Abstract
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
| Original language | English |
|---|---|
| Pages (from-to) | 1641-1654 |
| Journal | Quaternary Science Reviews |
| Volume | 18 |
| DOIs | |
| Publication status | Published - 1999 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 14 Life Below Water
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