Assay Conditions Influence Affinities of Rat Organic Cation Transporter 1: Analysis of Mutagenesis in the Modeled Outward-Facing Cleft by Measuring Effects of Substrates and Inhibitors on Initial Uptake.

The effects of mutations in the modeled outward-open cleft of rat organic cation transporter 1 (rOCT1) on affinities of substrates and inhibitors were investigated. Human embryonic kidney 293 cells were stably transfected with rOCT1 or rOCT1 mutants, and uptake of the substrates 1-methyl-4-phenylpyridinium+ (MPP+) and tetraethylammonium+ (TEA+) or inhibition of MPP+ uptake by the nontransported inhibitors tetrabutylammonium+ (TBuA+), tetrapentylammonium+ (TPeA+), and corticosterone was measured. Uptake measurements were performed on confluent cell layers using a 2-minute incubation or in dissociated cells using incubation times of 1, 5, or 10 seconds. With both methods, different apparent Michaelis-Menten constant (Km) values, different IC50 values, and varying effects of mutations were determined. In addition, varying IC50 values for the inhibition of MPP+ uptake and varying effects of mutations were obtained when different MPP+ concentrations far below the apparent Km value were used for uptake measurements. Eleven mutations were investigated by measuring initial uptake in dissociated cells and employing 0.1 µM MPP+ for uptake during inhibition experiments. Altered affinities for substrates and/or inhibitors were observed when Phe160, Trp218, Arg440, Leu447, and Asp475 were mutated. The mutations resulted in changes of apparent Km values for TEA+ and/or MPP+ Mutation of Trp218 and Asp475 led to altered IC50 values for TBuA+, TPeA+, and corticosterone, whereas the mutation of Phe160 and Leu447 changed the IC50 values for two inhibitors. Thereby amino acids in the outward-facing conformation of rOCT1 could be identified that interact with structurally different inhibitors and probably also with different substrates.

Microbial reduction of Fe(III) in the presence of oxygen under low pH conditions.

In acidic, coal mining lake sediments, facultatively anaerobic Acidiphilium species are probably involved in the reduction of Fe(III). Previous results indicate that these bacteria can co-respire O2 and Fe(III). In this study, we investigated the capacity of the sediment microbiota to reduce Fe(III) in the presence of O2 at pH 3. In sediment microcosms with 4% O2 in the headspace, the concentration of Fe(II) increased at a rate of 1.03 micromol (g wet sediment)-1 day-1 within the first 7 days of incubation which was similar to the rate obtained with controls incubated under anoxic conditions. However, in microcosms incubated under air, Fe(II) was consumed after a lag phase of 8 h with a rate of 2.66 micromol (g wet sediment)-1 day-1. Acidiphilium cryptum JF-5, isolated from this sediment, reduced soluble Fe(III) with either 4 or 21% O2 in the headspace, and concomitantly consumed O2. However, the rate of Fe(II) formation normalized for cell density decreased under oxic conditions. Schwertmannite, the predominant Fe(III)-mineral of this sediment, was also reduced by A. cryptum JF-5 under oxic conditions. The rate of Fe(II) formation by A. cryptum JF-5 decreased after transfer from preincubation under air in medium lacking Fe(III). Acidiphilium cryptum JF-5 did not form Fe(II) when preincubated under air and transferred to anoxic medium containing Fe(III) and chloramphenicol, an inhibitor of protein synthesis. These results indicate that: (i) the reduction of Fe(III) can occur at low O2 concentrations in acidic sediments; (ii) Fe(II) can be oxidized at O2 concentrations near saturation; and (iii) the enzyme(s) responsible for the reduction of Fe(III) in A. cryptum JF-5 are not constitutive.