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Human dispersals in Europe

Colonisation of the European continent

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Through Europe, Homo and Speciation

The expansion of humans into Europe was accompanied by migrations into Asia, where fossil remains have been attributed to Homo erectus and various subspecies such as H. e. pekinensis, and more derived groups such as H. floresiensis and H. luzonensis. Neanderthals and Denisovan remains have also been recovered from multiple sites in the Altai mountains in Siberia (Chagyrskaya, Okladnikov, and Denisova caves) some of which has produced additional Neanderthal and Denisovan genome sequences which revealed evidence of ancient admixture with modern humans.

Miocene and pre-European hominids

Fossil evidence of several species pre-dating the genus Homo (i.e., "humans") as well as its enclosing group Hominina (australopithecines) but generally agreed to be part of the family Hominidae (hominids, the great apes) have been recovered in what is today the European continent. Importantly however, neither the permanent geographic separation between North Africa and Western Europe nor the connection between Africa and Eurasia existed prior to the Miocene epoch, when the Eurasian, Arabian, and African continental plates collided and resulted in a sporadically continuous landmass, prolonged biotic exchange, and the end of the last remnants of the Tethys Ocean. Thus it is considered anachronistic to refer to distinct European and African bioregions prior to and during this process, including the expansion of Miocene taxa into "Europe" per se. More properly, these taxa are referred to as having existed in various Miocene paleoregions such as the Western and Central Paratethys, the Carpathian origeny, the Aegean and Pannonian Basin palaeolands, etc.

In the Early Miocene, Europe had a subtropical climate and was intermittently connected to Africa by land bridges such as the Gomphoterian bridge. At the same time, Africa was becoming more arid, prompting the dispersal of its tropical fauna—including primates—north into the proto-European continent. Apes first appear in the European fossil record 17 million years ago with Griphopithecus. The closely related Kenyapithecus is also known from fossils in Germany, Slovakia and Turkey. Both Griphopithecus and Kenyapithecus are considered likely to be ancestral to the great apes. From 13 million to 9 million years ago, hominids flourished in Europe and underwent an adaptive radiation as they diversified in response to a gradually cooling climate. Middle Miocene European hominids include Pierolapithecus, Anoiapithecus, Dryopithecus, Hispanopithecus, and Rudapithecus. The diversity and early appearance of great apes in Europe has led some scientists to theorise that hominids in fact evolved there, before dispersing "back to Africa" in the Middle Miocene.

Around 9 million years ago most of Europe's hominid species fell victim to the Vallesian crisis, an extinction event caused by the disappearance of the continent's forests. Some hominid species survived the event: Oreopithecus, which became isolated in forest refugia; and Ouranopithecus, which adapted to the open environments of the late Miocene. However, both were extinct by 7 million years ago.

In 2017, a reanalysis of Graecopithecus fossils from Greece and Bulgaria, previously associated with Ouranopithecus, concluded that the species was in fact a hominin dating to just after the last common ancestor of humans and chimpanzees (about 7.2 million years ago). The authors suggested that the origins of the human lineage were therefore in the Mediterranean, not Africa. Others are sceptical of their claims.

Although subtropical conditions returned to Europe in the Pliocene (5.33–2.58 million years ago), there are no known fossil hominids from this period.

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