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Increased continental weathering flux during orbital-scale sea-level highstands: Evidence from Nd and O isotope trends in Middle Pennsylvanian cyclic carbonates

Marine GeologyEngineeringPaleoenvironmental ChangePaleoceanographyGeographyGeologyGeochemistryEarth System ScienceSea-level HistoryPaleoclimatologyOrbital-scale Sea-level HighstandsEarth ScienceEarth's ClimateTectonics