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The Mesozoic limestones of Piatra Craiului Massif were deposited in the Dâmbovicioara sedimentary area, at the easternmost part of the Getic carbonate platform. In order to study the microfacies and to provide a more detailed biostratigraphy, we sampled the carbonate succession from Piatra Craiului Massif along several sections. Identified microfacies point to reef slope, carbonate platform margin and restricted, lagoon-type internal depositional environments. Some of the identifieddoi:10.5038/1937-8602.59.1.1 fatcat:vb7ovduoarau7b3zy3q5ysw23u