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Warrenisuchus facts for kids

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Temporal range: Early Triassic, Induan
Warrenisuchus ontogenesis.jpg
Skulls at various ontogenic stages
Scientific classification e
Kingdom: Animalia
Phylum: Chordata
Order: Temnospondyli
Suborder: Stereospondyli
Clade: Capitosauria
Genus: Warrenisuchus
Maganuco et al., 2009
Type species
Warrenisuchus aliciae
(Warren and Hutchinson, 1988) (originally Parotosuchus aliciae)

Warrenisuchus is an extinct genus of temnospondyl amphibian from the Early Triassic of Queensland, Australia. It belongs to a diverse group of Triassic temnospondyls called Capitosauria. The type species Warrenisuchus aliciae was erected in 2009. W. aliciae was originally described as a species of Parotosuchus in 1988, which is known from other species that have been found in Europe, Africa, and Antarctica. In 2000 it was then assigned to a new genus called Rewanobatrachus along with the newly named species R. gunganj, which was declared the type species of the genus. However, R. gunganj was later reclassified as a species of Watsonisuchus, invalidating the name Rewanobatrachus and requiring that R. aliciae be placed in its own genus, which was named Warrenisuchus. However, several studies suggest that Warrenisuchus aliciae may be a species of Watsonisuchus as well. Unlike most capitosaurs, Warrenisuchus is known from many juvenile skulls less than 4 centimetres (1.6 in) in length.


Warrenisuchus is known from several fossil specimens. The holotype skeleton preserves most of the skull and lower jaws, the pectoral girdle, the forward-most vertebrae and ribs, and the right hind limb and the paratype specimen includes a partial skull and pectoral girdle. All known specimens of Warrenisuchus are very small; the largest skull is only 3.9 centimetres (1.5 in) long and the smallest is 1.1 centimetres (0.43 in) long (adult capitosaurs can have skulls over a meter in length). They show many characteristics of juvenile individuals such as large eye sockets, rounded heads (adult capitosaurs typically have triangular heads), loose joints between skull bones, small tabular horns, and pineal foramina close to the back of the eye sockets (as opposed to farther back on the skull table). The smallest specimens seem to represent the stage of development immediately after metamorphosis when gills have been lost and the skull bones have thickened but the vertebrae remain poorly developed.



Below is a cladogram from Maganuco et al. (2009):


Sclerothorax hypselonotus

Warrenisuchus aliciae

Edingerella madagascariensis

Watsonisuchus gunganj

Watsonisuchus magnus

Watsonisuchus rewanensis

Wetlugasaurus angustifrons

Parotosuchus orenburgensis

Stanocephalosaurus pronus


Cyclotosaurus robustus

Tatrasuchus wildi

Stenotosaurus stantonensis

Xenotosuchus africanus

Cherninia denwai

Wellesaurus peabodyi

Paracyclotosaurus davidi



Odenwaldia heidelbergensis


Mastodonsaurus giganteus

Eryosuchus garjainovi

Yuanansuchus laticeps

Quasicyclotosaurus campi


Warrenisuchus fossils are the most common components of an amphibian fauna that existed in eastern Australia during the Early Triassic. They are preserved in the Arcadia Formation, which dates back to the Induan stage. Other temnospondyl amphibians from the Arcadia Formation include rhytidosteids and brachyopoids. Another amphibian fauna existed around the same time in western Australia and includes a greater diversity of brachyopoids along with rhytidosteids, trematosaurids, and the capitosaur Edingerella, which was a close relative of Warrenisuchus.

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