Pliocene Hominin Dispersal to southern Africa:

Choice or Chance?

Modern humans migrated to colder regions out of Africa during the Pleistocene (Out-of-Africa). However, evidence suggests that early hominins already inhabited temperate zones in South Africa millions of years earlier, i.e. during the Pliocene. PLIODIS will explore the possible causes for this pan-African distribution of early hominins and how it may have shaped the course of our evolutionary history. To do so, we will reconstruct the geomorphological changes in the Kalahari/proto-Limpopo basin and the Zambezian region, explore the climatic and vegetation changes in deep time and examine the hominin fossil record against this ecological backdrop.


PLIODIS will tests several hypotheses: that early hominin ranges in East Africa expanded and contracted with changing wet and dry phases; that shifts in dispersal corridors led to intermittent gene flow between eastern African and southern African populations; and that tectonic changes eventually turned the Zambezi River into a significant barrier, leading to the endemism among South African hominins.

Three Key Questions

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Landscape

How did changes in drainage systems and landscape topography shape conncectivity between eastern and southern Africa, thereby creating/closing potential dispersal corridors between the regions?

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Environment

What role did climate shifts and vegetation change play in the opening or closing of these potential migration routes?

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Biology

How did early hominins respond to ecological changes? What was the population dynamics between eastern and southern African hominins (e.g., drift, hybridization, endemism)?