Increases in fine-and silt-grained terrigenous components from MIS 5.3 to the Middle Holocene imply that sea ice on the Bering Sea slope extended continuously in a cooling climate.
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MIS5.;3期至中全新世;不断增加的陆源砂级和粉砂级颗粒组分说明随着气候的逐渐变冷;陆架海冰在不断扩张
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