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A review of ammonia-oxidizing bacteria and archaea in Chinese soils

机译:中国土壤中氨氧化细菌和古细菌的研究进展

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摘要

Ammonia (NH3) oxidation, the first and rate-limiting step of nitrification, is a key step in the global Nitrogen (N) cycle. Major advances have been made in recent years in our knowledge and understanding of the microbial communities involved in ammonia oxidation in a wide range of habitats, including Chinese agricultural soils. In this mini-review, we focus our attention on the distribution and community diversity of ammonia-oxidizing bacteria (AOB) and ammonia oxidizing archaea (AOA) in Chinese soils with variable soil properties and soil management practices. The niche differentiation of AOB and AOA in contrasting soils have been functionally demonstrated using DNA-SIP (stable isotope probing) methods, which have shown that AOA dominate nitrification processes in acidic soils, while AOB dominated in neutral, alkaline and N-rich soils. Finally, we discuss the composition and activity of ammonia oxidizers in paddy soils, as well as the mitigation of the greenhouse gas nitrous oxide (N2O) emissions and nitrate leaching via inhibition of nitrification by both AOB and AOA.
机译:氨(NH3)氧化是硝化的第一步,也是限速步骤,是全球氮(N)循环的关键步骤。近年来,我们对包括中国农业土壤在内的多种生境中氨氧化所涉及的微生物群落的认识和了解已取得重大进展。在本小型审查中,我们将重点放在具有可变土壤特性和土壤管理实践的中国土壤中的氨氧化细菌(AOB)和氨氧化古细菌(AOA)的分布和群落多样性。使用DNA-SIP(稳定同位素探测)方法已在功能上证明了AOB和AOA在生态土壤中的生态位分化,这表明AOA在酸性土壤中的硝化过程中占主导地位,而AOB在中性,碱性和富氮土壤中则占主导地位。最后,我们讨论了稻田土壤中氨氧化剂的组成和活性,以及​​通过抑制AOB和AOA硝化作用来减轻温室气体一氧化二氮(N2O)排放和硝酸盐浸出。

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