000168713 001__ 168713
000168713 005__ 20260217214838.0
000168713 0247_ $$2doi$$a10.1016/j.palaeo.2011.07.015
000168713 0248_ $$2sideral$$a73943
000168713 037__ $$aART-2011-73943
000168713 041__ $$aeng
000168713 100__ $$0(orcid)0000-0003-3950-1630$$aCastanera, D.$$uUniversidad de Zaragoza
000168713 245__ $$aNew evidence of a herd of titanosauriform sauropods from the lower Berriasian of the Iberian range (Spain)
000168713 260__ $$c2011
000168713 5203_ $$aA study of the undescribed part of the Las Cerradicas tracksite in Galve (Teruel, Spain) has revealed 6 trackways made by small sauropods showing gregarious behaviour (parallel trackways). Las Cerradicas is located towards the top of the Villar del Arzobispo Formation (early Berriasian). The wide-gauge condition, the manus–pes distance, the kidney-shaped morphology of the manus, and the subtriangular morphology of the pes (with a big digit I that swells medially and a narrow heel oriented posterolaterally) suggest that the sauropods in question are more similar to Sauropodichnus giganteus than to any other sauropod ichnotaxa. Some of the features point to the titanosauriforms as the best candidates to be the trackmakers. Recent work in bone histology, the differences with respect to other Iberian tracksites of similar age, and the differences with respect to other sauropod herds of the track record, do not allow us to establish whether the sauropods were juvenile or dwarfs. The sauropod skeletal record and other large sauropod footprints in the Villar del Arzobispo Formation could tip the scales in favour of the first hypothesis.
000168713 540__ $$9info:eu-repo/semantics/closedAccess$$aAll rights reserved$$uhttp://www.europeana.eu/rights/rr-f/
000168713 590__ $$a2.392$$b2011
000168713 591__ $$aGEOSCIENCES, MULTIDISCIPLINARY$$b31 / 170 = 0.182$$c2011$$dQ1$$eT1
000168713 591__ $$aPALEONTOLOGY$$b4 / 49 = 0.082$$c2011$$dQ1$$eT1
000168713 591__ $$aGEOGRAPHY, PHYSICAL$$b14 / 44 = 0.318$$c2011$$dQ2$$eT1
000168713 655_4 $$ainfo:eu-repo/semantics/article$$vinfo:eu-repo/semantics/publishedVersion
000168713 700__ $$aBarco, J. L.$$uUniversidad de Zaragoza
000168713 700__ $$aDíaz-Martínez, I.
000168713 700__ $$aGascón, J. H.
000168713 700__ $$aPérez-Lorente, F.
000168713 700__ $$0(orcid)0000-0003-1732-9155$$aCanudo, J. I.$$uUniversidad de Zaragoza
000168713 7102_ $$12000$$2655$$aUniversidad de Zaragoza$$bDpto. Ciencias de la Tierra$$cÁrea Paleontología
000168713 773__ $$g310, 3-4 (2011), 227-237$$pPalaeogeogr. palaeoclimatol. palaeoecol.$$tPALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY$$x0031-0182
000168713 8564_ $$s2677762$$uhttps://zaguan.unizar.es/record/168713/files/texto_completo.pdf$$yVersión publicada
000168713 8564_ $$s976040$$uhttps://zaguan.unizar.es/record/168713/files/texto_completo.jpg?subformat=icon$$xicon$$yVersión publicada
000168713 909CO $$ooai:zaguan.unizar.es:168713$$particulos$$pdriver
000168713 951__ $$a2026-02-17-20:14:02
000168713 980__ $$aARTICLE