Age determinations for ODP Sites in the Norwegian-Greenland Sea ...
Records of biogenic and terrigenous components have been obtained from the interval corresponding to the last 2.6 m.y. of ODP Sites 643 and 644 in order to reconstruct surface and deep water regimes in the Norwegian Sea.Surface water regimes record long lasting moderate glacial conditions during the...
| Main Authors: | , |
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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PANGAEA
1994
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| Subjects: | |
| Online Access: | https://dx.doi.org/10.1594/pangaea.702108 https://doi.pangaea.de/10.1594/PANGAEA.702108 |
| Summary: | Records of biogenic and terrigenous components have been obtained from the interval corresponding to the last 2.6 m.y. of ODP Sites 643 and 644 in order to reconstruct surface and deep water regimes in the Norwegian Sea.Surface water regimes record long lasting moderate glacial conditions during the interval 2.6 1.0 Ma. Small intrusions of Atlantic water episodically penetrated into the Norwegian Sea forming a narrow tongue along the eastern margin, which is documented at Site 644. The polar front was most probably situated between the Site 644 and 643 locations on the outer Voring Plateau during these time intervals. Deep water regimes reflect long-term persistent corrosive bottom waters, most probably due to a weakly undersaturated water column and a low rate of carbonate shell production in surface waters. Deep water production in the Norwegian-Greenland Sea may have operated in a different way, e.g. brine formation during winter sea ice growth. Bottom waters were oxygenated throughout the entire period, ... : Supplement to: Henrich, Rüdiger; Baumann, Karl-Heinz (1994): Evolution of the Norwegian Current and the Scandinavian Ice Sheets during the past 2.6 m.y,: evidence from ODP Leg 104 biogenic carbonate and terrigenous records. Palaeogeography, Palaeoclimatology, Palaeoecology, 108(1-2), 75-94 ... |
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