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Planktic foraminifera shell chemistry response to seawater chemistry: Pliocene-Pleistocene seawater Mg/Ca, temperature and sea level change

Planktic foraminifera shell chemistry response to seawater chemistry: Pliocene-Pleistocene seawater Mg/Ca, temperature and sea level change
Planktic foraminifera shell chemistry response to seawater chemistry: Pliocene-Pleistocene seawater Mg/Ca, temperature and sea level change
Foraminifera Mg/Ca paleothermometry forms the basis of a substantial portion of ocean temperature reconstruction over the last 5 Ma. Furthermore, coupled Mg/Ca–oxygen isotope (δ18O) measurements of benthic foraminifera can constrain eustatic sea level (ESL) independent of paleo-shoreline derived approaches. However, this technique suffers from uncertainty regarding the secular variation of the Mg/Ca seawater ratio (Mg/Casw) on timescales of millions of years. Here we present coupled seawater–test Mg/Ca–temperature laboratory calibrations of Globigerinoides ruber in order to test the widely held assumptions that (1) seawater–test Mg/Ca co-vary linearly, and (2) the Mg/Ca–temperature sensitivity remains constant with changing Mg/Casw. We find a nonlinear Mg/Catest–Mg/Casw relationship and a lowering of the Mg/Ca–temperature sensitivity at lower than modern Mg/Casw from 9.0% °C−1 at Mg/Casw = 5.2 mol mol−1 to
at 3.4 mol mol−1. Using our calibrations to more accurately calculate the offset between Mg/Ca and biomarker-derived paleotemperatures for four sites, we derive a Pliocene Mg/Casw ratio of ∼4.3 mol mol−1. This Mg/Casw implies Pliocene ocean temperature 0.9–1.9 °C higher than previously reported and, by extension, ESL ∼30 m lower compared to when one assumes that Pliocene Mg/Casw is the same as at present. Correcting existing benthic foraminifera datasets for Mg/Casw indicates that deep water source composition must have changed through time, therefore seawater oxygen isotope reconstructions relative to present day cannot be used to directly reconstruct Pliocene ESL.
0012-821X
139-148
Evans, D.
878c65c7-eab9-4362-896b-166e165eb94b
Brierley, C.
fea91a57-dd3c-47db-873d-3fb319f14c2b
Raymo, M.E.
eda6af85-8c8a-40d8-8777-a262b1e03ab4
Erez, J.
6f95b6b8-cd13-4164-b773-ac7e637293bb
Müller, W.
5516e747-008e-49d9-912f-942b668fa1a0
Evans, D.
878c65c7-eab9-4362-896b-166e165eb94b
Brierley, C.
fea91a57-dd3c-47db-873d-3fb319f14c2b
Raymo, M.E.
eda6af85-8c8a-40d8-8777-a262b1e03ab4
Erez, J.
6f95b6b8-cd13-4164-b773-ac7e637293bb
Müller, W.
5516e747-008e-49d9-912f-942b668fa1a0

Evans, D., Brierley, C., Raymo, M.E., Erez, J. and Müller, W. (2016) Planktic foraminifera shell chemistry response to seawater chemistry: Pliocene-Pleistocene seawater Mg/Ca, temperature and sea level change. Earth and Planetary Science Letters, 438, 139-148. (doi:10.1016/j.epsl.2016.01.013).

Record type: Article

Abstract

Foraminifera Mg/Ca paleothermometry forms the basis of a substantial portion of ocean temperature reconstruction over the last 5 Ma. Furthermore, coupled Mg/Ca–oxygen isotope (δ18O) measurements of benthic foraminifera can constrain eustatic sea level (ESL) independent of paleo-shoreline derived approaches. However, this technique suffers from uncertainty regarding the secular variation of the Mg/Ca seawater ratio (Mg/Casw) on timescales of millions of years. Here we present coupled seawater–test Mg/Ca–temperature laboratory calibrations of Globigerinoides ruber in order to test the widely held assumptions that (1) seawater–test Mg/Ca co-vary linearly, and (2) the Mg/Ca–temperature sensitivity remains constant with changing Mg/Casw. We find a nonlinear Mg/Catest–Mg/Casw relationship and a lowering of the Mg/Ca–temperature sensitivity at lower than modern Mg/Casw from 9.0% °C−1 at Mg/Casw = 5.2 mol mol−1 to
at 3.4 mol mol−1. Using our calibrations to more accurately calculate the offset between Mg/Ca and biomarker-derived paleotemperatures for four sites, we derive a Pliocene Mg/Casw ratio of ∼4.3 mol mol−1. This Mg/Casw implies Pliocene ocean temperature 0.9–1.9 °C higher than previously reported and, by extension, ESL ∼30 m lower compared to when one assumes that Pliocene Mg/Casw is the same as at present. Correcting existing benthic foraminifera datasets for Mg/Casw indicates that deep water source composition must have changed through time, therefore seawater oxygen isotope reconstructions relative to present day cannot be used to directly reconstruct Pliocene ESL.

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More information

Accepted/In Press date: 13 January 2016
e-pub ahead of print date: 29 January 2016
Published date: 4 February 2016

Identifiers

Local EPrints ID: 502413
URI: http://eprints.soton.ac.uk/id/eprint/502413
ISSN: 0012-821X
PURE UUID: 64a95839-343a-4d68-963a-44eb95b3f2fc
ORCID for D. Evans: ORCID iD orcid.org/0000-0002-8685-671X

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Date deposited: 25 Jun 2025 16:44
Last modified: 26 Jun 2025 02:10

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Contributors

Author: D. Evans ORCID iD
Author: C. Brierley
Author: M.E. Raymo
Author: J. Erez
Author: W. Müller

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