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Y-DNA · Paterno linaje

C1B2A1

Y-DNA Haplogroup C1B2A1

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 C1B2A1

Origins and Evolution

Y-DNA haplogroup C1B2A1 is a derived subclade of C1B2A, itself nested within the broader C1b2 branch. Given the phylogenetic position of C1B2A and observed geographic concentrations, C1B2A1 most plausibly originated in the Wallacea region (eastern Indonesia / Island Southeast Asia) during the transition from the Late Pleistocene into the Early Holocene (on the order of ~14 kya in this account). Its emergence represents a continuation of deep Paleolithic male lineages that were established in Island Southeast Asia and Near Oceania during the late Pleistocene coastal and island colonization events.

Divergence of C1-derived lineages in Wallacea and Near Oceania is compatible with a model in which early C lineages spread along island chains and coastal refugia, with C1B2A1 forming as a localized branch that later contributed to the paternal pool of both Wallacean islanders and populations east into Near Oceania.

Subclades (if applicable)

At present, available population and phylogenetic data indicate C1B2A1 contains further downstream diversity that is primarily localized and often private to island populations. Many of these downstream variants have low sample counts in published databases, reflecting limited sampling and the patchy preservation of ancient DNA in tropical island contexts. Future high-resolution sequencing and targeted surveys are likely to further resolve regional subbranches that distinguish populations of Sulawesi, the Maluku Islands, Nusa Tenggara, and Near Oceanian islands.

Geographical Distribution

C1B2A1 shows a strongly island-centered distribution concentrated in Wallacea and parts of Near Oceania. Modern and population-genetic surveys report the haplogroup at high to moderate frequencies in eastern Indonesian islands (Sulawesi, Maluku, Nusa Tenggara) and detectable frequencies in Near Oceanian groups (Papua New Guinea, Bismarck Archipelago, Solomon Islands). The lineage is also observed at lower frequencies among some Melanesian groups, coastal Austronesian-speaking communities in eastern Indonesia, and sporadically in the Philippines, Taiwan, and southern Japan — consistent with maritime contact, Austronesian expansion, and later admixture. Trace occurrences appear in diasporic and admixed Southeast Asian groups.

The restriction of higher frequencies to island and coastal populations is consistent with a history of maritime mobility, founder effects on islands, and long-term genetic continuity of male lineages in relatively isolated island communities.

Historical and Cultural Significance

C1B2A1 is informative for reconstructing human prehistory in a complex contact zone where deep Paleolithic lineages met expanding Holocene groups. The pattern — localized deep-rooting paternal lineages persisting into the present — aligns with archaeological and linguistic evidence for long-term occupation of Wallacea and Near Oceania by pre-Austronesian hunter-gatherer populations and later admixture with Austronesian-speaking farmers and Lapita-associated communities. Where C1B2A1 is present at appreciable frequency, it often marks paternal ancestry that predates the Austronesian agricultural expansion, making it useful for disentangling pre-Neolithic substrata from later demic movements in genetic studies.

Because ancient DNA from tropical islands is sparse, interpretations rely heavily on modern population sampling and comparisons to better-sampled Papuan and Melanesian groups. The haplogroup therefore serves as a target for future genetic and archaeological integration to better resolve timing and routes of island dispersals.

Conclusion

Y-DNA haplogroup C1B2A1 is a regionally important paternal lineage in Wallacea and Near Oceania that preserves a signal of late Pleistocene–Early Holocene island colonization and subsequent interaction with Holocene migrations. Its present distribution — concentrated in island Southeast Asia and parts of Near Oceania with scattered occurrences elsewhere — reflects a history of maritime settlement, founder effects on islands, and later admixture with Austronesian and other regional populations. Continued high-resolution Y-chromosome sequencing and expanded sampling in underrepresented islands will clarify its internal structure and deepen understanding of island prehistory.

Pontos- Chave

  • Origins and Evolution
  • Subclades (if applicable)
  • 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 C1B2A1. 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 C1B2A1 Actual ~14,000 years ago Mesolithic 14,000 years 0 4 0
2 C1B2A ~18,000 years ago Mesolithic 18,000 years 1 7 0
3 C1B2 ~28,000 years ago Paleolithic 28,000 years 1 7 0
4 C1B ~35,000 years ago Paleolithic 35,000 years 2 28 0
5 C1 ~45,000 years ago Paleolithic 45,000 years 2 92 0
6 C ~60,000 years ago Paleolithic 60,000 years 3 406 35

Subclados (0)

Rama terminal: não há subclasses registrados

Perfil de Referência

No mundo

Distribuição geográfica e presença moderna

Origem registada

Wallacea (Island Southeast Asia)

Distribuição moderna

The populations where Y-DNA haplogroup C1B2A1 is found include:

  1. Wallacean island populations (e.g., Sulawesi, Maluku, Nusa Tenggara)
  2. Near Oceanian groups (Papua New Guinea, Bismarck Archipelago, Solomon Islands)
  3. Melanesian populations at varying frequencies
  4. Austronesian-speaking coastal communities in eastern Indonesia
  5. Selected insular South Asian/Timorese populations at low frequency
  6. Sporadic occurrences in parts of the Philippines, Taiwan, and southern Japan
  7. Diasporic or admixed groups across Southeast Asia and Oceania (trace occurrences)

Presença regional

Near Oceania / Melanesia High
Australia (Indigenous groups) Moderate
Southeast Asia (eastern islands / Wallacea) Low
Near Oceania (Papua New Guinea, Bismarcks, Solomon Islands) Moderate
Melanesia (wider) Moderate
East Asia (Philippines, Taiwan, southern Japan) Low
Insular South Asia (Timor and nearby islands) 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. ~14k años de antigüedad

    Haplogrupo C1B2A1

    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 C1B2A1

Associações registradas

Esses rótulos descrevem os contextos arqueológicos registrados para as amostras de referência vinculadas a C1B2A1. Uma associação não demonstra que todos os portadores pertenceram a uma cultura ou seguiram uma rota migratória específica.

1983 Ancient Polynesian Botocudo Historic Polynesian Hoabinhian Late Vanuatu Post-Lapita Vanuatu Saudeleur Culture Vanuatu Historical
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 2026-06-15
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.