Abstract
| Original language | English |
|---|---|
| Pages (from-to) | 442-445 |
| Journal | Nature |
| Volume | 405 |
| DOIs | |
| Publication status | Published - 2000 |
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Past temperature and d18O of surface ocean waters inferred from foraminiferal Mg/Ca ratios. / Elderfield, H.; Ganssen, G.M.
In: Nature, Vol. 405, 2000, p. 442-445.Research output: Contribution to Journal › Article › Academic › peer-review
TY - JOUR
T1 - Past temperature and d18O of surface ocean waters inferred from foraminiferal Mg/Ca ratios.
AU - Elderfield, H.
AU - Ganssen, G.M.
PY - 2000
Y1 - 2000
N2 - 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
AB - 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
U2 - 10.1038/35013033
DO - 10.1038/35013033
M3 - Article
VL - 405
SP - 442
EP - 445
JO - Nature
JF - Nature
SN - 0028-0836
ER -