| Roca Formation | |
|---|---|
| Stratigraphic range: Maastrichtian-late Danian (pre-Tiupampan) ~ | |
 Roca Formation in Barda Norte, General Roca, Río Negro | |
| Type | Geological formation |
| Unit of | Malargüe Group |
| Sub-units | 3 members |
| Underlies | El Carrizo & Pircala Formations |
| Overlies | Jagüel Formation |
| Thickness | Up to 58 m (190 ft) |
| Lithology | |
| Primary | Limestone, claystone, siltstone |
| Other | Gypsum |
| Location | |
| Coordinates | 38°54′S 67°36′W / 38.9°S 67.6°W |
| Approximate paleocoordinates | 41°30′S 56°00′W / 41.5°S 56.0°W |
| Region | Río Negro, Neuquén, La Pampa & Mendoza Provinces |
| Country |  Argentina |
| Extent | Neuquén Basin |
| Type section | |
| Named for | General Roca |
    Roca Formation, Argentina (Argentina) | |
The Roca Formation is a Cretaceous to Paleogene lithostratigraphic unit, located in the Neuquén Basin.[1] It crops out in the Argentinian provinces of Río Negro, Neuquén, La Pampa, and Mendoza.[2] Its deposition is diachronous, beginning during the Maastrichtian in the north of its distribution, and later moving to the south, where its strata reached the Late Danian. It lies transitionally above the Jagüel Formation, and the top of the formation is marked by a regional unconformity due to an Eocene and Oligocene orogenic pulse. These two units belong to the Malargüe Group. The marine sediments of the Jagüel and Roca Formations were deposited during a transgression from the Atlantic Ocean, beginning in the Maastrichtian and ending in the Danian.[3][4]
The stratotype of the Roca Formation is located 12 kilometres (7.5 mi) north of General Roca, Río Negro (39º40´S, 67º32´W). The fossiliferous beds of the Roca Formation were discovered by G. Rohde Windhausen (1914), who was also the first author to describe these sediments. Schiller (1922) took samples of one section along the Zanjón Roca, from the northern part of General Roca to Horno de Cal (lime kiln). This author proposed to name the lime kiln as the "classic area", and the westward cliffs from the lime kiln as the "model area" of these beds. The lithological composition of this type locality contains gray-yellowish and highly fossiliferous limestones, with greenish claystones and marls, and abundant gypsum at the top. The basal and middle sections are approximately 26 metres (85 ft) thick (Weber, 1972).[5]
- ^ Roca Formation at Fossilworks.org
- ^ Rodríguez, María Fernanda (2011). "El Grupo Malargüe (Cretácico Tardío-Paleógeno Temprano) en la Cuenca Neuquina". Relatorio del XVIII Congreso Geológico Argentino. Neuquén.
- ^ Archuby, Fernando; Salgado, Leonardo; Brezina, Soledad; Parras, Ana (2016). "Dos orillas, dos mundos: Paleontología del Alto Valle del río Negro". El Ojo del Cóndor. 7: 10–15.
- ^ Malumián, Norberto; Náñez, Carolina (2011). "The Late Cretaceous–Cenozoic transgressions in Patagonia and the Fuegian Andes: foraminifera, palaeoecology, and palaeogeography". Biological Journal of the Linnean Society. 103 (2): 269–288. doi:10.1111/j.1095-8312.2011.01649.x.
- ^ del Río, Claudia; Conchero, Andrea; Martínez, Sergio A. (2011). "The Maastrichtian – Danian at General Roca (Patagonia, Argentina): a reappraisal of the chronostratigraphy and biostratigraphy of a type locality". Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen. 259/2 (2): 129–156. doi:10.1127/0077-7749/2011/0103. hdl:11336/68472.