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Succession of methanogenic archaea in rice straw incorporated into a Japanese rice field: estimation by PCR-DGGE and sequence analyses

机译:日本稻田中稻草中产甲烷甲烷古菌的演替:通过PCR-DGGE估计和序列分析

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摘要

The succession and phylogenetic profiles of methanogenic archaeal communities associated with rice straw decomposition in rice-field soil were studied by polymerase chain reaction-denaturing gradient gel electrophoresis (PCR-DGGE) analysis followed by 16S rDNA sequencing. Nylon bags containing either leaf sheaths or blades were buried in the plowed layer of a Japanese rice field under drained conditions during the off-crop season and under flooded conditions after transplanting. In addition, rice straw samples that had been buried in the rice field under drained conditions during the off-crop season were temporarily removed during spring plowing and then re-buried in the same rice field under flooded conditions at transplanting. Populations of methanogenic archaea were examined by amplification of the 16S rRNA genes in the DNA extracted from the rice straw samples. No PCR product was produced for samples of leaf sheath or blade prior to burial or after burial under drained conditions, indicating that the methanogen population was very small during decomposition of rice straw under oxic conditions. Many common bands were observed in rice straw samples of leaf sheath and blade during decomposition of rice straw under flooded conditions. Cluster analysis based on DGGE patterns divided methanogenic archaeal communities into two groups before and after the mid-season drainage. Sequence analysis of DGGE bands that were commonly present were closely related to Methanomicrobiales and Rice cluster I. Methanomicrobiales, Rice cluster I and Methanosarcinales were major members before the mid-season drainage, whereas the DGGE bands that characterized methanogenic archaeal communities after the mid-season drainage were closely related to Methanomicrobiales. These results indicate that mid-season drainage affected the methanogenic archaeal communities irrespective of their location on rice straw (sheath and blade) and the previous history of decomposition during the off-crop season.
机译:通过聚合酶链反应-变性梯度凝胶电泳(PCR-DGGE)分析,然后进行16S rDNA测序,研究了稻田土壤中与稻草分解相关的产甲烷古细菌群落的演替和系统发育概况。含有叶鞘或叶片的尼龙袋被埋在日本稻田的耕层中,在非农作物生长季节处于排水条件下,而在移植后处于淹水条件下。另外,在春季耕作期间,将在非农作物季节在排水条件下埋没在稻田中的稻草样品临时移出,然后在移栽时在淹没条件下重新埋入同一稻田中。通过扩增从稻草样品中提取的DNA中的16S rRNA基因,检查产甲烷菌的种群。在排水条件下进行埋葬之前或之后,没有为叶鞘或叶片样品生成PCR产物,这表明在有氧条件下稻草分解过程中产甲烷菌的数量非常少。在淹没条件下稻草分解期间,在稻草的叶片鞘和叶片样品中观察到许多共同的谱带。基于DGGE模式的聚类分析将产甲烷的古生菌群落分为中,季排水前后两组。经常出现的DGGE带的序列分析与甲烷微粒和水稻簇I密切相关。甲烷微粒,水稻簇I和甲烷菌鼻藻是季中排水之前的主要成员,而DGGE带是季后甲烷化古生菌群落的特征。引流与甲烷微粒有关。这些结果表明,季中排水影响产甲烷的古生菌群落,而不论它们在稻草上(鞘和叶片)的位置以及非农作物季节以前的分解史。

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