Long-distance electron transport occurs globally in marine sediments

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...

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Bibliographic Details
Published in:Biogeosciences
Main Authors: Burdorf, Laurine D.W., Tramper, Anton, Seitaj, Dorina, Meire, Lorenz, Hidalgo-Martinez, Silvia, Zetsche, Eva Maria, Boschker, Henricus T.S., Meysman, Filip J.R.
Format: Article in Journal/Newspaper
Language:English
Published: 2017
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Online Access:https://pure.au.dk/portal/da/publications/longdistance-electron-transport-occurs-globally-in-marine-sediments(88b9fe5f-40c2-4c2c-ad1e-3e6213ce6f4b).html
https://doi.org/10.5194/bg-14-683-2017
https://pure.au.dk/ws/files/120650496/bg_14_683_2017.pdf
http://www.scopus.com/inward/record.url?scp=85012279027&partnerID=8YFLogxK
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Summary: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.