Earth:Mackunda Formation
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| Mackunda Formation Stratigraphic range: Late Albian ~105.3–99.7 Ma | |
|---|---|
| Type | Geological formation |
| Unit of | Rolling Downs Group |
| Underlies | Winton Formation |
| Overlies | Allaru Formation |
| Thickness | Up to 275 m (902 ft) |
| Lithology | |
| Primary | Sandstone, siltstone, shale, marl |
| Location | |
| Coordinates | [ ⚑ ] : 22°44′03″S 142°08′30″E / 22.73417°S 142.14167°E |
| Paleocoordinates | [ ⚑ ] 52°54′S 132°00′E / 52.9°S 132.0°E |
| Region | |
| Country | |
| Extent | Eromanga Basin |
The Mackunda Formation is a geological formation in Queensland, Australia whose strata date back to the Early Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.[1] It consists primarily of interbedded and cross bedded greensand, with variably calcareous shale, with local ferricrete.[2]
Vertebrate paleofauna
| Archosaurs | ||||
|---|---|---|---|---|
| Genus | Species | Presence | Notes | Images |
| Ctenochasmatoidea[3] | Indeterminate | Queensland, Australia.[3] | ||
| Iguanodontidae[4] | Indeterminate | Queensland, Australia.[4] | ||
| Muttaburrasaurus[1] | M. langdoni | Queensland, Australia.[1] | "Skull and postcrania, fragmentary skeleton."[5] | |
See also
- List of dinosaur-bearing rock formations
References
- ↑ 1.0 1.1 1.2 Weishampel, David B; et al. (2004). "Dinosaur distribution (Early Cretaceous, Australasia)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 573-574. ISBN 0-520-24209-2.
- ↑ "Mackunda Formation". https://asud.ga.gov.au/search-stratigraphic-units/results/10952.
- ↑ 3.0 3.1 Fletcher, T. L.; Salisbury, S. W. (2010). "New pterosaur fossils from the Early Cretaceous (Albian) of Queensland, Australia". Journal of Vertebrate Paleontology 30 (6): 1747–1759. doi:10.1080/02724634.2010.521929. Bibcode: 2010JVPal..30.1747F.
- ↑ 4.0 4.1 Bartholomai, A. (1966). "Fossil footprints in Queensland". Australian Natural History 15 (5): 147–150.
- ↑ "Table 19.1," in Weishampel, et al. (2004). Page 416.

