Research Projects in the Department of Archaeology

Tracking the early emergence of derived Homo-like cerebral features in the hominin fossil record can be expected to contribute to an understanding of the timing (i.e., chronology) and mode (i.e., process) of critical brain changes. Because brain tissue is not preserved in the fossil record, studies of hominin brain evolution focus on brain endocasts (i.e., replicas of the inner table of the bony braincase).

How did our ancestors walk? Perhaps the greatest challenge that this question has posed in the past, is the lack of methodological applications in which no study has previously reconstructed how our ancestors moved using biomechanical modelling techniques. We need to consider not just individual bones when reconstructing movement, but to look at the full body to begin to tell the story of our ancestors’ movement. Muscles animate our body, permitting us to walk, run and even dance. We must reconstruct the muscles of the body to understand ancestral locomotion.

Despite recent progress in molecular analyses and the constant increase of the hominin remains in the fossil record, the chronological, geographical and evolutionary context of the emergence of the genus Homo remains largely debated. More importantly, the identity of our direct ancestors and assessment of the adaptations characterizing our genus remain unclear.

Traumatic death affects our daily life, but how did traumatic mortality affect human behaviour from an evolutionary perspective? TRAUMOBITA aims to understand how traumatic mortality among prehistoric humans shaped our behaviour during the Late Pleistocene to the Middle Holocene. Confirming that how we died had an enormous influence on our ancestors and represents an enormous change in how we understand human societies.

As the complex mosaic of Quaternary human lineages across and beyond Africa becomes increasingly apparent, an accurate chronology is critical to disentangle the patterns and process, particularly those that link human evolution to palaeoenvironmental and climatic change.