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mtDNA · 母亲 lineage

N9B

mtDNA Haplogroup N9B

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 N9B 的历史背景

Origins and Evolution

mtDNA haplogroup N9b is a daughter lineage of macro-haplogroup N9, itself derived from macro-haplogroup N. Based on phylogenetic placement and coalescence estimates for closely related N9 subclades, N9b most likely diversified in Northeast/East Asia during the Late Upper Paleolithic to early Holocene (roughly ~20–15 kya, here approximated as ~18 kya). Its emergence fits the broader pattern of mitochondrial diversification in East Asia following the Last Glacial Maximum, when populations expanded locally and recolonized temperate zones.

Subclades

N9b contains several internal branches (often reported in the literature as N9b1, N9b2, etc.) with different geographic emphases. Some sublineages show strong localization within the Japanese archipelago (including lineages associated with the indigenous Jomon and later Ryukyu populations), while others are found at low frequencies across continental Northeast Asia. The internal structure indicates both deep persistence in island populations and occasional gene flow between islands and the mainland.

Geographical Distribution

N9b is most frequent and characteristic in the Japanese archipelago, especially in populations with greater retention of indigenous maternal lineages (e.g., some Ainu- and Ryukyu-associated groups), and in ancient Jomon samples. It is also present at lower frequencies among mainland East Asian populations (Koreans, some Han Chinese groups), and among some Siberian/Far Eastern groups (e.g., Nivkh, Ulchi) where contact with coastal Northeast Asians occurred. Scattered low-frequency occurrences appear in parts of Southeast Asia and Central Asia, typically interpreted as resulting from prehistoric or historic gene flow.

Historical and Cultural Significance

Because of its concentration in Jomon-associated remains and in modern populations of the Japanese islands, N9b is widely used as a maternal marker for studying prehistoric population continuity and isolation in Japan. The persistence of N9b lineages in island populations through the Holocene supports models where pockets of maternal ancestry survived regional cultural transitions (for example, the transition from Jomon to Yayoi in parts of the archipelago) and contributed to the modern genetic landscape. N9b's distribution also informs reconstructions of coastal and inland contacts between Northeast Asia and the archipelagos.

Conclusion

N9b is a regionally informative mtDNA lineage that reflects a mixture of deep local continuity in the Japanese islands and limited but detectable connections with mainland Northeast Asia and adjacent regions. Its pattern—relatively high frequency in specific island populations and low frequency on the continent—is consistent with a Late Upper Paleolithic origin followed by localized persistence and occasional dispersal during the Holocene.

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 N9B。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 N9B 当前 ~18,000 years ago Mesolithic 18,000 years 3 0 21
2 N9 ~25,000 years ago Paleolithic 25,000 years 3 178 0
3 N ~60,000 years ago Paleolithic 60,000 years 16 26,150 13
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

Siblings (2)

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/East Asia)

现代发行

The populations where mtDNA haplogroup N9B is found include:

  1. Japanese populations (notably in Hokkaido, Tohoku, and Ryukyu/Okinawa regions)
  2. Ancient Jomon-era remains from the Japanese archipelago
  3. Ainu and Ryukyuan-related modern groups with elevated indigenous maternal ancestry
  4. Koreans and some Northeast Asian mainland populations (lower frequencies)
  5. Indigenous peoples of the Far East / coastal Siberia (e.g., Nivkh, Ulchi; sporadic occurrences)
  6. Han Chinese and other East Asian populations at low frequencies
  7. Southeast Asian populations (rare and localized occurrences)
  8. Central Asian and West Eurasian occurrences that are generally rare and attributable to later or sparse prehistoric gene flow
  9. Modern urban and mixed populations across East and Southeast Asia due to recent admixture
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. ~18k 年前

    Haplogroup N9B

    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. ~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 mtDNA 分支 N9B 考古关联

有记录的协会

这些标签描述与 N9B 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。

Early Jomon Initial Jomon Jomon
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 N9B 的直接携带者 12 名,子分支携带者 9 名

10 显示 ^ 21 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 East Asian individual, Tohoku. Fukushima. Sanganji Shell Mound, Japan (1,370-1,127 BCE)
Sample ID: Sanganji131421-3
Japan The Jomon Period in Japan 1370 BCE - 1127 BCE Jomon N9b Direct
AI生成的示例性肖像 Jomon individual, Tohoku. Fukushima. Sanganji Shell Mound, Japan (1,370-1,127 BCE)
Sample ID: Sanganji131421-3
Japan The Jomon Period in Japan 1370 BCE - 1127 BCE N9b Direct
AI生成的示例性肖像 Jomon individual, Tohoku. Fukushima. Sanganji Shell Mound, Japan (1,370-1,127 BCE)
Sample ID: Sanganji131421-3
Japan The Jomon Period in Japan 1370 BCE - 1127 BCE N9b Direct
AI生成的示例性肖像 Jomon individual, Tohoku. Fukushima. Sanganji Shell Mound, Japan (1,370-1,127 BCE)
Sample ID: Sanganji131421-3
Japan The Jomon Period in Japan 1370 BCE - 1127 BCE N9b Direct
AI生成的示例性肖像 Chiba HG Jomon individual, Rokutsu Shell Mound, Japan (1,382-1,134 BCE)
Sample ID: I13885
Japan Jomon Period Japan 1382-1134 calBCE (3015±20 BP, PSUAMS-7945) Jomon N9b Direct
AI生成的示例性肖像 Chiba HG Jomon individual, Rokutsu Shell Mound, Japan (1,386-1,212 BCE)
Sample ID: I13882
Japan Jomon Period Japan 1386-1212 calBCE (3025±20 BP, PSUAMS-7937) Jomon N9b Direct
AI生成的示例性肖像 East Asian individual, Tohoku. Fukushima. Sanganji Shell Mound, Japan (1,404-1,263 BCE)
Sample ID: Sanganji131464
Japan The Jomon Period in Japan 1404 BCE - 1263 BCE Jomon N9b Direct
AI生成的示例性肖像 Jomon individual, Tohoku. Fukushima. Sanganji Shell Mound, Japan (1,404-1,263 BCE)
Sample ID: Sanganji131464
Japan The Jomon Period in Japan 1404 BCE - 1263 BCE N9b Direct
AI生成的示例性肖像 Jomon individual, Tohoku. Fukushima. Sanganji Shell Mound, Japan (1,404-1,263 BCE)
Sample ID: Sanganji131464
Japan The Jomon Period in Japan 1404 BCE - 1263 BCE N9b Direct
AI生成的示例性肖像 Jomon individual, Tohoku. Fukushima. Sanganji Shell Mound, Japan (1,404-1,263 BCE)
Sample ID: Sanganji131464
Japan The Jomon Period in Japan 1404 BCE - 1263 BCE N9b 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

21 个古代 DNA 样本的地理分布,涵盖 N9B 及其下游分支的携带者

直接承运人 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 2026-02-16
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。