Spinoaequalis
| Spinoaequalis Temporal range: Late Carboniferous,
| |
|---|---|
| |
| Restoration | |
Scientific classification 
| |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Reptilia |
| Order: | †Araeoscelidia |
| Genus: | †Spinoaequalis deBraga & Reisz, 1995 |
| Species | |
| |
Spinoaequalis is an extinct genus of diapsid reptile.
The 30 cm (1 ft) long creature, known from fossils found in Kansas, United States, was one of the first diapsids, along with Petrolacosaurus. It was also the first reptile to return to the water, evolving shortly after Hylonomus, the oldest confirmed reptile. Spinoaequalis was not fully aquatic, frequently returning to dry land. It probably swam using its laterally flattened, fanned tail. Its name means "symmetrical spine" referring to its deep, laterally compressed tail. Spinoaequalis has been found along with beautifully preserved marine fish, suggesting it occasionally left fresh water streams for the sea.
Spinoaequalis was described and named by Michael deBraga and Robert Reisz in 1995.[1]
References
[edit]- ^ deBraga, Michael; Reisz, Robert R. (1995). "A new diapsid reptile from the uppermost Carboniferous (Stephanian) of Kansas" (PDF). Palaeontology. 38 (1): 199–212. Archived from the original (PDF) on 2011-09-28.
| ||||||||||||||||||||||
| ||||||||||||||||||||||
 | This article about a prehistoric reptile is a stub. You can help Wikipedia by expanding it. |
 | This article related to a Carboniferous animal is a stub. You can help Wikipedia by expanding it. |