Parángula Formation
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| Parángula Formation | |
|---|---|
| Stratigraphic range: | |
Holotype of Barinasuchus arveloi, recovered from the Parángula Formation | |
| Type | Geological formation |
| Underlies | Río Yuca Formation |
| Overlies | El Mene Formation |
| Thickness | 550–1,600 m[1] |
| Lithology | |
| Primary | Sandstone |
| Other | Shales, claystones |
| Location | |
| Approximate paleocoordinates | 9°18′N 66°06′W / 9.3°N 66.1°W |
| Region | Barina, Portuguesa |
| Country | Venezuela |
| Type section | |
| Named for | Quebrada Parángula |
| Named by | Mackenzie, 1937 |
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]