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River systems play crucial roles in the global carbon balance; however, the environmental consequences of sediment dredging on carbon dioxide (CO 2 ) emissions and carbon sequestration potential remain poorly understood. This study presents the first systematic investigation linking sediment dredging to long-term carbon sequestration dynamics in river ecosystems, addressing critical uncertainties in anthropogenic impacts on aquatic carbon balance. Over a three-year period, dredging significantly altered CO 2 flux ( f CO 2 ) and dissolved CO 2 partial pressure ( p CO 2 ), with pronounced seasonal variability driven by dissolved organic carbon as a key predictor. Microbial community composition shifted from Cyanobacteria to Gammaproteobacteria and Flavobacteria dominance, accompanied by enhanced Calvin cycle enzyme gene expression and suppression of alternative carbon fixation pathways. While phytoplankton biomass, particularly Cyanobacteria, declined sharply during dredging, carbon sequestration potential exceeded predredging levels within three years of monitoring, indicating strong resilience in riverine carbon storage capacity. Our findings indicate that (1) dredging-induced community restructuring enhances chemoautotrophic carbon fixation through modified expression of rTCA cycle components and Calvin cycle optimization, (2) phytoplankton carbon biomass and chlorophyll a emerge as primary drivers of postdredging carbon sequestration pathways, and (3) gross primary production peaks at 960.8 mg C m –2 d –1 through synergistic phytoplankton interactions. These mechanistic discoveries, which quantify relationships between microbial taxa, metabolic gene expression, and carbon fluxes, establish new insights for predicting ecosystem responses to anthropogenic disturbances in river ecosystems.
Hao et al. (Thu,) studied this question.