Reconstruction of deep-water conditions in the North Atlantic during MIS 9 based on benthic foraminiferal assemblages

被引:0
|
作者
S. A. Kostygov
E. S. Kandiano
H. A. Bauch
机构
[1] Saint Petersburg State University,Faculty of Geography and Geoecology
[2] Leibniz Institute of Marine Sciences (IFM-GEOMAR),undefined
[3] Mainz Academy of Sciences and Literature,undefined
来源
Oceanology | 2010年 / 50卷
关键词
Benthic Foraminifera; Marine Isotope Stage; North Atlantic Deep Water; North Atlantic Current; Mediterranean Outflow Water;
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摘要
Marine isotope stage (MIS) 9 is one of the least investigated Pleistocene interglaciations. The present study describes reconstructions of deep-water conditions during this time interval based on benthic foraminiferal assemblages from sediment core M23414 (Rockall Plateau, North Atlantic). The results of faunal analysis were supported by planktic δ18O, sea surface temperature reconstructions based on planktic foraminiferal assemblages and content of ice rafted debris. Statistical data processing using principal component analysis revealed five climate-related benthic foraminiferal associations that changed in response to alterations of deep-water circulation.
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页码:397 / 407
页数:10
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