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Haplogroup G2a6a

G-Y128028

Macro-haplogroup
G
Parent clade
G2a6
Formed (estimate)
c. 8,500–10,500 years before present
TMRCA (estimate)
c. 4,500–6,000 years ago

Overview

G2a6a is a downstream lineage of G2a6 that appears to have developed within the highland–foothill zones of the southern Caucasus and northwest Iran. It reflects a paternal lineage tied to the mobile herding and mixed farming communities of the late Chalcolithic and early Bronze Age. While less common today than many G2a2-derived branches, G2a6a maintains a notable presence in regions with deep prehistoric settlement continuity.

Geographic distribution

The lineage is most frequently observed in Armenia, northwest Iran, eastern Turkey, and parts of Azerbaijan. Low-frequency occurrences in northeastern Iraq and the Caspian fringe likely reflect Bronze Age and later trans-regional interactions. The geographic clustering strongly associates the lineage with highland ecological niches.

Ancient DNA

  • Chalcolithic Armenian individuals exhibit Y-chromosome structures resembling G2a6-related basal nodes.
  • Early Bronze Age Kura-Araxes males show partial haplotypic overlap with G2a6-derived lineages.
  • No full-resolution ancient assignment exists yet for G2a6a.

Phylogeny & subclades

G2a6a forms the primary definable branch of G2a6, marked by Y128028. Internal phylogeny is modest, featuring regional Caucasus-centered microlineages. It stands parallel to the deeper radiations of G2a2, forming part of the highland West Asian cluster of G2a diversity.

  • G2a6a* (basal)
  • G2a6a1 (Y128041-associated)
  • Regional Armenian/Caucasus microbranches

Notes & context

G2a6a’s importance lies in its reflection of early pastoral and agro-pastoral dynamics across the southern Caucasus and northwest Iran. Its stable geographic pattern complements archaeological evidence of long-lived highland cultural networks stretching from the Zagros to the Kura basin.