Abstract
Sediment-hosting hydrothermal systems in the Okinawa Trough maintain a large amount of liquid, supercritical and hydrate phases of CO2 in the seabed. The emission of CO2 may critically impact the geochemical, geophysical and ecological characteristics of the deep-sea sedimentary environment. So far it remains unclear whether microbial communities that have been detected in such high-CO2 and low-pH habitats are metabolically active, and if so, what the biogeochemical and ecological consequences for the environment are. In this study, RNA-based molecular approaches and radioactive tracer-based respiration rate assays were combined to study the density, diversity and metabolic activity of microbial communities in CO2-seep sediment at the Yonaguni Knoll IV hydrothermal field of the southern Okinawa Trough. In general, the number of microbes decreased sharply with increasing sediment depth and CO2 concentration. Phylogenetic analyses of community structure using reverse-transcribed 16S ribosomal RNA showed that the active microbial community became less diverse with increasing sediment depth and CO2 concentration, indicating that microbial activity and community structure are sensitive to CO2 venting. Analyses of RNA-based pyrosequences and catalyzed reporter deposition-fluorescence in situ hybridization data revealed that members of the SEEP-SRB2 group within the Deltaproteobacteria and anaerobic methanotrophic archaea (ANME-2a and -2c) were confined to the top seafloor, and active archaea were not detected in deeper sediments (13–30 cm in depth) characterized by high CO2. Measurement of the potential sulfate reduction rate at pH conditions of 3–9 with and without methane in the headspace indicated that acidophilic sulfate reduction possibly occurs in the presence of methane, even at very low pH of 3. These results suggest that some members of the anaerobic methanotrophs and sulfate reducers can adapt to the CO2-seep sedimentary environment; however, CO2 and pH in the deep-sea sediment were found to severely impact the activity and structure of the microbial community.
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Acknowledgements
We thank the shipboard science party of the SO196 cruise and the crew and operation teams of the RV Sonne and ROV Quest 4000 for their support in sample collection. We also thank Noriaki Masui for technical assistance. We are grateful to Katrin Knittel and Sara Kleindienst for helpful discussion regarding CARD-FISH using the SEEP2-658 probe. This work was supported in part by a Grant-in-Aid from the Japan Society for the Promotion of Science (JSPS) Fellows (20-10764, to KY), a Grant-in-Aid for Scientific Research: Project TAIGA (New Scientific Research on Innovative Areas, 20109003, to MS and TU), the JSPS Funding Program for the Next Generation of World-Leading Researchers (NEXT Program, to FI), the JSPS Strategic Fund for Strengthening Leading-edge Research and Development (to JAMSTEC), the Max Planck Society (MPG project funds) and project SUMSUN (grant no. 03G0196B), funded by the German Federal Ministry of Education and Research.
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Yanagawa, K., Morono, Y., de Beer, D. et al. Metabolically active microbial communities in marine sediment under high-CO2 and low-pH extremes. ISME J 7, 555–567 (2013). https://doi.org/10.1038/ismej.2012.124
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DOI: https://doi.org/10.1038/ismej.2012.124
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