Hydrothermal vent ecology

What are deep-sea hydrothermal vent systems?

Deep-sea hydrothermal vents are unique habitats for life. They occur, e.g., along mid-ocean ridges, in bac-arc basins, and at submerged island arc volcanoes in areas where a heat source such as a magma chamber is located close to the seafloor. At these sites, cold oxygenated seawater entrained in the rock gets heated and chemicaly modified before it is again emitted into the water column as high temperature (generally >200°C) fluid at focused and low temperature (generally <100°C) fluid at diffuse vents. These fluids are, depending on the geological settings, enrichted in reduced compounds such as hydrogen sulphide, hydrogen, methane and iron. They are used by chemoautotrophic microorganisms, building up biomass which can further be used as energy source by heterotrophic organisms altogether leading to unique, highly productive oases amidst the predominantly food-limited deep-sea.

Niche-partitioning of co-occurring sulphur-oxidising bacteria in the Manus back-arc basin

Primary production  at deep sea hydrothermal vents, is carried out by chemolithoautotrophic microorganisms, with the oxidation of reduced sulfur compounds being a major driver for microbial carbon fixation. As a systematic study investigating niche-partitioning of co-occurring SOB at hydrothermal vents was still missing, and as a follow up of Pjevac et al. (2014), we systematically investigated niche differentiation of key sulfur-oxidising bacteria in the Manus back-arc basin (Meier et al., 2017). Thirtythree diffuse fluid and water column samples and 23 samples from surfaces of chimneys, rocks and fauna were subjected to a combined analyses of 16S RNA gene sequences, metagenomes and real-time in situ measured geochemical parameters. We found Sulfurovum-related Epsilonbacteraeota mainly attached to surfaces exposed to diffuse venting, while the SUP05-clade Gammaproteobacteria dominated the bacterioplankton in highly diluted mixtures of vent fluids and seawater. The high diversity observed for Sulfurimonas- and Sulfurovum-related Epsilonbacteraeota was proposed to be caused by the high variation of environmental parameters such as oxygen and sulfide concentrations across small spatial and temporal scales.

Heterotrophic bacteria at deep-sea hydrothermal vents

Heterotrophic bacteria likely play an important role in re-mineralisation of carbon fixed by chemolithoautotrophs closing the carbon cycle in vent ecosystems. In two of our studies we targeted these yet under investigated heterotrophic part of free-living microbial communities at vents. We could find various Gammaproteobacteria assimilating acetate in diffuse fluids from the Manus Basin bac-arc basin, and identified a novel clade of Nautiliales-related Epsilonbacteraeota in diffuse fluids at the Menez Gwen hydrothermal field on the Mid Atlantic Ridge (Winkel et al., 2014). At Menez Gwen we also studied mixing gradients of hydrothermal fluids with seawater from the diffuse fluid discharge points on, up to the buoyant parts of hydrothermal plumes, applying a combination of high throughput 16S rRNA gene tag sequencing, fluorescence in situ hybridisation, and targeted metagenome analysis, combined with geochemical analyses and thermodynamic considerations (Meier et al. 2016). Close to the discharge areas of diffuse fluids, which were dominated by chemolithoautotrophic Epsilonbacteraeota, in areas where environmental conditions still supported chemolithoautotrophic processes, we detected microbial communities enriched for versatile heterotrophic Alpha- and Gammaproteobacteria. Analysing genomic bins, the potential for alkane degradation could be shown for several genera and yet uncultured clades. The results suggests that diffuse fluids already contain to a low extend microorganisms that can quickly respond to the availability of carbon compounds, and that these hotspots of chemolithoautotrophic life at hydrothermal discharge points support a “belt” of heterotrophic bacteria significantly different from the dominating oligotrophic microbiota of the deep sea.

Microbial life on hydrothermal chimneys

Hydrothermal (sulphide) chimneys are the most impressive signboard of deep-sea hydrothermal vents. They form, when hot, acidic, metal- and sulphide-rich fluids, poor in magnesium and sulphate, are emitted into cold oxygenated seawater. Thereby mineral composition and structure of the chimneys strongly depends on the geological setting influencing physico-chemical characteristics of the fluids. Correlating with the steep physico-chemical gradients in such chimney structures, they are inhabited by diverse microbial taxa.

Life on active chimneys

Within the scope of our studies, we found surface scrapes of hydrothermal chimneys recovered from the Manus Basin back-arc spreading system to contain various chemolithoautotrophic Epsilonbacteraeota, while the abundance and distribution of other putative primary producers (e.g., Gammaproteobacteria, Zetaproteobacteria, and Aquificae) was variable between structures of different venting regimes (Reeves et al., 2014; Meier et al., 2017). Using proteogenomics (Pjevac et al. 2018), we identified overlaps in the in situ functional profiles, despite differences in microbial community composition and venting regime. The highly diverse microbial community colonizing a black smoker chimney had a highly redundant metabolic potential. In contrast, the considerably less diverse community colonizing a diffusely venting chimney displayed a higher metabolic versatility. An increased diversity on the phylogenetic level was thus not directly linked to an increased metabolic diversity in microbial communities that colonize hydrothermal chimneys. We could also show that a diversified copy of a key gene of the sox sulfur oxidation pathway, SoxY (SoxY-II), was truly expressed, suggesting a significant role in sulfur cycling at hydrothermal vents.

Life on dead chimneys

Compared to active chimneys, even less is known about the composition and metabolic activity of microbial communities inhabiting inactive massive sulfide chimneys. In another proteogenomic study, we identified two major types of microbial communities, distinctly different from those described for active chimneys, on inactive chimneys of comparable mineralogical origin: One type was characterized by a dominance of Nitrospirae-related putative anaerobic, autotrophic sulfate reducers and the other one by aerobic sulfide-oxidizing autotrophic Gammaproteobacteria (Meier et al. 2019). We provided new insights into the lifestyle of as yet poorly characterized clades, such as Nitrospirae and Gammaproteobacteria of the Woeseiacea-family and the Siboglinidae symbionts-related (SSr)-clade. Our results support the role of the Woeseiaceae-family and the SSr-clade as important catalysts of sulfide mineral weathering and primary producers in benthic marine habitats.