Ice-rafted fossils of late Cretaceous and Tertiary age were detected in Pleistocene-Pliocene glacially influenced sediments of the Vdring 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
Two ultra-high resolution IMAGES sediment cores from the SW continental slope of the Barents Sea and...
Geological evidence indicates that sediment reworking is common around the continental margins and a...
Ocean circulation changes along the continental shelf of the Nordic and Barents Seas have been inves...
Ice-rafted fossils of late Cretaceous and Tertiary age were detected in Pleistocene-Pliocene glacial...
The long-term record of glacial/interglacial cycles indicates three major paleoceanographic regimes ...
Studies of ice-rafted detritus in ODP holes from the Norwegian Sea document a series of glacial epis...
The long-term record of glacial/interglacial cycles indicates three major paleoceanographic regimes ...
Sedimentological and faunal records from the transitional period marking the onset of widespread nor...
International audienceAbstract Fluctuations in benthic foraminiferal faunas over the last 130,000 yr...
Sedimentological and faunal records from the transitional period marking the onset of widespread nor...
Sediment fluxes were highest in the Norwegian Sea during late glacial/early deglacial periods, i.e.,...
The abundance and composition of the upper Cenozoic terrigenous coarse-sand fraction (250 µm-2 mm) a...
Sites 642, 643, and 644 were investigated for planktonic foraminifers. Frequent occurrences of barre...
Based on benthic and planktic foraminifera, Bolboforma, oxygen isotope measurements and seismic data...
Four Tertiary wells on the Halten Terrace, Norway are studied and benthic foraminifers and other mic...
Two ultra-high resolution IMAGES sediment cores from the SW continental slope of the Barents Sea and...
Geological evidence indicates that sediment reworking is common around the continental margins and a...
Ocean circulation changes along the continental shelf of the Nordic and Barents Seas have been inves...
Ice-rafted fossils of late Cretaceous and Tertiary age were detected in Pleistocene-Pliocene glacial...
The long-term record of glacial/interglacial cycles indicates three major paleoceanographic regimes ...
Studies of ice-rafted detritus in ODP holes from the Norwegian Sea document a series of glacial epis...
The long-term record of glacial/interglacial cycles indicates three major paleoceanographic regimes ...
Sedimentological and faunal records from the transitional period marking the onset of widespread nor...
International audienceAbstract Fluctuations in benthic foraminiferal faunas over the last 130,000 yr...
Sedimentological and faunal records from the transitional period marking the onset of widespread nor...
Sediment fluxes were highest in the Norwegian Sea during late glacial/early deglacial periods, i.e.,...
The abundance and composition of the upper Cenozoic terrigenous coarse-sand fraction (250 µm-2 mm) a...
Sites 642, 643, and 644 were investigated for planktonic foraminifers. Frequent occurrences of barre...
Based on benthic and planktic foraminifera, Bolboforma, oxygen isotope measurements and seismic data...
Four Tertiary wells on the Halten Terrace, Norway are studied and benthic foraminifers and other mic...
Two ultra-high resolution IMAGES sediment cores from the SW continental slope of the Barents Sea and...
Geological evidence indicates that sediment reworking is common around the continental margins and a...
Ocean circulation changes along the continental shelf of the Nordic and Barents Seas have been inves...