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Y-DNA · 父权 lineage

C1A

Y-DNA Haplogroup C1A

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 C1A 的历史背景

Origins and Evolution

Haplogroup C1A (commonly written C1a in many phylogenies) is an early branching lineage within haplogroup C that arose during the Upper Paleolithic after the initial migration of non-African Y-chromosome lineages into Eurasia. Based on its phylogenetic position under C1, coalescent estimates and the distribution of descendant lineages place its origin roughly in the Late Pleistocene (on the order of ~40–50 kya), probably somewhere in East to Southeast Eurasia, with subsequent regional differentiation.

C1A is best understood as a split that produced geographically distinct descendant clades which persisted in different refugia and later demographic contexts. The pattern of deep divergence combined with very restricted modern distributions indicates an ancient widespread presence followed by strong regional drift, founder effects, and local continuity in some areas (notably the Japanese archipelago) and near-extirpation or low frequency in others (notably parts of Europe).

Subclades (if applicable)

  • C1a1 (C-M8): A lineage concentrated in Japan today and well-documented in Jomon-associated and modern Japanese populations (including Ainu and Ryukyuan groups). This subclade shows a clear pattern of long-term local continuity within the Japanese islands.

  • C1a2 (C-V20): A lineage recorded in Palaeolithic and Mesolithic European hunter-gatherer remains and present at very low frequencies in some modern European populations. C-V20 represents an ancient westward branch of C1A that survived in Europe in relict form among hunter-gatherer groups.

  • Additional very rare or unclassified early-branching lineages have been reported sporadically in Eurasia and reflect deep substructure within C1A at low modern frequency.

Geographical Distribution

The modern distribution of C1A is fragmented and marked by strong regional signals in two principal zones:

  • East Asia (Japan): High relative prevalence of the C-M8 subclade in certain Japanese populations, including indigenous Ainu and Ryukyuan groups, and presence among people with Jomon ancestry signals long-term continuity.

  • Europe (ancient / rare modern occurrences): C-V20 appears in Upper Paleolithic and Mesolithic European samples and survives at very low frequencies in some contemporary Europeans, indicating an ancient presence followed by replacement or dilution by later population movements.

Outside these focal areas, C1A occurs only sporadically in Northeast Asia and parts of Central Asia at very low frequencies, consistent with ancient dispersal routes and later population turnovers.

Historical and Cultural Significance

Because C1A lineages are tied to Upper Paleolithic and Mesolithic contexts, they are particularly informative for reconstructing very early population structure in Eurasia and for tracing local continuity in regions with deep pre-Neolithic occupation.

  • In the Japanese archipelago, the association of C-M8 with Jomon-related ancestry makes C1A an important marker for studies of prehistoric peopling, island isolation, and the genetic legacy of pre-agricultural societies.

  • In Europe, the presence of C-V20 in Paleolithic and Mesolithic remains highlights the diversity of male lineages among early hunter-gatherers and helps contrast continental hunter-gatherer genetic substrates with later Neolithic and Bronze Age expansions.

C1A is generally not associated with major Late Neolithic or Bronze Age expansions (e.g., Steppe-associated Y-DNA influxes), which explains its low frequency in many modern continental populations and its role as a marker of older substrata.

Conclusion

Y-DNA haplogroup C1A exemplifies an ancient Eurasian paternal lineage that split early within haplogroup C and subsequently persisted in geographically restricted refugia. Its main scientific value lies in illuminating Upper Paleolithic and Mesolithic population structure — especially continuity in the Japanese archipelago and relict distributions among European hunter-gatherers — and in serving as a contrast to the later, large-scale demographic events that reshaped Eurasian Y-chromosome diversity.

关键点

  • Origins and Evolution
  • Subclades (if applicable)
  • 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 C1A。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 C1A 当前 ~45,000 years ago Paleolithic 45,000 years 2 56 2
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

Siblings (1)

来自同一父分支的分支( oplogroup)

参考简介

哪里是这个世界

地理分布和现代存在

记录来源

East / Southeast Asia (Eurasia)

现代发行

The populations where Y-DNA haplogroup C1A is found include:

  1. Japanese populations (notably Ainu and Ryukyuan groups)
  2. Ancient European hunter-gatherers (Upper Paleolithic / Mesolithic remains)
  3. Sporadic modern occurrences in Western and Southern Europe (very low frequency)
  4. Northeast Asian and Siberian groups (rare, scattered samples)
  5. Low-frequency reports from some Central Asian populations

区域存在

Western Europe Low
East Asia (islands) Moderate
Northern Asia / Siberia Low
Northeast Asia / Siberia Low
Central Asia 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. ~50k 年前

    上旧石器

    高级工具制造、艺术和文化爆炸

  2. ~45k 年前

    Haplogroup C1A

    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
  3. ~20k 年前

    上一个冰川最大值

    上一个冰河时代的高峰,人口隔离

  4. ~10k 年前

    新石器革命

    农业开始,定居社区形成

  5. ~5k 年前

    青铜时代

    金属加工、书写和早期文明

  6. ~3k 年前

    铁器时代

    铁工具,扩大贸易网络

  7. ~2.5k 年前

    古典时代

    希腊和罗马文明蓬勃发展

  8. 现

    现日

    现代时代

参考简介

考古学背景

已记录的 Y-DNA 分支 C1A 考古关联

有记录的协会

这些标签描述与 C1A 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。

Anatolian Epipaleolithic Goyet Cave Pavlovian Culture Solutrean Sunghir Culture Turkey_Catalhoyuk_EN Turkey_Catalhoyuk_MN
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.
参考简介

样本目录

单倍群 C1A 的直接携带者 1 名,子分支携带者 1 名

2 显示 ^ 2 匹配样本

Portraits是AI生成的插图,样本标签和加入ID识别参考记录.

纵向 样本 国家 大纪元 日期 文化 Y-DNA 匹配
AI生成的示例性肖像 European Paleolithic individual, Troisieme caverne of Goyet cave, Belgium (33,678-32,771 BCE)
Sample ID: GoyetQ116-1
Belgium Upper Paleolithic Goyet Cave Q116-1, Belgium 33678 BCE - 32771 BCE Goyet Cave C1a Direct
AI生成的示例性肖像 Grand Est Bas Rhin EN individual, Grand-Est (East). Schwindratzheim. Lotissement Les Terrasses de la Zorn, France (5,250-4,900 BCE)
Sample ID: Schw72-15
France Early Neolithic Grand Est, France 5250-4900 BCE Linear Pottery Culture C1a2 下游分支
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。

参考简介

载体分布图

2 个古代 DNA 样本的地理分布,涵盖 C1A 及其下游分支的携带者

直接承运人 子舱载体
时间段过滤器
所有时间段
显示全部样本
参考简介

时间分布

载体在考古时期的分布

参考简介

地理分布

按有记录的抽样国家计算,反映的是现有的参考选择,而不是人口频率。

参考简介

国家 × 大纪元发行

比较各国和考古时期记录的样本数量。选择一个人口密集的细胞来检查样本。

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。