Cajones Formation
The Cajones Formation is a Turonian geologic formation of central Bolivia. The fluvial sandstones in Amboró National Park preserve fossils of Yacarerani boliviensis.[1][2] The formation is correlated with the Adamantina Formation of the Paraná Basin in Brazil and the Bajo de la Carpa Formation of the Neuquén Basin in Patagonia, Argentina.[3]
Cajones Formation Stratigraphic range: Turonian ~94–85 Ma | |
---|---|
Type | Geological formation |
Lithology | |
Primary | Sandstone |
Location | |
Coordinates | 17.6°S 63.9°W |
Approximate paleocoordinates | 23.4°S 41.5°W |
Region | Santa Cruz Department |
Country | Bolivia |
Extent | Cordillera Oriental |
Type section | |
Named for | Cajones de Ichilo River |
Cajones Formation (Bolivia) |
See also
References
- Novas et al., 2009, p.1316
- Amboro National Park at Fossilworks.org
- Novas et al., 2009, p.1319
Bibliography
- Novas, F.E.; D.F. Pais; D. Pol; I.S. Carvalho; A. Scanferla; A. Mones, and M.S. Riglos. 2009. Bizarre notosuchian crocodyliform with associated eggs from the Upper Cretaceous of Bolivia. Journal of Vertebrate Paleontology 29. 1316–1320. Accessed 2019-03-03.
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