Their data reveal large differences between the individual stagnation events with regard to the Fe-P dissolution rates. This may explain the deviation of the long-term mean from our estimate, which refers to a specific period. A detailed analysis of the temporal variability in the phosphate and total CO2 concentrations during the full cycle from anoxic to oxic and back to anoxic conditions provided insight into a number of processes that are important for the cycling

of phosphorus in the deep water of the Baltic Sea. It was shown that the frequently documented abrupt decrease in PO4 concentrations, occurring concurrently with the change from anoxic to oxic conditions caused by a water renewal event, is to a large extent due to dilution and only partly a consequence of the precipitation of iron- 3-hydroxo-phosphates. Owing to the low concentrations of dissolved iron in the water column and the limited capacity of FeO(OH) to NVP-BGJ398 in vivo bind PO4, the formation of Fe-P in the water column is low and takes place predominantly at the sediment surface where, depending on the redox conditions, Fe accumulates as either oxide or sulphide. The formation of Fe-P is thus a slow process since

it requires the transport of PO4 to the sediment surface by vertical and/or lateral mixing. The release of Fe-P previously deposited by a shift from anoxic to oxic conditions amounted to about 50 mmol m−2. However, this value cannot be generalized because it depends on the PO4 accumulation during the previous stagnation Nutlin-3a manufacturer period. It was further shown that the dissolution and precipitation of Fe-P during changing redox conditions constitute a closed cycle and that in the long term, phosphate is added to the system only triclocarban by mineralization of organic matter approximately according to the Redfield ratio. Hence, PO4 is recycled in the same way as carbon and nitrogen, and anoxic conditions do not generate an extra source

of PO4. We thank the staff of the Monitoring Programme of the Leibniz Institute for Baltic Sea Research for their reliability during sampling and chemical analysis and especially H. Kubsch for performing the total CO2 analysis with great care. “
“Wind-driven coastal upwelling is a typical phenomenon in the Baltic Sea (Gidhagen 1987, Myrberg & Andrejev 2003) with strong upwelling events occurring with an annual average frequency of up to 30% in some parts of the Baltic (Kowalewski & Ostrowski 2005). In the Gulf of Finland, a sub-basin of the Baltic Sea oriented from west to east, wind-driven coastal upwelling events are caused by either westerly or easterly wind forcing, which must have been operating for at least 60 h to generate an upwelling in the Gulf (Haapala et al. 1994). Upwellings and related mesoscale structures (meanders, filaments and eddies) in the region have been studied with different methods – field observations (e.g. Haapala et al. 1994, Lips et al. 2009, Kuvaldina et al. 2010), remote sensing (Kahru et al.