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Cited by 187

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Accurate estimation of sea surface temperatures using dissolution‐corrected calibrations for Mg/Ca paleothermometry

Rosenthal, Yair, Lohmann, George P.·2002·Paleoceanography

Abstract

Paired δ 18 O and Mg/Ca measurements on the same foraminiferal shells offer the ability to independently estimate sea surface temperature (SST) changes and assess their temporal relationship to the growth and decay of continental ice sheets. The accuracy of this method is confounded, however, by the absence of a quantitative method to correct Mg/Ca records for alteration by dissolution. Here we describe dissolution‐corrected calibrations for Mg/Ca‐paleothermometry in which the preexponent constant is a function of size‐normalized shell weight: (1) for G. ruber (212–300 μm) (Mg/Ca)ruber = (0.025 wt + 0.11) e0.095 T and (b) for G. sacculifer (355–425 μm) (Mg/Ca)sacc = (0.0032 wt + 0.181) e0.095 T. The new calibrations improve the accuracy of SST estimates and are globally applicable. With this correction, eastern equatorial Atlantic SST during the Last Glacial Maximum is estimated to be 2.9° ± 0.4°C colder than today.

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Metadata

Authors
Rosenthal, Y., & Lohmann, G. P.
Venue
Paleoceanography
Published
2002-09
Volume
17
Issue
3
ISSN
  • 0883-8305 (ISSN-L)
  • 1944-9186
OpenAlex
W1754578189
Cited by
187
References
1
FWCI
5.92
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Accurate estimation of sea surface temperatures using dissolution‐corrected calibrations for Mg/Ca paleothermometry. https://app.cochat.ai/papers/10.1029/2001pa000749
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Rosenthal, Y., & Lohmann, G. P. (2002). Accurate estimation of sea surface temperatures using dissolution‐corrected calibrations for Mg/Ca paleothermometry. Paleoceanography. https://doi.org/10.1029/2001pa000749

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