Short communication: “Stratigraphical and sedimentological study of sedimentary rocks bearing late Albian giant Titanosaurs from central Patagonia, Argentina”
Keywords:
Giant titanosaurs, Patagonia, Late Albian, Cerro Castaño Member, Fluvial environment.Abstract
In the central Chubut province, within the Somuncurá-Cañadón Asfalto basin, an outstanding accumulation of vertebrate fossils, including remains of giant titanosaurs, was discovered. Such dinosaur clade constitutes one of the largest found in the world. This contribution provides a preliminary stratigraphic and sedimentological study in order to specify the temporal and stratigraphic position of the vertebrate accumulation, as well as understanding the depositional systems in which the dinosaurs developed. The titanousar remains are contained in the upper section of the Cerro Castaño Member (Cerro Barcino Formation), close to the boundary with the overlying Las Plumas Member. The fossil-bearing rocks are composed of sandstones and tuffaceous sandstones, formerly deposited within floodplains of a volcaniclastic, meandering fluvial system.
References
Anselmi, G., J.L. Panza, J.M.D. Cortés y D. Ragona, 2005. Hoja Geológica 4569-II, El Sombrero, Provincia de Chubut. Instituto de Geología y Recursos Minerales, Servicio Geológico Minero Argentino, Boletín 271:70 p. Buenos Aires.
Codignotto, J., F. Nullo, J. Panza y C. Proserpio, 1978. Estratigrafía del Grupo Chubut, entre Paso de Indios y Las Plumas, Chubut. 7º Congreso Geológico Argentino Actas:471-480, Neuquén.
Figari, E.G., R.A. Scasso, R.N. Cúneo y I. Escapa, 2015. Estrati- grafía y evolución geológica de la Cuenca de Cañadón Asfalto, provincia del Chubut, Argentina. Latin American Journal of Sedimentology and Basin Analysis 22:135-169.
Ruz Gatto, D., A.M. Umazano y J.M. Krause, 2016. Paleoambiente depositacional del Miembro Las Plumas (Formación Cerro Bar- cino) en Cerro Las Leoneras, Cretácico de Patagonia. 12° Jornadas Pampeanas de Ciencias Naturales Actas:103, Santa Rosa.
Downloads
Published
How to Cite
Issue
Section
License
This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.