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Denitrification and DNRA at the Baltic Sea oxic-anoxic interface: Substrate spectrum and kinetics
Stockholm University, Faculty of Science, Department of Geological Sciences. Lund University, Sweden.
Stockholm University, Faculty of Science, Department of Ecology, Environment and Plant Sciences. IGB-Leibniz-Institute of Freshwater Ecology and Inland Fisheries, Germany.
Stockholm University, Faculty of Science, Department of Applied Environmental Science (ITM). Stockholm University, Faculty of Science, Stockholm University Baltic Sea Centre.
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Number of Authors: 6
2016 (English)In: Limnology and Oceanography, ISSN 0024-3590, E-ISSN 1939-5590, Vol. 61, no 5, 1900-1915 p.Article in journal (Refereed) Published
Abstract [en]

The dependence of denitrification and dissimilatory nitrate reduction to ammonium (DNRA) on different electron donors was tested in the nitrate-containing layer immediately below the oxic-anoxic interface (OAI) at three stations in the central anoxic basins of the Baltic Sea. Additionally, pathways and rates of fixed nitrogen transformation were investigated with N-15 incubation techniques without addition of donors. Denitrification and anammox were always detected, but denitrification rates were higher than anammox rates. DNRA occurred at two sites and rates were two orders of magnitude lower than denitrification rates. Separate additions of dissolved organic carbon and sulfide stimulated rates without time lag indicating that both organotrophic and lithotrophic bacterial populations were simultaneously active and that they could carry out denitrification or DNRA. Manganese addition stimulated denitrification and DNRA at one station, but it is not clear whether this was due to a direct or indirect effect. Ammonium oxidation to nitrite was detected on one occasion. During denitrification, the production of nitrous oxide (N2O) was as important as dinitrogen (N-2) production. A high ratio of N2O to N-2 production at one site may be due to copper limitation, which inhibits the last denitrification step. These data demonstrate the coexistence of a range of oxidative and reductive nitrogen cycling processes at the Baltic OAI and suggest that the dominant electron donor supporting denitrification and DNRA is organic matter. Organotrophic denitrification is more important for nitrogen budgets than previously thought, but the large temporal variability in rates calls for long-term seasonal studies.

Place, publisher, year, edition, pages
2016. Vol. 61, no 5, 1900-1915 p.
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Biological Sciences Earth and Related Environmental Sciences
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URN: urn:nbn:se:su:diva-135046DOI: 10.1002/lno.10343ISI: 000383621800025OAI: oai:DiVA.org:su-135046DiVA: diva2:1043998
Available from: 2016-11-01 Created: 2016-10-31 Last updated: 2016-11-01Bibliographically approved

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Bonaglia, StefanoKlawonn, IsabellBrüchert, Volker
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Department of Geological SciencesDepartment of Ecology, Environment and Plant SciencesDepartment of Applied Environmental Science (ITM)Stockholm University Baltic Sea Centre
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