Earth:Huitrera Formation

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Short description: Geological formation in Argentina
Huitrera Formation
Stratigraphic range: Early Eocene (Casamayoran)
54.69–53.79 Ma
TypeGeological formation
UnderliesCollón Curá Formation
OverliesAngostura Colorada Formation
ThicknessUp to 1,300 m (4,300 ft)
Lithology
PrimaryMudstone, sandstone
OtherAndesites, dacitic & rhyolitic ignimbrites, volcanic breccias, tuffs & trachybasalts
Location
Coordinates [ ⚑ ] : 41°00′S 71°12′W / 41.0°S 71.2°W / -41.0; -71.2
Paleocoordinates [ ⚑ ] 43°30′S 61°12′W / 43.5°S 61.2°W / -43.5; -61.2
RegionNeuquén & Río Negro Provinces
CountryArgentina
ExtentNeuquén Basin
Type section
Named forCerro Huitrera
Named byRavazzoli & Sesana
Year defined1977
Huitrera Formation is located in Argentina
Huitrera Formation
Huitrera Formation (Argentina)

The Huitrera Formation is a geological formation in the Neuquén Basin in northern Patagonian Argentina whose strata date back to the Early Eocene of the Paleogene, or Casamayoran in the South American land mammal age classification.

The formation is together with the Reyhuau basalts part of the Pilcaniyeu Belt, a volcanic belt active in Paleocene to middle Eocene times.[1]

Description

The Huitrera Formation was first defined by Ravazzoli and Sesana in 1977. The name has been used to identify various volcaniclastic sequences, among others in the Ñirihuau fold-and-thrust belt.[2] The up to 1,300 metres (4,300 ft) thick formation comprises mudstones and sandstones deposited in a crater lake environment. Part of the formation comprises andesites, dacitic and rhyolitic ignimbrites, volcanic breccias, tuffs and trachybasalts.[3]

The formation was initially described as Late Eocene to Early Oligocene, but was later dated to 54.24 ± 0.45 Ma, meaning the Huitrera Formation is Ypresian, or in the SALMA classification, Casamayoran in age.

Fossil content

The following macrofossils were reported from the formation:[4]

The formation has also provided many pollen, analyzed in 2003 by Melendi et al.[12]

See also

References

  1. Fernández Paz et al., 2020
  2. Escosteguy & Franchi, 2010, p.420
  3. Prez & Massafero, 2013, p.228
  4. Huitrera Formation at Fossilworks.org
  5. Degrange, F. J.; Pol, D.; Puerta, P.; Wilf, P. (2021). "Unexpected larger distribution of Paleogene stem-rollers (Aves, Coracii): new evidence from the Eocene of Patagonia, Argentina". Scientific Reports 11 (1): Article number 1363. doi:10.1038/s41598-020-80479-8. PMID 33446824. 
  6. Báez & Pugener, 2003
  7. Aranciaga et al., 2019
  8. Jin et al., 2020
  9. Ramírez et al., 2016
  10. Jud et al., 2018
  11. Barrera et al., 2012
  12. Melendi et al., 2003

Bibliography

  • Fernández Paz, Lucía; Iannelli, Sofía B.; Echaurren, Andrés; Ramos, Miguel; Bechis, Florencia; Litvak, Vanesa D.; Encinas, Alfonso; Kasemann, Simone et al. (2020). "The late Eocene–early Miocene El Maitén Belt evolution: Magmatic response to the changing subduction zone geodynamics". Journal of South American Earth Sciences 103. doi:10.1016/j.jsames.2020.102713. http://rid.unrn.edu.ar/bitstream/20.500.12049/7023/1/Fern%c3%a1ndez%20Paz%20etal_2020_JSAES_Review%20El%20Mait%c3%a9n%20Belt.pdf. 
  • Jin, Mengjie; Andreas Zwick; Adam Ślipiński; John W. M. Marris; Michael C. Thomas, and Hong Pang. 2020. A comprehensive phylogeny of flat bark beetles (Coleoptera: Cucujidae) with a revised classification and a new South American genus. Systematic Entomology 45. 248–268. doi:10.1111/syen.12392
  • Aranciaga Rolando, Alexis M.; Federico L. Agnolin, and Julián Corsolini. 2019. A new pipoid frog (Anura, Pipimorpha) from the Paleogene of Patagonia. Paleobiogeographical implications. Comptes Rendus Palevol 18. 725–734. doi:10.1016/j.crpv.2019.04.003
  • Jud, Nathan A.; Ari Iglesias; Peter Wilf, and Maria A. Gandolfo. 2018. Fossil moonseeds from the Paleogene of West Gondwana (Patagonia, Argentina). American Journal of Botany 105. 927–942. doi:10.1002/ajb2.1092 PMID 29882954
  • Ramírez, Leonardo C.; Juan Corsolini, and Osvaldo Di Iorio. 2016. First fossil record of parasitic flat-bark beetle (Coleoptera: Passandridae) from the Eocene of Patagonia, Argentina. Ameghiniana 53. 160–169. doi:10.5710/AMGH.29.11.2015.2920
  • Prez, Horacio, and Gabriela Massaferro. 2013. Geología y geomorfología del tramo superior del Arroyo Comallo, Río Negro. Contribuciones Científicas GÆA 26. 221–234. Accessed 2020-06-13.
  • Barreda, V.D.; L. Palazzesi; L. Katinas; J.V. Criscri; M.C. Telleria; K. Bremer; M.G. Passala; F. Bechis, and R. Corsolini. 2012. An extinct Eocene taxon of the daisy family (Asteraceae): evolutionary, ecological and biogeographical implications. Annals of Botany 109. 127-134.
  • Escosteguy, Leonardo, and Mario Franchi. 2010. Estratigrafía de la región de Chapelco, Provincia del Neuquén. Revista de la Asociación Geológica Argentina 66. 418–429. Accessed 2020-06-13.
  • Báez, Ana M., and L. Analia Pugener. 2003. Ontogeny of a new Palaeogene pipid frog from southern South America and xenopodinomorph evolution. Zoological Journal of the Linnean Society 139. 439–476. doi:10.1046/j.1096-3642.2003.00085.x
  • Melendi, D.L.; L.H. Scafati, and W. Volkheimer. 2003. Palynostratigraphy of the Paleogene Huitrera Formation in N-W Patagonia, Argentina. Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen 228. 205-273.