Open Access
- 1 September 2015
- journal article
- research article
- Published by American Society for Microbiology in Applied and Environmental Microbiology
- Vol. 81 (17) , 6003-6011
Abstract
In marine sediments cathodic oxygen reduction at the sediment surface can be coupled to anodic sulfide oxidation in deeper anoxic layers through electrical currents mediated by filamentous, multicellular bacteria of theDesulfobulbaceaefamily, the so-called cable bacteria. Until now, cable bacteria have only been reported from marine environments. In this study, we demonstrate that cable bacteria also occur in freshwater sediments. In a first step, homogenized sediment collected from the freshwater stream Giber Å, Denmark, was incubated in the laboratory. After 2 weeks, pH signatures and electric fields indicated electron transfer between vertically separated anodic and cathodic half-reactions. Fluorescencein situhybridization revealed the presence ofDesulfobulbaceaefilaments. In addition,in situmeasurements of oxygen, pH, and electric potential distributions in the waterlogged banks of Giber Å demonstrated the presence of distant electric redox coupling in naturally occurring freshwater sediment. At the same site, filamentousDesulfobulbaceaewith cable bacterium morphology were found to be present. Their 16S rRNA gene sequence placed them as a distinct sister group to the known marine cable bacteria, with the genusDesulfobulbusas the closest cultured lineage. The results of the present study indicate that electric currents mediated by cable bacteria could be important for the biogeochemistry in many more environments than anticipated thus far and suggest a common evolutionary origin of the cable phenotype withinDesulfobulbaceaewith subsequent diversification into a freshwater and a marine lineage.Keywords
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