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Occurrence of unusual steroids and hopanoids derived from aerobic methanotrophs at an active marine mud volcano

机译:在活跃的海洋泥火山中发生由好氧甲烷氧化菌衍生的不寻常的类固醇和类胡萝卜素

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Surface sediment samples from two microbial habitats (centre and adjacent Beggiatoa mats) at an active CH4-emitting Mud volcano on the Norwegian margin of the Barents Sea (Haakon Mosby Mud Volcano - HMMV) were analyzed for their steroid and hopanoid biomarker distributions and associated stable carbon isotopic composition. Substantial abundances of a suite of six steroids (four 4 alpha-methyl sterols and two 4 alpha-methyl steroid diols) and three hopanoids (diploptene, diplopterol and Delta(2) -diplopterol) were found, together with biomarkers from anaerobic methanotrophic consortia (ANME-3/Desulfobulbus aggregates) at the surface sediment of the mats. All of the steroid and hopanoid biomarkers, some not been described before, were substantially depleted in C-13 (delta(13) C between -77% and -68%), proving biosynthesis by an organism involved in methane consumption. Molecular analysis (16S rRNA sequencing and fluorescence in situ hybridisation) performed in a parallel study showed that, besides ANME-3/Desulfobulbus consortia, aerobic methanotrophs of the order Methylococcales are also abundant with high cell numbers. These independent findings suggest a spatially close vicinity of active aerobic and anaerobic methanotrophic communities on the order of millimetres, not reported before for the marine environment. At the centre location, where methane oxidation is performed solely by Methylococcales species, predominantly 4 alpha-methyl-3 beta-sterols, together with high abundances of specific fatty acids (i.e. C-16:1 omega 9c and C-16:1 omega 8c), were detected. The additional presence of new and unusual biomarkers for aerobic methanotrophy at the Beggiatoa mats seems to indicate either varying strains of Methylococcales types or an energy stress adaptation of the dominant species at the latter sampling site. Moreover, consideration is given to the new biomarkers being intermediates in the biosynthetic formation of steroids and hopanoids in methanotrophic bacteria. (C) 2007 Elsevier Ltd. All rights reserved.
机译:分析了来自巴伦支海挪威边缘一个活跃的CH4排放泥浆火山(Haakon Mosby Mud Volcano-HMMV)的两个微生物生境(中心和邻近的Beggiatoa垫)的表面沉积物样本的类固醇和类an生物标志物分布以及相关的稳定状态碳同位素组成。发现大量的六种类固醇(四个4α-甲基甾醇和两个4个α-甲基甾体二醇)和三个hop类化合物(双倍戊烯,双蝶呤和Delta(2)-双蝶呤),以及来自厌氧甲烷菌群的生物标志物( ANME-3 /脱硫球团聚集在垫子的表面沉积物中。所有的类固醇和类胡萝卜素生物标记物,其中一些以前未作描述,都被C-13大量消耗(δ(13)C在-77%和-68%之间),证明参与甲烷消耗的生物体能够进行生物合成。在一项平行研究中进行的分子分析(16S rRNA测序和荧光原位杂交)表明,除了ANME-3 / Desulfobulbus财团以外,甲基球菌菌的好氧甲烷氧化菌也很丰富,细胞数量很高。这些独立的发现表明,活跃的需氧和厌氧甲烷营养群落在空间上接近毫米级,这是海洋环境以前没有报道的。在中心位置,甲烷氧化仅由甲基球菌物种进行,主要是4种α-甲基-3β-固醇,以及大量的特定脂肪酸(即C-16:1ω9c和C-16:1ω 8c),被检测到。在Beggiatoa垫上,新的和不寻常的生物标记对好氧甲烷氧化菌的存在似乎表明,甲基球菌类型的菌株不同,或者在后一个采样点对优势种的能量胁迫适应能力强。此外,考虑了新的生物标志物是甲烷营养细菌中类固醇和类胡潘生物合成的中间体。 (C)2007 Elsevier Ltd.保留所有权利。

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