Amino acid transport by Sphingomonas sp. strain Ant 17 isolated from oil-contaminated Antarctic soil

Abstract

The Antarctic bacterial isolate Sphingomonas sp. strain Ant 17 utilized a wide range of L-isomer amino acids as the sole carbon and energy source for growth. The pH and temperature optima for growth on amino acids were pH 7.0 and 15°C, respectively. Growth on serine and tryptophan was inhibited by uncouplers and inhibitors of oxidative phosphorylation, but not by monensin, a Na⁺/H⁺ antiporter, suggesting that sodium gradients were not specifically required for growth on these amino acids. Serine transport was via a high-affinity (apparent K _m of 8 μM) permease specific for both the L- and D-isomer. Tryptophan transport exhibited biphasic kinetics with both high-affinity (apparent K _m of 2.5 μM) and low-affinity (non-saturable) uptake systems detected. The high-affinity system was specific for L-tryptophan, L-tyrosine, and L-phenylalanine whereas the low-affinity permease was specific for L-tryptophan and L-phenylalanine, but not L-tyrosine. Neither orthovanadate nor sodium arsenate, inhibitors of ATP-dependent permeases, had any significant inhibitory effect on the rate of serine and tryptophan transport. The protonophore carbonyl cyanide m-chlorophenylhydrazone completely abolished serine and tryptophan transport; maximum rates of solute uptake were observed at acidic pH values (pH 4.0–5.0) for both amino acids. These results suggest that an electrochemical potential of protons is the driving force for serine and tryptophan transport by Ant 17. These high-affinity proton-driven permeases function over environmental extremes (e.g. broad temperature and pH range) that are likely to prevail in the natural habitat of this bacterium.