Overview
O1b2 is a major branch of O1b originating during the Late Pleistocene and forms a central paternal component of Korean and Japanese populations. Earlier literature mislabeled this clade as “O2b”, but updated phylogenies recognize it as O1b2 under the O1b-F3651 umbrella. O1b2 has deep roots in northeast Asian forager and proto-agricultural populations and played an important role in the formation of ancient cultures on the Korean Peninsula and the Japanese archipelago.
Geographic distribution
Very common in Japan (particularly among Yamato and Ryukyu populations) and high in Korea. Lower frequencies exist in Manchuria, Primorye, Mongolia and northern China. Small traces occur in some Tungusic and Ainu-related groups.
Ancient DNA
- Ancient samples from the Jōmon–Yayoi transition show paternal signals upstream of O1b2.
- Bronze Age sites in Korea reveal lineages compatible with O1b2-level ancestry.
- Distribution patterns suggest population continuity from prehistoric northeast Asian groups into historic Korean and Japanese populations.
Phylogeny & subclades
O1b2 is parallel to the O1b1 branch (which includes M95). The internal structure includes several region-specific subbranches, some of which are concentrated in Japan and Korea.
Notes & context
O1b2 is indispensable for reconstructing Korean and Japanese paternal genetic formation and must be included in any complete O atlas.
References & external links