Marques M P M, Batista de Carvalho L A E, Gonçalves D, Cunha E, Parker S F
Molecular Physical-Chemistry R&D Unit, Department of Chemistry, University of Coimbra, 3004-535 Coimbra, Portugal.
Department of Life Sciences, University of Coimbra, 3000-456 Coimbra, Portugal.
R Soc Open Sci. 2021 Oct 27;8(10):210774. doi: 10.1098/rsos.210774. eCollection 2021 Oct.
This study aims to analyse human bones exposed to low/medium temperatures (200-650°C) under experimentally controlled conditions, both oxidizing and reducing, using complementary optical and neutron vibrational spectroscopy techniques. Clear differences were observed between the aerobically and anaerobically heated bones. The organic constituents disappeared at lower temperatures for the former ( 300°C), while they lingered for higher temperatures in anaerobic environments ( 450-550°C). Unsaturated non-graphitizing carbon species (chars) were detected mainly for anaerobically heated samples, and cyanamide formation occurred only at 650°C in reducing settings. Overall, the main changes were observed from 300 to 400°C in anaerobic conditions and from 450 to 500°C in aerobic environments. The present results enabled the identification of specific spectroscopic biomarkers of the effect of moderate temperatures (less than or equal to 650°C) on human bone, thus contributing to a better characterization of forensic and archaeological skeletal remains subject to heating under distinct environmental settings. In particular, these data may provide information regarding cannibalism or ancient bone boiling and defleshing rituals.
本研究旨在利用互补的光学和中子振动光谱技术,在实验控制的氧化和还原条件下,分析暴露于低温/中温(200 - 650°C)的人类骨骼。在有氧和无氧加热的骨骼之间观察到明显差异。对于前者(300°C),有机成分在较低温度下消失,而在厌氧环境中(450 - 550°C),它们在较高温度下仍存在。不饱和非石墨化碳物种(炭)主要在无氧加热的样品中检测到,并且氰胺的形成仅在还原环境中的650°C时发生。总体而言,在厌氧条件下,主要变化在300至400°C之间观察到,而在有氧环境中则在450至500°C之间。目前的结果能够识别中等温度(小于或等于650°C)对人类骨骼影响的特定光谱生物标志物,从而有助于更好地表征在不同环境条件下受热的法医和考古骨骼遗骸。特别是,这些数据可能提供有关同类相食或古代骨头煮沸和去肉仪式的信息。