Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/71241
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dc.contributor.authorClauzel, Thibaulten_US
dc.contributor.authorMaréchal, Chloéen_US
dc.contributor.authorFourel, Françoisen_US
dc.contributor.authorBarral, Abelen_US
dc.contributor.authorAmiot, Romainen_US
dc.contributor.authorBetancort, Juan Franciscoen_US
dc.contributor.authorLomoschitz, Alejandroen_US
dc.contributor.authorMeco, Joaquínen_US
dc.contributor.authorLécuyer, Christopheen_US
dc.date.accessioned2020-04-04T05:06:40Z-
dc.date.available2020-04-04T05:06:40Z-
dc.date.issued2020en_US
dc.identifier.issn1096-0287en_US
dc.identifier.otherScopus-
dc.identifier.urihttp://hdl.handle.net/10553/71241-
dc.description.abstractThe study of paleoclimates enables us to improve and better constrain climate models in order to forecast future climate variations. Marine Isotope Stage 11 (MIS11), which began around 425,000 yr BP and lasted about 65,000 yr, is a warm isotope stage of paramount importance, because the astronomical configuration was similar to the one characterizing the Holocene. Therefore, this warm isotope stage is the most appropriate analog to present-day climate known to date. This study aims to provide new data on sea-surface temperatures (SSTs) inferred from the carbon and oxygen isotope compositions of skeletal carbonates of marine invertebrates preserved in two marine deposits of the Canary Islands located at Piedra Alta, Lanzarote, and Arucas, Gran Canaria. According to published isotopic fractionation equations the marine deposit from Arucas recorded SSTs of 15.9 ± 2.2°C on average, while the tsunamite from Piedra Alta recorded SSTs of 21.2 ± 1.9°C on average. Absolute dating, mollusc assemblages, and calculated marine temperatures suggest that the Arucas marine deposit corresponds to the beginning of MIS11, while the Piedra Alta tsunamite was formed during MIS11c. These results show that low latitudes also experienced sizable SST changes during interglacial stages.en_US
dc.languageengen_US
dc.relation.ispartofQuaternary Researchen_US
dc.sourceQuaternary Research [ISSN 1096-0287], v. 94, p. 195-209en_US
dc.subject2506 Geologíaen_US
dc.subject2416 Paleontologíaen_US
dc.subject.otherCanary Archipelagoen_US
dc.subject.otherClimate Changeen_US
dc.subject.otherMis11en_US
dc.subject.otherMolluscen_US
dc.subject.otherSea-Surface Temperatureen_US
dc.subject.otherStable Isotopeen_US
dc.subject.otherTsunamien_US
dc.titleReconstruction of sea-surface temperatures in the Canary Islands during Marine Isotope Stage 11en_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1017/qua.2019.65en_US
dc.identifier.scopus85082416478-
dc.contributor.authorscopusid57211668486-
dc.contributor.authorscopusid6701582006-
dc.contributor.authorscopusid35733761600-
dc.contributor.authorscopusid55935360500-
dc.contributor.authorscopusid8346978200-
dc.contributor.authorscopusid6602503518-
dc.contributor.authorscopusid6507150380-
dc.contributor.authorscopusid6602093969-
dc.contributor.authorscopusid35240298200-
dc.description.lastpage209-
dc.description.firstpage195-
dc.relation.volume94-
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.utils.revisionen_US
dc.identifier.ulpgces
dc.description.sjr0,872
dc.description.jcr2,72
dc.description.sjrqQ1
dc.description.jcrqQ3
dc.description.scieSCIE
dc.description.erihplusERIH PLUS
item.fulltextSin texto completo-
item.grantfulltextnone-
crisitem.author.deptGIR IOCAG:Geología Aplicada y Regional-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Ingeniería Civil-
crisitem.author.orcid0000-0002-8812-0351-
crisitem.author.orcid0000-0001-7658-9956-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameLomoschitz Mora-Figueroa, Alejandro-
crisitem.author.fullNameMeco Cabrera, Joaquín Francisco-
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