Overview
Q-L323 is a minor but phylogenetically valid branch within the broader Q-M346 radiation. It is most closely associated with central and north-central Siberian forest-steppe populations. Although rare today, the lineage reflects a demographic layer linked to small-scale, sedentary-forager societies that occupied transitional zones between the Upper Yenisei and the Central Siberian Plateau during the mid-Holocene. This branch highlights paternal continuity independent of later Turkic, Tungusic, and Mongolic expansions.
Geographic distribution
Observed at low frequency among Khakas, Shor, Selkup, and certain mixed Siberian groups. Occasional presence in Altai–Sayan region likely reflects historical contact rather than major demographic impact.
Ancient DNA
- Ancient individuals from the central Siberian plateau show partial ancestry linkable to L323-level clades.
- Temporal estimates align with stable mid-Holocene settlement patterns in forest-steppe ecotones.
- Genetic patterns indicate slow expansion and high levels of drift typical of micro-populations.
Phylogeny & subclades
L323 branches shallowly and contains only small subclusters, consistent with drift-driven populations.
Notes & context
Although rare, Q-L323 helps clarify fine-scale Siberian paternal history and complements the mapping of Q-M346 diversity.
References & external links