The structure of Termination II (penultimate deglaciation and Eemian) in the North Atlantic.

A study of the 140-100 ka interval in core T90-9P from the North Atlantic (45°N, 25°W), based on analysis of oxygen and carbon isotope records from planktonic and benthonic foraminifera, and from the bulk sediment fine fraction facilitates a detailed paleoceanographic reconstruction of the penultima...

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Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Lototskaya, A., Ganssen, G.M.
Format: Article in Journal/Newspaper
Language:English
Published: 1999
Subjects:
Online Access:https://research.vu.nl/en/publications/3dbf5bc3-19f1-497a-9e15-da5273bc1099
https://doi.org/10.1016/S0277-3791(99)00011-6
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Summary:A study of the 140-100 ka interval in core T90-9P from the North Atlantic (45°N, 25°W), based on analysis of oxygen and carbon isotope records from planktonic and benthonic foraminifera, and from the bulk sediment fine fraction facilitates a detailed paleoceanographic reconstruction of the penultimate deglaciation (Termination II), and of the Eemian interglacial (δ