The Curré Formation is a geologic formation of the Taraba Basin Group in Costa Rica. The deltaic conglomerates preserve fossils dating back to the Late Miocene to Early Pliocene period (Hemphillian).[1]

Curré Formation
Stratigraphic range: Hemphillian
~10.3–4.9 Ma
TypeFormation
Unit ofTaraba Basin Group
UnderliesEl Brujo & La Cruz Formations
OverliesTérraba Formation
Lithology
PrimaryConglomerate
Location
Coordinates8°54′N 83°06′W / 8.9°N 83.1°W / 8.9; -83.1
Approximate paleocoordinates8°48′N 83°06′W / 8.8°N 83.1°W / 8.8; -83.1
RegionLimón & Puntarenas Provinces
Country Costa Rica
ExtentTaraba Basin
Type section
Named forRey Curré
Curré Formation is located in Costa Rica
Curré Formation
Curré Formation (Costa Rica)

Fossil content edit

The following fossils have been found in the formation:

See also edit

References edit

  1. ^ Curré Formation at Fossilworks.org
  2. ^ Rincón et al., 2020

Bibliography edit

  • Rincón, Ascanio D.; Ana L. Valerio, and César Laurito. 2020. Primer registro fósil de un Megatheriidae-Megatheriinae para el Hemphilliano (Mioceno Tardío) de San Gerardo de Limoncito, Formación Curré, Costa Rica. Revista Geológica de América Central 62. 1–24. . doi:10.15517/rgac.v62i0.41278

Further reading edit

  • C. Laurito, A. L. Valerio, E. Ovares, A. Hernández, and D. Pizarro. 2008. Peces Fósiles de la localidad Las Lomas de Siquirres cause del Río Reventazón, Formación Río Banano, Mioceno Superior, Provincia de Limón, Costa Rica [Fossil fishes of the Las Lomas de Siquirres Locality, Reventazon river, Rio Banano Formation, Late Miocene, Limon province, Costa Rica]. Revista Geológica de América Central 38:11-25
  • C. A. Laurito and A. L. Valerio. 2008. The first record of Gavialosuchus americanus Sellards (1915)† (Eusuchia: Crocodylidae, Tomistominae) for the Late Tertiary of Costa Rica and Central America. Revista Geológica de América Central 39:107-115