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Riverine-coastal carbon dynamics, acidification, and CO2 outgassing in an intensive mariculture bay
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DOI：10.1016/j.agee.2025.109972.png)
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Abstract
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• Coupled DIC and δ13CDIC analysis enabled quantification of carbonate system alteration. • Organic matter degradation dominated the main channel, causing acidification. • Summer phytoplankton production buffered acidification in western bay waters. • Remineralized exogenous nitrogen and nitrification intensified oxygen consumption. • Net carbon dioxide outgassing occurred throughout Sansha Bay in winter and summer.
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