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Dead carbon in stalagmites: carbonate bedrock paleodissolution vs. ageing of soil organic matter. Implications for 13 C variations in speleothems

Organic GeochemistryBiogeochemistryEngineeringDead CarbonOrganic-rich Sedimentary RockGeochemistryC VariationsCarbon CycleSpeleothem RecordEarth ScienceCarbonate Bedrock Paleodissolution