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A thesis submitted to the Faculty of Science, University of the Witwatersrand, Johannesburg, in fulfilment of the requirements for the degree of Doctor of Philosophy. 25th of July 2013, Johannesburg. / The cave deposits at Malapa, on the Malapa Nature Reserve, Cradle of Humankind World Heritage Site, Gauteng Province, South Africa, have yielded the remains of two extremely well-preserved hominins (Australopithecus sediba) and associated fauna, dated by U/Pb methods and palaeomagnetism to 1.977-1.8 Ma. The state of preservation of the hominins and some of the non-hominin material, characterised by complete and near complete elements, antimeric sets of bones, specimens in articulation, and well-preserved bone surfaces, is remarkable in the context of Plio-Pleistocene fossil assemblages accumulated in caves, and indicates a unique combination of taphonomic processes, not yet observed in contemporaneous cave deposits in the region. A comprehensive approach, including palaeontological, physical, and spatial analyses of the hominins and associated fauna was undertaken to determine, describe and interpret the taphonomy of the faunal material, with particular reference to the holotype and paratype of Au. sediba, Malapa Hominin 1 (MH1) and Malapa Hominin 2 (MH2). An innovative combination of Computed-Tomography (CT), micro-CT scanning and virtual reconstruction techniques was applied to create a 3D model of a selected area of the Malapa cave, with renderings of the two near-complete Au. sediba skeletons. The original burial position of the hominins was reconstructed, which necessitated the refitting of ex situ fossils into in situ deposits. The spatial distribution and orientation of the hominin remains illustrate a very low degree of dispersal of the bones, indicative of very little disruption between death and burial, due to an absence of damage by scavengers and possible natural mummification. The very few carnivore-damaged bones and relative abundance of complete and/or articulated specimens, the presence of antimeric sets of bones in the faunal assemblage, as well as the diversity of the faunal spectrum, and the significant percentage of animals with climbing proclivities (such as carnivores and hominins) indicate that the majority of the faunal material recovered was most likely accumulated via a natural death trap. Their bodies came to rest in a deep area of the cave system with restricted access to iii scavengers. Skeletons and bones accumulated in a talus cone below a vertical shaft. There, they decomposed, and became buried without major disruption by biotic or abiotic agents. A new forensic approach, referred to as palaeoforensic taphonomy, was followed in each step of the taphonomic analysis of the two hominins in order to reconstruct the processes of decay, disarticulation, burial and preservation. Results show that both individuals did probably not enter the cave system at the same time. They reached skeletonization and were slightly weathered before final burial, indicating several years of exposure before burial. Insects proved to be the primary modifiers of the hominin remains, pre- and post-depositional with hide beetles (Omorgus squalidus) providing the closest match for some of the fossil modifications observed. Based on the high number of articulated remains, the absence of preferential orientation for the elongated bones and of significant movement of the hominin remains inside the deposit, the debris flow hypothesis that was previously proposed as the principal agent to explain the burial of the hominins and other well-preserved animals is challenged. Evidence of natural mummification before burial for MH1 and MH2 suggests the possible preservation of soft tissue. The innovative 3D techniques applied in this research to conduct the spatial analysis of the fossils proved useful to address taphonomic questions, and will serve as a guide for future excavations of the Malapa in situ deposits, especially for locating the missing skeletal elements of MH1 and MH2.

Cusirisna Cave was discovered in the 1870s by Dr. Earl Flint, an explorer for the Harvard Peabody Musuem. The human remains and artifacts found in the cave were collected and sent to the museum, where they have remained since, unanalyzed. In December 2011, Dr. Clifford T. Brown and I analyzed the osteological material and artifacts because we thought they might be related to the Preclassic cave complexes of neighboring Honduras, an idea originally suggested by Dr. James Brady. I analyzed the human remains while Dr. Brown studied the artifacts. This thesis presents the results of the analyses and compare the findings to other mortuary complexes in Mesoamerica. Despite the paucity of material culture, information regarding context, and the small sample size, I propose Cusirisna as a place of exceptional ritual importance. This project adds to our understanding of cave bioarchaeology, mortuary practices in Mesoamerica, and the prehistory of Nicaragua. / by Kendra L. Philmon. / Thesis (M.A.)--Florida Atlantic University, 2012. / Includes bibliography. / Mode of access: World Wide Web. / System requirements: Adobe Reader.

Estimation of time since death is an important variable when investigating legal cases involving decomposing human remains; however it has been sparsely studied in controlled environments. Decomposition rates are largely influenced by external factors with temperature being the most critical factor. The decomposition rates can also be influenced by insect infestation, chemical residues, and burial, yet little research has been conducted to document how various factors alter the rate and process of decomposition. A common occurrence at human remains recovery sites is the deposit of residues from criminal activities such as gunpowder and explosives. This experiment will look at gunpowder residue’s effects on porcine remains and the insect infestation after exposure. This study was conducted in two phases: the 1st experiment being conducted in the late spring and the 2nd in the early fall. For each experiment two carcasses were covered with gunpowder residue while one carcass served as a control (no residue). The physical decomposition processes as well as ambient temperature were documented for each carcass. The results for the study showed variable findings between the control and experimental subjects. The insect infestation of the remains was consistent with the data from previous entomological studies conducted from areas of similar climate and terrain. Factors that may have influenced the results are discussed in reference to the effects of the gunpowder residue on the decomposing remains.

Thesis (Ph. D.)--University of Chicago, Dept. of Anthropology, March 1999. / Includes bibliographical references. Also available on the Internet.

This study focuses on the assessment of the depositional activity that occurred in six caves of the Petexbatun region of the Peten, Guatemala through a quantitative analysis of the human skeletal material recovered from them. Five of these caves are associated with the site of Dos Pilas; the sixth cave (Cueva de Los Quetzales) is located beneath the site of Las Pacayas. The cave is an important aspect of the Maya worldview, as evidenced in the artifactual and skeletal material found in caves by archaeological exploration. My study is specifically focused on the assessment of the primary and/or secondary burial of Maya dead within these caves via analyses of the relative skeletal element frequencies, the minimum and probable number of individuals, and the identification of human cut marks. Based on these lines of evidence and data from preliminary reports, between 100 and 150 individuals of both sexes and various age groups were primarily deposited/buried in these caves. Secondary activity may be inferred based on evidence of human-made cut marks on several elements. There is no osteological evidence to support the hypothesis of human sacrifice. I was unable to determine the status of the individuals deposited in the caves. The best interpretation is that several types of depositional activity occurred within these caves over time.