4.5 Article

Importance of microbial iron reduction in deep sediments of river-dominated continental-margins

Journal

MARINE CHEMISTRY
Volume 178, Issue -, Pages 22-34

Publisher

ELSEVIER SCIENCE BV
DOI: 10.1016/j.marchem.2015.12.003

Keywords

Iron reduction; Sulfate reduction; Continental margin; Sediments; Carbon remineralization

Funding

  1. National Science Foundation [OCE-0851156, OCE-1151698]
  2. Agence Nationale de la Recherche [ANR-11-BS56-0030]
  3. Agence Nationale de la Recherche (ANR) [ANR-11-BS56-0030] Funding Source: Agence Nationale de la Recherche (ANR)
  4. Directorate For Geosciences
  5. Division Of Ocean Sciences [1438648] Funding Source: National Science Foundation
  6. Division Of Ocean Sciences
  7. Directorate For Geosciences [1151698] Funding Source: National Science Foundation

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Remineralization of organic carbon in deep-sea sediments is thought to proceed primarily via aerobic respiration and sulfate reduction because the supply of nitrate and metal oxides is not usually significant in deep-sea sediments. Dissimilatory metal reduction, on the other hand, may represent a dominant pathway in coastal and continental shelf sediments where delivery of terrigenous Fe(III) and Mn(IV/III) oxides is sufficiently high or where physical mixing processes near the sediment-water interface can result in the reoxidation of Fe2+ or Mn2+. Passive continental margin sediments receiving outflow from large rivers are well-known deposition centers for organic carbon and may also be hotspots for metal-reducing microbial activity, considering the simultaneous rapid deposition of unconsolidated metal oxides of terrigenous origin. Despite its potential, only a few studies have examined the role of microbial metal reduction in C-org remineralization in these environments. To investigate carbon remineralization processes in continental margin sediments, shallow cores across channels and levees in the Congo River fan (similar to 5000 m) and Louisiana slope (<1800 m) were profiled for the main redox species involved in early diagenesis using a combination of voltammetric gold mercury (Au/Hg) microelectrodes and conventional analyses. Interestingly, metal reduction dominated carbon remineralization processes in the top similar to 20 cm of sediment subject to high deposition, while evidence for sulfate reduction was lacking. These findings suggest that dissimilatory Fe(III) reduction may be more significant than previously thought in continental slope sediments, which may have important implications on carbon cycling in marine environments. In addition, these findings may have geological implications in controlling atmospheric oxygen levels over geological time and the evolution of microbial life on Earth. (C) 2015 Elsevier B.V. All rights reserved.

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