| Bushveld Sandstone | |
|---|---|
| Stratigraphic range: Hettangian-Sinemurian ~ | |
| Type | Geological formation |
| Unit of | Stormberg Group |
| Lithology | |
| Primary | Sandstone |
| Location | |
| Coordinates | 22°48′S 29°18′E / 22.8°S 29.3°E |
| Approximate paleocoordinates | 37°54′S 4°42′E / 37.9°S 4.7°E |
| Region | Mpumalanga, Limpopo |
| Country | South Africa |
The Bushveld Sandstone is a geological formation dating to roughly between 201 and 189 million years ago and covering the Carnian to Norian stages. The Bushveld Sandstone is found in Transvaal, South Africa, and is a member of the Stormberg Group. As its name suggests, it consists mainly of sandstone. Fossils of the prosauropod dinosaur Massospondylus have been recovered from the Bushveld Sandstone.
The Bushveld Sandstone was thought to be Late Triassic age, but was considered to be temporally correlative to the Clarens Formation by Smith et al. (1993).
Dinosaur tracks are located in Transvaal.
| Dinosaurs | ||||
|---|---|---|---|---|
| Genus | Species | Presence | Notes | Images |
| Gigantoscelus | G. molengraaffi | Geographically located in Transvaal. | Remains now considered to be of indeterminate prosauropod origin. "Distal femur." | |
| Gryponyx | G. transvaalensis | Geographically located in Transvaal. | Remains now considered to be of indeterminate prosauropod origin. "Ungual, distal metatarsal." | |
| Massospondylus | M. carinatus | Geographically located in Transvaal. Geochronologically located in Early Jurassic strata. | ||
Color key
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Notes
Uncertain or tentative taxa are in small text
crossed out taxa are discredited.