A · BT · CT · CF · F · J · J1-M267 · J1b-Z1853

Haplogroup J1b-Z1853

Macro-haplogroup
J
Parent clade
J1-M267
Formed (estimate)
c. 15,000–20,000 years before present
TMRCA (estimate)
c. 7,000–9,000 years ago

Overview

J1b-Z1853 forms one of the fundamental early branches of the J1-M267 lineage, diverging prior to both the major highland-associated J1-Z1828 radiation and the massive Arabian-centered J1-P58 expansion. The formation of J1b likely occurred during the early Holocene among upland populations inhabiting northern Mesopotamia, the Anatolian highlands, and the piedmont zones of the Zagros. Unlike P58—which underwent explosive Bronze Age expansions—J1b represents a moderate, regionally anchored lineage that retained strong cultural continuity with early agro-pastoral societies. J1b’s demographic history mirrors the transformation of the northern Fertile Crescent from mobile hunter-herder communities to sedentary agricultural societies. Its present rarity masks a once influential role in shaping the paternal landscape of the early highland–foothill ecotone cultures.

Geographic distribution

Modern concentrations of J1b appear primarily in northeastern Syria, southeastern Turkey, northern Iraq, and the Armenian highlands. Scattered frequencies extend into western Iran, the Caucasus, and occasionally the Levant. These distributions reflect long-term survival in upland and foothill refugia that resisted absorption into later P58-dominated Arabian expansions. Trace amounts across Mediterranean Europe likely represent minor ancient mobility rather than recent migrations. J1b’s presence in the Zagros and upper Tigris regions is particularly notable, marking it as a paternal lineage deeply tied to the early Holocene heartland of goat domestication and proto-agropastoral lifeways.

Ancient DNA

  • Early Neolithic samples from the Çayönü, Göbekli Tepe, and Karaca Dağ region show upstream J1-M267* signals compatible with the basal divergence leading to J1b.
  • Chalcolithic and Early Bronze Age individuals from the Upper Tigris and Euphrates basins demonstrate downstream variants consistent with Z1853-related ancestry.
  • Armenian highland Iron Age samples contain J1 lineages that may represent attenuated or drifted derivatives of early J1b.

Phylogeny & subclades

J1b-Z1853 forms a sister branch to J1-Z1828 and may represent the earliest major highland-oriented lineage of J1. Its internal structure suggests several microbranches concentrated around eastern Anatolia and the Armenian highlands. Despite its deep age, its surviving phylogenetic diversity is moderate, reduced by Bronze Age population turnovers dominated by J2, R1b-Z2103, and later Iranian-related expansions.

  • J1b* basal
  • Northern Mesopotamian microclusters
  • Armenian highland rare derivatives

Notes & context

J1b provides a crucial window into early Holocene paternal structure in the northern Fertile Crescent, offering a highland counterpart to the desert-margin ancestry preserved in J1a and a predecessor to the massive expansions of J1-P58 and J1-Z1828.