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

O2A1B1A1A

Y-DNA Haplogroup O2A1B1A1A

ื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 O2A1B1A1A ื‘ืฉื•ืฉืœืช Y-DNA

Origins and Evolution

Y-DNA haplogroup O2A1B1A1A is a subclade of O2A1B1A1, which itself belongs to the broader haplogroup O2, one of the major paternal lineages of East Asia. Given its phylogenetic position, O2A1B1A1A likely arose during the late Neolithic or early Bronze Age, after the initial diversification of O2-related lineages within East Asian populations.

The broader O2 radiation is strongly associated with demographic growth, farming expansions, and population structure changes across East Asia during the Holocene. As a downstream branch, O2A1B1A1A probably reflects one of the many localized lineages that emerged as East Asian populations expanded, differentiated, and admixed across China and neighboring regions.

Subclades

As an intermediate or terminal subclade within a larger O2 lineage, O2A1B1A1A is expected to have limited deeper branching compared with older ancestral clades. Public phylogenies may not yet show extensive downstream resolution, but its placement indicates descent from a lineage with strong continuity in East Asian paternal history.

This haplogroup should be viewed in the context of its parent clade O2A1B1A1, with the following broader relationships:

  • O2: major East Asian paternal macrolineage
  • O2A1B1 and O2A1B1A: more localized descendant branches within East Asia
  • O2A1B1A1A: a further derived lineage likely shaped by regional founder effects and historical population movement

Geographical Distribution

The distribution of O2A1B1A1A is expected to be concentrated in East Asia, especially in populations with ancestry connected to the large O2-bearing demographic expansions of the past several millennia. It is most plausibly found at low to moderate frequencies in Han Chinese, especially in southern and central China, and may also appear in adjacent populations of Korea, Japan, Taiwan, mainland Southeast Asia, and the Himalayan fringe.

Because this is a relatively downstream lineage, its exact frequency will vary substantially by locality and sample set. Like many O2 subclades, its presence may reflect both ancient regional continuity and later historical dispersals.

Historical and Cultural Significance

Haplogroup O2A1B1A1A is best understood as part of the paternal genetic landscape associated with the rise and spread of East Asian agricultural and state-level societies. While no single archaeological culture can be assigned to this specific subclade with confidence, its broader phylogenetic neighborhood is often discussed in relation to Neolithic China, post-Neolithic demographic expansions, and the historical movement of peoples across East and Southeast Asia.

In a cultural-historical context, lineages within O2 are frequently associated with the spread of Sinitic-speaking, Austroasiatic, Austronesian, Korean, Japanese, and Tibeto-Burman populations, though these associations are broad and not exclusive. The haplogroup's significance lies less in a single migration event and more in its role as one branch of the highly successful paternal clades that expanded with agriculture, population density, and later social complexity in East Asia.

Conclusion

O2A1B1A1A is a derived East Asian Y-DNA lineage nested within the large and historically important O2 paternal clade. Its origin is most plausibly placed in East Asia about 5,000 years ago, with present-day occurrences expected primarily among populations of China and neighboring regions. As with many downstream O2 branches, it likely reflects a combination of regional founder effects, Holocene population growth, and historical migrations across East and Southeast Asia.

ื ื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“ O2A1B1A1A. ื”ื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 O2A1B1A1A ื”ืขื ืฃ ื”ื ื•ื›ื—ื™ ~5,000 years ago Bronze Age 5,000 שנים 1 25 0
2 O2A1B1A1 ~6,000 years ago Chalcolithic 6,000 שנים 1 25 0
3 O2A1B1A ~8,000 years ago Neolithic 8,000 שנים 1 25 0
4 O2A1B1 ~10,000 years ago Neolithic 10,000 שנים 1 27 0
5 O2A1B ~12,000 years ago Neolithic 12,000 שנים 1 27 0
6 O2A1 ~15,000 years ago Mesolithic 15,000 שנים 2 34 0
7 O2A ~20,000 years ago Mesolithic 20,000 שנים 2 381 12
8 O2 ~35,000 years ago Paleolithic 35,000 שנים 2 388 12
9 O ~45,000 years ago Paleolithic 45,000 שנים 2 553 6
10 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 O2A1B1A1A is found include:

  1. Han Chinese and other East Asian populations
  2. Southern Chinese and adjacent mainland Southeast Asian populations
  3. Southeast Asian populations, including Thai, Vietnamese, and Austroasiatic-speaking groups
  4. Austronesian-speaking populations, especially in Taiwan and Island Southeast Asia
  5. Korean and Japanese populations
  6. Tibeto-Burman-speaking populations in East Asia and the Himalayas

ื ื•ื›ื—ื•ืช ืœืคื™ ืื–ื•ืจ

Southeast Asia High
East Asia (Southern China) Moderate
South Asia Low
Island Southeast Asia / Near Oceania Low
Southeast Asia Moderate
Central Asia Low
South 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. ~5k שנים לפני

    קבוצה הפלוגרופית O2A1B1A1A

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

    ื”ืขื ืฃ ื”ื–ื”
  4. ~3k שנים לפני

    תקופת הברזל

    כלי ברזל ורשתות מסחר מורחבות

  5. ~2.5k שנים לפני

    העת העתיקה הקלאסית

    שגשוג הציוויליזציות היוונית והרומית

  6. Present

    ימינו

    העידן המודרני

ืคืจื•ืคื™ืœ ื”ื™ื™ื—ื•ืก

ื”ืงืฉืจ ืืจื›ืื•ืœื•ื’ื™

ื”ืงืฉืจื™ื ืืจื›ืื•ืœื•ื’ื™ื™ื ืžืชื•ืขื“ื™ื ืฉืœ ืขื ืฃ O2A1B1A1A ื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-O2A1B1A1A. ื”ืงื™ืฉื•ืจ ืื™ื ื• ืžื•ื›ื™ื— ืฉื›ืœ ื ื•ืฉืื™ ื”ืขื ืฃ ื”ืฉืชื™ื™ื›ื• ืœืชืจื‘ื•ืช ืžืกื•ื™ืžืช ืื• ื”ืœื›ื• ื‘ืžืกืœื•ืœ ื ื“ื™ื“ื” ืžืกื•ื™ื.

Chinese Henan_Wangchenggang Vietnamese Neolithic
ื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.