Potential role of nitrite-dependent anaerobic methane oxidation in methane consumption and nitrogen removal in Chinese paddy fields

• DOI: 10.1016/j.scitotenv.2022.156534
• Publication Date: 2022-06-06T15:09:53Z
• Authors: Wang-ting Yang; Wei-qi Wang; Li-dong Shen; Ya-nan Bai; Xin Liu; Mao-hui Tian; Chun Wang; Yan-fang Feng; Yang Liu; Yu-ling Yang; Jia-qi Liu; Cai-yu Geng
• Keywords: Bacteria; Nitrogen; 15. Life on land; 01 natural sciences; Carbon; 6. Clean water; Soil; 13. Climate action; RNA, Ribosomal, 16S; Denitrification; Anaerobiosis; Methane; Oxidation-Reduction; Nitrites; Phylogeny; 0105 earth and related environmental sciences

Nitrite-dependent anaerobic methane oxidation (n-damo), catalyzed by bacteria closely related to Candidatus Methylomirabilis oxyfera, links the global carbon and nitrogen cycles. Currently, the contribution of n-damo in controlling methane emissions and nitrogen removal, and the key regulatory factors of this process in Chinese paddy fields are poorly known. Here, soil samples from 20 paddy fields located in different climate zones across China were collected to examine the n-damo activity and bacterial communities. The n-damo activity and bacterial abundance varied from 1.05 to 5.97 nmol CH4 g-1 (dry soil) d-1 and 2.59 × 105 to 2.50 × 107 copies g-1 dry soil, respectively. Based on the n-damo activity, it was estimated that approximately 0.91 Tg CH4 and 2.17 Tg N could be consumed annually via n-damo in Chinese paddy soils. The spatial variations in n-damo activity and community structure of n-damo bacteria were significantly (p < 0.05) affected by the soil ammonium content, labile organic carbon content and pH. Furthermore, significant differences in n-damo activity, bacterial abundance and community composition were observed among different climate zones. The n-damo activity was found to be positively correlated with the mean annual air temperature. Taken together, our results demonstrated the potential importance of n-damo in both methane consumption and nitrogen removal in Chinese paddy soils, and this process was regulated by local soil and climatic factors.