The formation is present in the Northern Territory, Queensland, South Australia, and New South Wales. It is a sedimentary unit, principally made up of mudstone and siltstone, with calcareous concretions. Its maximum thickness is 600 metres. Its age is somewhere from Aptian to Albian, that is between 113 and 98 Mya. The formation is part of the Wilgunya Sibgroup, which in turn is part of the Rolling Downs Group of the Eromanga and Surat Basins. The named beds are: Coreena, Doncaster, Jones Vally, Ranmoor, and Trimble Members.
|Placeholders of the Placeholder Formation|
|Notopala Cotton, 1935||† Notopala albascopularis (Etheridge, 1902)||White Cliffs, New South Wales||the oldest freshwater snail in Australia|
- Geoscience Australia: Stratigraphic Units Database
- Kear B. P., Hamilton-Bruce R. J., Smith B. J. & Gowlett-Holmes K. L. (2003). "Reassessment of Australia's oldest freshwater snail, Viviparus (?) albascopularis Etheridge, 1902 (Mollusca : Gastropoda : Viviparidae), from the Lower Cretaceous (Aptian, Wallumbilla Formation) of White Cliffs, New South Wales". Molluscan Research 23(2): 149-158. doi:10.1071/MR03003, PDF.
|This article about a specific stratigraphic formation is a stub. You can help Wikipedia by expanding it.|