Articles | Volume 14, issue 22
https://doi.org/10.5194/bg-14-5171-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-14-5171-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Ferrihydrite-associated organic matter (OM) stimulates reduction by Shewanella oneidensis MR-1 and a complex microbial consortia
Rebecca Elizabeth Cooper
Aquatic Geomicrobiology, Friedrich Schiller University, 07743 Jena, Germany
Karin Eusterhues
Department of Hydrogeology, Institute of Geosciences, Friedrich Schiller University, 07743 Jena, Germany
Carl-Eric Wegner
Aquatic Geomicrobiology, Friedrich Schiller University, 07743 Jena, Germany
Kai Uwe Totsche
Department of Hydrogeology, Institute of Geosciences, Friedrich Schiller University, 07743 Jena, Germany
Kirsten Küsel
CORRESPONDING AUTHOR
Aquatic Geomicrobiology, Friedrich Schiller University, 07743 Jena, Germany
The German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, 07743 Leipzig, Germany
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Latest update: 20 Nov 2024
Short summary
In this study we show increasing organic matter (OM) content on ferrihydrite surfaces enhances Fe reduction by the model Fe reducer S. oneidensis and a microbial consortia extracted from peat. Similarities in reduction rates between S. oneidensis and the consortia suggest electron shuttling dominates in OM-rich soils. Community profile analyses showed enrichment of fermenters with pure ferrihydrite, whereas OM–mineral complexes favored enrichment of Fe-reducing Desulfobacteria and Pelosinus sp.
In this study we show increasing organic matter (OM) content on ferrihydrite surfaces enhances...
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