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Molecular mechanism of anaerobic ammonium oxidation

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Kartal,  B.
Research Group for Microbial Physiology, Department of Biogeochemistry, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Strous,  M.
Microbial Fitness Group, Max Planck Institute for Marine Microbiology, Max Planck Society;

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Citation

Kartal, B., Maalcke, W. J., de Almeida, N. M., Cirpus, I., Gloerich, J., Geerts, W., et al. (2011). Molecular mechanism of anaerobic ammonium oxidation. Nature, 479(7371), 127-U159.


Cite as: http://hdl.handle.net/21.11116/0000-0001-C8F9-5
Abstract
Two distinct microbial processes, denitrification and anaerobic ammonium oxidation (anammox), are responsible for the release of fixed nitrogen as dinitrogen gas (N2) to the atmosphere1,2,3,4. Denitrification has been studied for over 100 years and its intermediates and enzymes are well known5. Even though anammox is a key biogeochemical process of equal importance, its molecular mechanism is unknown, but it was proposed to proceed through hydrazine (N2H4)6,7. Here we show that N2H4 is produced from the anammox substrates ammonium and nitrite and that nitric oxide (NO) is the direct precursor of N2H4. We resolved the genes and proteins central to anammox metabolism and purified the key enzymes that catalyse N2H4 synthesis and its oxidation to N2. These results present a new biochemical reaction forging an N–N bond and fill a lacuna in our understanding of the biochemical synthesis of the N2 in the atmosphere. Furthermore, they reinforce the role of nitric oxide in the evolution of the nitrogen cycle.