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Haplogroup J2a-Y18973

Macro-haplogroup
J
Parent clade
J2a-M67
Formed (estimate)
c. 7,800 to 10,000 years before present
TMRCA (estimate)
c. 2,000 to 3,200 years ago

Overview

J2a-Y18973 represents a downstream element of the J2a-M67 highland-centered radiation and is strongly linked to the demographic history of eastern Anatolia, the Armenian plateau and northern Mesopotamia. Its early formation aligns with the consolidation of upland agricultural societies in the early Holocene, marked by the appearance of fortified upland settlements, terraced agriculture and enduring obsidian trade networks between the Lake Van region, the Upper Euphrates basin and the northern Zagros foothills. Through the Bronze Age, Y18973-bearing communities were embedded in the highland settlement systems that formed the backbone of regional metallurgy, pastoral mobility and mountain corridor trade. Its downstream phylogenetic structure points to a series of microregional founder events in enclosed valleys and plateau basins. Iron Age and classical populations across the Armenian highlands, eastern Anatolia and northern Mesopotamia preserve paternal haplogroups that align well with the expected demographic footprint of Y18973.

Geographic distribution

Armenia, eastern Turkey, northwest Iran, northern Iraq; occasional presence in Georgia and eastern Syria.

Ancient DNA

  • Early Bronze Age Armenian individuals carry upstream J2a-M67 diversity consistent with this lineage.
  • Chalcolithic Upper Tigris individuals show markers aligned with basal Y18973.
  • Bronze Age eastern Anatolian sites contain ancestral branches connected to this clade.
  • Iron Age settlements across northern Mesopotamia preserve downstream J2a signatures matching Y18973.
  • Classical highland sites maintain microbranches reflecting long-term upland continuity.

Phylogeny & subclades

A highland-rooted J2a-M67 subclade with diversification across mountain basins and plateau margins.

  • Y18973*
  • Armenian plateau microbranches
  • Upper Euphrates derivatives

Notes & context

Y18973 is fundamental for tracing Holocene and Bronze Age upland demographic continuity in eastern Anatolia and the Armenian plateau.