ABSTRACT
Life in Movile Cave (Romania) relies entirely on carbon fixation by bacteria. The microbial community in the surface water of Movile Cave’s hypoxic air bells is dominated by large spherical-ovoid bacteria we identified as Thiovulum sp. (Campylobacterota). These form a separate phylogenetic cluster within the Thiovulaceae, consisting mostly of freshwater cave bacteria. We compared the closed genome of this Thiovulum to that of the marine strain Thiovulum ES, and to a genome we assembled from public data from the sulfidic Frasassi caves. The Movile and Frasassi Thiovulum were very similar, differing greatly from the marine strain. Based on their genomes, cave Thiovulum can switch between aerobic and anaerobic sulfide oxidation using O2 and NO3- as electron acceptors, respectively. NO3-, is likely reduced to NH3 via dissimilatory nitrate reduction to ammonia using periplasmic nitrate reductase (Nap) and hydroxylamine oxidoreductase. Thus, Thiovulum, is likely important to both S and N cycles in sulfidic subterranean aquatic ecosystems. Additionally, we suggest that the short peritrichous flagella-like structures typical of Thiovulum are type IV pili, for which genes were found in all Thiovulum genomes. These pili may play a role in veil formation, connecting adjacent cells and the exceptionally fast swimming of these bacteria.
Competing Interest Statement
The authors have declared no competing interest.
