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Two-phased collapse of the shallow-water carbonate factory during the late Pliensbachian–Toarcian driven by changing climate and enhanced continental weathering in the Northwestern Gondwana Margin

Marine GeologyEngineeringTwo-phased CollapsePaleoenvironmental ChangeGeographyGeologyPaleoclimatologyContinental WeatheringEarth ScienceShallow-water Carbonate FactoryTectonics