Microbial diversity and methanogenic activity of Antrim Shale formation waters from recently fractured wells

dc.contributor.author Wuchter, Cornelia
dc.contributor.author Banning, Erin C.
dc.contributor.author Mincer, Tracy J.
dc.contributor.author Drenzek, Nicholas J.
dc.contributor.author Coolen, Marco J. L.
dc.date.accessioned 2014-03-31T16:52:51Z
dc.date.available 2014-03-31T16:52:51Z
dc.date.issued 2013-12-06
dc.description © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Frontiers in Microbiology 4 (2013): 367, doi:10.3389/fmicb.2013.00367. en_US
dc.description.abstract The Antrim Shale in the Michigan Basin is one of the most productive shale gas formations in the U.S., but optimal resource recovery strategies must rely on a thorough understanding of the complex biogeochemical, microbial, and physical interdependencies in this and similar systems. We used Illumina MiSeq 16S rDNA sequencing to analyze the diversity and relative abundance of prokaryotic communities present in Antrim shale formation water of three closely spaced recently fractured gas-producing wells. In addition, the well waters were incubated with a suite of fermentative and methanogenic substrates in an effort to stimulate microbial methane generation. The three wells exhibited substantial differences in their community structure that may arise from their different drilling and fracturing histories. Bacterial sequences greatly outnumbered those of archaea and shared highest similarity to previously described cultures of mesophiles and moderate halophiles within the Firmicutes, Bacteroidetes, and δ- and ε-Proteobacteria. The majority of archaeal sequences shared highest sequence similarity to uncultured euryarchaeotal environmental clones. Some sequences closely related to cultured methylotrophic and hydrogenotrophic methanogens were also present in the initial well water. Incubation with methanol and trimethylamine stimulated methylotrophic methanogens and resulted in the largest increase in methane production in the formation waters, while fermentation triggered by the addition of yeast extract and formate indirectly stimulated hydrogenotrophic methanogens. The addition of sterile powdered shale as a complex natural substrate stimulated the rate of methane production without affecting total methane yields. Depletion of methane indicative of anaerobic methane oxidation (AMO) was observed over the course of incubation with some substrates. This process could constitute a substantial loss of methane in the shale formation. en_US
dc.description.sponsorship Tracy J. Mincer was supported for this project from NSF CHE-OCE Award # 1131415. en_US
dc.format.mimetype application/pdf
dc.identifier.citation Frontiers in Microbiology 4 (2013): 367 en_US
dc.identifier.doi 10.3389/fmicb.2013.00367
dc.identifier.uri https://hdl.handle.net/1912/6519
dc.language.iso en_US en_US
dc.publisher Frontiers Media en_US
dc.relation.uri https://doi.org/10.3389/fmicb.2013.00367
dc.rights Attribution 3.0 *
dc.rights.uri http://creativecommons.org/licenses/by/3.0/ *
dc.subject Antrim gas shale en_US
dc.subject Biogenic gas en_US
dc.subject Formation water en_US
dc.subject Fermenting bacteria en_US
dc.subject Methanogens en_US
dc.title Microbial diversity and methanogenic activity of Antrim Shale formation waters from recently fractured wells en_US
dc.type Article en_US
dspace.entity.type Publication
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