Publications by Colleges and Departments (MSU - Bozeman)

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    Hydrogeochemistry and coal-associated bacterial populations from a methanogenic coal bed
    (2016-05) Barnhart, Elliott P.; Weeks, Edwin P.; Jones, Elizabeth J. P.; Ritter, Daniel J.; McIntosh, Jennifer C.; Clark, Arthur C.; Ruppert, Leslie F.; Cunningham, Alfred B.; Vinson, David S.; Orem, William; Fields, Matthew W.
    Biogenic coalbed methane (CBM), a microbially-generated source of natural gas trapped within coal beds, is an important energy resource in many countries. Specific bacterial populations and enzymes involved in coal degradation, the potential rate-limiting step of CBM formation, are relatively unknown. The U.S. Geological Survey (USGS) has established a field site, (Birney test site), in an undeveloped area of the Powder River Basin (PRB), with four wells completed in the Flowers-Goodale coal bed, one in the overlying sandstone formation, and four in overlying and underlying coal beds (Knoblach, Nance, and Terret). The nine wells were positioned to characterize the hydraulic conductivity of the Flowers-Goodale coal bed and were selectively cored to investigate the hydrogeochemistry and microbiology associated with CBM production at the Birney test site. Aquifer-test results indicated the Flowers-Goodale coal bed, in a zone from about 112 to 120 m below land surface at the test site, had very low hydraulic conductivity (0.005 m/d) compared to other PRB coal beds examined. Consistent with microbial methanogenesis, groundwater in the coal bed and overlying sandstone contain dissolved methane (46 mg/L average) with low δ13C values (− 67‰ average), high alkalinity values (22 meq/kg average), relatively positive δ13C-DIC values (4‰ average), and no detectable higher chain hydrocarbons, NO3−, or SO42 −. Bioassay methane production was greatest at the upper interface of the Flowers-Goodale coal bed near the overlying sandstone. Pyrotag analysis identified Aeribacillus as a dominant in situ bacterial community member in the coal near the sandstone and statistical analysis indicated Actinobacteria predominated coal core samples compared to claystone or sandstone cores. These bacteria, which previously have been correlated with hydrocarbon-containing environments such as oil reservoirs, have demonstrated the ability to produce biosurfactants to break down hydrocarbons. Identifying microorganisms involved in coal degradation and the hydrogeochemical conditions that promote their activity is crucial to understanding and improving in situ CBM production.
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    Cultivation of a native alga for biomass and biofuel accumulation in coal bed methane production water
    (2016-11) Hodgkiss, Logan H.; Nagy, J.; Barnhart, Elliott P.; Cunningham, Alfred B.; Fields, Matthew W.
    Coal bed methane (CBM) production has resulted in thousands of ponds in the Powder River Basin of low-quality water in a water-challenged region. A green alga isolate, PW95, was isolated from a CBM production pond, and analysis of a partial ribosomal gene sequence indicated the isolate belongs to the Chlorococcaceae family. Different combinations of macro- and micronutrients were evaluated for PW95 growth in CBM water compared to a defined medium. A small level of growth was observed in unamended CBM water (0.15 g/l), and biomass increased (2-fold) in amended CBM water or defined growth medium. The highest growth rate was observed in CBM water amended with both N and P, and the unamended CBM water displayed the lowest growth rate. The highest lipid content (27%) was observed in CBM water with nitrate, and a significant level of lipid accumulation was not observed in the defined growth medium. Growth analysis indicated that nitrate deprivation coincided with lipid accumulation in CBM production water, and lipid accumulation did not increase with additional phosphorus limitation. The presented results show that CBM production wastewater can be minimally amended and used for the cultivation of a native, lipid-accumulating alga.
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    Investigation of coal-associated bacterial and archaeal populations from a diffusive microbial sampler (DMS)
    (2013-08) Barnhart, Elliott P.; Bowen De León, Kara; Ramsay, Bradley D.; Cunningham, Alfred B.; Fields, Matthew W.
    The Powder River Basin (PRB) in southeastern Montana and northeastern Wyoming contains massive coal deposits with biologically generated coal bed methane (CBM). The microbial ecology of an area within a coal bed influenced by recent groundwater recharge was sampled with a diffusive microbial sampler (DMS). The DMS contained native coal material and was incubated in situ (57 m depth) to allow colonization of the coal particles. Pyrotag sequence analyses of SSU rRNA gene sequences from the coal contained within the post-incubation DMS detected methylotrophic and hydrogenotrophic methanogenic archaea along with diverse bacterial communities. Microbial enrichments (coal or acetate/H2) were established from the DMS, and the enriched bacterial and archaeal communities were characterized via clone library analysis. The in situ bacterial communities were more diverse than the archaeal communities, and the archaeal populations differed between coal incubated in situ and in laboratory enrichments. In addition, bacterial diversity was higher for laboratory enrichments with coal compared to enrichments without coal. The elucidation of relationships between microorganisms involved in coal degradation and metabolite (acetate, H2) utilization within coal-dependent microbial communities is crucial to understanding and improving in situ coal bed methane production.
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    Potential Role of Acetyl-CoA Synthetase (acs) & Malate Dehydrogenase (mae) in the Evolution of the Acetate Switch in Bacteria and Archaea
    (2015-08) Barnhart, Elliott P.; McClure, Marcella A.; Johnson, Kiki; Cleveland, Sean; Hunt, Kristopher A.; Fields, Matthew W.
    Although many Archaea have AMP-Acs (acetyl-coenzyme A synthetase) and ADP-Acs, the extant methanogenic genus Methanosarcina is the only identified Archaeal genus that can utilize acetate via acetate kinase (Ack) and phosphotransacetylase (Pta). Despite the importance of ack as the potential urkinase in the ASKHA phosphotransferase superfamily, an origin hypothesis does not exist for the acetate kinase in Bacteria, Archaea, or Eukarya. Here we demonstrate that Archaeal AMP-Acs and ADP-Acs contain paralogous ATPase motifs previously identified in Ack, which demonstrate a novel relation between these proteins in Archaea. The identification of ATPase motif conservation and resulting structural features in AMP- and ADP-acetyl-CoA synthetase proteins in this study expand the ASKHA superfamily to include acetyl-CoA synthetase. Additional phylogenetic analysis showed that Pta and MaeB sequences had a common ancestor, and that the Pta lineage within the halophilc archaea was an ancestral lineage. These results suggested that divergence of a duplicated maeB within an ancient halophilic, archaeal lineage formed a putative pta ancestor. These results provide a potential scenario for the establishment of the Ack/Pta pathway and provide novel insight into the evolution of acetate metabolism for all three domains of life.
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