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Haplogroup G1a

G-L1323

Macro-haplogroup
G
Parent clade
G1
Formed (estimate)
c. 13,000–16,000 years before present
TMRCA (estimate)
c. 7,000–9,000 years ago

Overview

G1a (L1323) is the principal radiating branch of G1 and contains the majority of its global diversity. Formed near the dawn of the Holocene, G1a underwent a series of expansions from its Iranian–Caspian homeland, spreading both westward into the Caucasus and eastward along emerging Central Asian cultural networks. The lineage’s demographic history aligns closely with the rise of pastoralist economies in the Iranian Plateau and surrounding steppe–foothill ecotones. Later Bronze and Iron Age migrations—including those associated with Iranian-speaking groups and early nomadic confederations—played a major role in distributing G1a across parts of Central Asia and the Caspian basin.

Geographic distribution

The highest concentrations are found in Iran, especially in the western, northwestern and southern Caspian regions. Strong frequencies occur among Kazakh tribes—particularly in clans historically linked to early nomadic Iranian or Turkic confederations. Moderate presence appears in Turkmenistan, Uzbekistan and Tajikistan. In the Caucasus, G1a appears most frequently in Azerbaijan and Armenia. Minor but consistent frequencies occur in Gulf populations and Pakistan’s northwest highlands.

Ancient DNA

  • Bronze Age Iran and the Zagros region show G1a-compatible SNPs in pastoralist-associated individuals.
  • Iron Age Central Asian burials (Saka/Scythian-related) include individuals with upstream G1a SNP signatures.
  • No verified Neolithic presence outside West Asia, reflecting its non-participation in Anatolian-to-European farmer expansions.

Phylogeny & subclades

G1a contains numerous internal clusters, including major splits forming Iranian-centered and Central Asian-centered lineages. One major subcluster (including G1a1) is tightly tied to Iranian Plateau populations, while others show strong associations with medieval and early historic nomadic expansions into Central Asia. Its phylogeny is more star-like than G1 overall, indicating a broad early Holocene radiation followed by repeated founder events.

  • G1a* basal
  • G1a1 (major Iranian-centered sub-branch)
  • Central Asian founder-effect microclades
  • Pakistan/Afghanistan localized clusters

Notes & context

G1a is indispensable for understanding the demographic history of western Iran and Central Asia. Its distribution aligns closely with ethno-linguistic patterns, making it a valuable lineage for interpreting historical nomadic and highland cultural dynamics.