| 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]