跳转到主内容
mtDNA · 母亲 lineage

B4C1B

mtDNA Haplogroup B4C1B

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 B4C1B 的历史背景

Origins and Evolution

mtDNA haplogroup B4C1B sits within the broader B4 maternal lineage, a clade that arose in East Asia during the Late Pleistocene to early Holocene and later diversified into numerous regional subclades. B4C1B is defined as a downstream branch of the intermediate node B4C1A'B (a substructure within the B4C complex). Based on the phylogenetic position of B4C1B relative to other B4 subclades and comparative coalescence estimates for B4 lineages, a reasonable inference places the origin of B4C1B in the early Holocene (roughly 10–15 kya), likely associated with post-glacial population structure and coastal or riverine forager populations in northeastern/coastal East Asia. However, direct molecular-clock dating specific to B4C1B is limited, so the estimate above is provisional.

Subclades (if applicable)

As an intermediate/terminal branch in Phylotree-style classifications, B4C1B may contain minor internal variation (private mutations) detectable only with full mitogenome sequencing. Published references and public databases show that many B4C sublineages are split into A and B branches (e.g., B4C1A, B4C1B), with sister clades sometimes restricted to particular islands, coastal areas, or ethnolinguistic groups. At present, comprehensive subclade resolution for B4C1B is incomplete: additional complete mtDNA genomes and phylogenetic curation are needed to resolve any internal branching and to name downstream subclades robustly.

Geographical Distribution

Available data and reasonable phylogeographic inference indicate that B4C1B is primarily found in East Asia, with strongest signals from northeastern and coastal regions. Sporadic occurrences or related B4C lineages have been reported in neighboring areas (e.g., parts of Southeast Asia, Taiwan, and island Northeast Asia), suggesting limited dispersal or gene flow from core East Asian source populations. Because sampling density for many small indigenous groups and ancient remains remains uneven, the apparent distribution may expand as targeted mitogenome studies increase.

Key points about distribution:

  • The clade is best described as regional rather than pan-Asian, with higher likelihood in coastal and Northeast Asian contexts.
  • Co-occurrence with other Northeast Asian maternal lineages (e.g., D4 subclades, N9b in some contexts) is expected in mixed coastal or island populations.
  • Low-frequency detections in Southeast Asia or Pacific-adjacent groups cannot be excluded but require confirmation with full mitogenomes.

Historical and Cultural Significance

Because B4C1B is a relatively deep East Asian subclade, it likely reflects post-glacial population structure and the demographic dynamics of Holocene coastal foragers and early sedentary communities. Potential cultural associations (based on geography and time depth) include:

  • Early Holocene coastal hunter-gatherers and later regional Mesolithic/Neolithic communities in northeastern/coastal East Asia.
  • Possible presence in prehistoric populations that contributed maternally to modern Japanese, Ryukyuan, Korean, and some Tungusic or Amur-region groups, though the degree of contribution is uncertain.
  • Unlike the widely dispersed Austronesian-associated B4a Polynesian motif, B4C1B appears to be a more regionally constrained lineage and therefore is less directly tied to long-range maritime expansions.

Overall, the cultural-significance picture for B4C1B is one of a regional maternal lineage that helps reconstruct local maternal ancestries and migrations across the early Holocene in East Asia.

Conclusion

B4C1B is a useful phylogenetic marker within the B4 family for studying maternal population structure in northeastern and coastal East Asia. Current evidence points to an early Holocene origin and a regional distribution, but the haplogroup remains undersampled: full mitogenome sequencing of both modern and ancient individuals from targeted regions (northeast/coastal East Asia, Taiwan, northern Japan, and nearby islands) is needed to refine age estimates, define internal substructure, and clarify historical movements associated with this lineage. Until such data are available, statements about precise distribution and cultural ties should be regarded as provisional and hypothesis-generating.

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 B4C1B。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 B4C1B 当前 ~12,000 years ago Neolithic 12,000 years 1 13 3
2 B4C1A'B - - - 2 20 0
3 B4C1 ~6,000 years ago Chalcolithic 6,500 years 2 20 0
4 B4C ~9,000 years ago Neolithic 9,000 years 2 21 3
5 B4 ~28,000 years ago Paleolithic 28,000 years 4 1,122 7
6 B4'5 ~40,000 years ago Paleolithic 40,000 years 2 1,432 0
7 RA - - - 3 1,452 0
8 R ~55,000 years ago Paleolithic 55,000 years 17 22,830 57
9 NA - - - 1 22,830 0
10 N ~60,000 years ago Paleolithic 60,000 years 16 26,150 13
11 L3 ~70,000 years ago Paleolithic 70,000 years 7 30,162 6
12 L3'4 - - - 2 30,212 0
13 L3'4'6 - - - 2 30,216 0
14 L2'3'4'6 - - - 2 31,333 0
15 L2'3'4'5'6'7 - - - 2 31,349 0
16 L1'2'3'4'5'6'7 - - - 2 31,852 0
17 L ~160,000 years ago Paleolithic 160,000 years 2 32,236 5

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 Asia (Northeast Asia)

现代发行

The populations where mtDNA haplogroup B4C1B is found include:

  1. Northeast Asian populations (e.g., regions of northern Japan and neighboring coastal areas)
  2. Mainland East Asian groups (sampled individuals from Korean and northeastern Chinese contexts)
  3. Insular East Asian populations (e.g., parts of the Ryukyu/Izu island chains where regional B4 lineages appear)
  4. Indigenous coastal forager-descended groups in the Amur and adjacent littoral zones
  5. Occasional/low-frequency reports in nearby Southeast Asian or Taiwanese samples (pending confirmation with full mitogenomes)
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. ~12k 年前

    Haplogroup B4C1B

    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 B4C1B 考古关联

有记录的协会

这些标签描述与 B4C1B 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。

China_Tibet_Sangdalongguo_IA Chinese Paleolithic Coastal Neolithic Early Avar Ming Dynasty Tianyuan Culture Upper Yellow River 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 B4C1B 的子分支携带者 3 名(当前选定的参考样本中没有直接携带者)

3 显示 ^ 3 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 Early Avar-o High East Asia individual, Kunpeszér-Felsőpeszéri út (Bács-Kiskun County), Hungary (580-670 CE)
Sample ID: KUP024
Hungary Hungary EarlyAvar 550-700 CE Early Avar B4c1b2 下游分支
AI生成的示例性肖像 Early Avar-o High East Asia individual, Kunpeszér-Felsőpeszéri út (Bács-Kiskun County), Hungary (580-670 CE)
Sample ID: KUP026
Hungary Hungary EarlyAvar 550-700 CE Early Avar B4c1b2 下游分支
AI生成的示例性肖像 Early Avar-o High East Asia individual, Bács-Kiskun County. Kunpeszér-Felsőpeszériút. Homokbánya, Hungary (625-675 CE)
Sample ID: KFP-31
Hungary Hungary EarlyAvar 600-700 CE Early Avar B4c1b2 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

3 个古代 DNA 样本的地理分布,涵盖 B4C1B 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。