Cabello-Yeves Pedro J, Callieri Cristiana, Picazo Antonio, Mehrshad Maliheh, Haro-Moreno Jose M, Roda-Garcia Juan J, Dzhembekova Nina, Slabakova Violeta, Slabakova Nataliya, Moncheva Snejana, Rodriguez-Valera Francisco
Evolutionary Genomics Group, Departamento de Producción Vegetal y Microbiología, Universidad Miguel, Hernández, San Juan de Alicante, Alicante, Spain.
National Research Council (CNR), Institute of Water Research (IRSA), Verbania, Italy.
Environ Microbiome. 2021 Mar 16;16(1):5. doi: 10.1186/s40793-021-00374-1.
The Black Sea is the largest brackish water body in the world, although it is connected to the Mediterranean Sea and presents an upper water layer similar to some regions of the former, albeit with lower salinity and temperature. Despite its well-known hydrology and physicochemical features, this enormous water mass remains poorly studied at the microbial genomics level.
We have sampled its different water masses and analyzed the microbiome by shotgun and genome-resolved metagenomics, generating a large number of metagenome-assembled genomes (MAGs) from them. We found various similarities with previously described Black Sea metagenomic datasets, that show remarkable stability in its microbiome. Our datasets are also comparable to other marine anoxic water columns like the Cariaco Basin. The oxic zone resembles to standard marine (e.g. Mediterranean) photic zones, with Cyanobacteria (Synechococcus but a conspicuously absent Prochlorococcus), and photoheterotrophs domination (largely again with marine relatives). The chemocline presents very different characteristics from the oxic surface with many examples of chemolithotrophic metabolism (Thioglobus) and facultatively anaerobic microbes. The euxinic anaerobic zone presents, as expected, features in common with the bottom of meromictic lakes with a massive dominance of sulfate reduction as energy-generating metabolism, a few (but detectable) methanogenesis marker genes, and a large number of "dark matter" streamlined genomes of largely unpredictable ecology.
The Black Sea oxic zone presents many similarities to the global ocean while the redoxcline and euxinic water masses have similarities to other similar aquatic environments of marine (Cariaco Basin or other Black Sea regions) or freshwater (meromictic monimolimnion strata) origin. The MAG collection represents very well the different types of metabolisms expected in this kind of environment. We are adding critical information about this unique and important ecosystem and its microbiome.
黑海是世界上最大的半咸水体,尽管它与地中海相连,且其上水层与地中海的某些区域相似,但其盐度和温度较低。尽管其水文和物理化学特征广为人知,但在微生物基因组学层面,这片巨大的水体仍未得到充分研究。
我们对黑海不同水团进行了采样,并通过鸟枪法和基因组解析宏基因组学分析了微生物群落,从中产生了大量的宏基因组组装基因组(MAG)。我们发现与先前描述的黑海宏基因组数据集有各种相似之处,这些数据集显示出其微生物群落具有显著的稳定性。我们的数据集也可与其他海洋缺氧水柱(如卡里亚科盆地)相媲美。有氧区类似于标准的海洋(如地中海)光合区,以蓝细菌(聚球藻,但明显没有原绿球藻)和光异养生物为主(同样主要是与海洋亲缘关系的生物)。化学跃层呈现出与有氧表面非常不同的特征,有许多化能无机营养代谢(硫球藻属)和兼性厌氧微生物的例子。正如预期的那样,无氧的厌氧区具有与贫营养湖底部相同的特征,以硫酸盐还原作为主要的能量产生代谢,有一些(但可检测到)甲烷生成标记基因,以及大量生态 largely unpredictable 的“暗物质”精简基因组。
黑海有氧区与全球海洋有许多相似之处,而氧化还原跃层和无氧水团与其他源于海洋(卡里亚科盆地或黑海其他区域)或淡水(贫营养单盐层)的类似水生环境有相似之处。MAG 集合很好地代表了这种环境中预期的不同代谢类型。我们正在添加有关这个独特而重要的生态系统及其微生物群落的关键信息。