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dc.contributor.authorRooker, Jay R.es_ES
dc.contributor.authorWells, R.J. Davides_ES
dc.contributor.authorAddis, P.es_ES
dc.contributor.authorArrizabalaga, H.es_ES
dc.contributor.authorBaptista, Migueles_ES
dc.contributor.authorBearzi, Giovannies_ES
dc.contributor.authorDance, Michael A.es_ES
dc.contributor.authorFraile, Igaratzaes_ES
dc.contributor.authorLacoue-Labarthe, Thomases_ES
dc.contributor.authorLee, Jessica M.es_ES
dc.contributor.authorMegalofonou, P.es_ES
dc.contributor.authorRosa, Ruies_ES
dc.contributor.authorSobrino, Ignacioes_ES
dc.contributor.authorSykes, António V.es_ES
dc.contributor.authorUrgeles, Rogeres_ES
dc.date.accessioned2020-07-30T08:43:02Z-
dc.date.available2020-07-30T08:43:02Z-
dc.date.issued2020-07-
dc.identifier.citationJournal of the Royal Society Interface 17(168): 20200309 (2020)es_ES
dc.identifier.otherCEX2019-000928-S-
dc.identifier.urihttp://hdl.handle.net/10261/217216-
dc.description9 pages, 6 figures, 1 table.-- Data are available as part of the electronic supplementary material https://doi.org/10.6084/m9.figshare.c.5073446es_ES
dc.description.abstractNatural markers (δ13C and δ18O stable isotopes) in the cuttlebones of the European common cuttlefish (Sepia officinalis) were determined for individuals collected across a substantial portion of their range in the Northeast Atlantic Ocean (NEAO) and Mediterranean Sea. Cuttlebone δ13C and δ18O were quantified for core and edge material to characterize geochemical signatures associated with early (juvenile) and recent (sub-adult/adult) life-history periods, respectively. Regional shifts in cuttlebone δ13C and δ18O values were detected across the 12 sites investigated. Individuals collected from sites in the NEAO displayed more enriched δ13C and δ18O values relative to sites in the Mediterranean Sea, with the latter also showing salient differences in both markers among western, central and eastern collection areas. Classification success based on cuttlebone δ13C and δ18O values to four geographical regions (NEAO, western, central and eastern Mediterranean Sea) was relatively high, suggesting that environmental conditions in each region were distinct and produced area-specific geochemical signatures on the cuttlebones of S. officinalis. A modified δ13C and δ18O baseline was developed from sites proximal to the Strait of Gibraltar in both the NEAO and Mediterranean Sea to assess potential mixing through this corridor. Nearly, all (95%) of δ13C and δ18O signatures of S. officinalis collected in the area of the NEAO closest to the Strait of Gibraltar (Gulf of Cadiz) matched the signatures of specimens collected in the western Mediterranean, signifying potential movement and mixing of individuals through this passageway. This study extends the current application of these geochemical markers for assessing the natal origin and population connectivity of this species and potentially other taxa that inhabit this geographical areaes_ES
dc.description.sponsorshipThis work was supported by the McDaniel Charitable Foundation (J.R.R.), Texas A&M University (J.R.R., R.J.D.W.), Spanish Ministry of Science, Innovation and Universities, OCTOSET Project RTI2018-097908-B-I00, MCIU/AEI/FEDER, EU (R.V.), and Portuguese Foundation for Science and Technology MARE UID/MAR/04292/2013 (R.R.). A.S. was supported through Fundação para a Ciência e a Tecnologia (IF/00576/2014 contract and Plurennial funding to CCMARUID/Multi/04326/2013)es_ES
dc.description.sponsorshipWith the funding support of the ‘Severo Ochoa Centre of Excellence’ accreditation (CEX2019-000928-S), of the Spanish Research Agency (AEI)-
dc.language.isoenges_ES
dc.publisherRoyal Society (Great Britain)es_ES
dc.relationMICIU/ICTI2017-2020/RTI2018-097908-B-I00es_ES
dc.relation.isversionofPublisher's versiones_ES
dc.rightsopenAccesses_ES
dc.subjectCephalopod-
dc.subjectMigration-
dc.subjectCuttlefish-
dc.subjectGeochemistry-
dc.subjectPopulation structure-
dc.titleNatural geochemical markers reveal environmental history and population connectivity of common cuttlefish in the Atlantic Ocean and Mediterranean Seaes_ES
dc.typeartículoes_ES
dc.identifier.doihttp://dx.doi.org/10.1098/rsif.2020.0309-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttps://doi.org/10.1098/rsif.2020.0309es_ES
dc.identifier.e-issn1742-5662-
dc.rights.licensehttps://creativecommons.org/licenses/by/4.0/es_ES
dc.contributor.funderMcDaniel Charitable Foundationes_ES
dc.contributor.funderTexas A&M Universityes_ES
dc.contributor.funderMinisterio de Ciencia, Innovación y Universidades (España)es_ES
dc.contributor.funderFundação para a Ciência e a Tecnologia (Portugal)es_ES
dc.contributor.funderAgencia Estatal de Investigación (España)-
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.identifier.funderhttp://dx.doi.org/10.13039/100007904es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100001871es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100011033es_ES
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