Caturrita Formation

The following taxa have been discovered so far in the Caturrita Formation:

These deposits of the Caturrita Formation settled out in an alluvial flood-plain.

The last two sites are close to the Cerrito hill and belong already to the Caturrita Formation.

This outcrop is located in Caturrita Formation.

And belongs to Caturrita Formation.

Remains have been found in the Caturrita Formation of the geopark of Paleorrota.

Jachaleria candelariensis occurs in the Caturrita Formation.

It belongs to the Caturrita Formation and the Santa Maria Formation.

Paleorrota is in Santa Maria Formation and Caturrita Formation.

The Caturrita Formation reaches a maximum thickness of 60 meters, but generally oscillates around values of 30 meters.

Because the Caturrita Formation consists of terrestrial sandstones, that evolution would have had its origins in a terrestrial, not coastal, habitat.

Brasilodon was found in Paleorrota (Caturrita Formation), a geopark located in Brazil.

It was recovered from the red beds of the Caturrita Formation, which is the geologic formation where similarly old dinosaurs like Saturnalia have been found.

The sediments of the Caturrita Formation belong to the upper section of the Santa Maria Supersequence.

The region has several paleontological, geological strata the Santa Maria Formation and Caturrita Formation.

The Caturrita Formation is a rock formation found in Rio Grande do Sul, Brazil.

Faxinalipterus is a genus of pterosaur from the Late Triassic Caturrita Formation of southern Brazil.

Only tree trunks with Permineralization survived into the rivers of Santa Maria Formation and Caturrita Formation.

Outcrops of the Caturrita Formation are found in the Brazilian state of Rio Grande do Sul.

The Caturrita Formation contains a biozone for tetrapods, the so-called "Ictidosauria Assemblage Zone" Ca-1.

The Caturrita Formation also hosts the stratigraphic marker level "Jachaleria" named after the dicynodont Jachaleria candelariensis.

The clayey sediments of the Alemoa Member gradually give way to the more sandy, rarely conglomeratic, Caturrita Formation, which finishes with an unconformity.

The Caturrita Formation was once regarded as a member of the stratigraphically higher Botucatu Formation or was expanded to include the Mata Sandstone.

Several specimens of Riograndia guaibensis have been found in the towns of Candelária and Faxinal do Soturno in the Caturrita Formation.

Sacisaurus (referred to in Portuguese as sacissauro) is a dinosauriform from the Late Triassic (Carnian to Norian) Caturrita Formation of southern Brazil.