Abstract
Between 2 and 3
km depth, North Pacific deep waters contain a plume of water with high silicic acid concentrations. The plume extends outward from Cascadia Basin (the Washington Margin), where waters can contain in excess of 200
μM off the coast of Oregon and Washington. To identify the source of the high Si concentrations in Cascadia Basin, we measured silicic acid and germanium concentrations in deep waters, and their fluxes from sediments using incubated cores. The mean flux of silicic acid into bottom waters is 0.81±0.05
mmol/m
2-day, and the Ge/Si ratio of this flux is 0.7±0.1
μmol/mol. A box model, incorporating these results with hydrographic data, indicates that (1) no more than 5% of the silicic acid added to Basin deep waters can have a hydrothermal source (either hot or warm seeps), and (2) the total input of silicic acid to Basin deep waters is 0.06±0.02
Tmol/y. This input is nearly all from remineralized biogenic debris and should contribute about 0.5% of the 14
Tmol/y that are estimated to be necessary to maintain the North Pacific plume.