Integrating high-resolution Sr/Ca and ultrastructural analyses of the Tridacna squamosa shell to reconstruct sub-daily seawater temperature variation

dc.contributor.authorBrosset, Cornélia
dc.contributor.authorLiu, Chengcheng
dc.contributor.authorYang, Haotian
dc.contributor.authorYan, Hong
dc.contributor.authorSchöne, Bernd R.
dc.date.accessioned2025-07-24T15:10:56Z
dc.date.available2025-07-24T15:10:56Z
dc.date.issued2024
dc.description.abstractModern and fossil bivalves record environmental variability in their shells in the form of chemical and ultrastructural properties as well as changes in growth rate. These proxy data can be placed in precise temporal context based on growth pattern analysis. Some species such as tridacnids grow particularly fast providing unique insights into environmental changes on the time scale of weather which opens new opportunities for paleoclimate research. Here, we assessed the potential use of the fluted giant clam (Tridacna squamosa) to reconstruct sub-daily sea surface temperature (SST) fluctuations from shell Sr/Ca ratios. Through a combined μm-scale analysis of shell Sr/Ca (NanoSIMS) and ultrastructure (SEM) it was possible to study shell material produced during daytime (growth increments) and nighttime (growth lines) separately. Unlike coarser resolution chemical analysis (LA-ICP-MS and ICP-OES), this approach revealed a significant positive correlation between SST and Sr/Ca during daytime (R2 = 0.36, p < 0.001). The correlation further increased when the NanoSIMS data of several consecutive daily increments were combined to match the sampling resolution of LA-ICP-MS and ICP-OES data, i.e., four days to two weeks (R2 of up to 0.86, p < 0.001). With an uncertainty of at least ± 1.5 °C, the applicability of the Sr/Ca thermometer remains limited considering that T. squamosa only occurs in ecosystems with minimal seasonal temperature amplitudes. Consistent daily Sr/Ca cycles were observed with local maxima at growth lines. This cyclic pattern was found even when the ultrastructure morphology varied or when the complex crossed-lamellar ultrastructure of the shell deviated from its typical configuration during extreme weather events. Therefore, Sr/Ca is likely not directly linked to the shell ultrastructure, but instead both properties are driven by underlying physiological factors.en
dc.identifier.doihttps://doi.org/10.25358/openscience-12820
dc.identifier.urihttps://openscience.ub.uni-mainz.de/handle/20.500.12030/12841
dc.language.isoeng
dc.rightsCC-BY-4.0
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subject.ddc550 Geowissenschaftende
dc.subject.ddc550 Earth sciencesen
dc.titleIntegrating high-resolution Sr/Ca and ultrastructural analyses of the Tridacna squamosa shell to reconstruct sub-daily seawater temperature variationen
dc.typeZeitschriftenaufsatz
jgu.apc.netprice2255,71
jgu.apc.price2413,62
jgu.apc.taxrate7
jgu.apc.transformationcontractElsevier
jgu.dfg.year2024
jgu.journal.titlePalaeogeography, palaeoclimatology, palaeoecology
jgu.journal.volume659
jgu.nationalcurrency.eur2255,71
jgu.organisation.departmentFB 09 Chemie, Pharmazie u. Geowissensch.
jgu.organisation.nameJohannes Gutenberg-Universität Mainz
jgu.organisation.number7950
jgu.organisation.placeMainz
jgu.organisation.rorhttps://ror.org/023b0x485
jgu.pages.alternative112663
jgu.publisher.doi10.1016/j.palaeo.2024.112663
jgu.publisher.eissn1872-616X
jgu.publisher.nameElsevier Science
jgu.publisher.placeAmsterdam [u.a.]
jgu.publisher.year2024
jgu.rights.accessrightsopenAccess
jgu.subject.ddccode550
jgu.subject.dfgNaturwissenschaften
jgu.type.dinitypeArticleen_GB
jgu.type.resourceText
jgu.type.versionPublished version

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