Microphytobenthos activity and fluxes at the sediment-water interface: interactions and spatial variability

In this study oxygen and nutrient fluxes and denitrification rates across the sediment-water interface were measured via intact core incubations with a twofold aim: show whether microphytobenthos activity affects these processes and analyse the dispersion of replicate measurements. Eighteen intact sediment cores (i.d. 8 cm) were randomly sampled from a shallow microtidal brackish pond at Tjarno, on the west coast of Sweden, and were incubated in light and in darkness simulating in situ conditions. During incubation O₂, inorganic N and SiO₂ fluxes and denitrification rates (isotope pairing) were measured. Assuming mean values of 18 cores as best estimate of true average (BEA), the accuracy of O₂, NH₄ ⁺, NO₃ ^- and SiO₂ fluxes calculated for an increasing number of subsamples was tested. At the investigated site, microalgae strongly influenced benthic O₂, inorganic N and SiO₂ fluxes and coupled (D_n) and uncoupled (D_w) denitrification through their photosynthetic activity. In the shift between dark and light conditions NH₄ ⁺ and SiO₂ effluxes (60 and 110 µmol m^-2h^-1) and D_n (5 µmol m^-2 h^-1) dropped to zero, NO₃ ^- uptake (70 µmol m^-2 h^-1) showed a 30% increase, while D_w (20 µmol m^-2 h^-1) showed an 80% decrease. For O₂ and NO₃ ^- dark fluxes, 4 core replicates were sufficient to obtain averages within 5-10% of the best estimated mean, while 10-20% accuracy was obtained with 4-12 replicates for SiO₂ and >10 replicates for NH₄ ⁺ dark fluxes. Mean accuracy was considerably lower for all light incubations, probably due to the patchy distribution of the benthic microalgal community.