| Wallumbilla Formation | |
|---|---|
|
Stratigraphic range:
Aptian-
Albian, ~ | |
| Type | Geological formation |
| Unit of | Rolling Downs Group |
| Sub-units | Trimble Member, Ranmoor Member, Jones Valley Member, Doncaster Member, Coreena Member |
| Underlies | Toolebuc & Griman Creek Formations |
| Overlies | Cadna-Owie & Bungil Formations |
| Thickness | 600 m (2,000 ft) |
| Lithology | |
| Primary | Mudstone, siltstone |
| Other | Sandstone, limestone |
| Location | |
| Coordinates | 20°48′S 143°42′E / 20.8°S 143.7°E |
| Approximate paleocoordinates | 60°12′S 124°24′E / 60.2°S 124.4°E |
| Region | 
New South Wales
Northern Territory
Queensland
South Australia |
| Country | 
Australia |
| Extent | Eromanga Basin |
  Wallumbilla Formation (Australia) | |
The Wallumbilla Formation is an Aptian geologic formation found in Australia. Plesiosaur and theropod remains are among the fossils that have been recovered from its strata.
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 125 and 101 Mya. The formation is part of the Wilgunya Subgroup, which in turn is part of the Rolling Downs Group of the Eromanga and Surat Basins. The named beds are the Coreena, Doncaster, Jones Valley, Ranmoor, and Trimble Members. [1]
| Paleofauna of the Wallumbilla Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
| Notopala Cotton, 1935 | † Notopala albascopularis (Etheridge, 1902) | White Cliffs, New South Wales | The oldest freshwater snail in Australia. [2] | |||
| Kronosaurus | Indeterminate | White Cliffs | A pliosaur, also found in Queensland's Toolebuc Formation and Colombia's Paja Formation | |||
| Theropoda | Indeterminate | |||||
| Platypterygius | Indeterminate | An ichthyosaur | ||||
- ^ 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.
- E. F. Riek. 1954. A second specimen of the dragon-fly Aeschnidiopsis flindersiensis (Woodward) from the Queensland Cretaceous. The Proceedings of the Linnean Society of New South Wales 79:61-62
| Wallumbilla Formation | |
|---|---|
|
Stratigraphic range:
Aptian-
Albian, ~ | |
| Type | Geological formation |
| Unit of | Rolling Downs Group |
| Sub-units | Trimble Member, Ranmoor Member, Jones Valley Member, Doncaster Member, Coreena Member |
| Underlies | Toolebuc & Griman Creek Formations |
| Overlies | Cadna-Owie & Bungil Formations |
| Thickness | 600 m (2,000 ft) |
| Lithology | |
| Primary | Mudstone, siltstone |
| Other | Sandstone, limestone |
| Location | |
| Coordinates | 20°48′S 143°42′E / 20.8°S 143.7°E |
| Approximate paleocoordinates | 60°12′S 124°24′E / 60.2°S 124.4°E |
| Region |
New South Wales
Northern Territory
Queensland
South Australia |
| Country |
Australia |
| Extent | Eromanga Basin |
Wallumbilla Formation (Australia) | |
The Wallumbilla Formation is an Aptian geologic formation found in Australia. Plesiosaur and theropod remains are among the fossils that have been recovered from its strata.
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 125 and 101 Mya. The formation is part of the Wilgunya Subgroup, which in turn is part of the Rolling Downs Group of the Eromanga and Surat Basins. The named beds are the Coreena, Doncaster, Jones Valley, Ranmoor, and Trimble Members. [1]
| Paleofauna of the Wallumbilla Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Abundance | Notes | Images |
| Notopala Cotton, 1935 | † Notopala albascopularis (Etheridge, 1902) | White Cliffs, New South Wales | The oldest freshwater snail in Australia. [2] | |||
| Kronosaurus | Indeterminate | White Cliffs | A pliosaur, also found in Queensland's Toolebuc Formation and Colombia's Paja Formation | |||
| Theropoda | Indeterminate | |||||
| Platypterygius | Indeterminate | An ichthyosaur | ||||
- ^ 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.
- E. F. Riek. 1954. A second specimen of the dragon-fly Aeschnidiopsis flindersiensis (Woodward) from the Queensland Cretaceous. The Proceedings of the Linnean Society of New South Wales 79:61-62