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Effects of enclosure time on the community composition of methanotrophs in the soils of the Inner Mongolia grasslands

机译:围封时间对内蒙古草原土壤甲烷营养菌群落组成的影响

摘要

Despite the great number of studies about methane uptake and its response to grazing in the Inner Mongolia grasslands, only a few focused on the methanotrophic composition. This study aimed to investigate the methanotrophic community structure and abundance, then to analyze the abiotic driving factors of methanotrophic community structure in different enclosed times in this area. In this study we chose typical grasslands in the Xilin River Basin of Inner Mongolia, China to investigate methanotrophic community structure and abundance under different enclosure treatments as follows: 79E (grassland enclosed since 1979), 99E (grassland enclosed since 1999), and G (freely grazed grassland). A clone library was used to reveal the methanotroph community structure, and their relationships with abiotic factors were analyzed by redundancy analysis. Methanotroph abundance was determined by real-time PCR. The OTUs of the three treatments mainly belonged to Type I methanotrophs, probably caused by the high pH value. Among all OTUs, only OTU1 belonged to upland soil cluster gamma (USC-gamma), whose abundance was the largest in all OTUs, indicating the USC-gamma cluster was the main one to oxidize CH4 in the Inner Mongolia grasslands. Methanotrophic abundance (represented by the pmoA gene copies per gram of dry weight soil) decreased with the enclosure time as G (4.5 x 10(7)) > 99E (2.8 x 10(7)) > 79E (2.0 x 10(7)), mainly caused by the lower soil moisture content in G. Lower soil moisture content facilitates more CH4 and O-2 diffusive into soil thus leading to the proliferation of methanotrophs. This study found a high abundance of methanotrophs in the soils of the Inner Mongolia grasslands, with the USC-gamma cluster having the largest abundance, which may play a key role in oxidizing CH4 in the Inner Mongolia grasslands. Combined with those of previous studies, the results showed an obvious change of methanotrophic community composition with the increase of enclosure time.
机译:尽管在内蒙古草原上进行了大量关于甲烷吸收及其对放牧的反应的研究,但只有少数研究集中在甲烷营养成分上。这项研究旨在调查甲烷营养群落结构和丰富度,然后分析该地区不同封闭时间甲烷营养群落结构的非生物驱动因素。在这项研究中,我们选择了中国内蒙古锡林河流域的典型草地,研究了不同围封处理下的甲烷营养群落结构和丰度:79E(1979年以来围封的草地),99E(1999年以来围封的草地)和G(自由放牧的草原)。使用克隆文库揭示甲烷营养菌的群落结构,并通过冗余分析分析它们与非生物因子的关系。通过实时PCR测定甲烷营养菌的丰度。三种处理的OTUs主要属于I型甲烷营养菌,可能是由于高pH值引起的。在所有OTU中,只有OTU1属于高地土壤簇γ(USC-γ),其丰度在所有OTU中最大,表明USC-γ簇是内蒙古草原氧化CH4的主要簇。甲烷营养水平的丰度(以每克干重土壤的pmoA基因拷贝数表示)随封闭时间而降低,因为G(4.5 x 10(7))> 99E(2.8 x 10(7))> 79E(2.0 x 10(7) ),主要是由于G中较低的土壤含水量引起的。较低的土壤含水量有助于更多的CH4和O-2扩散到土壤中,从而导致甲烷营养生物的扩散。这项研究发现内蒙古草原土壤中甲烷氧化菌的含量很高,其中USC-γ团簇的丰度最大,这可能在内蒙古草原氧化CH4方面起着关键作用。结合以前的研究,结果表明,随着封闭时间的增加,甲烷营养群落组成发生了明显变化。

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