1. 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
- Author
-
Elisavet Stamataki, Amanda Sengelov, Eugène Warmenbol, Charlotte Sabaux, Philippe Claeys, Barbara Veselka, Martine Vercauteren, Rica Annaert, Ioannis Kontopoulos, Marta Hlad, Kevin Salesse, Christophe Snoeck, Mathieu Boudin, Giacomo Capuzzo, Sarah Dalle, Guy De Mulder, Georges Verly, De la Préhistoire à l'Actuel : Culture, Environnement et Anthropologie (PACEA), Centre National de la Recherche Scientifique (CNRS)-Université de Bordeaux (UB), Université libre de Bruxelles (ULB), Vrije Universiteit Brussel (VUB), University of Copenhagen = Københavns Universitet (KU), Sorbonne Université - Faculté des Lettres - UFR Histoire de l'art et archéologie (SU UFR HAA), Sorbonne Université (SU), Institut Royal du Patrimoine Artistique, Universiteit Gent = Ghent University [Belgium] (UGENT), Multidisciplinary Archaeological Research Institute, Analytical, Environmental & Geo-Chemistry, History, Archeology, Arts, Philosophy and Ethics, Faculty of Arts and Philosophy, Earth System Sciences, Chemistry, and Bondioli, Luca
- Subjects
Swine ,[SDV]Life Sciences [q-bio] ,WOOD CONSTITUENTS ,Psychologie appliquée ,Carbonates ,Combustion ,Social Sciences ,Oxygen Isotopes ,Exothermic Reactions ,01 natural sciences ,Oxygen ,Biochemistry ,Isotopes of oxygen ,Apatite ,OXYGEN ,Animal Products ,Spectroscopy, Fourier Transform Infrared ,Medicine and Health Sciences ,0601 history and archaeology ,Bone mineral ,Mammals ,Carbon Isotopes ,Multidisciplinary ,Isotope ,δ13C ,Feet ,Chemical Reactions ,Eukaryota ,APATITE ,Agriculture ,06 humanities and the arts ,Limiting ,Sciences bio-médicales et agricoles ,Stable isotope ,STRUCTURAL CARBONATE ,Body Remains ,Chemistry ,Leather ,Archaeology ,Environmental chemistry ,visual_art ,Vertebrates ,Physical Sciences ,visual_art.visual_art_medium ,Medicine ,Legs ,Anatomy ,Biologie ,Research Article ,Chemical Elements ,010506 paleontology ,[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory ,δ18O ,Science ,chemistry.chemical_element ,Bone and Bones ,CALCINED BONES ,COMBUSTION ,Cadaver ,Animals ,Humans ,0105 earth and related environmental sciences ,060101 anthropology ,History and Archaeology ,Organisms ,Chemical Compounds ,Biology and Life Sciences ,Proteins ,RATIOS ,TRANSFORMATION ,Shoes ,Cremation ,chemistry ,FTIR ,Body Limbs ,Amniotes ,BODIES ,Zoology ,Collagens ,CRYSTALLINITY - 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., SCOPUS: ar.j, info:eu-repo/semantics/published
- Published
- 2021
- Full Text
- View/download PDF