In-stream metabolism and atmospheric carbon sequestration in a groundwater-fed karst stream
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文摘
In-stream metabolism controls diel cycles of DIC concentrations of karst streams. DIC uptake by photosynthesis exceeds DIC release by respiration at the study site. The excess uptake of 73 t C km− 2 a− 1 is about half the oceanic biological pump. The in-stream photosynthetic C sink could affect the global carbon budget.

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