Abstract

Various parameters of bacterial activity were measured in the Kara Sea system (Arctic) including the freshwater endmembers of the rivers Ob and Yenisei during August/September 2001. Average bacterial production in surface water was highest in the rivers (13.5 pg C l -1 d -1 ) and decreased towards the estuaries (5.8 pg C l -1 d -1 ) and the open Kara Sea (2.4 pg C l -1 d -1 ). Bacterial production in the salinity gradient was significantly correlated to chlorophyll a concentrations (r = 0.78, p 100%) than glucose uptake (<10%). Addition of filtered water from the Yenisei to untreated water from the Kara Sea caused no increase in bacterial production relative to the controls, indicating that riverine dissolved organic material is not the primary source of labile compounds for the bacterial community of the Kara Sea. Based on a bacterial growth efficiency of 27% that was derived from bacterial production and respiration measurements, our estimates for the bacterial carbon demand confine the export of surplus primary production from the Kara Sea to the central Arctic.

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