Water mass evolution of the Greenland Sea since late glacial times

Four sediment cores from the central and northern Greenland Sea basin, a crucial area for the renewal of North Atlantic deep water, were analyzed for planktic foraminiferal fauna, planktic and benthic stable oxygen and carbon iso- topes as well as ice-rafted debris to reconstruct the environ- mental...

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Bibliographic Details
Main Authors: Telesiński, Maciej Mateusz, Spielhagen, Robert F, Bauch, Henning A
Format: Dataset
Language:English
Published: PANGAEA 2014
Subjects:
Greenland
Greenland Sea
Nordic Seas
North Atlantic Deep Water
North Atlantic
Sea ice
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.832368
https://doi.org/10.1594/PANGAEA.832368

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