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Gasparinisaura
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Gasparinisaura (meaning "Gasparini's lizard") is a of herbivorous from the . The first fossils of Gasparinisaura were found in 1992 near in Río Negro Province, . The , Gasparinisaura cincosaltensis, was named and described in 1996 by and . The generic name honors Argentine palaeontologist Zulma Brandoni de Gasparini. The specific name refers to Cinco Saltos.Coria, R. A., and L. Salgado. (1996). "A basal iguanodontian (Ornithischia: Ornithopoda) from the Late Cretaceous of South America". Journal of Vertebrate Paleontology 16: 445–457


Discovery
The , MUCPv-208, was uncovered in 1992 in a layer of the Anacleto Formation, dating from the early , about 83 million years old. It consists of a partial skeleton with skull, lacking much of the vertebral column. The is MUCPv-212, a tail with lower hindlimb elements. In 1997, three additional specimens were described: MUCPv 213, a partial skeleton with skull; MCSPv 111, a postcranial skeleton; and MCSPv 112, a skull with hindlimbs and pelvis. The three later specimens represent juvenile individuals.Salgado, L., Coria, R.A., and Heredia, S., 1997, "New materials of Gasparinisaura cincosaltensis (Ornithischia: Ornithopoda) from the Upper Cretaceous of Argentina", Journal of Paleontology 71: 933–940 In 2008, present with all three juvenile specimens were described.Ignacio A. Cerda, 2008, "Gastroliths in an ornithopod dinosaur", Acta Palaeontologica Polonica 53(2): 351-355


Description
Gasparinisaura was a small bipedal herbivore. In 2010, Gregory S. Paul estimated the length at and the weight at .Paul, G.S., 2010, The Princeton Field Guide to Dinosaurs, Princeton University Press p. 278

Gasparinisaura had a rounded head that was moderately elongated. The eye sockets were very large and placed in a high position. The rather long back of the head was pendant. The had a front branch that was thin and wedged between the and the ; the back of the jugal was high and broad. The had a long ascending process touching the , a basal trait. The jaw joints were low. There were about twelve, rather large, maxillary or dentary teeth in each upper or lower jaw. The forelimbs were lightly built. The ilium was short and low, the pubis thin. The hindlimbs were relatively long and powerful, with a short and a long lower leg. The foot was long and the first was reduced to a splint, a derived trait. The tail featured low plate-like triangular chevrons that were expanded towards the back, which is unique in the .

The gastroliths discovered formed clusters of up to hundred-forty rounded and polished stones in the abdomen with an average stone diameter of about eight millimetres. Representing about 0.3% of total body weight, they were voluminous enough to function as a gastric mill, a function sometimes denied for gastroliths because of their insufficient relative mass, being an order of magnitude lower.


Classification
Gasparinisaurus was originally considered by the describers to have been a basal , the most basal member of the . A phylogenetic analysis included in the description of the Antarctic ornithopod shows that the latter and Gasparinisaura are part of , a of hypsilophodonts known from South America, Antarctica and maybe Australia. Gasparinisaura would be the basalmost member of this group. Sebastián Rozadilla, Federico L. Agnolin, Fernando E. Novas, Alexis M. Aranciaga Rolando, Matías J. Motta, Juan M. Lirio & Marcelo P. Isasi, 2016, "A new ornithopod (Dinosauria, Ornithischia) from the Upper Cretaceous of Antarctica and its palaeobiogeographical implications", Cretaceous Research 57: 311–324

based in the phylogenetic analysis of Rozadilla et al., 2016:

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