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Stratification of Archaea in the Deep Sediments of a Freshwater Meromictic Lake: Vertical Shift from Methanogenic to Uncultured Archaeal Lineages

机译:淡水湖泊中沉积物中古生菌的分层:从产甲烷到未培养古生菌世系的垂直转移

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摘要

As for lineages of known methanogens, several lineages of uncultured archaea were recurrently retrieved in freshwater sediments. However, knowledge is missing about how these lineages might be affected and structured according to depth. In the present study, the vertical changes of archaeal communities were characterized in the deep sediment of the freshwater meromictic Lake Pavin. For that purpose, an integrated molecular approach was performed to gain information on the structure, composition, abundance and vertical stratification of archaeal communities thriving in anoxic freshwater sediments along a gradient of sediments encompassing 130 years of sedimentation. Huge changes occurred in the structure and composition of archaeal assemblages along the sediment core. Methanogenic taxa (i.e. Methanosaeta and Methanomicrobiales) were progressively replaced by uncultured archaeal lineages (i.e. Marine Benthic Group-D (MBG-D) and Miscellaneous Crenarchaeal Group (MCG)) which are suspected to be involved in the methane cycle.
机译:至于已知产甲烷菌的血统,经常从淡水沉积物中回收数个未培养的古细菌。但是,缺少有关这些血统如何根据深度受到影响和构造的知识。在本研究中,古生菌群落的垂直变化以淡水淡紫色的帕文湖的深层沉积为特征。为此目的,进行了一种综合分子方法,以获取关于缺氧淡水沉积物中沿包括沉积130年的沉积物梯度而繁盛的古细菌群落的结构,组成,丰度和垂直分层的信息。沿沉积物核心的古细菌群的结构和组成发生了巨大变化。产甲烷类群(即甲烷菌和甲烷微粒)逐渐被未培养的古细菌谱系(即海洋底栖动物D组(MBG-D)和杂甲鱼科(MCG))所取代,它们涉嫌参与甲烷循环。

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