Arcadia Formation, Australia
Arcadia Formation | |
---|---|
Stratigraphic range: Induan-Olenekian ~ | |
Type | Geological formation |
Unit of | Rewan Group |
Sub-units | Rewan Formation & Sagittarius Sandstone Members |
Underlies | Brumby Sandstone Member, conformity Sagittarius Sandstone |
Overlies | unconformity Glenidal Formation |
Thickness | Up to 500 m (1,600 ft) |
Lithology | |
Primary | Red mudstone, siltstone, fine grained sandstone |
Location | |
Coordinates | 24°48′S 148°00′E / 24.8°S 148.0°E |
Approximate paleocoordinates | 58°00′S 136°00′E / 58.0°S 136.0°E |
Region | Queensland |
Country | Australia |
Extent | Bowen Basin |
Type section | |
Year defined | 1988 |
The Arcadia Formation is a geological formation located within central-eastern Queensland, Australia, which has been aged between the Induan–Olenekian epoch of the Early-Triassic period. It is most well known for its abundance of Early-Triassic aged fossils, most notably its high diversity of Amphibians.
Description
The Arcadia Formation is a sequence of sandstones and mudstones deposited as a result of freshwater rivers & lakes during the Induan–Olenekian epoch. The Arcadia Formation represents one of the oldest known Mesozoic formation within the entirety of Australia, as well as it is preserving relatively well-preserved specimens for its age and country. The time at which the Arcadia Formation takes place was still recovering from the recent Permian–Triassic extinction event and as a result the global biodiversity had remained low throughout much of the lower Triassic. The world currently was generally a hot and arid environment reaching an average temperature more than 80o S. This is suggested by the red color of sediments found within the Bowen Basin.
The fauna and flora from the Formation are not abruptly unique from the known fauna or flora from the rest of the world at this time, however The Arcadia Formation has an unusually high diversity of Amphibians, with 90% of the fauna from the Arcadia Formation being made up of Amphibians. So far, the formation’s fauna is known to of been made up of brachiopods, fish, amphibians, and reptiles. There is also a high diversity of ichnotaxa based on coprolites.
Vertabrate paleofauna
Fish
Fish | ||||
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Genus | Species | Presence | Notes | Images |
Aphelodus | A. anapes | A single tooth | An Sagenodontid. | |
Namatozodia | N. pitikanta | An Incomplete skull | An Gnathorhizid. | |
Ptychoceratodus | P. phillipsi | An Sagenodontid. | ||
Actinopterygii | Indeterminate | Scales | ||
Osteichthyes | Indeterminate | Scales and coprolites | ||
Saurichthys | Indeterminate | Partial Skull |
Amphibians
Fish | ||||
---|---|---|---|---|
Genus | Species | Presence | Notes | Images |
Acerastea | A. wadeae | Partial Skeleton. | A Derwentiid. |