Consumption of tropospheric levels of methyl bromide by C1 compound-utilizing bacteria and comparison to saturation kinetics

Pure cultures of methylotrophs and methanotrophs are known to oxidize methyl bromide (MeBr); however, their ability to oxidize tropospheric concentrations (parts per trillion by volume [pptv]) has not been tested. Methylotrophs and methanotrophs were able to consume MeBr provided at levels that mimicked the tropospheric mixing ratio of MeBr (12 pptv) at equilibrium with surface waters (≈2 pM). Kinetic investigations using picomolar concentrations of MeBr in a continuously stirred tank reactor (CSTR) were performed using strain IMB-1 andLeisingeria methylohalidivorans strain MB2^T— terrestrial and marine methylotrophs capable of halorespiration. First-order uptake of MeBr with no indication of threshold was observed for both strains. Strain MB2^T displayed saturation kinetics in batch experiments using micromolar MeBr concentrations, with an apparent K _s of 2.4 μM MeBr and aV _max of 1.6 nmol h⁻¹(10⁶ cells)⁻¹. Apparent first-order degradation rate constants measured with the CSTR were consistent with kinetic parameters determined in batch experiments, which used 35- to 1 × 10⁷-fold-higher MeBr concentrations. Ruegeria algicola (a phylogenetic relative of strain MB2^T), the common heterotrophs Escherichia coli andBacillus pumilus, and a toluene oxidizer,Pseudomonas mendocina KR1, were also tested. These bacteria showed no significant consumption of 12 pptv MeBr; thus, the ability to consume ambient mixing ratios of MeBr was limited to C₁ compound-oxidizing bacteria in this study. Aerobic C₁ bacteria may provide model organisms for the biological oxidation of tropospheric MeBr in soils and waters.