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 |
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Pages (from-to) | 1641-1654 |
Journal | Quaternary Science Reviews |
Volume | 18 |
DOIs | |
Publication status | Published - 1999 |