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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Bacteriohopanepolyols in a stratified cyanobacterial mat from Kiritimati (Christmas Island, Kiribati)
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Bacteriohopanepolyols in a stratified cyanobacterial mat from Kiritimati (Christmas Island, Kiribati)

机译:来自基里蒂马蒂(基里巴斯圣诞节岛)的层状蓝藻垫中的细菌型霍帕烷多元醇

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Bacteriohopanepolyols (BHPs) are lipids of distinct bacterial groups and are, along with geohopanoids as their diagenetic products, ubiquitous in microbial mats, sediments, soils and oil. Among BHP-producing bacteria, Cyanobacteria are of special interest since occurrences of C-2 methylated and other geohopanoids are interpreted as signals of oxygenic photoautotrophs in the early oceans. However, many questions, with respect to the source and function of hopanoids, remain open. Cyanobacterial mats are complex systems in terms of biogeochemical zones and hence, harbor phylogenetically and metabolically diverse photoautotrophic and heterotrophic microorganisms. Whereas Cyanobacteria are key microbial players for carbon fixation in these mat systems, most other bacterial and archaeal groups feed on their metabolic products and/or perform anoxygenic photosynthesis in deeper low-light regimes.We have analyzed the abundance and distribution of BHPs in distinct layers of a stratified mat from a hypersaline lake on Kiritimati. Suites of BHPs were observed, with the majority probably originating from (proteo-)bacteria thriving in the deeper layers of the mat and not in upper layers where mat-forming Cyanobacteria are prevalent. Interestingly, the BHPs in the deepest layer include C-2 methylated structures, which likely do not originate from Cyanobacteria, but rather from α-Proteobacteria thriving at the redoxcline of this stratified microbial system.
机译:细菌类庚烷多元醇(BHP)是不同细菌类的脂质,并且与作为类成岩产物的类人猿一样,在微生物垫,沉积物,土壤和石油中普遍存在。在产生BHP的细菌中,蓝细菌特别受关注,因为C-2甲基化和其他类类大地生物的发生被解释为早期海洋中氧合自养生物的信号。但是,关于类胡桃碱的来源和功能的许多问题仍未解决。就生物地球化学区域而言,蓝藻席子是复杂的系统,因此,它们在系统发育和代谢上具有多种光合自养和异养微生物。蓝细菌是这些垫系统中碳固定的关键微生物,而大多数其他细菌和古细菌群体以其代谢产物为食并/或在更深的弱光条件下进行产氧光合作用。基里蒂马蒂的超盐湖分层垫观察到了必和必拓的套件,其中大多数可能起源于(蛋白)细菌,在垫层的较深层而不是在形成垫层的蓝细菌很普遍的上层繁荣。有趣的是,最深层中的BHP包括C-2甲基化结构,这可能不是起源于蓝细菌,而是起源于在这种分层微生物系统的氧化还原层上繁盛的α-变形杆菌。

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