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2 erved in T. thermophila is present in marine Thiobacillus and Thiomicrospira species, production of e
3 opseudomonas, Methyloversatilis, Caldilinea, Thiobacillus, Azoarcus, Hyphomicrobium, and Leptothrix.
9 e, we provide evidence for the capability of Thiobacillus denitrificans to anaerobically oxidize a pu
10 ical oxidants (nitrate and/or nitrite) or by Thiobacillus denitrificans, a widespread, denitrifying,
12 of a mixture of thiobacillus thiooxidans and thiobacillus ferooxidans microorganisms with an optimum
15 lements (IS elements) are similar to IST2 of Thiobacillus ferrooxidans and several related elements.
16 re of the Cu(I) form of the rusticyanin from Thiobacillus ferrooxidans has been calculated from a tot
17 highly oxidizing cupredoxin rusticyanin from Thiobacillus ferrooxidans has been determined by the met
19 d genome sequence of the biomining bacterium Thiobacillus ferrooxidans strain ATCC23270 was assembled
20 in rusticyanin (Rc) from the bacterium Acido-thiobacillus ferrooxidans, it was possible to demonstrat
26 nt populations, while significant amounts of Thiobacillus-related OTUs were detected in the lower lay
27 ophiles and lithotrophs, typically Truepera, Thiobacillus, Rubrobacter; significant increases in micr
30 Community analysis revealed the dominance of Thiobacillus spp., whose genomes harbour a previously un
32 as to investigate the effect of a mixture of thiobacillus thiooxidans and thiobacillus ferooxidans mi
34 in H2O approach the corresponding values in Thiobacillus versutus MADH (C==O stretch at 1612 cm-1, l