Sediment resuspension caused by simulated storms led to a dramatic short-term increase of aminopeptidase (AMPase) and P-glucosidase (GLCase) activities and bacterial secondary production in coastal waters during a mesocosm experiment in Knebel Vig, Denmark. Perturbation of sediments strongly affected the kinetic parameters of AMPase and GLCase in the water column of the enclosures. V, , , values of AMPase and GLCase determined 4 h after a simulated storm event were 24 % and 43 % higher, respectively, than those assayed during the calm period. Sediment resuspension in enclosures ('storm enclosures') had the most pronounced effect on GLCase apparent K, (Michaelis constant) values, which increased 2.6 times (163 %) after sediment resuspension. AMPase K,,, values were approximately 1.6 times higher after sediment resuspension than before sediment resuspension. Changes in of the V, , and K,,, values of GLCase and AMPase in storm enclosures were accompanied by longer turnover tlmes for enzymatic hydrolysis of substrates. GLCase and AMPase after sediment resuspension had noticeably higher specific activities than before the storm event. GLCase and AMPase specific activities produced by an 'average' single bacterium were 2.4 and 2.1 times higher, respectively, after the storm event. Sediment in the water caused a situation in which most GLCase activity (68%) was associated with the particle size fraction >l0 pm. AMPase activity after a storm event also shifted towards the > 10 pm size fractions. Activities of free AMPase and GLCase dissolved in the water were low and contributed 8% and 14-16%, respectively, to the total activity of these enzymes. Results of simultaneously radiolabeling size-fractionated samples with [3H]thymidine and ['"]protein hydrolysate showed that the water column of storm enclosures was inhabited by metabolically different bacterial populations before and after sediment resuspension. The response of the suspended microbial assen~blages to the storm event was very rapid but short-term; enzymatic activity levels returned to pre-storm levels within 24 h. Our rnesocosm experiments demonstrated that sediment resuspension caused by simulated storms had a pronounced stimulatory effect on the rates of microbial enzymatic degradation of organic matter in a coastal ecosystem.