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anoxic zone. Phylotypes were related to members of hydrocarbon-degrading
consortia, SAR406 cluster, and to Desulfobacterium anilini [58]. Perry et al.
[37] isolated Shewanella putrefaciens from the Black Sea water column, a res-
piratory facultative anaerobe that can reduce quantitatively thiosulfate, sulfite,
and elemental sulfur to sulfide. Shewanella species were accounted for 20 to
50% of the total bacterial counts in the suboxic zone (10 5 cells ml 1 ) [30].
Several authors speculated that due to their respiratory versatility, Shewanella
may play a significant role in both, metal and sulfur cycling.
Figure 4. Combined depth profiles of sulfate reduction rates (SRR) and dark 14 CO 2 fixation
rates (CO 2 fix) in the open Black Sea at Station 4 in May 1988; 44˚20.23'N, 32˚09.54'E, depth
1998 m.
Bacteria of the Nitrogen Cycling. A brief overview of different bacter-
ial groups related to the sulfur cycling present in the Black Sea chemocline
shows that autotrophic and chemolithotrophic thiobacilli of Thiobacillus and
Thiomicrospira genera play an important role in the chemosynthesis and sul-
fide oxidation in the chemocline. Some of these strains may use nitrate as an
electron acceptor in oxidizing sulfide [52, 56, 57], but the depth distribution of
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