Strong coupling between biomineral morphology and Sr/Ca of Arctica islandica (Bivalvia) : implications for Shell Sr/Ca-based temperature estimates
Bivalve shells serve as powerful high-resolution paleoclimate archives. However, the number of reliable temperature proxies is limited. It has remained particularly difficult to extract temperature signals from shell Sr/Ca, although Sr is routinely employed in other biogenic aragonites. In bivalves,...
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Johannes Gutenberg-Universität Mainz
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ftunivmainzpubl:oai:openscience.ub.uni-mainz.de:20.500.12030/6904 2023-05-15T15:22:30+02:00 Strong coupling between biomineral morphology and Sr/Ca of Arctica islandica (Bivalvia) : implications for Shell Sr/Ca-based temperature estimates Brosset, Cornélia Höche, Nils Shirai, Kotaro Mertz-Kraus, Regina Schöne, Bernd R. 2022 https://openscience.ub.uni-mainz.de/handle/20.500.12030/6904 https://hdl.handle.net/20.500.12030/6904 https://doi.org/10.25358/openscience-6893 eng eng Johannes Gutenberg-Universität Mainz http://doi.org/10.25358/openscience-6893 https://openscience.ub.uni-mainz.de/handle/20.500.12030/6904 2075-163X CC BY https://creativecommons.org/licenses/by/4.0/ openAccess CC-BY Minerals. 12. 5. 2022. -. -. 500 ddc:550 ddc:560 Zeitschriftenaufsatz publishedVersion Text doc-type:article 2022 ftunivmainzpubl https://doi.org/20.500.12030/6904 https://doi.org/10.25358/openscience-6893 2023-01-08T23:38:04Z Bivalve shells serve as powerful high-resolution paleoclimate archives. However, the number of reliable temperature proxies is limited. It has remained particularly difficult to extract temperature signals from shell Sr/Ca, although Sr is routinely employed in other biogenic aragonites. In bivalves, Sr/Ca is linked to the prevailing microstructure and is sometimes affected by kinetics. Here, the hypothesis is tested that temperature can be reconstructed from shell Sr/Ca once microstructure and/or growth-rate-related bias has been mathematically eliminated. Therefore, the relationship between Sr/Ca and increment width, as well as biomineral unit size, has been studied in three different shell portions of field-grown Arctica islandica specimens. Subsequently, microstructure and/or growth-rate-related variation was removed from Sr/Ca data and residuals compared to temperature. As demonstrated, the hypothesis could not be verified. Even after detrending, Sr/Ca remained positively correlated to water temperature, which contradicts thermodynamic expectations and findings from inorganic aragonite. Any temperature signal potentially recorded by shell Sr/Ca is overprinted by other environmental forcings. Unless these variables are identified, it will remain impossible to infer temperature from Sr/Ca. Given the coupling with the biomineral unit size, a detailed characterization of the microstructure should remain an integral part of subsequent attempts to reconstruct temperature from Sr/Ca. Article in Journal/Newspaper Arctica islandica Gutenberg Open Science (Open-Science-Repository of the Johannes Gutenberg-University Mainz) |
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Open Polar |
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Gutenberg Open Science (Open-Science-Repository of the Johannes Gutenberg-University Mainz) |
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ftunivmainzpubl |
language |
English |
topic |
ddc:550 ddc:560 |
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ddc:550 ddc:560 Brosset, Cornélia Höche, Nils Shirai, Kotaro Mertz-Kraus, Regina Schöne, Bernd R. Strong coupling between biomineral morphology and Sr/Ca of Arctica islandica (Bivalvia) : implications for Shell Sr/Ca-based temperature estimates |
topic_facet |
ddc:550 ddc:560 |
description |
Bivalve shells serve as powerful high-resolution paleoclimate archives. However, the number of reliable temperature proxies is limited. It has remained particularly difficult to extract temperature signals from shell Sr/Ca, although Sr is routinely employed in other biogenic aragonites. In bivalves, Sr/Ca is linked to the prevailing microstructure and is sometimes affected by kinetics. Here, the hypothesis is tested that temperature can be reconstructed from shell Sr/Ca once microstructure and/or growth-rate-related bias has been mathematically eliminated. Therefore, the relationship between Sr/Ca and increment width, as well as biomineral unit size, has been studied in three different shell portions of field-grown Arctica islandica specimens. Subsequently, microstructure and/or growth-rate-related variation was removed from Sr/Ca data and residuals compared to temperature. As demonstrated, the hypothesis could not be verified. Even after detrending, Sr/Ca remained positively correlated to water temperature, which contradicts thermodynamic expectations and findings from inorganic aragonite. Any temperature signal potentially recorded by shell Sr/Ca is overprinted by other environmental forcings. Unless these variables are identified, it will remain impossible to infer temperature from Sr/Ca. Given the coupling with the biomineral unit size, a detailed characterization of the microstructure should remain an integral part of subsequent attempts to reconstruct temperature from Sr/Ca. |
format |
Article in Journal/Newspaper |
author |
Brosset, Cornélia Höche, Nils Shirai, Kotaro Mertz-Kraus, Regina Schöne, Bernd R. |
author_facet |
Brosset, Cornélia Höche, Nils Shirai, Kotaro Mertz-Kraus, Regina Schöne, Bernd R. |
author_sort |
Brosset, Cornélia |
title |
Strong coupling between biomineral morphology and Sr/Ca of Arctica islandica (Bivalvia) : implications for Shell Sr/Ca-based temperature estimates |
title_short |
Strong coupling between biomineral morphology and Sr/Ca of Arctica islandica (Bivalvia) : implications for Shell Sr/Ca-based temperature estimates |
title_full |
Strong coupling between biomineral morphology and Sr/Ca of Arctica islandica (Bivalvia) : implications for Shell Sr/Ca-based temperature estimates |
title_fullStr |
Strong coupling between biomineral morphology and Sr/Ca of Arctica islandica (Bivalvia) : implications for Shell Sr/Ca-based temperature estimates |
title_full_unstemmed |
Strong coupling between biomineral morphology and Sr/Ca of Arctica islandica (Bivalvia) : implications for Shell Sr/Ca-based temperature estimates |
title_sort |
strong coupling between biomineral morphology and sr/ca of arctica islandica (bivalvia) : implications for shell sr/ca-based temperature estimates |
publisher |
Johannes Gutenberg-Universität Mainz |
publishDate |
2022 |
url |
https://openscience.ub.uni-mainz.de/handle/20.500.12030/6904 https://hdl.handle.net/20.500.12030/6904 https://doi.org/10.25358/openscience-6893 |
genre |
Arctica islandica |
genre_facet |
Arctica islandica |
op_source |
Minerals. 12. 5. 2022. -. -. 500 |
op_relation |
http://doi.org/10.25358/openscience-6893 https://openscience.ub.uni-mainz.de/handle/20.500.12030/6904 2075-163X |
op_rights |
CC BY https://creativecommons.org/licenses/by/4.0/ openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/20.500.12030/6904 https://doi.org/10.25358/openscience-6893 |
_version_ |
1766353150281777152 |