| Huayquerías Formation | |
| Period: | Messinian |
| Age: | Messinian-Zanclean (defined as Huayquerian) ~ |
| Type: | Geological formation |
| Prilithology: | Mudstone |
| Otherlithology: | Sandstone, tuff |
| Underlies: | Tunuyán Formation |
| Thickness: | Up to 126m (413feet) |
| Coordinates: | -33.8°N -69°W |
| Paleocoordinates: | 34°N -66.9°W |
| Region: | Mendoza Province |
| Country: | Argentina |
| Extent: | Frontal Cordillera & Cuyo Basin |
| Namedby: | Kraglievitch |
| Year Ts: | 1934 |
| Region Ts: | Mendoza Province |
| Country Ts: | Argentina |
The Huayquerías Formation (Spanish; Castilian: Formación Huayquerías) is a Late Miocene fossiliferous geological formation of the Frontal Cordillera and Cuyo Basin of Argentina. The formation crops out in the central Mendoza Province.
The formation, with a maximum thickness of 126m (413feet), comprises reddish mudstones with thin beds of tuffs and sandstones, deposited in a fluvial, environment. The tuff in the formation is dated to 5.84 ± 0.41 Ma, placing it in the Huayquerian SALMA, the age named after the formation by Kraglievitch in 1934.
The formation has provided fossils of the procyonid Cyonasua pascuali and the litoptern Huayqueriana cristata, named after the formation.
The Huayqueriás Formation, present in the Frontal Cordillera and the neighboring Cuyo Basin, was described in 1934 by Kraglievitch as the basis for the Huayquerian South American land mammal age. The name Huayquerías means "badlands".[1] The formation comprises reddish mudstones with mudcracks, paleoburrows and ichnofossils of vertebrates. Thin sandstone layers of up to 12cm (05inches) thick exist in the formation. An ashfall bed exists at 83m (272feet) below the contact with the slightly angular unconformably[2] overlying Tunuyán Formation in a total section of 126m (413feet).[3] The tuff has been dated using 40K/40Ar analysis to 5.84 ± 0.41 Ma.[4]
See also: Huayquerian. The Huayquerías Formation has been used to define the Huayquerian South American land mammal age, ranging from 9.0 to 6.8 Ma. However, later analysis of the ashfall bed in the formation, provided a much younger age of 5.84 ± 0.41 Ma, extending the temporal range of the Huayquerian SALMAans until near the Miocene-Pliocene limit. The Huayqueriás Formation has provided fossils of Cyonasua pascuali,[5] and the litoptern Huayqueriana cristata, the latter of which, named after the formation.[1]