Abstract
Determining the past record of temperature and salinity of ocean surface waters is essential for understanding past changes in climate, such as those which occur across glacial-interglacial transitions. As a useful proxy, the oxygen isotope composition (δ
Original language | English |
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Pages (from-to) | 442-445 |
Journal | Nature |
Volume | 405 |
DOIs | |
Publication status | Published - 2000 |