On the ecological scenario of the first hominin dispersal out of Africa

The archaeopaleontological site of Dmanisi in Georgia, dated to ∼1.8 Ma, provides evidence on the first hominin dispersal out of Africa, while the sites of Barranco León and Fuente Nueva-3 in Spain, dated to ∼1.4 Ma, record the earliest hominin settlements in Europe. However, a number of issues related to the dispersal route, the climatic conditions and the ecological scenario of this dispersal event are subject to debate. In a recent paper in L’anthropologie, Agustí and Lordkipanidze (2019) proposed an alternative scenario for the arrival of hominins in the Caucasus, which they conceived as a forest refugium area during the Early Pleistocene, and discarded that their dispersal coincided with that of other members of the Ethiopian and Asian faunas, like the sabertooth Megantereon whitei or the giant hyena Pachycrocuta brevirostris. Our review of these issues suggests that: (i) the elongated sabers and reduced postcanine teeth of African M. whitei limited the ability of this predator to process the prey carcass, which resulted in scavengeable resources for the Dmanisi hominins; (ii) the mass estimate in excess of 100 kg obtained for the trochlear perimeter of the distal humerus of the hyena from Dmanisi shows that it can be confidently ascribed to the genus Pachycrocuta; (iii) the postcranial anatomy of the Dmanisi hominins was not advantageous for scavenging tree-stored prey; (iv) the laterally flattened upper canines of M. whitei could not withstand the loads that would result from climbing a prey carcass into a tree; (v) paleobotanical analyses suggest a temperate grassland ecosystem in Dmanisi, not dominant forest conditions, with enhanced aridity in the level of hominin occupation; (vi) similarly, the low frequency of arboreal pollen in the Levantine Corridor at ∼1.8 Ma points to more arid conditions than today in this area; (vii) many archaeopaleontological sites of the Rift Valley and its extension towards the Red Sea, the Levant and the Caucasus show evidence of tectonic, volcanic and/or hydrothermal events; and (viii) the delay of 400 ka in the arrival of hominins in Western Europe did not result from a lower availability of scavengeable resources