CSIC, Institute of Catalysis, 28049 Madrid, Spain.
Environ Microbiol. 2012 Jan;14(1):268-81. doi: 10.1111/j.1462-2920.2011.02634.x. Epub 2011 Oct 31.
So far only little is known about the microbial ecology of Mediterranean deep-sea hypersaline anoxic lakes (DHALs). These brine lakes were formed by evaporite dissolution/brine seeps and are important model environments to provide insights into possible metabolisms and distributions of microorganisms on the early Earth. Our study on the Lake Thetis, a new thalassohaline DHAL located South-East of the Medriff Corridor, has revealed microbial communities of contrasting compositions with a high number of novel prokaryotic candidate divisions. The major finding of our present work is co-occurrence of at least three autotrophic carbon dioxide fixation pathways in the brine-seawater interface that are likely fuelled by an active ramified sulphur cycle. Genes for the reductive acetyl-CoA and reductive TCA pathways were also found in the brine suggesting that these pathways are operational even at extremely elevated salinities and that autotrophy is more important in hypersaline environments than previously assumed. Surprisingly, genes coding for RuBisCo were found in the highly reduced brine. Three types of sulphide oxidation pathways were found in the interface. The first involves a multienzyme Sox complex catalysing the complete oxidation of reduced sulphur compounds to sulphate, the second type recruits SQR sulphide:quinone reductase for oxidation of sulphide to elemental sulphur, which, in the presence of sulphide, could further be reduced by polysulphide reductases in the third pathway. The presence of the latter two allows a maximal energy yield from the oxidation of sulphide and at the same time prevents the acidification and the accumulation of S(0) deposits. Amino acid composition analysis of deduced proteins revealed a significant overrepresentation of acidic residues in the brine compared with the interface. This trait is typical for halophilic organisms as an adaptation to the brine's extreme hypersalinity. This work presents the first metagenomic survey of the microbial communities of the recently discovered Lake Thetis whose brine constitutes one of saltiest water bodies ever reported.
迄今为止,人们对地中海深海高盐缺氧湖(DHAL)的微生物生态了解甚少。这些卤水湖是由蒸发盐溶解/卤水渗出形成的,是研究早期地球上微生物可能代谢和分布的重要模型环境。我们对位于梅德里夫海峡东南部的新的半咸水 DHAL——泰蒂斯湖的研究揭示了微生物群落的组成截然不同,其中存在大量新型的原核候选分类群。我们目前工作的主要发现是在卤水-海水界面处至少存在三种共生固碳途径,这些途径可能由活跃的分支硫循环提供动力。在卤水中还发现了还原性乙酰辅酶 A 和还原性三羧酸循环途径的基因,这表明即使在极高的盐度下,这些途径也是可行的,并且在高盐环境中自养作用比之前认为的更为重要。令人惊讶的是,在高度还原的卤水中发现了编码 RuBisCo 的基因。在界面处发现了三种硫化物氧化途径。第一种途径涉及多酶 Sox 复合物,可将还原态硫化合物完全氧化为硫酸盐;第二种途径利用 SQR 硫化物:醌还原酶将硫化物氧化为元素硫,在硫化物存在的情况下,元素硫可进一步被第三种途径中的多硫化物还原酶还原。后两种途径的存在允许从硫化物的氧化中获得最大的能量产量,同时防止酸化和 S(0) 沉积物的积累。推导蛋白的氨基酸组成分析显示,与界面相比,卤水中的酸性残基明显过量。这种特征是嗜盐生物的典型特征,是对卤水极端高盐度的适应。这项工作首次对最近发现的泰蒂斯湖的微生物群落进行了宏基因组调查,其卤水是有记录以来最咸的水体之一。