Overview
I2a2b1 (S2606) represents a key Central European lineage descending from the I2-L38 (I2a2b) cluster. This clade has strong archaeological connections to Neolithic and Chalcolithic communities in the Rhine–Danube interaction zone and appears frequently in early farmer-associated genetic datasets. Later continuity through the Bronze Age and Iron Age suggests incorporation into emerging continental cultural complexes.
Geographic distribution
Modern frequencies peak in Germany, Belgium, Luxembourg, Switzerland, eastern France and Austria. Minor frequencies occur in the British Isles and Scandinavia due to later mobility.
Ancient DNA
- Late Neolithic Rhine–Danube samples include lineages ancestral to S2606.
- Bell Beaker-associated individuals in Central Europe have yielded close upstream variants.
- Early Bronze Age south German burials show microclades within the I2a2b structure.
Phylogeny & subclades
I2a2b1 descends from the I2-L38 trunk. SNP S2606 marks a major subdivision separating it from parallel continental branches. The downstream topology reveals slow but steady diversification tied to local prehistoric populations.
- I2-Y15575
- I2-S2606* basal clades
Notes & context
I2a2b1 is a meaningful marker for studying the paternal genetic impact of early European farming populations and their interaction with indigenous Mesolithic substrata.
References & external links