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Applied and Environmental Microbiology, November 2003, p. 6447-6454, Vol. 69, No. 11
0099-2240/03/$08.00+0     DOI: 10.1128/AEM.69.11.6447-6454.2003
Copyright © 2003, American Society for Microbiology. All Rights Reserved.

Anaerobic Ammonium Oxidation Measured in Sediments along the Thames Estuary, United Kingdom

Mark Trimmer,* Joanna C. Nicholls, and Bruno Deflandre{dagger}

School of Biological Sciences, Queen Mary, University of London, London E1 4NS, United Kingdom

Received 15 May 2003/ Accepted 11 August 2003

Until recently, denitrification was thought to be the only significant pathway for N2 formation and, in turn, the removal of nitrogen in aquatic sediments. The discovery of anaerobic ammonium oxidation in the laboratory suggested that alternative metabolisms might be present in the environment. By using a combination of 15N-labeled NH4+, NO3-, and NO2- (and 14N analogues), production of 29N2 and 30N2 was measured in anaerobic sediment slurries from six sites along the Thames estuary. The production of 29N2 in the presence of 15NH4+ and either 14NO3- or 14NO2- confirmed the presence of anaerobic ammonium oxidation, with the stoichiometry of the reaction indicating that the oxidation was coupled to the reduction of NO2-. Anaerobic ammonium oxidation proceeded at equal rates via either the direct reduction of NO2- or indirect reduction, following the initial reduction of NO3-. Whether NO2- was directly present at 800 µM or it accumulated at 3 to 20 µM (from the reduction of NO3-), the rate of 29N2 formation was not affected, which suggested that anaerobic ammonium oxidation was saturated at low concentrations of NO2-. We observed a shift in the significance of anaerobic ammonium oxidation to N2 formation relative to denitrification, from 8% near the head of the estuary to less than 1% at the coast. The relative importance of anaerobic ammonium oxidation was positively correlated (P < 0.05) with sediment organic content. This report of anaerobic ammonium oxidation in organically enriched estuarine sediments, though in contrast to a recent report on continental shelf sediments, confirms the presence of this novel metabolism in another aquatic sediment system.


* Corresponding author. Mailing address: School of Biological Sciences, Queen Mary, University of London, London E1 4NS, United Kingdom. Phone: 44 (0)20 7882 3007. Fax: 44 (0)20 8983 0973. E-mail: m.trimmer{at}qmul.ac.uk.

{dagger} Present address: Laboratoire de Géochimie des Eaux, Université Denis Diderot Paris 7 and Institut Physique du Globe de Paris, Paris, France.


Applied and Environmental Microbiology, November 2003, p. 6447-6454, Vol. 69, No. 11
0099-2240/03/$08.00+0     DOI: 10.1128/AEM.69.11.6447-6454.2003
Copyright © 2003, American Society for Microbiology. All Rights Reserved.




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