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]

Description

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]

Fossils

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]

Vertebrate fauna

Fish

fish of the Redonda Formation
Taxa Presence Notes Images

Cionichthys

Skull fragments A redfieldiid
Semionotus

Ceratodus

A lungfish

Coelacanthidae indet.

Fragmentary material Possibly assignable to Chinlea or Quayia

Hemicalypterus

scales A dapediid

Semionotus

Abundant, found in large deathbeds A semionotid

Synornichthys

Skull fragments A redfieldiid

Stereospondyls

Stereospondyls of the Redonda Formation
Taxa Presence Notes Images

Apachesaurus

Numerous specimens

A metoposaurid, possibly juveniles of Koskinonodon

Apachesaurus

Synapsids

Synapsids of the Redonda Formation
Taxa Presence Notes Images

Redondagnathus

teeth

A trirachodontid cynodont

Archosauriforms

Archosauriforms of the Redonda Formation
Taxa Presence Notes Images

Apachesuchus

Osteoderms

An aetosaur similar to Neoaetosauroides

Redondasaurus
Vancleavea

Redondasaurus

Numerous skulls and other skeletal remains

A phytosaur

Redondasuchus

Osteoderms and other fragments

A typothoracisine aetosaur related to Typothorax

Redondavenator

Snout bones and a scapulocoracoid

A large, predatory basal crocodylomorph

Vancleavea

Osteoderms An unusual non-archosaurian archosauriform

History of investigation

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]

See also

References

  1. ^ a b Dobrovolny and Summerson 1947
  2. ^ a b c Griggs and Read 1959
  3. ^ a b Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
  4. ^ a b c Lucas and Hunt 1989

Bibliography

  • Dobrovolny, Ernest; Summerson, C.H. (1947). "Geology of northwestern Quay County, New Mexico". U.S. Geological Survey Oila Nd Gas Investigations Map. OM-62. doi:10.3133/om62.
  • Griggs, R.L.; Read, C.B. (1959). "Revisions in Stratigraphic Nomenclature in Tucumcari-Sabinoso Area, Northeastern New Mexico: GEOLOGICAL NOTES". AAPG Bulletin. 43 (8): 2003–2007. doi:10.1306/0BDA5E8E-16BD-11D7-8645000102C1865D.
  • Lucas, S.G.; Hunt, A.P. (1989). "Revised Triassic stratigraphy in the Tucumcari basin, east-central New Mexico". In Lucas, S.G.; Hunt, A.P. (eds.). Dawn of the age of dinosaurs in the American southwest. New Mexico Museum of Natural History and Science. pp. 150–170. Retrieved 17 September 2020.
  • Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.
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