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Haplogroup J2a-Y15831

Macro-haplogroup
J
Parent clade
J2a-M67
Formed (estimate)
c. 8,000 to 11,000 years before present
TMRCA (estimate)
c. 2,700 to 4,000 years ago

Overview

J2a-Y15831 represents a key highland-centered lineage within the J2a-M67 radiation. Its formation took place during the consolidation of early Holocene agricultural communities across the Armenian plateau, the Upper Tigris region and surrounding uplands of eastern Anatolia. Environmental stability in these upland basins enabled continuity of small-scale agro-pastoral groups who became important contributors to the later demographic landscapes of the Bronze Age. The structure of Y15831 suggests that it diversified within isolated highland micro-regions rather than participating in large coastal expansions. By the Bronze Age, the lineage was deeply embedded in cultural zones linked to Kura–Araxes derived communities and early fortified settlements. Iron Age demographic layers show continued presence across mountain valleys and upland plains, reflecting long-term population stability and localized continuity.

Geographic distribution

Armenia, eastern Turkey, northwest Iran, northern Iraq; moderate in Georgia; low in northern Syria.

Ancient DNA

  • Bronze Age Armenian plateau individuals show upstream patterns aligning with Y15831.
  • Chalcolithic Upper Tigris sites contain J2a diversity consistent with early phases of this lineage.
  • Eastern Anatolian Bronze Age burials exhibit paternal markers tied to this clade.
  • Iron Age upland populations preserve downstream components.
  • Classical populations of mountain basins show continuity with Y15831 derivatives.

Phylogeny & subclades

A highland-based J2a-M67 lineage with substructure concentrated in eastern Anatolian and Armenian uplands.

  • Y15831*
  • Armenian plateau microclades
  • Upper Tigris offshoots

Notes & context

Y15831 is critical for reconstructing long-term highland continuity in eastern Anatolia and the Armenian plateau.