Pliocene Hominin Dispersal to southern Africa: Choice or Chance?
This project investigates the evolutionary adaptability of early hominins in South Africa through geomorphological, palaeoecological, and fossil analyses to understand their dispersal and diversity.
Projectdetails
Introduction
Modern humans are unique in their ability to adapt to, and to thrive in, different environments. This trait facilitated their dispersal out-of-Africa to higher latitudes, i.e., to temperate and seasonal habitats, during the Pleistocene. However, there are Plio-Pleistocene hominins at higher latitudes in South Africa (SA) from ~3.7 Ma onwards.
Research Questions
Did human behavioural/physiological flexibility evolve early in our evolutionary history? Alternatively, did Pliocene hominins occupy such temperate zones due to different palaeoclimatic conditions in deep time and/or due to stochastic events?
Project Objectives
To untangle these questions, this project will:
- Determine the geomorphological and palaeoecological changes in the Kalahari/proto-Limpopo basin.
- Create dynamic palaeo-precipitation/-vegetation models from various archives.
- Carry out detailed anatomical, functional, and morphometric analyses of the hominin fossil record.
- Combine the datasets to appraise species diversity (functional adaptations), gene flow (hybridization), and dispersal scenarios (palaeobiogeography).
Working Hypotheses
Three key working hypotheses underlie the proposal:
- >2.6 Ma: East African (EA) hominin ranges expanded/contracted in accord with wet and dry phases; periodically, the southernmost populations became reproductively isolated. Early SA hominins represent descendants of Australopithecus anamensis and Australopithecus afarensis, respectively.
- ~2.6-1.5 Ma: With the onset of the Northern Hemisphere Glaciation and the re-organisation of the drainage pattern within the Kalahari basin, dispersal corridors repeatedly closed (vicariance) and opened, resulting in intermittent levels of gene flow (i.e., hybridization) between EA and SA hominins.
- <~1.5 Ma: Tectonic and hydrographic changes led to the Zambezi River becoming a powerful barrier during the Pleistocene. SA hominins younger than 1.5 Ma are likely the result of endemism; competitive exclusion amongst these hominins resulted in the exploitation of distinct ecological niches.
Financiële details & Tijdlijn
Financiële details
Subsidiebedrag | € 2.499.248 |
Totale projectbegroting | € 2.499.248 |
Tijdlijn
Startdatum | 1-8-2024 |
Einddatum | 31-7-2029 |
Subsidiejaar | 2024 |
Partners & Locaties
Projectpartners
- SENCKENBERG GESELLSCHAFT FUR NATURFORSCHUNGpenvoerder
- UNIVERSITY OF THE WITWATERSRAND JOHANNESBURG
Land(en)
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