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Ostracods as proxies for marginal marine to non-marine intervals in the mid-Cretaceous carbonate platform of the Central Tunisian Atlas (North Africa): Response to major short-term sea-level falls

Marine GeologyEngineeringMarginal MarinePaleoceanographyGeographyCentral Tunisian AtlasCretaceous PeriodGeologyGeochronologyCretaceous-paleogene BoundaryEarth ScienceNorth AfricaTectonics