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Ice-rafted debris (IRD) from sediment traps, surficial sediments, and sediment cores were investigated in order to reconstruct the extent history of sea-ice cover during the last 100kyrs in the Okhotsk Sea. The seasonal IRD buried into the sediments, during and just after sea-ice melting in spring, consists of silt- and sand- size terrigenous particles. The spatial distribution of IRD within surficial...
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