Affiliation:
1. Microbiology Unit, Department of Natural Resource Sciences, Macdonald Campus of McGill University, Ste-Anne-de-Bellevue, Québec, Canada H9X 3V9
Abstract
We report the effect of CH
4
and of CH
4
oxidation on nitrification in freshwater sediment from Hamilton Harbour, Ontario, Canada, a highly polluted ecosystem. Aerobic slurry experiments showed a high potential for aerobic N
2
O production in some sites. It was suppressed by C
2
H
2
, correlated to NO
3
-
production, and stimulated by NH
4
+
concentration, supporting the hypothesis of a nitrification-dependent source for this N
2
O production. Diluted sediment slurries supplemented with CH
4
(1 to 24 μM) showed earlier and enhanced nitrification and N
2
O production compared with unsupplemented slurries (≤1 μM CH
4
). This suggests that nitrification by methanotrophs may be significant in freshwater sediment under certain conditions. Suppression of nitrification was observed at CH
4
concentrations of 84 μM and greater, possibly through competition for O
2
between methanotrophs and NH
4
+
-oxidizing bacteria and/or competition for mineral N between these two groups of organisms. In Hamilton Harbour sediment, the very high CH
4
concentrations (1.02 to 6.83 mM) which exist would probably suppress nitrification and favor NH
4
+
accumulation in the pore water. Indeed, NH
4
+
concentrations in Hamilton Harbour sediment are higher than those found in other lakes. We conclude that the impact of CH
4
metabolism on N cycling processes in freshwater ecosystems should be given more attention.
Publisher
American Society for Microbiology
Subject
Ecology,Applied Microbiology and Biotechnology,Food Science,Biotechnology
Cited by
49 articles.
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