Distribution of planktonic foraminifers in ODP Hole 104-642A (Table 2)@en

Ice-rafted fossils of late Cretaceous and Tertiary age were detected in Pleistocene-Pliocene glacially influenced sediments of the Voring Plateau, eastern Norwegian Sea. The ice-rafted associations contain frequent Inoceramus (Bivalvia) prisms and rare occurrences of both benthic and planktonic foraminifers of Miocene, Oligocene, and Maastrichtian to Campanian age. As source areas, shallow outcrops on the Norwegian Continental Shelf as well as the Greenland Shelf and the North and Baltic Seas have to be considered.在挪威海东部沃林海台（Voring Plateau）的更新世-上新世受冰川作用影响的沉积物中，检出白垩纪晚期及第三纪的冰筏化石（ice-rafted fossils）。该冰筏组合（ice-rafted associations）中常见双壳纲（Bivalvia）叠瓦蛤属（Inoceramus）的棱柱壳体，且零星产出中新世（Miocene）、渐新世（Oligocene）以及马斯特里赫特期（Maastrichtian）至坎潘期（Campanian）的底栖与浮游有孔虫（foraminifers）。其物源区需纳入挪威大陆架（Norwegian Continental Shelf）、格陵兰大陆架（Greenland Shelf）以及北海与波罗的海的浅层出露区域。