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Published on: July 24, 2016
Iron requirement for Mn(II) oxidation by Leptothrix discophora SS-1
Iman A El Gheriany1, Daniela Bocioaga, Anthony G Hay
1School of Civil and Environmental Engineering, Cornell University, Ithaca, New York 14853, USA.
Iron limitation reduces the manganese(II) oxidation ability of Leptothrix discophora SS-1. This suggests iron is crucial for manganese oxidation, possibly as a component of the manganese-oxidizing factor (MOF).
Area of Science:
- Biogeochemistry
- Microbial Metabolism
- Environmental Science
Background:
- Biogenic manganese oxides are formed through microbial oxidation of Mn(II), a critical process in manganese geochemical cycling.
- Leptothrix discophora SS-1 is a model bacterium for studying extracellular Mn(II) oxidation, often attributed to a manganese-oxidizing factor (MOF).
Purpose of the Study:
- To investigate the influence of iron availability on the rate of extracellular Mn(II) oxidation by Leptothrix discophora SS-1.
- To explore the mechanistic role of iron in Mn(II) oxidation and its potential interaction with the MOF.
Main Methods:
- Culturing Leptothrix discophora SS-1 in media with varying iron concentrations (limited vs. sufficient).
- Evaluating extracellular Mn(II) oxidation rates under different iron conditions.
- Assessing the impact of copper supplementation and analyzing mofA gene transcript levels via quantitative PCR.
Main Results:
- Iron-limited cultures exhibited significantly reduced Mn(II) oxidation rates compared to iron-sufficient cultures.
- The addition of copper did not restore Mn(II) oxidation in iron-limited conditions.
- Iron limitation did not affect mofA gene transcription levels, suggesting post-transcriptional regulation.
Conclusions:
- Iron availability is critical for efficient Mn(II) oxidation by Leptothrix discophora SS-1.
- The data suggest iron may be a direct component of the MOF or indirectly influence Mn(II) oxidation through other cellular functions.
- Further research is needed to elucidate the precise mechanistic role of iron in this biogeochemical process.
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