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Redonda Formation

Geologic formation exposed in eastern New Mexico

The Redonda Formation is a geologic formation exposed in eastern New Mexico. It contains vertebrate fossils of the late Triassic Period. Fossil theropod tracks have been reported from the formation.

01Description

The formation consists of interbedded fine-grained red-brown sandstone and mudstone. It conformably overlies the Bull Canyon Formation and underlies the Entrada Formation.

The formation is interpreted as having been deposited in a lake with an area of about 5,000 square kilometres (1,900 sq mi).

Semionotus
Semionotus
Apachesaurus
Apachesaurus

02Fossils

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.

Vertebrate fauna

Fish

fish of the Redonda Formation
Taxa Presence Notes Images

Cionichthys

Skull fragments A redfieldiid

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

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

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
Redondasaurus
Redondasaurus

03History of investigation

The unit was first named as the Redonda Member of the Chinle Formation by Dobrovolny and Summerson in 1947. 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.

Vancleavea
Vancleavea
Watch videos about Redonda FormationExplainers and documentaries on YouTube (opens in a new tab)

Sources and credits

This article is adapted from the Wikipedia article Redonda Formation, written by its contributors and licensed under CC BY-SA 4.0. Fathomly has changed the layout, removed citation markers, navigation and maintenance notices, and adjusted punctuation. This adapted version is shared under the same license. For references, see the original article.

Images, from Wikimedia Commons:

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