Toro Toro Formation | |
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Stratigraphic range: Late Campanian ~ | |
![]() Dinosaur ichnofossils in the Toro Toro Formation | |
Type | Geological formation |
Unit of | Puca Group |
Lithology | |
Primary | Sandstone |
Other | Mudstone, gypsum |
Location | |
Coordinates | 18°06′S65°48′W / 18.1°S 65.8°W |
Approximate paleocoordinates | 21°18′S47°48′W / 21.3°S 47.8°W |
Region | Cochabamba Department |
Country | Bolivia |
Extent | Potosí Basin |
Type section | |
Named for | Torotoro National Park |
The Toro Toro Formation is a Late Campanian geologic formation pertaining to the Puca Group of central Bolivia. The porous yellowish medium-to-coarse grained ferruginous (iron-containing) sandstones and mudstones with gypsum intercalations, deposited in a beach environment, preserve many ichnofossils of Ligabueichnium bolivianum , Dromaeopodus sp. , [1] Ornithopoda indet., Theropoda indet. and Titanosauridae indet. [2] The formation has provided the earliest known tracksite of dinosaurs in Bolivia. [3] The Toro Toro Formation represents part of the postrift stage in an alluvial to deltaic environment within the Potosí Basin. The formation is a local equivalent of the Chaunaca Formation. [4] The most famous of the dinosaur tracksites is Cal Orcko, however these are in the El Molino Formation