M. Fukui et al., Physiology, phylogenetic relationships, and ecology of filamentous sulfate-reducing bacteria (genus Desulfonema), ARCH MICROB, 172(4), 1999, pp. 193-203
Microscopy of organic-rich sulfidic sediment samples of marine and freshwat
er origin revealed filamentous, multicellular microorganisms with gliding m
otility. Many of these neither contained sulfur droplets such as the Beggia
toa species nor exhibited the autofluorescence of the chlorophyll-containin
g cyanobacteria. A frequently observed morphological type of filamentous mi
croorganism was enriched under anoxic conditions in the dark with isobutyra
te plus sulfate. Two strains of filamentous, gliding sulfate-reducing bacte
ria, Tokyo 01 and Jade 02, were isolated in pure cultures. Both isolates ox
idized acetate and other aliphatic acids. Enzyme assays indicated that the
terminal oxidation occurs via the anaerobic C-1 pathway (carbon monoxide de
hydrogenase pathway). The 16S rRNA genes of the new isolates and of the two
formerly described filamentous species of sulfate-reducing bacteria, Desul
fonema limicola and Desulfonema magnum, were analyzed. All four strains wer
e closely related to each other and affiliated with the delta-subclass of P
roteobacteria. Another close relative was the unicellular Desulfococcus mul
tivorans. Based on phylogenetic relationships and physiological properties,
Strains Tokyo 01 and Jade 02 are assigned to a new species, Desulfonema is
himotoi. A new, fluorescently labeled oligonucleotide probe targeted agains
t 16S rRNA was designed so that that it hybridized specifically with whole
cells of Desulfonema species. Filamentous bacteria that hybridized with the
same probe were detected in sediment samples and in association with the f
ilamentous sulfur-oxidizing bacterium Thioploca in its natural habitat. We
conclude that Desulfonema species constitute an ecologically significant fr
action of the sulfate-reducing bacteria in organic-rich sediments and micro
bial mats.