Stuart E G Findlay

abstract Free-living, planktonic heterotrophic bacteria comprise a major portion of the living biomass of organisms in the Hudson River. Mean densities of bacteria are >5 x 109 cells/L and abundances generally decrease in a downstream pattern. Bacterial growth is rapid with cells doubling about once per day during the warmer months. Demand for carbon is high and consequently the contribution of bacteria to ecosystem respiration is large, particularly in the mid-Hudson where phytoplankton respiration is low The high demand for carbon and lack of strong correlation with phytoplankton abundance suggests bacteria are largely reliant on allochthonous carbon delivered from the watershed. Dissolved organic carbon (DOC) dominates the load from the watershed and bacteria have demonstrated roughly equal ability to grow on DOC derived from several different sources and tributaries. Bacterial abundance increased following the zebra mussel invasion in the early 1990s probably due to zebra mussel removal of important grazers on bacteria.

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