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- W2111064819 endingPage "129" @default.
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- W2111064819 abstract "Sediment core M23414 from the Rockall Plateau (North Atlantic) covering the last two climatic cycles, marine isotope stages (MIS) 7 to 1, was investigated for glacial–interglacial variations in the deep-sea benthic ostracode fauna. A highly diversified ostracode fauna including 98 species was found. Two climate-related assemblages were identified, associated with interglacial and peak glacial periods, respectively. The ‘interglacial’ group occurs during the end of MIS 7, 5 and 1 and is composed of the genera Henryhowella, Pelecocythere, Echinocythereis, Cytherella, Bradleya, Aversovalva and Eucytherura. The ‘glacial’ group consists of the genera Acetabulastoma (which is known as ‘sea ice indicator’ in the modern Arctic Ocean), Polycope, Bythoceratina, ?Rhombobythere,and some species possibly belonging to the genus Pseudocythere and is found during MIS 6, 4 and 2. These longer-term variations within the ostracode fauna seem related to the particular glacial and interglacial climate conditions that affected both deep-water production as well as primary production in the surface waters. However, a detailed comparison of ostracode abundances with the occurrence of events marked by increased ice-rafted debris reveals also much shorter-term climate related changes in the ostracode fauna. Thus, the temporal fluctuations within ostracode assemblages reflect long- and short-term alterations of the deep-sea environment that are clearly linked to climate changes." @default.
- W2111064819 created "2016-06-24" @default.
- W2111064819 creator A5049411177 @default.
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- W2111064819 date "2000-08-01" @default.
- W2111064819 modified "2023-09-26" @default.
- W2111064819 title "Species composition and glacial–interglacial variations in the ostracode fauna of the northeast Atlantic during the past 200,000years" @default.
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- W2111064819 doi "https://doi.org/10.1016/s0377-8398(00)00034-7" @default.
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