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1 Department of Biology, Faculty of Science, SDU 2 Nordic Center for Earth Evolution (NordCEE), Department of Biology, Faculty of Science, SDU 3 Clinical Microbiology, Department of Clinical Research, Det Sundhedsvidenskabelige Fakultet, SDU 4 Max Planck Institute for Marine Microbiology 5 Aarhus Universitet 6 Department of Biology, Faculty of Science, SDU
Processes, precursors and relative importance
Emission of the greenhouse gas nitrous oxide (N2O) from freshwater and terrestrial invertebrates has exclusively been ascribed to N2O production by ingested denitrifying bacteria in the anoxic gut of the animals. Our study of marine molluscs now shows that also microbial biofilms on shell surfaces are important sites of N2O production. The shell biofilms of Mytilus edulis, Littorina littorea and Hinia reticulata contributed 18-94% to the total animal-associated N2O emission. Nitrification and denitrification were equally important sources of N2O in shell biofilms as revealed by 15N-stable isotope experiments with dissected shells. Microsensor measurements confirmed that both nitrification and denitrification can occur in shell biofilms due to a heterogeneous oxygen distribution. Accordingly, ammonium, nitrite and nitrate were important drivers of N2O production in the shell biofilm of the three mollusc species. Ammonium excretion by the animals was found to be sufficient to sustain N2O production in the shell biofilm. Apparently, the animals provide a nutrient-enriched microenvironment that stimulates growth and N2O production of the shell biofilm. This animal-induced stimulation was demonstrated in a long-term microcosm experiment with the snail H.reticulata, where shell biofilms exhibited the highest N2O emission rates when the animal was still living inside the shell. © 2012 John Wiley & Sons Ltd and Society for Applied Microbiology.
Environmental Microbiology, 2013, Vol 15, Issue 7, p. 1943-1955
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