Ammonium cycling by Antarctic zooplankton in winter

Elemental composition and excretion rates of ammonium-nitrogen of zooplankton, ranging over more than five orders of magnitude in body size, were measured in mid-winter in coastal waters west of the Antarctic Peninsula. Excretion rates were constant for the initial 12 h of incubation in the four species tested, and experimental stocking densities of up to 126 mg dry wt l^-1 did not cause variability in the rate of ammonium production. Weight-specific excretion rates of freshly caught Euchaeta antarctica, Conchoecia sp., Thysanoessa macrura, Euphausia superba, and early stage copepodites of Metridia gerlachei were not significantly different from those reported in summer. However, adult copepods of M. gerlachei and Calanoides acutus appear to have reduced their nitrogen metabolism during winter. Turnover rates of body nitrogen increased with diminishing size, ranging from <0.5% body N d^-1 for large E. superba to >7% body N d^-1 for CII and CIII copepodites of M. gerlachei. Only the nitrogen turnover rates of C. acutus were sufficiently low as to suggest that it could survive the entire austral winter without feeding. Phytoplankton and bacterioplankton were virtually absent in both the water column and the sea-ice. We conclude that carnivory is the dominant trophic mode of the pelagic zooplankton community in Antarctica during winter. Production of ammonium-nitrogen by the zooplankton community probably accounts for M10% of the total ammonium regenerated prior to the annual spring bloom.     

The “Seili-index” for the Prediction of Chlorophyll-α Levels in the Archipelago Sea of the northern Baltic Sea,southwest Finland

Environmental Modeling & Assessment - To build a forecasting tool for the state of eutrophication in the Archipelago Sea, we fitted a Generalized Additive Mixed Model (GAMM) to marine...