The sulfate-reducing bacterium Desulfovibrio desulfuricans strain CSN
(DSM 9104) oxidized H-2 with thiosulfate, sulfate, sulfite, nitrite, n
itrate and oxygen with rates increasing (in the order listed) from 20
to 525 nmol H-2 min(-1) mg(-1) protein. Nitrate reduction was induced
by nitrate or limiting concentrations of sulfate during growth, while
all other activities were constitutive. Oxygen prevented reduction of
all other electron accepters, while nitrate and nitrite blocked the re
duction of the sulfur compounds. In the presence of H-2 and reduced su
lfur compounds, H-2 was the preferred electron donor. The cells oxidiz
ed thiosulfate or sulfite coupled to the reduction of nitrate to ammon
ia. This represents a novel type of metabolism connecting the sulfur a
nd nitrogen cycles. It is concluded that oxygen is the preferred elect
ron acceptor of D. desulfuricans. Sulfate reduction in oxic environmen
ts must be due to different organisms or mechanisms.