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Mineralogical and compositional changes in bones exposed on soil surfaces in Amboseli National Park, Kenya: diagenetic mechanisms and the role of sediment pore fluids

Mineralogical and compositional changes in bones exposed on soil surfaces in Amboseli National Park, Kenya: diagenetic mechanisms and the role of sediment pore fluids
Mineralogical and compositional changes in bones exposed on soil surfaces in Amboseli National Park, Kenya: diagenetic mechanisms and the role of sediment pore fluids
Bones exposed on tropical savannah grasslands of Amboseli National Park, Kenya undergo extensive post-mortem alteration within 40 years. A combined analytical approach involving TEM microscopy, trace metal analysis, FTIR spectroscopy, and petrographic analysis has revealed a complex, dynamic diagenetic environment operating within exposed bones, driven by evaporative transport of soil water from the bone/soil interface to the upper exposed surface of the bone. This process results in extensive bone/soil-water interaction, and is responsible for increases in the concentrations of trace elements such as Ba and La of 100 – >1000% within 15 years. The maximum and mean size of bone crystallites increases with continued exposure. This change in mean crystallite length is correlated positively with increases in bone crystallinity, which in turn is associated with degradation of the bone protein. Microbial decomposition is rarely observed in the Amboseli bones, but where present resulted in severe dissolution–reprecipitation of bone mineral. Many bones showed extensive permineralization of the larger vascular spaces with calcite and barite and, to a lesser extent, crandallite. Permineralization of unburied bones may account for 95% reduction in macro (micron–millimeter scale) porosity in the bone within 2 years of death.
We produce a model for pre-burial diagenesis of bone in arid tropical environments that highlights extensive alteration of bone chemistry within 1–40 years post-mortem.
bone, diagenesis, crystallinity, collagen, trace elements, permineralization, amboseli
0305-4403
721-739
Trueman, Clive N.G.
d00d3bd6-a47b-4d47-89ae-841c3d506205
Behrensmeyer, Anna K.
7ffc7b45-c0a2-4422-a061-4fda629a6477
Tuross, Noreen
3e9c5325-abd0-4e83-b6cd-b07063274e18
Weiner, Steve
2b4dde9b-c6d0-4d8a-a54c-cc8c0fe67ac5
Trueman, Clive N.G.
d00d3bd6-a47b-4d47-89ae-841c3d506205
Behrensmeyer, Anna K.
7ffc7b45-c0a2-4422-a061-4fda629a6477
Tuross, Noreen
3e9c5325-abd0-4e83-b6cd-b07063274e18
Weiner, Steve
2b4dde9b-c6d0-4d8a-a54c-cc8c0fe67ac5

Trueman, Clive N.G., Behrensmeyer, Anna K., Tuross, Noreen and Weiner, Steve (2004) Mineralogical and compositional changes in bones exposed on soil surfaces in Amboseli National Park, Kenya: diagenetic mechanisms and the role of sediment pore fluids. Journal of Archaeological Science, 31 (6), 721-739. (doi:10.1016/j.jas.2003.11.003).

Record type: Article

Abstract

Bones exposed on tropical savannah grasslands of Amboseli National Park, Kenya undergo extensive post-mortem alteration within 40 years. A combined analytical approach involving TEM microscopy, trace metal analysis, FTIR spectroscopy, and petrographic analysis has revealed a complex, dynamic diagenetic environment operating within exposed bones, driven by evaporative transport of soil water from the bone/soil interface to the upper exposed surface of the bone. This process results in extensive bone/soil-water interaction, and is responsible for increases in the concentrations of trace elements such as Ba and La of 100 – >1000% within 15 years. The maximum and mean size of bone crystallites increases with continued exposure. This change in mean crystallite length is correlated positively with increases in bone crystallinity, which in turn is associated with degradation of the bone protein. Microbial decomposition is rarely observed in the Amboseli bones, but where present resulted in severe dissolution–reprecipitation of bone mineral. Many bones showed extensive permineralization of the larger vascular spaces with calcite and barite and, to a lesser extent, crandallite. Permineralization of unburied bones may account for 95% reduction in macro (micron–millimeter scale) porosity in the bone within 2 years of death.
We produce a model for pre-burial diagenesis of bone in arid tropical environments that highlights extensive alteration of bone chemistry within 1–40 years post-mortem.

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More information

Published date: June 2004
Keywords: bone, diagenesis, crystallinity, collagen, trace elements, permineralization, amboseli

Identifiers

Local EPrints ID: 37979
URI: http://eprints.soton.ac.uk/id/eprint/37979
ISSN: 0305-4403
PURE UUID: 5c2a0e05-6f7c-4c3b-a777-001f7d5dcb0b
ORCID for Clive N.G. Trueman: ORCID iD orcid.org/0000-0002-4995-736X

Catalogue record

Date deposited: 26 May 2006
Last modified: 16 Mar 2024 03:35

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Contributors

Author: Anna K. Behrensmeyer
Author: Noreen Tuross
Author: Steve Weiner

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