Sulfidogenesis from 2-aminoethanesulfonate (taurine) fermentation by a morphologically unusual sulfate-reducing bacterium, Desulforhopalus singaporensis sp nov.
Tj. Lie et al., Sulfidogenesis from 2-aminoethanesulfonate (taurine) fermentation by a morphologically unusual sulfate-reducing bacterium, Desulforhopalus singaporensis sp nov., APPL ENVIR, 65(8), 1999, pp. 3328-3334
A pure culture of an obligately anaerobic marine bacterium was obtained fro
m an anaerobic enrichment culture in which taurine (2-aminoethanesulfonate)
was the sole source of carbon, energy, and nitrogen, Taurine fermentation
resulted in acetate, ammonia, and sulfide as end products. Other sulfonates
, including 2-hydroxyethanesulfonate (isethionate) and cysteate (alanine-3-
sulfonate), were not fermented. When malate was the sole source of carbon a
nd energy, the bacterium reduced sulfate, sulfite, thiosulfate, or nitrate
(reduced to ammonia) but did not use fumarate or dimethyl sulfoxide as a te
rminal electron acceptor for growth. Taurine-grown cells had significantly
lower adenylylphosphosulfate reductase activities than sulfate-grown cells
had, which was consistent with the notion that sulfate was not released as
a result of oxidative C-S bond cleavage and then assimilated. The name Desu
lforhopalus singaporensis is proposed for this sulfate-reducing bacterium,
which is morphologically unusual compared to the previously described sulfa
te-reducing bacteria by virtue of the spinae present on the rod-shaped, gra
m-negative, nonmotile cells; endospore formation was not discerned, nor was
desulfoviridin detected. Granules of poly-beta-hgdroxybutyrate were abunda
nt in taurine-grown cells. This organism shares with the other member of th
e genus Desulforhopalus which has been described a unique 13-base deletion
in the 16S ribosomal DNA. It differs in several ways from a recently descri
bed endospore-forming anaerobe (K. Denger, H. Laue, and A. M. Cook, Arch. M
icrobiol. 168:297-301, 1997) that reportedly produces thiosulfate but not s
ulfide from taurine fermentation. D. singaporensis thus appears to be the f
irst example of an organism which exhibits sulfidogenesis during taurine fe
rmentation. Implications for sulfonate sulfur in the sulfur cycle are discu
ssed.