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...
Published in: | Quaternary Science Reviews |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
1999
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Subjects: | |
Online Access: | https://research.vu.nl/en/publications/3dbf5bc3-19f1-497a-9e15-da5273bc1099 https://doi.org/10.1016/S0277-3791(99)00011-6 |
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 |
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