Irati Formation

Irati Formation Stratigraphic range: Early Permian ~278.4–270 Ma PreꞒ Ꞓ O S D C P T J K Pg N
The Irati Formation belongs to the Gondwana I megasequence
Type	Geological formation
Unit of
Underlies	(Paraná Basin) (Pelotas Basin)
Overlies
Area	1,000,000 km2 (390,000 sq mi)
Thickness	up to 80 m (260 ft)
Lithology
Primary	Black shale
Other	Sandstone
Location
Coordinates	25°30′S 50°42′W / 25.5°S 50.7°W / -25.5; -50.7Coordinates: 25°30′S 50°42′W / 25.5°S 50.7°W / -25.5; -50.7
Region	Paraná & Pelotas Basins Goiás, Mato Grosso do Sul, Mato Grosso, São Paulo, Paraná, Santa Catarina, Rio Grande do Sul
Country	Brazil
Type section
Named by	White
Year defined	1908
Approximate paleocoordinates	45°48′S 29°42′W / 45.8°S 29.7°W / -45.8; -29.7
The Paraná Basin in South America

Irati Formation is the name of a geological formation of the Paraná Basin in Brazil. It has previously been dated as Late Permian using palynomorphs, but is now dated as Early Permian using zircon ages obtained from bentonite layers. The base of the formation has been dated at 278.4 ± 2.2 Ma.^[1][2] Exposures of the Irati Formation are to be found in the South (Geopark of Paleorrota), southeastern Brazil and in the states of Goiás, Mato Grosso, São Paulo, Paraná, Santa Catarina, Rio Grande do Sul and Mato Grosso do Sul.^[1] The formation is part of the , underlying the and overlying the . The formation has been deposited in a environment.^[3] The Irati Formation, with a maximum thickness of 80 metres (260 ft), was defined and named by White in 1908.^[4]

Fossil content[]

The formation is particularly famous for the occurrences of the mesosaurs Mesosaurus tenuidiens,^[5] and Stereosternum tumidum. Other fossils found in the formation are ,^[6] and crustaceans of the genera , , , and .^[7] It is considered time equivalent to the Whitehill Formation of the Ecca Group of the Karoo Supergroup of southern Africa and the Mangrullo Formation of Uruguay.^[8]

See also[]

• Geology of Brazil
• Paleontological sites of Brazil
• Ganigobis Formation

References[]

Bibliography[]

• Da Costa, Guilherme Estevam. 2015. Fácies sedimentares e composição de folhelhos da Formação Irati (Eopermiano) da Bacia do Paraná na região de Bom Retiro, Leste de Santa Catarina, 1–67. Universidade Federal de Santa Catarina, UFSC. Accessed 2017-08-03.
• Diduch, Ana Paula. 2011. Descrição de Crustacea Malacostraca da Formação Irati, Permiano Superior, Bacia do Paraná, Brasil, 1–52. Universidade Federal do Paraná, UFPR. Accessed 2017-08-03.
• Piñeiro, G.; A. Ramos; C.S. Goso; F. Scarabino, and M. Laurin. 2012. Unusual Environmental Conditions Preserve a Permian Mesosaur-Bearing Konservat-Lagerstätte from Uruguay. Acta Palaeontologica Polonica 57. 1–299.
• Ventura Santos, Roberto; Paulo A. Souza; Carlos José Souza de Alvarenga; Elton Luiz Dantas; Marcio Martins Pimentel; Claudinei Gouveia de Oliveira, and Laury Medeiros de Araújo. 2006. [ Shrimp U–Pb zircon dating and palynology of bentonitic layers from the Permian Irati Formation, Paraná Basin, Brazil]. Gondwana Research 9. 456–463. Accessed 2017-08-03.