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Bajo Barreal Formation
Geological formations From Wikipedia, the free encyclopedia
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The Bajo Barreal Formation is a geological formation in the Golfo San Jorge Basin of Chubut and Santa Cruz, Argentina whose strata date back to the Middle Cenomanian to Late Turonian. The formation was first described by Teruggi & Rossetto in 1963.[1] The sandstones, claystones, mudstones, conglomerates and tuff were deposited in a fluvial environment.[2] The upper part of formation is laterally equivalent to the Yacimiento El Trébol and Meseta Espinosa Formation and the lower part to the Laguna Palacios, Cañadón Seco and Comodoro Rivadavia Formations. The Bajo Barreal Formation is a reservoir rock in the Golfo San Jorge Basin.[3]
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Vertebrate paleofauna
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Notes Uncertain or tentative taxa are in small text; |
Dinosaurs
Indeterminate abelisauroids and titanosaurs have been recovered from the formation.
Ornithopods
Sauropods
Theropods
- Other fossils
Other fossils found in the formation include:[16][17][18]
- Bonapartemys bajobarrealis
- Prochelidella argentinae
- Anura indet.
- Chelonia indet.
- Crocodylia indet.
- Pterosauria indet.
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See also
- List of dinosaur-bearing rock formations
- Mata Amarilla Formation, contemporaneous formation of the Austral Basin
- Lisandro Formation, contemporaneous formation of the Neuquén Basin
References
Further reading
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