000121225 001__ 121225
000121225 005__ 20240319081023.0
000121225 0247_ $$2doi$$a10.1016/j.earscirev.2022.104251
000121225 0248_ $$2sideral$$a131655
000121225 037__ $$aART-2022-131655
000121225 041__ $$aeng
000121225 100__ $$0(orcid)0000-0002-2430-7424$$aAurell, Marcos$$uUniversidad de Zaragoza
000121225 245__ $$aLatest Cretaceous palaeogeographic evolution of northeast Iberia: Insights from the Campanian continental Montalbán subbasin (Spain)
000121225 260__ $$c2022
000121225 5060_ $$aAccess copy available to the general public$$fUnrestricted
000121225 5203_ $$aThis work characterizes for the first time the 500–700 m-thick uppermost Cretaceous continental sedimentary succession of the Allueva Fm recorded in the northeastern margin of the Iberian basin, in the Montalbán subbasin (Maestrazgo domain, Spain). The middle-upper Campanian age of this unit constrained here by new paleomagnetic and biostratigraphic data involves major revision of previous stratigraphic and palaeogeographic interpretations. The uplift of the northern marginal areas of the Montalbán subbasin onwards from the middle Campanian supplied the coarse terrigenous-clastic sediments common in the alluvial Allueva Fm. Moreover, a sharp increase of the sedimentation rates (from 4 to 19 cm/ky) from the lower to the middle-upper part of the Allueva Fm has been related to further increase of the tectonic activity during the middle part of the late Campanian. Also relevant are the new discovered vertebrate sites mostly found in the marginal areas of a large lacustrine-palustrine carbonate system developed during the latest Campanian. Vertebrate sites include a fossil assemblage with abundance of titanosaur sauropod dinosaurs as well as the presence of ornithopod dinosaurs and crocodylomorphs. A review of the dinosaur fossil sites recorded in other Iberian subbasins shows a similar fossil assembage occurrence during the late Campanian–earliest Maastrichtian timespan, previous to the faunal turnover that took place in the Ibero-Armorican landmass around the onset of the late Maastrichtian. The stratigraphic, sedimentological and paleontological characterization of the successions recorded during the initial stages of development of the Montalbán subbasin have major implication to understand the latest Cretaceous palaeogeographic evolution of northeast Iberia. Comparative review to other latest Cretaceous continental successions deposited in other domains of the Iberian basin indicates a south to north migration of newly developed subsident subbasins: during the Campanian (South Iberian domain), during the middle-late Campanian (northern Maestrazgo domain), and during the Maastrichtian (central Castillian domain).
000121225 536__ $$9info:eu-repo/grantAgreement/ES/DGA/E18$$9info:eu-repo/grantAgreement/ES/MEC/FPU16-03064$$9info:eu-repo/grantAgreement/ES/MICINN/PID2021-122612OB-I00
000121225 540__ $$9info:eu-repo/semantics/openAccess$$aby-nc-nd$$uhttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
000121225 590__ $$a12.1$$b2022
000121225 592__ $$a3.807$$b2022
000121225 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b5 / 202 = 0.025$$c2022$$dQ1$$eT1
000121225 593__ $$aEarth and Planetary Sciences (miscellaneous)$$c2022$$dQ1
000121225 594__ $$a20.0$$b2022
000121225 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000121225 700__ $$aTorromé, Diego$$uUniversidad de Zaragoza
000121225 700__ $$aGasca, José M.
000121225 700__ $$aCalvín, Pablo
000121225 700__ $$0(orcid)0000-0002-6792-1563$$aPérez-Pueyo, Manuel$$uUniversidad de Zaragoza
000121225 700__ $$0(orcid)0000-0002-2426-7450$$aParrilla-Bel, Jara
000121225 700__ $$aMedrano-Aguado, Eduardo$$uUniversidad de Zaragoza
000121225 700__ $$aMartín-Closas, Carles
000121225 700__ $$aVicente, Alba
000121225 700__ $$aSierra-Campos, Pablo
000121225 700__ $$0(orcid)0000-0003-1732-9155$$aCanudo, José I.$$uUniversidad de Zaragoza
000121225 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000121225 7102_ $$12000$$2280$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Estratigrafía
000121225 773__ $$g235 (2022), 104251 [26 pp.]$$pEarth-sci. rev.$$tEarth-Science Reviews$$x0012-8252
000121225 8564_ $$s16805667$$uhttps://zaguan.unizar.es/record/121225/files/texto_completo.pdf$$yVersión publicada
000121225 8564_ $$s2479629$$uhttps://zaguan.unizar.es/record/121225/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000121225 909CO $$ooai:zaguan.unizar.es:121225$$particulos$$pdriver
000121225 951__ $$a2024-03-18-16:24:49
000121225 980__ $$aARTICLE