Please use this identifier to cite or link to this item: https://cir.cenieh.es/handle/20.500.12136/396
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dc.contributor.authorBlain, Hugues-Alexandre-
dc.contributor.authorAgustí, Jordi-
dc.contributor.authorLópez-García, Juan Manuel-
dc.contributor.authorHaddoumi, Hamid-
dc.contributor.authorAouraghe, Hassan-
dc.contributor.authorEl-Hammouti, Kamal-
dc.contributor.authorPérez-González, Alfredo-
dc.contributor.authorChacón Navarro, María Gema-
dc.contributor.authorSala, Robert-
dc.date.accessioned2018-06-04T14:05:29Z-
dc.date.issued2013-07-
dc.identifier.citationJournal of Vertebrate Paleontology, 2013, 33 (4), 804-816es_ES
dc.identifier.issn0272-4634-
dc.identifier.issn1937-2809-
dc.identifier.urihttp://cir.cenieh.es/handle/20.500.12136/396-
dc.description.abstractThe fossil amphibians and squamate reptiles from the late Miocene (Vallesian) of Guefaït-1 are described for the first time. The herpetofaunal assemblage is composed of Discoglossinae indet., Lacertidae indet., Dopasia sp. (Anguidae), Colubridae s. l. indet., and Naja cf. antiqua (Elapidae). This herpetofaunal assemblage is less diverse than the Moroccan herpetofauna from the middle and early late Miocene mainly because of the absence of Afro-tropical taxa, probably due to increasing aridity; likewise, it is less diverse than the Plio-Pleistocene herpetofauna, which was enriched by the entry of some European taxa during the Messinian Crisis. The presence of a discoglossine frog, different from all existing European and North African genera, in the late Miocene of Guefaït-1 suggests that the diversity of this group in the Miocene of North Africa may have been greater than previously thought. The occurrence of an anguid lizard of the genus Dopasia in the Miocene of Morocco is confirmed and may constitute the earliest record of the genus for Africa. The range of the cobra Naja antiqua, until now only known from the middle Miocene (Mellalesian) of Beni Mellal, Morocco, is extended; this constitutes the latest record of the species.es_ES
dc.description.sponsorshipThe work carried out in Guefaït (eastern Morocco) has been possible thanks to the financial support of the Spanish Agency of International Cooperation for Development: AECID (PCI) projects number A/4542/05, A/011208/07, A/019244/08, and A1/039433/1. H.-A.B. is grateful to J. E. González (MNCN, Madrid) and S. Bailon (MNHN, Paris) for facilitating access to the material for osteological comparison in their care; and to the staff of the Servei de Recursos Científic I Tecnic of the University Rovira I Virgili (Tarragona) for their help during the realization of the pictures using an environmental scanning electron microscope. J.M. L.-G. is beneficiary of a Beatriu de Pinós postdoctoral fellowship (2011BP-A00272) from the Generalitat de Catalunya, a grant co-funded by the European Union through the Marie Curie Actions of the 7th Framework Program for R+D. M.G.C. has been supported by postdoctoral grant from the Juan de la Cierva Subprogram (JCI-2010-07683), with the financial sponsorship of the Spanish Ministry of Science and Innovation. This paper is also part of the projects CGL2012-38358/BTE and HAR2010-19957 (Spanish Ministry of Science and Innovation and Spanish Ministry of Economy and Competitiveness) and SGR2009-188 and SGR2009-324 (Generalitat de Catalunya).es_ES
dc.language.isoenes_ES
dc.publisherTaylor & Francises_ES
dc.rightsinfo:eu-repo/semantics/openAccess-
dc.titleAmphibians and squamate reptiles from the Late Miocene (Vallesian) of Eastern Morocco (Guefaït-1, Jerada Province)es_ES
dc.typeArticlees_ES
dc.identifier.doi10.1080/02724634.2013.740541-
dc.relation.publisherversionhttps://doi.org/10.1080/02724634.2013.740541es_ES
dc.date.available2018-06-04T14:05:29Z-
Appears in Collections:Geocronología y Geología

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