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Y-DNA · Paterno linaje

E2B

Y-DNA Haplogroup E2B

Um perfil de referência de um ramo de linhagem. Compartilhar haplogrupos não demonstra uma relação familiar ou uma identidade cultural.

Perfil de Referência

Contexto do ramo

Contexto histórico de la rama de linaje Y-DNA E2B

Origins and Evolution

Y-DNA haplogroup E2B sits as a downstream branch within haplogroup E2 (itself derived from the broader haplogroup E). Based on the parent clade's estimated time depth (~30 kya) and the observed geographic concentration of descendant lineages, E2B most plausibly arose in eastern Africa during the Late Pleistocene (roughly on the order of tens of thousands of years ago). Its origin likely reflects continuing diversification of male lineages that had already differentiated within Africa after the primary radiation of haplogroup E.

E2B shows genetic patterns consistent with a deep, regionally structured lineage: relatively old coalescence times for some subbranches combined with localized high-frequency pockets in pastoralist and Rift Valley populations, and low-frequency occurrences in neighboring regions. This pattern is typical for African Y-lineages that persisted in place while neighboring populations experienced demographic shifts during the Holocene (for example, pastoralist movements and later Bantu expansions).

Subclades

E2B consists of one or more downstream branches that have been detected at low to moderate frequencies in regional Y-chromosome surveys; these subclades tend to show geographic specificity (for example, distinct subbranches enriched in Horn of Africa samples versus those found in central African groups). Sample sizes for many of these subclades remain limited, so full internal structure and a robust SNP-based naming hierarchy continue to be refined as more targeted sequencing and large-scale genotyping are performed.

Because E2 is a relatively minor component of continental African Y diversity compared with major clades like E1b1a (M2) and E1b1b (M215), E2B's subclades often appear as localized lineages that provide insight into regional demographic events (deep continuity, local differentiation, and later movements such as pastoral expansions).

Geographical Distribution

E2B is most consistently observed in East Africa, especially in the Horn (Ethiopia, Somalia and adjacent groups) and among some Rift Valley pastoralist populations. It is found at moderate frequencies in parts of eastern and central Africa, while occurrences in West Africa, North Africa and the Near East are generally rare and sporadic. The transatlantic slave trade accounts for occasional low-frequency detections in African-descended populations of the Americas and the Caribbean.

The distribution pattern—concentration in the Horn and eastern Africa with scattered presences elsewhere—supports a long-term East African origin with both local persistence and limited gene flow into adjoining regions during the Holocene.

Historical and Cultural Significance

E2B does not map neatly onto a single archaeological culture; instead, its history appears connected to a series of regional demographic processes in eastern Africa. These include deep Late Stone Age continuity in local hunter‑gatherer and forager groups and later pastoralist expansions during the African Holocene that reshaped population structure in the Rift Valley and Horn. In some areas E2B lineages are found among groups engaged in pastoralism or agro-pastoral livelihoods, suggesting they were part of the male ancestry that participated in movements of herding peoples as the environment and subsistence strategies changed.

E2B may also be present at low levels among populations affected by the Bantu expansion and other historical migrations, but it is not itself a hallmark of the Bantu-associated E1b1a lineage; rather, its presence in some Bantu-speaking communities reflects regional admixture and assimilation.

Conclusion

E2B is a regionally important but overall minor Y-chromosome lineage that helps illuminate deep paternal structure within eastern and central Africa. Its pattern—an East African origin, persistence in the Horn and Rift Valley, and low-frequency presence beyond—aligns with what is known about the diversification of haplogroup E in Africa and with later Holocene demographic events such as pastoralist expansions and interregional admixture. Continued sampling and high-resolution sequencing will refine its internal branching and improve understanding of its role in African population history.

Pontos- Chave

  • Origins and Evolution
  • Subclades
  • Geographical Distribution
  • Historical and Cultural Significance
  • Conclusion
Perfil de Referência

Árvore e relações

Contexto filogenético e subclasse

Trajectória evolutiva

Sigue las ramas superiores registradas hasta E2B. Las fechas son estimaciones y pueden cambiar al revisarse los datos de referencia.

Passos Haplogrupo Antiguidade estimada Época arqueológica Tempo decorrido Subclasses imediatas Portadores modernos analisados Referências antigas
1 E2B Actual ~18,000 years ago Mesolithic 18,000 years 2 32 0
2 E2 ~30,000 years ago Paleolithic 30,000 years 2 39 0
3 E ~50,000 years ago Paleolithic 50,000 years 3 1,813 3

Ramas hermanas (1)

Outros ramos do mesmo haplogrupo superior

Perfil de Referência

No mundo

Distribuição geográfica e presença moderna

Origem registada

East Africa

Distribuição moderna

The populations where Y-DNA haplogroup E2B is found include:

  1. Horn of Africa populations (Ethiopian, Somali and neighboring Cushitic and Semitic groups)
  2. Eastern African pastoralist and Rift Valley groups
  3. Central African forager and some Bantu-speaking communities
  4. West African groups at low frequency (rare occurrences)
  5. North African and Near Eastern populations at very low frequencies (sporadic)
  6. African-descended populations in the Americas and Caribbean (via the transatlantic slave trade, low frequency)

Presença regional

East Africa Moderate
Central Africa Low
North Africa Low
West Africa Low
Middle East Low
Southern Europe Low
North America (diaspora) Low
Horn of Africa Moderate
West Africa Low
North Africa Low
Contexto Histórico

Uma ramificação através do tempo

Formação estimada em uma cronologia histórica ampla. Os marcadores temporais contribuem contexto e não implicam relação com culturas concretas.

  1. ~20k años de antigüedad

    Último máximo glacial

    Máxima extensão da última glaciação e isolamento de populações

  2. ~18k años de antigüedad

    Haplogrupo E2B

    Formação estimada deste ramo Y-DNA; as datas e localizações são estimativas de referência.

    Este ramo
  3. ~10k años de antigüedad

    Revolução neolítica

    Início da agricultura e formação de comunidades sedentárias

  4. ~5k años de antigüedad

    Idade do Bronze

    Metalurgia, escrita e primeiras civilizações

  5. ~3k años de antigüedad

    Idade do Ferro

    Ferramentas de ferro e ampliação de redes comerciais

  6. ~2.5k años de antigüedad

    Antiguidades clássicas

    Desenvolvimento das civilizações grega e romana

  7. Actualidad

    Actualidad

    Idade moderna

Perfil de Referência

Contexto arqueológico

Asociaciones arqueológicas registradas para la rama Y-DNA E2B

Associações registradas

Esses rótulos descrevem os contextos arqueológicos registrados para as amostras de referência vinculadas a E2B. Uma associação não demonstra que todos os portadores pertenceram a uma cultura ou seguiram uma rota migratória específica.

Early Pastoral Neolithic Kansyore Culture Kindoki Late Anatolian Chalcolithic Lindi Swahili Makwasinyi Medieval Italian Modern Period PPNB Pre-Aksumite Syrian Bronze
As atribuições culturais baseiam-se no contexto arqueológico das amostras de DNA antigo e podem representar associações regionais de períodos concretos.
PATERNAL LINHAGEM · DNA ANTIGO

Mapa de testes de linhagems antigos

Siga os clados superiores até este ramo e explora onde se encontraram portadores antigos.

A carregar as observações antigas...

Os marcadores são locais de achados arqueológicos. Uma linha de descontínua representa uma transição geográfica proposta e incerta entre ramos consecutivos, apoiada em várias observações fechadas; não é uma rota de viagem exata, um local de nascimento ou um teste de descendência direta. As amostras do clado parental podem pertencer a outros ramos descendentes. As datas das amostras são distintas das datas de formação dos haplogrupos são mantidas.

Dados

Dados e proveniência

Informações sobre fontes e qualidade dos dados

Última actualização 2026-06-16
Pontuação de confiança 50/100
Cobertura Low

Fonte de Dados

A classificação, as datas estimadas e o contexto geográfico refletem os dados de referência registrados e podem mudar ao revisar os testes. A cobertura de amostras é desigual; os locais registrados e as associações arqueológicas não estabelecem a origem pessoal nem a identidade cultural.