ื“ื™ืœื•ื’ ืœืชื•ื›ืŸ ื”ืจืืฉื™
mtDNA ยท ืฉื•ืฉืœืช אימהית

S2A

mtDNA Haplogroup S2A

ื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 S2A ื‘ืฉื•ืฉืœืช mtDNA

Origins and Evolution

mtDNA haplogroup S2A is a downstream branch of haplogroup S2, itself derived from the broader Oceanian haplogroup S. The parent clade S2 has deep roots in the Sahul region dating to the Late Pleistocene (the broader S lineage is typically placed around the Upper Pleistocene), and S2A likely formed locally within New Guinea or nearby Sahul populations in the Late Pleistocene to early Holocene (roughly the last ~16 thousand years). Its emergence reflects in situ diversification of maternal lineages after the initial settlement of Sahul by anatomically modern humans and the subsequent isolation, drift, and population structure that characterize Near Oceania.

Genetic processes important to the origin of S2A include founder effects from small, isolated groups, long-term population structure among Papuan and Aboriginal groups, and later limited inter-island dispersals that moved maternal lineages between New Guinea, nearby islands, and the Australian continent. Because S2A is nested within S2, its phylogenetic position helps resolve finer-scale maternal history within Sahul and the early Holocene demographic dynamics of Near Oceania.

Subclades

S2A is itself an intermediate clade within S2. Depending on the resolution of mitogenome surveys, S2A may contain further sub-branches that are geographically structured (for example, sublineages more common in particular New Guinea highland or coastal groups, or in specific Melanesian islands). High-resolution whole-mitogenome studies tend to reveal localized subclades reflecting village- or island-level founder events; however, S2A overall remains a Papuan/Melanesian-centered lineage rather than one associated with the Austronesian/Lapita maternal expansion.

Geographical Distribution

S2A is primarily a Near Oceanian lineage with its highest representation in populations descended from the original Sahul settlers. Observed patterns include:

  • Presence across Papua New Guinea among both coastal and interior Papuan-speaking groups, often at moderate to locally high frequencies.
  • Occasional detection among Aboriginal Australian groups, consistent with shared deep Sahul ancestry and ancient gene flow or retention of ancestral variation.
  • Occurrence in Island Melanesia (e.g., Solomon Islands and neighboring islands), where localized founder events and coastal exchange networks have transmitted some Papuan maternal lineages.
  • Low to moderate frequencies in Torres Strait Islander groups, reflecting their geographic bridging position between New Guinea and Australia.
  • Very occasional findings in nearby parts of Island Southeast Asia (e.g., eastern Indonesia) that reflect either ancient coastal contact or later low-level dispersal.

The distribution reflects a pattern of deep regional continuity with limited long-distance spread; in many cases S2A is concentrated in areas with strong Papuan genetic continuity.

Historical and Cultural Significance

S2A documents the Pleistoceneโ€“Holocene continuity of maternal ancestry in Sahul and is therefore informative about the demographic history of Papuan and Aboriginal groups prior to and during the Holocene. Because S2A is not generally associated with the Austronesian/Lapita expansions that reshaped parts of Near Oceania around 3โ€“3.5 kya, its presence often marks populations or subpopulations that retained substantial pre-Austronesian maternal ancestry.

In archaeological terms, S2A is best interpreted as part of the genetic signal of Pre-Lapita Sahul foragers and later Holocene Papuan communities rather than a marker of later farming expansions. When S2A appears alongside Austronesian-linked mtDNA haplogroups (e.g., B4a1a-derived lineages) in coastal or island populations, it indicates admixture between indigenous maternal lineages and incoming Austronesian groups during the late Holocene.

Conclusion

mtDNA haplogroup S2A is a regionally important maternal lineage in Near Oceania that preserves information about the deep settlement and local diversification of populations within Sahul. As genomic sampling and mitogenome resolution improve across New Guinea, Australia and neighboring islands, S2A and its subclades will continue to refine reconstructions of population structure, migration corridors, and the timing of demographic events in this geographically complex region.

ื ื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“ S2A. ื”ื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 S2A ื”ืขื ืฃ ื”ื ื•ื›ื—ื™ ~16,000 years ago Mesolithic 16,000 שנים 1 0 0
2 S2 ~28,000 years ago Paleolithic 28,000 שנים 2 3 0
3 S ~50,000 years ago Paleolithic 50,000 שנים 2 279 0
4 N ~60,000 years ago Paleolithic 60,000 שנים 16 26,150 13
5 L3 ~70,000 years ago Paleolithic 70,000 שנים 7 30,162 6
6 L3'4 - - - 2 30,212 0
7 L3'4'6 - - - 2 30,216 0
8 L2'3'4'6 - - - 2 31,333 0
9 L2'3'4'5'6'7 - - - 2 31,349 0
10 L1'2'3'4'5'6'7 - - - 2 31,852 0
11 L ~160,000 years ago Paleolithic 160,000 שנים 2 32,236 5

ืชืช-ืขื ืคื™ื (1)

ืขื ืคื™ื ืื—ื™ื (1)

ืขื ืคื™ื ื ื•ืกืคื™ื ืžืื•ืชื” ืงื‘ื•ืฆื” ื”ืคืœื•ื’ืจื•ืคื™ืช ืื‘

ืคืจื•ืคื™ืœ ื”ื™ื™ื—ื•ืก

ื”ื™ื›ืŸ ื”ืขื ืฃ ืžื•ืคื™ืข

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

ืžื•ืฆื ืžืชื•ืขื“

New Guinea / Sahul (Island Southeast Asia–New Guinea)

ืชืคื•ืฆื” ื ื•ื›ื—ื™ืช

The populations where mtDNA haplogroup S2A is found include:

  1. Indigenous populations of Papua New Guinea
  2. Indigenous (Aboriginal) populations of Australia
  3. Populations of Island Melanesia (e.g., Solomon Islands and nearby islands)
  4. Torres Strait Islander groups (at low to moderate frequencies)
  5. Very occasional occurrences in nearby Island Southeast Asia reflecting historical contact or limited dispersal
ื”ื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. ~20k שנים לפני

    שיא עידן הקרח האחרון

    שיא עידן הקרח האחרון, ואוכלוסיות שנותרו מבודדות

  2. ~16k שנים לפני

    קבוצה הפלוגרופית S2A

    אומדן להיווצרות ענף mtDNA זה. תאריכים ומיקומים הם אומדני ייחוס.

    ื”ืขื ืฃ ื”ื–ื”
  3. ~10k שנים לפני

    המהפכה הנאוליתית

    ראשית החקלאות והתגבשות קהילות יושבות קבע

  4. ~5k שנים לפני

    תקופת הברונזה

    עיבוד מתכות, כתב וציוויליזציות מוקדמות

  5. ~3k שנים לפני

    תקופת הברזל

    כלי ברזל ורשתות מסחר מורחבות

  6. ~2.5k שנים לפני

    העת העתיקה הקלאסית

    שגשוג הציוויליזציות היוונית והרומית

  7. Present

    ימינו

    העידן המודרני

ืคืจื•ืคื™ืœ ื”ื™ื™ื—ื•ืก

ื”ืงืฉืจ ืืจื›ืื•ืœื•ื’ื™

ื”ืงืฉืจื™ื ืืจื›ืื•ืœื•ื’ื™ื™ื ืžืชื•ืขื“ื™ื ืฉืœ ืขื ืฃ S2A ืž-mtDNA

ื”ืงืฉืจื™ื ืžืชื•ืขื“ื™ื

ืชื•ื•ื™ื•ืช ืืœื” ืžืชืืจื•ืช ื”ืงืฉืจื™ื ืืจื›ืื•ืœื•ื’ื™ื™ื ืžืชื•ืขื“ื™ื ืฉืœ ื“ื’ื™ืžื•ืช ื”ื™ื™ื—ื•ืก ื”ืžืงื•ืฉืจื•ืช ืœ-S2A. ื”ืงื™ืฉื•ืจ ืื™ื ื• ืžื•ื›ื™ื— ืฉื›ืœ ื ื•ืฉืื™ ื”ืขื ืฃ ื”ืฉืชื™ื™ื›ื• ืœืชืจื‘ื•ืช ืžืกื•ื™ืžืช ืื• ื”ืœื›ื• ื‘ืžืกืœื•ืœ ื ื“ื™ื“ื” ืžืกื•ื™ื.

Australia_PreEuropean NSW Aboriginal
ืกื™ื•ื•ื’ ื”ืชืจื‘ื•ื™ื•ืช ืžื‘ื•ืกืก ืขืœ ื”ื”ืงืฉืจ ื”ืืจื›ืื•ืœื•ื’ื™ ืฉืœ ื“ื’ื™ืžื•ืช ื“ื "ื ืขืชื™ืง, ื•ื”ื•ื ืขืฉื•ื™ ืœืฉืงืฃ ืงืฉืจื™ื ืื–ื•ืจื™ื™ื ื‘ืชืงื•ืคื•ืช ืžืกื•ื™ืžื•ืช.
ืคืจื•ืคื™ืœ ื”ื™ื™ื—ื•ืก

ืื™ื ื“ืงืก ื“ื’ื™ืžื•ืช

ืžืกืคืจ ื“ื’ื™ืžื•ืช ืชืช-ื”ืขื ืคื™ื ืฉืœ ื”ืงื‘ื•ืฆื” ื”ื”ืคืœื•ื’ืจื•ืคื™ืช S2A ื”ื•ื 3. ืื™ืŸ ื“ื’ื™ืžื•ืช ื‘ื”ืชืืžื” ื™ืฉื™ืจื” ื‘ืงื‘ื•ืฆืช ื”ื™ื™ื—ื•ืก ื”ื ื•ื›ื—ื™ืช.

3 ืžื•ืฆื’ื•ืช ยท 3 ื“ื’ื™ืžื•ืช ืชื•ืืžื•ืช

ื”ื“ื™ื•ืงื ืื•ืช ื”ื ืื™ื•ืจื™ื ืฉื ื•ืฆืจื• ื‘ื‘ื™ื ื” ืžืœืื›ื•ืชื™ืช. ืฉืžื•ืช ื”ื“ื’ื™ืžื•ืช ื•ืžื–ื”ื™ ื”ื”ืคืงื“ื” ืžื–ื”ื™ื ืืช ืจืฉื•ืžื•ืช ื”ื™ื™ื—ื•ืก.

ื“ื™ื•ืงืŸ ื”ื“ื’ื™ืžื” ื”ืžื“ื™ื ื” ื”ืชืงื•ืคื” ื”ืชืืจื™ืš ื”ืชืจื‘ื•ืช mtDNA ืกื•ื’ ื”ื”ืชืืžื”
ืฉื—ื–ื•ืจ ืืžื ื•ืชื™ ืฉื ื•ืฆืจ ื‘ื‘ื™ื ื” ืžืœืื›ื•ืชื™ืช ืฉืœ ื”ื“ื’ื™ืžื” Pre European individual, Willandra Lakes Region (New South Wales), Australia (292-1,908 CE)
ืžื–ื”ื” ื“ื’ื™ืžื”: WLH4
Australia Australia PreEuropean 400-1800 CE Australia_PreEuropean S2a1a תת-ענף
ืฉื—ื–ื•ืจ ืืžื ื•ืชื™ ืฉื ื•ืฆืจ ื‘ื‘ื™ื ื” ืžืœืื›ื•ืชื™ืช ืฉืœ ื”ื“ื’ื™ืžื” Pre European individual, Barham Forest/Koondrook-Perricoota (New South Wales), Australia (400-500 CE)
ืžื–ื”ื” ื“ื’ื™ืžื”: KP2
Australia Aboriginal Australians of New South Wales 400-500 CE NSW Aboriginal S2a1a תת-ענף
ืฉื—ื–ื•ืจ ืืžื ื•ืชื™ ืฉื ื•ืฆืจ ื‘ื‘ื™ื ื” ืžืœืื›ื•ืชื™ืช ืฉืœ ื”ื“ื’ื™ืžื” Aboriginal Australian individual, Willandra Lakes Region (New South Wales), Australia (410-1,788 CE)
ืžื–ื”ื” ื“ื’ื™ืžื”: WLH4_L3
Australia Aboriginal Australians of New South Wales 410 CE - 1788 CE NSW Aboriginal S2a1a תת-ענף
ענף אימהי 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.

ืคืจื•ืคื™ืœ ื”ื™ื™ื—ื•ืก

ืžืคืช ืชืคื•ืฆืช ื”ื“ื’ื™ืžื•ืช

ื”ืชืคื•ืฆื” ื”ื’ืื•ื’ืจืคื™ืช ืฉืœ ื“ื’ื™ืžื•ืช ื“ื "ื ืขืชื™ืง ื‘ื”ืชืืžื” ื™ืฉื™ืจื” ืœืงื‘ื•ืฆื” S2A ืื• ืœืชืช-ื”ืขื ืคื™ื ืฉืœื”. ืžืกืคืจ ื“ื’ื™ืžื•ืช: 3

ื“ื’ื™ืžื” ืžืชืช-ืขื ืฃ
ืกื™ื ื•ืŸ ืœืคื™ ืชืงื•ืคื”
ื›ืœ ื”ืชืงื•ืคื•ืช
ื›ืœ ื”ื“ื’ื™ืžื•ืช ืžื•ืฆื’ื•ืช
ืคืจื•ืคื™ืœ ื”ื™ื™ื—ื•ืก

ืชืคื•ืฆื” ื‘ื–ืžืŸ

ืชืคื•ืฆืช ื”ื“ื’ื™ืžื•ืช ืขืœ ืคื ื™ ื”ืชืงื•ืคื•ืช ื”ืืจื›ืื•ืœื•ื’ื™ื•ืช

ืคืจื•ืคื™ืœ ื”ื™ื™ื—ื•ืก

ืชืคื•ืฆื” ื’ืื•ื’ืจืคื™ืช

ืžืกืคืจ ื”ื“ื’ื™ืžื•ืช ืœืคื™ ื”ืžื“ื™ื ื” ื”ืžืชื•ืขื“ืช ืฉืœื”ืŸ. ื”ืกืคื™ืจื•ืช ืžืฉืงืคื•ืช ืืช ื“ื’ื™ืžื•ืช ื”ื™ื™ื—ื•ืก ื”ื–ืžื™ื ื•ืช, ื‘ืœื™ ืœืžื“ื•ื“ ืืช ืชื“ื™ืจื•ืช ื”ืงื‘ื•ืฆื•ืช ื”ื”ืคืœื•ื’ืจื•ืคื™ื•ืช ื‘ืื•ื›ืœื•ืกื™ื™ื”.

ืคืจื•ืคื™ืœ ื”ื™ื™ื—ื•ืก

ืชืคื•ืฆืช ื”ื“ื’ื™ืžื•ืช ืœืคื™ ืžื“ื™ื ื” ื•ืชืงื•ืคื”

ื”ืฉื•ื• ืืช ืžืกืคืจ ื”ื“ื’ื™ืžื•ืช ื”ืžืชื•ืขื“ื•ืช ืœืคื™ ืžื“ื™ื ื•ืช ื•ืชืงื•ืคื•ืช ืืจื›ืื•ืœื•ื’ื™ื•ืช. ื‘ื—ืจื• ืชื ืขื ืชื•ืฆืื•ืช ื›ื“ื™ ืœืจืื•ืช ืื—ืช ืžื”ื“ื’ื™ืžื•ืช.

ื”ื ืชื•ื ื™ื

ื”ื ืชื•ื ื™ื ื•ืžืงื•ืจื•ืชื™ื”ื

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

ืขื“ื›ื•ืŸ ืื—ืจื•ืŸ 2026-02-16
ื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.