A New Sauropod: Tastavinsaurus Sanzi Gen. Et Sp. Nov. from the Early Cretaceous (Aptian) of Spain

By J. Canudo, R. Royo‐Torres, G. Cuenca‐Bescós. 2008

114 citations recorded by the source corpus.

Subfields: Nature and Landscape Conservation, Paleontology

View Paper: https://www.semanticscholar.org/paper/55194c952e38b2b32af61968f89c61ef92adff9d

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Citations in the corpus

Osteology of the Late Jurassic Portuguese sauropod dinosaur Lusotitan atalaiensis (Macronaria) and the evolutionary history of basal titanosauriforms (2013, methodology): “This core data set was supplemented with characters from subsequent phylogenetic analyses (i.e. Upchurch et al., 2004a; Curry Rogers, 2005; Canudo et al., 2008; Remes et al., 2009; Chure et al., 2010; Ksepka & Norell, 2010; Carballido et al., 2011b; Whitlock, 2011b; D’Emic, 2012, 2013; Mannion et…”
Revision of the sauropod dinosaur Diamantinasaurus matildae Hocknull et al. 2009 from the mid-Cretaceous of Australia: Implications for Gondwanan titanosauriform dispersal (2015, background): “This morphology occurs in several other somphospondylans, including Malawisaurus, Opisthocoelicaudia and Tastavinsaurus (Mannion et al., 2013).”
Postcranial axial skeleton of Europasaurus holgeri (Dinosauria, Sauropoda) from the Upper Jurassic of Germany: implications for sauropod ontogeny and phylogenetic relationships of basal Macronaria (2014, background): “The neural arch is anteriorly positioned in the centrum, a widespread character among titanosauriforms (Salgado et al. 1997) and closely related forms (e.g. Tastavinsaurus; Canudo et al. 2008).”
Anatomy of the basal titanosaur (Dinosauria, Sauropoda) Andesaurus delgadoi from the mid-Cretaceous (Albian–early Cenomanian) Río Limay Formation, Neuquén Province, Argentina: implications for titanosaur systematics (2011, background): “Most sauropods possess subcircular obturator foramina, but there are several titanosauriforms with oval foramina that are also oriented and positioned similarly to Andesaurus, e.g. Tastavinsaurus (Canudo et al., 2008: fig.”
The Osteology of Chubutisaurus insignis Del Corro, 1975 (Dinosauria: Neosauropoda) from the ‘Middle’ Cretaceous of Central Patagonia, Argentina (2011, methodology): “14B), as is also observed in other macronarians (e.g., Euhelopus Wiman, 1929; Tastavinsaurus, Canudo et al., 2008), but having a smaller angle than in derived titanosaurs (e.g., Rapetosaurus, Curry Rogers and Foster, 2001; Saltasaurus, Powell, 1992).”
The early evolution of titanosauriform sauropod dinosaurs (2012, methodology): “One most parsimonious cladogram was reported by Canudo et al. (2008), but the polytomies those authors depict implies that the number of most parsimonious cladograms is equal to at least nine.”
A Reappraisal of the Late Cretaceous Argentinean Sauropod Dinosaur Argyrosaurus superbus, with a Description of a New Titanosaur Genus (2012, unknown): “This bifurcated morphology is a feature traditionally thought to be restricted to derived titanosaurs (e.g., Antarctosaurus, Opisthocoelicaudia, and Saltasaurus; Powell, 1992; Upchurch, 1998), but is present in a wider array of titanosauriforms, including Giraffatitan (HMN MBR 2698 [St 149]; P.D.M.,”