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The evolution of early diagenetic signals in Bering Sea subseafloor sediments in response to varying organic carbon deposition over the last 4.3Ma

Organic GeochemistryBiogeochemistryMarine GeologyEngineeringChemical OceanographyPaleoceanographyEarly DiagenesisEarly Diagenetic SignalsMarine ChemistryOceanographyLast 4.3MaSedimentologyEarth ScienceOrganic Carbon Deposition