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Y-DNA · Paterno linaje

C2A1A2A2

Y-DNA Haplogroup C2A1A2A2

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 C2A1A2A2

Origins and Evolution

Y-DNA haplogroup C2A1A2A2 sits as a downstream subclade of C2A1A2A, itself a branch of the broader M217-derived C2 lineages that are prevalent across northern Eurasia. Based on the phylogenetic position of C2A1A2A2 and the estimated late-Holocene emergence of its parent clade (C2A1A2A at ~3 kya), a coalescence time in the order of ~2 kya (late Iron Age / early historical period) is a reasonable inference. The lineage likely arose among populations occupying the forest-steppe and steppe zones of Mongolia, southern Siberia and adjacent areas where C2-M217 diversity is concentrated.

Population genetic and ancient DNA research on related C2 branches shows repeated patterns of persistence and local expansions among pastoralist and semi-nomadic groups; C2A1A2A2 is best interpreted as one of the regional sublineages that participated in those demographic dynamics during the late Holocene and later historical expansions.

Subclades

C2A1A2A2 represents a terminal (or near-terminal) branch within the C2A1A2A clade. Depending on sampling density some studies recover further downstream splits while other datasets report C2A1A2A2 as a single defined lineage in modern populations. Its close relationship to other C2A1A2A subclades implies a shared ancestry and parallel geographic patterns; fine-scale SNP-resolution or high-coverage Y-STR profiling is required to resolve internal structure and recent sub-branches.

Geographical Distribution

The modern distribution of C2A1A2A2 is concentrated in the Central–East Asian and southern Siberian region, with highest frequencies in populations with Mongolic and Tungusic heritage. Recorded occurrences include:

  • Mongolic-speaking groups (e.g., multiple Mongol clans, Buryats)
  • Tungusic-speaking peoples (e.g., Evenks, Evens, Oroqen and related groups)
  • Sakha (Yakut) and other north Siberian populations where C2 lineages are common
  • Some southern Siberian Turkic-speaking clans (e.g., selected Tuvan and Altai lineages)
  • Low-frequency occurrences in Northeast Asian populations (sporadic in Koreans, Japanese)
  • Very rare or isolated occurrences in a small number of Indigenous North American samples, consistent with older C2 diversity and post-glacial dispersals

These patterns reflect both long-term persistence in northern Eurasia and episodes of demographic spread, including medieval-era mobility associated with steppe polities.

Historical and Cultural Significance

While C2A1A2A2 is not tied to a single archaeological culture in the same way as some deep-time haplogroups, its geographic and temporal profile links it to the late Iron Age and historical-era steppe and forest-steppe societies of Inner Asia. This includes likely presence among confederations and polities that dominated Mongolia and adjacent regions (for example later Xiongnu/Xianbei-era peoples and medieval Mongol expansions), and among communities practicing mobile pastoralism and mixed hunting–foraging economies.

Genetic studies of modern populations and targeted ancient DNA sampling indicate that C2-M217-derived subclades were often overrepresented in elite or mobile male lineages in historical sources; therefore C2A1A2A2 may reflect localized founder effects, patrilineal clan expansions, or both, during the past two millennia. Nevertheless, care is needed in linking any single Y-haplogroup to complex cultural identities — multiple haplogroups typically coexisted within steppe societies, and gene flow and admixture have reshaped regional patterns repeatedly.

Conclusion

C2A1A2A2 is a late-Holocene, northern Eurasian Y-lineage rooted in the C2-M217 radiation and concentrated among Mongolic- and Tungusic-associated populations of Mongolia and southern Siberia. Its inferred origin around ~2 kya and distribution are consistent with regional demographic processes — localized expansions, clan-level founder effects, and participation in broader steppe mobility during the Iron Age and medieval periods. Further high-resolution SNP discovery and ancient DNA sampling in Inner Asia will refine the internal branching, precise age estimates, and the historical movements tied to this subclade.

Note: age estimates and geographic inferences are based on the haplogroup's phylogenetic context and published patterns for related C2 subclades; they should be updated as denser sampling and higher-resolution sequencing data become available.

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 C2A1A2A2. 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 C2A1A2A2 Actual ~2,000 years ago Roman Period 2,000 years 1 0 0
2 C2A1A2A ~3,000 years ago Iron Age 3,000 years 1 0 0
3 C2A1A2 ~4,000 years ago Bronze Age 4,000 years 1 0 0
4 C2A1A ~6,000 years ago Chalcolithic 6,000 years 4 3 0
5 C2A1 ~12,000 years ago Neolithic 12,000 years 1 3 0
6 C2A ~18,000 years ago Mesolithic 18,000 years 1 38 0
7 C2 ~40,000 years ago Paleolithic 40,000 years 2 99 24
8 C ~60,000 years ago Paleolithic 60,000 years 3 406 35
Perfil de Referência

No mundo

Distribuição geográfica e presença moderna

Origem registada

Central–East Asia (Mongolia / Southern Siberia)

Distribuição moderna

The populations where Y-DNA haplogroup C2A1A2A2 is found include:

  1. Mongolic-speaking groups (e.g., Mongols, Buryats)
  2. Tungusic peoples of Siberia (e.g., Evenks, Evens, Oroqen)
  3. Sakha (Yakut) and other North Siberian populations
  4. Selected Turkic groups of southern Siberia (e.g., some Tuvan and Altai clans)
  5. Low-frequency occurrences in Northeast Asian populations (e.g., Koreans, Japanese)
  6. Very rare/isolated occurrences in some Indigenous North American samples

Presença regional

East Asia (Mongolia, Inner Mongolia, northern China) High
Central Asia (Kazakhstan, Kyrgyzstan – localized clans) Moderate
South Siberia (Buryatia, Tuva, adjacent regions) Moderate
Northeast Asia High
Northern Asia (Siberia) High
Northern Americas (rare) 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. ~10k años de antigüedad

    Revolução neolítica

    Início da agricultura e formação de comunidades sedentárias

  2. ~5k años de antigüedad

    Idade do Bronze

    Metalurgia, escrita e primeiras civilizações

  3. ~3k años de antigüedad

    Idade do Ferro

    Ferramentas de ferro e ampliação de redes comerciais

  4. ~2.5k años de antigüedad

    Antiguidades clássicas

    Desenvolvimento das civilizações grega e romana

  5. ~2k años de antigüedad

    Haplogrupo C2A1A2A2

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

    Este ramo
  6. Actualidad

    Actualidad

    Idade moderna

Perfil de Referência

Contexto arqueológico

Asociaciones arqueológicas registradas para la rama Y-DNA C2A1A2A2

Associações registradas

Esses rótulos descrevem os contextos arqueológicos registrados para as amostras de referência vinculadas a C2A1A2A2. Uma associação não demonstra que todos os portadores pertenceram a uma cultura ou seguiram uma rota migratória específica.

Boisman China_AmurRiverBasin_LatePaleolithic Irkutsk Culture Ob River Culture Russia_AltaiKrai_Eneolithic Russia_AltaiKrai_N Russia_AltaiKrai_N_Itkul Russia_EN_Kitoi Selenge Culture Xiongnu
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.