Evidence for microbial attenuation of particle flux in the Amundsen Gulf and Beaufort Sea: elevated hydrolytic enzyme activity on sinking aggregates

Export of autochthonously produced particulate organic carbon (POC) is a globally important mechanism for sequestering carbon in the deep sea. The role of microbial hydrolytic activity in attenuating POC flux is generally understudied, and particularly complex on Arctic continental shelves influenced by other sources of POC. To evaluate this role, we used fluorogenic substrate analogs to measure extracellular enzyme activity (EEA) associated with particle size fractions considered suspended (1–70 μm) and sinking (>70 μm). Samples were collected by in situ filtration at depths of 25–100 m at ten stations (156–1,142 m deep) in the Amundsen Gulf and Beaufort Sea in June–July, 2008, during the Circumpolar Flaw Lead project. Significant positive correlations observed between EEA and both chlorophyll a and δ 13 C POC suggest that EEA is elevated in waters dominated by marine-derived POC. No difference in bulk EEA was observed between size fractions, but POC- and cell-specific EEA was significantly elevated on sinking aggregates. Calculations show that 2–44% of carbon retention in surface waters could be attributed to mobilization by enzymes associated with sinking aggregates, and up to 57% if enzymes associated with suspended particles are included. Model results suggest that microbial attenuation of POC below the euphotic zone is a quantitatively important mechanism for carbon loss, especially when particles are sinking slowly. The role of microbes in attenuating POC flux on Arctic shelves appears to have been underestimated previously and may become increasingly important if climate warming brings increased marine productivity.