Huincul Formation

Huincul Formation
Stratigraphic range: late Cenomanian
Type Geological formation
Unit of Neuquén Group
Underlies Cerro Lisandro Formation
Overlies Candeleros Formation
Thickness 250 m
Lithology
Primary Sandstone
Location
Region Neuquén Province
Country  Argentina

The Huincul Formation is a geologic formation that outcrops in Río Negro and Neuquén provinces of Argentina. It is the second formation in the Río Limay Subgroup, the oldest subgroup within the Neuquén Group. Formerly that subgroup was treated as a formation, and the Huincul Formation was known as the Huincul Member.[1]

The type locality of the Huincul Formation is near the town of Plaza Huincul in Neuquén province.[2] This formation conformably overlies the Candeleros Formation, and it is in turn overlain by the Lisandro Formation.

The Huincul Formation is thought to represent an arid environment with ephemeral or seasonal streams.[3] In some areas, it is up to 250 meters thick. It is mainly composed of green and yellow sandstones and can easily be differentiated from the overlying Lisandro Formation, which is red in color. The Candeleros Formation, underlying the Huincul, is composed of darker sediments, making all three formations easily distinguishable.[4]

Age

Era: Mesozoic
Period: Late Cretaceous
Faunal stage: late Cenomanian
Absolute Age: ~97 to ~94 mya

Paleontology

Argentinosaurus huinculensis
Mapusaurus roseae

Fossil bones are rarely found in the Huincul Formation. However, remains of Argentinosaurus huinculensis, one of the largest land animals known, were found in the Huincul Formation, and this species is named after it.[1] One of the largest predators known, Mapusaurus, has also been recovered from a bonebed in this formation.[3]

Animal fossils found in the Huincul Formation include:

See also

Footnotes

  1. ↑ 1.0 1.1 Sánchez et al. (2006)
  2. ↑ Wichmann (1929)
  3. ↑ 3.0 3.1 Coria & Currie (2006)
  4. ↑ Leanza et al. (2004), Sánchez et al. (2006)

References