Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Sci Total Environ. 2022 Jul 10;829:154590. doi: 10.1016/j.scitotenv.2022.154590. Epub 2022 Mar 17.
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 NO, 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.
在人类世,氮污染正成为人类和地球系统面临的一个日益严峻的挑战。微生物氮循环始于好氧硝化作用,它也是关键的限速步骤。一个多世纪以来,人们一直认为硝化作用是依次发生的,包括氨氧化,产生亚硝酸盐,然后亚硝酸盐氧化,生成硝酸盐。然而,厚壁菌门的 comammox 细菌及其代谢途径的发现改变了这一认知。此外,这也为我们提供了有关复杂氮循环网络的新知识。在 comammox 过程中,氨可以通过氨单加氧酶、羟胺脱氢酶和亚硝酸盐氧化还原酶等酶复合物的后续活性在一个细胞中被完全氧化为硝酸盐。在过去的五年中,对 comammox 的研究取得了很大的进展。然而,仍有许多问题尚未解决,包括 comammox 对硝化作用的贡献有多大?多样性有多大,是否有新的菌株有待发现?comammox 细菌是否会产生温室气体 NO,以及它们可能在多大程度上导致全球气候变化?这四个方面对于农田氮管理、水环境保护以及缓解全球气候变化都具有重要意义。由于在各种陆地和水生生态系统中都检测到了大量的 comammox 细菌和途径,这表明 comammox 过程可能在全球氮循环中发挥着重要作用。