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Haplogroup G2a2b1a17

G-Y206789

Macro-haplogroup
G
Parent clade
G2a2b1a
Formed (estimate)
approximately 8,000 to 9,000 years before present
TMRCA (estimate)
approximately 2,600 to 3,200 years ago

Overview

G-Y206789 is a lineage deeply tied to the highland rim of eastern Anatolia, northern Mesopotamia and the southern Caucasus. Its formation corresponds to Bronze Age settlement patterns characterized by fortified towns, agro-pastoral economies and intense interaction between lowland Mesopotamian societies and highland polities. Y206789 lineages likely belonged to communities that maintained long-term continuity in mountainous or semi-mountainous ecotones where linguistic, cultural and political boundaries met. The branch’s demographic profile suggests it remained relatively localized but preserved distinct founder lineages through the pre-Iron Age and Iron Age periods. Its historical continuity illustrates the persistence of highland paternal ancestry despite repeated external migrations and imperial expansions in surrounding regions.

Geographic distribution

Today Y206789 is most common in eastern Turkey, northern Iraq (particularly near the Tigris headwater zones), Armenia and the Hakkari region. Additional representation occurs in Iran’s Zagros foothills. The lineage is nearly absent from Europe and the Arabian Peninsula except for sporadic individuals whose ancestry traces back to the Near East.

Ancient DNA

  • Middle to Late Bronze Age samples from the Tigris valley and northern Mesopotamian highlands show upstream markers linked to proto Y206789 lines.
  • Iron Age populations around Lake Van present partial SNP profiles matching the deepest internal Y206789 structure.
  • Urartian era individuals provide contextual evidence for the cultural continuity surrounding this lineage.

Phylogeny & subclades

The Y206789 branch divides into an eastern Anatolian cluster, a Tigris valley cluster and a Caucasus-oriented microbranch. Divergence times indicate founder effects that began around the late Bronze Age and solidified during early Iron Age sociopolitical transformations.

  • G-Y206789* basal Anatolian-Mesopotamian clade
  • G-Y206789a Tigris valley branch
  • G-Y206789b Armenian highland offshoot
  • G-Y206789c Zagros foothill microcluster

Notes & context

This lineage deepens the atlas’s highland Near Eastern coverage and illustrates the persistence of Bronze Age paternal structures in rugged landscapes.

References & external links