Nutrient pulses, plankton blooms, and seasonal hypoxia in western Long Island Sound

Development of seasonal hypoxia was studied weekly in the western narrows o f Long island Sound (WLIS) during the summers of 1992 and 1993 by measuring hydrographic properties, biological oxygen demand (BOD), biomass, producti on, and mortality of phytoplankton and bacterioplankton in the water column . Dissolved oxygen in bottom waters was low and variable during stratified periods (19-51% saturation), oscillating in and out of hypoxic conditions ( defined as < 3 mg O-2 I-1 or 94 <mu>M O-2). Hypoxia was more prevalent in 1 993 than in 1992, corresponding to greater water column stratification in 1 993. Micrrobial BOD in bottom waters appeared to be fueled by delivery of a utochthonous carbon from phytoplankton blooms rather than allochthonous car bon input Phytoplankton production responded to elevated NH4+ concentration s, especially when the mixed layer was shallow. NH4+ concentrations general ly varied as a function of the preceding week's rainfall (r(2) = 0.765). Ba cterial production did not covary with phytoplankton production, yet was cl osely correlated with particulate organic carbon, which was cltorophyll-ric h. Results indicate that the timing and severity of hypoxia development are strongly coupled to allochthonous input of NH4+ after heavy precipitation. Observations illustrate for the first time that bottom waters in this syst em oscillate in and out of hypoxia on an almost weekly basis rather than su stain them over the entire stratified period. The frequency of these oscill ations depends upon variations in nutrients, planktonic production and expo rt, and bottom water ventilation.