Bone diagenesis at the micro-scale: Bone alteration patterns during multiple burial phases at Al Khiday (Khartoum, Sudan) between the Early Holocene and the II century AD

Histological analysis is widely applied to archaeological and fossil bones in order to identify diagenetic changes in bone microstructure. Diagenetic processes, affecting bones from the body deposition to the discovery, strongly depend on environmental conditions; therefore the study of diagenetic alterations provides valuable information on the taphonomic history of bones and on their burial environment. Histological analysis was performed on 58 samples of human compact bone found at Al Khiday (Khartoum, Sudan), a multi-stratified archaeological site that revealed a cemetery with distinct burial phases dating from the Early Holocene to the II century AD. The well-defined archaeological context provides a set of bone samples belonging to the same site but buried in different phases and under different environmental conditions: Central Sudan was characterised by a humid environment with seasonal swamps and palaeo-lakes in the Early Holocene, while in the II century AD the environmental conditions were more similar to the current arid climate of the Sub-Saharan belt. ng electron microscopy (SEM) and high-resolution X-ray computed micro-tomography (μ-CT) analysis revealed extensive bacterial and fungal attack, and secondary phases precipitation and dissolution in the samples. The analysis of textural relationships between each diagenetic feature enabled to establish a relative chronological sequence of events acting during burial. Moreover, different patterns of diagenetic alterations were observed for burial phases of different ages, proving a strong relationship between diagenesis and environmental conditions.