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A methane-driven microbial food web in a wetland rice soil

机译:湿地水稻土中甲烷驱动的微生物食物网

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摘要

Methane oxidation is a key process controlling methane emission from anoxic habitats into the atmosphere. Methanotrophs, responsible for aerobic methane oxidation, do not only oxidize but also assimilate methane. Once assimilated, methane carbon may be utilized by other organisms. Here we report on a microbial food web in a rice field soil driven by methane. A thin layer of water-saturated rice field soil was incubated under opposing gradients of oxygen and C-13-labelled methane. Bacterial and eukaryotic communities incorporating methane carbon were analysed by RNA-stable isotope probing (SIP). Terminal restriction fragment length polymorphism (T-RFLP) and cloning showed that methanotrophs were the most prominent group of bacteria incorporating methane carbon. In addition, a few Myxobacteria-related sequences were obtained from the 'heavy' rRNA fraction. Denaturing gradient gel electrophoresis (DGGE) targeting 18S rRNA detected various groups of protists in the 'heavy' rRNA fraction including naked amoeba (Lobosea and Heterolobosea), ciliates (Colpodea) and flagellates (Cercozoa). Incubation of soil under different methane concentrations in air resulted in the development of distinct protozoan communities. These results suggest that methane carbon is incorporated into non-methanotrophic pro- and microeukaryotes probably via grazing, and that methane oxidation is a shaping force of the microeukaryotic community depending on methane availability.
机译:甲烷氧化是控制甲烷从缺氧栖息地向大气排放的关键过程。甲烷营养菌,负责好氧甲烷的氧化,不仅氧化而且吸收甲烷。一旦被吸收,甲烷碳可被其他生物利用。在这里,我们报道了甲烷驱动的稻田土壤中的微生物食物网。在氧气和C-13标记的甲烷的相反梯度下孵育一薄层水饱和的稻田土壤。通过RNA稳定同位素探测(SIP)分析了含有甲烷碳的细菌和真核生物群落。末端限制性片段长度多态性(T-RFLP)和克隆表明,甲烷氧化菌是掺入甲烷碳的最主要细菌。此外,从“重” rRNA片段中获得了一些与粘杆菌相关的序列。靶向18S rRNA的变性梯度凝胶电泳(DGGE)在“重” rRNA组分中检测到各种不同的原生生物,包括裸阿米巴(Lobosea和Heterolobosea),纤毛虫(Colpodea)和鞭毛虫(Cercozoa)。在空气中甲烷浓度不同的情况下,土壤的孵化导致形成独特的原生动物群落。这些结果表明,甲烷碳很可能通过放牧并入非亚甲基营养原核生物和微真核生物,并且甲烷氧化是微真核生物群落的形成力,具体取决于甲烷的可利用性。

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