Large
amounts of terrigenous organic matter (TOM) are delivered
to the ocean every year. However, removal processes of TOM in the
ocean are still poorly constrained. Here, we report results from a
339-day dark incubation experiment with a unique system holding a
vertically stratified freshwater–seawater column. The quality
and quantity of dissolved organic matter (DOM), RNA-based size-fraction
microbial communities, and environmental factors were high-frequency-monitored.
Microbial processes impacted TOM composition, including an increased
DOM photobleaching rate with incubation time. The mixed layer had
changed the bacterial community structure, diversity, and higher oxygen
consumption rate. A two-end member modeling analysis suggested that
estimated nutrient concentrations and prokaryotic abundance were lower,
and total dissolved organic carbon was higher than that of the measured
values. These results imply that DOM biodegradation was stimulated
during freshwater–seawater mixing. In the bottom layer, fluorescent
DOM components increased with the incubation time and were significantly
positively related to highly unsaturated, oxygenated, and presumably
aromatic compound molecular formulas. These results suggest that surfaced-derived
TOM sinking leads to increased DOM transformation and likely results
in carbon storage in the bottom water. Overall, these results suggest
that microbial transforming TOM plays more important biogeochemical
roles in estuaries and coastal oceans than what we know before.