Iron uptake from ferrated (59Fe) pseudobactin (PSB), a Pseudomonas putida siderophore, by various plant species was studied in nutrient solution culture under short term (10 h) and long term (3 weeks) conditions. In the short term experiments, 59Fe uptake rate from 59FePSB by dicots (peanuts, cotton and sunflower) was relatively low when compared with 59Fe uptake rate from 59FeEDDHA. Iron uptake rate from 59FePSB was pH and concentration dependent, as was the Fe uptake rate from 59FeEDDHA. The rate was about 10 times lower than that of Fe uptake from the synthetic chelate. Results were similar for long term experiments.Monocots (sorghum) in short term experiments exhibited significantly higher uptake rate of Fe from FePSB than from FeEDDHA. In long term experiments, FePSB was less efficient than FeEDDHA as an Fe source for sorghum at pH 6, but the same levels of leaf chlorophyll concentration were obtained at pH 7.3.Fe uptake rates by dicots from the siderophore and FeEDDHA were found to correlate with Fe reduction rates and reduction potentials (E0) of both chelates. Therefore, it is suggested that the reduction mechanism governs the Fe uptake process from PSB by dicots. Further studies will be conducted to determine the role of pH in Fe aquisition from PSB by monocots.
The synthetically produced fluorescent siderophore NBD-desferrioxamine B (NBD-DFO), an analog of the natural siderophore ferrioxamine B, was used to study iron uptake by plants. 5"Fe uptake rates by cotton (Gossypium spp.) and maize (Zea mays L.) plants from the modified siderophore were similar to those of the natural one. In longer-term uptake experiments (3 weeks), both siderophore treatments resulted in similar leaf chlorophyll concentration and dry matter yield. These results suggest that the synthetic derivative acts similarly to the natural siderophore. The NBD-DFO is fluorescent only when unferrated and can thus be used as a probe to follow iron removal from the siderophore. Monitoring of the fluorescence increase in a nutrient solution containing Fe3"-NBD-DFO showed that iron uptake by plants occurs at the cell membrane. The rate of iron uptake was significantly lower in both plant species in the presence of antibiotic agent, thus providing evidence for iron uptake by rhizosphere microbes that otherwise could have been attributed to plant uptake. Confocal fluorescence microscopy revealed that iron was taken up from the complex by cotton plants, and to a much lesser extent by maize plants. The active cotton root sites were located at the main and lateral root tips. Significant variations in the location and the intensity of the uptake were noticed under nonaxenic conditions, which suggested that rhizosphere microorganisms play an important role in NBD-DFO-mediated iron uptake.binding capacity, has raised the question of whether these siderophores may be used by plants as an Fe source (14).A number of researchers investigated the possibility of plant utilization of various microbial siderophores including ferrichrome A (19), agrobactin (3), pseudobactin (1, 2, 12, 13), and ferrioxamine B (9, 10). A variety of plant species were shown to acquire Fe from ferrioxamine B, such as tomato (23), oat (9, 20, 21), sunflower and sorghum (8), and peanut and cotton (1).The mechanism by which plants utilize microbial siderophores has not yet been elaborated to a satisfying extent and it is a topic of controversy. Although some investigators proposed a specific Fe uptake mechanism (9, 11), others did not support this hypothesis (1, 5,22).In this study, Fe uptake from ferrioxamine B by maize (Zea mays L.) and cotton (Gossypium spp.) plants was investigated using the synthetic fluorescent ferrioxamine B analog NBD-DFO2 as a probe. NBD-DFO has been designed to be nonfluorescent when saturated with Fe3+, but to gain fluorescence upon Fe3+ release. NBD-DFO, therefore, allows one to monitor the location and the dynamics of cellular Fe uptake. This research focused on the uptake mechanism in maize and cotton (monocot and dicot, respectively) and on the possibility of microbial involvement in the Fe uptake process. MATERIALS AND METHODS Studies
The stability constants of the fluorescent siderophore pseudobactin St3 (PSB3) produced by Pseudomonas putida strain 3 with Fe3, Cu2+, Mn2+, Zn2+, and Fe2+ were determined using fluorescence spectroscopy and potentiometric titrations. Stability constants for PSB3, with Fe3+, Fe2+, Mn2+, and Zn2+ were determined based on titration to saturation of a PSB3 ligand solution with either of the metals, then back‐titrating the solution with an EDTA solution along with simultaneous measurements of fluorescence and visible spectra. A nonlinear curve fitting between the fluorescence intensity (Y) and the concentration (C) of the metal or EDTA was used for the determination of the concentrations of the free and complexed ligands. The overall stability constant (log KML) obtained for Fe3+ by this method was the same as that obtained by visible spectrosopy. The log KML. values obtained by fluorescence spectroscopy for Mn2+ and Zn2+ (17.5 and 19.4, respectively) were in good agreement with log KML values obtained by potentiometric titration (17.3 and 19.8, respectively). It was found that two chromatography bands obtained from PSB3 solutions isolated and purified from cultures grown under different conditions chelated Fe3+ with practically the same affinity. The log KML of PSB3 with Fe3+, Zn2+, Cu2+, Mn2+, and Fe2+ were calculated using the protonation constants determined by potentiometry (pKa1 = 11.28, pKa2 = 7.74, pKa3 = 5.35) and were found to be 29.6, 19.8, 22.3, 17.3, and 8.3, respectively.
Effects of rhizosphere microorganisms on Fe uptake by oat (Avena sativa) and maize (Zea mays) were studied in short-term (10 h) nutrient solution experiments. Fe was supplied either as microbial siderophores (pseudobactin [PSB] or ferrioxamine B
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