Past temperature and d18O of surface ocean waters inferred from foraminiferal Mg/Ca ratios.

H. Elderfield; G.M. Ganssen

doi:10.1038/35013033

Past temperature and d18O of surface ocean waters inferred from foraminiferal Mg/Ca ratios.

H. Elderfield, G.M. Ganssen

Earth and Climate

Research output: Contribution to Journal › Article › Academic › peer-review

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	https://doi.org/10.1038/35013033
Publication status	Published - 2000

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10.1038/35013033

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

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title = "Past temperature and d18O of surface ocean waters inferred from foraminiferal Mg/Ca ratios.",

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",

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AU - Elderfield, H.

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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

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SP - 442

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JO - Nature

JF - Nature

SN - 0028-0836

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Past temperature and d18O of surface ocean waters inferred from foraminiferal Mg/Ca ratios.

Abstract

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Stable isotope data and calcification temperature from planktic foraminifera in sediment core BOFS31/1K

Cite this