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Carbon isotope evidence for sedimentary discontinuities in the lower Toarcian of the Lusitanian Basin (Portugal): Sea level change at the onset of the Oceanic Anoxic Event

Marine GeologySea Level ChangeEngineeringCarbon Isotope EvidenceIsotope GeochemistryGeologyLusitanian BasinGeochemistrySea-level HistorySedimentologyEarth Science