Gomez-Saez Gonzalo V, Pop Ristova Petra, Sievert Stefan M, Elvert Marcus, Hinrichs Kai-Uwe, Bühring Solveig I
Hydrothermal Geomicrobiology Group, MARUM - Center for Marine Environmental Sciences, University of BremenBremen, Germany.
Biology Department, Woods Hole Oceanographic Institution, Woods HoleMA, USA.
Front Microbiol. 2017 Apr 21;8:702. doi: 10.3389/fmicb.2017.00702. eCollection 2017.
The unique geochemistry of marine shallow-water hydrothermal systems promotes the establishment of diverse microbial communities with a range of metabolic pathways. In contrast to deep-sea vents, shallow-water vents not only support chemosynthesis, but also phototrophic primary production due to the availability of light. However, comprehensive studies targeting the predominant biogeochemical processes are rare, and consequently a holistic understanding of the functioning of these ecosystems is currently lacking. To this end, we combined stable isotope probing of lipid biomarkers with an analysis of the bacterial communities to investigate if chemoautotrophy, in parallel to photoautotrophy, plays an important role in autotrophic carbon fixation and to identify the key players. The study was carried out at a marine shallow-water hydrothermal system located at 5 m water depth off Dominica Island (Lesser Antilles), characterized by up to 55°C warm hydrothermal fluids that contain high amounts of dissolved Fe. Analysis of the bacterial diversity revealed of the as the most abundant bacterial class. Furthermore, the presence of key players involved in iron cycling generally known from deep-sea hydrothermal vents (e.g., and ), supported the importance of iron-driven redox processes in this hydrothermal system. Uptake of C-bicarbonate into bacterial fatty acids under light and dark conditions revealed active photo- and chemoautotrophic communities, with chemoautotrophy accounting for up to 65% of the observed autotrophic carbon fixation. Relatively increased C-incorporation in the dark allowed the classification of C, C, and C as potential lipid biomarkers for bacterial chemoautotrophy in this ecosystem. Highest total C-incorporation into fatty acids took place at the sediment surface, but chemosynthesis was found to be active down to 8 cm sediment depth. In conclusion, this study highlights the relative importance of chemoautotrophy compared to photoautotrophy in a shallow-water hydrothermal system, emphasizing chemosynthesis as a prominent process for biomass production in marine coastal environments influenced by hydrothermalism.
海洋浅水热液系统独特的地球化学性质促进了具有一系列代谢途径的多样微生物群落的建立。与深海热液喷口不同,浅水热液喷口不仅支持化学合成,还因有光照而支持光合初级生产。然而,针对主要生物地球化学过程的全面研究很少,因此目前缺乏对这些生态系统功能的整体理解。为此,我们将脂质生物标志物的稳定同位素探测与细菌群落分析相结合,以研究化学自养作用是否与光合自养作用并行,在自养碳固定中发挥重要作用,并确定关键参与者。该研究在多米尼克岛(小安的列斯群岛)水深5米处的一个海洋浅水热液系统中进行,该系统的特征是高达55°C的温暖热液流体,其中含有大量溶解铁。细菌多样性分析显示,[具体细菌类别]是最丰富的细菌类群。此外,深海热液喷口通常已知的参与铁循环的关键参与者(如[具体细菌名称]和[具体细菌名称])的存在,支持了铁驱动的氧化还原过程在该热液系统中的重要性。在光照和黑暗条件下,细菌脂肪酸对碳酸氢盐的摄取揭示了活跃的光合和化学自养群落,化学自养作用占观察到的自养碳固定的比例高达65%。黑暗中相对增加的碳掺入使得[具体碳同位素]、[具体碳同位素]和[具体碳同位素]可被归类为该生态系统中细菌化学自养作用的潜在脂质生物标志物。脂肪酸中总碳掺入量最高发生在沉积物表面,但发现化学合成在沉积物深度达8厘米处仍有活性。总之,这项研究突出了在浅水热液系统中化学自养作用相对于光合自养作用的相对重要性,强调了化学合成是受热液作用影响的海洋沿海环境中生物量生产的一个突出过程。