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Bauru Group

Coordinates: 19°42′S 48°00′W / 19.7°S 48.0°W / -19.7; -48.0
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Bauru Group
Stratigraphic range: Late Cretaceous (Coniacian-Maastrichtian)
~89–66 Ma
TypeGroup
Unit ofBauru Sub-basin
Sub-unitsAraçatuba, Adamantina, Uberaba, Marília, Vale do Rio do Peixe, Cambambe, São José do Rio Preto & Presidente Prudente Formations
UnderliesAlluvium
OverliesCaiuá Group
Lithology
PrimarySandstone
OtherConglomerate, siltstone, mudstone, coal
Location
Coordinates19°42′S 48°00′W / 19.7°S 48.0°W / -19.7; -48.0
Approximate paleocoordinates24°24′S 29°12′W / 24.4°S 29.2°W / -24.4; -29.2
RegionMinas Gerais, São Paulo, General Salgado, Itapecuru-Mirim, Mato Grosso
Country Brazil
ExtentParaná Basin
Type section
Named forBauru
Bauru Group is located in Brazil
Bauru Group
Bauru Group (Brazil)

The Bauru Group is a geological group of the Bauru Sub-basin, Paraná Basin in Minas Gerais, São Paulo, General Salgado, Itapecuru-Mirim, Mato Grosso, Brazil whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.[1]

Subdivisions

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According to a 2016 study:[2]

The Bauru Basin covers an area of approximately 379.362 km2 located almost exclusively in Brazil.., with selected outcrops in Northeastern Paraguay (Fúlfaro, 1996). This Cretaceous sedimentary succession reflects changing nonmarine environments, such as eolian, lacustrine, fluvial and alluvial fans.

The Bauru Group was divided by Fernandes and Coimbra (1996) in four formations, namely Adamantina, Uberaba, Araçatuba and Marília.[3] In 1998, Fernandes revised the group and recognize six formations, Uberaba, Vale do Rio do Peixe, Araçatuba, São José do Rio Preto, Presidente Prudente and Marília.[4] The Adamantina Formation was divided in Vale do Rio do Peixe, São José do Rio Preto and Presidente Prudente Formations.[4]

Vertebrate paleofauna

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Molluscan paleofauna

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Gastropoda

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Bivalvia

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See also

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References

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  1. ^ Weishampel, David B. (2004). "Dinosaur distribution (Late Cretaceous, South America)". In Weishampel, David B.; Dodson, Peter; Osmólska, Halszka (eds.). The Dinosauria (2nd ed.). University of California Press. pp. 600–604. ISBN 0-520-24209-2.
  2. ^ Costa Menegazzoa, Mirian; Catuneanu, Octavian; Chang, Hung Kiang (2016). "The South American retroarc foreland system: The development of the Bauru Basin in the back-bulge province". Marine and Petroleum Geology. 73: 131–156. Bibcode:2016MarPG..73..131M. doi:10.1016/j.marpetgeo.2016.02.027. hdl:11449/165168. Retrieved November 28, 2021. The fossil record indicates that sediment accumulated from the Cenomanian to early Paleocene, beginning after the Mochica Phase of the Andean orogeny.
  3. ^ Fernandes, L.A.; Coimbra, A.M.A (1996). "Bacia Bauru (Cretáceo Superior, Brasil)". Anais da Academia Brasileira de Ciências. 68 (2): 195–205.
  4. ^ a b Fernandes, L.A. & Coimbra, A.M. (2000a). "Revisão estratigráfica da parte oriental da Bacia Bauru (Neocretáceo)". Revista Brasileira de Geociências. 30 (4): 717–728. doi:10.25249/0375-7536.2000304717728 (inactive 1 November 2024).{{cite journal}}: CS1 maint: DOI inactive as of November 2024 (link)
  5. ^ a b c d e f g h i j Simone, L.R.L. & Mezzalira, S. 1994. Fossil Molluscs of Brazil. Boletim do Instituto Geológico 11: 1–202.
  6. ^ Ghilardi, RP; Carbonaro, FA; & Simone, LRL. 2011. Physa mezzalirai, a new cretaceous basommatophoran from Adamantina formation, Brazil. Strombus 18(1-2): 1-14. "Strombus online". Archived from the original on 2012-10-26. Retrieved 2012-07-17.