Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6961
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dc.contributor.authorallLancis, C.; Universidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Aptdo. 99. 03080 San Vicente del Raspeig, Alicanteen
dc.contributor.authorallTent-Manclús, J. E.; Universidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Aptdo. 99. 03080 San Vicente del Raspeig, Alicanteen
dc.contributor.authorallSoria, J. M.; Universidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Aptdo. 99. 03080 San Vicente del Raspeig, Alicanteen
dc.contributor.authorallCorbí, H.; Universidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Aptdo. 99. 03080 San Vicente del Raspeig, Alicanteen
dc.contributor.authorallDinarès-Turell, J.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallYébenes, A.; Universidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Aptdo. 99. 03080 San Vicente del Raspeig, Alicanteen
dc.date.accessioned2011-03-14T14:53:03Zen
dc.date.available2011-03-14T14:53:03Zen
dc.date.issued2010en
dc.identifier.urihttp://hdl.handle.net/2122/6961en
dc.description.abstractThe Serravallian-Tortonian boundary was a time of strong tectonic activity in the Betic Cordillera. The Early Tortonian sediments continue to be under debate because no clear fossil attributions are available. These sediments have been assigned an Early Tortonian age by indirect stratigraphic criteria or by the absence of fossil content older or younger in age. The present work documents the Les Moreres- Albatera composite section, probably the most complete section of the Tortonian age in the Betic Cordillera, despite a major time gap of about 1 Ma due to an intra-Tortonian tectonic event. The section has two limestone units at the bottom (El Castellà) and the top (Las Ventanas) and two intermediate marly units, the lower Les Moreres and the upper Galería de los Suizos divided by the Raya del Búho Conglomerate. The calcareous nannoplankton biozones from CN5b/NN7 to CN9a/NN11a (Okada & Bukry, 1980; Martini, 1971) have been identified, as have the planktonic foraminifera biozones from MMi9 to MMi12a (Lourens et al. 2004). The calcareous nannoplankton biostratigraphy has allowed the identification of a time gap that includes the upper part of the CN7/NN9 biozones to the lower part of the CN9a/NN11a (Okada &Bukry, 1980; Martini, 1971). The integrated palaeomagnetic and biostratigraphic study of Albatera section has allowed to calibrate the C4r.1r/C4n.2n chron boundary.en
dc.language.isoSpanishen
dc.publisher.nameInstituto Geológico y Minero de Españaen
dc.relation.ispartofRevista Española de Micropaleontologíaen
dc.relation.ispartofseries3 / 42 (2010)en
dc.subjectBetic Cordilleraen
dc.subjectMioceneen
dc.subjectTortonianen
dc.subjectCalcareous nannoplanktonen
dc.subjectPlanktonic foraminiferaen
dc.subjectBiostratigraphyen
dc.titleNannoplankton and planktonic foraminifera biostratigraphy of the eastern Betics during the Tortonian (SE Spain)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber321 - 344en
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.06. Paleoceanography and paleoclimatologyen
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transporten
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.10. Stratigraphyen
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dc.description.obiettivoSpecifico2.2. Laboratorio di paleomagnetismoen
dc.description.journalTypeN/A or not JCRen
dc.description.fulltextrestricteden
dc.contributor.authorLancis, C.en
dc.contributor.authorTent-Manclús, J. E.en
dc.contributor.authorSoria, J. M.en
dc.contributor.authorCorbí, H.en
dc.contributor.authorDinarès-Turell, J.en
dc.contributor.authorYébenes, A.en
dc.contributor.departmentUniversidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Aptdo. 99. 03080 San Vicente del Raspeig, Alicanteen
dc.contributor.departmentUniversidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Aptdo. 99. 03080 San Vicente del Raspeig, Alicanteen
dc.contributor.departmentUniversidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Aptdo. 99. 03080 San Vicente del Raspeig, Alicanteen
dc.contributor.departmentUniversidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Aptdo. 99. 03080 San Vicente del Raspeig, Alicanteen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentUniversidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Aptdo. 99. 03080 San Vicente del Raspeig, Alicanteen
item.openairetypearticle-
item.cerifentitytypePublications-
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item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Apto. 99. 03080 San Vicente del Raspeig. Alicante-
crisitem.author.deptDepartamento de Ciencias de la Tierra y del Medio Ambiente, Universidad de Alicante, Apdo. Correos 99, 03080 Alicante, Spain-
crisitem.author.deptUniversidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente. Apto. 99. 03080 San Vicente del Raspeig. Alicante-
crisitem.author.deptDepartamento de Ciencias de la Tierra y del Medio Ambiente. Universidad de Alicante. Apdo. Correos 99, 03080 Alicante.-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptUniversidad de Alicante, Departamento de Ciencias de la Tierra y del Medio Ambiente, Apto. 99, 03080 San Vicente del Raspeig, Alicante, Spain-
crisitem.author.orcid0000-0002-5546-2291-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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