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Y-DNA · 父权 lineage

C1B2A1

Y-DNA Haplogroup C1B2A1

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 C1B2A1 的历史背景

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.

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 C1B2A1。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 C1B2A1 当前 ~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

Subclades (0)

终端分支 -没有记录的子密钥

参考简介

哪里是这个世界

地理分布和现代存在

记录来源

Wallacea (Island Southeast Asia)

现代发行

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)

区域存在

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
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. ~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

  2. ~14k 年前

    Haplogroup C1B2A1

    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. ~10k 年前

    新石器革命

    农业开始,定居社区形成

  4. ~5k 年前

    青铜时代

    金属加工、书写和早期文明

  5. ~3k 年前

    铁器时代

    铁工具,扩大贸易网络

  6. ~2.5k 年前

    古典时代

    希腊和罗马文明蓬勃发展

  7. 现

    现日

    现代时代

参考简介

考古学背景

已记录的 Y-DNA 分支 C1B2A1 考古关联

有记录的协会

这些标签描述与 C1B2A1 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。

1983 Ancient Polynesian Botocudo Historic Polynesian Hoabinhian Late Vanuatu Post-Lapita Vanuatu Saudeleur Culture Vanuatu Historical
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。