“…Therefore, a greater proportion of DON is likely bioavailable to phytoplankton in the northern part of BB, either directly or via bacterial remineralization. Cyanobacteria and chlorophytes, generally with a wide salinity tolerance, have been associated with freshwater inputs as well as riverine sources of DON and high residence times in estuaries (Paerl et al, 2003;Pinckney et al, 1998). In northern BB, low salinities, organic N enrichment from anthropogenic sources (Hunchak-Kariouk and Nicholson, 2001;Wienben and Baker, 2009), silica limitation, and high residence times all likely play a role in sustaining the high summer concentrations of pico-chlorophytes and cyanobacteria characteristic of the IBSP study site.…”