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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

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Ornithischians

More information Ornithischians of the Cerro Fortaleza Formation, Taxa ...

Sauropods

More information Sauropods of the Cerro Fortaleza Formation, Taxa ...

Theropods

More information Theropods of the Cerro Fortaleza Formation, Taxa ...

Fish

More information Fish of the Cerro Fortaleza Formation, Taxa ...
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See also

References

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