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Dry/Wet Cycles Change the Activity and Population Dynamics of Methanotrophs in Rice Field Soil

机译:干/湿循环改变稻田土壤中甲烷菌的活性和种群动态

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The methanotrophs in rice field soil are crucial in regulating the emission of methane. Drainage substantially reduces methane emission from rice fields. However, it is poorly understood how drainage affects microbial methane oxidation. Therefore, we analyzed the dynamics of methane oxidation rates, composition (using terminal restriction fragment length polymorphism [T-RFLP]), and abundance (using quantitative PCR [qPCR]) of methanotroph pmoA genes (encoding a subunit of particulate methane monooxygenase) and their transcripts over the season and in response to alternate dry/wet cycles in planted paddy field microcosms. In situ methane oxidation accounted for less than 15% of total methane production but was enhanced by intermittent drainage. The dry/wet alternations resulted in distinct effects on the methanotrophic communities in different soil compartments (bulk soil, rhizosphere soil, surface soil). The methanotrophic communities of the different soil compartments also showed distinct seasonal dynamics. In bulk soil, potential methanotrophic activity and transcription of pmoA were relatively low but were significantly stimulated by drainage. In contrast, however, in the rhizosphere and surface soils, potential methanotrophic activity and pmoA transcription were relatively high but decreased after drainage events and resumed after reflooding. While type II methanotrophs dominated the communities in the bulk soil and rhizosphere soil compartments (and to a lesser extent also in the surface soil), it was the pmoA of type I methanotrophs that was mainly transcribed under flooded conditions. Drainage affected the composition of the methanotrophic community only minimally but strongly affected metabolically active methanotrophs. Our study revealed dramatic dynamics in the abundance, composition, and activity of the various type I and type II methanotrophs on both a seasonal and a spatial scale and showed strong effects of dry/wet alternation cycles, which enhanced the attenuation of methane flux into the atmosphere.
机译:稻田土壤中的甲烷营养菌对于调节甲烷的排放至关重要。排水大大减少了稻田的甲烷排放。然而,人们很少了解排水如何影响微生物甲烷的氧化。因此,我们分析了甲烷氧化菌pmoA基因(编码颗粒甲烷单加氧酶的一个亚基)的甲烷氧化速率,组成(使用末端限制性片段长度多态性[T-RFLP])和丰度(使用定量PCR [qPCR])的动力学和在整个稻田中,以及在种植后的稻田缩影中响应交替的干/湿循环时,它们的转录本。原位甲烷氧化仅占甲烷总产量的不到15%,但间歇性排水可增强甲烷氧化。干/湿交替对不同土壤区室(疏散土壤,根际土壤,表层土壤)的甲烷营养群落产生明显影响。不同土壤区室的甲烷营养群落也表现出明显的季节动态。在散装土壤中,潜在的甲烷营养活性和pmoA的转录水平相对较低,但受到排水的刺激。相反,在根际和表层土壤中,潜在的甲烷营养活性和pmoA转录水平相对较高,但在排水事件发生后降低,而在重新注水后恢复。虽然II型甲烷营养生物在整个土壤和根际土壤区隔中占主导地位(在较小程度上也在表层土壤中),但I型甲烷营养生物的pmoA主要在淹水条件下转录。排水对甲烷营养群落的组成影响很小,但对代谢活性甲烷营养的影响很大。我们的研究揭示了季节和空间尺度上各种I型和II型甲烷营养生物的丰度,组成和活性的动态变化,并显示了干/湿交替循环的强烈影响,这增强了甲烷通入甲烷气的衰减。大气层。

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