ื“ื™ืœื•ื’ ืœืชื•ื›ืŸ ื”ืจืืฉื™
Y-DNA ยท ืฉื•ืฉืœืช אבהית

O2A1B1A1A1A1E1A1

Y-DNA Haplogroup O2A1B1A1A1A1E1A1

ืคืจื•ืคื™ืœ ื™ื™ื—ื•ืก ืฉืœ ืขื ืฃ ืฉื•ืฉืœืช ืื—ื“. ืงื‘ื•ืฆื” ื”ืคืœื•ื’ืจื•ืคื™ืช ืžืฉื•ืชืคืช ืื™ื ื” ืงื•ื‘ืขืช ืงืฉืจ ืžืฉืคื—ืชื™ ื•ืื™ื ื” ืžื’ื“ื™ืจื” ื–ื”ื•ืช ืชืจื‘ื•ืชื™ืช.

ืคืจื•ืคื™ืœ ื”ื™ื™ื—ื•ืก

ืจืงืข ื”ืขื ืฃ

ื”ื”ืงืฉืจ ื”ื”ื™ืกื˜ื•ืจื™ ืฉืœ ืขื ืฃ O2A1B1A1A1A1E1A1 ื‘ืฉื•ืฉืœืช Y-DNA

Origins and Evolution

Y-DNA haplogroup O2A1B1A1A1A1E1A1 is a highly derived subclade of the broader O2 paternal lineage, which is one of the major Y-chromosome lineages associated with East Asian populations. Because it sits several branches downstream from O2, this lineage is expected to have very shallow time depth, likely emerging during the late Holocene through localized diversification rather than representing an ancient deep split.

As a terminal or near-terminal branch of a recent East Asian lineage, O2A1B1A1A1A1E1A1 likely reflects microevolutionary processes such as drift, founder effects, and localized population growth. In practical terms, this means the haplogroup is probably uncommon overall but may be detectable at low frequency within specific regional or ethnolinguistic groups.

Subclades

Because this lineage is extremely downstream, its known phylogenetic context is primarily defined by its relationship to its parent clade O2A1B1A1A1A1E1A. Additional downstream substructure may exist, but unless sampled extensively in regional sequencing studies, such internal branching may remain poorly resolved or private to specific families and local populations.

In comparative population genetics, this kind of deep-but-recent subclade often appears in datasets as a rare marker of recent paternal ancestry rather than a widespread historical lineage. Its phylogenetic significance lies in helping connect broad regional O2 diversity to finer-scale population history.

Geographical Distribution

The distribution of O2A1B1A1A1A1E1A1 is expected to be centered in East Asia, with possible extension into southern China, mainland Southeast Asia, and adjacent regions where O2 subclades are common. Based on the parent clade context, it may occur in Han Chinese, related southern Chinese groups, and nearby populations with historical gene flow from East Asian source populations.

Low-frequency presence in Korean, Japanese, Tibeto-Burman, and some Austronesian-speaking groups is also plausible, especially in populations shaped by repeated migrations and admixture across East and Southeast Asia. However, any such occurrences would likely be sparse and highly local.

Historical and Cultural Significance

There is no strong evidence to associate this exact subclade with a single archaeological culture, but its broader O2 ancestry is commonly linked to Holocene demographic expansions in East Asia, including the spread of farming populations, language dispersals, and regional population growth during the Neolithic and later periods.

For a very recent branch like O2A1B1A1A1A1E1A1, historical significance is usually found at the family or community level rather than in major prehistoric migration events. It may represent a lineage that expanded within a localized population, potentially tied to surname lineages, clan histories, or small-scale regional demographic events in historical China and neighboring areas.

Conclusion

Y-DNA haplogroup O2A1B1A1A1A1E1A1 is a very recent East Asian paternal lineage nested within the expansive O2 branch. Its rarity and narrow phylogenetic position suggest localized formation and limited geographic spread, making it most useful for fine-scale ancestry reconstruction rather than broad deep-time population history.

ื ืงื•ื“ื•ืช ืขื™ืงืจื™ื•ืช

  • Origins and Evolution
  • Subclades
  • Geographical Distribution
  • Historical and Cultural Significance
  • Conclusion
ืคืจื•ืคื™ืœ ื”ื™ื™ื—ื•ืก

ืขืฅ ื”ืฉื•ืฉืœืช ื•ื”ืขื ืคื™ื ื”ืงืฉื•ืจื™ื

ืžืงื•ื ื”ืขื ืฃ ื‘ืขืฅ ื”ืฉื•ืฉืœืช ื•ืชืช-ื”ืขื ืคื™ื ืฉืœื•

ืžืกืœื•ืœ ื”ื”ืชืคืฆืœื•ืช ืฉืœ ื”ืฉื•ืฉืœืช

ืขืงื‘ื• ืื—ืจ ืขื ืคื™ ื”ืื‘ ื”ืžืชื•ืขื“ื™ื ืขื“ O2A1B1A1A1A1E1A1. ื”ืชืืจื™ื›ื™ื ื”ื ืื•ืžื“ื ื™ื ื•ืขืฉื•ื™ื™ื ืœื”ืฉืชื ื•ืช ื›ืฉื ืชื•ื ื™ ื”ื™ื™ื—ื•ืก ืžืชืขื“ื›ื ื™ื.

ืฉืœื‘ื™ ื”ืชืคืฆืœื•ืช ื”ืงื‘ื•ืฆื” ื”ื”ืคืœื•ื’ืจื•ืคื™ืช ื’ื™ืœ ืžืฉื•ืขืจ ื”ืชืงื•ืคื” ื”ืืจื›ืื•ืœื•ื’ื™ืช ื”ื–ืžืŸ ืฉื—ืœืฃ ืขื ืคื™ื ื™ืฉื™ืจื™ื ื“ื’ื™ืžื•ืช ืžื•ื“ืจื ื™ื•ืช ืฉื ื‘ื“ืงื• ืงื™ืฉื•ืจื™ื ืขืชื™ืงื™ื
1 O2A1B1A1A1A1E1A1 ื”ืขื ืฃ ื”ื ื•ื›ื—ื™ ~1,000 years ago Medieval 1,000 שנים 1 0 0
2 O2A1B1A1A1A1E1A ~1,000 years ago Medieval 1,000 שנים 1 0 0
3 O2A1B1A1A1A1E1 ~2,000 years ago Medieval 1,500 שנים 1 0 0
4 O2A1B1A1A1A1E ~2,000 years ago Classical Antiquity 2,500 שנים 1 6 0
5 O2A1B1A1A1A1 ~4,000 years ago Bronze Age 3,500 שנים 2 25 0
6 O2A1B1A1A1A ~4,000 years ago Bronze Age 3,500 שנים 1 25 0
7 O2A1B1A1A1 ~4,000 years ago Bronze Age 4,000 שנים 1 25 0
8 O2A1B1A1A ~5,000 years ago Bronze Age 5,000 שנים 1 25 0
9 O2A1B1A1 ~6,000 years ago Chalcolithic 6,000 שנים 1 25 0
10 O2A1B1A ~8,000 years ago Neolithic 8,000 שנים 1 25 0
11 O2A1B1 ~10,000 years ago Neolithic 10,000 שנים 1 27 0
12 O2A1B ~12,000 years ago Neolithic 12,000 שנים 1 27 0
13 O2A1 ~15,000 years ago Mesolithic 15,000 שנים 2 34 0
14 O2A ~20,000 years ago Mesolithic 20,000 שנים 2 381 12
15 O2 ~35,000 years ago Paleolithic 35,000 שנים 2 388 12
16 O ~45,000 years ago Paleolithic 45,000 שנים 2 553 6
17 NO ~45,000 years ago Paleolithic 45,000 שנים 4 801 12

ืชืช-ืขื ืคื™ื (1)

ืคืจื•ืคื™ืœ ื”ื™ื™ื—ื•ืก

ื”ื™ื›ืŸ ื”ืขื ืฃ ืžื•ืคื™ืข

ืชืคื•ืฆื” ื’ืื•ื’ืจืคื™ืช ื•ื ื•ื›ื—ื•ืช ื ื•ื›ื—ื™ืช

ืžื•ืฆื ืžืชื•ืขื“

East Asia

ืชืคื•ืฆื” ื ื•ื›ื—ื™ืช

The populations where Y-DNA haplogroup O2A1B1A1A1A1E1A1 is found include:

  1. Han Chinese and related East Asian populations
  2. Southern Chinese populations
  3. Mainland Southeast Asian populations such as Vietnamese and Thai groups
  4. Austronesian-speaking populations, including Taiwanese groups and Island Southeast Asians
  5. Korean and Japanese populations
  6. Tibeto-Burman-speaking populations in China and the Himalayas

ื ื•ื›ื—ื•ืช ืœืคื™ ืื–ื•ืจ

Southeast Asia High
East Asia (southern China, Guangxi/Yunnan) Moderate
Island Southeast Asia and Taiwan Low
Southeast Asia Moderate
Central Asia Low
ื”ืงืฉืจ ื”ื™ืกื˜ื•ืจื™

ืขื ืฃ ืœืื•ืจืš ื–ืžืŸ

ืื•ืžื“ืŸ ื”ื™ื•ื•ืฆืจื•ืช ื‘ืฆื™ืจ ื–ืžืŸ ื”ื™ืกื˜ื•ืจื™ ืจื—ื‘. ืกืžื ื™ ื”ืชืงื•ืคื•ืช ื ื•ืชื ื™ื ื”ืงืฉืจ ื•ืื™ื ื ืžืจืžื–ื™ื ืขืœ ืงืฉืจ ืœืชืจื‘ื•ื™ื•ืช ืžืกื•ื™ืžื•ืช.

  1. ~10k שנים לפני

    המהפכה הנאוליתית

    ראשית החקלאות והתגבשות קהילות יושבות קבע

  2. ~5k שנים לפני

    תקופת הברונזה

    עיבוד מתכות, כתב וציוויליזציות מוקדמות

  3. ~3k שנים לפני

    תקופת הברזל

    כלי ברזל ורשתות מסחר מורחבות

  4. ~2.5k שנים לפני

    העת העתיקה הקלאסית

    שגשוג הציוויליזציות היוונית והרומית

  5. ~1k שנים לפני

    קבוצה הפלוגרופית O2A1B1A1A1A1E1A1

    אומדן להיווצרות ענף Y-DNA זה. תאריכים ומיקומים הם אומדני ייחוס.

    ื”ืขื ืฃ ื”ื–ื”
  6. Present

    ימינו

    העידן המודרני

ืคืจื•ืคื™ืœ ื”ื™ื™ื—ื•ืก

ื”ืงืฉืจ ืืจื›ืื•ืœื•ื’ื™

ื”ืงืฉืจื™ื ืืจื›ืื•ืœื•ื’ื™ื™ื ืžืชื•ืขื“ื™ื ืฉืœ ืขื ืฃ O2A1B1A1A1A1E1A1 ืž-Y-DNA

ื”ืงืฉืจื™ื ืžืชื•ืขื“ื™ื

ืชื•ื•ื™ื•ืช ืืœื” ืžืชืืจื•ืช ื”ืงืฉืจื™ื ืืจื›ืื•ืœื•ื’ื™ื™ื ืžืชื•ืขื“ื™ื ืฉืœ ื“ื’ื™ืžื•ืช ื”ื™ื™ื—ื•ืก ื”ืžืงื•ืฉืจื•ืช ืœ-O2A1B1A1A1A1E1A1. ื”ืงื™ืฉื•ืจ ืื™ื ื• ืžื•ื›ื™ื— ืฉื›ืœ ื ื•ืฉืื™ ื”ืขื ืฃ ื”ืฉืชื™ื™ื›ื• ืœืชืจื‘ื•ืช ืžืกื•ื™ืžืช ืื• ื”ืœื›ื• ื‘ืžืกืœื•ืœ ื ื“ื™ื“ื” ืžืกื•ื™ื.

China_LBA_EIA Chinese Henan_Wangchenggang Longsangquduo Culture Sukhbaatar Culture Vietnamese Neolithic Xiongnu
ืกื™ื•ื•ื’ ื”ืชืจื‘ื•ื™ื•ืช ืžื‘ื•ืกืก ืขืœ ื”ื”ืงืฉืจ ื”ืืจื›ืื•ืœื•ื’ื™ ืฉืœ ื“ื’ื™ืžื•ืช ื“ื "ื ืขืชื™ืง, ื•ื”ื•ื ืขืฉื•ื™ ืœืฉืงืฃ ืงืฉืจื™ื ืื–ื•ืจื™ื™ื ื‘ืชืงื•ืคื•ืช ืžืกื•ื™ืžื•ืช.
ענף אבהי ยท DNA ืงื“ื•ื

ืžืคืช ืจืื™ื•ืช ืงื“ื•ืžื•ืช ืœืขื ืฃ ื”ืฉื•ืฉืœืช

ืขืงื‘ื• ืื—ืจ ืขื ืคื™ ื”ืžืงื•ืจ ื”ืžื•ื‘ื™ืœื™ื ืœืขื ืฃ ื–ื”, ื•ื’ืœื• ื”ื™ื›ืŸ ื ืžืฆืื• ื”ื“ื’ื™ืžื•ืช ื”ืงื“ื•ืžื•ืช ื”ืงืฉื•ืจื•ืช ืืœื™ื•.

ื˜ื•ืขืŸ ืชืฆืคื™ื•ืช ืงื“ื•ืžื•ืช...

ื”ืกื™ืžื•ื ื™ื ืžืฆื™ื™ื ื™ื ืžืงื•ืžื•ืช ืžืฆื™ืื” ืืจื›ืื•ืœื•ื’ื™ื™ื. ืงื• ืžืงื•ื•ืงื• ื”ื•ื ืžืขื‘ืจ ื’ืื•ื’ืจืคื™ ืžื•ืฆืข ื•ืœื ื•ื“ืื™ ื‘ื™ืŸ ืขื ืคื™ื ืขื•ืงื‘ื™ื, ื”ื ืชืžืš ื‘ื›ืžื” ืชืฆืคื™ื•ืช ืžืชื•ืืจื›ื•ืช. ืื™ืŸ ื–ื” ืžืกืœื•ืœ ืžื“ื•ื™ืง, ืžืงื•ื ืœื™ื“ื” ืื• ื”ื•ื›ื—ื” ืœื™ืจื™ื“ื” ื™ืฉื™ืจื”. ื“ื’ื™ืžื•ืช ืžืขื ืคื™ ื”ืžืงื•ืจ ืขืฉื•ื™ื•ืช ืœื”ืฉืชื™ื™ืš ืœืขื ืคื™ ืฆืืฆืื™ื ืื—ืจื™ื. ื”ืคืขืจื™ื ื ืฉืืจื™ื ื‘ืžืงื•ื ืฉื‘ื• ื”ืจืื™ื•ืช ืื™ื ืŸ ืžืกืคื™ืงื•ืช. ืชืืจื™ื›ื™ ื”ื“ื’ื™ืžื•ืช ืฉื•ื ื™ื ืžืชืืจื™ื›ื™ ื”ื™ื•ื•ืฆืจื•ืช ื”ื”ืคืœื•ื’ืจื•ืค.

ื”ื ืชื•ื ื™ื

ื”ื ืชื•ื ื™ื ื•ืžืงื•ืจื•ืชื™ื”ื

ืžื™ื“ืข ืขืœ ื”ืžืงื•ืจื•ืช ื•ืื™ื›ื•ืช ื”ื ืชื•ื ื™ื

ืขื“ื›ื•ืŸ ืื—ืจื•ืŸ 2026-06-17
ืจืžืช ื‘ื™ื˜ื—ื•ืŸ 50/100
ื›ื™ืกื•ื™ Low

ืžืงื•ืจ ื”ื ืชื•ื ื™ื

ื”ืกื™ื•ื•ื’, ื”ืชืืจื™ื›ื™ื ื”ืžืฉื•ืขืจื™ื ื•ื”ื”ืงืฉืจ ื”ื’ืื•ื’ืจืคื™ ืžืฉืงืคื™ื ืืช ื ืชื•ื ื™ ื”ื™ื™ื—ื•ืก ื”ืžืชื•ืขื“ื™ื, ื•ื”ื ืขืฉื•ื™ื™ื ืœื”ืฉืชื ื•ืช ื›ืฉื”ืจืื™ื•ืช ื ื‘ื“ืงื•ืช ืžื—ื“ืฉ. ื›ื™ืกื•ื™ ื”ื“ื’ื™ืžื•ืช ืžืฉืชื ื”, ื•ืžื™ืงื•ืžื™ื ืžืชื•ืขื“ื™ื ื•ืงืฉืจื™ื ืืจื›ืื•ืœื•ื’ื™ื™ื ืื™ื ื ืžื•ื›ื™ื—ื™ื ืžื•ืฆื ืื™ืฉื™ ืื• ื–ื”ื•ืช ืชืจื‘ื•ืชื™ืช.