Key Laboratory of Marine Biogenetic Resources, Third Institute of Oceanography, State Oceanic Administration, Xiamen, 361005, People's Republic of China.
Antonie Van Leeuwenhoek. 2011 May;99(4):739-51. doi: 10.1007/s10482-011-9548-3. Epub 2011 Jan 13.
Microorganisms are known to play fundamental roles in the biogeochemical cycling of carbon in the coastal environments. To get to know the composition and ecological roles of the archaeal communities within the sediments of the Pearl River Estuary, Southern China, the diversity and vertical distribution of archaea in a sediment core was reported based on the 16S rRNA and mcrA genes for the first time. Quantitative PCR analysis revealed that archaea were present at 10(6)-10(7) 16S rRNA gene copies/g (wet weight) in the sediment core, and the proportion of mcrA versus 16S rRNA gene copies varied from 11 to 45%. 16S rRNA gene libraries were constructed and analyzed for the top layer (0-6 cm), middle layer (18-24 cm), sulfate-methane transition zone (SMTZ, 32-42 cm), and bottom layer (44-50 cm) sediments. The results indicated that Miscellaneous Crenarchaeotal Group (MCG) was the main component in the sediments. The MCG archaea could be further divided into six subgroups: MCG-A, B, C, D, E, and F. On the other hand, mcrA sequences from methanogens related to the order Methanomicrobiales and ANME-2 methanotrophs were detected in all sediment layers. Taken together, our data revealed a largely unknown archaeal community in which MCG dominated within the Pearl River estuarine sediments, while methanogens and methane-oxidizing archaea putatively involving in methane metabolism, were also found in the community. This is the first important step towards elucidating the biogeochemical roles of these archaea in the Pearl River Estuary.
微生物在沿海环境的碳生物地球化学循环中起着至关重要的作用。为了了解中国南方珠江口沉积物中古菌的组成和生态作用,首次基于 16S rRNA 和 mcrA 基因报道了沉积物中古菌的多样性和垂直分布。定量 PCR 分析显示,古菌在沉积物核心中存在于 10(6)-10(7) 16S rRNA 基因拷贝/g(湿重),并且 mcrA 与 16S rRNA 基因拷贝的比例从 11%到 45%不等。构建并分析了表层(0-6 cm)、中层(18-24 cm)、硫酸盐-甲烷过渡区(SMTZ,32-42 cm)和底层(44-50 cm)沉积物的 16S rRNA 基因文库。结果表明,混杂古菌群(MCG)是沉积物中的主要成分。MCG 古菌可进一步分为六个亚群:MCG-A、B、C、D、E 和 F。另一方面,在所有沉积物层中都检测到与甲烷微菌目相关的产甲烷菌和 ANME-2 甲烷氧化古菌的 mcrA 序列。总之,我们的数据揭示了一个在珠江口河口沉积物中占主导地位的古菌群落,其中 MCG 占主导地位,而参与甲烷代谢的产甲烷菌和甲烷氧化古菌也存在于该群落中。这是阐明这些古菌在珠江口的生物地球化学作用的重要第一步。
Antonie Van Leeuwenhoek. 2011-1-13
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