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Iron-reducing bacteria decompose lignin by electron transfer from soil organic matter
Carolina Merino1, Yakov Kuzyakov2, Karina Godoy3
1Center of Plant, Soil Interaction and Natural Resources Biotechnology Scientific and Technological Bioresource Nucleus (BIOREN), Temuco, Chile; Laboratory of Conservation and Dynamics of Volcanic Soils, Department of Chemical Sciences and Natural Resources, Universidad de La Frontera, Temuco, Chile; Network for Extreme Environmental Research, Universidad de la Frontera, Temuco, Chile.
Iron-reducing bacteria (IRB) use lignin in soil organic matter as an energy source, facilitating the reduction of iron oxides. This process enhances carbon dioxide release, showing IRB
Area of Science:
- Soil microbiology and biogeochemistry.
- Organic matter decomposition and nutrient cycling.
Background:
- Iron-reducing bacteria (IRB) are key players in anaerobic soil electron transfer.
- Understanding how IRB utilize energy from organic matter decomposition, particularly lignin, is crucial.
- The electron transfer mechanisms and energy acquisition by IRB remain a significant research question.
Purpose of the Study:
- To investigate the hypothesis that IRB obtain electrons from reduced soil organic matter (SOM) via lignin oxidation.
- To determine the role of specific IRB strains, Geobacter metallireducens and Geobacter lovleyi, in lignin degradation and iron reduction.
- To quantify the impact of IRB inoculation on carbon dioxide (CO2) release and iron (II) production across diverse soil types.
Main Methods:
- Isolation and identification of IRB from various global soil samples using phospholipid fatty acid (PLFA) analysis and PCR.
- Inoculation of IRB into diverse soil samples and monitoring of parallel processes.
- Measurement of CO2 release, Fe(II) production, H2O2 consumption, and lignin depolymerization using fluorescence imaging.
Main Results:
- Geobacter metallireducens and Geobacter lovleyi were prevalent IRB strains that significantly increased ligninolytic enzyme activity.
- IRB inoculation led to a 140% increase in CO2 release compared to Fenton reactions and a 40% decrease compared to non-sterile soils.
- CO2 release strongly correlated with Fe(II) production and H2O2 consumption, particularly in iron-rich Basaltic-Antarctic soils where lignin depolymerization was highest.
Conclusions:
- Iron-reducing bacteria effectively oxidize lignin in soil organic matter across various soil types and pH ranges.
- A conceptual model of electron shuttling from lignin-containing SOM to IRB for energy production and Fe(III) reduction is proposed.
- IRB play a vital role in the anaerobic decomposition of soil organic matter, linking lignin oxidation to iron reduction.
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