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Several expansions of populations of archaic humans (genus ''Homo'') out of Africa and throughout Eurasia took place in the course of the Lower Paleolithic, and into the beginning Middle Paleolithic, between about 2.1 million and 0.2 million years ago (Ma). These expansions are collectively known as Out of Africa I, in contrast to the expansion of ''Homo sapiens'' (anatomically modern humans) into Eurasia, which may have begun shortly after 0.2 million years ago (known in this context as "Out of Africa II"). The earliest presence of ''Homo'' (or indeed any hominin) outside of Africa dates to close to 2 million years ago. A 2018 study claims human presence at Shangchen, central China, as early as 2.12 Ma based on magnetostratigraphic dating of the lowest layer containing stone artefacts. "Eight major magnetozones are recorded in the Shangchen section, four of which have normal polarity (N1 to N4) and four of which have reversed polarity (R1 to R4). By comparison with the geomagnetic polarity timescale ..magnetozone N4 corresponds to the Réunion excursion (2.13–2.15 Ma) in L28." The oldest known human skeletal remains outside of Africa are from Dmanisi, Georgia (Dmanisi skull 4), and are dated to 1.8 Ma. These remains are classified as ''Homo erectus georgicus''. Later waves of expansion are proposed around 1.4 Ma (early Acheulean industries), associated with ''Homo antecessor'' and 0.8 Ma (cleaver-producing Acheulean groups), associated with ''Homo heidelbergensis''. Until the early 1980s, early humans were thought to have been restricted to the African continent in the Early Pleistocene, or until about 0.8 Ma; Hominin migrations outside East Africa were apparently rare in the Early Pleistocene, leaving a fragmentary record of events.

Early dispersals

Pre-''Homo'' hominin expansion out of Africa is suggested by the presence of ''Graecopithecus'' and ''Ouranopithecus'', found in Greece and Anatolia and dated to c. 8 million years ago, but these are probably Homininae but not Hominini. Possibly related are the Trachilos footprints found in Crete, dated to close to 6 million years ago. ''Australopithecina'' emerge about 5.6 million years ago, in East Africa (Afar Depression). Gracile australopithecines (''Australopithecus afarensis'') emerge in the same region, around 4 million years ago. The earliest known retouched tools were found in Lomekwi, Kenya, and date back to 3.3 Ma, in the late Pliocene. They might be the product of ''Australopithecus garhi'' or ''Paranthropus aethiopicus'', the two known hominins contemporary with the tools. Genus ''Homo'' is assumed to have emerged by around 2.8 million years ago, with ''Homo habilis'' being found at Lake Turkana, Kenya. The delineation of the "human" genus, ''Homo'', from Australopithecus is somewhat contentious, for which reason the superordinate term "hominin" is often used to include both. "Hominin" technically includes chimpanzees as well as pre-human species as old as 10 million years ago (the separation of Homininae into Hominini and Gorillini). The earliest known hominin presence outside of Africa, dates to close to 2 million years ago. A 2018 study claims evidence for human presence at Shangchen, central China, as early as 2.12 Ma based on magnetostratigraphic dating of the lowest layer containing stone artefacts. It has been suggested that ''Homo floresiensis'' was descended from such an early expansion. It is not clear whether these earliest hominins leaving Africa should be considered ''Homo habilis'', or a form of early ''Homo'' or late ''Australopithecus'' closely related to ''Homo habilis'', or a very early form of ''Homo erectus''. In any case, the morphology of ''H. floresiensis'' has been found to show greatest similarity with ''Australopithecus sediba'', ''Homo habilis'' and Dmanisi Man, raising the possibility that the ancestors of ''H. floresiensis'' left Africa before the appearance of ''H. erectus''. A phylogenetic analysis published in 2017 suggests that ''H. floresiensis'' was descended from a species (presumably Australopithecine) ancestral to ''Homo habilis'', making it a "sister species" either to ''H. habilis'' or to a minimally ''habilis''-''erectus''-''ergaster''-''sapiens'' clade, and its line is older than ''H. erectus'' itself. On the basis of this classification, ''H. floresiensis'' is hypothesized to represent a hitherto unknown and very early migration out of Africa, dating to before 2.1 million years ago. A similar conclusion is suggested by the date of 2.1 Ma for the oldest Shangchen artefacts.

''Homo erectus''

''Homo erectus'' emerges just after 2 million years ago. Early ''H. erectus'' would have lived face to face with ''H. habilis'' in East Africa for nearly half a million years. The oldest ''Homo erectus'' fossils appear almost contemporaneously, shortly after two million years ago, both in Africa and in the Caucasus. The earliest well-dated Eurasian ''H. erectus'' site is Dmanisi in Georgia, securely dated to 1.8 Ma.1.85-1.78 Ma 95% CI. A skull found at Dmanisi is evidence for caring for the old. The skull shows that this ''Homo erectus'' was advanced in age and had lost all but one tooth years before death, and it is perhaps unlikely that this hominid would have survived alone. It is not certain, however, that this is sufficient proof for caring – a partially paralysed chimpanzee at the Gombe reserve survived for years without help. The earliest known evidence for African ''H. erectus'', dubbed ''Homo ergaster'', is a single occipital bone (KNM-ER 2598), described as "H. erectus-like", and dated to about 1.9 Ma (contemporary with ''Homo rudolfensis''). This is followed by a fossil gap, the next available fossil being KNM-ER 3733, a skull dated to 1.6 Ma. Early Pleistocene sites in North Africa, the geographical intermediate of East Africa and Georgia, are in poor stratigraphic context. The earliest of the dated is Ain Hanech in northern Algeria (c. 1.8 – 1.2 Ma), an Oldowan grade layer. These sites attest that early ''Homo erectus'' have crossed the North African tracts, which are usually hot and dry. There is little time between ''Homo erectus''’ apparent arrival in South Caucasus around 1.8 Ma, and its probable arrival in East and Southeast Asia. There is evidence of ''H. erectus'' in Yuanmou, China, dating to 1.7 Ma and in Sangiran, on Java, Indonesia, from 1.66 Ma. Ferring et al. (2011) suggest that it was still ''Homo habilis'' that reached West Asia, and that early ''H. erectus'' developed there. ''H. erectus'' would then have dispersed from West Asia, to East Asia (Peking Man) Southeast Asia (Java Man), back to Africa (''Homo ergaster''), and to Europe (Tautavel Man). It appears ''H. erectus'' took longer to move into Europe, the earliest site being Barranco León in southeastern Spain dated to 1.4 Ma, associated with ''Homo antecessor'', and a controversial Pirro Nord in Southern Italy, allegedly from 1.7 – 1.3 Ma. The paleobiogeography of early human dispersals in western Eurasia characterizes ''H''. ex gr. ''erectus'' as a temperature sensitive stenobiont, that failed to disperse north of the Alpide Belt. The geographically restricted earliest human presence in the Iberian Peninsula should be regarded as evidence of a sustainable presence of human population in this isolated area. The Pannonian plain, situated south-west of the Carpathian Mountains, was apparently characterized by a comparatively warm climate similar to that of the Mediterranean Area, while the climate of the western European paleobiogeographic area was mitigated by Gulf Stream influence and could support the episodic hominin dispersals toward the Iberian Peninsula. Apparently, the faunal exchanges between southeastern Europe and the Near East and southern Asia were controlled by the complex interaction of such geographic obstacles as the Bosporus and the Manych Strait, the climate barrier from the north of the Greater Caucasus range, and the 41 kyr glacial Milankovitch cycles that repeatedly closed the Bosporus and thus triggered the two-way faunal exchange between southeastern Europe and the Near East, and, apparently, the further westward dispersal of the archaic hominins in Eurasia. By 1 Ma, ''Homo erectus'' had spread across Eurasia (mostly restricted to latitudes south of the 50th parallel north). It is hard to say, however, whether settlement was continuous in Western Europe, or if successive waves repopulated the territory in glacial interludes. Early Acheulean tools at Ubeidiya from 1.4 Ma is some evidence for a continuous settlement in the West, as successive waves out of Africa after then would likely have brought Acheulean technology to Western Europe. The presence of Lower Paleolithic human remains in Indonesian islands is good evidence for seafaring by ''Homo erectus'' late in the Early Pleistocene. Bednarik suggests that navigation had appeared by 1 Ma, possibly to exploit offshore fishing grounds. He has reproduced a primitive dirigible (steerable) raft to demonstrate the feasibility of faring across the Lombok Strait on such a device, which he believes to have been done before 850 ka. The strait has maintained a width of at least 20 km for the whole of the Pleistocene. Such an achievement by ''Homo erectus'' in the Early Pleistocene offers some strength to the suggested water routes out of Africa, as the Gibraltar, Sicilian, and Bab-el-Mandeb exit routes are harder to consider if watercraft are deemed beyond the capacities of ''Homo erectus''.

''Homo heidelbergensis''

Archaic humans in Europe beginning about 0.8 Ma (cleaver-producing Acheulean groups) are classified as a separate, erectus-derived species, known as ''Homo heidelbergensis''. ''H. heidelbergensis'' from about 0.4 Ma develops its own characteristic industry, known as Clactonian. ''H. heidelbergensis'' is closely related to ''Homo rhodesiensis'' (also identified as ''Homo heidelbergensis sensu lato'' or African ''H. heidelbergensis''), known to be present in southern Africa by 0.3 Ma. ''Homo sapiens'' emerges in Africa before about 0.3 Ma from a lineage closely related to early ''H. heidelbergensis''. The first wave of "Out of Africa II and "earliest presence of ''H. sapiens'' in West Asia, may date to between .3 and 0.2 Ma, and ascertained for 0.13 Ma. Genetic research also indicates that a later migration wave of ''H. sapiens'' (from .07-.05 Ma) from Africa is responsible for all to most of the ancestry of current non-African populations.

Routes out of Africa

Most attention as to the route taken from Africa to West Asia is given to the Levantine land corridor and the Bab-el-Mandeb straits. The latter connects the Horn of Africa and Arabia, and may have allowed dry passage during some periods of the Pleistocene. Another candidate is the Strait of Gibraltar. A route across the Strait of Sicily was suggested in the 1970s but is now considered unlikely.

Levantine corridor

The use by hominins of the Levantine corridor, connecting Egypt via the Sinai peninsula with the Eastern Mediterranean, has been associated to the phenomenon of rising and declining humidity of the desert belt of northern Africa, known as the Sahara pump. The numerous hominin sites in the Levant, such as Ubeidiya and Misliya cave, are used as indicators of this migration route. As of 2012, the genetic analysis of human populations in Africa and Eurasia supports the concept that during the Paleolithic and Mesolithic periods, this route was more important for bi-directional human migrations between Africa and Eurasia than was the Horn of Africa.

Horn of Africa to Arabia (Bab el-Mandeb)

Bab-el-Mandeb is a 30 km strait between East Africa and the Arabian Peninsula, with a small island, Perim, 3 km off the Arabian bank. The strait has a major appeal in the study of Eurasian expansion in that it brings East Africa close to Eurasia. It does not require hopping from one water body to the next across the North African desert. The land connection with Arabia disappeared in the Pliocene, and though it may have briefly reformed, the evaporation of the Red Sea and associated increase in salinity would have left traces in the fossil record after just 200 years and evaporite deposits after 600 years. Neither have been detected. A strong current flows from the Red Sea into the Indian Ocean and crossing would have been difficult without a land connection. Oldowan grade tools are reported from Perim Island, implying that the strait could have been crossed in the Early Pleistocene, but these finds have yet to be confirmed.

Strait of Gibraltar

The Strait of Gibraltar is the Atlantic entryway to the Mediterranean, where Spanish and Moroccan banks are only 14 km apart. A decrease in sea levels in the Pleistocene due to glaciation would not have brought this down to less than 10 km. Deep currents push westwards, and surface water flows strongly back into the Mediterranean. Entrance into Eurasia across the strait of Gibraltar could explain the hominin remains at Barranco León in southeastern Spain (1.4 Ma) and Sima del Elefante in northern Spain (1.2 Ma). But the site of Pirro Nord in southern Italy, allegedly from 1.3 – 1.7 Ma, suggests a possible arrival from the East. Resolution is insufficient to settle the matter.

Strait of Sicily

Passage across the Strait of Sicily was suggested by Alimen (1975) based on the 1973 discovery of Oldowan grade tools in Sicily. Radiometric dates, however, have not been produced, and the artefacts might as well be from the Middle Pleistocene, and it is unlikely that there was a land bridge during the Pleistocene.

Causes for dispersal



Climate change and hominin flexibility

For a given species in a given environment, available resources will limit the number of individuals that can survive indefinitely. This is the carrying capacity. Upon reaching this threshold, individuals may find it easier to gather resources in the poorer yet less exploited peripheral environment than in the preferred habitat. ''Homo habilis'' could have developed some baseline behavioural flexibility prior to its expansion into the peripheries (such as encroaching into the predatory guild). This flexibility could then have been positively selected and amplified, leading to ''Homo erectus'' adaptation to the peripheral open habitats. A new and environmentally flexible hominin population could have come back to the old niche and replaced the ancestral population. Moreover, some step-wise shrinking of the woodland and the associated reduction of hominin carrying capacity in the woods around 1.8 Ma, 1.2 Ma, and 0.6 Ma would have stressed the carrying capacity's pressure for adapting to the open grounds. With ''Homo erectus'' new environmental flexibility, favourable climate fluxes likely opened it the way to the Levantine corridor, perhaps sporadically, in the Early Pleistocene.

Chasing fauna

Lithic analysis implies that Oldowan hominins were not predators. However, ''Homo erectus'' appears to have followed animal migrations to the north during wetter periods, likely as a source of scavenged food. The sabre-tooth cat Megantereon was an apex predator of the Early and Middle Pleistocene (before MIS 12). It became extinct in Africa c. 1.5 Ma, but had already moved out through the Sinai, and is among the faunal remains of the Levantine hominin site of Ubeidiya, c. 1.4 Ma. It could not break bone marrow and its kills were likely an important food source for hominins, especially in glacial periods. In colder Eurasian times, the hominin diet would have to be principally meat-based and Acheulean hunters must have competed with cats.

Coevolved zoonotic diseases

Bar-Yosef and Belfer-Cohen suggest that the success of hominins within Eurasia once out of Africa is in part due to the absence of zoonotic diseases outside their original habitat. Zoonotic diseases are those that are transmitted from animals to humans. While a disease specific to hominins must keep its human host alive long enough to transmit itself, zoonotic diseases will not necessarily do so as they can complete their life cycle without humans. Still, these infections are well accustomed to human presence, having evolved alongside them. The higher an African ape's population density, the better a disease fares. 55% of chimps at the Gombe reserve die of disease, most of them zoonotic. The majority of these diseases are still restricted to hot and damp African environments. Once hominins had moved out into drier and colder habitats of higher latitudes, one major limiting factor in population growth was out of the equation.

Physiological traits

While ''Homo habilis'' was certainly bipedal, its long arms are indicative of an arboreal adaptation. ''Homo erectus'' had longer legs and shorter arms, revealing a transition to obligate terrestriality, though it remains unclear how this change in relative leg length might have been an advantage. Sheer body size, on the other hand, seems to have allowed for better walking energy efficiency and endurance. A larger ''Homo erectus'' would also dehydrate more slowly and could thus cover greater distances before facing thermoregulatory limitations. The ability for prolonged walking at a normal pace would have been a decisive factor for effective colonisation of Eurasia.

See also

*Archaic humans in Southeast Asia *Archaic humans *Interbreeding between archaic and modern humans

References



Further reading

* * * (online). * (paperback). * (online). * * (online). {{portal bar |Evolutionary biology|Science Category:Archaeological_theory Category:Homo erectus Category:Peopling of the world Category:Prehistoric migrations