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botucatu+formation Latitude and Longitude:

29°42′S 52°24′W / 29.7°S 52.4°W / -29.7; -52.4
From Wikipedia, the free encyclopedia
Botucatu Formation
Stratigraphic range: Aptian
Type Geological formation
Unit of São Bento Group
Underlies Serra Geral Formation
Overlies Rio do Rasto Formation
Lithology
Primary Sandstone
Location
Coordinates 29°42′S 52°24′W / 29.7°S 52.4°W / -29.7; -52.4
Approximate paleocoordinates 30°36′S 19°30′W / 30.6°S 19.5°W / -30.6; -19.5
Region Rio Grande do Sul
Country  Brazil
  Uruguay
Extent Paraná & Pelotas Basins
Type section
Named for Botucatu

Geologic map of the Paraná Basin with the Paleozoic and Mesozoic units in light blue

The Botucatu Formation is an Aptian geologic formation of the Paraná and Pelotas Basins in southern Brazil and northern Uruguay. The formation is composed of quartzitic sandstones, deposited in an eolian environment. [1] Fossil theropod tracks have been reported from the formation. [2]

Description

The sandstone is fine-textured and well sorted, containing no pebbles; its colour is occasionally white, yellowish, and reddish, but more commonly it is pinkish. Nearly always it is silicified and therefore compact and hard. [3] The formation was deposited in an arid desert environment, characterized by sabkhas and wadis. [4]

Fossil content

Among the following fossils were reported from the Botucatu Formation: [3]

Ichnofossils

See also

References

  1. ^ Petrolli & Pimentel, 2014, p.1
  2. ^ Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
  3. ^ a b São Bento quarry, Araraquara at Fossilworks.org
  4. ^ a b Leonardi, 1994, p.50
  5. ^ Leonardi, Giuseppe; Fernandes, Marcelo Adorna; Carvalho, Ismar de Souza; Schutzer, Julia Beatrice; Silva, Rafael Costa da (2023-09-30). "Farlowichnus rapidus new ichnogen., new ichnosp.: A speedy and small theropod in the Early Cretaceous Botucatu paleodesert (Paraná Basin), Brazil". Cretaceous Research. 153: 105720. doi: 10.1016/j.cretres.2023.105720. ISSN  0195-6671.

Bibliography

Further reading

  • Leonardi, G. 1989. Inventory and statistics of the South American dinosaurian ichnofauna and its paleobiological interpretation. In D. D. Gillette & M. G. Lockley (ed.), Dinosaur Tracks and Traces 165–178.
  • Leonardi, G. 1980. On the discovery of an abundant ichno-fauna (vertebrates and invertebrates) in the Botucatu Formation s.s. in Araraquara, São Paulo, Brazil. Anais da Academia Brasileira de Ciências 52(3):559-567 link.
  • Leonardi, G., Carvalho, I.S., and Fernandes, M.A. 2007. The desert ichnofauna from Botucatu Formation (Upper Jurassic–Lower Cretaceous), Brazil. In: Carvalho, I.S., Cassab, R.C.T., Schwanke, C., Carvalho, M.A., Fernandes, A.C.S., Rodrigues, M.A.C., Carvalho, M.S.S., Arai, M., and Oliveira, M.E.Q. (eds.). Paleontologia: Cenários da Vida, I. Interciência, Rio de Janeiro, Brazil. p, 372–383. link.

botucatu+formation Latitude and Longitude:

29°42′S 52°24′W / 29.7°S 52.4°W / -29.7; -52.4
From Wikipedia, the free encyclopedia
Botucatu Formation
Stratigraphic range: Aptian
Type Geological formation
Unit of São Bento Group
Underlies Serra Geral Formation
Overlies Rio do Rasto Formation
Lithology
Primary Sandstone
Location
Coordinates 29°42′S 52°24′W / 29.7°S 52.4°W / -29.7; -52.4
Approximate paleocoordinates 30°36′S 19°30′W / 30.6°S 19.5°W / -30.6; -19.5
Region Rio Grande do Sul
Country  Brazil
  Uruguay
Extent Paraná & Pelotas Basins
Type section
Named for Botucatu

Geologic map of the Paraná Basin with the Paleozoic and Mesozoic units in light blue

The Botucatu Formation is an Aptian geologic formation of the Paraná and Pelotas Basins in southern Brazil and northern Uruguay. The formation is composed of quartzitic sandstones, deposited in an eolian environment. [1] Fossil theropod tracks have been reported from the formation. [2]

Description

The sandstone is fine-textured and well sorted, containing no pebbles; its colour is occasionally white, yellowish, and reddish, but more commonly it is pinkish. Nearly always it is silicified and therefore compact and hard. [3] The formation was deposited in an arid desert environment, characterized by sabkhas and wadis. [4]

Fossil content

Among the following fossils were reported from the Botucatu Formation: [3]

Ichnofossils

See also

References

  1. ^ Petrolli & Pimentel, 2014, p.1
  2. ^ Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
  3. ^ a b São Bento quarry, Araraquara at Fossilworks.org
  4. ^ a b Leonardi, 1994, p.50
  5. ^ Leonardi, Giuseppe; Fernandes, Marcelo Adorna; Carvalho, Ismar de Souza; Schutzer, Julia Beatrice; Silva, Rafael Costa da (2023-09-30). "Farlowichnus rapidus new ichnogen., new ichnosp.: A speedy and small theropod in the Early Cretaceous Botucatu paleodesert (Paraná Basin), Brazil". Cretaceous Research. 153: 105720. doi: 10.1016/j.cretres.2023.105720. ISSN  0195-6671.

Bibliography

Further reading

  • Leonardi, G. 1989. Inventory and statistics of the South American dinosaurian ichnofauna and its paleobiological interpretation. In D. D. Gillette & M. G. Lockley (ed.), Dinosaur Tracks and Traces 165–178.
  • Leonardi, G. 1980. On the discovery of an abundant ichno-fauna (vertebrates and invertebrates) in the Botucatu Formation s.s. in Araraquara, São Paulo, Brazil. Anais da Academia Brasileira de Ciências 52(3):559-567 link.
  • Leonardi, G., Carvalho, I.S., and Fernandes, M.A. 2007. The desert ichnofauna from Botucatu Formation (Upper Jurassic–Lower Cretaceous), Brazil. In: Carvalho, I.S., Cassab, R.C.T., Schwanke, C., Carvalho, M.A., Fernandes, A.C.S., Rodrigues, M.A.C., Carvalho, M.S.S., Arai, M., and Oliveira, M.E.Q. (eds.). Paleontologia: Cenários da Vida, I. Interciência, Rio de Janeiro, Brazil. p, 372–383. link.

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