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mtDNA · 母亲 lineage

R30B1

mtDNA Haplogroup R30B1

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 R30B1 的历史背景

Origins and Evolution

mtDNA haplogroup R30B1 is a downstream subclade of R30B, itself a branch of the broader R30 lineage. Given the parent R30B has an estimated time depth near the Early Holocene (~12 kya) and the observed low, localized diversity of R30B-derived lineages, R30B1 most likely arose on the South Asian subcontinent during the Early–to–Mid Holocene (roughly ~9 kya) as a locally differentiated maternal lineage. The pattern—low frequency and deep regional localization—is consistent with many South Asian-specific R- and M-derived lineages that formed as small, structured populations expanded and fragmented after the Last Glacial Maximum and into the Holocene.

Genetically, R30B1 carries the diagnostic mutations that define R30B with one or more additional private mutations that distinguish it as a named subclade; published population screens and sequence-based studies report only sporadic occurrences, indicating limited demographic expansion compared with some other South Asian maternal clades.

Subclades

At present, R30B1 is a low-diversity clade in available sequence databases and population surveys. Detailed high-resolution mitogenome sequencing in South Asian samples has identified R30B1 as a distinct branch off R30B, but internal substructure within R30B1 is limited in published datasets. Ongoing and future complete mitogenome surveys could reveal additional internal subclades, but currently R30B1 is best treated as a small, regionally restricted sublineage.

Geographical Distribution

R30B1 displays a geographically focused distribution centered on South Asia with rare detections beyond the subcontinent. Modern survey results and forensic/population studies report the haplogroup in diverse Indian populations (tribal, caste, and regional groups), occasional Pakistani and Sri Lankan samples, and very sporadic occurrences in neighboring regions of Central and West Asia and limited Southeast Asian surveys. A small number of detections are also recorded among diasporic South Asian communities. In total, R30B1 is represented by only a handful of modern sequences and a few (four) ancient DNA samples in curated databases, consistent with a long-standing but low-frequency presence in the region.

Historical and Cultural Significance

Because R30B1 is neither common nor widely dispersed, its historical signal is subtle: it likely reflects localized maternal continuity among South Asian populations through the Holocene rather than a major migratory expansion. Its presence in diverse social strata (tribal groups, caste communities, and regional populations) suggests deep, pre-historic establishment in the region prior to later historical processes that reshaped South Asian demography (for example, Bronze Age urbanization, medieval migrations, and historical trade-related movements). The identification of R30B1 in a small number of archaeological samples demonstrates it was present in some past populations sampled by aDNA studies, supporting continuity scenarios at local scales.

Conclusion

R30B1 is an informative example of a low-frequency, regionally restricted South Asian maternal lineage. It contributes to the picture of South Asia as a region of high maternal diversity with many deep, locally evolved haplogroups. While not a marker of large-scale prehistoric movements, R30B1 helps trace microevolutionary and genealogical histories within the subcontinent; fuller understanding will depend on expanded whole-mitogenome sampling of modern and ancient South Asian populations.

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 R30B1。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 R30B1 当前 ~9,000 years ago Neolithic 9,000 years 0 2 0
2 R30B ~12,000 years ago Neolithic 12,000 years 2 17 5
3 R30 ~15,000 years ago Mesolithic 15,000 years 2 37 0
4 R ~55,000 years ago Paleolithic 55,000 years 17 22,830 57
5 NA - - - 1 22,830 0
6 N ~60,000 years ago Paleolithic 60,000 years 16 26,150 13
7 L3 ~70,000 years ago Paleolithic 70,000 years 7 30,162 6
8 L3'4 - - - 2 30,212 0
9 L3'4'6 - - - 2 30,216 0
10 L2'3'4'6 - - - 2 31,333 0
11 L2'3'4'5'6'7 - - - 2 31,349 0
12 L1'2'3'4'5'6'7 - - - 2 31,852 0
13 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

South Asia

现代发行

The populations where mtDNA haplogroup R30B1 is found include:

  1. Diverse populations of the Indian subcontinent (including tribal groups, caste communities, and regional populations)
  2. Pakistani population samples (sporadic detections)
  3. Sri Lankan populations (rare detections)
  4. Central Asian groups (occasional detections in some Uzbek/Tajik samples)
  5. Populations on the Iranian plateau and parts of West Asia (low frequency, occasional)
  6. Southeast Asian populations in limited surveys (rare occurrences)
  7. Diasporic South Asian communities globally (low frequency detections)
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. ~9k 年前

    Haplogroup R30B1

    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
  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 R30B1 考古关联

有记录的协会

这些标签描述与 R30B1 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。

Barikot Boisman Cambodian Iron Age China_Tibet_Sangdalongguo_IA Ganj Dareh Culture Katelai Culture Linear Pottery Culture Loebanr Culture Roopkund Culture Shahr-i Sokhta Culture Taiwanese Iron 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 R30B1 的直接携带者 5 名

5 显示 ^ 5 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 Historic H individual, Swat Valley. Barikot, Pakistan (45 BCE-66 CE)
Sample ID: I7714
Pakistan Historic Barikot 46 calBCE - 66 calCE (2005±20 BP, PSUAMS-6207) Barikot R30b1 Direct
AI生成的示例性肖像 Tibet Sangdalongguo IA individual, Sangdalongguo (Tibet, Ngari Prefecture), China (374-26 BCE)
Sample ID: SDLG8
China China Tibet Sangdalongguo IA 350-50 BCE China_Tibet_Sangdalongguo_IA R30b1 Direct
AI生成的示例性肖像 IA individual, Swat Valley. Loebanr, Pakistan (1,000-800 BCE)
Sample ID: I10001
Pakistan The Loebanr Iron Age Culture of Pakistan 1000-800 BCE Loebanr Culture R30b1 Direct
AI生成的示例性肖像 IA individual, Swat Valley. Loebanr, Pakistan (1,000-800 BCE)
Sample ID: I12985
Pakistan The Loebanr Iron Age Culture of Pakistan 1000-800 BCE Loebanr Culture R30b1 Direct
AI生成的示例性肖像 IA individual, Swat Valley. Katelai, Pakistan (1,000-800 BCE)
Sample ID: I12447
Pakistan The Pakistan Katelai Iron Age Culture 1000-800 BCE Katelai Culture R30b1 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

5 个古代 DNA 样本的地理分布,涵盖 R30B1 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。