human evolution Hominin habitats

The section Background and beginnings in the Miocene describes certain global climatic changes that reduced forested areas and induced more open terrestrial biomes during the Late Miocene Epoch (11.2–5.3 mya). During the succeeding Pliocene Epoch (5.3–1.8 mya) these changes only intensified. In Africa, primates diversified. In Eurasia, contrarily, hominins disappeared by the beginning of the Pliocene. The only descendants of Late Miocene primates in Asia are the extinct Early-Middle Pleistocene Gigantopithecus blacki of southern China and northern Vietnam and the present-day orangutans and gibbons of South and Southeast Asia.

It is reasonable to expect that the increased variety and shifting distribution of African biomes stimulated new hominin lifeways, some of which led to survival and others of which did not. Insofar as habitats have been (or can be) discerned from evidence found with the Pliocene hominin species, hominins inhabited a variety of biomes in eastern, central, and southern Africa. In central Ethiopia, Ardipithecus ramidus is associated with faunal and floral remains indicating a woodland habitat. Later remains, in northern Ethiopia, indicate Australopithecus afarensis inhabited a mosaic of riverine forest, lowland woodland, savanna, and dry bushland. In northern Kenya Australopithecus anamensis lived in dry open woodland or bushland with a gallery forest along a nearby river. In central Chad the northernmost and westernmost species, Australopithecus bahrelghazali, appears to have lived in a mosaic of open and wooded biomes near a river. Mammalian fossils from Lomekwi, northern Kenya, indicate that Kenyanthropus platyops inhabited a relatively well-watered area of forest or closed woodland or the forest edge between them. The habitat of the 3.5-million-year-old Laetoli hominins in northern Tanzania was arguably a mosaic of open grassland and more-closed woodland. The area may have been wetter than it is now. No permanent water source has been identified for the Laetoli area during the Pliocene. Later in the Pliocene, Australopithecus garhi was active on broad, grassy plains bordering a lake in central Ethiopia. Models of the habitat of Australopithecus africanus, based on fauna from the two major South African cave sites—Sterkfontein and Makapansgat—stress closed-canopy wooded conditions: either dry woodland with grasslands nearby or subtropical forest. During the tenures of H. habilis and P. boisei at Olduvai Gorge, northern Tanzania, the climate changed from moist to dry and again to moist before a long dry span that began two million years ago. Specimens of both of these Olduvai hominins are mostly from the shore of an ancient saline, alkaline lake. At Koobi Fora, northern Kenya, specimens of H. habilis have been more commonly found in lake-margin deposits, while those of P. boisei are equally common in river and lake-margin sediments. Fossil pollen indicates that highland forest was nearby and that near the lake there were grassy areas and dense woodland and shrubland.

At Konso, southern Ethiopia, P. boisei lived in a grassland habitat. Elsewhere in eastern Africa, P. aethiopicus was associated with closed habitats. The South African cave sites (Swartkrans, Kromdraai, and Drimolen) of P. robustus are associated with open and even arid habitats, but these may not reflect its actual foraging preference.

One of the more profound effects of Pliocene habitat changes was honing the energy-conservant bipedal stride at the time that Homo species deployed out of Africa and into Eurasia. Shortly after Homo evolved in Africa, some species ventured to temperate biomes in Eurasia and then to subtropical and tropical biomes in South and Southeast Asia. Subsequently there was a migration back to Africa, perhaps as early as 1.8–0.9 mya. This hemispheric dispersion of Homo is associated with elaboration of stone tool kits, increased brain size, and reduction in size of the jaws and teeth—all of which are the subject of the next section.