Please use this identifier to cite or link to this item: http://doi.org/10.25358/openscience-9648
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dc.contributor.authorBrosset, Cornélia-
dc.contributor.authorHöche, Nils-
dc.contributor.authorWitbaard, Rob-
dc.contributor.authorNishida, Kozue-
dc.contributor.authorShirai, Kotaro-
dc.contributor.authorMertz-Kraus, Regina-
dc.contributor.authorSchöne, Bernd R.-
dc.date.accessioned2023-11-07T14:49:21Z-
dc.date.available2023-11-07T14:49:21Z-
dc.date.issued2023-
dc.identifier.urihttps://openscience.ub.uni-mainz.de/handle/20.500.12030/9666-
dc.description.abstractSeawater temperature is an essential quantity for paleoclimatological and paleoecological studies. A potential archive that can provide century-long, temporally well-constrained and high-resolution temperature proxy data is available in the form of bivalve shells. However, the number of well-accepted and robust temperature proxies contained in shells is limited to stable oxygen isotopes and carbonate clumped isotopes. Many studies have therefore investigated the possibility to reconstruct temperature from element/Ca properties, specifically Sr/Ca ratios in case of aragonitic shells. As demonstrated here, in agreement with thermodynamic expectations and the lattice strain model, shell Sr/Ca of laboratory-grown Arctica islandica specimens is strongly positively coupled to water temperature. If ultrastructure-related bias is mathematically eliminated, up to 75% of the variability in shell Sr/Ca data can be explained by water temperature. However, in field-grown specimens, this relationship is superimposed by other environmental variables that can hardly be quantified and mathematically eliminated. The explained variability of Sr/Ca is reduced to merely 26% and the prediction uncertainty too large for reliable temperature estimates. Most likely, the equable, less biased conditions in the laboratory resulted in the production of a more uniform shell ultrastructure (with larger and more elongated biomineral units) which in turn was associated with less variable Sr/Ca values and a stronger link to water temperature. Without a detailed understanding and quantification of the factors controlling ultrastructural variations in field-grown bivalves, it remains impossible to employ shell Sr/Ca of wild A. islandica specimens for precise temperature estimates, merely a qualitative temperature reconstruction seems feasible.en_GB
dc.language.isoengde
dc.rightsCC BY*
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/*
dc.subject.ddc540 Chemiede_DE
dc.subject.ddc540 Chemistry and allied sciencesen_GB
dc.subject.ddc550 Geowissenschaftende_DE
dc.subject.ddc550 Earth sciencesen_GB
dc.subject.ddc560 Paläontologiede_DE
dc.subject.ddc560 Paleontologyen_GB
dc.subject.ddc570 Biowissenschaftende_DE
dc.subject.ddc570 Life sciencesen_GB
dc.subject.ddc590 Tiere (Zoologie)de_DE
dc.subject.ddc590 Zoological sciencesen_GB
dc.titleSr/Ca in shells of laboratory-grown bivalves (Arctica islandica) serves as a proxy for water temperature : implications for (paleo)environmental research?en_GB
dc.typeZeitschriftenaufsatzde
dc.identifier.doihttp://doi.org/10.25358/openscience-9648-
jgu.type.contenttypeScientific articlede
jgu.type.dinitypearticleen_GB
jgu.type.versionPublished versionde
jgu.type.resourceTextde
jgu.organisation.departmentFB 09 Chemie, Pharmazie u. Geowissensch.de
jgu.organisation.number7950-
jgu.organisation.nameJohannes Gutenberg-Universität Mainz-
jgu.rights.accessrightsopenAccess-
jgu.journal.titleFrontiers in Marine Sciencede
jgu.journal.volume10de
jgu.pages.alternative1279164de
jgu.publisher.year2023-
jgu.publisher.nameFrontiers Mediade
jgu.publisher.placeLausannede
jgu.publisher.issn2296-7745de
jgu.organisation.placeMainz-
jgu.subject.ddccode540de
jgu.subject.ddccode550de
jgu.subject.ddccode560de
jgu.subject.ddccode570de
jgu.subject.ddccode590de
jgu.publisher.doi10.3389/fmars.2023.1279164de
jgu.organisation.rorhttps://ror.org/023b0x485-
jgu.subject.dfgLebenswissenschaftende
Appears in collections:DFG-491381577-G

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