“…Since their discovery, cable bacteria have been found at the oxic-anoxic interface in a wide range of aquatic sediment environments, including marine (e.g., Malkin et al, 2014 ; Burdorf et al, 2017 ), freshwater ( Risgaard-Petersen et al, 2015 ), and aquifer ( Müller et al, 2016 ) sediments. In these environments, cable bacteria strongly influence the elemental cycling of sulfur, iron, phosphorus, and methane ( Risgaard-Petersen et al, 2012 ; Seitaj et al, 2015 ; Sulu-Gambari et al, 2016 ; Scholz et al, 2020 ). Additionally, cable bacteria have been found attached to the anode of a benthic microbial fuel cell placed in anaerobic conditions ( Reimers et al, 2017 ) or in association with oxygenated zones around plant roots ( Scholz et al, 2019 ) and worm tubes in marine sediments ( Aller et al, 2019 ).…”