Biogeosciences, 16, 811–829, 2019 https://doi.org/10.5194/bg-16-811-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Mineral formation induced by cable bacteria performing long-distance electron transport in marine sediments Nicole M. J. Geerlings1, Eva-Maria Zetsche2,3, Silvia Hidalgo-Martinez4, Jack J. Middelburg1, and Filip J. R. Meysman4,5 1Department of Earth Sciences, Utrecht University, Princetonplein 8a, 3584 CB Utrecht, the Netherlands 2Department of Marine Sciences, University of Gothenburg, Carl Skottsberg gata 22B, 41319 Gothenburg, Sweden 3Department of Estuarine and Delta Systems, Royal Netherlands Institute for Sea Research, Utrecht University, Korringaweg 7, 4401 NT Yerseke, the Netherlands 4Department of Biology, Ecosystem Management Research Group, Universiteit Antwerpen, Universiteitsplein 1, 2160 Antwerp, Belgium 5Department of Biotechnology, Delft University of Technology, Van der Maasweg 9, 2629 HZ Delft, the Netherlands Correspondence: Nicole M. J. Geerlings (
[email protected]) Received: 10 October 2018 – Discussion started: 22 October 2018 Revised: 10 January 2019 – Accepted: 26 January 2019 – Published: 13 February 2019 Abstract. Cable bacteria are multicellular, filamentous mi- esize that the complete encrustation of filaments might create croorganisms that are capable of transporting electrons over a diffusion barrier and negatively impact the metabolism of centimeter-scale distances. Although recently discovered, the cable bacteria. these bacteria appear to be widely present in the seafloor, and when active they exert a strong imprint on the local geochemistry. In particular, their electrogenic metabolism in- 1 Introduction duces unusually strong pH excursions in aquatic sediments, which induces considerable mineral dissolution, and subse- 1.1 Cable bacteria quent mineral reprecipitation.