The non-marine ostracod Cypridea Bosquet is surprisingly diverse worldwide, especially in the Cretaceous. Due to their short temporal distribution, many Cypridea species together with other typical Pre-Salt ostracod genera, such as Ilhasina Krömmelbein, Paracypridea Swain, Petrobrasia Krömmelbein, Reconcavona Krömmelbein, and Theriosynoecum Branson, have provided a robust biostratigraphic framework for Brazilian and Western African basins. The Recôncavo-Tucano Basin, located in the Bahia State, was the first Brazilian oil basin. This huge Mesozoic paleolake has over a hundred of ostracod species, most of the genus Cypridea, which allowed the development of a biostratigraphic chart with nine biozones and several subzones. This biostratigraphic framework has been used for correlations with most of the non-marine sections of NE and SE Brazilian basins, including the Sanfranciscana Basin, whose lacustrine outcrops correspond to the Quiricó Formation. Nevertheless, in a recent publication on ostracods and the age of the Quiricó Formation, Cypridea species were erroneously identified. Consequently, a Valanginian age was wrongly proposed for the base of that formation, and the stratigraphic and geographical distributions of some species were erroneously extended. The present study reveals that none Cypridea species of the Quiricó Formation is conspecific with the Recôncavo-Tucano Basin species, including Cypridea hystrix Krömmelbein, and, consequently, a Valanginian age is discarded for the base of that formation.