Cordobés Formation
| Cordobés Formation | |
|---|---|
| Stratigraphic range: Pragian-Emsian ~ | |
| Type | Geological formation |
| Unit of | Durazno Group |
| Underlies | La Paloma Formation |
| Overlies | Cerrezuelo Formation |
| Thickness | 92 m (302 ft) |
| Lithology | |
| Primary | Shale |
| Other | Fine sandstone |
| Location | |
| Coordinates | 33°00′S 55°00′W / 33.0°S 55.0°W |
| Approximate paleocoordinates | 68°30′S 136°12′W / 68.5°S 136.2°W |
| Region | Durazno Department |
| Country |  Uruguay |
| Extent | Norte Basin |
| Type section | |
| Named for | Arroyo Cordobés |
| Named by | Bossi |
| Year defined | 1966 |
  Cordobés Formation (Uruguay) | |
The Cordobés Formation is an Early Devonian (Pragian to Emsian) geologic formation of the Durazno Group in the Paraná Basin in the Durazno Department of central Uruguay. The shallow marine shales preserve trilobite, bivalve, gastropod and brachiopod fossils.[1][2]
Description[edit]
The Cordobés Formation is characterized by reddish fine shale deposited in a shallow marine environment.
Fossil content[edit]
The following fossils have been reported from the formation:[1][3]
See also[edit]
References[edit]
- ^ a b Emsian Loc. 1 of Melo: Uraguayan outcrop belt at Fossilworks.org
- ^ Daners et al., 2017
- ^ Melo, 1988
Bibliography[edit]
- Daners, Gloria; Alain Le Hérissé; Pierre Breuer, and Gerardo Veroslavsky. 2017. Pragian–Emsian palynomorphs from the Cordobés Formation, Norte Basin, Uruguay: stratigraphically restricted and regionally correlative palynological events in the cool-water Malvinokaffric Realm. Palynology 41(sup1). 121–137. . doi:10.1080/01916122.2017.1366115 ISSN 0191-6122
- Melo, J. H. G. 1988. The Malvinokaffric realm in the Devonian of Brazil. N. J. McMillan, A. F. Embry, and D. J. Glass, eds. Devonian of the World, Volume I, 669–703. Canadian Society of Petroleum Geologists. Calgary, Alberta, Canada.