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dc.contributor.authorCanudo, José Ignacio
dc.contributor.authorGasca Pérez, José Manuel 
dc.contributor.authorMoreno-Azanza, Miguel
dc.contributor.authorAurell, M.
dc.date.accessioned2024-02-09T12:58:26Z
dc.date.available2024-02-09T12:58:26Z
dc.date.issued2012
dc.identifier.citationCANUDO JI, GASCA JM, MORENO-AZANZA M, AURELL M. New information about the stratigraphic position and age of the sauropod Aragosaurus ischiaticus from the Early Cretaceous of the Iberian Peninsula. Geological Magazine. 2012;149(2):252-263. doi:10.1017/S0016756811000732es_ES
dc.identifier.issn0016-7568
dc.identifier.urihttp://hdl.handle.net/10366/155648
dc.description.abstract[EN]The sauropod Aragosaurus ischiaticus Sanz, Buscalioni, Casanovas & Santafé, 1987 was the first dinosaur to be described in Spain. The holotype was recovered from the site of Las Zabacheras (Galve, Teruel province). This site has traditionally been situated in the El Castellar Formation (in the lower part of the Wealden facies). Recently, it has been proposed that the remains of Aragosaurus stem from the Villar del Arzobispo Formation (late Tithonian-upper part of the early Berriasian), which would mean that the sauropod was almost 15 million years older than previously thought. Detailed field work has been carried out, making it possible to pinpoint the position of the low-angle unconformity between the Villar del Arzobispo Formation and the El Castellar Formation. This unconformity originated as a result of block tilting that occurred during the early stages of the Early Cretaceous rifting episode. The upper levels of the Jurassic sequence (i.e. the Villar del Arzobispo Formation) were exposed to erosion and karstification, leading to the formation of a discontinuous conglomeratic level. This level has been locally preserved at the bottom of the Wealden syn-rift sequence (i.e. the El Castellar Formation). The results of our detailed mapping demonstrate that the Aragosaurus holotype was found in the lower part of the El Castellar Formation. Moreover, our revision of the existing datings suggests that the El Castellar Formation as a whole is Valanginian?-early Barremian in age. Given that Aragosaurus was located in its lower part, it is probably Valanginian?-Hauterivian in age.es_ES
dc.description.sponsorshipThis paper forms part of the projects CGL2007-62469 and CGL2010-16447 and is subsidized by the Spanish Ministry of Science and Innovation, the European Regional Development Fund and the Government of Aragón (‘Grupos Consolidados’ and ‘Dirección General de Patrimonio Cultural’).FPI grant (B064/08B) from the Government of Aragón.es_ES
dc.format.mimetypeapplication/pdf
dc.language.isoenges_ES
dc.publisherCambridge University Presses_ES
dc.subjectAragosauruses_ES
dc.subjectDinosaures_ES
dc.subjectDatinges_ES
dc.subjectCastellar Formationes_ES
dc.subjectVillar del Arzobispo Formationes_ES
dc.subjectEarly Cretaceouses_ES
dc.titleNew information about the stratigraphic position and age of the sauropodAragosaurus ischiaticusfrom the Early Cretaceous of the Iberian Peninsula.es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publishversionhttps://doi.org/10.1017/S0016756811000732es_ES
dc.subject.unesco2506 Geologíaes_ES
dc.subject.unesco2416.05 Paleontología de Los Vertebradoses_ES
dc.subject.unesco2506.19 Estratigrafíaes_ES
dc.identifier.doi10.1017/S0016756811000732
dc.relation.projectIDCGL2007-62469es_ES
dc.relation.projectIDCGL2010-16447es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.identifier.essn1469-5081
dc.journal.titleGeological Magazinees_ES
dc.volume.number149es_ES
dc.issue.number2es_ES
dc.page.initial252es_ES
dc.page.final263es_ES
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones_ES


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