Marree Subgroup | |
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Stratigraphic range: Aptian-Albian[1] | |
Type | Subgroup |
Unit of | Rolling Downs Group |
Sub-units | Bellinger Sandstone, Bulldog Shale, Coorikiana Sandstone, Oodnadatta Formation |
Underlies | Mackunda & Winton Formations |
Overlies | Parabarana Sandstone, Cadna-owie Formation |
Lithology | |
Primary | Siltstone |
Other | Gravel, conglomerate, shale, clay |
Location | |
Coordinates | 30°26′0″S 137°10′0″E / 30.43333°S 137.16667°E |
Approximate paleocoordinates | 57°06′S 117°18′E / 57.1°S 117.3°E |
Region | South Australia |
Country | Australia |
Extent | Eromanga Basin |
Type section | |
Named for | Marree |
Named by | Forbes |
Year defined | 1966 |
The Marree Subgroup, previously described as Maree Formation and Marree Formation, is a geological subgroup in the Eromanga Basin of South Australia whose strata date back to the Aptian. The subgroup was first described as a formation by Forbes in 1966.[2][3] Dinosaur remains are among the fossils that have been recovered from the formation.[1]
An opalised plesiosaur specimen of the genus Umoonasaurus has been nicknamed 'Eric' and was described in 1998 by Schroeder.[4] The decapod crab Dioratiopus salebrosus was described in 1980.[5]