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dc.provenanceCONICET-
dc.creatorEagle, R. A.-
dc.creatorEler, J. M.-
dc.creatorTripati, A. K.-
dc.creatorRes, J. B.-
dc.creatorFreitas, P. S.-
dc.creatorHeibental, C .-
dc.creatorWanamaker, A. D., Jr.-
dc.creatorTaviani, M.-
dc.creatorElliot, M.-
dc.creatorMarenssi, Sergio Alfredo-
dc.creatorNakamura, K.-
dc.creatorRamirez, P.-
dc.creatorRoy, K .-
dc.date2017-01-09T21:57:18Z-
dc.date2017-01-09T21:57:18Z-
dc.date2013-05-
dc.date2016-11-24T18:38:16Z-
dc.date.accessioned2019-04-29T15:45:05Z-
dc.date.available2019-04-29T15:45:05Z-
dc.date.issued2013-05-
dc.identifierEagle, R. A.; Eler, J. M.; Tripati, A. K.; Res, J. B.; Freitas, P. S.; et al.; The influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks; Copernicus Publications; Biogeosciences; 10; 5-2013; 4591-4606-
dc.identifier1726-4170-
dc.identifierhttp://hdl.handle.net/11336/11018-
dc.identifier1726-4189-
dc.identifier.urihttp://rodna.bn.gov.ar:8080/jspui/handle/bnmm/301084-
dc.descriptionThe shells of marine mollusks are widely used archives of past climate and ocean chemistry. Whilst the measurement of mollusk δ 18O to develop records of past climate change is a commonly used approach, it has proven challenging to develop reliable independent paleothermometers that can be used to deconvolve the contributions of temperature and fluid composition on molluscan oxygen isotope compositions. Here we investigate the temperature dependence of 13C–18O bond abundance, denoted by the measured parameter 147, in shell carbonates of bivalve mollusks and assess its potential to be a useful paleothermometer. We report measurements on cultured specimens spanning a range in water temperatures of 5 to 25 ◦C, and field collected specimens spanning a range of −1 to 29 ◦C. In addition we investigate the potential influence of carbonate saturation state on bivalve stable isotope compositions by making measurements on both calcitic and aragonitic specimens that have been cultured in seawater that is either supersaturated or undersaturated with respect to aragonite. We find a robust relationship between 147 and growth temperature. We also find that the slope of a linear regression through all the 147 data for bivalves plotted against seawater temperature is significantly shallower than previously published inorganic and biogenic carbonate calibration studies produced in our laboratory and go on to discuss the possible sources of this difference. We find that changing seawater saturation state does not have significant effect on the 147 of bivalve shell carbonate in two taxa that we examined, and we do not observe significant differences between 147-temperature relationships between calcitic and aragonitic taxa.-
dc.descriptionFil: Eagle, R. A.. University of California; Estados Unidos. California Institute of Technology; Estados Unidos-
dc.descriptionFil: Eler, J. M.. California Institute of Technology; Estados Unidos-
dc.descriptionFil: Tripati, A. K.. University of California; Estados Unidos-
dc.descriptionFil: Res, J. B.. University Of North Carolina; Estados Unidos-
dc.descriptionFil: Freitas, P. S.. Laboratorio Nacional de Energia e Geologia; Portugal-
dc.descriptionFil: Heibental, C .. Geomar-helmholtz Centre For Ocean Research Kiel; Alemania-
dc.descriptionFil: Wanamaker, A. D., Jr.. University of Iowa; Estados Unidos-
dc.descriptionFil: Taviani, M.. Consiglio Nazionale Delle Ricerche. Istituto di Scienze Marine; Italia. Woods Hole Oceanographic Institution; Estados Unidos-
dc.descriptionFil: Elliot, M.. Universite de Nantes; Francia-
dc.descriptionFil: Marenssi, Sergio Alfredo. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina-
dc.descriptionFil: Nakamura, K.. California State University; Estados Unidos-
dc.descriptionFil: Ramirez, P.. California State University; Estados Unidos-
dc.descriptionFil: Roy, K .. University of California; Estados Unidos-
dc.formatapplication/pdf-
dc.formatapplication/pdf-
dc.languageeng-
dc.publisherCopernicus Publications-
dc.relationinfo:eu-repo/semantics/altIdentifier/url/http://www.biogeosciences.net/10/4591/2013/-
dc.rightsinfo:eu-repo/semantics/openAccess-
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/-
dc.sourcereponame:CONICET Digital (CONICET)-
dc.sourceinstname:Consejo Nacional de Investigaciones Científicas y Técnicas-
dc.sourceinstacron:CONICET-
dc.source.urihttp://hdl.handle.net/11336/11018-
dc.subjectSTABLE ISOTOPES-
dc.subjectPALEOTEMPERATURES-
dc.subjectSHELLS-
dc.subjectGeoquímica y Geofísica-
dc.subjectCiencias de la Tierra y relacionadas con el Medio Ambiente-
dc.subjectCIENCIAS NATURALES Y EXACTAS-
dc.titleThe influence of temperature and seawater carbonate saturation state on 13C-18O bond ordering in bivalve mollusks-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/publishedVersion-
dc.typeinfo:ar-repo/semantics/articulo-
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