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黑海厌氧氨氧化菌进行的厌氧氨氧化作用

Anaerobic ammonium oxidation by anammox bacteria in the Black Sea.

作者信息

Kuypers Marcel M M, Sliekers A Olav, Lavik Gaute, Schmid Markus, Jørgensen Bo Barker, Kuenen J Gijs, Sinninghe Damsté Jaap S, Strous Marc, Jetten Mike S M

机构信息

Max Planck Institute for Marine Microbiology, Department of Biogeochemistry, Celsiusstrasse 1, 28359 Bremen, Germany.

出版信息

Nature. 2003 Apr 10;422(6932):608-11. doi: 10.1038/nature01472.

Abstract

The availability of fixed inorganic nitrogen (nitrate, nitrite and ammonium) limits primary productivity in many oceanic regions. The conversion of nitrate to N2 by heterotrophic bacteria (denitrification) is believed to be the only important sink for fixed inorganic nitrogen in the ocean. Here we provide evidence for bacteria that anaerobically oxidize ammonium with nitrite to N2 in the world's largest anoxic basin, the Black Sea. Phylogenetic analysis of 16S ribosomal RNA gene sequences shows that these bacteria are related to members of the order Planctomycetales performing the anammox (anaerobic ammonium oxidation) process in ammonium-removing bioreactors. Nutrient profiles, fluorescently labelled RNA probes, 15N tracer experiments and the distribution of specific 'ladderane' membrane lipids indicate that ammonium diffusing upwards from the anoxic deep water is consumed by anammox bacteria below the oxic zone. This is the first time that anammox bacteria have been identified and directly linked to the removal of fixed inorganic nitrogen in the environment. The widespread occurrence of ammonium consumption in suboxic marine settings indicates that anammox might be important in the oceanic nitrogen cycle.

摘要

在许多海洋区域,固定无机氮(硝酸盐、亚硝酸盐和铵盐)的可利用性限制了初级生产力。异养细菌将硝酸盐转化为N₂(反硝化作用)被认为是海洋中固定无机氮的唯一重要汇。在此,我们提供证据表明,在世界上最大的缺氧盆地——黑海,存在细菌能利用亚硝酸盐将铵盐厌氧氧化为N₂。对16S核糖体RNA基因序列的系统发育分析表明,这些细菌与在去除铵盐的生物反应器中进行厌氧氨氧化(anammox)过程的浮霉菌目成员相关。营养物质分布、荧光标记RNA探针、¹⁵N示踪实验以及特定“梯烷”膜脂的分布表明,从缺氧深层水向上扩散的铵盐在有氧区下方被厌氧氨氧化细菌消耗。这是首次在环境中鉴定出厌氧氨氧化细菌并将其与固定无机氮的去除直接联系起来。在亚缺氧海洋环境中广泛存在铵盐消耗现象,这表明厌氧氨氧化在海洋氮循环中可能很重要。

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