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Synthetic and practical reconstructions of SST and seawater pH using the novel multiproxy SMITE method

Synthetic and practical reconstructions of SST and seawater pH using the novel multiproxy SMITE method
Synthetic and practical reconstructions of SST and seawater pH using the novel multiproxy SMITE method

Geochemical proxies of sea surface temperature (SST) and seawater pH (pH sw) in scleractinian coral skeletons are valuable tools for reconstructing tropical climate variability. However, most coral skeletal SST and pH sw proxies are univariate methods that are limited in their capacity to circumvent non-climate-related variability. Here we present a novel multivariate method for reconstructing SST and pH sw from the geochemistry of coral skeletons. Our Scleractinian Multivariate Isotope and Trace Element (SMITE) method optimizes reconstruction skill by leveraging the covariance across an array of coral elemental and isotopic data with SST and pH sw. First, using a synthetic proxy experiment, we find that SMITE SST reconstruction statistics (correlation, accuracy, and precision) are insensitive to noise and variable calibration period lengths relative to Sr/Ca. While SMITE pH sw reconstruction statistics remain relative to δ 11B throughout the same synthetic experiment, the magnitude of the long-term trend in pH sw is progressively lost under conditions of moderate-to-high analytical uncertainty. Next, we apply the SMITE method to an array of seven coral-based geochemical variables (B/Ca, δ 11B, Li/Ca, Mg/Ca, Sr/Ca, U/Ca & Li/Mg) measured from two Bermudan Porites astreoides corals. Despite a <3.5 year calibration period, SMITE SST and pH sw estimates exhibit significantly better accuracy, precision, and correlation with their respective climate targets than the best single- and dual-proxy estimators. Furthermore, SMITE model parameters are highly reproducible between the two coral cores, indicating great potential for fossil applications (when preservation is high). The results shown here indicate that the SMITE method can outperform the most common coral-based SST and pH sw reconstructions methods to date, particularly in datasets with a large variety of geochemical variables. We therefore provide a list of recommendations and procedures for users to begin implementing the SMITE method as well as an open-source software package to facilitate dissemination of the SMITE method.

Animals, Anthozoa/chemistry, Hydrogen-Ion Concentration, Seawater/chemistry, Temperature, Trace Elements/analysis
1932-6203
e0305607
Hughes, Hunter P.
130e0fd2-57b9-4171-a42e-04ea44f4b641
Thompson, Diane
d95b6969-c9c6-455e-a4c0-955f450c606f
Foster, Gavin L.
fbaa7255-7267-4443-a55e-e2a791213022
Lees, Jonathan
5665c969-29a8-4430-9f4c-46a9e68521ad
Surge, Donna
7d88cb57-54f6-4e18-93c2-0b88234d27ae
Standish, Christopher D.
0b996271-da5d-4c4f-9e05-a2ec90e8561d
Hughes, Hunter P.
130e0fd2-57b9-4171-a42e-04ea44f4b641
Thompson, Diane
d95b6969-c9c6-455e-a4c0-955f450c606f
Foster, Gavin L.
fbaa7255-7267-4443-a55e-e2a791213022
Lees, Jonathan
5665c969-29a8-4430-9f4c-46a9e68521ad
Surge, Donna
7d88cb57-54f6-4e18-93c2-0b88234d27ae
Standish, Christopher D.
0b996271-da5d-4c4f-9e05-a2ec90e8561d

Hughes, Hunter P., Thompson, Diane, Foster, Gavin L., Lees, Jonathan, Surge, Donna and Standish, Christopher D. (2024) Synthetic and practical reconstructions of SST and seawater pH using the novel multiproxy SMITE method. PLoS ONE, 19 (6 June), e0305607, [e0305607]. (doi:10.1371/journal.pone.0305607).

Record type: Article

Abstract

Geochemical proxies of sea surface temperature (SST) and seawater pH (pH sw) in scleractinian coral skeletons are valuable tools for reconstructing tropical climate variability. However, most coral skeletal SST and pH sw proxies are univariate methods that are limited in their capacity to circumvent non-climate-related variability. Here we present a novel multivariate method for reconstructing SST and pH sw from the geochemistry of coral skeletons. Our Scleractinian Multivariate Isotope and Trace Element (SMITE) method optimizes reconstruction skill by leveraging the covariance across an array of coral elemental and isotopic data with SST and pH sw. First, using a synthetic proxy experiment, we find that SMITE SST reconstruction statistics (correlation, accuracy, and precision) are insensitive to noise and variable calibration period lengths relative to Sr/Ca. While SMITE pH sw reconstruction statistics remain relative to δ 11B throughout the same synthetic experiment, the magnitude of the long-term trend in pH sw is progressively lost under conditions of moderate-to-high analytical uncertainty. Next, we apply the SMITE method to an array of seven coral-based geochemical variables (B/Ca, δ 11B, Li/Ca, Mg/Ca, Sr/Ca, U/Ca & Li/Mg) measured from two Bermudan Porites astreoides corals. Despite a <3.5 year calibration period, SMITE SST and pH sw estimates exhibit significantly better accuracy, precision, and correlation with their respective climate targets than the best single- and dual-proxy estimators. Furthermore, SMITE model parameters are highly reproducible between the two coral cores, indicating great potential for fossil applications (when preservation is high). The results shown here indicate that the SMITE method can outperform the most common coral-based SST and pH sw reconstructions methods to date, particularly in datasets with a large variety of geochemical variables. We therefore provide a list of recommendations and procedures for users to begin implementing the SMITE method as well as an open-source software package to facilitate dissemination of the SMITE method.

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More information

Accepted/In Press date: 3 June 2024
Published date: 25 June 2024
Additional Information: Publisher Copyright: © 2024 Hughes et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Keywords: Animals, Anthozoa/chemistry, Hydrogen-Ion Concentration, Seawater/chemistry, Temperature, Trace Elements/analysis

Identifiers

Local EPrints ID: 491716
URI: http://eprints.soton.ac.uk/id/eprint/491716
ISSN: 1932-6203
PURE UUID: 2f788614-9215-4515-bd39-c200753c335d
ORCID for Gavin L. Foster: ORCID iD orcid.org/0000-0003-3688-9668
ORCID for Christopher D. Standish: ORCID iD orcid.org/0000-0002-9726-295X

Catalogue record

Date deposited: 03 Jul 2024 16:33
Last modified: 12 Jul 2024 01:52

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Contributors

Author: Hunter P. Hughes
Author: Diane Thompson
Author: Gavin L. Foster ORCID iD
Author: Jonathan Lees
Author: Donna Surge

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