| Colalura Sandstone | |
|---|---|
|  Stratigraphic range: middle Bajocian  ~  | |
| Type | Geological formation | 
| Unit of | Champion Bay Group | 
| Underlies | Bringo Shale, Newmarracarra Limestone [1] | 
| Overlies | Moonyoonooka Sandstone | 
| Thickness | Maximum 8.5 m (28 ft) | 
| Lithology | |
| Primary | Sandstone, conglomerate | 
| Other | Claystone, siltstone, shale | 
| Location | |
| Coordinates | 28°42′S114°48′E / 28.7°S 114.8°E | 
| Approximate paleocoordinates | 39°48′S57°30′E / 39.8°S 57.5°E | 
| Region | Western Australia | 
| Country | Australia | 
| Extent | Perth Basin | 
The Colalura Sandstone is a Middle Jurassic geologic formation of the Perth Basin of Western Australia. The formation overlies the Moonyoonooka Sandstone. [2]
Dinosaur remains have been recovered from the formation. [3]
Few remains of the sandstone have been assigned to a genus. Unassigned remains include rare reptilian bones such as an isolated plesiosaur vertebra and paddle. [1]
| Vertebrates | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images | 
| Ozraptor | O. subotaii | Western Australia | The distal end of a tibia [1] [3] | The single bone is of a questionable theropod identity. [4] | ||
| Sauropoda | Indeterminate | Caudal vertebra | ||||
Petrified wood is very common in the Colalura Sandstone. [1]