The La Cantera Formation is a geologic formation in Argentina originating from the Late Aptian. Fossil theropod tracks have been reported in the formation. The formation, deposited under lacustrine conditions, also has provided fossil plants, insects, fish, and gastropods.
Fossil content Among others, the following fossils have been reported from the formation:
Insects Hemiptera Canteronecta irajae Notonecta mazzoniae
Flora
See also List of dinosaur-bearing rock formations List of stratigraphic units with theropod tracks
References
Bibliography Castillo, Elías; Sánchez, María Lidia; Prámparo, Mercedes B. (2016), La Formación La Cantera: un ejemplo de relleno lacustre durante el pico de subsidencia del sistema de rift de Sierras Pampeanas Occidentales, San Luis (Cretácico Inferior), VII Congreso Latinoamericano de Sedimentología, retrieved 2019-02-16 Castillo Elías, Gabriela (2014), Depósitos lacustres de la Formación La Cantera (Aptiano Tardío), Sierras de El Gigante, cuenca de San Luis: nuevos aportes sedimentológicos, XIV Reunión Argentina de Sedimentología, retrieved 2019-02-16 Petrulevicius, J. F.; Nel, A.; Sallenave, A. S. (2010), "Recent genus Notonecta (Insecta: Heteroptera: Notonectidae) in the Lower Cretaceous of San Luis, Argentina: Palaeoecological implications", Annales de la Société Entomologique de France, 46 (1–2): 247–253, doi:10.1080/00379271.2010.10697665 Weishampel, David B.; Dodson, Peter; Osmólska, Halszka (2004), The Dinosauria, 2nd edition, Berkeley: University of California Press, pp. 1–880, ISBN 0-520-24209-2, retrieved 2019-02-21{{citation}}: CS1 maint: publisher location (link) Prámparo, M. B (1994), "Lower Cretaceous palynoflora of the La Cantera Formation, San Luis Basin: correlation with other Cretaceous palynofloras of Argentina", Cretaceous Research, 15 (2): 193–203, Bibcode:1994CrRes..15..193P, doi:10.1006/cres.1994.1010 Mazzoni, A. F (1985), "Notonectidae (Hemiptera, Heteroptera) de la formación La Cantera (Cretácico Inferior), Provincia de San Luis, Argentina", Boletin de la Academia Nacional de Ciencias, 56: 259–273
