Pontefract Alexandra, Zhu Ting F, Walker Virginia K, Hepburn Holli, Lui Clarissa, Zuber Maria T, Ruvkun Gary, Carr Christopher E
Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, United States.
Department of Molecular Biology, Massachusetts General Hospital, Boston, MA, United States.
Front Microbiol. 2017 Sep 26;8:1819. doi: 10.3389/fmicb.2017.01819. eCollection 2017.
Life can persist under severe osmotic stress and low water activity in hypersaline environments. On Mars, evidence for the past presence of saline bodies of water is prevalent and resulted in the widespread deposition of sulfate and chloride salts. Here we investigate Spotted Lake (British Columbia, Canada), a hypersaline lake with extreme (>3 M) levels of sulfate salts as an exemplar of the conditions thought to be associated with ancient Mars. We provide the first characterization of microbial structure in Spotted Lake sediments through metagenomic sequencing, and report a bacteria-dominated community with abundant Proteobacteria, Firmicutes, and Bacteroidetes, as well as diverse extremophiles. Microbial abundance and functional comparisons reveal similarities to Ace Lake, a meromictic Antarctic lake with anoxic and sulfidic bottom waters. Our analysis suggests that hypersaline-associated species occupy niches characterized foremost by differential abundance of Archaea, uncharacterized Bacteria, and Cyanobacteria. Potential biosignatures in this environment are discussed, specifically the likelihood of a strong sulfur isotopic fractionation record within the sediments due to the presence of sulfate reducing bacteria. With its high sulfate levels and seasonal freeze-thaw cycles, Spotted Lake is an analog for ancient paleolakes on Mars in which sulfate salt deposits may have offered periodically habitable environments, and could have concentrated and preserved organic materials or their biomarkers over geologic time.
在高盐环境中,生命能够在严重的渗透胁迫和低水分活度条件下存续。在火星上,过去存在盐水水体的证据很普遍,这导致了硫酸盐和氯化物盐的广泛沉积。在此,我们以加拿大不列颠哥伦比亚省的斑点湖为例进行研究,该湖是一个硫酸盐盐含量极高(超过3M)的高盐湖,被认为是与古代火星相关条件的典型代表。我们通过宏基因组测序首次对斑点湖沉积物中的微生物结构进行了表征,并报告了一个以细菌为主的群落,其中富含变形菌门、厚壁菌门和拟杆菌门,以及多种极端微生物。微生物丰度和功能比较显示,其与艾斯湖有相似之处,艾斯湖是南极一个有缺氧和含硫底水的半咸湖。我们的分析表明,与高盐相关的物种占据的生态位主要特征是古菌、未分类细菌和蓝细菌的丰度差异。本文讨论了这种环境中潜在的生物特征,特别是由于硫酸盐还原菌的存在,沉积物中可能存在强烈的硫同位素分馏记录。由于硫酸盐含量高且有季节性冻融循环,斑点湖可作为火星上古代古湖的模拟物,在这些古湖中,硫酸盐盐沉积物可能提供了周期性的宜居环境,并可能在地质时期浓缩和保存了有机物质或其生物标志物。