Physicochemical changes in bone bioapatite during the late postmortem interval pre- and post-burning

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dc.contributor.authorVégh, Emese I.
dc.contributor.authorMarquez-Grant, Nicholas
dc.contributor.authorSchulting, Rick J.
dc.date.accessioned2022-04-14T09:20:56Z
dc.date.available2022-04-14T09:20:56Z
dc.date.issued2022-02-21
dc.description.abstractPostmortem chemical transformation of bone bioapatite can take place during early diagenesis resulting in a more thermodynamically stable mineral phase. This paper examines the impact of a 1-year postmortem interval on unburnt and burnt bone’s structural and chemical alterations. This question is of importance for the reconstruction of funerary practices involving cremation in the archaeological record, as well as forensic anthropological investigations. Fleshed pig (Sus scrofa) tibiae were left exposed in a field, then collected at 14, 34, 91, 180, 365-day intervals prior to being burnt in an outdoor fire (≤750 °C bone temperature). Fresh (fleshed) tibiae acted as unburnt and burnt controls. Also included in the study were two cremated human bone fragments from Middle/Late Neolithic (ca. 3300–2500 cal BC) Ireland. Samples were analysed for major and trace elements by wavelength dispersive electron microprobe analyser (EMP-WDS) and molecular structures by Fourier Transform Infrared Spectroscopy (FTIR). Linear regression, PCA, LDA, and MANOVA were performed for statistical analysis. Results indicate that the concentrations of elements associated with extracellular fluid (K, Na, Cl) change with the postmortem interval (PMI) and survive burning. K values under 0.07 ± 0.01 wt% in inner and mid-cortical zones of burnt bones suggest that bones were not burnt immediately after death. Using this criterion, results from the archaeological samples would indicate a PMI of at least weeks to months prior to cremation. Ca, P, Fe, Al, Si, and Sr are not significantly altered with burning, and Fe, Al, Si, Sr are also unaffected by the PMI. In unburnt bones increased crystallinity and carbonate loss are detectable in <1 year, but both are obscured by burning. Structurally, the carbonate to phosphate ratio (C/P), the phosphate high temperature (PHT), and cyanamide to phosphate (CN/P) are the most useful ratios for discriminating between unburnt and burnt bones.en_UK
dc.identifier.citationVégh EI, Márquez-Grant N, Schulting RJ. (2022) Physicochemical changes in bone bioapatite during the late postmortem interval pre- and post-burning, Applied Spectroscopy, Volume 76, Issue 9, September 2022, pp. 1080–1099en_UK
dc.identifier.eissn1943-3530
dc.identifier.issn0003-7028
dc.identifier.urihttps://doi.org/10.1177/00037028221085600
dc.identifier.urihttp://dspace.lib.cranfield.ac.uk/handle/1826/17769
dc.language.isoenen_UK
dc.publisherSageen_UK
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectcremationen_UK
dc.subjectelectron microprobeen_UK
dc.subjectFTIRen_UK
dc.subjectpotassiumen_UK
dc.subjecttaphonomyen_UK
dc.titlePhysicochemical changes in bone bioapatite during the late postmortem interval pre- and post-burningen_UK
dc.typeArticleen_UK

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