Colalura Sandstone
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′S 114°48′E / 28.7°S 114.8°E |
Approximate paleocoordinates | 39°48′S 57°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]
Vertebrate paleofauna
[edit]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 |
Flora
[edit]Petrified wood is very common in the Colalura Sandstone.[1]
See also
[edit]References
[edit]- ^ a b c d Long, J.A.; Molnar, R.E. (1998). "A new Jurassic theropod dinosaur from Western Australia" (PDF). Records of the Western Australian Museum. 19: 121–129.
- ^ "Australian Stratigraphic Units Database, Geoscience Australia".
- ^ a b Weishampel, David B.; Dodson, Peter; Osmólska, Halszka, eds. (6 November 2004). The Dinosauria (Second Ed.). University of California Press. pp. 1–861. ISBN 978-0-520-24209-8.
- ^ Rahut, O.W.M. (2005). "Osteology and Relationships of a New Theropod Dinosaur from the Middle Jurassic of Patagonia" (PDF). Palaeontology. 48 (1): 87–110. Bibcode:2005Palgy..48...87R. doi:10.1111/j.1475-4983.2004.00436.x.