Taphonomy and diagenesis of submerged bone: An experimental approach

Bone taphonomy and diagenesis contribute to anthropological analysis in forensic investigations by attempting to reconstruct the relationship between human cadaveric remains and their postmortem depositional environment. The rare aquatic taphonomic experiments have been delivering conflicting results on the influence of time and the environment on the decay of bone and teeth, especially considering that the main diagenetic processes can lead to fragmentation, progressive dissolution or fossilization. The aim of this experimental, quantitative, randomized and controlled 2-year study was to analyse the taphonomy and diagenesis of submerged terrestrial mammalian bones to achieve a more accurate estimation of both the post-mortem interval (PMI) and the post-mortem submersion interval (PMSI) in the short term. Three parameters of bone diagenesis, the Oxford Histological Index (OHI), the total porosity and the collagen content of cortical bone were analysed by MicroCT Scan, bright-field Light Microscopy (Picrosirius Red stain), Scanning Electron Microscopy (SEM) and Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) on 75 sheep femurs and tibias placed in four distinct types of environment (natural saltwater, natural freshwater, an artificial seawater solution and exposed to the air) vs. non-exposed controls. LA-ICP-MS was soon discontinued because no measurable changes of the elemental profiles could be detected. Multivariate statistical analysis was applied to the collected data. The macroscopical preservation was consistently excellent (OHI=5). The total porosity and the degradation of collagen were greater underwater than in subaerial exposure, whereas demineralization zones and bioerosion tunnelling appeared after 12 months in the air-exposed samples only. Underwater, the continuous movement, the correlated abrasion by sand and sediment and the constant alkaline pH (≥ 8) can explain the progressive removal of the mineral component and the subsequent exposure of collagen to bioeroders and chemical hydrolysis. On land, the same process occurs at a slower rate on account of the seasonality of the water flow, however, the action of the more abundant and diversified species of bioeroding microorganisms appears more efficient. Despite some limitations, this study indicates that three parameters of bone diagenesis can predict the depositional environment of terrestrial mammalian bone characterized by a PMI and/or PMSI of at least 12 months.