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mtDNA · 母亲 lineage

M13

mtDNA Haplogroup M13

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 M13 的历史背景

Origins and Evolution

Haplogroup M13 sits within the larger macro-haplogroup M, a major branch of the non-African mitochondrial phylogeny that diversified rapidly after the Out-of-Africa dispersal. Given its position under the intermediate node M13'46'61, M13 most likely represents an early Paleolithic split of M that occurred as modern humans expanded across South and Southeast Asia. Coalescence time estimates for many M subclades typically fall in the range of ~40–60 kya; based on phylogenetic position and comparative age estimates for sibling clades, a plausible origin for M13 is in the Upper Paleolithic (on the order of 40–50 kya), although precise dating requires more sequence-based calibration and broader sampling.

Because M13 is a relatively rare and understudied lineage in many published datasets, interpretations of its internal structure and demographic history remain provisional. Ancient DNA sampling and expanded modern population surveys are necessary to refine timing and geography.

Subclades

As an intermediate clade within the M13'46'61 grouping, M13 may include downstream subclades identified in detailed mitogenome studies, but many of these remain sparsely sampled or are defined only by limited control-region variants in older studies. Known sister branches under the same parent (for example M46 and M61) help place M13 within a cluster of early M diversification across South and Southeast Asia. Where full mitochondrial genomes have been obtained, subclade definition improves; however, for M13 specifically, many putative subclades require further confirmation with complete mitogenomes.

Geographical Distribution

Based on available population genetics studies and reasonable phylogeographic inference, M13 is most reliably reported at low to moderate frequencies in parts of South Asia and at low frequencies across island Southeast Asia and Near Oceania. Scattered reports — often at very low frequency — exist in other regions, which can reflect ancient dispersals or more recent gene flow. Sampling bias (unequal sampling of indigenous and rural groups) and limited mitogenome resolution in some studies mean that apparent absences in some areas may simply reflect lack of data rather than true absence.

Key points about distribution:

  • Core signal: Likely centered in South or nearby regions of Southeast Asia where early M diversification is richest.
  • Island Southeast Asia / Near Oceania: Low-frequency occurrences may reflect ancient coastal dispersals or later maritime movements (including Austronesian-era gene flow) in some island populations.
  • Scattered occurrences: Occasional reports outside these regions can reflect long-distance dispersal, historic trade networks, or later migrations.

Historical and Cultural Significance

Because M13 is deep-rooted and generally rare, its most significant contribution is as a marker of early maternal diversification in South/Southeast Asia rather than being tied to a single archaeological culture. Interpretations in cultural terms are therefore cautious:

  • Paleolithic hunter-gatherer context: The origin timing places M13 within the Upper Paleolithic hunter-gatherer phase of human prehistory in South/Southeast Asia.
  • Neolithic and later periods: Low-frequency presence in some island and coastal populations means M13 could have been carried along coastal migration routes and later influenced by Neolithic farmer expansions and Austronesian movements; however, it is not a dominant Neolithic marker like some haplogroups associated strongly with farming expansions.
  • Modern population structure: In contemporary genetic surveys, M13 provides information about local maternal ancestry and deep regional continuity when observed in indigenous or isolated groups.

Conclusion

mtDNA M13 is best understood as a rare, ancient maternal lineage within macro-haplogroup M that likely arose in South or Southeast Asia in the Upper Paleolithic and persisted at low to moderate frequencies in the region. Its full phylogenetic complexity and precise prehistoric movements remain incompletely resolved due to limited sampling and mitogenome data; targeted whole-mitochondrial sequencing across understudied populations and integration with ancient DNA will clarify its subclades, age, and geographic history.

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 M13。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 M13 当前 ~45,000 years ago Paleolithic 45,000 years 2 6 0
2 M13'46'61 - - - 1 9 0
3 M ~60,000 years ago Paleolithic 60,000 years 42 2,671 41
4 L3 ~70,000 years ago Paleolithic 70,000 years 7 30,162 6
5 L3'4 - - - 2 30,212 0
6 L3'4'6 - - - 2 30,216 0
7 L2'3'4'6 - - - 2 31,333 0
8 L2'3'4'5'6'7 - - - 2 31,349 0
9 L1'2'3'4'5'6'7 - - - 2 31,852 0
10 L ~160,000 years ago Paleolithic 160,000 years 2 32,236 5
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 or Southeast Asia

现代发行

The populations where mtDNA haplogroup M13 is found include:

  1. Various South Asian populations (including some tribal and rural groups in the Indian subcontinent)
  2. Island and coastal populations of Southeast Asia (Indonesia, Philippines and nearby archipelagos) reported at low frequency
  3. Austronesian-speaking groups in Madagascar and parts of the Indian Ocean rim in isolated cases
  4. Near Oceanian and Melanesian groups at low frequency in some surveys (potentially reflecting ancient coastal dispersals)
  5. Occasional, low-frequency reports in East African coastal populations, likely reflecting historical or recent gene flow
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 M13

    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. ~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 mtDNA 分支 M13 考古关联

有记录的协会

这些标签描述与 M13 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。

British Neolithic Goyet Cave Gravettian Iberomaurusian Indonesian Hunter-Gatherer Culture Malaysian Neolithic Ostuni Culture Spanish Gravettian Vietnamese Neolithic
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 M13 的子分支携带者 7 名(当前选定的参考样本中没有直接携带者)

7 显示 ^ 7 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 Xinjiang Xikakandasayi Historical individual, Xinjiang. Bayinguoleng(Bayingolin) Region. Qiemo(Qarqan/Cherchen) County. Xikakandasayi, China (254-406 CE)
Sample ID: C795
China China Xinjiang Xikakandasayi Historical 254-406 calCE Xikakandasayi Culture M13a1b 下游分支
AI生成的示例性肖像 Qinghai Dulan Wayan Reservoir Site Classical individual, Dulan Wayan reservoir site (Dulan County, Reshui town), China (706-883 CE)
Sample ID: BB2006
China Dulan-Wayan Culture 706-883 calCE (1220±20 BP, LZU-18106) Dulan-Wayan M13a2 下游分支
AI生成的示例性肖像 Austronesian individual, West Peninsular Kelantan. Gua Cha Cave, Malaysia (744-398 BCE)
Sample ID: Ma912
Malaysia Malaysia LN 744 BCE - 398 BCE Malaysian Neolithic M13c 下游分支
AI生成的示例性肖像 Malaysia N individual, West Peninsular Kelantan. Gua Cha Cave, Malaysia (744-398 BCE)
Sample ID: Ma912
Malaysia Neolithic Malaysia 744 BCE - 398 BCE M13c 下游分支
AI生成的示例性肖像 Tibet Longsangquduo individual, Longsangquduo (Shigatse), China (900-1,200 CE)
Sample ID: C5154
China Tibetan Plateau (Longsangquduo) 900-1200 CE Longsangquduo Culture M13a2 下游分支
AI生成的示例性肖像 Austroasiatic individual, Man Bac, Vietnam (1,889-1,742 BCE)
Sample ID: I1859
Vietnam Vietnam N 1889 BCE - 1742 BCE Vietnamese Neolithic M13b 下游分支
AI生成的示例性肖像 Vietnam N individual, Man Bac, Vietnam (1,889-1,742 BCE)
Sample ID: I1859
Vietnam Vietnam N 1889 BCE - 1742 BCE Vietnamese Neolithic M13b 下游分支
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

7 个古代 DNA 样本的地理分布,涵盖 M13 及其下游分支的携带者

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 2026-06-14
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。