The long-term record of glacial/interglacial cycles indicates three major paleoceanographic
regimes in the Norwegian Sea. The period since the first major glaciation over Scandinavia …

Sediment fluxes were highest in the Norwegian Sea during late glacial/early deglacial
periods, ie, at oxygen isotope transition 4 3, below transition 6 5, at various levels within …

Planktonic foraminiferal assemblages in Norwegian Sea sediments show that during the
past 450,000 years a glacial regime, characterized by permanent sea-ice cover and the …

Sedimentological, isotopic and magnetostratigraphic investigations of Ocean Drilling
Program and Deep Sea Drilling Project sites 642, 643, 644 and 610 document the …

Synoptically mapped faunal abundance and faunal composition data, derived from a suite of
24 Norwegian Sea cores, were used to derive sea‐surface temperatures for the last glacial …

In a region of generally thin Holocene sediment cover along the outer Norwegian
continental margin, a 565 cm long piston core was taken, which contained more than 4 m of …

Studies of ice-rafted detritus in ODP holes from the Norwegian Sea document a series of
glacial episodes in the surroundings of the Norwegian—Greenland Sea from the late …

The present temperature regime of the Norwegian and Greenland Seas results largely from
the warm Norwegian Current. This current is partially responsible for the maritime climates of …

Despite a long history of investigation, critical issues regarding the last glacial cycle in
northwest Europe remain unresolved. One of these refers to the extent, timing and dynamics …

DSDP/ODP drilling in the northern North Atlantic reveals that so far the onset of northern
hemisphere cooling deduced from the occurrence of ice-rafted debris (IRD) in deep-sea …