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寒冷地下含水层群落的基因组解析为适应高二氧化碳浓度的新型微生物提供了代谢见解。

Genomic resolution of a cold subsurface aquifer community provides metabolic insights for novel microbes adapted to high CO concentrations.

作者信息

Probst Alexander J, Castelle Cindy J, Singh Andrea, Brown Christopher T, Anantharaman Karthik, Sharon Itai, Hug Laura A, Burstein David, Emerson Joanne B, Thomas Brian C, Banfield Jillian F

机构信息

Department of Earth and Planetary Sciences, University of California, Berkeley, 307 McCone Hall, CA, 94720, USA.

Department of Plant and Microbial Biology, University of California, Berkeley, CA, 94720, USA.

出版信息

Environ Microbiol. 2017 Feb;19(2):459-474. doi: 10.1111/1462-2920.13362. Epub 2016 Jul 7.

DOI:10.1111/1462-2920.13362
PMID:27112493
Abstract

As in many deep underground environments, the microbial communities in subsurface high-CO ecosystems remain relatively unexplored. Recent investigations based on single-gene assays revealed a remarkable variety of organisms from little studied phyla in Crystal Geyser (Utah, USA), a site where deeply sourced CO -saturated fluids are erupted at the surface. To provide genomic resolution of the metabolisms of these organisms, we used a novel metagenomic approach to recover 227 high-quality genomes from 150 microbial species affiliated with 46 different phylum-level lineages. Bacteria from two novel phylum-level lineages have the capacity for CO fixation. Analyses of carbon fixation pathways in all studied organisms revealed that the Wood-Ljungdahl pathway and the Calvin-Benson-Bassham Cycle occurred with the highest frequency, whereas the reverse TCA cycle was little used. We infer that this, and selection for form II RuBisCOs, are adaptions to high CO -concentrations. However, many autotrophs can also grow mixotrophically, a strategy that confers metabolic versatility. The assignment of 156 hydrogenases to 90 different organisms suggests that H is an important inter-species energy currency even under gaseous CO -saturation. Overall, metabolic analyses at the organism level provided insight into the biochemical cycles that support subsurface life under the extreme condition of CO saturation.

摘要

与许多深层地下环境一样,地下高二氧化碳生态系统中的微生物群落仍相对未被探索。最近基于单基因分析的调查揭示了美国犹他州水晶间歇泉中来自研究较少的门的大量生物,在该地点,深层来源的二氧化碳饱和流体在地表喷发。为了提供这些生物代谢的基因组分辨率,我们使用了一种新颖的宏基因组方法,从隶属于46个不同门级谱系的150个微生物物种中恢复了227个高质量基因组。来自两个新的门级谱系的细菌具有固定二氧化碳的能力。对所有研究生物的碳固定途径分析表明,伍德-Ljungdahl途径和卡尔文-本森-巴斯姆循环出现的频率最高,而反向TCA循环很少被使用。我们推断,这以及对II型核酮糖-1,5-二磷酸羧化酶的选择是对高二氧化碳浓度的适应。然而,许多自养生物也可以混合营养生长,这是一种赋予代谢多功能性的策略。将156种氢化酶分配给90种不同生物表明,即使在气态二氧化碳饱和的情况下,氢也是一种重要的种间能量货币。总体而言,在生物体水平上的代谢分析为在二氧化碳饱和的极端条件下支持地下生命的生化循环提供了见解。

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