PLIODIS
Financiado
Pliocene Hominin Dispersal to southern Africa: Choice or Chance?
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 Pleisto...
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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Duración del proyecto: 59 meses
Fecha Inicio: 2024-08-01
Fecha Fin: 2029-07-31
Fecha Fin: 2029-07-31
Línea de financiación: concedida
El organismo HORIZON EUROPE notifico la concesión del proyecto el día 2024-08-01
Línea de financiación objetivo
El proyecto se financió a través de la siguiente ayuda:
ERC-2023-ADG:
ERC ADVANCED GRANTS
Cerrada
hace 1 año
Presupuesto
El presupuesto total del proyecto asciende a
2M€
Líder del proyecto
SENCKENBERG GESELLSCHAFT FUR NATURFORSCHUNG
No se ha especificado una descripción o un objeto social para esta compañía.
Perfil tecnológico
TRL
4-5
Perfil tecnológico
TRL
4-5