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Haplogroup R-Y38

Macro-haplogroup
R
Parent clade
R-M73
Formed (estimate)
c. 9000 - 11000 years before present
TMRCA (estimate)
c. 4500 - 6000 years ago

Overview

Haplogroup R-Y38 represents one of the earliest diverging downstream branches of the R-M73 macro lineage and provides a critical genetic link to the late Mesolithic and early Holocene expansion of forager communities across the western Siberian basin. Its formation coincides with a period of climatic stabilization after the retreat of the last glacial systems, allowing small hunter fisher groups to expand into new ecological zones along the middle Ob, Irtysh and Tobol river networks. These groups maintained high mobility but also engaged in periodic semi sedentary occupations around resource rich lakes and river systems. The downstream phylogeny of Y38 demonstrates moderate branching, suggesting that separate micro populations developed by the mid Holocene. Archaeological contexts from the region show parallel developments, including refinements in woodworking techniques, widespread adoption of composite tools and intensified use of aquatic resources. The coherence between the archaeological record and the genetic structure of Y38 makes the lineage a significant anchor in reconstructing prehistoric population movements in western Siberia. Modern traces of R-Y38 are rare but detectable in parts of southwestern Siberia, especially among groups with long standing historical ties to the forest steppe corridor. The lineage survived demographic transformations brought by Bronze Age steppe pastoralists and later influences from Ugric and Turkic expansions, indicating that isolated pockets of Holocene foragers persisted in marginal ecological zones.

Geographic distribution

Western Siberian basin, middle Ob and Irtysh river systems, Tobol region.

Ancient DNA

  • Mesolithic forager sites in the middle Ob basin show upstream R-M73 signals compatible with early Y38 ancestry.
  • Neolithic cultures of the forest steppe exhibit mixed genetic profiles with components tied to Y38 bearing populations.
  • Early Bronze Age individuals in western Siberia carry upstream clades consistent with Y38 related groups.

Phylogeny & subclades

R-Y38 shows early internal branching patterns tied to ecologically stable riverine and wetland regions of western Siberia.

  • R-Y38*
  • Middle Ob microbranch
  • Irtysh forest-steppe cluster

Notes & context

A key lineage for reconstructing postglacial recolonization patterns in the forest-steppe corridor of western Siberia.