Micro-organism activity in aggregate layers in shallow eutrophic brackish water as influenced by wind induced mixing; an experimental approach

In the shallow eutrophic waters of the Darss-Zingst-ecosystem (Baltic Sea) wind induced mixing of the water column, and resuspension of sediment is an important phenomenon. Incubation experiments (7 days) with natural water were performed in the laboratory under simulated mixing conditions in order to assess the effects on abundance, biomass and activity of bacteria, heterotrophic nanoflagellates and ciliates in the water column and upper bottom layers. Under calm mixing conditions a bottom layer developed, rich in organic aggregates. Bacterial biomass increased through increase of bacteria abundance and doubled cell volume. Consequently, biomass of flagellates and, more pronounced, of ciliates increased. The bottom layer, comprising only 15% of the incubated volume, containedca. 60% of the bacterial biomass and ca. 55% of production, 75 and 95% of flagellate biomass, and ca. 70% of ciliate biomass. It is concluded that bottom layers rich in organic aggregates, although not being present permanently, play an important role in the shallow Darss-Zingst-ecosystem.