The Rosablanca Formation (, Kir) is a geological formation of the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes and the Middle Magdalena Basin. The formation consists of grey limestones, dolomites and shales with at the upper part sandstones. The formation dates to the Early Cretaceous period; Valanginian epoch and has a thickness of in the valley of the Sogamoso River.
Definition The formation was first defined by Wheeler in 1929.
Description Lithologies The Rosablanca Formation is characterised by a sequence of grey limestones, dolomites and shales with a maximum thickness of in the Sogamoso River valley.Galvis & Valencia, 2009, p.17
Stratigraphy and depositional environment The Rosablanca Formation overlies the Arcabuco Formation and is overlain by the Ritoque Formation. The age has been estimated to be Valanginian. Stratigraphically, the formation is time equivalent with the Macanal Formation.
Fossils Fossils of the decapod crustacean Diaulax rosablanca have been found in and named after the Rosablanca Formation.Gómez et al., 2015 In 2019, fossils of brachiopod Sellithyris elizabetha were described from the formation.Rojas & Sandy, 2019 In 2020 remains of indeterminate pterosaurs were described from the formation, including pterodactyloids and non-Pteranodontian ornithocheiroids. In 2005 the remains of Platychelyid sea turtle Notoemys zapatocaensis were described, and in 2023 the limbs and shell elements of protostegids were described as some of the largest Early Cretaceous turtles. The hybodont shark Strophodus has been reported from the formation.
Outcrops
The Rosablanca Formation is found, apart from its type locality on the Mesa de Los Santos, Santander, in Boyacá and the Middle Magdalena Basin.
Regional correlations
See also
Geology of the Eastern Hills Geology of the Ocetá Páramo Geology of the Altiplano Cundiboyacense
Notes and references Notes
References
Bibliography
Maps
External links