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Y-DNA · Paterno linaje

C1B

Y-DNA Haplogroup C1B

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 C1B

Origins and Evolution

Haplogroup C1b is a primary branch of the broader C1 lineage (which itself split from haplogroup C in Eurasia). Based on its phylogenetic position and coalescent estimates for related lineages, C1b most likely formed during the Late Pleistocene after the initial C expansion out of southern Asia, with a probable origin roughly ~30–40 kya in South or Southeast Asia. The clade represents part of the mosaic of Paleolithic paternal lineages that accompanied human settlement of South Asia, Island Southeast Asia and, in some sublineages, the peopling of Oceania.

Mutational markers used to define C1b vary by study and naming system; some well-sampled sublineages (often reported under legacy marker names in older literature) are concentrated in South Asian populations, while other branches show affinities to Island Southeast Asia and Near-Oceanian groups. The structure of C1b suggests an early split from C1 followed by regional differentiation and localized drift, producing a pattern of geographically restricted but temporally deep lineages.

Subclades (if applicable)

C1b comprises several downstream branches that differ in geographic profile and relative age. In high-level terms:

  • South Asian-centered clades — multiple lineages found at modest frequencies across the Indian subcontinent and adjacent regions; these reflect long-term local continuity and pockets of higher frequency due to drift or founder effects.
  • Island Southeast Asia/Oceanian-affiliated clades — branches that reach into Wallacea, Island Southeast Asia and Near Oceania, consistent with early coastal dispersals and later Austronesian-era movements in some cases.
  • Sporadic northern/central Asian occurrences — low-frequency or relict lineages recorded in Central and Northeast Asia, probably reflecting ancient northward movements or later gene flow.

Different studies and phylogenetic revisions use marker names and shorthand (e.g., older literature referencing M356-like markers for South Asian lineages); modern high-resolution SNP-based trees refine these relationships but continue to support C1b as a multi-branch clade with deep regional structure.

Geographical Distribution

The modern distribution of C1b is patchy and regionally concentrated rather than ubiquitous. Highest relative frequencies and diversity are generally observed in parts of South Asia and selected Island Southeast Asian populations, with detectable presence in Oceania and very low-frequency occurrences in Central and Northeast Asia. Patterns are consistent with an early Pleistocene presence in southern Asia followed by localized differentiation, occasional long-distance dispersals, and genetic drift shaping modern frequencies.

Archaeogenetic data occasionally recover C1b or related markers in ancient samples, which helps anchor its antiquity in the region but also highlights that many modern occurrences are the result of complex demographic histories rather than a single recent expansion.

Historical and Cultural Significance

C1b carriers likely participated in a variety of subsistence and migration episodes through the Late Pleistocene and Holocene. The clade predates Neolithic farming expansions in South and Southeast Asia and is therefore often associated—at least in part—with pre-agricultural hunter-gatherer populations who later interacted with incoming farming and seafaring groups. Some downstream lineages may have been incorporated into Austronesian-speaking populations during the Holocene, while others remained regionally restricted, contributing to the paternal diversity of modern South Asian, Island Southeast Asian and Oceanian peoples.

Because C1b lineages are not generally tied to a single archaeological complex across their entire range, their cultural associations are best described as context-dependent: in some areas they reflect deep pre-Neolithic continuity, and in others they appear within Holocene maritime and farmer-pastoralist contexts.

Conclusion

C1b is a deep-rooted Eurasian branch of haplogroup C that illuminates early coastal and inland demographic processes in South and Southeast Asia and the subsequent peopling of parts of Island Southeast Asia and Oceania. Its current, uneven geographic distribution reflects a long history of ancient settlement, local drift, and later migrations rather than a single dramatic recent spread. High-resolution SNP studies and more ancient DNA sampling across South and Southeast Asia will continue to refine the internal structure and migration history of this lineage.

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 C1B. 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 C1B Actual ~35,000 years ago Paleolithic 35,000 years 2 28 0
2 C1 ~45,000 years ago Paleolithic 45,000 years 2 92 0
3 C ~60,000 years ago Paleolithic 60,000 years 3 406 35

Ramas hermanas (1)

Outros ramos do mesmo haplogrupo superior

Perfil de Referência

No mundo

Distribuição geográfica e presença moderna

Origem registada

South & Southeast Asia

Distribuição moderna

The populations where Y-DNA haplogroup C1B is found include:

  1. South Asian populations (India, Pakistan, Sri Lanka and surrounding areas)
  2. Austronesian-speaking peoples of Island Southeast Asia
  3. Papuan and Melanesian groups in Near Oceania (select subclades)
  4. Indigenous Australian groups (rare/relict occurrences in some studies)
  5. Selected Central Asian groups (low frequency)
  6. Northeast Asian populations (sporadic occurrences in Siberia, Japan, Korea, China)
  7. Diasporic or historically admixed groups in West Eurasia (rare/trace occurrences)

Presença regional

Oceania (Near Oceania) Moderate
Southeast Asia (Island Southeast Asia) Low
Australia (Indigenous Australian populations) Low
South Asia Low
Central Asia Low
Northeast Asia Low
Western Europe 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. ~50k años de antigüedad

    Paleolítico superior

    Desenvolvimento de ferramentas, arte e diversidade cultural

  2. ~35k años de antigüedad

    Haplogrupo C1B

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

    Este ramo
  3. ~20k años de antigüedad

    Último máximo glacial

    Máxima extensão da última glaciação e isolamento de populações

  4. ~10k años de antigüedad

    Revolução neolítica

    Início da agricultura e formação de comunidades sedentárias

  5. ~5k años de antigüedad

    Idade do Bronze

    Metalurgia, escrita e primeiras civilizações

  6. ~3k años de antigüedad

    Idade do Ferro

    Ferramentas de ferro e ampliação de redes comerciais

  7. ~2.5k años de antigüedad

    Antiguidades clássicas

    Desenvolvimento das civilizações grega e romana

  8. Actualidad

    Actualidad

    Idade moderna

Perfil de Referência

Contexto arqueológico

Asociaciones arqueológicas registradas para la rama Y-DNA C1B

Associações registradas

Esses rótulos descrevem os contextos arqueológicos registrados para as amostras de referência vinculadas a C1B. Uma associação não demonstra que todos os portadores pertenceram a uma cultura ou seguiram uma rota migratória específica.

Botocudo Buran-Kaya Early Bronze Indonesian Hoabinhian Huatuyan Culture Kostenki Culture Qinchang Culture Saudeleur Culture Sunghir Culture Yinwang Culture
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.