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在斯瓦尔巴德的高北极温泉中,硫氧化化能自养细菌主导着微生物群。

Sulfur-oxidizing chemolithotrophic proteobacteria dominate the microbiota in high arctic thermal springs on Svalbard.

机构信息

Center for Geobiology, Department of Biology, University of Bergen, Bergen, Norway.

出版信息

Astrobiology. 2011 Sep;11(7):665-78. doi: 10.1089/ast.2010.0551. Epub 2011 Sep 7.

Abstract

The thermal springs Trollosen and Fisosen, located on the High Arctic archipelago Svalbard, discharge saline groundwaters rich in hydrogen sulfide and ammonium through a thick layer of permafrost. Large amounts of biomass that consist of filamentous microorganisms containing sulfur granules, as analyzed with energy dispersive X-ray analysis, were found in the outflow. Prokaryotic 16S rRNA gene libraries and quantitative polymerase chain reaction (qPCR) analyses reported bacteria of the γ- and ɛ-proteobacterial classes as the dominant organisms in the filaments and the planktonic fractions, closely related to known chemolithoautotrophic sulfur oxidizers (Thiotrix and Sulfurovum). Archaea comprised ∼1% of the microbial community, with the majority of sequences affiliated with the Thaumarchaeota. Archaeal and bacterial genes coding for a subunit of the enzyme ammonia monooxygenase (amoA) were detected, as well as 16S rRNA genes of Nitrospira, all of which is indicative of potential complete nitrification in both springs. 16S rRNA sequences related to methanogens and methanotrophs were detected as well. This study provides evidence that the microbial communities in Trollosen and Fisosen are sustained by chemolithotrophy, mainly through the oxidation of reduced sulfur compounds, and that ammonium and methane might be minor, additional sources of energy and carbon.

摘要

位于高北极斯瓦尔巴群岛的特罗尔松恩和菲斯松恩热泉通过一层厚厚的永冻层排放出富含硫化氢和氨的盐地下水。在流出物中发现了大量的生物质,这些生物质由含有硫颗粒的丝状微生物组成,如能量色散 X 射线分析所示。原核 16S rRNA 基因文库和定量聚合酶链反应 (qPCR) 分析报告称,γ-和ɛ-变形菌门的细菌是丝状生物和浮游生物部分的主要生物,与已知的化能自养硫氧化菌(硫杆菌属和硫硫杆菌属)密切相关。古菌约占微生物群落的 1%,大部分序列与泉古菌门有关。检测到编码氨单加氧酶 (amoA) 酶亚基的古菌和细菌基因,以及硝化螺菌属的 16S rRNA 基因,所有这些都表明这两个泉中都存在潜在的完全硝化作用。还检测到与产甲烷菌和甲烷氧化菌相关的 16S rRNA 序列。本研究表明,特罗尔松恩和菲斯松恩的微生物群落主要通过还原硫化合物的氧化作用得以维持,而氨和甲烷可能是次要的、额外的能量和碳源。

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