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Y-DNA · 父权 lineage

C2A1A2A2

Y-DNA Haplogroup C2A1A2A2

一个家族分支的参考简介 。 共享haplogroups 无法建立家庭关系或文化认同 。

参考简介

部门背景

Y-DNA 谱系分支 C2A1A2A2 的历史背景

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.

关键点

  • Origins and Evolution
  • Subclades
  • Geographical Distribution
  • Historical and Cultural Significance
  • Conclusion
参考简介

树形关系( N)

phylgenetic 上下文和子拼写

进化路径

沿已记录的上级分支追溯至 C2A1A2A2。年代为估计值,可能随参考数据更新而调整。

步骤 单倍群 年龄估计 考古时代 时间流逝 直系后裔 被测试的现代后裔 古代连接
1 C2A1A2A2 当前 ~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
参考简介

哪里是这个世界

地理分布和现代存在

记录来源

Central–East Asia (Mongolia / Southern Siberia)

现代发行

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

区域存在

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
历史背景

分枝穿越时间

大致历史时间范围内的估计形成情况:周期标志提供了背景,并不意味着与特定文化的联系。

  1. ~10k 年前

    新石器革命

    农业开始,定居社区形成

  2. ~5k 年前

    青铜时代

    金属加工、书写和早期文明

  3. ~3k 年前

    铁器时代

    铁工具,扩大贸易网络

  4. ~2.5k 年前

    古典时代

    希腊和罗马文明蓬勃发展

  5. ~2k 年前

    Haplogroup C2A1A2A2

    此 Y-DNA 分支的形成时间为推定值,日期和地点仅作参考。

    这个分支
  6. 现

    现日

    现代时代

参考简介

考古学背景

已记录的 Y-DNA 分支 C2A1A2A2 考古关联

有记录的协会

这些标签描述与 C2A1A2A2 相关的参考样本所处的考古背景。仅凭这种关联,无法判断所有携带者都属于某种文化或沿同一路线迁徙。

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
文化任务基于古代DNA样本的考古背景,可能代表特定时期的区域协会.
PATERNAL LINEAGE · ANCIENT DNA

古代世系证据地图

跟随母舰飞向这个分支 探索古代载体的发现地点

正在装入古老的观测...

标记是考古发现地点。一个破碎的连接器是连续分支之间一种不确定的、拟议中的地理过渡,辅以多个日期的观察;它不是一个准确的旅行路线、出生地或直接血统的证明。父系样本可能属于其他后代分支。在证据不足的地方,差距依然存在。样本日期与随机群形成日期不同。

数据

数据证明( P)

来源信息和数据质量

上次更新 2026-06-15
信心分数 50/100
覆盖范围 Low

数据来源

分类、估计日期和地理背景反映了所记录的参考数据,随着证据的修订而可能发生变化,样本覆盖范围不均匀;所记录的地点和考古协会没有确定个人出身或文化特征。