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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Volume 14, issue 3 | Copyright
Biogeosciences, 14, 683-701, 2017
https://doi.org/10.5194/bg-14-683-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 10 Feb 2017

Research article | 10 Feb 2017

Long-distance electron transport occurs globally in marine sediments

Laurine D. W. Burdorf1, Anton Tramper1, Dorina Seitaj1,2, Lorenz Meire3,4, Silvia Hidalgo-Martinez1, Eva-Maria Zetsche1,5, Henricus T. S. Boschker1, and Filip J. R. Meysman1,2 Laurine D. W. Burdorf et al.
  • 1NIOZ Royal Netherlands Institute for Sea Research, Department of Estuarine and Delta Systems, and Utrecht University, Korringaweg 7, 4401 NT Yerseke, the Netherlands
  • 2Department of Analytical, Environmental and Geo-Chemistry, Vrije Universiteit Brussel, Pleinlaan 2, 1050 Brussels, Belgium
  • 3Greenland Institute of Natural Resources, Greenland Climate Research Centre, P.O. Box 570, Kivioq 5, 3900 Nuuk, Greenland
  • 4Arctic Research Centre, Aarhus University, 8000 Aarhus, Denmark
  • 5Department of Marine Sciences, University of Gothenburg, Carl Skottsberg gata 22B, 41319 Gothenburg, Sweden

Abstract. Recently, long filamentous bacteria have been reported conducting electrons over centimetre distances in marine sediments. These so-called cable bacteria perform an electrogenic form of sulfur oxidation, whereby long-distance electron transport links sulfide oxidation in deeper sediment horizons to oxygen reduction in the upper millimetres of the sediment. Electrogenic sulfur oxidation exerts a strong impact on the local sediment biogeochemistry, but it is currently unknown how prevalent the process is within the seafloor. Here we provide a state-of-the-art assessment of its global distribution by combining new field observations with previous reports from the literature. This synthesis demonstrates that electrogenic sulfur oxidation, and hence microbial long-distance electron transport, is a widespread phenomenon in the present-day seafloor. The process is found in coastal sediments within different climate zones (off the Netherlands, Greenland, the USA, Australia) and thrives on a range of different coastal habitats (estuaries, salt marshes, mangroves, coastal hypoxic basins, intertidal flats). The combination of a widespread occurrence and a strong local geochemical imprint suggests that electrogenic sulfur oxidation could be an important, and hitherto overlooked, component of the marine cycle of carbon, sulfur and other elements.

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Recently, long filamentous bacteria have been reported to conduct electrons over centimetre distances in marine sediments. These so-called cable bacteria have an electricity-based metabolism, effectively turning the seafloor into a natural battery. In this study we demonstrate a global occurrence of these cable bacteria in marine sediments, spanning a large range of climate zones (off Greenland, the USA, Australia, the Netherlands) and a large range of coastal habitats.
Recently, long filamentous bacteria have been reported to conduct electrons over centimetre...
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