A · A1 · A1b · A1b1 · BT · CT · CF · F · K · K2 · P · R · R1 · R1a · R1a1 · R1a1a · R1a1a1 · R1a-Z283 · R1a-Z282 · R1a-Z280 · R1a-Y33 · R1a-Y2613 · R1a-Y2619

Haplogroup R1a-Y2619

Macro-haplogroup
R
Parent clade
R1a-Y2613
Formed (estimate)
c. 3,400 - 3,800 years before present (estimate)
TMRCA (estimate)
c. 2,200 - 2,600 years ago (estimate)

Overview

R1a-Y2619 is one of the principal subbranches under R1a-Y2613 and exhibits a complex and deeply structured phylogeny. Emerging in the late Bronze Age, Y2619 lineages became part of the dense cultural and demographic networks that characterized the forest zone of Belarus, Russia and northern Ukraine. Archaeological contexts indicate that early Y2619 ancestors participated in the evolution of fortified hilltop settlements, ritual sites and regional exchange systems linking Baltic and Slavic populations. During the Iron Age, Y2619 became widespread among groups occupying the upper Volga and Dnieper regions. These populations played central roles in cultural traditions that included the Milograd and early Baltic hillfort cultures. Over time, Y2619 became increasingly tied to proto Slavic and eastern Baltic peoples. Its significant diversification during the early medieval era reflects founder effects associated with the rise of Slavic tribal confederations and the early Rus state. Today, R1a-Y2619 remains a prominent component of eastern European paternal variation and is especially valued in genetic genealogy for its fine regional resolution.

Geographic distribution

R1a-Y2619 occurs at high frequencies in Belarus and western Russia. It is also common in Lithuania, Latvia and northern Ukraine. Moderate levels appear in Poland, Estonia and northeastern Germany. Smaller clusters are found in the Balkans due to medieval Slavic migrations.

Ancient DNA

  • Iron Age individuals from the upper Volga region carry lineages mapping to early Y2619.
  • Baltic hillfort cultures show traces of deeper Y33 → Y2613 → Y2619 ancestry.
  • Proto Slavic burials in the Polesia region contain downstream Y2619 individuals.
  • Medieval Krivich and Dregovich sites show strong continuity with Y2619.
  • Forest-steppe Iron Age sites in Belarus and northern Ukraine reveal early Y2619 substructure.

Phylogeny & subclades

Y2619 includes several deep subbranches such as Y2620, YP623 and regionally anchored Slavic microclusters. The phylogeny demonstrates considerable medieval expansion layered over older Bronze Age structure.

  • R1a-Y2620
  • R1a-YP623
  • Additional Slavic microclusters

Notes & context

R1a-Y2619 is important for high-resolution analysis of eastern Slavic and Baltic populations and provides a fine-scale view of medieval demographic expansions.