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首页> 外文期刊>FEMS Microbiology Ecology >Quantification of mcrA by quantitative fluorescent PCR in sediments from methane seep of the Nankai Trough
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Quantification of mcrA by quantitative fluorescent PCR in sediments from methane seep of the Nankai Trough

机译:通过定量荧光PCR定量分析南海海槽甲烷渗流沉积物中的mcrA

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摘要

A quantitative fluorogenic PCR method for group-specific methyl coenzyme M reductase subunit A genes (mcrA) from methanotrophic archaea was established and applied to the characterization of microbial communities in anoxic methane seep sediments at the accretionary prism of the Nankai Trough. All of the previously identified subgroups of anaerobic methanotroph (ANME) mcrA genes were detected in the cores up to 25 cm below the seafloor, but distributional patterns of mcrA genes were found to differ according to depth. These findings suggest a distinct distribution of phylogenetically and physiologically diverse methanotrophic archaea that mediate methane oxidation in the anoxic sediments. This quantification method will contribute to future investigations of methanotrophic microbial ecosystems in anoxic marine sediments.
机译:建立了甲烷营养古细菌群体特异性甲基辅酶M还原酶亚基A基因(mcrA)的定量荧光PCR方法,并将其用于表征南开槽增生棱镜上缺氧甲烷渗透沉积物中的微生物群落。在海底以下最多25 cm的岩心中检测到了所有先前确定的厌氧甲烷营养(ANME)mcrA基因亚组,但发现mcrA基因的分布模式根据深度而有所不同。这些发现表明,系统发育和生理学上不同的甲烷营养古菌的独特分布,介导了缺氧沉积物中的甲烷氧化。这种量化方法将有助于未来研究缺氧海洋沉积物中的甲烷营养微生物生态系统。

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