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Pliocene and Pleistocene chronostratigraphy and paleoenvironment of the central Arctic Ocean, using deep water agglutinated foraminifera

机译:北冰洋中部的上新世和更新世年代地层和古环境,使用深水凝集的有孔虫

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摘要

Deep-water agglutinated foraminifera (DWAF) were studied from Cores PS2177-5, Ps2200-5, Ps2212-3 and PS2185-6; from the R/V POLARSTERN ARK-VIII/3 Cruise in the central Arctic Ocean. The sediments were non-calcareous containing a sparse assemblage of eleven DWAF species. A chronostratigraphic framework is presented for Cores PS2200-t and Ps2185-6. Paleoenviron- mental data suggests a bathyal environment (2000-4000m) affected by water masses in the Arctic Ocean. The taxonomy of all of the DWAF found is presented and illustrated. A new species of the Family Trochamminidae; Trochammina lomonosovensis n. Sp. Is de- Scribed and illustrated.
机译:从Core PS2177-5,Ps2200-5,Ps2212-3和PS2185-6研究了深水凝集性有孔虫(DWAF);来自北冰洋中部的R / V POLARSTERN ARK-VIII / 3游轮。沉积物是非钙质的,包含11种DWAF物种的稀疏组合。提出了针对PS2200-t和Ps2185-6岩心的年代地层框架。古环境数据表明,受北冰洋水团影响的海床环境(2000-4000m)。介绍并说明了所有发现的DWAF的分类。 Tro科的新种;罗蒙索夫菌Sp。进行了说明和图示。

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