Diversity and metabolic potential of microbial communities in a site of continental serpentinization
The geochemical process of serpentinization releases energy and organic carbon: two of the basic requirements need ed to support life. Sites of active serpentinization in the deep subsurface provide the intriguing possibility of a non-photosynthetically -supported biosphere. However, serpentinizatio...
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| Format: | Text |
| Language: | English |
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University of Utah
2016
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| Online Access: | https://dx.doi.org/10.26053/0h-9e35-6mg0 https://collections.lib.utah.edu/ark:/87278/s6zw4w64 |
| Summary: | The geochemical process of serpentinization releases energy and organic carbon: two of the basic requirements need ed to support life. Sites of active serpentinization in the deep subsurface provide the intriguing possibility of a non-photosynthetically -supported biosphere. However, serpentinization also creates conditions, such as high pH and limited electron acceptor s, which may limit microbial growth and diversity. Gaining an understanding of the identity and metabolic potential of microbes that thrive in these environments may provide insight as to whether serpentinization is sufficient to independently support life. Tablelands Ophiolite in Gros Morne National Park, Newfoundland, Canada is a continental site of serpentinization where serpentinite springs form surface pools. These pools provide easy sampling access to subsurface fluids and may allow for sampling of the subsurface microbial community. However, identification of members of the subsurface community in these pools is complicated by both surface contamination and contamination by organisms that inhabit the transition zone where hydrogen-rich subsurface fluids meet oxygen -rich surface fluids. This study was designed to distinguish among these potential sources of microorganisms by using a sampling technique that more effectively samples subsurface fluids. Community dissimilarity comparisons using environmental 16S rRNA gene sequencing indicate that the sampling design led to more direct access to subsurface fluids. These results are supported by metagenomic analyses that show metabolic pathways consistent with non- photosynthetic carbon fixation in the samples expected to represent subsurface fluids and that show hydrogen oxidation pathways in samples associated with the surface sources. These results provide a clearer picture of the diversity and metabolic potential of microbial communities potentially inhabiting subsurface, serpentinite-hosted habitats. |
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