Río Neuquén Subgroup
The Río Neuquén Subgroup is a geological subgroup in the Neuquén Basin, Neuquén Province, Argentina, whose strata date back to the Late Cretaceous. The subgroup, formerly defined as a formation, is the middle unit of the Neuquén Group and contains the Plottier, Sierra Barrosa Formation,[1] Los Bastos Formation,[2] and Portezuelo Formations.[3][4][5] The subgroup overlies the Río Limay Subgroup and is overlain by the Río Colorado Subgroup.[6] Dinosaur remains are among the fossils that have been recovered from the formation.[7]
Río Neuquén Subgroup Stratigraphic range: Late Turonian-Late Coniacian ~91–86 Ma | |
---|---|
Type | Subgroup |
Unit of | Neuquén Group |
Sub-units | Plottier, Sierra Barrosa, Los Bastos & Portezuelo Formations |
Underlies | Río Colorado Subgroup |
Overlies | Río Limay Subgroup |
Thickness | Up to 155 m (509 ft) |
Lithology | |
Primary | Sandstone |
Other | Claystone, limestone, mudstone |
Location | |
Coordinates | 37.4°S 69.1°W |
Approximate paleocoordinates | 42.2°S 49.4°W |
Region | Mendoza, Río Negro & Neuquén Provinces |
Country | Argentina |
Extent | Neuquén Basin |
Type section | |
Named for | Neuquén River |
Río Neuquén Subgroup (Argentina) |
Fossil content
Dinosaurs | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Antarctosaurus[8] | A. giganteus[8] | "[Two] femora, pubis."[9] | Río Neuquén remains previously referred to A. giganteus are now attributed to an indeterminate sauropod.[8] | |||
A. wichmannianus[8] | ||||||
Megaraptor[8] | M. namunhuaiquii[8] | "Partial forelimb, manus, and pes."[10] | ||||
Patagonykus[8] | P. puertai[8] | "Partial postcranial skeleton."[11] | ||||
Rinconsaurus[8] | R. cadamirus[8] | |||||
Titanosaurus[8] | Indeterminate[8] | Titanosaurus is now considered a nomen dubium. | ||||
Unenlagia[8] | U. comahuensis[8] | "Fragmentary postcrania."[12] | ||||
See also
- List of dinosaur-bearing rock formations
References
- Garrido, 2011, p.237
- Garrido, 2011, p.236
- Balgord & Carapa, 2014, p.6
- Balgord, 2017, p.455
- Lebinson et al., 2018, p.252
- Leanza et al., 2004, p.63
- Weishampel, 2004, pp. 600-604
- "Río Neuquén Formation." Weishampel, et al. (2004). Pg. 603.
- "Table 13.1," in Weishampel, et al. (2004). Page 270.
- "Table 10.1," in Weishampel, et al. (2004). Page 199.
- "Table 11.1," in Weishampel, et al. (2004). Page 211.
- "Table 10.1," in Weishampel, et al. (2004). Page 198.
Bibliography
- Balgord, Elizabeth A. 2017. Triassic to Neogene evolution of the south-central Andean arc determined by detrital zircon U-Pb and Hf analysis of Neuquén Basin strata, central Argentina (34°S–40°S). Lithosphere 9. 453–462.
- Balgord, Elizabeth A., and Barbara Carapa. 2014. Basin evolution of Upper Cretaceous–Lower Cenozoic strata in the Malargüe fold-and-thrust belt: northern Neuquen Basin, Argentina. Basin Research _. 1–24. Accessed 2019-02-22.
- Garrido, Alberto C. 2011. El Grupo Neuquén (Cretácico Tardío) en la Cuenca Neuquina, 231–244. XVIII Congreso Geológico Argentino. Accessed 2019-02-23.
- Leanza, H.A.; S. Apesteguia; F.E. Novas, and M.S. De la Fuente. 2004. Cretaceous terrestrial beds from the Neuquén Basin (Argentina) and their tetrapod assemblages. Cretaceous Research 25. 61-87. Accessed 2019-02-16.
- Lebinson, Fernando; Martín Turienzo; Natalia Sánchez; Vanesa Araujo; María Celeste D'Annunzio, and Luis Dimieri. 2018. The structure of the northern Agrio fold and thrust belt (37°30’ S), Neuquén Basin, Argentina. Andean Geology 45. 249–273. Accessed 2019-02-22.
- Weishampel, David B.; Peter Dodson, and Halszka (eds.) Osmólska. 2004. The Dinosauria, 2nd edition, 1–880. Berkeley: University of California Press. Accessed 2019-02-21.ISBN 0-520-24209-2
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.