skip to main content

DOE PAGESDOE PAGES

Title: Impact of Organic Carbon Electron Donors on Microbial Community Development under Iron- and Sulfate-Reducing Conditions

Although iron- and sulfate-reducing bacteria in subsurface environments have crucial roles in biogeochemical cycling of C, Fe, and S, how specific electron donors impact the compositional structure and activity of native iron- and/or sulfate-reducing communities is largely unknown. To understand this better, we created bicarbonate-buffered batch systems in duplicate with three different electron donors (acetate, lactate, or glucose) paired with ferrihydrite and sulfate as the electron acceptors and inoculated them with subsurface sediment as the microbial inoculum. Sulfate and ferrihydrite reduction occurred simultaneously and were faster with lactate than with acetate. 16S rRNA-based sequence analysis of the communities over time revealed that Desulfotomaculum was the major driver for sulfate reduction coupled with propionate oxidation in lactate-amended incubations. The reduction of sulfate resulted in sulfide production and subsequent abiotic reduction of ferrihydrite. In contrast, glucose promoted faster reduction of ferrihydrite, but without reduction of sulfate. Interestingly, the glucose-amended incubations led to two different biogeochemical trajectories among replicate bottles that resulted in distinct coloration (white and brown). The two outcomes in geochemical evolution might be due to the stochastic evolution of the microbial communities or subtle differences in the initial composition of the fermenting microbial community and its development via the usemore » of different glucose fermentation pathways available within the community. Synchrotron-based x-ray analysis indicated that siderite and amorphous Fe(II) were formed in the replicate bottles with glucose, while ferrous sulfide and vivianite were formed with lactate or acetate. As a result, these data sets reveal that use of different C utilization pathways projects significant changes in microbial community composition over time that uniquely impact both the geochemistry and mineralogy of subsurface environments.« less
Authors:
 [1] ;  [2] ;  [2] ;  [2] ;  [2] ;  [2] ;  [2] ;  [3]
  1. Argonne National Lab. (ANL), Argonne, IL (United States); Korea Institute of Science and Technology (KIST) - Gangneung Institute, Gangneung (South Korea)
  2. Argonne National Lab. (ANL), Argonne, IL (United States)
  3. Univ. of Akron, Akron, OH (United States)
Publication Date:
Grant/Contract Number:
AC02-06CH11357
Type:
Accepted Manuscript
Journal Name:
PLoS ONE
Additional Journal Information:
Journal Volume: 11; Journal Issue: 1; Journal ID: ISSN 1932-6203
Publisher:
Public Library of Science
Research Org:
Argonne National Lab. (ANL), Argonne, IL (United States)
Sponsoring Org:
USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC-23), Subsurface Biogeochemical Research
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; 59 BASIC BIOLOGICAL SCIENCES; electron donor; iron reduction; microbial community development; sulfate reduction; sulfates; glucose; sulfides; glucose metabolism; sediment; fermentation; oxidation
OSTI Identifier:
1399243

Kwon, Man Jae, O’Loughlin, Edward J., Boyanov, Maxim I., Brulc, Jennifer M., Johnston, Eric R., Kemner, Kenneth M., Antonopoulos, Dionysios A., and Senko, John M.. Impact of Organic Carbon Electron Donors on Microbial Community Development under Iron- and Sulfate-Reducing Conditions. United States: N. p., Web. doi:10.1371/journal.pone.0146689.
Kwon, Man Jae, O’Loughlin, Edward J., Boyanov, Maxim I., Brulc, Jennifer M., Johnston, Eric R., Kemner, Kenneth M., Antonopoulos, Dionysios A., & Senko, John M.. Impact of Organic Carbon Electron Donors on Microbial Community Development under Iron- and Sulfate-Reducing Conditions. United States. doi:10.1371/journal.pone.0146689.
Kwon, Man Jae, O’Loughlin, Edward J., Boyanov, Maxim I., Brulc, Jennifer M., Johnston, Eric R., Kemner, Kenneth M., Antonopoulos, Dionysios A., and Senko, John M.. 2016. "Impact of Organic Carbon Electron Donors on Microbial Community Development under Iron- and Sulfate-Reducing Conditions". United States. doi:10.1371/journal.pone.0146689. https://www.osti.gov/servlets/purl/1399243.
@article{osti_1399243,
title = {Impact of Organic Carbon Electron Donors on Microbial Community Development under Iron- and Sulfate-Reducing Conditions},
author = {Kwon, Man Jae and O’Loughlin, Edward J. and Boyanov, Maxim I. and Brulc, Jennifer M. and Johnston, Eric R. and Kemner, Kenneth M. and Antonopoulos, Dionysios A. and Senko, John M.},
abstractNote = {Although iron- and sulfate-reducing bacteria in subsurface environments have crucial roles in biogeochemical cycling of C, Fe, and S, how specific electron donors impact the compositional structure and activity of native iron- and/or sulfate-reducing communities is largely unknown. To understand this better, we created bicarbonate-buffered batch systems in duplicate with three different electron donors (acetate, lactate, or glucose) paired with ferrihydrite and sulfate as the electron acceptors and inoculated them with subsurface sediment as the microbial inoculum. Sulfate and ferrihydrite reduction occurred simultaneously and were faster with lactate than with acetate. 16S rRNA-based sequence analysis of the communities over time revealed that Desulfotomaculum was the major driver for sulfate reduction coupled with propionate oxidation in lactate-amended incubations. The reduction of sulfate resulted in sulfide production and subsequent abiotic reduction of ferrihydrite. In contrast, glucose promoted faster reduction of ferrihydrite, but without reduction of sulfate. Interestingly, the glucose-amended incubations led to two different biogeochemical trajectories among replicate bottles that resulted in distinct coloration (white and brown). The two outcomes in geochemical evolution might be due to the stochastic evolution of the microbial communities or subtle differences in the initial composition of the fermenting microbial community and its development via the use of different glucose fermentation pathways available within the community. Synchrotron-based x-ray analysis indicated that siderite and amorphous Fe(II) were formed in the replicate bottles with glucose, while ferrous sulfide and vivianite were formed with lactate or acetate. As a result, these data sets reveal that use of different C utilization pathways projects significant changes in microbial community composition over time that uniquely impact both the geochemistry and mineralogy of subsurface environments.},
doi = {10.1371/journal.pone.0146689},
journal = {PLoS ONE},
number = 1,
volume = 11,
place = {United States},
year = {2016},
month = {1}
}

Works referenced in this record:

Enumeration and Characterization of Iron(III)-Reducing Microbial Communities from Acidic Subsurface Sediments Contaminated with Uranium(VI)
journal, December 2003

Ferrozine---a new spectrophotometric reagent for iron
journal, June 1970
  • Stookey, Lawrence L.
  • Analytical Chemistry, Vol. 42, Issue 7, p. 779-781
  • DOI: 10.1021/ac60289a016

Biostimulation of iron reduction and subsequent oxidation of sediment containing Fe-silicates and Fe-oxides: Effect of redox cycling on Fe(III) bioreduction
journal, July 2007

Search and clustering orders of magnitude faster than BLAST
journal, August 2010