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Los yacimientos de vertebrados continentales del Aragoniense superior (Mioceno medio) de Toril, Cuenca de Calatayud-Daroca

dc.contributor.authorAzanza, B.
dc.contributor.authorAlonso Zarza, Ana María
dc.contributor.authorÁlvarez-Sierra, M. Ángeles
dc.contributor.authorCalvo Sorando, José Pedro
dc.contributor.authorFraile Gracia, Susana
dc.contributor.authorGarcía-Paredes, I.
dc.contributor.authorGómez, E.
dc.contributor.authorHernández Fernández, Manuel
dc.contributor.authorMeulen, Albert J. van der
dc.contributor.authorMiguel, D. de
dc.contributor.authorMontoya, Plini
dc.contributor.authorMorales Romero, Jorge
dc.contributor.authorMurelaga, Xabier
dc.contributor.authorPeláez Campomanes, Pablo
dc.contributor.authorPérez, B.
dc.contributor.authorQuiralte, Victoria
dc.contributor.authorSalesa Calvo, Manuel J
dc.contributor.authorSánchez, Israel M.
dc.contributor.authorSanchez Marco, Antonio
dc.contributor.authorSoria, D.
dc.date.accessioned2023-06-20T12:47:09Z
dc.date.available2023-06-20T12:47:09Z
dc.date.issued2004
dc.description.abstractThe paleontological sites of Toril 3A and B (Upper Aragonian, Biozone C3, MN 7/8) posses an exceptional and abundant fauna of vertebrates. From 1997 until 2001 these two localities have been object of systematic paleontological excavations. Up to now 36 species of large and small mammals have been found in these localities; the association of vertebrates also includes amphibians, reptiles and birds, among the remains of fossils birds it is frequent to found egg shell fragments. There are not significant differences in the qualitative and quantitative faunistic composition of the two sites; in both the undetermined bone fragments and the remains of chelonians, most of them dermal bones, are the dominant fossils. An important characteristic is the abundance of small size hornless ruminants, which are quite scarce in the stratified sites of the Spanish Aragonian. Neither there are differences in the composition of the micromammals, the association is overwhelmingly dominated (more than 95%) for different cricetid species; in Toril 3A beavers reappears for the first time during the Aragonian, and they will be frequent in younger faunas of the same basin. The fossils were deposited in different sedimentary environments, related with alluvial and shallow lacustrine environments.
dc.description.departmentDepto. de Mineralogía y Petrología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.sponsorshipDirección General de Enseñanza Superior e Investigación Científica
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/60740
dc.identifier.issn1576-5172
dc.identifier.officialurlhttp://www.sociedadgeologica.es/publicaciones_geotemas.html
dc.identifier.urihttps://hdl.handle.net/20.500.14352/52515
dc.issue.number2
dc.journal.titleGeotemas
dc.language.isospa
dc.page.final274
dc.page.initial271
dc.publisherSociedad Geológica de España.
dc.relation.projectIDPB98-0691(C01, C02 y C03).
dc.rights.accessRightsopen access
dc.subject.cdu567/569
dc.subject.keywordVertebrates
dc.subject.keywordMammals
dc.subject.keywordUpper Aragonian
dc.subject.keywordToril-Nombrevilla
dc.subject.keywordDaroca
dc.subject.ucmPaleontología
dc.subject.unesco2416 Paleontología
dc.titleLos yacimientos de vertebrados continentales del Aragoniense superior (Mioceno medio) de Toril, Cuenca de Calatayud-Daroca
dc.typejournal article
dc.volume.number6
dspace.entity.typePublication
relation.isAuthorOfPublicationf29ff48e-a667-4a09-89eb-a8c1b3d55083
relation.isAuthorOfPublication4aa3824b-ca03-45fd-b468-ebd78cb1ac8f
relation.isAuthorOfPublicatione3f6cd28-60a6-4428-8f81-6350e1d14dbe
relation.isAuthorOfPublicationd7d8897f-0be5-4679-a9a1-87e0ef379cc1
relation.isAuthorOfPublication.latestForDiscovery4aa3824b-ca03-45fd-b468-ebd78cb1ac8f

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