Yang Xiao-Ru, Li Hu, Nie San-An, Su Jian-Qiang, Weng Bo-Sen, Zhu Gui-Bing, Yao Huai-Ying, Gilbert Jack A, Zhu Yong-Guan
Key Laboratory of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen, China.
Key Laboratory of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen, China University of Chinese Academy of Sciences, Beijing, China.
Appl Environ Microbiol. 2015 Feb;81(3):938-47. doi: 10.1128/AEM.02664-14. Epub 2014 Nov 21.
The anaerobic oxidation of ammonium (anammox) process has been observed in diverse terrestrial ecosystems, while the contribution of anammox to N2 production in paddy soils is not well documented. In this study, the anammox activity and the abundance and diversity of anammox bacteria were investigated to assess the anammox potential of 12 typical paddy soils collected in southern China. Anammox bacteria related to "Candidatus Brocadia" and "Candidatus Kuenenia" and two novel unidentified clusters were detected, with "Candidatus Brocadia" comprising 50% of the anammox population. The prevalence of the anammox was confirmed by the quantitative PCR results based on hydrazine synthase (hzsB) genes, which showed that the abundance ranged from 1.16 × 10(4) to 9.65 × 10(4) copies per gram of dry weight. The anammox rates measured by the isotope-pairing technique ranged from 0.27 to 5.25 nmol N per gram of soil per hour in these paddy soils, which contributed 0.6 to 15% to soil N2 production. It is estimated that a total loss of 2.50 × 10(6) Mg N per year is linked to anammox in the paddy fields in southern China, which implied that ca. 10% of the applied ammonia fertilizers is lost via the anammox process. Anammox activity was significantly correlated with the abundance of hzsB genes, soil nitrate concentration, and C/N ratio. Additionally, ammonia concentration and pH were found to be significantly correlated with the anammox bacterial structure.
在不同的陆地生态系统中均观察到了厌氧氨氧化(anammox)过程,然而,厌氧氨氧化对稻田土壤中N2产生的贡献尚无充分记录。在本研究中,对12种采自中国南方的典型稻田土壤的厌氧氨氧化活性、厌氧氨氧化细菌的丰度和多样性进行了调查,以评估其厌氧氨氧化潜力。检测到与“Candidatus Brocadia”和“Candidatus Kuenenia”相关的厌氧氨氧化细菌以及两个新的未鉴定菌群,其中“Candidatus Brocadia”占厌氧氨氧化菌总数的50%。基于肼合酶(hzsB)基因的定量PCR结果证实了厌氧氨氧化的普遍性,结果显示每克干重的丰度范围为1.16×10^4至9.65×10^4拷贝。在这些稻田土壤中,通过同位素配对技术测得的厌氧氨氧化速率为每克土壤每小时0.27至5.25 nmol N,占土壤N2产生量的0.6%至15%。据估计,中国南方稻田中与厌氧氨氧化相关的氮每年总损失量为2.50×10^6 Mg,这意味着约10%的施用氮肥通过厌氧氨氧化过程损失。厌氧氨氧化活性与hzsB基因丰度、土壤硝酸盐浓度和C/N比显著相关。此外,发现氨浓度和pH与厌氧氨氧化细菌结构显著相关。