Meier Dimitri V, Pjevac Petra, Bach Wolfgang, Hourdez Stephane, Girguis Peter R, Vidoudez Charles, Amann Rudolf, Meyerdierks Anke
Max Planck Institute for Marine Microbiology, Bremen, Germany.
Department of Geosciences and MARUM-Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany.
ISME J. 2017 Jul;11(7):1545-1558. doi: 10.1038/ismej.2017.37. Epub 2017 Apr 4.
At deep-sea hydrothermal vents, primary production is carried out by chemolithoautotrophic microorganisms, with the oxidation of reduced sulfur compounds being a major driver for microbial carbon fixation. Dense and highly diverse assemblies of sulfur-oxidizing bacteria (SOB) are observed, yet the principles of niche differentiation between the different SOB across geochemical gradients remain poorly understood. In this study niche differentiation of the key SOB was addressed by extensive sampling of active sulfidic vents at six different hydrothermal venting sites in the Manus Basin, off Papua New Guinea. We subjected 33 diffuse fluid and water column samples and 23 samples from surfaces of chimneys, rocks and fauna to a combined analysis of 16S rRNA gene sequences, metagenomes and real-time in situ measured geochemical parameters. We found Sulfurovum Epsilonproteobacteria mainly attached to surfaces exposed to diffuse venting, while the SUP05-clade dominated the bacterioplankton in highly diluted mixtures of vent fluids and seawater. We propose that the high diversity within Sulfurimonas- and Sulfurovum-related Epsilonproteobacteria observed in this study derives from the high variation of environmental parameters such as oxygen and sulfide concentrations across small spatial and temporal scales.
在深海热液喷口,初级生产由化能自养微生物进行,还原硫化合物的氧化是微生物碳固定的主要驱动力。观察到硫氧化细菌(SOB)密集且高度多样化的群落,但不同SOB在地球化学梯度上的生态位分化原理仍知之甚少。在本研究中,通过对巴布亚新几内亚近海马努斯盆地六个不同热液喷口处的活跃硫化物喷口进行广泛采样,研究了关键SOB的生态位分化。我们对33个扩散流体和水柱样本以及23个来自烟囱、岩石和动物表面的样本进行了16S rRNA基因序列、宏基因组和现场实时测量的地球化学参数的综合分析。我们发现硫还原弧菌属ε-变形菌主要附着在暴露于扩散喷口的表面,而SUP05进化枝在喷口流体和海水的高度稀释混合物中的浮游细菌中占主导地位。我们认为,本研究中观察到的与硫单胞菌属和硫还原弧菌属相关的ε-变形菌内的高度多样性源于氧和硫化物浓度等环境参数在小空间和时间尺度上的高度变化。