000063342 001__ 63342
000063342 005__ 20171129112118.0
000063342 0247_ $$2doi$$a10.1371/journal.pone.0072579
000063342 0248_ $$2sideral$$a82357
000063342 037__ $$aART-2013-82357
000063342 041__ $$aeng
000063342 100__ $$aVila, B.
000063342 245__ $$aThe latest succession of dinosaur tracksites in Europe: hadrosaur ichnology, track production and paleoenvironments.
000063342 260__ $$c2013
000063342 5060_ $$aAccess copy available to the general public$$fUnrestricted
000063342 5203_ $$aA comprehensive review and study of the rich dinosaur track record of the Tremp Formation in the southern Pyrenees of Spain (Southwestern Europe) shows a unique succession of footprint localities prior to the end-Cretaceous mass extinction event. A description of some 30 new tracksites and data on sedimentary environments, track occurrence and preservation, ichnology and chronostratigraphy are provided. These new track localities represent various facies types within a diverse set of fluvial environments. The footprint discoveries mostly represent hadrosaurian and, less abundantly, to sauropod dinosaurs. The hadrosaur tracks are significantly smaller in size than, but morphologically similar to, those of North America and Asia and are attributable to the ichnogenus Hadrosauropodus. The track succession, with more than 40 distinct track levels, indicates that hadrosaur footprints in the Ibero-Armorican region occur predominantly in the late Maaastrichtian (at least above the early Maastrichtian–late Maastrichtian boundary). The highest abundance is found noticeably found in the late Maastrichtian, with tracks occurring in the C29r magnetochron, within about the latest 300,000 years of the Cretaceous.
000063342 536__ $$9info:eu-repo/grantAgreement/ES/MICINN/CGL2010-16447$$9info:eu-repo/grantAgreement/ES/MICINN/CGL2011-30069-C02-01-BTE$$9info:eu-repo/grantAgreement/ES/MICINN/CGL2011-30069-C02-02-BTE$$9info:eu-repo/grantAgreement/ES/MICINN/JDC-2011-Subprograma Juan de la Cierva$$9info:eu-repo/grantAgreement/ES/MINECO/BES-2012-052366-FPI
000063342 540__ $$9info:eu-repo/semantics/openAccess$$aby$$uhttp://creativecommons.org/licenses/by/3.0/es/
000063342 590__ $$a3.534$$b2013
000063342 591__ $$aMULTIDISCIPLINARY SCIENCES$$b8 / 56 = 0.143$$c2013$$dQ1$$eT1
000063342 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000063342 700__ $$aOms, O.
000063342 700__ $$aFondevilla, V.
000063342 700__ $$aGaete, R.
000063342 700__ $$aGalobart, À.
000063342 700__ $$aRiera, V.
000063342 700__ $$0(orcid)0000-0003-1732-9155$$aCanudo, J.I.$$uUniversidad de Zaragoza
000063342 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDepartamento de Ciencias de la Tierra$$cPaleontología
000063342 773__ $$g8, 9 (2013), e72579 [15 pp]$$pPLoS One$$tPLoS One$$x1932-6203
000063342 8564_ $$s884713$$uhttp://zaguan.unizar.es/record/63342/files/texto_completo.pdf$$yVersión publicada
000063342 8564_ $$s125743$$uhttp://zaguan.unizar.es/record/63342/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000063342 909CO $$ooai:zaguan.unizar.es:63342$$particulos$$pdriver
000063342 951__ $$a2017-11-28-13:52:11
000063342 980__ $$aARTICLE