HOMININ EVOLUTION IN SETTINGS OF STRONG ENVIRONMENTAL VARIABILITY
Examples will show how these criteria are fulfilled relevant to variability selection explanations of the Plio-Pleistocene Oldowan expansion and the middle Pleistocene transition from Acheulean to Middle Stone Age. Especially relevant to these explanations is the framework of alternating high- and low-climate variability in tropical Africa, with key events in hominin evolution concentrated in the predicted longest intervals of high climate variability. A synthesis of environmental indicators cautions against an exclusive focus on the end members of environmental fluctuation (driest or wettest, warmest or coolest), and argues for the impact of the entire range of amplified variability in shaping evolutionary change. New theoretical modeling and simulations, furthermore, point to how adaptive versatility is selected as environmental variability is amplified. A relatively novel view thus emerges in which important changes in stone technology, life history, sociality, and other aspects of hominin behavior are understood as adaptive responses to heightened habitat instability.
This research has been supported by the Smithsonian’s Human Origins Program, the Peter Buck Fund for Human Origins Research, and the NSF HOMINID Program (BCS-0128511), with fieldwork permits and logistics supported by the National Museums of Kenya.