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The Aragonian and Vallesian high-resolution micromammal succession in the Calatayud-Montalbán Basin (Aragón, Spain)

dc.contributor.authorGarcía Paredes, Israeles-ES
dc.contributor.authorÁlvarez Sierra, María de los Ángeleses-ES
dc.contributor.authorvan den Hoek-Ostende, Lars W.es-ES
dc.contributor.authorHernández Ballarín, Verónicaes-ES
dc.contributor.authorHordijk, Keeses-ES
dc.contributor.authorLópez Guerrero, Palomaes-ES
dc.contributor.authorOliver, Adrianaes-ES
dc.contributor.authorPeláez-Campomanes de Labra, Pabloes-ES
dc.date.accessioned2020-09-02T01:38:50Z
dc.date.available2020-09-02T01:38:50Z
dc.date.issued06/10/2016es_ES
dc.identifier.issn1631-0683es_ES
dc.identifier.uri10.1016/j.crpv.2015.09.014es_ES
dc.descriptionArtículos en revistases_ES
dc.description.abstractWe present an updated taxonomy and faunal distribution of the micromammal fossil record from the Aragonian and Lower Vallesian of the Calatayud-Montalbán Basin. The analysed record includes the orders Rodentia, Eulipotyphla, and Lagomorpha. The pattern of species turnover shows seven major faunal events, which are correlated with major climate changes based on marine stable oxygen and carbon isotope records. Episodes δ18O Mi-2 and Mi-3 are significantly correlated with major micromammal turnover at the boundaries between the Lower and Middle Aragonian and the Middle and Upper Aragonian, respectively. Our results support the existence of a selective turnover during the Aragonian and Lower Vallesian.es-ES
dc.description.abstractWe present an updated taxonomy and faunal distribution of the micromammal fossil record from the Aragonian and Lower Vallesian of the Calatayud-Montalbán Basin. The analysed record includes the orders Rodentia, Eulipotyphla, and Lagomorpha. The pattern of species turnover shows seven major faunal events, which are correlated with major climate changes based on marine stable oxygen and carbon isotope records. Episodes δ18O Mi-2 and Mi-3 are significantly correlated with major micromammal turnover at the boundaries between the Lower and Middle Aragonian and the Middle and Upper Aragonian, respectively. Our results support the existence of a selective turnover during the Aragonian and Lower Vallesian.en-GB
dc.format.mimetypeapplication/pdfes_ES
dc.language.isoen-GBes_ES
dc.rightses_ES
dc.rights.uries_ES
dc.sourceRevista: Comptes Rendus Palevol, Periodo: 2, Volumen: 15, Número: 7, Página inicial: 781, Página final: 789es_ES
dc.titleThe Aragonian and Vallesian high-resolution micromammal succession in the Calatayud-Montalbán Basin (Aragón, Spain)es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.description.versioninfo:eu-repo/semantics/publishedVersiones_ES
dc.rights.holderSujeto a Copyrightes_ES
dc.rights.accessRightsinfo:eu-repo/semantics/restrictedAccesses_ES
dc.keywordsNeogene; Miocene; Faunal turnover; Global climatic events; Biodiversityes-ES
dc.keywordsNeogene; Miocene; Faunal turnover; Global climatic events; Biodiversityen-GB


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