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  • 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