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The stratigraphic distribution of warm-water molluscs, planktonic foraminifers and diatoms in Plio-Pleistocene strata (3.5–0.8 Ma) of the Sea of Japan coast of Japan is the basis for reconstructing the history of the Tsushima Current. The results indicate: (1) the Tsushima Current flowed at 3.5, 3.2, 2.9, 2.4 and 1.9 Ma, in the 3.5–1.7 Ma interval; (2) the current flowed at every interglacial highstand,...
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