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通过稳定同位素探测揭示英国塞文河口潮汐沉积物不同生物地球化学深度带中的原核生物功能多样性。

Prokaryotic functional diversity in different biogeochemical depth zones in tidal sediments of the Severn Estuary, UK, revealed by stable-isotope probing.

机构信息

Cardiff School of Biosciences, Cardiff University, Wales, UK.

出版信息

FEMS Microbiol Ecol. 2010 May;72(2):179-97. doi: 10.1111/j.1574-6941.2010.00848.x. Epub 2010 Feb 15.

Abstract

Stable isotope probing of prokaryotic DNA was used to determine active prokaryotes using (13)C-labelled substrates (glucose, acetate, CO(2)) in sediment slurries from different biogeochemical zones of the Severn Estuary, UK. Multiple, low concentrations (5 x 100 microM) of (13)C-substrate additions and short-term incubations (7 days) were used to minimize changes in the prokaryotic community, while achieving significant (13)C-incorporation. Analysis demonstrated clear metabolic activity within all slurries, although neither the net sulphate removal nor CH(4) production occurred in the anaerobic sulphate reduction and methanogenesis zone slurries. Some similarities occurred in the prokaryotic populations that developed in different sediment slurries, particularly in the aerobic and dysaerobic zone slurries with (13)C-glucose, which were dominated by Gammaproteobacteria and Marine Group 1 Archaea, whereas both anaerobic sediment slurries incubated with (13)C-acetate showed incorporation into Epsilonproteobacteria and other bacteria, with the sulphate reduction zone slurry also showing (13)C-acetate utilization by Miscellaneous Crenarchaeotic Group Archaea. The lower potential energy methanogenesis zone slurries were the only conditions where no (13)C-incorporation into Archaea occurred, despite Bacteria being labelled; this was surprising because Archaea have been suggested to be adapted to low-energy conditions. Overall, our results highlight that uncultured prokaryotes play important ecological roles in tidal sediments of the Severn Estuary, providing new metabolic information for novel groups of Archaea and suggesting broader metabolisms for largely uncultivated Bacteria.

摘要

采用稳定同位素探针技术,利用(13)C 标记的葡萄糖、乙酸盐、CO2 等底物,对英国塞文河口不同生物地球化学区的沉积物悬浮液中的活性原核生物进行了研究。采用多次添加低浓度(5×100μM)(13)C 底物和短期培养(7 天)的方法,最大限度地减少原核生物群落的变化,同时实现显著的(13)C 掺入。分析表明,所有悬浮液中都存在明显的代谢活性,尽管在缺氧硫酸盐还原和产甲烷区的悬浮液中既没有净硫酸盐去除,也没有 CH4 产生。在不同沉积物悬浮液中培养的原核生物种群存在一些相似之处,特别是在好氧和乏氧区的(13)C-葡萄糖悬浮液中,主要由γ变形菌纲和海洋组 1 古菌组成,而用(13)C-乙酸盐培养的两种缺氧沉积物悬浮液均显示出 ε变形菌纲和其他细菌的掺入,硫酸盐还原区的悬浮液还显示出古菌利用(13)C-乙酸盐,而较低潜能的产甲烷区的悬浮液则是唯一没有发生(13)C 掺入古菌的条件,尽管细菌被标记;这令人惊讶,因为古菌被认为适应于低能量条件。总体而言,我们的结果强调了未培养的原核生物在塞文河口潮汐沉积物中发挥着重要的生态作用,为新型古菌群提供了新的代谢信息,并暗示了广泛未培养细菌的代谢途径。

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