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Pliocene Hominin Dispersal to southern Africa: Choice or Chance?

Project description

Understanding hominin dispersal to southern Africa in the Plio-Pleistocene

Modern humans migrated to colder regions out of Africa during the Pleistocene, but evidence suggests that early hominins inhabited temperate zones in South Africa millions of years ago. The ERC-funded PLIODIS project will explore changes in the Kalahari/proto-Limpopo basin and examine the hominin fossil record to better understand species diversity, gene flow, and dispersal patterns in deep time. The project will test 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 East African and South African populations, and that tectonic changes eventually turned the Zambezi River into a significant barrier, prompting South African hominins to adapt to distinct ecological niches.

Objective

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 ~3.7Ma onwards. 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? To untangle these questions this project will: (1) determine the geomorphological and palaeoecological changes in the Kalahari/proto-Limpopo basin, (2) create dynamic palaeo-precipitation/-vegetation models from various archives, (3) carry out detailed anatomical, functional and morphometric analyses of the hominin fossil record and (4) combine the datasets to appraise species diversity (functional adaptations), geneflow (hybridization) and dispersal scenarios (palaeobiogeography). 3 key working hypotheses underlie the proposal:
1. >2.6Ma 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. ~2.6-1.5Ma 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.
3. <~1.5Ma Tectonic and hydrographic changes led to the Zambezi River becoming a powerful barrier during the Pleistocene. SA hominins younger than 1.5Ma are likely the result of endemism; competitive exclusion amongst these hominins resulted in exploitation of distinct ecological niches

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Call for proposal

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(opens in new window) ERC-2023-ADG

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Host institution

SENCKENBERG GESELLSCHAFT FUR NATURFORSCHUNG
Net EU contribution

Net EU financial contribution. The sum of money that the participant receives, deducted by the EU contribution to its linked third party. It considers the distribution of the EU financial contribution between direct beneficiaries of the project and other types of participants, like third-party participants.

€ 1 955 216,25
Address
SENCKENBERGANLAGE 25
60325 FRANKFURT
Germany

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Region
Hessen Darmstadt Frankfurt am Main, Kreisfreie Stadt
Activity type
Other
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Total cost

The total costs incurred by this organisation to participate in the project, including direct and indirect costs. This amount is a subset of the overall project budget.

€ 1 955 216,25

Beneficiaries (2)

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