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Cerro Fortaleza Formation
Geological formation in Argentina From Wikipedia, the free encyclopedia
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The Cerro Fortaleza Formation, in older literature described as Pari Aike Formation, is a Late Cretaceous geologic formation of Campanian to Maastrichtian age[1][2] (although it has formerly been reported to be Cenomanian to Santonian)[3] of the Austral Basin in southern Patagonia, Argentina.
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Description
The sandstones of the formation were deposited in a fluvial environment. The formation has an estimated thickness of 460 metres (1,510 ft) and overlies the Anita Formation, while it is overlain by the La Irene Formation.[4] These formations are considered Campanian and Maastrichtian in age, respectively,[4][3] making the Cerro Fortaleza Formation aged between them.
Paleobiota
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The giant titanosaurs Puertasaurus and Dreadnoughtus, the megaraptoran Orkoraptor, the berthasaurid Austrocheirus isasii, and the ornithopod Talenkauen have been recovered from the formation alongside turtles and crocodiles.[5][6][7]
Dinosaurs
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Notes Uncertain or tentative taxa are in small text; |
Ornithischians
Sauropods
Theropods
Fish
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