Velocisaurus was probably around 1.5 meters (4.9 feet) long, based on a tibia length of 14 centimetres (5.5 in).[1] This makes it the smallest noasaurid, after Berthasaura. The foot is unique in that the middle (third) metatarsal has become the main weight-bearing element. Its upper end has thickened whereas the shafts of the adjoining second and fourth metatarsals have thinned considerably. Such a configuration is unknown for other theropods, including birds. Bonaparte explained it as an adaptation for a cursorial (running) lifestyle. The high speed would have been necessary to escape larger theropods; Bonaparte suggested that Velocisaurus was itself an omnivore, as indicated by the fact that the sole claw found, of the fourth toe, was not trenchant but relatively straight.[2]
Velocisaurus can be characterized by several traits unknown in other Abelisauroids. These include:[3]
A subtriangular cross section of the femur, with the medial and lateral sides converging to form a thick crest pointing anteriorly (a subtriangular cross section of the femur is also known in Masiakasaurus).
A long and slender tibia with a large anteriorly flat distal end to accommodate a large ascending process of the astragalus (reminiscent of derived coelurosaurs and ornithomimids).
Very thin and rod-like metatarsals II and IV (metatarsal II is reduced to a lesser extent in other noasaurids and some abelisaurids as well).
An anteroposteriorly short and dorsoventrally tall subtriangular pedal phalanx IV-1, with a narrow dorsal surface.
In a 2001 study conducted by Bruce Rothschild and other paleontologists, 12 foot bones referred to Velocisaurus were examined for signs of stress fracture, but none were found.[6]
^Grillo, O. N.; Delcourt, R. (2016). "Allometry and body length of abelisauroid theropods: Pycnonemosaurus nevesi is the new king". Cretaceous Research. 69: 71–89. doi:10.1016/j.cretres.2016.09.001.
^ abBonaparte J.F. (1991). "Los vertebrados fósiles de la Formación Rio Colorado, de la Ciudad de Neuquén y Cercanías, Cretácico Superior, Argentina" [The fossil vertebrates of the Rio Colorado Formation, of the city of Neuquén and surroundings, Upper Cretaceous, Argentina]. Revista del Museo Argentino de Ciencias Naturales "Bernardino Rivadavia" e Instituto Nacional de Investigación de las Ciencias Naturales. Paleontología4: 17-123
^F. AGNOLÍN, F. NOVAS and S. APESTEGUÍA (2003). "Velocisaurids in South America and Madagascar". Ameghiniana40(4): 77R. Museo Argentino de Ciencias Naturales ‘B. Rivadavia’, Av. Ángel Gallardo 470, (1405) Buenos Aires, Argentina
^F. E. Novas, F. L. Agnolin, and S. Bandyopadhyay, 2004, "Cretaceous theropods from India: a review of specimens described by Huene and Matley (1933)", Revista del Museo Argentino de Ciencias Naturales, nuevo serie6(1): 67-103
^Rothschild, B., Tanke, D. H., and Ford, T. L., 2001, Theropod stress fractures and tendon avulsions as a clue to activity: In: Mesozoic Vertebrate Life, edited by Tanke, D. H., and Carpenter, K., Indiana University Press, p. 331-336.