Abstract
The effects of a major storm event (Hurricane Gordon) on the biogeochemistry of Atlantic coastal and Gulf Stream waters were investigated during a research cruise in November 1994. Prestorm, NH4+, NO3+, and PO4−3 concentrations were consistently well below 1 μM, whereas after the storm, nutrient concentrations were higher in the surface‐water samples: >2 μM, in some instances. Primary and secondary (bacterial) production were stimulated by factors of 5 and 2, respectively, up to 4 d following the storm. Bioassay experiments showed that additions of inorganic N stimulated chlorophyll a (Chl a) concentrations, 14CO2 fixation, and stable isotope fractionations both before and after the storm, but the addition of phosphate had a greater impact in post‐storm experiments. The δ15n of particulate nitrogen (PN) varied from +5 to +1.5‰ before Gordon, then afterward attained a consistent value of +3.0‰. Sedimentary organic δ15n values were similar to water‐column organic N, and the δ15n of dissolved NH4+ from surface sediments (+4.0‰) almost matched the δ15n of water‐column particulates. These results indicate that storm‐generated winds mixed sediments along with dissolved nutrients into surface waters, which supported a rapid increase in water‐column primary production.
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