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Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/17950
DC FieldValueLanguage
dc.contributor.authorMeco, J.en_US
dc.contributor.authorKoppers, Anthony A. P.en_US
dc.contributor.authorMiggins, Daniel P.en_US
dc.contributor.authorLomoschitz, Alejandroen_US
dc.contributor.authorBetancort-Lozano, Juan Franciscoen_US
dc.date.accessioned2016-07-21T02:30:30Z-
dc.date.accessioned2018-06-18T06:45:05Z-
dc.date.available2016-07-21T02:30:30Z-
dc.date.available2018-06-18T06:45:05Z-
dc.date.issued2015en_US
dc.identifier.issn0031-0182en_US
dc.identifier.urihttp://hdl.handle.net/10553/17950-
dc.description.abstractTwo new 40Ar/39Ar ages (*) and previously published K/Ar ages of basaltic pillow lava flows are coeval with closely-related fossiliferous marine layers, allowing us to establish the beginning (5.8; 5.0; 4.8Ma at Ajuí, Fuerteventura Island and 4.8±0.03Ma (2?)* at Tamaraceite) and a middle stage (4.20±0.18Ma (2?)* at La Esfinge in Gran Canaria Island) of Early Pliocene marine deposits in the Canary Islands. Here the presence of tropicopolitan fossils (Megaselachus megalodon, Janthina typica) suggests the influence of a possible Central American Circumtropical Current during the Pliocene and in the North Atlantic basin.en_US
dc.formatapplication/pdf-
dc.languageengen_US
dc.relation.ispartofPalaeogeography, Palaeoclimatology, Palaeoecologyen_US
dc.relation.isreplacedbyhdl:10553/54765-
dc.sourcePalaeogeography, Palaeoclimatology, Palaeoecology [ISSN 0031-0182], v. 435, p. 53-69en_US
dc.subject24 Ciencias de la vidaen_US
dc.subject2416 Paleontologíaen_US
dc.subject.otherCanary current originen_US
dc.subject.otherEarly Pliocene biogeographyen_US
dc.subject.otherPliocene climatic evolutionen_US
dc.subject.otherPliocene Canarian fossilsen_US
dc.subject.otherFossil Argonauta argoen_US
dc.titleThe Canary record of the evolution of the North Atlantic Pliocene: New Ar-40/Ar-39 ages and some notable palaeontological evidenceen_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.palaeo.2015.05.027en_US
dc.identifier.scopus84935031382-
dc.contributor.authorscopusid6602093969-
dc.contributor.authorscopusid6602493927-
dc.contributor.authorscopusid26039326000-
dc.contributor.authorscopusid6507150380-
dc.contributor.authorscopusid6602503518-
dc.description.lastpage69en_US
dc.description.firstpage53en_US
dc.relation.volume435en_US
dc.investigacionCienciasen_US
dc.rights.accessrightsinfo:eu-repo/semantics/openAccess-
dc.type2Artículoen_US
dc.utils.revisionSíen_US
dc.date.coverdateOctubre 2015en_US
dc.identifier.ulpgcSíen_US
dc.utils.zenodofilehttps://zenodo.org/record/4314766/files/Supplementary_G.C.La Esfinge.pdf?download=1;Supplementary_G.C.La Esfinge.pdf;120K;PDF
dc.utils.zenodofilehttps://zenodo.org/record/4314766/files/Supplementary_G.C.La Esfinge.pdf?download=1;Supplementary_G.C.La Esfinge.pdf;120K;PDF
dc.utils.zenodofilehttps://zenodo.org/record/4314766/files/Supplementary_G.C.La Esfinge.pdf?download=1;Supplementary_G.C.La Esfinge.pdf;120K;PDF
dc.utils.zenodofilehttps://zenodo.org/record/4314766/files/Supplementary_G.C.Tamaraceite.pdf?download=1;Supplementary_G.C.Tamaraceite.pdf;115K;PDF
dc.utils.zenodofilehttps://zenodo.org/record/4314766/files/Supplementary_G.C.La Esfinge.pdf?download=1;Supplementary_G.C.La Esfinge.pdf;120K;PDF
dc.utils.zenodofilehttps://zenodo.org/record/4314766/files/Supplementary_G.C.Tamaraceite.pdf?download=1;Supplementary_G.C.Tamaraceite.pdf;115K;PDF
dc.description.sjr1,476
dc.description.jcr2,525
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
item.fulltextCon texto completo-
item.grantfulltextopen-
crisitem.author.deptGIR IOCAG: Geología Aplicada y Regional-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Ingeniería Civil-
crisitem.author.orcid0000-0001-7658-9956-
crisitem.author.orcid0000-0002-8812-0351-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameMeco Cabrera, Joaquín Francisco-
crisitem.author.fullNameLomoschitz Mora-Figueroa, Alejandro-
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