Earth:Bajo de la Carpa Formation

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Short description: Geological formation in Argentina
Bajo de la Carpa Formation
Stratigraphic range: Mid-Late Santonian
~86–83 Ma
TypeGeological formation
Unit ofNeuquén Group
 Río Colorado Subgroup
UnderliesAnacleto Formation
OverliesRío Neuquén Subgroup
 Plottier Formation
ThicknessUp to 150 m (490 ft)
Lithology
PrimarySandstone
OtherMudstone, siltstone, paleosol
Location
Coordinates [ ⚑ ] : 38°48′S 68°48′W / 38.8°S 68.8°W / -38.8; -68.8
Paleocoordinates [ ⚑ ] 43°24′S 49°48′W / 43.4°S 49.8°W / -43.4; -49.8
RegionNeuquén & Río Negro Provinces
CountryArgentina
ExtentNeuquén Basin
Bajo de la Carpa Formation is located in Argentina
Bajo de la Carpa Formation
Bajo de la Carpa Formation (Argentina)

The Bajo de la Carpa Formation is a geologic formation of the Neuquén Basin that crops out in northern Patagonia, in the provinces of Río Negro and Neuquén, Argentina . It is the oldest of two formations belonging to the Río Colorado Subgroup within the Neuquén Group. Formerly, that subgroup was treated as a formation, and the Bajo de la Carpa Formation was known as the Bajo de la Carpa Member.[1]

At its base, this formation conformably overlies the Plottier Formation of the older Río Neuquén Subgroup, and it is in turn overlain by the Anacleto Formation, the youngest and uppermost formation of the Neuquén Group.[2][3]

The Bajo de la Carpa Formation can reach 150 metres (490 ft) in thickness in some locations, and consists mainly of sandstones of various colors, all of fluvial origin, with thin layers of mudstone and siltstone in between. Geological features such as geodes, chemical nodules, impressions of raindrops, and paleosols (fossil soils) are commonly found in this formation as well.[1][3]

Fossil content

Comahuesuchus brachybuccalis
Notosuchus terrestris

Vertebrate fossils are abundant within the Bajo de la Carpa Formation:

Small nests with eggs inside, found in this formation, probably belonged to the bird Neuquenornis.[3] Fossil wasp nests have also been found in these rocks.[1][3]

See also

References

  1. 1.0 1.1 1.2 Sánchez et al., 2006
  2. Fossa Mancini et al., 1938
  3. 3.0 3.1 3.2 3.3 3.4 Leanza et al., 2004
  4. Martinelli et al., 2012
  5. Lio et al., 2018
  6. Filippi et al., 2018a
  7. Coria et al., 2019
  8. Filippi, Leonardo S.; Juárez Valieri, Rubén D.; Gallina, Pablo A.; Méndez, Ariel H.; Gianechini, Federico A.; Garrido, Alberto C. (2023). "A rebbachisaurid-mimicking titanosaur and evidence of a Late Cretaceous faunal disturbance event in South-West Gondwana" (in en). Cretaceous Research. doi:10.1016/j.cretres.2023.105754. ISSN 0195-6671. 
  9. Filippi et al., 2018b
  10. Porfiri et al., 2018
  11. Cruzado Caballero et al., 2019
  12. Rozadilla, Sebastián; Agnolín, Federico; Manabe, Makoto; Tsuihiji, Takanobu; Novas, Fernando E. (September 2021). "Ornithischian remains from the Chorrillo Formation (Upper Cretaceous), southern Patagonia, Argentina, and their implications on ornithischian paleobiogeography in the Southern Hemisphere". Cretaceous Research 125: 104881. doi:10.1016/j.cretres.2021.104881. ISSN 0195-6671. Bibcode2021CrRes.12504881R. 

Bibliography

Further reading