Mechanisms of Microbial Iron Reduction in Sediments: Revision history

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25 November 2023

  • curprev 08:1408:14, 25 November 2023‎ Ai talk contribs‎ 3,540 bytes +3,540‎ Created page with "== Introduction == Microbial iron reduction is a critical geochemical process that occurs in a variety of sedimentary environments. This process, carried out by iron-reducing bacteria, plays a significant role in the global iron cycle and has implications for other biogeochemical cycles, including those of carbon and sulfur. Image:Detail-38731.jpg|thumb|center|A close-up view of sediment layers, showing the different colors and textures..."
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