Use of riverine organic matter in plankton

The use of riverine allochthonous organic matter by plankton in the northern Baltic Sea was studied using stable isotopes of carbon and nitrogen. Dissolved and particulate material was sampled in the main Swedish rivers entering the Bothnian Bay and the Bothnian Sea. At 4 sea stations, dissolved matter, plankton and nekton were sampled in l l size-classes: below 0.7 pm filtrate, 0.7-5, 5-20, 20-50, 50-100, 100-200, 200-500, 500-2500 pm, mysids (-10 and -20 mm) and hernng. A riverine influence could be detected in 613C, but not in 6 " ~ . Except for the 5-20 pm fraction, the carbon became enriched in 13C with increasing salinity in all plankton size-fractions. This mainly reflected differences in the 6I3c of phytoplankton, due to the different F13C of marine and riverine dissolved inorganic carbon. Plankton use of riverine dssolved organic carbon (DOC) was tested with a 2-component model. The 613C of riverine DOC and the basin phytoplankton were taken to represent the allochthonous and autochthonous signals, respectively. Use of riverine DOC was indicated for larger zooplankton (200-2500 pm) in the Bothnian Bay, confirming earlier suggestions of extensive use of riverine DOC in the zooplankton food webs in this basin. A new method to adjust 6I3C in zooplankton for variations in lipid content by analysis of covariance was successfully demonstrated. The isotope data reflect the presence of 2 trophic structures, coinciding with the rnicroheterotrophic food web (0.7-5 pm) and the classic grazing food web (>50 pm). From phytoplankton to large zooplankton, 6% increased linearly with the logarithm of organism size in all basins. This increase was steeper in the Bothnian Sea and the Baltic Proper, where zooplankton diversity is higher, than in the Bothnian Bay, possibly reflecting more complex food-web interactions.