Abstract
Microbial community structures in deep-sea hydrothermal vents fields are constrained by available energy yields provided by inorganic redox reactions, which are in turn controlled by chemical composition of hydrothermal fluids. In the past two decades, geochemical and microbiological studies have been conducted in deep-sea hydrothermal vents at three geographically different areas of the Southern Mariana Trough (SMT). A variety of geochemical data of hydrothermal fluids and an unparalleled microbiological dataset of various samples (i.e., sulfide structures of active vents, iron-rich mats, borehole fluids, and ambient seawater) are available for comparative analyses. Here, we summarize the geochemical and microbiological characteristics in the SMT and assess the relationship between the microbial community structures and the fluid geochemistry in the SMT by thermodynamic modeling. In the high temperature vent fluids, aerobic sulfide-oxidation has the potential to yield large amounts of bioavailable energy in the vent fluids, which is consistent with the detection of species related to sulfide-oxidizing bacteria (such as Thiomicrospira in the Gammaproteobacteria and Sulfurimonas in the Epsilonproteobacteria). Conversely, the bioavailable energy yield from aerobic iron-oxidation reactions in the low-temperature fluids collected from man-made boreholes and several natural vents were comparable to or higher than those from sulfide-oxidation. This is also consistent with the detection of species related to iron-oxidizing bacteria (Mariprofundus in the Zetaproteobacteria) in such low-temperature samples. The results of combination of microbiological, geochemical, and thermodynamic analyses in the SMT provide novel insights into the presence and significance of iron-based microbial ecosystems in deep-sea hydrothermal fields.
Highlights
Microbial ecosystems require energy for maintenance and prosperity
Based on the microbiological data that we reported previously (Kato et al, 2009a,b, 2010), the bacterial community structures in each habitat in the Southern Mariana Trough (SMT) were compared by principal coordination analysis (PCoA) using Fast UniFrac (Hamady et al, 2009)
The hydrogen concentration of the Archaean vent fluids would be variable and fortuitously fluctuating by phase separation and subsequent sub-seafloor mixing, the geochemical modeling result is generally consistent with microbiological observations that putativethermophilic hydrogen-oxidizing chemolithoautotrophs belonging to both domains Bacteria (e.g., Hydrogenimonas) and Archaea (e.g., Archaeoglobi) were detected in the Archaean site
Summary
Microbial ecosystems require energy for maintenance and prosperity. On land and in the sea surface, solar power is the main energy source. Based on the microbiological data that we reported previously (Kato et al, 2009a,b, 2010), the bacterial community structures in each habitat (i.e., active sulfide structures, iron-rich mats, borehole fluids and ambient seawater) in the SMT were compared by principal coordination analysis (PCoA) using Fast UniFrac (Hamady et al, 2009).
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