Earth:Lotena Formation

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Lotena Formation
Stratigraphic range: Late Callovian-Early Oxfordian
~165–160 Ma
TypeGeological formation
Unit ofLotena Group
Sub-unitsLa Estrechura, El Pichanal & El Vado Members
UnderliesLa Manga Formation
OverliesCuyo Group
 Lajas Formation
Thickness50–167 m (164–548 ft)
Lithology
PrimarySandstone, conglomerate
OtherLimestone, shale
Location
Coordinates [ ⚑ ] : 38°36′S 70°12′W / 38.6°S 70.2°W / -38.6; -70.2
Paleocoordinates [ ⚑ ] 35°54′S 31°42′W / 35.9°S 31.7°W / -35.9; -31.7
RegionNeuquén Basin
 Mendoza Province & Neuquén Province
  Northern Patagonia
CountryArgentina
Extent2,500 km2 (970 sq mi)
Type section
Named forCerro Lotena
Named byWeaver
Year defined1931
Lotena Formation is located in Argentina
Lotena Formation
Lotena Formation (Argentina)

The Lotena Formation is a geologic formation dated from the Late Callovian to Early Oxfordian in the Neuquén Basin in Mendoza Province, Argentina .[1] The formation, first defined by Weaver in 1931 and named after Cerro Lotena,[2] consists of fluvial conglomerates, calcareous sandstones and marine limestones and shales.[2][3] The Lotena Formation is overlain by the La Manga Formation and overlies the Lajas Formation of the Cuyo Group.[4] Initially, the fossil find of the pterosaur Herbstosaurus pigmaeus was reported from the formation,[5] but this fossil was found in the younger Vaca Muerta.[6] The formation is a reservoir rock in the Neuquén Basin.

See also

References

  1. Lotena Formation at Fossilworks.org
  2. 2.0 2.1 Zanettini et al., 2010, p.25
  3. Veiga et al., 2011, p.174
  4. Veiga et al., 2011, p.178
  5. Wellnhofer, 1991, p.81
  6. Herbstosaurus at Fossilworks.org

Bibliography