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Novel Euryarchaeotal Lineages Detected on Rice Roots and in the Anoxic Bulk Soil of Flooded Rice Microcosms

机译:水稻根部和缺水大米缺氧土壤中检测到的新Euryarchataltal谱系

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摘要

Because excised, washed roots of rice (Oryza sativa) immediately produce CH4 when they are incubated under anoxic conditions (P. Frenzel and U. Bosse, FEMS Microbiol. Ecol. 21:25–36, 1996), we employed a culture-independent molecular approach to identify the methanogenic microbial community present on roots of rice plants. Archaeal small-subunit rRNA-encoding genes were amplified directly from total root DNA by PCR and then cloned. Thirty-two archaeal rice root (ARR) gene clones were randomly selected, and the amplified primary structures of ca. 750 nucleotide sequence positions were compared. Only 10 of the environmental sequences were affiliated with known methanogens; 5 were affiliated with Methanosarcina spp., and 5 were affiliated with Methanobacterium spp. The remaining 22 ARR gene clones formed four distinct lineages (rice clusters I through IV) which were not closely related to any known cultured member of the Archaea. Rice clusters I and II formed distinct clades within the phylogenetic radiation of the orders “Methanosarcinales” and Methanomicrobiales. Rice cluster I was novel, and rice cluster II was closely affiliated with environmental sequences obtained from bog peat in northern England. Rice cluster III occurred on the same branch as Thermoplasma acidophilum and marine group II but was only distantly related to these taxa. Rice cluster IV was a deep-branching crenarchaeotal assemblage that was closely related to clone pGrfC26, an environmental sequence recovered from a temperate marsh environment. The use of a domain-specific oligonucleotide probe in a fluorescent in situ hybridization analysis revealed that viable members of the Archaea were present on the surfaces of rice roots. In addition, we describe a novel euryarchaeotal main line of descent, designated rice cluster V, which was detected in anoxic rice paddy soil. These results indicate that there is an astonishing richness of archaeal diversity present on rice roots and in the surrounding paddy soil.
机译:因为在缺氧条件下孵育后,切下的洗净的水稻根(Oryza sativa)会立即产生CH4(P。Frenzel和U. Bosse,FEMS Microbiol。Ecol。21:25-36,1996),因此我们采用了非培养分子方法鉴定水稻根部存在的产甲烷微生物群落。通过PCR直接从总根DNA中扩增古细菌小亚基rRNA编码基因,然后克隆。随机选择了32个古稻根(ARR)基因克隆,并扩增了约1个ca。比较了750个核苷酸序列位置。只有10个环境序列与已知的产甲烷菌有关。 5个隶属于甲烷菌属,5个隶属于甲烷杆菌属。其余的22个ARR基因克隆形成了四个不同的谱系(水稻簇I至IV),它们与古细菌的任何已知培养成员都没有密切的关系。水稻群集I和II在“甲烷藻”和“甲烷微粒”的系统发育辐射中形成了不同的进化枝。稻米群I是新颖的,而稻米群II与从英格兰北部沼泽泥炭中获得的环境序列紧密相关。水稻群III与嗜酸嗜热菌和海洋群II发生在同一分支上,但仅与这些类群有远距离的关系。水稻簇IV是一个深分支的crenarchaeotal组合,与克隆pGrfC26(从温带沼泽环境中回收的环境序列)密切相关。域特异性寡核苷酸探针在荧光原位杂交分析中的使用表明,古细菌的可行成员存在于稻根表面。另外,我们描述了一种在下降的缺氧稻田土壤中发现的新的欧洲人后裔主线,称为水稻簇V。这些结果表明,在稻根和周围的稻田土壤中存在着惊人的古细菌多样性。

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