Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/25064
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dc.contributor.authorCusack, Maggieen_UK
dc.contributor.authorParkinson, Daviden_UK
dc.contributor.authorPérez-Huerta, Albertoen_UK
dc.contributor.authorEngland, Jenniferen_UK
dc.contributor.authorCurry, Gordon Ben_UK
dc.contributor.authorFallick, Anthony Een_UK
dc.date.accessioned2017-03-03T22:52:09Z-
dc.date.available2017-03-03T22:52:09Zen_UK
dc.date.issued2007-09en_UK
dc.identifier.urihttp://hdl.handle.net/1893/25064-
dc.description.abstractWith their extensive fossil record and shells of stable low-Mg calcite, rhynchonelliform brachiopods are attractive sources of climate information via seawater temperature proxies such as stable oxygen isotope composition. In Terebratalia transversa (Sowerby) there is a progression towards oxygen isotope equilibrium in the calcite of the innermost secondary layer. This study confirms the lack of any vital effects influencing oxygen isotope composition of T. transversa, even in specialised areas of the innermost secondary layer. Calcite Mg/Ca ratio is another potential seawater temperature proxy, that has the advantage of not being influenced by salinity. Mg concentrations measured by electron microprobe analyses indicate that there is no concomitant decrease in Mg concentration towards the inner secondary layer, associated with the progressive shift towards oxygen isotope equilibrium. Mg distribution is heterogeneous throughout the shell and correlates with that of sulphur, which may be a proxy for organic components, suggesting that some of the Mg may not be in the calcite lattice. It is essential therefore, to determine the chemical environment of the magnesium ions to avoid any erroneous temperature extrapolations in brachiopods or any other calcite biomineral. en_UK
dc.language.isoenen_UK
dc.publisherCambridge University Press for Royal Society of Edinburghen_UK
dc.relationCusack M, Parkinson D, Pérez-Huerta A, England J, Curry GB & Fallick AE (2007) Relationship between δ18O and minor element composition of Terebratalia transversa. Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 98 (3-4), pp. 443-449. https://doi.org/10.1017/S1755691008075671en_UK
dc.rightsThe publisher does not allow this work to be made publicly available in this Repository. Please use the Request a Copy feature at the foot of the Repository record to request a copy directly from the author. You can only request a copy if you wish to use this work for your own research or private study.en_UK
dc.subjectBrachiopodsen_UK
dc.subjectcalciteen_UK
dc.subjectmagnesiumen_UK
dc.subjectoxygen isotopesen_UK
dc.subjectsulphuren_UK
dc.subjectvital effecten_UK
dc.titleRelationship between δ18O and minor element composition of Terebratalia transversaen_UK
dc.typeJournal Articleen_UK
dc.rights.embargodate2999-12-02en_UK
dc.rights.embargoreason[Cusack-etal-EESTRSE-2008.pdf] The publisher does not allow this work to be made publicly available in this Repository therefore there is an embargo on the full text of the work.en_UK
dc.identifier.doi10.1017/S1755691008075671en_UK
dc.citation.jtitleEarth and Environmental Science Transactions of the Royal Society of Edinburghen_UK
dc.citation.issn1755-6929en_UK
dc.citation.issn1755-6910en_UK
dc.citation.volume98en_UK
dc.citation.issue3-4en_UK
dc.citation.spage443en_UK
dc.citation.epage449en_UK
dc.citation.publicationstatusPublisheden_UK
dc.citation.peerreviewedRefereeden_UK
dc.type.statusVoR - Version of Recorden_UK
dc.author.emailmaggie.cusack@stir.ac.uken_UK
dc.citation.date01/09/2007en_UK
dc.contributor.affiliationBiological and Environmental Sciencesen_UK
dc.contributor.affiliationUniversity of Glasgowen_UK
dc.contributor.affiliationUniversity of Glasgowen_UK
dc.contributor.affiliationUniversity of Glasgowen_UK
dc.contributor.affiliationUniversity of Glasgowen_UK
dc.contributor.affiliationScottish Universities Environmental Research Centreen_UK
dc.identifier.isiWOS:000259046200023en_UK
dc.identifier.scopusid2-s2.0-54749095906en_UK
dc.identifier.wtid540885en_UK
dc.contributor.orcid0000-0003-0145-1180en_UK
dc.date.accepted2007-07-24en_UK
dc.date.filedepositdate2017-03-03en_UK
Appears in Collections:Biological and Environmental Sciences Journal Articles

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