Repeated movements out of Africa are compatible with a predominant shared source for the ancestry of living non-Africans. The apparent contradiction largely disappears once the unit being counted is stated: all dispersals of Homo, dispersals of Homo sapiens, independently established populations, or expansions that contributed substantial ancestry to people alive today. These are different historical claims.
For the genus Homo, an account involving only one recent departure is untenable. Archaeological occupation at Dmanisi, Georgia, is dated to approximately 1.85–1.78 Ma, long before the late Pleistocene expansion of Homo sapiens. The earliest occupation levels must be distinguished from the somewhat younger hominin-bearing deposits: the site is not a single instantaneous event. Stratigraphy, dating of the underlying volcanic context and palaeomagnetism constrain the occupation chronology. [ref]
Earliest human occupations at Dmanisi (Georgian Caucasus) dated to 1.85–1.78 Ma by Reid Ferring and others. Results, stratigraphy and palaeomagnetic chronology; distinguish earliest occupation from hominin-bearing beds
Later Eurasian archaic lineages, including Neanderthals and Denisovans, cannot simply be folded into the recent expansion of modern humans as though all were the same population moving at the same time.Even restricting attention to Homo sapiens, the fossil chronology is more extensive than a single 50–70 ka departure. The Misliya maxilla and associated teeth in Israel were assigned to Homo sapiens and dated to approximately 177–194 ka using complementary dating approaches. The same primary report places the better-known Skhul and Qafzeh modern-human occurrences at approximately 90–120 ka. [ref]
The earliest modern humans outside Africa by Israel Hershkovitz and others. Science 359, pp. 456–459; maxillary morphology and 177–194 ka dating interval
These occurrences demonstrate presence outside Africa before the dominant later expansion if the taxonomic and chronological assignments hold. They do not by themselves demonstrate uninterrupted occupation, a particular migration route through Arabia, or a large surviving genetic contribution to present-day Eurasians.Apidima adds an important but less secure claim. Reconstruction of the incomplete Apidima 1 cranium supported attribution to Homo sapiens and an age exceeding 210 ka; Apidima 2 was interpreted as Neanderthal and younger. [ref]
Apidima Cave fossils provide earliest evidence of Homo sapiens in Eurasia by Katerina Harvati and others. Nature 571, pp. 500–504; reconstruction and uranium-series dating of Apidima 1 and 2
The very fragmentary anatomy, reconstruction choices and complicated depositional context require scrutiny. An assigned minimum age is not an exact date of arrival, and a different reconstruction or taxonomic diagnosis can alter the biogeographic inference. The sensible argument for early departures therefore uses the converging set of dated remains and its uncertainty, rather than treating the oldest proposed specimen as a decisive, uncontested fact.The main evidence favouring a single principal source is genetic. Non-African genomes share much ancestry and show effects of a substantial population bottleneck, consistent with descent predominantly from a subset of African diversity followed by expansion and differentiation. Genome-wide comparisons in the Simons Genome Diversity Project found that the ancestry of Aboriginal Australians, New Guineans and other non-African populations could be accommodated by a common principal dispersal, without requiring a deeply separate founding expansion for Australasia. [ref]
The Simons Genome Diversity Project: 300 genomes from 142 diverse populations by Swapan Mallick and others. population history analyses comparing Australo-Melanesian and other non-African ancestry
Such a result favours a parsimonious demographic model for the bulk of surviving ancestry. It does not observe a unique group crossing a border on one date, nor rule out movements whose descendants disappeared.Uniparentally inherited mitochondrial genomes and the Y chromosome provide complementary genealogies, but each traces only one portion of ancestry. Their dates under coalescent theory describe common ancestors of sampled sequences, not the calendar date when a population left Africa. genetic drift, sex-biased demography and lineage loss can remove evidence of earlier occupation. Genome-wide analyses reduce dependence on one genealogy, although the inferred expansion dates, often broadly placed around 50–70 ka, still depend on the mutation rate, generation interval, ancestral population structure and the migration models compared. A prolonged connected expansion can resemble one founder event in a simplified model.
There is also genetic evidence that complicates an absolute single-expansion claim. One analysis inferred a small contribution to Papuan ancestry from an earlier expansion, while still attributing the great majority of non-African ancestry to a shared later expansion. [ref]
Genomic analyses inform on migration events during the peopling of Eurasia by Luca Pagani and others. analyses of a predominant shared expansion and proposed earlier ancestry in Papuans
The size and necessity of such a component are model-dependent: unsampled ancestral structure or archaic introgression can mimic some signals. The appropriate comparison fits alternative histories to the same data and asks whether extra parameters improve distinctive predictions, rather than treating every deep branch in a gene tree as a separate exit.Archaic admixture makes the ancestry history explicitly reticulate. Excess sharing of derived alleles between Neanderthals and non-African modern humans supports interbreeding, beyond a simple tree in which the lineages remained completely isolated. [ref]
A draft sequence of the Neandertal genome by Richard E. Green and others. Science 328, pp. 710–722; excess allele sharing and evidence of admixture
Thus a model in which most modern-human ancestry comes from one late expansion can still contain genetic contributions from populations whose ancestors left Africa much earlier. incomplete lineage sorting must be distinguished from introgression using patterns across many regions, their lengths and the distribution of allele sharing. Back-migration into Africa further prevents “African” and “non-African” from being permanently sealed categories.Africa itself should not be represented as a homogeneous ancestral village. Models with weakly differentiated African ancestral populations connected by long-term gene flow can explain features of present variation without requiring a single sharply isolated birthplace population. [ref]
A weakly structured stem for human origins in Africa by Aaron P. Ragsdale and others. Nature 617, pp. 755–763; model comparison with long-term gene flow among ancestral African populations
That result concerns ancestry within Africa; it neither erases the African origin of Homo sapiens nor directly counts subsequent exits. Geographically, northern routes through the Levant and southern routes through Arabia remain testable alternatives or complements. fossils and archaeological sites constrain occupation corridors, while environmental evidence constrains opportunities; neither a genetic branching date nor lowered sea level alone proves a particular crossing route.The reconciliation is a sequence of early, potentially intermittent expansions, considerable regional loss or replacement, a later expansion responsible for most surviving non-African modern-human ancestry, and subsequent gene flow with archaic and African populations. Testing it requires directly dated remains, secure taxonomic comparisons, independent genetic samples, explicit demographic alternatives and allowance for unsampled populations. “One dominant ancestry expansion” is a much narrower and better-supported proposition than “only one movement out of Africa”; multiple movements need not imply several equally large surviving founding ancestries.
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