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Haplogroup G2a1a

G-FGC661

Macro-haplogroup
G
Parent clade
G2a1
Formed (estimate)
c. 10,000–12,500 years before present
TMRCA (estimate)
c. 6,000–8,000 years ago

Overview

G2a1a represents an early split within the G2a1 branch, forming a lineage associated with late Neolithic and early Chalcolithic populations of the Iranian plateau and adjacent highlands. Archaeogenetic models suggest that G2a1a traces back to populations involved in the cultural and ecological transitions of the Zagros piedmont, where the shift from mobile foraging to mixed agro-pastoral lifeways first developed. Unlike the much later G2a2b1a-derived expansions that swept through Europe, G2a1a reflects a more regionally stable, conservative paternal line whose demographic history aligns closely with the plateau’s deep-rooted highland societies.

Geographic distribution

Modern carriers of G2a1a are most common in Iran—particularly in the central and western highland regions. Additional low-frequency occurrences are observed in eastern Turkey, the South Caucasus, parts of northern Mesopotamia, and marginally within Afghanistan and Turkmenistan. The lineage’s geographic concentration mirrors long-term cultural continuity zones extending from the central Zagros to the Armenian Highlands.

Ancient DNA

  • Possible G2a1a-related haplotypes appear in Late Neolithic and Chalcolithic Iranian genomes, particularly those linked with highland agro-pastoral communities.
  • Early Bronze Age individuals from northwest Iran show close affinity to G2a1a clades, indicating persistence into proto-urban cultural phases.
  • No fully confirmed ancient G2a1a sample exists due to partial Y-coverage in many Iranian plateau remains.

Phylogeny & subclades

G2a1a forms one of the earliest definable branches under G2a1, defined by FGC661 and associated SNP nodes. Internal structure is moderate, with a handful of identifiable clusters among Iranian and Armenian groups. The lineage stands parallel to G2a1b, together representing the primary diversification within G2a1. The phylogeny suggests an origin in highland West Asia, followed by slow, regionally contained expansions.

  • G2a1a* (basal)
  • G2a1a1 (FGC675-linked microbranch)
  • Numerous Iranian plateau–specific private clusters

Notes & context

G2a1a serves as an important marker of early highland West Asian paternal structure. Its stable geographic footprint makes it particularly valuable in modeling the demographic continuity of Iranian Neolithic and Chalcolithic societies, contrasted with the more expansive G2a2 lineages associated with European farming cultures.