厌氧氨氧化菌
铵
硝酸盐
亚硝酸盐
细菌
反硝化
反硝化细菌
环境化学
化学
生物
氮气循环
微生物代谢
氮气
生物化学
生态学
有机化学
遗传学
作者
Boran Kartal,Marcel M. M. Kuypers,Gaute Lavik,J.A.C. Schalk,Huub J. M. Op den Camp,Mike S. M. Jetten,Marc Strous
标识
DOI:10.1111/j.1462-2920.2006.01183.x
摘要
Summary Anaerobic ammonium‐oxidizing (anammox) bacteria oxidize ammonium with nitrite and produce N 2 . They reside in many natural ecosystems and contribute significantly to the cycling of marine nitrogen. Anammox bacteria generally live under ammonium limitation, and it was assumed that in nature anammox bacteria depend on other biochemical processes for ammonium. In this study we investigated the possibility of dissimilatory nitrate reduction to ammonium by anammox bacteria. Physically purified Kuenenia stuttgartiensis cells reduced 15 NO 3 – to 15 NH 4 + via 15 NO 2 – as the intermediate. This was followed by the anaerobic oxidation of the produced ammonium and nitrite. The overall end‐product of this metabolism of anammox bacteria was 15 N 15 N dinitrogen gas. The nitrate reduction to nitrite proceeds at a rate of 0.3 ± 0.02 fmol cell −1 day −1 (10% of the ‘normal’ anammox rate). A calcium‐dependent cytochrome c protein with a high (305 μmol min −1 mg protein −1 ) rate of nitrite reduction to ammonium was partially purified. We present evidence that dissimilatory nitrate reduction to ammonium occurs in Benguela upwelling system at the same site where anammox bacteria were previously detected. This indicates that anammox bacteria could be mediating dissimilatory nitrate reduction to ammonium in natural ecosystems.
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