Padillasaurus

The fossil was discovered by local farmers in a limestone nodule during the 1990s in Ricaurte, northeast of Villa de Leyva. The exact site of the find is unknown, however the rock matrix in which the fossil was located contains ammonite fossils bellowing to the species Gerhardtia galeatoides and Lytoceras sp., that allow the establishment of their origin in the middle Paja Formation which has been placed in the late Barremian, around 130 million years old. The fossil consists of vertebrae from the torso, sacrum and tail: all presumed to be from one individual. This specimen is the holotype assigned to the catalogue number JACVM 0001; this includes a rear dorsal vertebra, a series from the last two sacral vertebrae and first eight caudal vertebrae (these caudal vertebrae were found without their chevrons). The sacral vertebrae have been identified as the fourth and fifth. This fossil was donated by the farmers and became part of the collection at the museum of the Junta de Acción Comunal de la Vereda de Monquirá. Padillasaurus was originally described and named by José L. Carballido, Diego Pol, Mary L. Parra Ruge, Santiago Padilla Bernal, María E. Páramo-Fonseca y Fernando Etayo-Serna in 2015. The name of the genus pays homage to Carlos Bernardo Padilla, the founder of the Centro de Investigaciones Paleontológicas in Villa de Leyva, Colombia. The specific name, leivaensis, is named after Villa de Leyva, which is located nearby to where the vertebrae of the holotype specimen were discovered. Padillasaurus it is the first member officially named from South America. It is also the latest brachiosaurid known from the ancient continent of Gondwana. ==Description==

Padillasaurus was a medium-sized titanosauriform. Because of the few remains found it is difficult to determine what would have been its body size, but it may have been between long and weighed about . Padillasaurus is distinguished from other titanosauriforms in having its caudal vertebrae weakly expanded to the sides, and displaying divided side projections. The species shows some typical basic features of Titanosauriformes: the vertebra is opisthocoelic, with a convex front section and the back concave. The edges show large pleurocoels, pneumatic processes that connected to the hollow interior of the body of the vertebra, which consisted of several hollow cavities. The spine also had an additional lamina between the diapophysis and the body of the vertebra. The anterior caudal vertebrae are flattened or slightly concave from the front and from behind, or vice versa. The neural arches are positioned relatively forward. These have long ridges that run between the protuberances of the joint face and body of the vertebra. The side projections are oriented obliquely backwards and have a convex lower area. The caudal vertebrae have a height equal to half of its width. ==Phylogeny==

Padillasaurus was initially classified in the family Brachiosauridae based on its morphology. It had cavities in the sacral vertebrae that had no connection with the hollow interior of the vertebra, therefore lacking a true pleurocoel. This feature links it to the brachiosaurids. A cladistic analysis was unable to determine the exact relationships of Padillasaurus with other genera, finding a polytomy among basal forms including Padillasaurus, Abydosaurus, Brachiosaurus and Giraffatitan, while Cedarosaurus and Venenosaurus were occasionally recovered as sister taxa. Unlike Cretaceous brachiosaurids from North America, in which the spinous process of the caudal vertebrae leaned slightly forward, those of Padillasaurus were angled rearward. Cladogram from Carballido et al., 2015: == References ==