Chemotaxis and motility of Achromatium oxaliferum in response to oxygen, sulfide, and nitrate

Bacteria of the genus Achromatium are known for their large cell sizes and intracellular calcium carbonate deposits. Achromatium inhabit freshwater, brackish, and marine sediments where they accumulate to high abundances at the oxic-anoxic interface. These bacteria alter their vertical position in the sediment along with daily fluctuations in oxygen concentrations. Yet, the mechanism behind their migration in the sediment remains unknown. In this study, we used chemotaxis assays and time-lapse microphotography to analyze the motility and chemotactic behavior of Achromatium oxaliferum. Microscopic observations revealed that rolling and gliding were the main forms of locomotion exhibited by Achromatium. In absence of any stimulant, the movement appeared to be mostly random and changes in direction frequently occurred. Chemotaxis assays showed a negative chemotaxis of Achromatium to oxygen, sulfide, and nitrate, as evidenced by the change from undirected to directed locomotion against the respective chemical gradient. For periods of more than 1 hour, Achromatium cells moved continuously towards regions of low concentration. We further investigated whether the genetic repertoire of Achromatium corresponds to our observations. Based on lab experiments and bioinformatic analyses we conclude that Achomatium motility is propelled by type IV pili guided by a plethora of chemo- and photoreceptors. We conclude that Achromatium uses negative chemo- and phototaxis to confine their distribution in aquatic sediments between opposing oxygen and sulfide gradients. This allows Achromatium to dynamically adjust its position in redox gradients, and thus is likely to have a major contribution to its success in the global colonization of diverse aquatic sediments.