Towards a more labor-saving way in microbial ammonium oxidation: A review on complete ammonia oxidization (comammox)

硝化作用 氮气循环 硝酸盐 氨单加氧酶 环境化学 生态系统 营养污染 环境科学 化学 生态学 氮气 生物 污染 有机化学
作者
Guibing Zhu,Xiaomin Wang,Shanyun Wang,Longbin Yu,Gawhar Armanbek,Jie Yu,Liping Jiang,Dongdan Yuan,Zhongrui Guo,Hanrui Zhang,Lei Zheng,Lorenz Schwark,Mike S. M. Jetten,Asheesh Kumar Yadav,Yong‐Guan Zhu
出处
期刊:Science of The Total Environment [Elsevier BV]
卷期号:829: 154590-154590 被引量:86
标识
DOI:10.1016/j.scitotenv.2022.154590
摘要

In the Anthropocene, nitrogen pollution is becoming an increasing challenge for both mankind and the Earth system. Microbial nitrogen cycling begins with aerobic nitrification, which is also the key rate-limiting step. For over a century, it has been accepted that nitrification occurs sequentially involving ammonia oxidation, which produces nitrite followed by nitrite oxidation, generating nitrate. This perception was changed by the discovery of comammox Nitrospira bacteria and their metabolic pathway. In addition, this also provided us with new knowledge concerning the complex nitrogen cycle network. In the comammox process, ammonia can be completely oxidized to nitrate in one cell via the subsequent activity of the enzyme complexes, ammonia monooxygenase, hydroxylamine dehydrogenase, and nitrite oxidodreductase. Over the past five years, research on comammox made great progress. However, there still exist a lot of questions, including how much does comammox contribute to nitrification? How large is the diversity and are there new strains to be discovered? Do comammox bacteria produce the greenhouse gas N2O, and how or to which extent may they contribute to global climate change? The above four aspects are of great significance on the farmland nitrogen management, aquatic environment restoration, and mitigation of global climate change. As large number of comammox bacteria and pathways have been detected in various terrestrial and aquatic ecosystems, indicating that the comammox process may exert an important role in the global nitrogen cycle.
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