| Bajada Colorada Formation | |
|---|---|
| Stratigraphic range: Late Berriasian-Early Valanginian ~ | |
| Type | Geological formation |
| Unit of | Mendoza Group |
| Underlies | Agrio Formation |
| Overlies | Quintuco & Picún Leufú Formations |
| Lithology | |
| Primary | Sandstone, conglomerate |
| Other | Siltstone, claystone |
| Location | |
| Coordinates | 39°48′S 69°42′W / 39.8°S 69.7°W |
| Approximate paleocoordinates | 38°48′S 32°12′W / 38.8°S 32.2°W |
| Region | Neuquén Province |
| Country | Argentina |
| Extent | Neuquén Basin |
| Type section | |
| Named by | Roll |
| Year defined | 1939 |
The Bajada Colorada Formation is a geologic formation of the southern Neuquén Province in the Neuquén Basin of northern Patagonia, Argentina. The formation belongs to the Mendoza Group and is late Berriasian to early Valanginian in age. The formation is renowned for preserving fossil remains of Bajadasaurus pronuspinax, a genus of dicraeosaurid dinosaurs named after the formation.
The Bajada Colorada Formation, first defined by Roll in 1939, pertains to the Mendoza Group. It overlies the Quintuco and Picún Leufú Formations and is overlain by the Agrio Formation. The contact with the Agrio Formation is discordant and the unconformity has been dated to 134 Ma. The formation is laterally equivalent with the Mulichinco Formation. The formation comprises red and greenish-brown, fine to coarse grained conglomerates and thick-bedded sandstones with well-developed bands of light brown siltstones and reddish, pinkish grey and purple-reddish claystones. The formation was deposited in a fluvial environment, and the paleoenviroment resembled a braided river system with well-preserved channels and paleosols.
X-ray diffraction studies of sediments belonging to the Bajada Colorada Formation have revealed the presence of smectite, chlorite, illite and kaolinite.
The formation has provided fossils of:
Color key
|
Notes
Uncertain or tentative taxa are in small text
crossed out taxa are discredited.
| Ornithischians of the Bajada Colorada Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
| Ankylosauria Indet. | Indeterminate | Isolated scutes | ||||
| Stegosauria Indet. | Indeterminate | Sacral vertebrae, dorsal ribs and osteoderms | ||||
| Sauropods of the Bajada Colorada Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
| Bajadasaurus | B. pronuspinax | A nearly complete skull, both proatlases, atlantal neurapophyses, axis and the ?fifth cervical vertebra. | A dicraeosaurid sauropod | |||
| Leinkupal | L. laticauda | Cervical, dorsal caudal vertebrae remains and a braincase | A diplodocine diplodocid | |||
| Ninjatitan | N. zapatai | Partial postcranial skeleton, anterior caudal vertebra of the holotype might represent diplodocoid sauropod. | A titanosaurian sauropod | |||
| Theropods of the Bajada Colorada Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
| Abelisauridae Indet. | Indeterminate | Proximal half of a left tibia | ||||
| Abelisauroidea Indet. | Indeterminate | Am almost complete axis (MMCh-PV 67) and two isolated caudal centra (MMCh-PV 76 and 77) | ||||
| Megalosauridae Indet. | Indeterminate | Dental remains | ||||
| Theropoda Indet. | Indeterminate | Dental remains | 3 different morphotypes are present. | |||