| Santa Lucía Formation | |
| Type: | Geological formation |
| Period: | Paleocene |
| Age: | Maastrichtian-Paleocene (typically Tiupampan) ~ |
| Prilithology: | Shale, marl |
| Otherlithology: | Siltstone |
| Region: | Cochabamba |
| Coordinates: | -18.0128°N -65.4065°W |
| Unitof: | Potosí Basin |
| Underlies: | Cayara Formation |
| Overlies: | El Molino Formation |
| Thickness: | 381.35m (1,251.15feet) |
| Location Ts: | Tiupampa, Mizque |
| Coordinates Ts: | -18.0128°N -65.4065°W |
| Paleocoordinates Ts: | -20.7°N -52.5°W |
The Santa Lucía Formation is a Maastrichtian to Paleocene (Danian) geologic formation in Bolivia. Fossil ornithopod tracks have been reported from the Cretaceous lower part of the formation.[1] It is the type formation of the Tiupampan South American land mammal age.
The Santa Lucía Formation is a formation of the Potosí Basin in Bolivia dated to the Paleocene, 60 to 58.2 Ma.[2] It overlies the Cretaceous El Molino Formation and is overlain by the Cayara Formation. The formation is laterally equivalent with the Maíz Gordo Formation of northern Argentina,[3] and time-equivalent with the Salamanca Formation of Argentina, the Maria Farinha Formation of the Paraíba Basin in northern Brazil and the Guaduas Formation of the Altiplano Cundiboyacense and fossiliferous Cerrejón Formation of the Cesar-Ranchería Basin, Colombia.
The 381.35m (1,251.15feet) thick formation consists of reddish sandy shales, marls and siltstones deposited in a fluvial to lacustrine environment.[4] [5]
The oldest known "condylarth" fauna of the Tertiary of South America comes from basal Paleocene strata of the Santa Lucía Formation at Tiupampa. It includes five genera and seven species: Molinodus suarez, Tiuclaenus minutus, T. cotasi, T. robustus, Pucanodus gagnieri, Andinodus boliviensis, and Simoclaenus sylvaticus.[6] Because of its unique fauna, the Santa Lucía Formation at Tiupampa has been chosen as the earliest South American land mammal age giving rise to the Tiupampan.
At the Parotani tracksite, poorly preserved ichnofossils were found in the Maastrichtian part of the formation, left possibly by a carnosaur.[7]
The fossiliferous formation has provided the following fossils:
| Group | Fossils | Notes |
|---|---|---|
| Mammals | ||
| Reptiles & amphibians | Coniophis sp., Cynodontosuchus cf. rothi, Estesiella boliviensis, Kataria anisodonta, Lapparentemys vilavilensis, Podocnemis ?brasiliensis, Roxochelys cf. vilavilensis, Zulmasuchus querejazus, Aniliidae, Boidae, ?Madtsoiidae, Tropidophiidae, Gymnophiona, Carnosauria indet., Ornithopoda indet. | |
| Fishes | ||