Arizonasaurus
Extinct genus of reptiles

Arizonasaurus (meaning "Arizona reptile") is a genus of ctenosauriscid archosaur from the Middle Triassic (243 million years ago) Moenkopi Formation of what is now Arizona. It is known for having a large back sail formed by elongated neural spines of its vertebrae. The type and only known species is A. babbitti, named and described in 1947.
01Discovery and naming
The type species, Arizonasaurus babbitti, was named by Samuel Paul Welles in 1947 on the basis of a few teeth and a maxilla, labelled as specimen UCMP 36232. A fairly complete skeleton (~50%) was found in 2002 by Sterling Nesbitt.

02Description
Arizonasaurus had a sail made of tall neural spines. This sail was similar to those of other basal archosaurs, such as other ctenosauriscids like Ctenosauriscus, Bromsgroveia, and Hypselorhachis.
Arizonasaurus is described from two braincase specimens. Some ancestral features of these braincases are plesiomorphic for crurotarsans.
Below is a list of characteristics found by Nesbitt in 2005 that distinguish Arizonasaurus:
03Classification
Arizonasaurus was closely related to Ctenosauriscus; and, together with a few other genera, they make up Ctenosauriscidae. The ctenosauriscids were closely related to the poposaurids, as shown by a few shared derived characteristics. The pelvic girdle in Arizonasaurus unites this taxon with Ctenosauriscus, Lotosaurus, Bromsgroveia, and Hypselorhachis. Together, newly identified pseudosuchian features act as evidence that other poposauroids, such as Poposaurus, Sillosuchus, and Shuvosaurus, and ctenosauriscids form a monophyletic group that is more derived than rauisuchians.
Below is a phylogenetic cladogram simplified from Butler et al. in 2011 showing the cladistics of Archosauriformes, focusing mostly on Pseudosuchia:
| Poposauroidea |
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04Biogeography
Arizonasaurus is from the Middle Triassic Moenkopi Formation of northern Arizona. The presence of a poposauroid in the early Middle Triassic suggests that the divergence of birds and crocodiles occurred earlier than previously thought. Ctenosauriscids from the Middle Triassic allow the distribution of Triassic faunas to be more widespread, now in Europe, Asia, North America and Africa. The fauna of the Moenkopi Formation represents a stage transitional fauna between those of older and younger age.
Sources and credits
This article is adapted from the Wikipedia article “Arizonasaurus”, 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:
- Arizonasaurus babbiti.png by LiterallyMiguel, CC0
- Ctenosauriscid model.jpg by Ghedoghedo, CC BY-SA 4.0
- Arizonasaurus babbitti.jpg by Pat Holroyd, CC BY-SA 3.0
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