The Uberaba Formation is part of the Bauru Group. It is located in Uberaba, Minas Gerais State. This formation has yielded only disarticulated dinosaur specimens. Santucci (2002) noted that sauropod remains from the Uberaba Formation represent possibly basal titanosaurs.Sauropoda n.sp. et gen.Sauropoda Megalodontidae indet.Sauropoda Titanosauria indet.Aeolosaurus sp.References:Santucci, R. M. (2002). Revisao dos titanosaurideos do Cretaceo Superior do Brasil. Master Dissertation. Universidade Estadual Paulista/Rio Claro, 179 p.Candeiro, C. R. A. (2007) - Cretaceous biota of the Triangulo Mineiro region (Brazil): A review of recent finds / Biota cretacica de la region del Triangulo Mineiro (Brasil): Revision de hallazgos recientes. Estudios Geologicos, 63 (1) Jan-Jun 2007, pgs. 65-73. Dinosauriformes- SacisaurusDinosauria Owen, 1842- Teyuwasu- Ornithischia Seeley, 1888- Saurischia Seeley, 1887-- Herrerasauria Galton, 1985--- Staurikosaurus-- Sauropodomorpha Huene, 1932--- "Prosauropoda" Huene, 1920--- (?) Saturnalia ---- Unaysaurus--- Sauropoda Marsh, 1878---- Gravisauria Allain & Aquesbi, 2008----- Eusauropoda------Neosauropoda Bonaparte, 1986------- Macronaria-------- Titanosauria--------- Lithostrotia (ex-Titanosauridae)---------- Eutitanosauria----------- Aeolosaurini------------ Gondwanatitan------------ Adamantisaurus-- Theropoda Marsh, 1881-- (?) Guaibasaurus--- Ceratosauria Marsh, 1884---- Abelisauroidea Bonaparte & Novas, 1985----- Abelisauridae Bonaparte & Novas, 1985--- Tetanurae Gauthier, 1986---- Spinosauroidea----- Angaturama----- Irritator---- Avetheropoda Paul, 1988 (= Neotetanurae Sereno, 1999)----- Carnosauria ( = Allosauroidea Marsh, 1878)------ Carcharodontosauridae Stromer, 1931------- Carcharodontosaurinae------- Giganotosaurinae Coria & Currie, 2006----- Coelurosauria Huene, 1920 Pampadromaeus barberenai Cabreira, Schultz, Bittencourt, Soares, Fortier, Silva & Langer, 2011Place: Santa Maria Formation, Alemoa Member;Time: Late Triassic - Upper Carnian;Size: 1,5m.Etymology: . The generic name maximus means runner "from the Pampas", and specific name honours the Brazilian palaeontologist Mario C. Barberena.New stem-sauropodomorph (Dinosauria, Saurischia) from the Triassic of BrazilSergio F. Cabreira, Cesar L. Schultz, Jonathas S. Bittencourt, Marina B. Soares and Daniel C. Fortier, et al.NaturwissenschaftenDOI 10.1007/s00114-011-0858-0 Online FirstTM, 14 November 2011Abstract Post-Triassic theropod, sauropodomorph, and ornithischian dinosaurs are readily recognized based on the set of traits that typically characterize each of these groups. On the contrary, most of the early members of those lineages lack such specializations, but share a range of generalized traits also seen in more basal dinosauromorphs. Here, we report on a new Late Triassic dinosaur from the Santa Maria Formation of Rio Grande do Sul, southern Brazil. The specimen comprises the disarticulated partial skeleton of a single individual, including most of the skull bones. Based on four phylogenetic analyses, the new dinosaur fits consistently on the sauropodomorph stem, but lacks several typical features of sauropodomorphs, showing dinosaur plesiomorphies together with some neotheropod traits. This is not an exception among basal dinosaurs, the early radiation of which is characterized by a mosaic pattern of character acquisition, resulting in the uncertain phylogenetic placement of various early members of the group. Aeolosaurus maximus Santucci & Arruda-Campos, 2011Place: Adamantina Formation, near Monte Alto, Sao Paulo State;Time: Late Cretaceous - Campanian-Maastrichtian;Size: 16m.Etymology: . The specific name maximus means biggest.Santucci, R.M., & A.C. de Arruda-Campos. 2011. A new sauropod (Macronaria, Titanosauria) from the Adamantina Formation, Bauru Group, Upper Cretaceous of Brazil and the phylogenetic relationships of Aeolosaurini. Zootaxa 3085:1-33. Calvo, Jorge O. et al. (2007) - A new Cretaceous terrestrial ecosystem from Gondwana with the description of a new sauropod dinosaur. An. Acad. Bras. Cienc., Sept 2007, vol.79, no.3, p.529-541. ISSN 0001-3765 Abstract