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dc.contributor.authorGonzalvo Ballobar, C.
dc.date.accessioned2015-04-10T09:46:13Z
dc.date.available2015-04-10T09:46:13Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10308
dc.description.abstractThe study of planktic foraminifera assemblages across the Early/Middle Eocene in the Anoz and Agost sections allows to recognize the following biozones and subzones: Acarinma pentacamerata Biozone, Subbotina boweri Subzone and Truncorotaloides praetopilensis Subzone, in the Early Eocene, and Hantkenina nuttalli Biozone, Hantkenina nuttalli Subzone and Clobigerapsis subconglobata Subzone in the Middle Eocene. The quantitative study shows one warning trend across the Early/Middle Eocene boundaryen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherPlanktic foraminiferaen_US
dc.subject.otherBiostratigraphyen_US
dc.subject.otherPaleoecologyen_US
dc.subject.otherEoceneen_US
dc.subject.otherYpresianen_US
dc.subject.otherLutetianen_US
dc.titleEvolución de las asociaciones de foraminíferos planctónicos del tránsito Eoceno inferior-Eoceno medio en la Península Ibérica (Agost, Cordillera Bética y Anoz, Pirineos)en_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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