.R. and B.K. Curran 1986 The use of the hip joint in the separation of commingled remains (abstract), American Journal of Physical Anthropology 69:231. London, M.R. and D.R. Hunt 1998 Morphometric segregation of commingled remains using the femoral head and acetabulum (abstract), American Journal of Physical Anthropology 26 (suppl.):152. Lyman, R.L. 1987 Zooarchaeology and taphonomy: a general consideration. Journal of Ethnobiology 7:93–117. 1993 Density-mediated attrition of bone assemblages: new insights. In From Bones to Behavior, edited by J. Hudson, pp. 324–341. Center for Archaeological Investigations, Carbondale. 1994 Vertebrate Taphonomy, Cambridge University Press, Cambridge. Marean, C.W. and L.M. Spencer 1991 Impact of carnivore ravaging on zooarchaeological measures of element abundance, American Antiquity 56:645–658. McKern, T.W. 1958 The Use of Shortwave Ultraviolet Rays for the Segregation of Commingled Skeletal Remains. Environmental Protection Research and Developments Command, Quartermaster Research and Development Center Environmental Protection Research Division, Natick, MA. Murray, K.A. and J.C. Rose 1993 The analysis of cremains: a case study involving the inappropriate disposal of mortuary remains, Journal of Forensic Sciences 38:98–103. Nichol, R.K. and G.A. Creak 1979 Matched paired elements among archaeological bone remains: a computer procedure and some practical limitations, Newsletter of Computer Archaeology 14:6–16. Owsley, D.W. and W.M. Bass 1979 A demographic analysis of skeletons from the Larson site (39WW2) Walworth County, South Dakota: vital statistics, American Journal of Physical Anthropology 51:145–154.

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Owsley, D.W., H.E. Berryman, and W.M. Bass 1977 Demographic and osteological evidence for warfare at the Larson site, South Dakota, Plains Anthropologist Memoir 13:119–131. Payne, S. 1975 Partial recovery and sample bias. In Archaeozoological Studies, edited by A.T. Clason, pp. 7–17. American Elsevier, New York. Pietrusewsky, M. and L.M. Willacker 1997 The search for Father Bachelot: first Catholic missionary to the Hawaiian Islands (1827–1837), Journal of Forensic Sciences 42:208–212. Plug, I. 1984 MNI counts, pits and features, Frontiers: Southern African Archaeology Today, edited by M. Hall et al., British Archaeological Reports International Series, Oxford, 207:357–362. Plug, C. and I. Plug 1990 MNI counts as estimates of species abundance, South African Archaeological Bulletin 45:53–57. Ringrose, T.J. 1993 Bone counts and statistics: a critique. Journal of Archaeological Science 20:121–157. Rösing, F.W. and E. Pischtschan 1995 Re-individualisation of commingled skeletal remains, Advances in Forensic Sciences, edited by B. Jacob and W. Bonte, Verlag, Berlin, 7:38–41. Schwarcz, H.P. and M.J. Schoeninger 1991 Stable isotope analysis in human nutritional ecology, Yearbook of Physical Anthropology 34:283–322. Shotwell, J.A. 1995 An approach to the palaeoecology of mammals, Ecology 36:327–337. Sillen, A. and M. Kavanagh 1982 Strontium and paleodietary research: a review, Yearbook of Physical Anthropology 25:67–90. Snow C.C. and E.D. Folk 1965 Statistical assessment of commingled skeletal remains, American Journal of Physical Anthropology 32:423–427. Snow, C.C. and J.L. Luke 1970 The Oklahoma City child disappearances of 1967: forensic anthropology in the identification of skeletal remains, Journal of Forensic Sciences 15:125–153. Snow, C.C. and J.L. Luke 1984 The Oklahoma City child disappearances of 1967: forensic anthropology in the identification of skeletal remains. In Human Identification: Case Studies in Forensic Anthropology, edited by T.A. Rathbun and J.E. Buikstra, pp. 253-277. Charles C Thomas, Springfield, IL. Steele, D.G. and W.D. Parama 1981 Frequencies of dental anomalies and their potential effect on determining MNI counts, Plains Anthropologist 26(91):51–54. Stewart, T.D. 1937 The problem of the fragmentary human skeleton [abstract], American Journal of Physical Anthropology XXII(3, suppl. 1):7–8. Stewart, T.D. 1979 Essentials of Forensic Anthropology, Charles C Thomas, Springfield, IL.

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Ubelaker, D.H. 1974 Reconstruction of Demographic Profiles from Ossuary Skeletal Samples: A Case Study from the Tidewater Potomac, Smithsonian Contributions to Anthropology 18. 1989 Human Skeletal Remains: Excavation, Analysis, Interpretation, 2nd ed., Taraxacum, Washington. Ubelaker, D.H. and L.G. Grant 1989 Human skeletal remains: preservation or reburial?, Yearbook of Physical Anthropology 32:249–287. Walker, P.L., J.R. Johnson, and P.M. Lambert 1988 Age and sex biases in the preservation of human skeletal remains, American Journal of Physical Anthropology 76:183–188. Wild, L. and R. Nichol 1983 Estimation of the original number of individuals using estimators of the Krantz type, Journal of Field Archeology 10:337–344. Willey, P. 1990 Prehistoric Warfare on the Great Plains: Skeletal Analysis of the Crow Creek Massacre Victims, Garland, New York. 1997 Osteological Analysis of Human Skeletons Excavated from the Custer National Cemetery. Midwest Archeological Center Technical Report No. 50, National Park Service, Lincoln, NE. Willey, P., A. Galloway, and L. Snyder 1997 Bone mineral density and survival of elements and element portions in the bones of the Crow Creek Massacre victims, American Journal of Physical Anthropology 104:513–528. Winder, N.P. 1991 How many bones make five? The art and science of guesstimation in archaeozoology, International Journal of Osteoarcheology 1:111–126. 1992 The removal estimator: a ‘probable numbers’ statistic that requires no matching, International Journal of Osteoarcheology 2:15–18.

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Section 4

Modification of Bones, Soft Tissue, and Associated Materials

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Detecting the Postburial Fragmentation of Carpals, Tarsals, and Phalanges

19

CHRISTYANN M. DARWENT R. LEE LYMAN Contents Introduction Background Expanding the Method Mechanical and Nutritional Properties of Skeletal Elements Quantification Methods, Materials, and Caveats Results Skeletal Element Frequencies Sphericity Fragmentation Grease and Marrow Utility What Mediates Fragmentation? Discussion and Conclusions Acknowledgments References

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Introduction During the past 30 years paleontologists and zooarchaeologists have displayed a serious interest in taphonomy, a term originally coined and defined by Russian paleontologist I.A. Efremov (1940) as the study of the transition of organic remains from the biosphere into the lithosphere. Weigelt (1927; English translation, 1989) had previously proposed the term biostratinomy and defined it as the effects on organic remains that take place between the time of an organism’s death and the burial of its remains. Muller (1963) later proposed the term diagenesis to denote the effects on organic remains that take place between the time of their burial and their recovery by a paleontologist or zooarchaeologist. Taphonomy, therefore, concerns both the biostratinomic and diagenetic phases of what Efremov referred to as the science of the laws of embedding or burial. The burst of interest in taphonomy during the past 30 years has resulted in a marked increase in the number of published articles on the formation of the geological record of past life, particularly zoological life (Donovan, 1991; Lyman, 1994c). In zooarchaeology, the literature has focused most closely on deciphering taphonomic traces that signify aspects of biostratinomy for two reasons. First, this phase of taphonomic history is the one during which hominid taphonomic agents have their most direct input to the accumulation, modification, and deposition of faunal remains and, thus, is the one of most concern to zooarchaeologists interested in past human behavior (e.g., Hudson, 1993). Second, the processes comprising the biostratinomic phase are much more readily studied in an actualistic context than the processes operating during the diagenetic phase.* Literature concerning the digenetic phase of taphonomy has tended to be written largely by paleontologists who focus on fossilization processes, or those that maintain or alter the chemical composition of organic remains (e.g., Donovan, 1991). The few contributions by zooarchaeologist examining diagenetic processes center on recognizing what is often mislabeled as “postdepositional” fragmentation (e.g., Klein, 1989; Klein and CruzUribe, 1984:69–75; Marean, 1991; Villa and Mahieu, 1991). We say mislabeled because although deposition can be coincident with burial, actualistic research indicates that deposition can also, and often does, precede burial by various, sometimes taphonomically significant, lengths of time (e.g., Behrensmeyer, 1978). Marean (1991:677) defined “postdepositional processes … as including chemical and mechanical action on bones and teeth after the bones and teeth have entered the sediment and are no longer sources of food for mammals.” Although we agree with this definition, we prefer the term postburial because it avoids potential confusion that may result from use of the term postdepositional, particularly when it is not defined.** Researchers have attempted to discern the degree of fragmentation of faunal remains that is attributable to the weight of overburden and sedimentary compaction. It is suggested by some that the influence of these factors is greater on bones that have undergone chemical leaching and, therefore, are structurally weakened. Study of the degree of postburial fragmentation is important for several reasons. Most fundamentally, fragmentation influences identifiability and, hence, measures of abundance. An assemblage of broken bones and teeth * Actualistic research comprises observation, in this case, of taphonomic processes, documentation of the effects of these processes, and use of the latter to infer that similar processes produced similar effects in the past. ** In the present context, burial need not be a result of intentional human behavior. It can simply be the result of natural geological processes involving deposition of sediment.

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will produce higher NISP (number of identified specimens) counts than a taxonomically and skeletally identical assemblage of unbroken bones and teeth. Further, as individual skeletal elements become progressively more broken, the NISP value progressively decreases (Lyman, 1994b; Marshall and Pilgrim, 1993). This decrease occurs because smaller fragments are less likely to retain anatomically and taxonomically diagnostic landmarks. In this chapter we examine and expand one proposed method for recognition of diagenetic or postburial fragmentation so that it might be distinguished from biostratinomic fragmentation. Much of what we discuss owes its presence in the taphonomist’s analytical tool kit to the seminal work of others, and our contribution to the study of digenetic processes builds upon this research. We view our efforts here as another small step toward developing taphonomic methods that will allow paleontologists and zooarchaeologists (and perhaps forensic scientists) to decipher taphonomic histories of assemblages of bones and teeth, particularly the little-explored diagenetic phase of those histories.

Background Several years ago zooarchaeologist Curtis Marean (1991:692) hypothesized that “a bone’s resistance to postdepositional destruction is determined by its density, size and shape mediated by the postdepositional process involved (chemical or mechanical).” Marean did not evaluate this hypothesis, but instead described a method that he believed would allow analytical recognition of postburial fragmentation of bones. He discussed three prerequisites to his method: two concerned the skeletal elements used in the analysis and the other concerned quantification of bone specimens.* Skeletal remains to be used should, Marean reasoned, be those (a) that are seldom if ever broken by hominids or carnivores and (b) whose relative frequencies are not influenced by bone accumulation processes. Last, the unit of quantification should not be subject to inter-observer variation. The first and second requirements were met by using carpals and tarsals,** skeletal elements that Marean (1991) argued were seldom broken by hominids and carnivores and that all underwent similar transportation histories in actualistic contexts. He, therefore, reasoned that the relative frequencies of these skeletal elements would not be influenced by these processes, but perhaps would be by postburial processes. Marean met his third requirement by using a “completeness index” to characterize the degree of fragmentation. The completeness index “is derived by estimating for each specimen the fraction of the original compact bone that is present, summing the values, and dividing that by the total number of specimens ascribed to that bone and taxon” (Marean, 1991:685). For example, if three specimens of the astragalus are present, and one is complete (1.0), one comprises half of an astragalus (0.5), and one comprises a quarter of an astragalus (0.25), then one solves the equation [(1.0 + 0.5 + 0.25)/3] ¥ 100 = 58.3 to derive a percent completeness index (CI%) for the astragalus. The CI% value is properly read as the average completeness of the specimens for the skeletal element under consideration, such that in the preceding equation the value denotes that these three astragali are, on average, 58.3% complete skeletal elements. * A skeletal element is defined as “a single complete bone or tooth, a discrete, complete anatomical organ” (Lyman, 1994b:290). A specimen is “a discrete bone or tooth, or fragment thereof” (Lyman, 1994b:290). ** For purposes of brevity, we include the distal fibula, also known as the lateral malleolus, in the (artiodactyl) tarsal category.

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Marean (1991) noted that under experimental conditions hyenas often ingested articulated carpals and articulated tarsals: carpals seldom, if ever, displayed gnawing damage whereas among the tarsals only the calcaneum displayed such damage, and it did so only about half of the time. Both carpals and tarsals displayed corrosion subsequent to their ingestion and passage through the digestive tract. Marean reasoned that specimens displaying digestive corrosion should be omitted from calculation of the CI%. Similarly, he argued that specimens that had been burned should also be omitted because they are more brittle than unburned specimens (Stiner et al., 1995), and specimens that were heavily weathered (Behrensmeyer, 1978) should be omitted because of the possibility that cracks produced by subaerial weathering would result in greater fragmentation than unweathered specimens subsequent to burial. Finally, he indicated that carpals and tarsals displaying percussion damage should be omitted from specimens used to derive the CI% value because that value is meant to measure postburial fragmentation. The unnoted assumption underpinning the last is that percussion damage will result only from the impact of humanwielded hammerstones, an assumption we find untenable if the bones were recovered from a cave whose roof produces rock spalls that fall to the cave floor. When comparing the assemblages of artiodactyl carpals and tarsals from two African cave sites, Marean (1991:687) concluded that one assemblage had undergone much more “postdepositional destruction” than the other largely because the CI% was consistently lower across different carpals and tarsals in one collection than in the other. He also noted that (a) larger skeletal elements such as the astragalus and naviculo-cubiod displayed the greatest differences in CI% between the two assemblages and thus would likely provide the most reliable indication of postburial fragmentation, and (b) taxonomic differences in body size indicated that (larger) skeletal elements of larger taxa had lower CI% values than homologous elements in smaller-bodied taxa. Both of these observations suggest that larger bones tend to be more prone to fragmentation, before or after burial, than smaller bones.

Expanding the Method Marean (1991) suggested that collections with low CI% values indicate greater postburial fragmentation than those with high CI% values. Such an interpretation rests on a limited number of experiments and theoretical reasoning that suggest carpals and tarsals meet the criteria Marean specified for detecting postburial destruction. Actualistic research cited by Marean (1991), however, indicates that hominids do sometimes fracture carpals and the smaller tarsals. How, then, is fragmentation resulting from biostratinomic processes to be disentangled from fragmentation resulting from diagenetic processes? The theoretical reasons for analysis of carpals and tarsals relate to their mechanical properties as sedimentary particles and their value as food sources for predators relative to other skeletal elements. The former relates to Marean’s hypothesis that postburial fragmentation is mediated by density, size, and shape. The food value, as we indicate below, is also influenced by their size and shape. Consideration of each of these factors suggests ways to evaluate and expand Marean’s method for recognizing postburial fragmentation. Mechanical and Nutritional Properties of Skeletal Elements Carpals and tarsals are, by and large, compact skeletal elements. They tend to be structurally dense (Table 19.1), and they also tend to be spherical in shape (Figure 19.1). The notable

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Table 19.1 Structural Density, Volume (ml), Marrow Utility, and Grease Utility Values of Artiodactyl Carpals, Tarsals, and Phalanges

Skeletal Element Carpals Cuneiform (ulnar carpal) Lunar (intermediate carpal) Pisiform (accessory carpal) Scaphoid (radial carpal) Trapezoid magnum (carpal 2 +3) Unciform (fourth carpal) Tarsals Calcaneum Astragalus Naviculo-cuboid Tarsal 2 + 3 (external cuneiform) Distal fibula (lateral malleolus) Phalanges First phalanx Second phalanx Third phalanx a

b c

d e f

Structural Densitya

Volume

Marrow Utility Indexb

Grease Utility Indexb (36.47)c 5.03e 7.55e 2.51e 8.80e 7.55e 5.03e (29.87)c 46.96 32.47 21.56e 5.19e 3.12e 33.27 24.77 13.59

0.72 0.83 —f 0.98 0.74 0.78

2 3 1 3.5 3 2

0.64 0.61 0.62 —f 0.52

18 12 8.3 2 1.2

(1.0) 1.0d 1.0d 1.0d 1.0d 1.0d 1.0d (1.0)c 21.19 1.0 1.0d 1.0d 1.0d

0.57 0.35 0.25

6 4.3 3.7

30.00 22.15 1.0

Values are for deer (Odocoileus sp.) and are the greatest recorded of several taken for calcaneum, naviculocuboid, astragalus, first phalanx, and second phalanx. (From Lyman, R.L., Vertebrate Taphonomy, Cambridge University Press, Cambridge, U.K., 1994c, pp. 246–247.) From Binford, L.R., Nunamuit Ethnoarchaeology, Academic Press, New York, 1978, pp. 27, 33. Values in parentheses for all carpals as a single unit and, we assume, for the naviculo-cuboid, tarsal 2 + 3, and distal fibula as a single unit. (From Binford, L.R., Nunamuit Ethnoarchaeology, Academic Press, New York, 1978, pp. 27, 33.) Values assigned by Darwent and Lyman (see text for discussion). Values derived and assigned by Darwent and Lyman (see text for discussion). No data available.

exception to the latter is the calcaneum, a skeletal element that has a more rod-like shape. Artiodactyl carpals and tarsals all tend to have rather low nutritional values; they contain minimal amounts of grease and virtually no marrow, as indicated by Binford’s (1978) grease and marrow utility indices (Table 19.1). The theoretically significant points here are two. First, the relatively high structural density (g/cc) of these elements means that they require a great deal of force to break (Currey, 1984). In combination with the fact that carpals and tarsals have minimal interstitial space containing grease and marrow, this suggests that these elements would seldom be broken by hominids in order to extract potential sources of nutrition because the cost — particularly using primitive technologies — may well outweigh the return. For example, Marean’s (1991: 691) experiments prompted him to suggest “an extraordinary effort is required to break fresh compact bones by hammerstone percussion.” Carnivores may extract nutrients by ingesting carpals and tarsals whole, as documented by Marean’s (1991) experimental feeding of hyenas. The second important point with respect to the mechanical properties of bones is that relatively solid spheres, particularly small ones, can withstand significant compression and other forces without deformation or fracture. Hollow spheres (such as crania), solid or hollow rods (such as long bones), or solid or hollow plate-like structures (such as innominates and scapulae) cannot withstand forces of similar magnitude (Currey, 1984:147–150),

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1.0 trapezoid magnum

distal fibula

DISC

naviculocuboid

SPHERE lunar

scaphoid

cuneiform

unciform

pisiform

astragalus

tarsal 2 & 3

b/a

2nd phalanx

3rd phalanx

0.5

1st phalanx calcaneum

BLADE

ROD

0.1 0.1

0.5

1.0

c/b

Figure 19.1 Classification of shape of carpals, tarsals, and phalanges.

particularly if their groundward surface is not uniformly in contact with the sediments on which they lie. Tarsals, with the exception of the calcaneum, and carpals are small and relatively spherical and thus their groundward surface is typically in uniform contact with the sediments on which they lie. Thus, they are unlikely to be regularly fractured by mere sediment overburden weight, which is not to say that they will never be broken by this taphonomic factor. For example, catastrophic burial, such as a roof-fall event within a cave, may not only bury bones, but fracture them as well (e.g., Thomas and Mayer, 1983). Chemical leaching no doubt weakens all bones, but we have no data to evaluate this diagenetic process and do not consider it further here. If small spherical bones such as carpals and tarsals (except the calcaneum) are unlikely to be fractured except by diagenetic processes, then first and second phalanges should be more frequently broken than carpals and tarsals of the same taxon (Figure 19.1). This is because these phalanges contain more marrow and grease than carpals and tarsals (Table 19.1), and thus are more likely to be broken by predators (hominids or carnivores) during the biostratinomic phase. The second phalanx is also more likely to be broken than a carpal or tarsal because it is a hollow bone of rod-like shape, resulting in a greater probability of diagenetic fracture. First phalanges should be more broken than second phalanges because they are hollow rods and are longer than second phalanges, resulting in a greater probability of diagenetic fracture. For the same reason, the calcaneum, a relatively rod-like bone (Figure 19.1) with some marrow and grease (Table 19.1), should be relatively more broken than other tarsals and carpals as a result of both biostratinomic and diagenetic processes.

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There are two assumptions underlying the statements in the preceding paragraph. First, we assume that during the biostratinomic phase, hominids and carnivores that are fracturing bones for purposes of grease/marrow extraction will break these bones in direct proportion to (a) their grease/marrow content and (b) ease of fracture (shape, size, and density related). Second, we assume that the probability that diagenetic processes will result in fragmentation decreases as skeletal element shape shifts from rod-like to sphere-like, and as skeletal elements increase in density (decrease in food utility) and decrease in size. Note what is said in the two immediately preceding sentences. Predators acting during the biostratinomic phase will break skeletal elements relative to the ease of element fracturing, and diagenetic processes will break skeletal elements relative to their shape, density, and size, or their ease of fracture. In other words, we suspect Marean’s hypothesis that the fragmentation of skeletal elements will be mediated by the elements’ shape, density, and size is correct, but that it is correct regardless of the fracture agent. This belief leads us to suggest an expansion to Marean’s (1991) method. Marean focused exclusively on bones he thought would most likely not be broken during the biostratinomic phase; in his view, these are the carpals and tarsals. He noted that the calcaneum has a “small marrow cavity that may entice predator fragmentation” and thus he thought it “best to exclude calcanea from any analysis of postdepositional [postburial] destruction” (Marean, 1991:681). The same argument could be made for the first and second phalanges. We think it unlikely, however, that postburial fragmentation and destruction will be limited to only those skeletal elements not broken during the biostratinomic phase. In particular, we suspect that there will be a continuum from a low to a high degree of fragmentation, and that this continuum will correlate directly with several variables: bone shape as it alters from spheroid to rod-like or blade-like; bone size as it alters from small to large; and marrow and grease utility as these alter from minimum to maximum values. We also suspect that the degree of fragmentation will correlate inversely (coefficients will be negative) with structural density because as density decreases, skeletal elements will be less strong structurally. We expand Marean’s method and include phalanges and calcanea in our analyses below to evaluate our suspicions of a continuum of fragmentation. If statistically significant correlations are found between the degree of fragmentation and the food utility, shape, size, and density of skeletal elements, then it can be argued that the mere presence of fragmented carpals and tarsals is insufficient to indicate postburial fragmentation. Quantification Marean’s (1991) CI% value was proposed as an improvement to other means of measuring the degree of fragmentation, particularly that proposed by Klein and Cruz-Uribe (1984), who suggested that a NISP:MNI or NISP:MNE* ratio would provide a measure of fragmentation. In proposing the CI% value, Marean (1991:680) was correctly concerned that inter-observer variation in both (a) how MNI and MNE values were calculated, and (b) which identified specimens were included in the calculations, would influence results. The first concern hinges on the fact that MNI and MNE values are derived rather than observational * MNI values are derived from sets of all identified specimens and represent the minimum number of individual animals necessary to account for the specimens. MNE values are derived from sets of specimens of particular skeletal elements and represent the minimum number of skeletal elements necessary to account for the specimens.

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and thus they can be determined in various ways (e.g., Grayson, 1984; Lyman, 1994a). We believe, however, that if the observer is consistent within an analysis, then the MNI and MNE values will be consistently derived. We also believe that variation in the inclusion of specimens can influence not only NISP:MNI and NISP:MNE ratios, but the CI% value because the latter also depends on which specimens are included in the tally. Therefore, although we understand Marean’s concerns, we find them incompletely resolved by the use of the CI%. Consistent application of criteria for inclusion of specimens in NISP tallies and for derivation of MNE and MNI values should circumvent the problems Marean identifies. Of course, there will always be variation between analysts in terms of what, for example, Lyman believes is identifiable and what Darwent does. In other words, inter-observer bias will always be a problem, regardless of which measure of fragmentation is used. The NISP:MNE ratio is elsewhere termed the intensity of fragmentation (Lyman, 1994b:294). Lyman (1994b:294) suggested one could measure the extent of fragmentation as the “proportion of specimens [of a particular skeletal element] that are complete” or “%Whole,” and that in conjunction with the intensity of fragmentation, these two measures would provide two indices of the degree of fragmentation. The extent of fragmentation is easily observed within a collection as long as what is tallied as a complete or whole specimen is consistent from specimen to specimen. Unlike the CI%, the NISP:MNE ratio depends on whether specimens overlap anatomically or not; that is, for the intensity of fragmentation, the distal half of two humeri, both from the same side, would be tallied as a ratio of 2:2 (reduced to 1:1), whereas the CI% would be 50%. The former ratio would be 2:1 if one proximal half and one distal half that did not overlap anatomically were represented, whereas the CI% would still be 50% in this case. Our point here is that the different indices — CI%, NISP:MNE, %Whole — measure different properties of a collection (Lyman, 1994a). Is one more correct than the other? The only way that the preceding question can be answered is to agree on a variable that we wish to measure. The variable of interest in studies of postburial fragmentation is the degree of fragmentation, or what we define as a measure of how broken skeletal elements are. All three indices — CI%, NISP:MNE, %Whole — measure this variable. As we noted earlier, the CI% can be read as “the average completeness of specimens of element X.” The NISP:MNE ratio, too, is a statement concerning the completeness of specimens because it expresses the average number of specimens per skeletal element.* The NISP:MNE ratio contains the same information as the CI%, but it also contains the additional information of specimen overlap as expressed by the MNE. The %Whole index indicates the proportion of all specimens that are anatomically complete or that comprise an entire skeletal element, thus its information content overlaps with, but is less than, the other two because it only indirectly accounts for specimens comprising incomplete skeletal elements. In one sense, then, the amount of information regarding fragmentation increases from %Whole (with the least information), to CI%, to NISP:MNE. Because of information overlap, the latter * When Lyman (1994b:294) discussed the NISP:MNE index, he suggested that complete skeletal elements — whole bones — should not be included in the calculation. This suggestion was made there because the goal was to answer the two-part question, “How anatomically complete are the incomplete specimens, and how much anatomical overlap do incomplete specimens display?” The CI% merely asks, “How anatomically complete are all the specimens, on average?” Including anatomically complete specimens in the NISP:MNE ratio addressed the two-part question, “How anatomically complete are all specimens, on average, and how much anatomical overlap do the total specimens display?”

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two should be inversely correlated (see also Marean, 1991:689–690); and, the %Whole and CI% should also be correlated when the former is large across multiple skeletal elements because when this occurs, the CI% will also be large. The preceding suggests that Marean’s (1991) method may be expanded to include three indices of fragmentation. Each index contains similar information, but each also contains unique information. Correlations between the various fragmentation indices, or lack thereof, and the structural density, size, or shape of the skeletal elements may reveal aspects of fragmentation not otherwise discernable were only one of them used during analysis. Incorporation of the size, structural density, and shape of the bones into the analysis addresses Marean’s hypothesized relationship between these variables and the different aspects of the degree of fragmentation captured by the CI%, NISP:MNE, and %Whole indices.

Methods, Materials, and Caveats We chose a sample of bones recovered from archaeological deposits in Moses Coulee Cave (45DO331) in eastern Washington State, to evaluate and expand on Marean’s (1991) method. We chose this particular sample because (a) carpals, tarsals, and phalanges are abundant; (b) the majority of the specimens represent a single taxon; and (c) its postburial taphonomic history comprised a unique stage that potentially fragmented some of the specimens. Temporally diagnostic artifacts associated with the faunal remains span the last 10,000 years, and the bones we discuss here date to that entire time span. Finer temporal resolution is not possible because the site was not professionally excavated. Rather, the sediments within the cave and at the cave mouth were removed and redeposited several meters away from and in front of the cave in 1932 by a Fresno (Lyman, 1995).* The relocated sediments, the “spoils pile,” were screened and artifacts and faunal remains collected in 1988 and 1989 by avocational archaeologists. Lyman (1995) studied the faunal remains in 1993 and reported on the taxonomic composition of the collection. The majority of the bones from Moses Coulee Cave were readily identified as bighorn sheep (Ovis canadensis, NISP = 2190); a few represented deer (Odocoileus sp., NISP = 88), pronghorn antelope (Antilocapra americana, NISP = 19), wapiti (Cervus elaphus) NISP = 4, and bison (Bison bison) or domestic cow (Bos taurus, NISP bison + cow = 198) (bones modified into artifacts and isolated teeth were omitted). We reexamined the carpals, tarsals, and phalanges of deer-sized artiodactyls for purposes of analyses discussed here. Specimens of bighorn sheep, deer, pronghorn antelope, and those deer-sized bones that could not be identified to species are included. The fact that multiple taxa are included should have minimal influence on analytical results. This is true for two reasons. First, the three taxa are similar in size and basic body plan, and their bones are similar in size, shape, and density, so taxonomic differences are unlikely to have contributed to variation in the taphonomic histories of individual specimens. Second, it is likely that the majority of the carpals, tarsals, and phalanges discussed here represent bighorn sheep. This is because the specimens of these elements that were sufficiently * A Fresno is so-called because the Agricultural Works of Fresno, California, were a major manufacturer of them. A Fresno, also known as a buck scraper, is an earth digging and transporting device consisting of a crescent-shaped, bottomless bucket or scoop that is dragged along the ground. It has two runners upon which the scoop is lifted when it is filled.

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Table 19.2 Frequencies (NISP) of Carpals, Tarsals, and Phalanges of Bighorn Sheep, Deer, Pronghorn Antelope, and Deer-Sized Specimens from Moses Coulee Cave Skeletal Element Cuneiform Lunar Pisiform Scaphoid Trapezoid magnum Unciform Calcaneum Astragalus Naviculo-cuboid Tarsal 2 + 3 Distal fibula First phalanx Second phalanx Third phalanx a

Bighorn Sheep

Deer

Pronghorn Antelope

Deer-Sizeda

58 55 — 72 94 — 63 — 51 — — 203 155 106

1 8 — 6 2 — — — 3 — — 1 7 7

— — — — — — — — 1 — — 1 1 —

4 22 42 15 22 79 184 325 57 97 74 265 — —

Counts differ from Lyman (1995) because some specimens could not be relocated, and some new specimens were identified.

anatomically complete to allow identification to species are dominated by bighorn sheep remains (Table 19.2). Thus, even if specimens of multiple taxa are included in NISP tallies, the few non-bighorn specimens will have minimal influence on these tallies and on analytical results. We followed Marean’s (1991) procedure and recorded various data for each specimen. The skeletal element represented, whether it was burned, excessively weathered, corroded as a result of digestion, displayed carnivore or rodent gnawing damage, displayed butchering marks such as chopping or percussion scars, were recorded.* Modern fractures were noted when the fracture surface was a lighter color than an unfractured surface of a specimen. We also noted if the proximal epiphysis of first and second phalanges were fused to the diaphysis, and if the tuberosity of the calcaneum was fused to the shaft. If a specimen was incomplete, we evaluated its completeness by superimposing it on a 2-mm grid and estimating the amount remaining relative to a complete specimen. To insure against interobserver variation, Darwent recorded all data discussed here.** Faunal remains recovered from Moses Coulee Cave included specimens representing five genera and at least six species of carnivore. These include the gray wolf (Canis lupus, NISP =1); dog (C. familiaris) or coyote (C. latrans) (NISP = 38); red fox (Vulpes vulpes, * A number of carpals and tarsals have cut marks, but we do not consider them here. Similarly, few specimens display modern damage such as may have resulted from the 1932 mechanical movement by the Fresno of the sediment and bones; if present, such damage is superficial. ** To test for inter-observer bias in estimating specimen completeness, Darwent selected a sample of 10 first phalanx specimens and 10 naviculo-cuboid specimens. Lyman then estimated the completeness of each specimen and calculated the CI% for both samples. For the phalanges, Lyman’s CI% was 31.5% and Darwent’s was 34%; for the naviculo-cuboid, Lyman’s CI% was 42.5% and Darwent’s was 44.0%. This small test suggests inter-observer variation may influence CI% values.

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NISP = 7); long-tailed weasel (Mustela frenata, NISP = 1); badger (Taxida taxus, NISP = 4); and bobcat (Lynx rufus, NISP = 1). Of these, the canids and badger are the most likely to have created the gnawing and digestive corrosion damage evident on some of the carpals, tarsals, and phalanges (Lyman, 1995) In his experiments, Marean (1991) found that when metapodials were laid on an anvil and broken with a hammerstone, surfaces of carpals and tarsals articulated with the metapodials lacked percussion scars. He reasoned that the latter occurred because the carpals and tarsals “are encased in a thick and resistant ligament and tendon mass that cushions them from hammerstone blows” (Marean 1991:681). He also found that when carpals and tarsals are intentionally broken with a hammerstone, “the force needed to break a compact bone is so great that the hammerstone/anvil impact marks on the compact bone are extremely prominent and easily recognized” (Marean, 1991:681). Marean referenced Blumenschine and Selvaggio (1988) as illustrating the kinds of impact marks he found, and we consulted this paper, as well as a related one (Blumenschine and Selvaggio, 1991). To insure that we knew the kinds of attributes to look for when searching for percussion damage and to be able to recognize them, we experimentally broke carpals, tarsals, and phalanges of domestic pig (Sus scrofa) with a hammerstone. All specimens had been defleshed by boiling, and we chose specimens that were still greasy to replicate possible prehistoric conditions. We laid individual skeletal elements on a smooth hard surface (anvil), and struck them with a quartzite cobble. After fragmentation, we collected all fragments and inspected them for evidence of impact damage. In light of Marean’s statements, our observations are rather disconcerting. Percussion damage to some specimens was minimal; refitting fragments sometimes made it easier to detect the damage such as when an articular surface of adjacent fragments did not match up smoothly across two refit specimens. Further, some phalanges were broken, yet none of the resulting specimens displayed what we could unambiguously term percussion damage. The shaft or diaphysis was simply broken. No crushing of what a lithic technologist calls the platform or point of impact was observable. The same applied to some carpals and tarsals; a few of these simply broke or split into pieces. Finally, some specimens of all elements did not display percussion damage of any kind; for example, the 10 astragali we broke produced a total of 70 fragments (individual astragali produced 3 to 16 pieces). Of those 70 fragments, only 12 (17%) clearly displayed percussion damage; 2 astragali, 1 that broke into 3 pieces and another that broke into 7 pieces, produced no specimens with impact damage. Our observations have, we believe, extremely significant implications. They suggest that omitting specimens with percussion damage from derivations of fragmentation indices will not eliminate all specimens that were produced by hammerstone-generated fracturing. Because we as yet do not know how to account for this fact, we largely ignore it in our analysis. Further, we are unsure of the reason behind our results apparently not mimicking Marean’s. Perhaps it is because we did not precisely replicate his experimental protocol. We do not know, for example, if the carpals and tarsals he broke were defleshed, nor do we know the precise kinds of percussion damage he sought and found to be “extremely prominent and easily recognized.” And, Marean does not say that every specimen of carpal and tarsal generated by his breaking bones with a hammerstone retained percussion damage. Clearly, there is a need for more rigorous experimental fracturing of carpals, tarsals, and phalanges and more rigorous documentation of such, but we caution that all such

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experiments may be of more or less limited utility because of the particular historical contingencies of every instance of fragmentation.* With that caveat in mind, we turn to our analysis of the Moses Coulee Cave specimens.

Results The taxonomic and skeletal composition of the assemblage of carpals, tarsals, and phalanges we examined is summarized in Table 19.2. In this section, we ignore taxonomic distinctions and summarize other data we recorded for this collection and describe our analyses of these data. Because many of our analyses involve calculating the degree of correlation between certain variable pairs, we describe these variables and note their significance before turning to detailed analyses. Skeletal Element Frequencies There are a number of reasons why the frequencies of the different skeletal elements we consider here may vary. Given our analytical focus on fragmentation, two of the reasons are important in the present context. First, smaller specimens (especially fragments) may have been less often recovered than large specimens. To explore recovery bias, we correlated the frequency of complete specimens of each skeletal element with the average maximum dimension and also with the average minimum dimension of each. Our reasoning in doing so is simple. If recovery methods resulted in a biased collection, the smallest specimens would be the ones most likely to be overlooked and not recovered (e.g., Schaeffer, 1992; Watson, 1972), irrespective of whether a specimen represented a complete skeletal element. Recovery bias would, therefore, be reflected by a positive correlation between specimen size and frequency. Rather than measure each individual specimen, we used the maximum and minimum dimensions of complete skeletal elements as the measure of size. Our assumption was that handpicking specimens from sediments would depend on their maximum size, and recovering specimens from screens would depend on their minimum size. Relevant data are given in Table 19.3. There is no significant correlation between the minimum dimension and the number of whole skeletal elements (Spearman’s rho = –.244, p =. 4) nor between maximum dimension and the number of whole skeletal elements (rho = –.407, p = .15). These statistics, in conjunction with the facts that some specimens included in the NISP counts are less than 1 cm3 in size, and that .25-in. mesh screens were used to recover the remains (Lyman, 1995), suggest that recovery methods did not result in failure to collect small fragments of the skeletal elements under study here. The second reason specimen counts may be biased is that skeletal elements of lower structural density may have been more frequently destroyed by biostratinomic or diagenetic processes. One way to detect such destruction is to determine if the structural density of each skeletal element is inversely correlated with the NISP of each skeletal element. Our reasoning here is that skeletal elements of low structural density should be more fragmented (perhaps to the point of destruction or analytical invisibility) and thus have higher NISP * Although a machine could be built to precisely replicate the amount of force applied and the point of force application in test after test, microstructural variation in, say, each astragalus broken in conjunction with variation in amounts of adhering soft tissue and grease content would undoubtedly result in variation in fracturing and percussion damage.

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Table 19.3 Number of Whole Specimens, Average Minimum Dimension, and Average Maximum Dimension for Each Skeletal Element Skeletal Element Cuneiform Lunar Pisiform Scaphoid Trapezoid magnum Unciform Calcaneum Astragalus Naviculo-cuboid Tarsal 2+3 Distal fibula First phalanx Second phalanx Third phalanx a b

Number Wholea

Minimum Dimensionb

Middle Dimensionb

Maximum Dimensionb

44 56 22 59 75 53 12 60 27 67 48 10 38 25

10.2 15.5 8.4 12.7 10.5 13.3 22.3 21.4 20.8 8.6 12.0 16.5 14.8 11.7

19.5 17.7 12.8 17.2 20.8 14.6 30.4 26.0 28.1 13.2 17.5 20.5 18.1 21.7

25.0 23.3 18.8 23.6 21.4 19.6 84.5 39.4 30.8 20.7 19.0 52.7 32.5 39.3

Includes all complete specimens regardless of whether specimen is burned. Average of five specimens; all measurements are in millimeters.

values than elements of high structural density. The structural density of each skeletal element is given in Table 19.1, and the NISP values are given in Table 19.2; we summed the latter because we suspected taxonomic variation in structural density of the elements is minimal. The two variables are not correlated (rho = –.371, p = .236), suggesting that the overall NISP frequencies are not a function of density-mediated fragmentation and destruction. The bivariate scatterplot of these data, however, suggests that the NISP of phalanges, astragali, and calcanea may in part be a function of density-mediated processes, whereas the NISP of carpals, naviculo-cuboids, and distal fibulae are not (Figure 19.2). We return to this potentiality in our discussion of the influences of skeletal element shape on taphonomic history. Sphericity As indicated earlier, we suspect that as specimens approach perfect spheres in shape, they are less likely to be crushed or fragmented by sediment-overburden weight. This is because in part spheres have low surface-to-volume ratios. We used a method developed by sedimentologists (Zingg, 1935) to estimate the sphericity of the skeletal elements we studied. Sphericity is defined by the equation [(bc/a2)0.33] where a is the maximum dimension (length), b is the middle-magnitude dimension (width), and c is the minimum dimension (thickness). These three measurements are taken at mutually perpendicular axes and are not related to the anatomical orientation of the bones but rather to the bone’s shape. We measured these three dimensions on five complete specimens of each carpal, tarsal, and phalanx (Table 19.3), and then used the average of each dimension to calculate sphericity. Sphericity values for all elements are listed in Table 19.4. The higher the value, the greater the sphericity of the element. Sedimentologists also use the minimum, middle-magnitude, and maximum dimensions to plot specimens on a graph to ascertain shape (Figure 19.1). Four nominal shape categories are recognized on the graph; spherical or “equant” shapes fall in the upper right

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500

1st phalanx

400 astragalus

NISP

300 calcaneum

200 2nd phalanx

100

naviculocuboid 3rd phalanx

distal fibula

trapezoid magnum lunar

unciform

scaphoid

cuneiform

0 0.2

0.4

0.6

0.8

1.0

Structural Density

Figure 19.2 Bivariate scatterplot of NISP values per skeletal element against the structural density of each skeletal element.

quadrant; disc or “oblate” shapes fall in the upper left quadrant; blade shapes in the lower left quadrant; and rod or “prolate” shapes in the lower right quadrant (terms in quotes from Waters, 1992:27). Figure 19.1 suggests most carpals and some tarsals could be categorized as spheres whereas the calcaneum and first and second phalanges comprise rods. The third phalanx is the only blade-shaped element, and the trapezoid magnum and cuneiform are the only discs. Recall from our discussion of skeletal element frequencies that as the structural density of phalanges, astragali, and calcanea increased, it appeared that their respective frequencies increased whereas the frequencies of carpals, distal fibulae, and naviculo-cuboids displayed no relationship to their structural density (Figure 19.2). We suspect the reason for this is that the sphericity of the latter group of elements is greater than that of the former group. As indicated in Table 19.4, skeletal elements comprising the first group are the four least spherical elements, plus the seventh least spherical element (astragalus); skeletal elements comprising the other group include the six most spherical elements plus the eighth least spherical element (cuneiform). This observation suggests that the reason for the lack of relationship between the NISP frequencies of carpals, distal fibulae, and naviculo-cuboids and their structural densities, and the apparent relationship between the NISP frequencies of phalanges, calcanea, and astragali and their structural densities, may reside in differences in the degree to which they are fragmented. As we argued earlier, we expect skeletal elements that more closely approximate spheres to be less fragmented. In other words, are phalanges,

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Figure 19.3 Bighorn sheep astragali from Moses Coulee Cave. The specimen on the left is complete and undigested; the other four specimens, from left to right, display progressively greater degrees of digestive corrosion yet appear to have been ingested when complete. Table 19.4 Sphericity Values for Skeletal Elements Examined in This Study Skeletal Element Calcaneum First phalanx Third phalanx Second phalanx Tarsal 2 + 3 Pisiform Cuneiform Astragalus Scaphoid Trapezoid magnum Unciform Lunar Distal fibula Naviculo-cuboid

Sphericity 0.460 0.499 0.551 0.636 0.646 0.676 0.685 0.713 0.735 0.784 0.799 0.800 0.836 0.852

calcanea, and astragali more susceptible to fragmentation because they are less spherical in shape whereas carpals, distal fibulae, and naviculo-cuboids are less susceptible to fragmentation because they are more spherical? This is the topic we turn to next.

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Table 19.5 Indices of Fragmentation for All Carpals, Tarsals, and Phalanges from Moses Coulee Cave Skeletal Element

NISP

MNE

CI%

NISP:MNE

%Whole

Cuneiform Lunar Pisiform Scaphoid Trapezoid magnum Unciform Calcaneum Astragalus Naviculo-cuboid Tarsal 2 + 3 Distal fibula First phalanx Second phalanx Third phalanx

63 85 42 93 118 79 247 325 112 97 74 470 163 113

63 82 42 92 118 78 66 230 91 97 74 197 119 102

91.4 90.8 93.4 90.1 86.9 92.2 32.3 60.6 66.0 96.4 90.5 29.4 58.2 57.8

1 1.04 1 1.05 1 1.08 3.74 1.41 1.23 1 1 2.39 1.37 1.11

80.7 74.7 64.7 72.8 71.4 79.1 7.7 22.3 27.3 80.7 64.9 2.1 21.3 22.1

Table 19.6 Indices of Fragmentation for Unmodifieda Carpals, Tarsals, and Phalanges from Moses Coulee Cave Skeletal Element

NISP

MNE

CI%

NISP:MNE

%Whole

Cuneiform Lunar Pisiform Scaphoid Trapezoid magnum Unciform Calcaneum Astragalus Naviculo-cuboid Tarsal 2 + 3 Distal fibula First phalanx Second phalanx Third phalanx

51 58 27 55 78 59 59 107 53 69 45 325 103 76

51 57 27 55 78 59 26 91 50 69 45 159 71 67

92.9 89.3 94.8 95.7 70.6 93.3 43.4 80.1 78.2 97.7 90.2 29.7 53.2 59.3

1 1.02 1 1 1 1 2.27 1.17 1.06 1 1 2.04 1.45 1.13

82.3 72.4 66.7 85.5 74.7 78.3 20.3 35.3 38.2 84.1 66.7 2.8 22.3 23.7

a

Burned, gnawed, digested, and freshly broken specimens, and specimens with percussion damage, omitted.

Fragmentation For analytical purposes, we define modified specimens as those that display attributes of burning, digestive corrosion, rodent or carnivore gnawing, percussion damage, or some combination of these traces of (with the possible exception of percussion) biostratinomic damage. Unmodified specimens are those that display none of these attributes. The three indices of fragmentation for modified and unmodified specimens combined are listed in Table 19.5. Fragmentation index values for unmodified specimens are given in Table 19.6. The CI% and %Whole values tend to increase when modified specimens are omitted, as Marean’s (1991) analysis suggested they should. The majority of the NISP:MNE ratios, however, either do not change (five values) or they decrease only a small amount (six values). The single exception is the calcaneum, the NISP:MNE ratio for which decreases

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Table 19.7 Absolute and Relative Abundances of Carnivore Gnawed, Digested, Rodent Gnawed, and Burned Specimens from Moses Coulee Cavea

Skeletal Element

Total NISP

NISP Carnivore Gnawed

NISP Digested

NISP Rodent Gnawed

NISP Burned

NISP with Percussion

Cuneiform Lunar Pisiformb Scaphoidb Trapezoid magnum Unciform Calcaneum Astragalus Naviculo-cuboidb Tarsal 2 + 3 Distal fibulac First phalanxd Second phalanx Third phalanxe

63 85 42 93 118 79 247 325 112 97 74 470 163 113

2 (3.2) 0 4 (9.5) 6 (6.5) 6 (5.1) 7 (8.9) 90 (36.4) 51 (15.7) 9 (8.0) 7 (7.2) 0 10 (2.1) 4 (2.5) 5 (4.4)

3 (4.8) 10 (11.8) 4 (9.5) 6 (6.5) 7 (5.9) 5 (6.3) 0 6 (1.8) 10 (8.9) 7 (7.2) 4 (5.4) 33 (7.0) 25 (15.3) 3 (2.7)

1 (1.6) 0 1 (2.4) 1 (1.1) 0 0 1 (0.4) 0 1 (0.9) 0 0 9 (1.9) 6 (3.7) 15 (13.3)

6 (9.5) 17 (20.0) 7 (16.7) 26 (28.0) 26 (22.0) 8 (10.1) 96 (38.9) 152 (46.7) 38 (33.9) 14 (14.4) 27 (36.5) 88 (18.7) 25 (15.3) 21 (18.6)

0 0 0 0 1 (0.8) 0 1 (0.4) 9 (2.8) 2 (1.8) 0 0 13 (2.8) 0 0

a b c d e

Values in parentheses are relative (%) abundance of specimens with the indicated modification. One specimen displays more than one kind of modification. Two specimens display more than one kind of modification. Eight specimens display more than one kind of modification. Seven specimens display more than one kind of modification.

54% ([3.74 – 2.27] + [3.74 – 1]). This suggests that the calcaneum, the largest (Table 19.3) and also most rod-like (Figure 19.1) element, was the most prone to be fragmented if it was modified by burning, carnivore gnawing, and the like. Thirteen first phalanx specimens, nine astragali, two naviculo-cuboids, one trapezoid magnum, and one calcaneum display percussion damage, suggesting they were broken by human predators wielding hammerstones, by roof-fall, or by a combination of the two (Table 19.7). We had intended to correlate the number of specimens displaying percussion scars with marrow and grease utility values (see below) under the assumption that larger proportions of elements with higher utility values would display such modification than elements with lower utility values if the percussion scars were the result of human taphonomic agents. The low number of specimens with percussion scars precluded calculating a coefficient, but we note that the calcaneum and first phalanx have the greatest marrow and grease values (Table 19.1), suggesting that they may have been broken for that reason. However, we also note that these are the two most rod-like elements and thus are, we suspect, the most prone to diagenetic fragmentation. Diagenetic fragmentation could account for the fact that identical relative abundances of first phalanx and astragalus specimens display percussion damage. But so could biostratonomic fragmentation account for the relative frequencies of specimens displaying percussion damage because the naviculo-cuboid, with the third highest grease utility value, has the third greatest proportion of specimens with percussion damage. Gnawing damage by rodents may have obliterated some flake scars, though only a few specimens display such damage (Table 19.7). Part of the analytical difficulty we encountered is that some specimens were variously chewed and gnawed by carnivores, and the resulting damage could either have obliterated evidence of percussion scars or been confused with

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percussion scars. Also, modern damage to bones which may have resulted from mechanical movement (the 1932 Fresno) of the sediments possibly obliterated percussion damage, though we think this unlikely given that such damage is very superficial and does not occur on many specimens. Perhaps most importantly, as we noted when we experimentally broke pig carpals, tarsals, and phalanges, not all hammerstone-broken specimens can be expected to display obvious percussion damage. There is no statistically significant relationship between the minimum or maximum dimension of the elements (Table 19.3) and the proportion of carnivore gnawed or proportion of digested specimens (p > .2 for all tests); however, more than 18% of all tarsals display evidence of carnivore gnawing whereas only 5.2% of all carpals and 2.5% of all phalanges display such damage. This rank ordering is exactly the reverse for digestive corrosion: 8.2% of all phalanges, 7.3% of all carpals, and 3.2% of all tarsal specimens display digestive corrosion. It seems reasonable to suppose that larger elements are more prone to display evidence of gnawing whereas smaller elements are prone to display digestive corrosion, granting the assumption that larger elements are more difficult to ingest than smaller ones. However, as shown in Figure 19.3, astragali, the second largest skeletal element under consideration (Table 19.3), were at least occasionally ingested whole by Moses Coulee Cave carnivores and underwent various degrees of corrosive destruction as a result. This prompts us to wonder if there is a relationship between carnivore gnawing and digestive corrosion, and the food utility of the elements. Grease and Marrow Utility Binford (1978) determined the food value of many skeletal elements of two artiodactyls species. We chose to use caribou (Rangifer tarandus) index values for our analysis because this species is similar in body size and shape to the three taxa under consideration. Binford derived a grease utility value and a marrow utility value for all carpals as an articulated mass; the naviculo-cuboid, tarsal 2 + 3, and distal fibula (we believe) as an articulated mass; the isolated calcaneum; the isolated astragalus; the first phalanx; the second phalanx; and the third phalanx. We did two things to derive the marrow and grease utility values given in Table 19.1 for each isolated skeletal element. First, because all carpals, the naviculocuboid, tarsal 2 + 3, and distal fibula are compact bones with no marrow cavity, it is reasonable to assign them a marrow utility value of 1, which is identical to the value Binford assigned to the astragalus, a compact bone with no marrow cavity. Second, we determined the volume (via water displacement) for several complete specimens of each element and calculated the average. This was used to calculate a grease utility index value for the naviculo-cuboid, tarsals 2 + 3, distal fibula, and isolated carpals. For the three indicated tarsals, we multiplied the percent of the total volume of the three as represented by one element by the grease utility index for all three (29.87). For the six carpals, we multiplied the percent of the total volume of all six as represented by one element by the grease utility index for all six (36.47). These calculations produced the grease utility values for each individual carpal, naviculo-cuboid, tarsal 2 + 3, and distal fibula (Table 19.1). The proportion of carnivore-gnawed specimens per skeletal element is not correlated with either the marrow utility values or the grease utility values (p > .5 for both). Similarly, the proportion of digested specimens per skeletal element is not correlated with these food utility values (p > .5 for both). Finally, we note that the correlation between the simple sum of the two utility indices and the simple sum of the proportions of gnawed and digested

© 2002 by CRC Press LLC

Table 19.8 Correlation Coefficients (Spearman’s rho) Between Fragmentation Indices and the Summed Grease and Marrow Utility Indices Modified and Unmodified

Unmodified Only

Fragmentation Index

Rho

p

Rho

p

CI% NISP:MNE %Whole

–.833 .898 –.749

< .0001 < .0001 .0021

–.773 .906 –.688

.001 < .0001 .0065

specimens is statistically insignificant (p = .3). In other words, it does not seem that Moses Coulee Cave carnivores were exploiting the carpals, tarsals, and phalanges of deer-sized artiodactyls at intensities commensurate with the food value of those elements. Do the food indices have any relationship to the degree of fragmentation? In fact, they do. All three fragmentation indices, whether derived from modified plus unmodified specimens or from only unmodified specimens, are significantly correlated with the sum of the marrow and grease utility values (Table 19.8). Why might this be the case? In short, we believe this is a function of the size, shape, and density of the skeletal elements. What Mediates Fragmentation? According to Marean (1991:691), postburial fragmentation of bones will be indicated by small CI% values, particularly if those values are for the astragalus and naviculo-cuboid. Marean noted that he could not answer the question of how small “small” CI% values should be to unambiguously indicate postburial fragmentation. He focused on the fragmentation of what he considered to be “small, compact bones” and hypothesized that the density, size, and shape of skeletal elements would mediate their postburial fragmentation. To evaluate the influence of density on fragmentation, we correlated the three indices of fragmentation with the structural density of each skeletal element. Resulting coefficients are given in Table 19.9. If all modified and unmodified specimens (Table 19.5) are included, only the correlations between CI% and density, and between %Whole and density are significant. If only unmodified specimens (Table 19.6) are included, then all three coefficients can be considered significant (p < .085). This tends to corroborate Marean’s suggestion that inclusion of modified specimens will skew measures of fragmentation. More importantly, the coefficients suggest that the structural density of skeletal elements mediates their fragmentation irrespective of agent and process of fragmentation. To evaluate the influences of bone shape on fragmentation, we correlated the three indices of fragmentation with element sphericity (Table 19.4). Resulting coefficients are listed in Table 19.9. If all modified and unmodified specimens (Table 19.5) are included, only the correlation between %Whole and sphericity might be considered significant. If only unmodified specimens (Table 19.6) are included, then two coefficients, for %Whole and NISP:MNE, can be considered significant (p < .08). This also corroborates Marean’s suggestion that inclusion of modified specimens will skew results. Focusing then on the coefficients for unmodified s