Benthic foraminiferal biodiversity response to changing Arctic palaeoclimate

Four sediment cores recovered from 1000 to 2500 m water depth in the Arctic Ocean, tracing the inflowing Atlantic water from Fram Strait, Yermak Plateau, northern Barents Sea...本数据集包含4个采自北冰洋1000至2500米水深的沉积物岩芯（sediment cores），可用于示踪源自弗拉姆海峡（Fram Strait）、耶尔马克高原（Yermak Plateau）以及巴伦支海北部的大西洋流入水。