Rio Bonito Formation

Rio Bonito Formation
Stratigraphic range: Sakmarian-Artinskian
Type	Geological formation
Unit of	Guata Group, Paraná Basin
Underlies	Irati Formation (Paraná Basin) Palermo Formation (Pelotas Basin)
Overlies	Itararé Group (Paraná Basin) Pelotas Batholith & Dom Feliciano Belt (Pelotas Basin)
Lithology
Primary	Sandstone
Location
Coordinates	25°18′S 50°30′W / 25.3°S 50.5°W / -25.3; -50.5
Approximate paleocoordinates	45°42′S 29°24′W / 45.7°S 29.4°W / -45.7; -29.4
Region	São Paulo, Paraná, Santa Catarina, Rio Grande do Sul and Uruguay
Country	Brazil  Uruguay
Rio Bonito Formation (Brazil)

The Rio Bonito Formation is a geological formation of the Paraná and Pelotas Basins of Permian age. It is represented by a succession of cyclic sedimentary packages of sandstones, siltstones and shales which bear extensive deposits of coal that has been extracted since the 19th century.^[1] The Rio Bonito Formation was deposited in a coastal environment, formed by rivers, deltas, bays and estuaries with tidal plains, barrier islands and shallow marine platform, at a time when the Paraná Basin was a large gulf of the ancient supercontinent Gondwana. This gulf was open to the southwest, to the old ocean Panthalassa. The Rio Bonito Formation outcrops occur mainly in the eastern border of the Paraná Basin, in a narrow band in the states of São Paulo, Paraná, Santa Catarina, Rio Grande do Sul and Uruguay.^[2] The Rio Bonito Formation belongs to the second-order stratigraphic supersequence called Gondwana I.^[3]

The Glossopteris flora is characteristic of fossil sequences of the Gondwana supercontinent; it developed and became the dominant flora of the southern Permian to early Triassic, and became extinct at the end of that period. This flora is not only the main fossil content of the Rio Bonito Formation coals, the coal extracted as in Australia and South Africa's first work to record the occurrence of horizons megaflora associated with coal seams within a paleogeographic approach and palaeoclimatic in the Paraná Basin, was the study by White in 1908. This allowed a large correlation between Gondwana coal deposits in southern Brazil and those registered in South Africa, Australia, India and Antarctica, including showing that the latter has been in latitude near the south pole less than today, allowing the occurrence of an extensive flora.

Among others, the following fossil flora have been recovered from the formation:^[4]