These boots are made for burnin’: Inferring the position of the corpse and the presence of leather footwears during cremation through isotope (δ13C, δ18O) and infrared (FTIR) analyses of experimentally burnt skeletal remains

Research output: Contribution to journalJournal articleResearchpeer-review

Standard

These boots are made for burnin’ : Inferring the position of the corpse and the presence of leather footwears during cremation through isotope (δ13C, δ18O) and infrared (FTIR) analyses of experimentally burnt skeletal remains. / Salesse, Kevin; Stamataki, Elisavet; Kontopoulos, Ioannis; Verly, Georges; Annaert, Rica; Boudin, Mathieu; Capuzzo, Giacomo; Claeys, Philippe; Dalle, Sarah; Hlad, Marta; de Mulder, Guy; Sabaux, Charlotte; Sengeløv, Amanda; Veselka, Barbara; Warmenbol, Eugène; Vercauteren, Martine; Snoeck, Christophe.

In: PLoS ONE, Vol. 16, No. 10, e0257199, 2021.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Salesse, K, Stamataki, E, Kontopoulos, I, Verly, G, Annaert, R, Boudin, M, Capuzzo, G, Claeys, P, Dalle, S, Hlad, M, de Mulder, G, Sabaux, C, Sengeløv, A, Veselka, B, Warmenbol, E, Vercauteren, M & Snoeck, C 2021, 'These boots are made for burnin’: Inferring the position of the corpse and the presence of leather footwears during cremation through isotope (δ13C, δ18O) and infrared (FTIR) analyses of experimentally burnt skeletal remains', PLoS ONE, vol. 16, no. 10, e0257199. https://doi.org/10.1371/journal.pone.0257199

APA

Salesse, K., Stamataki, E., Kontopoulos, I., Verly, G., Annaert, R., Boudin, M., Capuzzo, G., Claeys, P., Dalle, S., Hlad, M., de Mulder, G., Sabaux, C., Sengeløv, A., Veselka, B., Warmenbol, E., Vercauteren, M., & Snoeck, C. (2021). These boots are made for burnin’: Inferring the position of the corpse and the presence of leather footwears during cremation through isotope (δ13C, δ18O) and infrared (FTIR) analyses of experimentally burnt skeletal remains. PLoS ONE, 16(10), [e0257199]. https://doi.org/10.1371/journal.pone.0257199

Vancouver

Salesse K, Stamataki E, Kontopoulos I, Verly G, Annaert R, Boudin M et al. These boots are made for burnin’: Inferring the position of the corpse and the presence of leather footwears during cremation through isotope (δ13C, δ18O) and infrared (FTIR) analyses of experimentally burnt skeletal remains. PLoS ONE. 2021;16(10). e0257199. https://doi.org/10.1371/journal.pone.0257199

Author

Salesse, Kevin ; Stamataki, Elisavet ; Kontopoulos, Ioannis ; Verly, Georges ; Annaert, Rica ; Boudin, Mathieu ; Capuzzo, Giacomo ; Claeys, Philippe ; Dalle, Sarah ; Hlad, Marta ; de Mulder, Guy ; Sabaux, Charlotte ; Sengeløv, Amanda ; Veselka, Barbara ; Warmenbol, Eugène ; Vercauteren, Martine ; Snoeck, Christophe. / These boots are made for burnin’ : Inferring the position of the corpse and the presence of leather footwears during cremation through isotope (δ13C, δ18O) and infrared (FTIR) analyses of experimentally burnt skeletal remains. In: PLoS ONE. 2021 ; Vol. 16, No. 10.

Bibtex

@article{4096032926ca4434b173cc3cdb4dcc45,
title = "These boots are made for burnin{\textquoteright}: Inferring the position of the corpse and the presence of leather footwears during cremation through isotope (δ13C, δ18O) and infrared (FTIR) analyses of experimentally burnt skeletal remains",
abstract = "Cremation is a complex mortuary practice, involving a number of activities of the living towards the dead before, during, and after the destruction of the bodily soft tissues by fire. The limiting information concerning these behavioral patterns obtained from the pyre remains and/or cremation deposits prevents the reconstruction of the handling of the corpse during the burning process. This pioneering study tries to determine the initial positioning of the corpse in the pyre and assess whether the deceased was wearing closed leather shoes during cremation through isotopic (δ13C, δ18O) and infrared (ATR-FTIR) analyses of experimentally burnt pig remains, used as a proxy for humans. The results obtained show that both the position of feet on or within the pyre and the presence of footwears may moderately-to-highly influence the oxygen isotope ratios of bone apatite carbonates and the cyanamide content of calcined bone in certain situations. By forming a protective layer, shoes appear to temporarily delay the burning of the underlying pig tissues and to increase the heat-shielding effect of the soft tissues protecting the bone mineral fraction. In such case, bioapatite bone carbonates exchange oxygen with a relatively more 18O-depleted atmosphere (due to the influence of lignin-derived oxygen rather than cellulose-derived oxygen), resulting in more pronounced decrease in the δ18Ocarb values during burning of the shoed feet vs. unshoed feet. The shift observed here was as high as 2.5. A concomitant isotopic effect of the initial location of the feet in the pyres was also observed, resulting in a top-to-bottom decrease difference in the δ18Ocarb values of shoed feet of about 1.4 between each deposition level tested. Finally, the presence of cyanamide (CN/P 0.02) seems to be indicative of closed footwear since the latter creates favorable conditions for its incorporation into bone apatite.",
author = "Kevin Salesse and Elisavet Stamataki and Ioannis Kontopoulos and Georges Verly and Rica Annaert and Mathieu Boudin and Giacomo Capuzzo and Philippe Claeys and Sarah Dalle and Marta Hlad and {de Mulder}, Guy and Charlotte Sabaux and Amanda Sengel{\o}v and Barbara Veselka and Eug{\`e}ne Warmenbol and Martine Vercauteren and Christophe Snoeck",
note = "Publisher Copyright: Copyright: {\textcopyright} 2021 Salesse et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.",
year = "2021",
doi = "10.1371/journal.pone.0257199",
language = "English",
volume = "16",
journal = "PLoS ONE",
issn = "1932-6203",
publisher = "Public Library of Science",
number = "10",

}

RIS

TY - JOUR

T1 - These boots are made for burnin’

T2 - Inferring the position of the corpse and the presence of leather footwears during cremation through isotope (δ13C, δ18O) and infrared (FTIR) analyses of experimentally burnt skeletal remains

AU - Salesse, Kevin

AU - Stamataki, Elisavet

AU - Kontopoulos, Ioannis

AU - Verly, Georges

AU - Annaert, Rica

AU - Boudin, Mathieu

AU - Capuzzo, Giacomo

AU - Claeys, Philippe

AU - Dalle, Sarah

AU - Hlad, Marta

AU - de Mulder, Guy

AU - Sabaux, Charlotte

AU - Sengeløv, Amanda

AU - Veselka, Barbara

AU - Warmenbol, Eugène

AU - Vercauteren, Martine

AU - Snoeck, Christophe

N1 - Publisher Copyright: Copyright: © 2021 Salesse et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

PY - 2021

Y1 - 2021

N2 - Cremation is a complex mortuary practice, involving a number of activities of the living towards the dead before, during, and after the destruction of the bodily soft tissues by fire. The limiting information concerning these behavioral patterns obtained from the pyre remains and/or cremation deposits prevents the reconstruction of the handling of the corpse during the burning process. This pioneering study tries to determine the initial positioning of the corpse in the pyre and assess whether the deceased was wearing closed leather shoes during cremation through isotopic (δ13C, δ18O) and infrared (ATR-FTIR) analyses of experimentally burnt pig remains, used as a proxy for humans. The results obtained show that both the position of feet on or within the pyre and the presence of footwears may moderately-to-highly influence the oxygen isotope ratios of bone apatite carbonates and the cyanamide content of calcined bone in certain situations. By forming a protective layer, shoes appear to temporarily delay the burning of the underlying pig tissues and to increase the heat-shielding effect of the soft tissues protecting the bone mineral fraction. In such case, bioapatite bone carbonates exchange oxygen with a relatively more 18O-depleted atmosphere (due to the influence of lignin-derived oxygen rather than cellulose-derived oxygen), resulting in more pronounced decrease in the δ18Ocarb values during burning of the shoed feet vs. unshoed feet. The shift observed here was as high as 2.5. A concomitant isotopic effect of the initial location of the feet in the pyres was also observed, resulting in a top-to-bottom decrease difference in the δ18Ocarb values of shoed feet of about 1.4 between each deposition level tested. Finally, the presence of cyanamide (CN/P 0.02) seems to be indicative of closed footwear since the latter creates favorable conditions for its incorporation into bone apatite.

AB - Cremation is a complex mortuary practice, involving a number of activities of the living towards the dead before, during, and after the destruction of the bodily soft tissues by fire. The limiting information concerning these behavioral patterns obtained from the pyre remains and/or cremation deposits prevents the reconstruction of the handling of the corpse during the burning process. This pioneering study tries to determine the initial positioning of the corpse in the pyre and assess whether the deceased was wearing closed leather shoes during cremation through isotopic (δ13C, δ18O) and infrared (ATR-FTIR) analyses of experimentally burnt pig remains, used as a proxy for humans. The results obtained show that both the position of feet on or within the pyre and the presence of footwears may moderately-to-highly influence the oxygen isotope ratios of bone apatite carbonates and the cyanamide content of calcined bone in certain situations. By forming a protective layer, shoes appear to temporarily delay the burning of the underlying pig tissues and to increase the heat-shielding effect of the soft tissues protecting the bone mineral fraction. In such case, bioapatite bone carbonates exchange oxygen with a relatively more 18O-depleted atmosphere (due to the influence of lignin-derived oxygen rather than cellulose-derived oxygen), resulting in more pronounced decrease in the δ18Ocarb values during burning of the shoed feet vs. unshoed feet. The shift observed here was as high as 2.5. A concomitant isotopic effect of the initial location of the feet in the pyres was also observed, resulting in a top-to-bottom decrease difference in the δ18Ocarb values of shoed feet of about 1.4 between each deposition level tested. Finally, the presence of cyanamide (CN/P 0.02) seems to be indicative of closed footwear since the latter creates favorable conditions for its incorporation into bone apatite.

U2 - 10.1371/journal.pone.0257199

DO - 10.1371/journal.pone.0257199

M3 - Journal article

C2 - 34644308

AN - SCOPUS:85117229596

VL - 16

JO - PLoS ONE

JF - PLoS ONE

SN - 1932-6203

IS - 10

M1 - e0257199

ER -

ID: 285518125