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.
References & external links