Microbial biomass production rates were determined in the brackish water of Kiel Fjord (Western Baltic Sea). The calculated rates are based on the actual uptake data of 14C-U-labelled carbohydrates (ribose, glucose, fructose and galactose). The relation to data obtained from uptake of HC-labelled phytoplankton exudates is discussed. The average microbial biomass production varied from 0.018 to 5.81 μg C I1 h-1. This represents an average of 15 % of the primary production over an annual cycle. A comparison with other data concerning microbial biomass production indicates that glucose may be used as a model to calculate fluxes of dissolved organic matter in this ecosystem. The amount of produced particulate matter by microheterotrophes is discussed with regard to higher trophic levels.
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Bölter et al. (1982) studied this question.
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