Abstract
Relatively warm climates and isolated deep water conditions prevailed prior to 13.6 Ma and between 5.6-4.8 Ma. The first major deep water outflow from the Norwegian-Greenland Sea into the North Atlantic took place at about 13.6 Ma. A major onset of ice-rafted debris is recorded at 2.56 Ma. -from Authors
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CITATION STYLE
Henrich, R., Wolf, T., Bohrmann, G., & Thiede, J. (1989). Cenozoic paleoclimatic and paleoceanographic changes in the Northern Hemisphere revealed by variability of coarse-fraction composition in sediments from the Voring Plateau - ODP Leg 104 drill sites. Proc., Scientific Results, ODP, Leg 104, Norwegian Sea, 75–188. https://doi.org/10.2973/odp.proc.sr.104.196.1989
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