Our research focuses on the role of seafloor processes in ocean chemical cycles, the biogeochemical influences of hypoxia and anoxia, and new electrochemical tools for ocean observing networks.
Over the last 10 years we have adopted the eddy covariance (EC) method as our main approach to studying benthic oxygen exchange, and we have applied EC to study the dynamics of fluxes on the Oregon shelf. Benthic oxygen fluxes represent the rate that oxygen dissolved in seawater is consumed (or produced) by the biological community at the seafloor. Essential to eddy covariance measurements are reliable, fast responding, low noise, and fully calibrated oxygen sensors. We are working on new sensor designs and comparing sensors made in our lab to commercially available optodes and microelectrodes. In 2018 and 2019, we will make repeated EC measurements at sites at 30 m and 80 m water depth adjacent to the Oregon line of the Ocean Observatories Initiative (OOI) Endurance Array to assess if there are changes in the biological activity of sediments due to seasonal changes in organic matter input from overlying waters. It is hypothesized that enough labile marine organic matter is retained in the shelf environment throughout the winter to support substantial benthic fluxes of oxygen, total carbon dioxide and nutrients that are important in setting bottom water conditions at the start of the summer upwelling season.
Benthic Microbial Fuel Cells
Our group also continues to develop and evaluate revolutionary benthic microbial fuel cells (BMFCs) – devices designed as self-refueling power sources for fixed seafloor sensors. We have demonstrated powering sonar modem/chemical sensor systems by unattended BMFCs at water depths ranging from 10-1000 m. We are investigating the microbial communities and chemistries that enable electron transfer in these systems. A unique discovery we made recently is finding multicellular, filamentous, sulfur-oxidizing bacteria, known as cable bacteria, attached to fibers of a carbon brush electrode serving as an anode of a benthic microbial fuel cell. This finding indicates that cable bacteria may in fact be facultative anaerobes. We are conducting follow-on work to use BMFCs to enrich for cable bacteria and to study their mechanisms of electron transport from cell to cell and to a solid electrode. To learn more about our research please go to the links above.