The
peoples of
Africa are characterized by regional genetic substructure and heterogeneity, depending on the respective ethno-linguistic identity, and, in part, explainable by the "multiregional evolution" of modern human lineages in various multiple regions of the African continent, as well as later admixture events, including back-migrations from Eurasia, of both highly differentiated
West and
East Eurasian components. Africans' genetic ancestry is largely partitioned by
geography and
language family, with populations belonging to the same ethno-linguistic groupings showing high genetic homogeneity and coherence. Gene flow, consistent with both short- and long-range migration events followed by extensive admixture and
bottleneck events, have influenced the regional genetic makeup and demographic structure of Africans. The historical
Bantu expansion had lasting impacts on the modern demographic make up of Africa, resulting in a greater genetic and linguistic homogenization. Genetic, archeologic, and linguistic studies added extra insight into this movement: "Our results reveal a genetic continuum of Niger–Congo speaker populations across the continent and extend our current understanding of the routes, timing and extent of the Bantu migration." Overall, different African populations display genetic diversity and substructure, but can be clustered in distinct but partially overlapping groupings: Afroasiatic-speaking populations also display variable amounts of West Asian (primarily
Natufian-like, but also
Neolithic Anatolian and
Iranian) admixtures from Eurasian backflow movements, with the remainder being primarily from autochthonous African genetic clusters, associated with
Nilotic-like ancestry. They also display affinity for the Paleolithic North African
Taforalt specimens of the
Iberomaurusian culture. • '
Eastern African hunter-gatherers', represented by
Hadza,
Sandawe,
Omotic-speakers, and the ancient Mota specimen; their phylogenetic relationship to other populations is not clear, but they display affinity to modern East and West African populations, and harbor Khoesan-like geneflow along a Northeast to Southwest cline, as well as later (West) Eurasian admixtures, but at lower amounts than among Afroasiatic-speakers. • "
Ancient East Africans" or "
Ancestral West/East Africans" associated with the common ancestor of modern
Niger-Congo and
Nilo-Saharan-speakers originated around 28,000 years ago, likely in the
Nile Valley region. They subsequently diverged at c. 18,000 years ago into the ancestors of West and West-Central African Niger-Congo and Bantu-speakers, and into the East African Nilo-Saharan/Nilotic-speakers. They represent the dominant and most widespreaded ancestry component of modern Africa, and are associated with relative recent population expansions linked to agriculture and pastoralist lifestyles. Genetic data indicates affinity for older hunter-gatherer groups in East Africa, but their exact relationship remains unclear. •
Austronesian-speaking Malagasy people in
Madagascar have received significant
East/Southeast Asian admixture associated with the
Austronesian expansion, with the remainder ancestry being primarily associated with West-Central and East African components. The estimated date of geneflow between these sources is c. 2,200 years ago.
Indigenous Africans The term '
indigenous Africans' refers to the populations with primarily indigenous (non-Eurasian) ancestries, consisting of
Niger–Congo speakers,
Nilo-Saharan speakers, the divergent and diverse
Khoisan grouping, as well as of several unclassified or
isolated ethnolinguistic groupings (see
unclassified languages of Africa). The origin of the
Afroasiatic languages remains disputed, with some proposing a
Middle Eastern origin, while others support an African origin with varying degrees of Eurasian and African components. The
Niger–Congo languages probably originated in or near the area where these languages were spoken prior to
Bantu expansion (i.e.
West Africa or
Central Africa). Its expansion may have been associated with the expansion of agriculture, in the
African Neolithic period, following the
desiccation of the Sahara in c. 3500 BCE.
Proto-Niger-Congo may have originated about 10,000 years before present in the "
Green Sahara" of Africa (roughly the
Sahel and southern
Sahara), and that its dispersal can be correlated with the spread of the
bow and arrow by migrating
hunter-gatherers, which later developed agriculture. Although the validity of the
Nilo-Saharan family remains controversial, the region between
Chad,
Sudan, and the
Central African Republic is seen as a likely candidate for its homeland prior to its dispersal around 10,000–8,000 BCE. The Southern African hunter-gatherers (Khoisan) are suggested to represent the autochthonous hunter-gatherer population of southern Africa, prior to the expansion of Bantu-speakers from Western/Central Africa and East African pastoralists. Khoisan show evidence for Bantu-related admixture, ranging from nearly ~0% to up to ~87.1%.
Out-of-Africa event The "
recent African origin of modern humans" proposes a "single origin" of
Homo sapiens within Africa. Recent genetic and archeologic data suggests that Homo sapiens-subgroups originated in multiple regions of Africa, not confined to a single sub-region of origin, with the last common ancestor of all modern humans expanding from a single region absorbing or replacing various deep lineages (described as archaic ghosts). The
H. sapiens ancestral to proper Eurasians most likely left
Northeastern Africa between 50,000 and 100,000 years ago. The "recent African origin" model proposes that all modern
non-African populations descend from one or several waves of
H. sapiens that left Africa 70,000–60,000 years ago. According to Durvasula et al. (2020), there are indications that 2% to 19% (≃6.6 to 7.0%) of the DNA of West African populations may have come from an unknown archaic hominin which split from the ancestor of humans and Neanderthals between 360 kya to 1.02 mya. However, Durvasula et al. (2020) also suggests that at least part of this archaic admixture is also present in Eurasians/non-Africans, and that the admixture event or events range from 0 to 124 ka B.P, which includes the period before the Out-of-Africa migration and prior to the African/Eurasian split (thus affecting in part the common ancestors of both Africans and Eurasians/non-Africans). Chen et al. (2020) found that Africans have higher
Neanderthal ancestry than previously thought. 2,504 African samples from all over Africa were analyzed and tested on Neanderthal ancestry. All African samples showed evidence for minor Neanderthal ancestry, but always at lower levels than observed in Eurasians.
Geneflow between Eurasian and African populations Significant Eurasian admixture is found in
Northern Africa, and among specific ethnic groups of the
Horn of Africa,
Northern Sudan, the
Sahel region, as well as among the
Malagasy people of
Madagascar. Various genome studies found evidence for multiple
prehistoric back-migrations from various
Eurasian populations and subsequent admixture with native groups. West Eurasian-associated geneflow arrived to Northern Africa during the Paleolithic (30,000 to 15,000 years ago), followed by other pre-Neolithic and Neolithic migration events. Genetic data on the
Taforalt samples "demonstrated that Northern Africa received significant amounts of gene-flow from Eurasia predating the Holocene and development of farming practices". Medieval geneflow events, such as the Arab expansion also left traces in various African populations. Pickrell et al. (2014) indicated that Western Eurasian ancestry eventually arrived through
Northeast Africa (particularly the Horn of Africa) to
Southeast Africa and
Southern Africa. Ramsay et al. (2018) also found evidence for significant Western Eurasian admixture in various parts of Africa, from both ancient and more recent migrations, being highest among populations from
Northern Africa, and some groups of the
Horn of Africa: In addition to the intrinsic diversity within the continent due to population structure and isolation, migration of Eurasian populations into Africa has emerged as a critical contributor to the genetic diversity. These migrations involved the influx of different Eurasian populations at different times and to different parts of Africa. Comprehensive characterization of the details of these migrations through genetic studies on existing populations could help to explain the strong genetic differences between some geographically neighbouring populations. This distinctive Eurasian admixture appears to have occurred over at least three time periods with ancient admixture in central west Africa (e.g., Yoruba from Nigeria) occurring between ~7.5 and 10.5 kya, older admixture in east Africa (e.g., Ethiopia) occurring between ~2.4 and 3.2 kya and more recent admixture between ~0.15 and 1.5 kya in some east African (e.g., Kenyan) populations. Subsequent studies based on LD decay and haplotype sharing in an extensive set of African and Eurasian populations confirmed the presence of Eurasian signatures in west, east and southern Africans. In the west, in addition to Niger-Congo speakers from The Gambia and Mali, the Mossi from Burkina Faso showed the oldest Eurasian admixture event ~7 kya. In the east, these analyses inferred Eurasian admixture within the last 4000 years in Kenya. Others argue that the first speakers of
Proto-Afroasiatic were based in Northeast Africa because that region includes the majority of the diversity of the Afroasiatic language family and has very diverse groups in close geographic proximity, which is sometimes considered a telltale sign for a linguistic geographic origin. A subset of the Proto-Afroasiatic population would have migrated to the
Levant during the late
Paleolithic, merging with local West-Eurasians and resulting in a population which would later give rise to
Natufian culture, associated with the early development of
agriculture and early Afroasiatic languages, or specifically pre-
proto-Semitic. In addition,
Y-haplogroup sub-lineage
E-M215 (also known as "E1b1b) and its derivative E-M35 are quite common among Afroasiatic speakers, and southwestern Ethiopia is a plausible source of these haplogroups. Under this African model, the linguistic group and carriers of this lineage would have arisen and dispersed together from Northeast Africa in the
Mesolithic, plausibly having already developed
subsistence patterns of
pastoralism and intensive plant usage and collection. The Near-Eastern agriculturalist hypothesis does not account for the domestication of plants
endemic to the Horn of Africa such as
teff,
ensete, and
Niger seed, nor does it account for the lack of evidence of intrusive agricultural populations or for the growing of
wheat,
barley, or
sorghum in that region prior to 3000 B.C. According to historian and linguist
Christopher Ehret, the form of intensive plant collection practiced by the Proto-Afroasiatic population in Northeast Africa may have been a precursor to the other agricultural practices that would later independently develop in the
Fertile Crescent and the Horn of Africa. David Schoenbrun, Christopher Ehret, Steven A. Brandt and Shomarka Keita (2025) have highlighted the problematic categorisation of genetic haplogroups characterised as ‘
African’ and ‘
Eurasian' in North African genome studies. In reference to the van de Loosdrecht et al. 2018 study on the epipalaeolithic Taforalt remains from
Morocco, which identified the
EM35 (primarily
EM78) common in north-eastern Africa but characterised the
mtDNA (female lineage haplogroups) of
U6 and
M1 as 'Eurasian', the authors questioned the classification of these maternal haplogroups despite their localised and long-established presence in ancient African populations. In their view, identifying a range of African populations may still remain an issue “since the idea of ‘African’ still gets stereotyped or restricted. (Accepting the
southwestern Asian/
Levantine geographical continuity with Africa eliminates a conceptual barrier related to racio-typological thinking permitting an
Africasian construct analogous to Eurasian.)”. Hodgson et al. (2014) found a distinct West-Eurasian ancestral component among studied Afroasiatic-speaking groups in the Horn of Africa (and to a lesser extent in North Africa and
West Asia), most prevalent among the ethnic
Somali. This ancestral component dubbed "Ethio-Somali" is most closely related to the "Maghrebi" (peaking in
Tunisians) component and is believed to have diverged from other
non-African ancestries around 23,000 years ago, and migrated back to Africa prior to developing agriculture (12–23 ka) from the Near East. This population would have crossed via the Sinai Peninsula and then split into two, with one branch continuing west across North Africa and the other heading south into the Horn of Africa. The authors propose that the "Ethio-Somali" component may have been a substantial ancestral component of the Proto-Afroasiatic-speaking population. Later migration from Arabia into the HOA beginning around 3 ka would explain the origin of the
Ethiosemitic languages at this time. Hodgson et al. also confirmed the existence of an ancestral component indigenous to the Horn of Africa - "Ethiopic" or "Omotic" (Pagani et al.) - which is most prevalent among speakers of the
Omotic branch of Afroasiatic in southwestern Ethiopia. Another 2004 mtDNA study featured samples from Gurna, Upper Egypt and clustered them together with the
Ethiopian and
Yemeni groups, in between the Near Eastern and other African sample groups. The E-M35 haplogroup subclade is found among all
Afro-Asiatic speaking regions, with the
M-78 clade now commonly thought to have arisen in either Sudan or Egypt, "or further south in the northeastern quadrant of Africa". In an analysis of 68 Ethiopian ethnic groups, Lopez et al. (2021) revealed that several groups belonging to the three AA classifications of Cushitic, Omotic and Semitic show high genetic similarity to each other on average. Furthermore, the Nilo-Saharan speakers in the southwest shared more recent ancestry with Bantu and Nilotics, in contrast Afro-Asiatic speakers in the northeast shared more recent ancestry with
Egyptians and other West Eurasians. The data also supported widespread recent intermixing among various ethnic groups.
Madagascar and the northern
Philippines. Specific East Asian-related ancestry is found among the
Malagasy speakers of
Madagascar at a medium frequency. The presence of this East Asian-related ancestry is mostly linked to the
Austronesian peoples expansion from
Southeast Asia. The peoples of
Borneo were identified to resemble the East Asian voyagers, who arrived on Madagascar. East Asian ancestry among Malagasy people was estimated at a mean average of 33%, but as high as ~75% among some Highlander groups and upper caste groups. Other haplogroups with a notable occurrence in the Egyptian populations have included the
J and
R haplogroups. A 2005 genetic study found close affinities of eastern sub-Saharan populations with Egypt in the phylogenetic trees through analysis of the short DNA sequences. The authors suggested that the influential role of the Nile River served as a migratory route and an agent of genetic flow which contributed to present-day
heterogeneity in Egypt. Dobon et al. (2015) identified an autosomal ancestral component that is commonly found among modern Afroasiatic-speaking populations (as well as
Nubians) in Northeast Africa. This Coptic component peaks among
Copts in
Sudan, which is differentiated by its lack of Arab influence, but shares common ancestry with the North African/Middle Eastern populations. It appears alongside a component that defines
Nilo-Saharan speakers of southwestern Sudan and
South Sudan. Arauna et al. (2017), analyzing existing genetic data obtained from
Northern African populations, such as
Berbers, described them as a mosaic of North African (Taforalt), Middle Eastern, European (
Early European Farmers), and
Sub-Saharan African-related ancestries. Chen et al. (2020) analyzed 2,504 African samples from all over Africa, and found archaic Neanderthal ancestry, among all tested African samples at low frequency. They also identified a European-related (West-Eurasian) ancestry segment, which seems to largely correspond with the detected Neanderthal ancestry components. European-related admixture among Africans was estimated to be between ~0% to up to ~30%, with a peak among Northern Africans. According to Chen et al. (2020), "These data are consistent with the hypothesis that back-migration contributed to the signal of Neanderthal ancestry in Africans. Furthermore, the data indicates that this back-migration came after the split of Europeans and East Asians, from a population related to the European lineage." Multiple studies found also evidence for geneflow of African ancestry towards Eurasia, specifically Europe and the Middle East. The analysis of 40 different West-Eurasian populations found African admixture at a frequency of 0% to up to ~15%.
Western Africa Hollfelder et al. (2021) concluded that West African
Yoruba people, which were previously used as "unadmixed reference population" for indigenous Africans, harbor minor levels of Neanderthal ancestry, which can be largely associated with back-migration of an "Ancestral European-like" source population. Sahelian populations like the
Toubou also showed admixture coming from Eurasians.
Southern Africa Low levels of West Eurasian ancestry (European or Middle Eastern) are found in Khoe–Kwadi Khoesan-speakers. It could have been acquired indirectly by admixture with migrating pastoralists from East Africa. This hypothesis of gene flow from eastern to southern Africa is further supported by other genetic and archaeological data documenting the spread of pastoralism from East to South Africa. ==Regional genomic overview==