Climatic change at the end of the last glaciation in Japan inferred from pollen in three cores from the Northwest Pacific Ocean
The AA. examine paleoclimatic evidence from northeast Asia. The primary data are pollen time-series from three high sedimentation-rate marine cores from which a cooling event described as coeval with the Younger Dryas Chronozone has been identified
Pollen and radiolarian records from deep-sea core RC 14-103: climatic reconstructions of northeast Japan and northwest Pacific for the last 90,000 years