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Haplogroup J2a-Z7539

Macro-haplogroup
J
Parent clade
J2a-M67
Formed (estimate)
c. 9,000 to 12,000 years before present
TMRCA (estimate)
c. 3,200 to 4,700 years ago

Overview

J2a-Z7539 is a downstream lineage within J2a-M67 with a demographic center that spans the Upper Tigris basin, the Armenian highlands and parts of eastern Anatolia. Its early formation corresponds to the middle Holocene stage when upland communities were expanding agricultural systems and participating in regional obsidian exchange networks. Archaeological parallels suggest a connection with early Chalcolithic fortified settlements and highland agro pastoral groups. During the Bronze Age, Z7539 bearing populations appear in demographic spheres tied to the Kura Araxes cultural continuum and the broader archaeological landscape of northern Mesopotamia. Its internal diversification tracks the emergence of fortified towns, metallurgical activity in highland zones and repeated interaction between the uplands and the northern Fertile Crescent.

Geographic distribution

Modern Z7539 frequencies reach their highest levels in southeastern Turkey, northern Iraq, Armenia and northwest Iran. Medium frequencies appear in Georgia, Syria and the northern Levant. Lower levels in central Anatolia and western Iran reflect secondary movements tied to Bronze Age and Iron Age interactions.

Ancient DNA

  • Upper Tigris Chalcolithic individuals contain J2a structures aligned with upstream Z7539.
  • Bronze Age highland individuals from Armenia exhibit J2a patterns consistent with early Z7539 diversification.
  • Eastern Anatolian Bronze Age remains show paternal lineages falling into the Z7539 related space.
  • Iron Age northern Mesopotamian samples include J2a profiles consistent with downstream Z7539.
  • Classical and medieval highland burials preserve continuity with this lineage.

Phylogeny & subclades

Z7539 comprises multiple upland oriented subbranches reflecting regional diversification across the Armenian highlands and Upper Tigris basin. The phylogeny suggests an early origin followed by substantial Bronze Age expansion.

  • Z7539* basal upland form
  • Armenian downstream clusters
  • Upper Tigris microbranches
  • North Mesopotamian derived lines

Notes & context

J2a-Z7539 is important for tracing long term population continuity in the upland zones bordering northern Mesopotamia.

References & external links