Now showing items 1-3 of 3
Late Holocene surface ocean conditions of the Norwegian Sea (Vøring Plateau)
(American Geophysical Union, 2003-06-04)
Late Holocene sea surface ocean conditions of the eastern Norwegian Sea (Vøring Plateau) are inferred from planktic stable isotopes and planktic foraminiferal assemblage changes in cores JM97-948/2A and MD95-2011 (66.97°N, ...
Inception of the Northern European Ice Sheet due to contrasting ocean and insolation forcing
About 115,000 years ago the last interglacial reached its terminus and nucleation of new ice sheet growth was initiated. Evidence from the northernmost Nordic Seas indicate that the inception of the last glacial was ...
A high-resolution study of Holocene paleoclimatic and paleoceanographic changes in the Nordic Seas
(American Geophysical Union, 2003-03-26)
High-resolution records from IMAGES core MD95-2011 in the eastern Norwegian Sea provide evidence for relatively large- and small-scale high-latitude climate variability throughout the Holocene. During the early and ...