Parángula Formation

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Thickness550–1,600 m[1]
Parángula Formation
Stratigraphic range: Oligocene–Miocene
Holotype of Barinasuchus arveloi, recovered from the Parángula Formation
TypeGeological formation
UnderliesRío Yuca Formation
OverliesEl Mene Formation
Thickness550–1,600 m[1]
Lithology
PrimarySandstone
OtherShales, claystones
Location
Approximate paleocoordinates9°18′N 66°06′W / 9.3°N 66.1°W / 9.3; -66.1
RegionBarina, Portuguesa
CountryVenezuela
Type section
Named forQuebrada Parángula
Named byMackenzie, 1937
Parángula Formation is located in Venezuela
Parángula Formation
Parángula Formation (Venezuela)

The Parángula Formation is a lithostratigraphic unit in the states of Barinas and Portuguesa[2] in Venezuela. It was deposited from the Oligocene to the Miocene.[3][1]

The Parángula Formation was first published about by A. N. Mackenzie in 1937, who used the name in reference to a series of sandstones, conglomerates, and mottled clays from the Parángula ravine.[4] In 1946, a further description of the formation's geology was published by R. A. Liddle.[5] In 1960, a thorough description of the stratigraphy of the Parángula Formation was published by G. R. Pierce. Pierce attempted to emend the name of the formation, renaming it to the Parángulo Formation,[6] though this was unsuccessful.[1]

Description

Fossils

References

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