A · BT · CT · CF · F · J · J2-M172 · J2a-M410 · J2a-M67 · J2a-Z7414

Haplogroup J2a-Z7414

Macro-haplogroup
J
Parent clade
J2a-M67
Formed (estimate)
c. 8,500 to 11,500 years before present
TMRCA (estimate)
c. 3,200 to 4,600 years ago

Overview

J2a-Z7414 is a downstream subclade of J2a-M67 with a demographic focus on the Upper Euphrates basin, the Armenian highlands and the adjoining regions of eastern Anatolia. Its origin corresponds to early Holocene agro pastoral expansions when permanent settlements began to crystallize in upland basins and river terraces. Archaeological parallels include early farming villages of eastern Anatolia, obsidian linked exchange networks and Chalcolithic fortified hilltop sites. Throughout the Bronze Age, Z7414 bearing groups appear within cultural networks connected to the Kura Araxes horizon, which spread across the South Caucasus, the Armenian plateau and northern Mesopotamia. The phylogenetic structure of the clade reflects upland centered expansion events influenced by metal production, herding routes and trans highland interaction systems.

Geographic distribution

Z7414 reaches its highest frequencies in Armenia, eastern Turkey and northwest Iran. Moderate frequencies occur in northern Iraq, Georgia and Syria. Lower levels in the Levant and central Anatolia represent later diffusion events tied to Bronze and Iron Age mobility.

Ancient DNA

  • Chalcolithic eastern Anatolian remains contain J2a lineages consistent with upstream Z7414 segments.
  • Bronze Age Armenian plateau individuals show paternal continuity with Z7414 related expansions.
  • Upper Euphrates Bronze Age burials include J2a patterns aligned with early Z7414 diversification.
  • Iron Age highland remains show J2a structures consistent with downstream Z7414 clusters.
  • Later classical highland populations preserve lineages linked to the Z7414 phylogeny.

Phylogeny & subclades

Z7414 forms several upland oriented microbranches under J2a-M67, displaying strong clustering in the Armenian highlands and eastern Anatolia. The phylogeny suggests localized founder effects combined with Bronze Age settlement intensification.

  • Z7414* basal upland variant
  • Armenian plateau derived branches
  • Upper Euphrates microclusters
  • Eastern Anatolian downstream lines

Notes & context

J2a-Z7414 is significant for understanding upland demographic continuity across the Armenian and eastern Anatolian highlands.

References & external links