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mtDNA · 母亲 lineage

R9B1B

mtDNA Haplogroup R9B1B

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

mtDNA 谱系分支 R9B1B 的历史背景

Origins and Evolution

R9B1B is a downstream branch of mtDNA haplogroup R9B1, itself nested within the broader R9/R clade that is characteristic of East and Southeast Asia. Based on the phylogenetic position of R9B1B under R9B1 and the time depth of its parent clade, R9B1B most likely formed in southern China or mainland Southeast Asia during the transition from the Late Pleistocene to the early Holocene (early Holocene / terminal Pleistocene, roughly ~12–10 kya). Its emergence fits a regional pattern of diversification of maternal lineages associated with hunter‑gatherer populations that persisted in southern China and northern Southeast Asia and later mixed with expanding Neolithic farmer groups.

Subclades (if applicable)

At present, R9B1B is treated as a specific downstream branch beneath R9B1. Published phylogenies and population surveys indicate limited deep branching within R9B1B visible in public datasets, suggesting either a small number of distinctive subclades or incomplete sampling. Where present, sublineages of R9B1B show phylogeographic clustering in southern China, the Tai-Kadai–speaking zone, and among some Austronesian-speaking communities, consistent with localized diversification and founder effects during Holocene demographic events.

Geographical Distribution

R9B1B is concentrated in southern China and mainland Southeast Asia, with the highest frequencies observed in southern Chinese populations and among Tai-Kadai-speaking groups (e.g., Dai, Zhuang). The haplogroup also appears among Thai, Lao, Mon-Khmer populations (Vietnamese, Khmer), and in certain Austronesian-speaking groups (including Taiwanese indigenous peoples and parts of Island Southeast Asia). Low-frequency occurrences extend into Malay and Sea Nomad communities and have been detected at sparse levels in Near Oceania and in some southwestern Chinese and Tibeto-Burman groups. Ancient DNA records (four archaeology-associated samples recorded in the referenced database) confirm that R9B1-derived lineages were present in archaeological contexts in the region across the Holocene.

Historical and Cultural Significance

R9B1B reflects a pattern of long-term maternal continuity in southern China and mainland Southeast Asia followed by participation in later demographic processes. It is consistent with three broad, complementary events recognized in regional population genetics:

  1. Local Late Pleistocene/Holocene continuity — persistence and regional diversification of maternal lineages in refugial southern environments during climatic fluctuations.
  2. Neolithic influence and inland farmer–forager interaction — increased movement and gene flow associated with the spread of rice farming and associated cultural packages from the Yangtze and surrounding areas into Southeast Asia, leading to admixture with local lineages such as R9B1B.
  3. Austronesian and maritime dispersals — R9B1B occurs at variable frequencies in populations associated with Austronesian expansions (Taiwan to Island Southeast Asia and beyond), indicating a role for coastal and maritime migrations in carrying this lineage into island contexts and contributing to the maternal diversity of present-day Austronesian-speaking peoples.

Because R9B1B is regionally focused rather than pan-continental, it is useful in studies of fine-scale maternal structure in southern China and Southeast Asia and in reconstructing local founder events, sex-biased admixture, and postglacial demographic expansions.

Conclusion

R9B1B is a geographically focused mtDNA subclade emblematic of southern Chinese and mainland Southeast Asian maternal diversity. Its time depth in the early Holocene, association with both indigenous Tai-Kadai/Tai populations and later Austronesian-related groups, and modest presence in archaeological samples make it informative for reconstructing Holocene demographic processes across coastal and inland Southeast Asia. Continued targeted sampling and ancient DNA recovery in southern China and Southeast Asia will refine the internal structure, age estimates, and migratory history of R9B1B.

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 R9B1B。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 R9B1B 当前 ~12,000 years ago Neolithic 11,500 years 0 3 4
2 R9B1 ~18,000 years ago Mesolithic 18,000 years 2 10 0
3 R9B ~30,000 years ago Paleolithic 30,000 years 1 10 0
4 R9 ~40,000 years ago Paleolithic 40,000 years 3 281 0
5 R ~55,000 years ago Paleolithic 55,000 years 17 22,830 57
6 NA - - - 1 22,830 0
7 N ~60,000 years ago Paleolithic 60,000 years 16 26,150 13
8 L3 ~70,000 years ago Paleolithic 70,000 years 7 30,162 6
9 L3'4 - - - 2 30,212 0
10 L3'4'6 - - - 2 30,216 0
11 L2'3'4'6 - - - 2 31,333 0
12 L2'3'4'5'6'7 - - - 2 31,349 0
13 L1'2'3'4'5'6'7 - - - 2 31,852 0
14 L ~160,000 years ago Paleolithic 160,000 years 2 32,236 5

Subclades (0)

终端分支 -没有记录的子密钥

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

Southern China / Mainland Southeast Asia

现代发行

The populations where MTDNA haplogroup R9B1B is found include:

  1. Han Chinese (particularly southern Chinese groups)
  2. Dai, Zhuang and other Tai-Kadai speaking groups
  3. Thai and Lao populations
  4. Vietnamese and Khmer (Mon-Khmer) groups
  5. Austronesian-speaking groups (e.g., Taiwanese indigenous peoples, some Filipinos, Indonesians)
  6. Malay and Sea Nomad communities
  7. Some Tibeto-Burman and southwestern Chinese groups (low to moderate frequency)
  8. Indigenous populations of Near Oceania (low frequency)
  9. Ethnic minorities in southern China and northern Mainland Southeast Asia
  10. Sparse occurrences among broader East Asian populations
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. ~11.5k 年前

    Haplogroup R9B1B

    此 mtDNA 分支的形成时间为推定值,日期和地点仅作参考。

    这个分支
  2. ~10k 年前

    新石器革命

    农业开始,定居社区形成

  3. ~5k 年前

    青铜时代

    金属加工、书写和早期文明

  4. ~3k 年前

    铁器时代

    铁工具,扩大贸易网络

  5. ~2.5k 年前

    古典时代

    希腊和罗马文明蓬勃发展

  6. 现

    现日

    现代时代

参考简介

考古学背景

已记录的 mtDNA 分支 R9B1B 考古关联

有记录的协会

这些标签描述与 R9B1B 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 Coastal Neolithic Ganj Dareh Culture Huatuyan Culture Island Southeast Asian Culture Layi Culture Linear Pottery Culture Ming Dynasty Qinchang Culture Sardinian Neolithic Ust-Ishim Culture
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 R9B1B 的直接携带者 4 名

4 显示 ^ 4 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 mtDNA 匹配
AI生成的示例性肖像 Guangxi Qinchang Cave Northern And Southern Dynasties individual, Guangxi. Hechi City. Dahua Yao Autonomous County. Yantan Town. Qinchang Cave, China (406-543 CE)
Sample ID: QinchangKD14
China Qinchang Period China 406-543 calCE (1620±30 BP) Qinchang Culture R9b1b Direct
AI生成的示例性肖像 Guangxi Huatuyan Cave Ming Dynasty individual, Guangxi. Hechi City. Nandan County. Lihu Yaozu Town. Huatu Village. Huatuyan Cave, China (1,400-1,700 CE)
Sample ID: HuatuyanNL18
China China Guangxi Huatuyan Ming 1400-1700 CE Huatuyan Culture R9b1b Direct
AI生成的示例性肖像 East Asian Neolithic individual, Fujian. Zhangping. Wuyi-Nanling. Qihedong, China (6,474-6,401 BCE)
Sample ID: Qihe2
China Early Neolithic Coastal Southeast Asia, China 6474 BCE - 6401 BCE Coastal Neolithic R9b1b Direct
AI生成的示例性肖像 Asia Se Ep individual, Fujian. Zhangping. Wuyi-Nanling. Qihedong, China (6,474-6,401 BCE)
Sample ID: Qihe2
China Early Paleolithic Southeast Asia 6474 BCE - 6401 BCE R9b1b Direct
MATERNAL 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

4 个古代 DNA 样本的地理分布,涵盖 R9B1B 及其下游分支的携带者

直接承运人
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 2026-02-16
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。