Edgcomb Virginia P, Pachiadaki Maria G, Mara Paraskevi, Kormas Konstantinos A, Leadbetter Edward R, Bernhard Joan M
Department of Geology & Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA, USA.
Department of Chemistry, University of Crete, Heraklion, Greece.
ISME J. 2016 Nov;10(11):2643-2657. doi: 10.1038/ismej.2016.58. Epub 2016 Apr 19.
Deep-sea hypersaline anoxic basins (DHABs) in the Eastern Mediterranean Sea are considered some of the most polyextreme habitats on Earth. In comparison to microbial activities occurring within the haloclines and brines of these unusual water column habitats near the Mediterranean seafloor, relatively little is known about microbial metabolic activities in the underlying sediments. In addition, it is not known whether activities are shaped by the unique chemistries of the different DHAB brines and whether evidence exists for active microbial eukaryotes in those sediments. Metatranscriptome analysis was applied to sediment samples collected using ROV Jason from underneath the haloclines of Urania, Discovery and L'Atalante DHABs and a control site. We report on expression of genes associated with sulfur and nitrogen cycling, putative osmolyte biosynthetic pathways and ion transporters, trace metal detoxification, selected eukaryotic activities (particularly of fungi), microbe-microbe interactions, and motility in sediments underlying the haloclines of three DHABs. Relative to our control sediment sample collected outside of Urania Basin, microbial communities (including eukaryotes) in the Urania and Discovery DHAB sediments showed upregulation of expressed genes associated with nitrogen transformations, osmolyte biosynthesis, heavy metals resistance and metabolism, eukaryotic organelle functions, and cell-cell interactions. Sediments underlying DHAB haloclines that have cumulative physico-chemical stressors within the limits of tolerance for microoorganisms can therefore be hotspots of activity in the deep Mediterranean Sea.
地中海东部的深海高盐缺氧盆地(DHABs)被认为是地球上一些最为极端的栖息地。与地中海海底附近这些不同寻常的水柱栖息地的盐跃层和卤水中发生的微生物活动相比,人们对其下伏沉积物中的微生物代谢活动了解相对较少。此外,尚不清楚这些活动是否受不同DHAB卤水独特化学性质的影响,以及在这些沉积物中是否存在活跃的微生物真核生物的证据。对使用遥控潜水器“杰森”从乌拉尼亚、发现号和阿塔兰特DHABs的盐跃层下方以及一个对照站点采集的沉积物样本进行了宏转录组分析。我们报告了与硫和氮循环、假定的渗透溶质生物合成途径和离子转运蛋白、微量金属解毒、选定的真核生物活动(特别是真菌)、微生物间相互作用以及三个DHABs盐跃层下伏沉积物中的运动性相关的基因表达情况。相对于我们在乌拉尼亚盆地外采集的对照沉积物样本,乌拉尼亚和发现号DHAB沉积物中的微生物群落(包括真核生物)显示出与氮转化、渗透溶质生物合成、重金属抗性和代谢、真核细胞器功能以及细胞间相互作用相关的表达基因上调。因此,在微生物耐受限度内具有累积物理化学应激源的DHAB盐跃层下伏沉积物可能是地中海深部的活动热点。