Английская Википедия:Bajo de la Carpa Formation

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Шаблон:Short description Шаблон:Infobox rockunit 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 Шаблон:Convert 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

Файл:Comahuesuchus BW.jpg
Comahuesuchus brachybuccalis
Файл:Notosuchus BW.jpg
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

Шаблон:Reflist

Bibliography

Further reading

  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. Шаблон:Cite journal
  9. Filippi et al., 2018b
  10. Porfiri et al., 2018
  11. Cruzado Caballero et al., 2019
  12. Шаблон:Cite journal