The Titanosaur Sauropods from the late Campanian–early Maastrichtian Allen Formation of Salitral Moreno, Río Negro, Argentina

dc.creatorGarcia, Rodolfo A.
dc.creatorSalgado, Leonardo
dc.date2011-09
dc.date.accessioned2023-08-30T16:47:18Z
dc.date.available2023-08-30T16:47:18Z
dc.identifierGarcia, Rodolfo A., Salgado, Leonardo. (2011). The Titanosaur Sauropods from the late Campanian–early Maastrichtian Allen Formation of Salitral Moreno, Río Negro, Argentina. Polish Academy Of Sciences. Institute Of Paleobiology; Acta Palaeontologica Polonica; 58; 2; pp.269-284
dc.identifier0567-7920
dc.identifier1732-2421
dc.identifierhttps://www.app.pan.pl/article/item/app20110055.html
dc.identifierhttp://hdl.handle.net/11336/9015
dc.identifierhttps://rid.unrn.edu.ar/jspui/handle/20.500.12049/2645
dc.identifierhttp://dx.doi.org/10.4202/app.2011.0055
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8537563
dc.descriptionFil: Garcia, Rodolfo A. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
dc.descriptionFil: Salgado, Leonardo. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.
dc.descriptionFil: Salgado, Leonardo. Universidad Nacional de Rio Negro. Sede Alto Valle; Argentina
dc.descriptionFil: Salgado, Leonardo. Instituto de Investigaciones en Paleobiologia y Geologia; Argentina
dc.descriptiontrue
dc.descriptionThe dinosaur record of the Salitral Moreno locality (Río Negro Province, Argentina) is characterized by a high diversity of herbivore taxa, among them hadrosaurs, ankylosaurs, and titanosaur sauropods, but carnivores are rare, consisting of only a few fragmentary bones of small forms. Titanosaurs are represented by Rocasaurus muniozi and Aeolosaurus sp., and at least four other taxa, represented by fragmentary material. The elements preserved include a cervical, dorsal and caudal vertebrae, chevron, humerii, ulnae, radii, metacarpal, femora, tibiae, metatarsal, ischia, pubis, and ilium. The Allen Formation is thought to be correlated with the Marília Formation in Brazil, and their faunas have certain elements in common such as aeolosaurines, but saltasaurines and hadrosaurs, are known exclusively from the Allen Formation. These ab− sences, and particularly that of the saltasaurines, may be because those sauropods originated late in the Cretaceous, probably in southern South America (Northern Patagonia?), and they did not have time to disperse to northern South America.
dc.formatapplication/pdf
dc.languageen
dc.relation58
dc.relationActa Palaeontologica Polonica
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/4.0/
dc.subjectCiencias Ambientales y de la Tierra
dc.subjectDinosauria
dc.subjectSaurischia
dc.subjectSauropodomorpha
dc.subjectSauropoda
dc.subjectTitanosauria
dc.subjectTitanosaur
dc.subjectSalitral Moreno
dc.subjectAllenFormation
dc.subjectMaastrichtian
dc.subjectPatagonia
dc.subjectCiencias Ambientales y de la Tierra
dc.titleThe Titanosaur Sauropods from the late Campanian–early Maastrichtian Allen Formation of Salitral Moreno, Río Negro, Argentina


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