chronologies, and a planktonic foraminiferal δ18O stratigraphy for the last 50,000 years from
Japan Sea cores from the Oki Ridge. In this paper we report AMS 14C results that allow us
to reconstruct a high-resolution chronology of the cores and discuss millennial scale climate
changes recorded in Japan Sea sediments. The sedimentation rate for the site increased
dramatically from the glacial stage to the Holocene as a result of significant hydrological …