| Redonda Formation | |
|---|---|
| Stratigraphic range: Norian ~ | |
| Type | Formation |
| Unit of | Chinle Group |
| Sub-units | Duke Ranch, Quay, Red Peak, San Jon Creek & Wallace Ranch members |
| Underlies | Entrada Formation |
| Overlies | Bull Canyon Formation |
| Thickness | 25–425 feet (7.6–129.5 m) |
| Lithology | |
| Primary | Shale |
| Other | Limestone, sandstone |
| Location | |
| Coordinates | 34°57′54″N103°42′04″W / 34.965°N 103.701°W |
| Approximate paleocoordinates | 9°54′N43°12′W / 9.9°N 43.2°W |
| Region | New Mexico |
| Country | United States |
| Type section | |
| Named for | Redonda Mesa |
| Named by | Dobrovolny and Summerson |
| Year defined | 1946 |
The Redonda Formation is a geologic formation exposed in eastern New Mexico. [1] It contains vertebrate fossils of the late Triassic Period. [2] Fossil theropod tracks have been reported from the formation. [3]
The formation consists of interbedded fine-grained red-brown sandstone and mudstone. It conformably overlies the Bull Canyon Formation [4] and underlies the Entrada Formation. [2]
The formation is interpreted as having been deposited in a lake with an area of about 5,000 square kilometres (1,900 sq mi). [4]
The formation has few fossil plants, with only Neocalamites reported, but it contains abundant invertebrate fossils (conchostracans and ostracods) and a diverse assemblage of vertebrate fossils. [4] [3]
This section needs additional citations for verification .(September 2020) |
| fish of the Redonda Formation | ||||
|---|---|---|---|---|
| Taxa | Presence | Notes | Images | |
| Skull fragments | A redfieldiid | |||
| A lungfish | ||||
Coelacanthidae indet. | Fragmentary material | Possibly assignable to Chinlea or Quayia | ||
| scales | A dapediid | |||
| Abundant, found in large deathbeds | A semionotid | |||
| Skull fragments | A redfieldiid | |||
| Stereospondyls of the Redonda Formation | ||||
|---|---|---|---|---|
| Taxa | Presence | Notes | Images | |
| Numerous specimens | A metoposaurid, possibly juveniles of Koskinonodon | |||
| Synapsids of the Redonda Formation | ||||
|---|---|---|---|---|
| Taxa | Presence | Notes | Images | |
| teeth | ||||
| Archosauriforms of the Redonda Formation | ||||
|---|---|---|---|---|
| Taxa | Presence | Notes | Images | |
| Osteoderms | An aetosaur similar to Neoaetosauroides | |||
| Numerous skulls and other skeletal remains | ||||
| Osteoderms and other fragments | A typothoracisine aetosaur related to Typothorax | |||
| Snout bones and a scapulocoracoid | A large, predatory basal crocodylomorph | |||
| Osteoderms | An unusual non-archosaurian archosauriform | |||
The unit was first named as the Redonda Member of the Chinle Formation by Dobrovolny and Summerson in 1947. [1] Griggs and Read raised the unit to formation rank in 1959, and also assigned an age of late Triassic based on the presence of tracks of a bipedal dinosaur and of a phytosaur skull. [2]