Cerro Barcino Formation
Template:Short description Script error: No such module "Infobox".Script error: No such module "check for unknown parameters". The Cerro Barcino Formation (also known as the Gorro Frigio Formation) is a geological formation in South America whose strata span the Early Cretaceous to the earliest Late Cretaceous. The top age for the formation has been estimated to be Cenomanian. Earlier estimates placed the formation until the Campanian.[1]
The formation was deposited in the Cañadón Asfalto Basin, a rift basin that started forming in the earliest Jurassic. Dinosaur remains are among the fossils that have been recovered from the formation.
The Cerro Barcino Formation is the second-youngest unit of the Chubut Group, which also includes the older Los Adobes Formation. Both formations cover a vast area in Chubut Province, Argentina. The two formations are distinguished by geological features suggesting a distinct change in climate, from a wetter, flood plain environment in the Los Adobes to a much more arid, desert-like environment in the Cerro Barcino.[1]
The Cerro Barcino Formation is subdivided into several subunits (members).[1] From oldest to youngest:
- Bayo Overo (Correlates with both the Puesto La Paloma and the Cerro Castaño members)
- Puesto La Paloma
- Characterized by arid plains interspersed with sand dunes
- Cerro Castaño
- A return to more humid, flood-plain conditions
- Las Plumas
The Puesto La Paloma Member dates from ~118-113 Ma, the Cerro Castaño Member dates from ~113-100.5 Ma, correlating with the Albian, and the Las Plumas Member dates from ~100.5-98 Ma.[2]
Fossil content
Possible rebbachisaurid remains are known from the La Paloma Member.[1][2]
Lepidosaurs (Kaikaifilusaurus minimus and Priosphenodon minimus) and testudinatans (Chubutemys copelloi and Prochelidella cerrobarcinae) are also discovered from this formation.[2]
Crurotarsans
| Crocodylomorphs | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
| Barcinosuchus[3] | B. gradilis | Near El Escorial village, Chubut Province | Cerro Castaño Member | Skull, mandible, and postcranial remains | A peirosaurid. The first crocodyliform from the Chubut Group | |
Dinosaurs
Sauropods
| Sauropods of the Cerro Barcino Formation | |||||
|---|---|---|---|---|---|
| Genus | Species | Member | Material | Notes | Images |
| Chubutisaurus[4] | C. insignis | Bayo Overo | Two partial skeletons | A basal somphospondylan | |
| Patagotitan[5] | P. mayorum | Cerro Castaño | Partial skeleton and other elements | A huge lognkosaur | |
Theropods
| Theropods of the Cerro Barcino Formation | |||||
|---|---|---|---|---|---|
| Genus | Species | Member | Material | Notes | Images |
| Abelisauroidea | Indeterminate | La Paloma member | Vertebrae | Very similar to the later and more large-bodied abelisauroids from South America such as Carnotaurus[6] | |
| Genyodectes[7] | G. serus | Cerro Castaño | Partial snout | A possible ceratosaurid | |
| "Megalosaurus" | "M." inexpectatus | Bayo Overo | Teeth | An indeterminate abelisaurid originally described as a species of Megalosaurus[8][9] | |
| Tyrannotitan[10] | T. chubutensis | Cerro Castaño | Two partial skeletons and teeth | A giant giganotosaurin carcharodontosaurid | |
See also
- List of dinosaur-bearing rock formations
- La Amarga Formation, contemporaneous fossiliferous formation of the Neuquén Basin
- Lohan Cura Formation, contemporaneous fossiliferous formation of the Neuquén Basin
- Río Belgrano Formation, contemporaneous fossiliferous formation of the Austral Basin
References
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- ↑ a b c d Rauhut et al., 2003
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- ↑ Weishampel et al., 2004, pp.563-570
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Bibliography
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- Cerro Barcino Formation
- Cretaceous Argentina
- Sandstone formations
- Mudstone formations of Argentina
- Conglomerate formations of Argentina
- Tuff formations of Argentina
- Alluvial deposits
- Fluvial deposits
- Fossiliferous stratigraphic units of South America
- Paleontology in Argentina
- Geology of Chubut Province