Mackunda Formation

Mackunda Formation
Stratigraphic range: Late Albian ~105.3–99.7  Ma PreꞒ Ꞓ O S D C P T J K Pg N
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″S142°08′30″E / 22.73417°S 142.14167°E / -22.73417; 142.14167
Approximate paleocoordinates	52°54′S132°00′E / 52.9°S 132.0°E / -52.9; 132.0
Region	Queensland
Country	Australia
Extent	Eromanga Basin
Mackunda Formation (Australia)

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	Materials	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]	An iguanodontian hadrosaur.

See also

• List of dinosaur-bearing rock formations

References

1. 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.
2. "Mackunda Formation". Australian Stratigraphic Units Database, Geoscience Australia. Retrieved 2019-10-06.
3. 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. Bibcode:2010JVPal..30.1747F. doi:10.1080/02724634.2010.521929. S2CID   128479527.
4. Bartholomai, A. (1966). "Fossil footprints in Queensland". Australian Natural History. 15 (5): 147–150.
5. "Table 19.1," in Weishampel, et al. (2004). Page 416.