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欧洲高山永久冻土和活动层中的微生物多样性。

Microbial diversity in European alpine permafrost and active layers.

作者信息

Frey Beat, Rime Thomas, Phillips Marcia, Stierli Beat, Hajdas Irka, Widmer Franco, Hartmann Martin

机构信息

Forest Soils and Biogeochemistry, Swiss Federal Research Institute WSL, Birmensdorf, Switzerland.

Snow and Permafrost, WSL Institute for Snow and Avalanche Research SLF, Davos, Switzerland.

出版信息

FEMS Microbiol Ecol. 2016 Mar;92(3). doi: 10.1093/femsec/fiw018. Epub 2016 Jan 31.

DOI:10.1093/femsec/fiw018
PMID:26832204
Abstract

Permafrost represents a largely understudied genetic resource. Thawing of permafrost with global warming will not only promote microbial carbon turnover with direct feedback on greenhouse gases, but also unlock an unknown microbial diversity. Pioneering metagenomic efforts have shed light on the permafrost microbiome in polar regions, but temperate mountain permafrost is largely understudied. We applied a unique experimental design coupled to high-throughput sequencing of ribosomal markers to characterize the microbiota at the long-term alpine permafrost study site 'Muot-da-Barba-Peider' in eastern Switzerland with an approximate radiocarbon age of 12 000 years. Compared to the active layers, the permafrost community was more diverse and enriched with members of the superphylum Patescibacteria (OD1, TM7, GN02 and OP11). These understudied phyla with no cultured representatives proposedly feature small streamlined genomes with reduced metabolic capabilities, adaptations to anaerobic fermentative metabolisms and potential ectosymbiotic lifestyles. The permafrost microbiota was also enriched with yeasts and lichenized fungi known to harbour various structural and functional adaptation mechanisms to survive under extreme sub-zero conditions. These data yield an unprecedented view on microbial life in temperate mountain permafrost, which is increasingly important for understanding the biological dynamics of permafrost in order to anticipate potential ecological trajectories in a warming world.

摘要

永久冻土是一种研究甚少的基因资源。随着全球变暖,永久冻土的融化不仅会促进微生物碳周转,对温室气体产生直接反馈,还会释放出未知的微生物多样性。开创性的宏基因组学研究揭示了极地地区永久冻土微生物群落的情况,但温带山地永久冻土在很大程度上仍未得到充分研究。我们采用了独特的实验设计,并结合核糖体标记的高通量测序,来表征瑞士东部长期进行高山永久冻土研究的地点“穆特-达-巴尔巴-佩德”的微生物群,该地点的放射性碳年龄约为12000年。与活跃层相比,永久冻土群落更加多样,且富含“Patescibacteria”超群(OD1、TM7、GN02和OP11)的成员。这些研究较少的门类没有培养出代表菌株,据推测其特点是基因组小且精简,代谢能力降低,适应厌氧发酵代谢以及可能的外共生生活方式。永久冻土微生物群中还富含已知具有各种结构和功能适应机制以在极端零下条件下生存的酵母和地衣化真菌。这些数据为温带山地永久冻土中的微生物生命提供了前所未有的见解,这对于理解永久冻土的生物动态以预测变暖世界中潜在的生态轨迹越来越重要。

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