Dinoflagellate cyst counts of sediment core GIK23071-3 ...

Marine sediments from the Vøring Plateau (Norwegian Sea) have been studied for their dinoflagellate cyst (dinocyst) and foraminiferal content in order to reconstruct sea-surface conditions in the eastern Norwegian Sea during Marine Isotope Stage (MIS) 5e. In combination with stable oxygen isotope an...

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Bibliographic Details
Main Authors: Van Nieuwenhove, Nicolas, Bauch, Henning A, Matthiessen, Jens
Format: Dataset
Language:English
Published: PANGAEA 2008
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.603233
https://doi.pangaea.de/10.1594/PANGAEA.603233
Description
Summary:Marine sediments from the Vøring Plateau (Norwegian Sea) have been studied for their dinoflagellate cyst (dinocyst) and foraminiferal content in order to reconstruct sea-surface conditions in the eastern Norwegian Sea during Marine Isotope Stage (MIS) 5e. In combination with stable oxygen isotope and ice rafted detritus (IRD) data, the variations in foraminiferal and dinocyst assemblage composition reflect a stepwise transition from the final phase of deglaciation (Termination II) into typical interglacial conditions. This stepwise change is repeated subsequently during the cooling conditions of glacial inception towards MIS 5d. The interval studied is characterized by relatively high abundances of Bitectatodinium tepikiense, in comparison to present-day values in the area, indicating a larger seasonal temperature amplitude with enhanced surface water stratification during MIS 5e. The important occurrence of the warm-temperate dinocyst Spiniferites mirabilis s.l. concurrent with subpolar foraminifers ... : <1 indicates that the species is present, but was not encountered during counting; a question mark indicates that the determination of the species is questionable; the number following the question mark gives the number of questionable specimens encountered during counting ...