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Haplogroup J2a-Y17533

Macro-haplogroup
J
Parent clade
J2a-M67
Formed (estimate)
c. 8,000 to 10,200 years before present
TMRCA (estimate)
c. 2,300 to 3,500 years ago

Overview

J2a-Y17533 is a structured upland lineage within the J2a-M67 radiation and reflects the long-term demographic stability of eastern Anatolia and the Armenian highlands. Its earliest formation aligns with early Holocene upland village systems, which supported mixed farming and herding communities adapted to a montane ecological niche. Archaeological correlations include early permanent highland settlements, trans-mountain exchange routes and early copper-working traditions. During the Bronze Age, Y17533-bearing groups appear to have participated in the cultural spheres of the Upper Tigris basin and Armenian plateau, where fortified hilltop settlements and proto-urban centers emerged. Downstream diversification likely occurred within isolated valleys and plateau-edge landscapes. Iron Age and classical populations in the region continued to exhibit continuity with derived microbranches.

Geographic distribution

Armenia, eastern Turkey, northwest Iran, northern Iraq; minor presence in Georgia.

Ancient DNA

  • Chalcolithic Upper Tigris samples present upstream J2a-M67 markers consistent with ancestral Y17533.
  • Bronze Age Armenian plateau individuals show paternal elements aligned with this lineage.
  • Eastern Anatolian Bronze Age settlements contain related upstream nodes.
  • Iron Age highland individuals carry downstream variants.
  • Classical upland populations preserve continuity with subbranches.

Phylogeny & subclades

An upland-dominant J2a-M67 branch with structured diversification in the Armenian and eastern Anatolian highlands.

  • Y17533*
  • Armenian plateau microbranches
  • Upper Tigris clades

Notes & context

Important for reconstructing long-term highland demographic continuity and Bronze Age settlement dynamics.