生物
缺氧水域
古细菌
微生物垫
甲烷微生物
甲烷
石油渗漏
甲烷厌氧氧化
克雷纳恰奥塔
甲烷利用细菌
甲烷菌
产甲烷
生态学
甲烷八叠球菌
细菌
古生物学
蓝藻
作者
Takuro Nunoura,Hanako Oida,Tomohiro Toki,Juichiro Ashi,Ken Takai,Koki Horikoshi
标识
DOI:10.1111/j.1574-6941.2006.00101.x
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.
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