Published March 15, 2024 | Version Supplemental material
Journal Article Open

Nondestructive geochemical characterization of fossil hominin taphonomy and burial history

  • 1. ROR icon California Institute of Technology
  • 2. ROR icon Stellenbosch University
  • 3. ROR icon National Museum of Natural History
  • 4. ROR icon Stony Brook University
  • 5. Turkana Basin Institute, P.O. Box 24467, 00502, Nairobi, Kenya
  • 6. ROR icon Brookhaven National Laboratory

Abstract

To date, only three Homo habilis specimens have been discovered that have associated craniodental and postcranial elements, providing a limited fossil record of the ontogeny and morphology of early members of the genus Homo. Recently, a nearly complete dentition, likely attributable to H. habilis, was discovered and excavated from early Pleistocene-age fluvial-lacustrine sediments of the upper Burgi Member of the Koobi Fora Formation at site F25787 in Area 13, near Ileret, Kenya. On the surface less than 15 m away, at site F25966, postcranial elements were found, which, if from the same individual as the nearby dentition, would represent the fourth associated craniodental and postcranial assemblage of this species. We developed a geochemical taphonomic history of these ca. 2 Ma hominin fossils using nondestructive X-ray based microanalytical tools (synchrotron and benchtop X-ray fluorescence chemical imaging and micro- and nano-computed tomography volumetric reconstruction), bulk analyses of sediments and paleosols at the excavation sites, and sedimentologic and stratigraphic observations. We integrate the chemical and physical taphonomic histories to test whether teeth (excavated in situ) and postcranial bones (eroded onto the outcrop surface) derive from a single individual. Minor differences in taphonomic history are attributable to the different biomineral properties of the dental and osseous components and to differences in physical damage during early post-mortem scavenging, dispersal, and burial in adjacent depositional settings. Microscale geochemical mapping enabled the temporal ordination of chemical and physical events in the specimens' chemical taphonomic histories. Specifically, authigenic Fe- and K-bearing clays and Y, U, and Sr uptake occurred in post-burial fractures in bones and were also incorporated pervasively throughout dentin in teeth. Barite mineralization occurred along the latest fractures in both materials, and as a coating on tooth roots. The stratigraphic, taphonomic, and geochemical evidence supports the interpretation that the hominin fossils represent a single individual. Successful application of these nondestructive sample characterization methods demonstrates capabilities for thorough interrogation of the taphonomic histories of other potential hominin fossil associations, enabling more robust and accurate palaeontologic constraints using those relationships.

Copyright and License

© 2024 Elsevier Ltd. All rights reserved.

Acknowledgement

We gratefully acknowledge the Kenyan Ministry of Gender, Culture, the Arts and Heritage; the Kenyan National Commission for Science, Technology, and Innovation; and the National Museums of Kenya. L. Leakey obtained the permits from the Kenyan Ministry of Gender, Culture, the Arts and Heritage for the transport of the hominin fossils and sediments for chemical composition analysis in 2019. Cyprian Nyete collected sedimentary rock samples from the excavation area. T. Present was partially supported by Simons Foundation Grant 668346. Portions of this research were performed at the Tender Energy Spectroscopy (TES) and the X-ray Fluorescence Microprobe (XFM) beamlines and used resources of the National Synchrotron Light Source II, a U.S. Department of Energy (DOE) Office of Science User Facility operated by Brookhaven National Laboratory under Contract No. DE-SC0012704. Construction of, and work at the TES Beamline was partly funded by the National Science Foundation, Earth Sciences (EAR-1128957), NASA (NNX13AD12G) and the Department of Energy, Geosciences (DE-FG02-12ER16342). Benchtop μXRF data was acquired in the Caltech GPS Division Analytical Facility with the support of Chi Ma and John Grotzinger, with partial support from the Simons Foundation. E. Niespolo was supported by a Barr Postdoctoral Fellowship (Caltech). Sediment analyses were performed at the Stellenbosch University BIOGRIP node, which is funded by the Department of Science and Innovation of South Africa.

Data Availability

All data is available in the Supplementary Material and archived at https://doi.org/10.17605/OSF.IO/H8GUC

Conflict of Interest

The authors declare the following financial interests/personal relationships which may be considered as potential competing interests: Theodore M. Present reports financial support was provided by Simons Foundation. Ryan Tappero reports financial support and administrative support were provided by US Department of Energy. Catherine Clarke reports financial support was provided by South Africa Department of Science and Innovation. Paul Northrup reports financial support was provided by National Science Foundation. Paul Northrup reports financial support was provided by NASA.

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Additional details

Related works

Is supplemented by
Dataset: 10.17605/OSF.IO/H8GUC (DOI)

Funding

Simons Foundation
668346
United States Department of Energy
DE-SC0012704
National Science Foundation
EAR-1128957
National Aeronautics and Space Administration
NNX13AD12G
United States Department of Energy
DE-FG02-12ER16342
California Institute of Technology
Barr Postdoctoral Fellowship -
Department of Science and Innovation

Dates

Submitted
2023-09-28
Accepted
2024-01-28
Available
2024-02-15
Version of record

Caltech Custom Metadata

Caltech groups
Division of Geological and Planetary Sciences (GPS)
Publication Status
Published