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Global marine redox evolution from the late Neoproterozoic to the early Paleozoic constrained by the integration of Mo and U isotope records

U Isotope RecordsMarine GeologyEngineeringPrecambrian GeologyIsotope GeochemistryEvolutionary BiologyEarly PaleozoicLate NeoproterozoicMarine ChemistryGeologyOxygen IsotopeGeochemistryGeochronologyEarth Science