Adamantina Formation

Eggs of Bauruoolithus were described in 2011 from the Adamantina Formation.

Campinasuchus is the fifth baurusuchid species from the Adamantina Formation to date.

The Adamantina Formation is part of the larger Bauru Basin, from which several other notosuchians have been found.

The Adamantina Formation is part of the Bauru Group of geologic formations.

Based on the types of deposits in the Adamantina Formation, Stratiotosuchus most likely lived alongside a river system with many small ephemeral lakes.

The Adamantina Formation is a geological formation in Brazil whose strata date back to the Late Cretaceous.

The Adamantina Formation, which is Turonian to Santonian in age, was deposited in semi-arid conditions around 95 million years ago.

It is known from the Turonian-Santonian Adamantina Formation of the Bauru Basin of Brazil.

See Adamantina Formation, Uberaba Formation and Marília Formation.

The first bone remains were found and collected in 1995 by Brazilian paleontologist William Nava, in red rocks from Adamantina Formation.

They come from the upper part of the Adamantina Formation, indicating a Late Cretaceous (possibly Campanian/Maastrichtian) age.

In 2011, fossilized eggs were described from the Late Cretaceous Adamantina Formation of Brazil that may have been laid by a baurusuchid, most probably Baurusuchus.

Morrinhosuchus is an extinct genus of notosuchian crocodyliform from the Late Cretaceous Adamantina Formation of Brazil.

Yacarerani presents similar teeth morphology to Adamantinasuchus navae, a crocodylomorph from Adamantina Formation, Bauru Group, Brazil.

Baurusuchus lived during the Turonian to Santonian stages (90-83.5 million years ago) of the Late Cretaceous Period, in Adamantina Formation, Brazil.

Its relatives include the similarly-sized Stratiotosuchus from the Adamantina Formation, and Pabweshi, from the Pakistani Pab Formation.

It was collected from the Adamantina Formation of the Bauru Basin, which dates to the Campanian and Maastrichtian stages of the Late Cretaceous.

While many small carnivorous crocodyliforms are known from the Adamantina Formation, Stratiotosuchus and Baurusuchus are believed to have been the only large carnivores the Adamantina ecosystem.

Physa mezzalirai dates from the Senonian (Upper Cretaceous) of the Adamantina Formation (Bauru Group), in São Paulo state, Brazil.

The teeth at the back of the jaw are bulbous in shape and circular in cross-section (this shape is only found in one other notosuchian, Mariliasuchus, also from the Adamantina Formation).

The Adamantina Formation was divided in Vale do Rio do Peixe, São José do Rio Preto and Presidente Prudente formations.

This skeleton and all other specimens of Stratiotosuchus come from the Adamantina Formation, which is either Turonian-Santonian in age (about 85 million years old) or Campanian-Maastrichtian in age (about 70 million years old).

Campinasuchus is known from four partial skulls from the Honorópolis District of the Adamantina Formation, Bauru Basin, dating to the Turonian or the Santonian stage of the late Cretaceous, about 93.5-83.5 million years ago.

The genus Adamantisaurus is named after the Adamantina Formation in the Brazilian state of São Paulo, where the fossil was found and also incorporates the Greek word sauros meaning 'lizard', the most common suffix used in dinosaur names.

It is known from the holotype MN 7230-V, an isolated left maxilla with partially preserved teeth, which was found in the Upper Cretaceous Adamantina Formation, part of the Bauru Group of São Paulo State, southeast Brazil.