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Title: Controls on Iron Reduction and Biomineralization over Broad Environmental Conditions as Suggested by the Firmicutes Orenia metallireducens Strain Z6

Abstract

Microbial iron reduction is a ubiquitous biogeochemical process driven by diverse microorganisms in a variety of environments. However, it is often difficult to separate the biological from the geochemical controls on bioreduction of Fe(III) oxides. In this study, we investigated the primary driving factor(s) that mediate secondary iron mineral formation over a broad range of environmental conditions using a single dissimilatory iron reducer, Orenia metallireducens strain Z6. A total of 17 distinct geochemical conditions were tested with differing pH (6.5–8.5), temperature (22–50 °C), salinity (2–20% NaCl), anions (phosphate and sulfate), electron shuttle (anthraquinone-2,6-disulfonate), and Fe(III) oxide mineralogy (ferrihydrite, lepidocrocite, goethite, hematite, and magnetite). The observed rates and extent of iron reduction differed significantly with kint between 0.186 and 1.702 mmol L–1 day–1 and Fe(II) production ranging from 6.3% to 83.7% of the initial Fe(III). Using X-ray absorption and scattering techniques (EXAFS and XRD), we identified and assessed the relationship between secondary minerals and the specific environmental conditions. It was inferred that the observed bifurcation of the mineralization pathways may be mediated by differing extents of Fe(II) sorption on the remaining Fe(III) minerals. These results expand our understanding of the controls on biomineralization during microbial iron reduction and aid the developmentmore » of practical applications.« less

Authors:
ORCiD logo [1];  [2]; ORCiD logo [3]; ORCiD logo [4];  [4];  [4];  [2];  [5];  [6];  [6];  [6];  [2]
+ Show Author Affiliations
  1. China Univ. of Geosciences, Wuhan (China); Univ. of Illinois at Urbana-Champaign, IL (United States)
  2. Univ. of Illinois at Urbana-Champaign, IL (United States)
  3. Argonne National Lab. (ANL), Argonne, IL (United States); Bulgarian Academy of Sciences, Sofia (Bulgaria)
  4. Argonne National Lab. (ANL), Argonne, IL (United States)
  5. Marine Biological Laboratory, Woods Hole, MA (United States)
  6. China Univ. of Geosciences, Wuhan (China)
Publication Date:
Research Org.:
Argonne National Laboratory (ANL), Argonne, IL (United States). Advanced Photon Source (APS)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER); National Aeronautics and Space Administration (NASA); National Natural Science Foundation of China (NSFC)
OSTI Identifier:
1774368
Grant/Contract Number:  
AC02-06CH11357; NNA13AA91A; 41877321; 91851211
Resource Type:
Accepted Manuscript
Journal Name:
Environmental Science and Technology
Additional Journal Information:
Journal Volume: 54; Journal Issue: 16; Journal ID: ISSN 0013-936X
Publisher:
American Chemical Society (ACS)
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; iron; redox reactions; phosphates; anions; minerals

Citation Formats

Dong, Yiran, Sanford, Robert A., Boyanov, Maxim I., Flynn, Theodore M., O’Loughlin, Edward J., Kemner, Kenneth M., George, Samantha, Fouke, Kaitlyn E., Li, Shuyi, Huang, Dongmei, Li, Shuzhen, and Fouke, Bruce W. Controls on Iron Reduction and Biomineralization over Broad Environmental Conditions as Suggested by the Firmicutes Orenia metallireducens Strain Z6. United States: N. p., 2020. Web. doi:10.1021/acs.est.0c03853.
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Dong, Yiran, Sanford, Robert A., Boyanov, Maxim I., Flynn, Theodore M., O’Loughlin, Edward J., Kemner, Kenneth M., George, Samantha, Fouke, Kaitlyn E., Li, Shuyi, Huang, Dongmei, Li, Shuzhen, & Fouke, Bruce W. Controls on Iron Reduction and Biomineralization over Broad Environmental Conditions as Suggested by the Firmicutes Orenia metallireducens Strain Z6. United States. https://doi.org/10.1021/acs.est.0c03853
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Dong, Yiran, Sanford, Robert A., Boyanov, Maxim I., Flynn, Theodore M., O’Loughlin, Edward J., Kemner, Kenneth M., George, Samantha, Fouke, Kaitlyn E., Li, Shuyi, Huang, Dongmei, Li, Shuzhen, and Fouke, Bruce W. Tue . "Controls on Iron Reduction and Biomineralization over Broad Environmental Conditions as Suggested by the Firmicutes Orenia metallireducens Strain Z6". United States. https://doi.org/10.1021/acs.est.0c03853. https://www.osti.gov/servlets/purl/1774368.
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@article{osti_1774368,
title = {Controls on Iron Reduction and Biomineralization over Broad Environmental Conditions as Suggested by the Firmicutes Orenia metallireducens Strain Z6},
author = {Dong, Yiran and Sanford, Robert A. and Boyanov, Maxim I. and Flynn, Theodore M. and O’Loughlin, Edward J. and Kemner, Kenneth M. and George, Samantha and Fouke, Kaitlyn E. and Li, Shuyi and Huang, Dongmei and Li, Shuzhen and Fouke, Bruce W.},
abstractNote = {Microbial iron reduction is a ubiquitous biogeochemical process driven by diverse microorganisms in a variety of environments. However, it is often difficult to separate the biological from the geochemical controls on bioreduction of Fe(III) oxides. In this study, we investigated the primary driving factor(s) that mediate secondary iron mineral formation over a broad range of environmental conditions using a single dissimilatory iron reducer, Orenia metallireducens strain Z6. A total of 17 distinct geochemical conditions were tested with differing pH (6.5–8.5), temperature (22–50 °C), salinity (2–20% NaCl), anions (phosphate and sulfate), electron shuttle (anthraquinone-2,6-disulfonate), and Fe(III) oxide mineralogy (ferrihydrite, lepidocrocite, goethite, hematite, and magnetite). The observed rates and extent of iron reduction differed significantly with kint between 0.186 and 1.702 mmol L–1 day–1 and Fe(II) production ranging from 6.3% to 83.7% of the initial Fe(III). Using X-ray absorption and scattering techniques (EXAFS and XRD), we identified and assessed the relationship between secondary minerals and the specific environmental conditions. It was inferred that the observed bifurcation of the mineralization pathways may be mediated by differing extents of Fe(II) sorption on the remaining Fe(III) minerals. These results expand our understanding of the controls on biomineralization during microbial iron reduction and aid the development of practical applications.},
doi = {10.1021/acs.est.0c03853},
journal = {Environmental Science and Technology},
number = 16,
volume = 54,
place = {United States},
year = {Tue Jul 21 00:00:00 EDT 2020},
month = {Tue Jul 21 00:00:00 EDT 2020}
}
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https://doi.org/10.1021/acs.est.0c03853
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