000109032 001__ 109032
000109032 005__ 20211216151746.0
000109032 0247_ $$2doi$$a10.1007/s41513-020-00145-w
000109032 0248_ $$2sideral$$a122535
000109032 037__ $$aART-2020-122535
000109032 041__ $$aeng
000109032 100__ $$aTorcida Fernández-Baldor, F.
000109032 245__ $$aNew data on sauropod palaeobiodiversity at the Jurassic-Cretaceous transition of Spain (Burgos)
000109032 260__ $$c2020
000109032 5060_ $$aAccess copy available to the general public$$fUnrestricted
000109032 5203_ $$aThe present paper studies a humerus (MDS-VPCR, 214) recovered from the site of Valdepalazuelos-Tenadas del Carrascal (Burgos, Spain). Geologically, it is located at the base of the Rupelo Formation (Cameros Basin), which is Tithonian-Berriasian in age. This formation is interpreted as shallow lacustrine/palustrine deposits with low-gradient margins and periodic changes in the water level. MDS-VPCR, 214 is gracile and straight, and has a larger mediolateral expansion at its proximal end than at the distal end. The deltopectoral crest is well expanded anteroposteriorly and extends towards the midline of the shaft. The distal articular head has radial and ulnar condyles similar in degree of development and there is a narrow groove between them. The distal articular surface is not divided between the ulnar and radial condyles; this surface extends towards the anterior and posterior surfaces of the humerus. MDS-VPCR, 214 shows significant morphological differences with respect to the humeri of the Iberian sauropods of the Jurassic-Cretaceous transition such as the turiasaurians Losillasaurus, Zby and Turiasaurus, the basal macronarians Lourinhasaurus and Aragosaurus, and the titanosauriforms Lusotitan, Galvesaurus.A phylogenetic analysis of MDS-VPCR, 214 relates it to Titanosauriformes probably a basal brachiosaurid related with the english genus of Kimmeridgian Duriatitan. Therefore MDS-VPCR, 214 is assigned provisionally to aff. Duriatitan.
000109032 536__ $$9info:eu-repo/grantAgreement/ES/DGA/Grupo de Referencia Aragosaurus-reconstrucciones paleoambientales y recursos geológicos$$9info:eu-repo/grantAgreement/ES/MICINN-FEDER/CGL2017-85038-P
000109032 540__ $$9info:eu-repo/semantics/openAccess$$aAll rights reserved$$uhttp://www.europeana.eu/rights/rr-f/
000109032 590__ $$a1.859$$b2020
000109032 591__ $$aGEOLOGY$$b18 / 48 = 0.375$$c2020$$dQ2$$eT2
000109032 592__ $$a0.592$$b2020
000109032 593__ $$aStratigraphy$$c2020$$dQ2
000109032 593__ $$aGeology$$c2020$$dQ2
000109032 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/acceptedVersion
000109032 700__ $$0(orcid)0000-0003-1732-9155$$aCanudo, J.I.$$uUniversidad de Zaragoza
000109032 700__ $$aHuerta, P.
000109032 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000109032 773__ $$g46, 4 (2020), 351-362$$pJ. iber. geol.$$tJOURNAL OF IBERIAN GEOLOGY$$x1698-6180
000109032 8564_ $$s773817$$uhttps://zaguan.unizar.es/record/109032/files/texto_completo.pdf$$yPostprint
000109032 8564_ $$s2342829$$uhttps://zaguan.unizar.es/record/109032/files/texto_completo.jpg?subformat=icon$$xicon$$yPostprint
000109032 909CO $$ooai:zaguan.unizar.es:109032$$particulos$$pdriver
000109032 951__ $$a2021-12-16-12:53:45
000109032 980__ $$aARTICLE