Seasonal dynamics of benthic O-2 uptake in a semienclosed bay: Importance of diffusion and faunal activity

The benthic O2 uptake and the O2 microdistribution in a coastal sediment of Aarhus Bay, Denmark, were investigated during a seasonal study. Measurements were performed in situ by a profiling lander and a flux chamber lander, as well as on recovered sediment cores. The O2 penetration depth, the diffusive O2 uptake, and the volumespecific O2 consumption rate strongly depended on the seasonal changes in bottom water O2 concentration and the sedimentation of organic carbon. The in situ O2 penetration depth varied between 0.5 mm in summer and 4.5 mm in winter. The diffusive O2 uptake varied between 8 and 30 mmol m−2 d−1, whereas the volume‐specific O2 consumption rate varied by a factor of 13. The O2 distribution was very sensitive to environmental controls, and microprofiles obtained in the laboratory tended to overestimate the in situ O2 penetration depths and underestimate the in situ diffusive O2 uptake. Three‐dimensional O2 flux calculations based on in situ microtopographic mapping showed that the actual diffusive exchange rate was ~10% higher than the simple one‐dimensional, microprofilederived diffusive O2 exchange. The total O2 uptake measured in the laboratory showed less distinct seasonal variation, but on the average, it was ~20% higher than the diffusive O2 uptake. The difference reflected the microtopography of the sediment surface and the contribution from benthic macrofauna. In situ total O2uptake was generally twice as high as laboratory rates, reflecting a higher fauna‐related O2 consumption in the larger enclosures incubated in situ. Annually, the in situ three‐dimensional diffusive O2 consumption was 6.2 mol O2 m−2, whereas the additional benthos‐mediated O2 uptake was 3.9 mol O2 m−2. Thus, 40% of the total O2 uptake was due to faunal activity and respiration. The present study demonstrates the importance of realistic faunal representation during sediment incubations in order to obtain correct benthic mineralization rates