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 |
---|---|
Pages (from-to) | 442-445 |
Journal | Nature |
Volume | 405 |
DOIs | |
Publication status | Published - 2000 |
Fingerprint
Dive into the research topics of 'Past temperature and d18O of surface ocean waters inferred from foraminiferal Mg/Ca ratios.'. Together they form a unique fingerprint.Datasets
-
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
Dataset