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
|Publication status||Published - 2000|
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Stable isotope data and calcification temperature from planktic foraminifera in sediment core BOFS31/1K
Elderfield, H. (Contributor) & Ganssen, G. M. (Contributor), Unknown Publisher, 3 Jun 2000
DOI: 10.1594/PANGAEA.143845, https://doi.pangaea.de/10.1594/PANGAEA.143845