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Q-mode principal component analysis (PCA) of a fossil diatom assemblage reveals the late Quaternary paleoceanography of the NW Pacific margin, based on submarine core KH94-3, LM-8 recovered off the Sanriku coast of NE Japan (38 o 53.46'N, 143 o 22.19'E). Overall, diatoms were abundant during interglacials, but low in abundance and poor in preservation during the last glacial, with...
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