Leng Lingqin, Chang Jiali, Geng Kan, Lu Yahai, Ma Ke
College of Resources and Environmental Sciences, China Agricultural University, Beijing, 100193, China.
Microb Ecol. 2015 Jul;70(1):88-96. doi: 10.1007/s00248-014-0540-0. Epub 2014 Dec 5.
Methanotrophs are crucial in regulating methane emission from rice field systems. Type II methanotrophs in particular are often observed in high abundance in paddy soil. Some cultivated species of Methylocystis are able to grow on acetate in the absence of methane. We hypothesize that the dominant type II methanotrophs in paddy soil might facultatively utilize acetate for growth, which we evaluate in the present study. The measurement of methane oxidation rates showed that the methanotrophic activity in paddy soil was inhibited by the addition of acetate compared to the continuous supplementation of methane, but the paddy soil maintained the methane oxidation capacity and recovered following methane supplementation. Terminal restriction fragment length polymorphism analysis (T-RFLP) combined with cloning and sequencing of pmoA genes showed that Methylocystis was enriched after incubation with added acetate, while the type I methanotrophs Methylocaldum/Methylococcus and Methylobacter were enriched by methane supplementation. A comparison of pmoA sequences obtained in this study with those in the public database indicated that they were globally widespread in paddy soils or in associated with rice roots. Furthermore, we performed stable isotope probing (SIP) of pmoA messenger RNA (mRNA) to investigate the assimilation of (13)C-acetate by paddy soil methanotrophs. RNA-SIP revealed that Methylocystis-related methanotrophs which shared the same genotype of the above enriched species were significantly labelled. It indicates that these methanotrophs actively assimilated the labelled acetate in paddy soil. Altogether, these results suggested that uncultivated Methylocystis species are facultative methanotrophs utilizing acetate as a secondary carbon source in paddy soil.
甲烷氧化菌在调控稻田系统甲烷排放方面至关重要。特别是II型甲烷氧化菌在稻田土壤中常常大量存在。一些甲基孢囊菌的培养物种能够在没有甲烷的情况下利用乙酸盐生长。我们假设稻田土壤中占主导地位的II型甲烷氧化菌可能兼性利用乙酸盐进行生长,本研究对此进行评估。甲烷氧化速率的测量表明,与持续补充甲烷相比,添加乙酸盐会抑制稻田土壤中的甲烷氧化活性,但稻田土壤保持了甲烷氧化能力,且在补充甲烷后得以恢复。末端限制性片段长度多态性分析(T-RFLP)结合pmoA基因的克隆和测序表明,添加乙酸盐孵育后甲基孢囊菌富集,而补充甲烷则使I型甲烷氧化菌甲基暖菌属/甲基球菌属和甲基杆菌属富集。将本研究获得的pmoA序列与公共数据库中的序列进行比较表明,它们在稻田土壤中或与水稻根系相关的区域广泛分布。此外,我们对pmoA信使核糖核酸(mRNA)进行了稳定同位素探测(SIP),以研究稻田土壤甲烷氧化菌对(13)C-乙酸盐的同化作用。RNA-SIP显示,与上述富集物种具有相同基因型的与甲基孢囊菌相关的甲烷氧化菌被显著标记。这表明这些甲烷氧化菌在稻田土壤中积极同化标记的乙酸盐。总之,这些结果表明,未培养的甲基孢囊菌物种是兼性甲烷氧化菌,在稻田土壤中利用乙酸盐作为第二碳源。