Evaluation of Reductive Release as a Mechanism for Iron Uptake from Ferrioxamine B by Chlorella vulgaris

The involvement of ferric reduction in the iron uptake mechanism of iron-stressed Chlorella vulgaris from ferrioxamine B was investigated. Some comparative data for ferric-citrate was also obtained. EPR and a spectrophotometric assay were used to measure Fe³⁺ reduction. These two methods differed in the absolute quantity but not in effectors of ferric reduction. The mechanism governing ferric reduction was investigated by use of respiratory inhibitors, uncouplers, alternative electron acceptors, and ATPase inhibitors. Reduction appears to play a role in iron uptake from both Fe³⁺-deferrioxamine B and Fe³⁺-citrate; however, the involvement of photoreduction in Fe³⁺-citrate uptake implies multiple reductive mechanisms could be involved.     

Characterization of siderophore-mediated iron transport inGeotrichum candidum,a non-siderophore producer

Summary Geotrichum candidum is capable of utilizing iron from hydroxamate siderophores of different structural classes. The relative rates of iron transport for ferrichrome, ferrichrysin, ferrioxamine B, fusigen, ferrichrome A, rhodotorulic acid, coprogen B, dimerium acid and ferrirhodin were 100%, 98%, 74%, 59%, 49%, 35%, 24%, 12% and 11% respectively. Ferrichrome, ferrichrysine and ferrichrome A inhibited [⁵⁹Fe]ferrioxamine-B-mediated iron transport by 71%, 68% and 28% respectively when added at equimolar concentrations to the radioactive complex. The inhibitory mechanism of [⁵⁹Fe]ferrioxamine B uptake by ferrichrome was non-competitive (K _i 2.4 M), suggesting that the two siderophores do not share a common transport system. Uptake of [⁵⁹Fe]ferrichrome, [⁵⁹Fe]rhodotorulic acid and [⁵⁹Fe]fusigen was unaffected by competition with the other two siderophores or with ferrioxamine B. Thus,G. candidum may possess independent transport systems for siderophores of different structural classes. The uptake rates of [¹⁴C]ferrioxamine B and⁶⁷Ga-desferrioxamine B were 30% and 60% respectively, as compared to [⁵⁹Fe]ferrioxamine B. The specific ferrous chelates, dipyridyl and ferrozine at 6 mM, caused 65% and 35% inhibition of [⁵⁹Fe]ferrioxamine uptake. From these results we conclude that, although about 70% of the iron is apparently removed from the complex by reduction prior to being transported across the cellular membrane, a significant portion of the chelated ligand may enter the cell intact. The former and latter mechanisms seem not to be mutually exclusive.     

The Bradyrhizobium japonicum fsrB gene is essential for utilization of structurally diverse ferric siderophores to fulfill its nutritional iron requirement

In Bradyrhizobium japonicum, iron uptake from ferric siderophores involves selective outer membrane proteins and non-selective periplasmic and cytoplasmic membrane components that accommodate numerous structurally diverse siderophores. Free iron traverses the cytoplasmic membrane through the ferrous (Fe²⁺) transporter system FeoAB, but the other non-selective components have not been described. Here, we identify fsrB as an iron-regulated gene required for growth on iron chelates of catecholate- and hydroxymate-type siderophores, but not on inorganic iron. Utilization of the non-physiological iron chelator EDDHA as an iron source was also dependent on fsrB. Uptake activities of ⁵⁵Fe³⁺ bound to ferrioxamine B, ferrichrome or enterobactin were severely diminished in the fsrB mutant compared with the wild type. Growth of the fsrB or feoB strains on ferrichrome were rescued with plasmid-borne E. coli fhuCDB ferrichrome transport genes, suggesting that FsrB activity occurs in the periplasm rather than the cytoplasm. Whole cells of an fsrB mutant are defective in ferric reductase activity. Both whole cells and spheroplasts catalyzed the demetallation of ferric siderophores that were defective in an fsrB mutant. Collectively, the data support a model whereby FsrB is required for reduction of iron and its dissociation from the siderophore in the periplasm, followed by transport of the ferrous ion into the cytoplasm by FeoAB.     

Identification of siderophores and siderophore-mediated uptake of iron in Stemphylium botryosum

Under iron-deficient conditions Stemphylium botryosum f. sp. lycopersici produces three major siderophores; dimerum acid, coprogen B and an unidentified monohydroxamate siderophore designated as A. The system of siderophores mediating uptake of iron was characterized. It exhibits active transport, saturation kinetics and an optimum at pH 6 and 30°. The rate of iron uptake via dimerum acid and coprogen B was four times higher than siderophore A. S. botryosum was capable of taking up iron from hydroxamate siderophores produced by other fungi, e.g. ferrichrome, fusigen, rhodotorulic acid but not ferrioxamine B. Double labelling experiments suggest that ferric coprogen B accumulates in mycelial cells as an intact chelate.     

Iron acquisition by plants: the reduction of ferrisiderophores by higher plant NADH: Nitrate reductase

Siderophores are avid Fe³⁺-chelators of microbial origin. Plant roots are colonized by fungi and bacteria which synthesize siderophores, and plants have been shown to metabolize these substances to obtain iron. We have previously shown that nitrate reductase from squash catalyzed the reduction of the ferrisiderophore ferrioxamine B with the subsequent loss of Fe²⁺. Using a spectrophotometric assay which traps Fe²⁺ in a ferrozine complex, we have noted that the substrate diversity of nitrate reductase as a ferrisiderophore reductase includes ferrichrome A, ferrichrome, ferrirhodotorulic acid, ferrischizokinen, and the novel siderophore ferri-‘AAHS’. These reductions were inhibited by polyclonal antibodies against nitrate reductase, but ferrisiderophore reductase activity, as evidenced with ferrirhodotorulic acid, was unaffected by low concentrations of azide. In addition, maximal activity occurred between pH 4 and 5, and appaarent K_m values were approx. 100 μmolar. Thus, we suggest that plant nitrate reductases might be involved in iron assimilation as well as nitrate reduction.     

Evidence for a specific uptake system for iron phytosiderophores in roots of grasses

Roots of grasses in response to iron deficiency markedly increase the release of chelating substances (`phytosiderophores') which are highly effective in solubilization of sparingly soluble inorganic Fe<sup>III</sup> compounds by formation of Fe<sup>III</sup>phytosiderophores. In barley (Hordeum vulgare L.), the rate of iron uptake from Fe<sup>III</sup>phytosiderophores is 100 to 1000 times faster than the rate from synthetic Fe chelates (e.g. Fe ethylenediaminetetraacetate) or microbial Fe siderophores (e.g. ferrichrome). Reduction of Fe<sup>III</sup> is not involved in the preferential iron uptake from Fe<sup>III</sup>phytosiderophores by barley. This is indicated by experiments with varied pH, addition of bicarbonate or of a strong chelator for Fe<sup>II</sup> (e.g. batho-phenanthrolinedisulfonate). The results indicate the existence of a specific uptake system for Fe<sup>III</sup>phytosiderophores in roots of barley and all other graminaceous species. In contrast to grasses, cucumber plants (Cucumis sativus L.) take up iron from Fe<sup>III</sup>phytosiderophores at rates similar to those from synthetic Fe chelates. Furthermore, under Fe deficiency in cucumber, increased rates of uptake of Fe<sup>III</sup>phytosiderophores are based on the same mechanism as for synthetic Fe chelates, namely enhanced Fe<sup>III</sup> reduction and chelate splitting. Two strategies are evident from the experiments for the acquisition of iron by plants under iron deficiency. Strategy I (in most nongraminaceous species) is characterized by an inducible plasma membrane-bound reductase and enhancement of H<sup>+</sup> release. Strategy II (in grasses) is characterized by enhanced release of phytosiderophores and by a highly specific uptake system for Fe<sup>III</sup>phytosiderophores. Strategy II seems to have several ecological advantages over Strategy I such as solubilization of sparingly soluble inorganic Fe<sup>III</sup> compounds in the rhizosphere, and less inhibition by high pH. The principal differences in the two strategies have to be taken into account in screening methods for resistance to `lime chlorosis'.     

Hydroxamate Production as a High Affinity Iron Acquisition Mechanism in Paracoccidioides Spp

Iron is a micronutrient required by almost all living organisms, including fungi. Although this metal is abundant, its bioavailability is low either in aerobic environments or within mammalian hosts. As a consequence, pathogenic microorganisms evolved high affinity iron acquisition mechanisms which include the production and uptake of siderophores. Here we investigated the utilization of these molecules by species of the Paracoccidioides genus, the causative agents of a systemic mycosis. It was demonstrated that iron starvation induces the expression of Paracoccidioides ortholog genes for siderophore biosynthesis and transport. Reversed-phase HPLC analysis revealed that the fungus produces and secretes coprogen B, which generates dimerumic acid as a breakdown product. Ferricrocin and ferrichrome C were detected in Paracoccidioides as the intracellular produced siderophores. Moreover, the fungus is also able to grow in presence of siderophores as the only iron sources, demonstrating that beyond producing, Paracoccidioides is also able to utilize siderophores for growth, including the xenosiderophore ferrioxamine. Exposure to exogenous ferrioxamine and dimerumic acid increased fungus survival during co-cultivation with macrophages indicating that these molecules play a role during host-pathogen interaction. Furthermore, cross-feeding experiments revealed that Paracoccidioides siderophores promotes growth of Aspergillus nidulans strain unable to produce these iron chelators. Together, these data denote that synthesis and utilization of siderophores is a mechanism used by Paracoccidioides to surpass iron limitation. As iron paucity is found within the host, siderophore production may be related to fungus pathogenicity.     

Role of Nitrosomonas europaea NitABC iron transporter in the uptake of Fe3+-siderophore complexes

Nitrosomonas europaea has a single three-gene operon (nitABC) encoding an iron ABC transporter system (NitABC). Phylogenetic analysis clustered the subunit NitB with Fe³⁺-ABC transporter permease components from other organisms. The N. europaea strain deficient in nitB (nitB::kan) grew well in either Fe-replete or Fe-limited media and in Fe-limited medium containing the catecholate-type siderophore, enterobactin or the citrate-based dihydroxamate-type siderophore, aerobactin. However, the nitB::kan mutant strain was unable to grow in Fe-limited media containing either the hydroxamate-type siderophores, ferrioxamine and ferrichrome or the mixed-chelating type siderophore, pyoverdine. Exposure of N. europaea cells to a ferrichrome analog coupled to the fluorescent moiety naphthalic diimide (Fhu-NI) led to increase in fluorescence in the wild type but not in nitB::kan mutant cells. Spheroplasts prepared from N. europaea wild type exposed to Fhu-NI analog retained the fluorescence, while spheroplasts of the nitB::kan mutant were not fluorescent. NitABC transports intact Fe³⁺-ferrichrome complex into the cytoplasm and is an atypical ABC type iron transporter for Fe³⁺ bound to ferrioxamine, ferrichrome or pyoverdine siderophores into the cytoplasm. The mechanisms to transport iron in either the Fe³⁺ or Fe²⁺ forms or Fe³⁺ associated with enterobactin or aerobactin siderophores into the cell across the cytoplasmic membrane are as yet undetermined.     

BIOLOGICAL AVAILABILITY OF IRON TO THE FRESHWATER CYANOBACTERIUM ANABAENA FLOS‐AQUAE1

Iron acquisition from various ferric chelates and colloids was studied using iron‐limited cells of Anabaena flos‐aquae (Lyng.) Brèb UTEX 1444, a cyanobacterial strain that produces high levels of siderophores under iron limitation. Various chelators of greatly varying affinity for Fe³⁺ (HEDTA, EDDHA, desferrioxamine mesylate, HBED, 8‐hydroxyquinoline) were assayed for the degree of iron acquisition by iron‐limited cyanobacterial cells. Iron uptake rates (measured by graphite furnace atomic absorption spectrometry) varied approximately inversely with calculated [Fe³⁺] (calculated as pFe) and decreased with increasing chelator‐to‐iron ratio. No iron uptake was observed when Fe³⁺ was chelated with HBED, the strongest of the tested chelators. Iron‐limited Anabaena cells were able to take up iron from 8‐hydroxyquinoline (oxine or 8HQ), a compound sometimes used to quantify aquatic iron bioavailability. Iron bound to purified humic acid was poorly available but did support some growth at high humic acid concentrations. These results suggest that for cyanobacteria, even tightly bound iron is biologically available, including to a limited extent iron bound to humic acids. However, iron bound to some extremely strong chelators (e.g. HBED) is likely to be biologically unavailable.     

Rapid evolution of a bacterial iron acquisition system

Under iron limitation, bacteria scavenge ferric (Fe³⁺) iron bound to siderophores or other chelates from the environment to fulfill their nutritional requirement. In gram‐negative bacteria, the siderophore uptake system prototype consists of an outer membrane transporter, a periplasmic binding protein and a cytoplasmic membrane transporter, each specific for a single ferric siderophore or siderophore family. Here, we show that spontaneous single gain‐of‐function missense mutations in outer membrane transporter genes of Bradyrhizobium japonicum were sufficient to confer on cells the ability to use synthetic or natural iron siderophores, suggesting that selectivity is limited primarily to the outer membrane and can be readily modified. Moreover, growth on natural or synthetic chelators required the cytoplasmic membrane ferrous (Fe²⁺) iron transporter FeoB, suggesting that iron is both dissociated from the chelate and reduced to the ferrous form within the periplasm prior to cytoplasmic entry. The data suggest rapid adaptation to environmental iron by facile mutation of selective outer membrane transporter genes and by non‐selective uptake components that do not require mutation to accommodate new iron sources.     

Utilization of microbial siderophores in iron acquisition by oat

Iron uptake by oat (Avena sativa cv Victory) was examined under hydroponic chemical conditions that required direct utilization of microbial siderophores for iron transport. Measurements of iron uptake rates by excised roots from the hydroxamate siderophores, ferrichrome, ferrichrome A, coprogen, ferrioxamine B (FOB), and rhodotorulic acid (RA) showed all five of the siderophores supplied iron, but that FOB and RA were preferentially utilized. FOB-mediated iron uptake increased four-fold when roots were preconditioned to iron stress and involved an active, iron-stress induced transport system that was inhibited by 5 millimolar sodium azide or 0.5 millimolar dinitrophenol. Kinetic studies indicated partial saturation with an apparent K_m of 5 micromolar when FOB was supplied at 0.1 to 50 micromolar concentrations. Whole plant experiments confirmed that 5 micromolar FOB was sufficient for plant growth. Siderophore-mediated iron transport was inhibited by Cr-ferrichrome, an analog of ferrated siderophore. Our results confirm the existence of a microbial siderophore iron transport system in oat which functions within the physiological concentrations produced and used by soil microorganisms.     

Fe nutrition demand and utilization by the green alga Dunaliella bardawil

The Fe nutritional demands, requirements and mechanisms of uptake by Dunaliella bardawil as well as potential Fe sources were studied. A comparison between Fe uptake from bacterial siderophores and from synthetic ferric chelates revealed algal growth response and chlorophyll synthesis to increasing concentrations and availability at a range of 0.01 μM–5 μM, as well as differences in efficiency. Furthermore, chloroplast ultrastructure, as observed by TEM, was affected by Fe deficiency, as was chlorophyll content. Ferric reduction is involved in the Fe uptake mechanism of Fe-stressed D. bardawil. Nutrient solution with controlled levels of free Fe²⁺ as well as spectrophotometric assays were used to measure Fe³⁺ reduction. This study shows that D. bardawil utilizes Fe³⁺ via a reduction mechanism, similar to that of strategy-I higher plants. This revised version was published online in June 2006 with corrections to the Cover Date.     

Iron transport in Streptomyces pilosus mediated by ferrichrome siderophores, rhodotorulic acid, and enantio-rhodotorulic acid

Streptomyces pilosus is one of several microbes which produce ferrioxamine siderophores. In the accompanying paper (G. Müller and K. Raymond, J. Bacteriol. 160:304-312), the mechanism of iron uptake mediated by the endogenous ferrioxamines B, D1, D2, and E was examined. Here we report iron transport behavior in S. pilosus as mediated by the exogenous siderophores ferrichrome, ferrichrysin, rhodotorulic acid (RA), and synthetic enantio-RA. In each case iron acquisition depended on metabolic energy and had uptake rates comparable to that of [55Fe]ferrioxamine B. However, the synthetic ferric enantio-RA (which has the same preferred chirality at the metal center as ferrichrome) was twice as effective in supplying iron as was the natural ferric RA complex, suggesting that stereospecific recognition at the metal center is involved in the transport process. Iron uptake mediated by ferrichrome and ferric enantio-RA was strongly inhibited by kinetically inert chromic complexes of desferrioxamine B. These inhibition experiments indicate that iron from these exogenous siderophores is transported by the same uptake system as ferrioxamine B. Since the ligands have no structural similarity to ferrioxamine B except for the presence of three hydoxamate groups, we conclude that only the hydroxamate iron center and its direct surroundings are important for recognition and uptake. This hypothesis is supported by the fact that ferrichrome A and ferrirubin, which are both substituted at the hydroxamate carbonyl groups, were not (or were poorly) effective in supplying iron to S. pilosus.     

Iron uptake by plants from microbial siderophores : a study with 7-nitrobenz-2 oxa-1,3-diazole-desferrioxamine as fluorescent ferrioxamine B analog

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. Short-term (10-hour) ⁵⁵Fe 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.     

Iron uptake from ferric citrate by Vibrio anguillarum

We report here that Vibrio anguillarum possesses a non-inducible active transport system which can efficiently supply iron to the cell from ferric citrate, independently of the siderophore-based mechanisms. The strains tested were able to grow in CM9 medium in iron-restricted conditions when ferric citrate was present in the medium. Moreover, the presence of ferric citrate inhibited the production of siderophores in the strains tested. V. anguillarum cells and isolated membranes could incorporate ⁵⁵Fe³⁺ complexed by citrate, without a difference between cells grown in the presence or absence of ferric citrate. The presence of 2,4-dinitrophenol, ferrozine, ferricyanide, trypsin, as well as low temperature produced a marked decrease or total inhibition of ⁵⁵Fe³⁺ uptake by the cells. All these results suggest that iron uptake from ferric citrate in V. anguillarum must be an energy-dependent process not induced by the presence of iron or citrate in the medium, mediated by a membrane protein(s), which may require an iron reduction step to function.     

The DNA gyrase inhibitors,nalidixic acid and oxolinic acid,prevent iron-mediated repression of catechol siderophore synthesis inAzotobacter vinelandii

Summary Low concentrations of nalidixic acid and oxolinic acid that were just inhibitory toAzotobacter vinelandii growth promoted the production of the catechol siderophores azotochelin and aminochelin, in the presence of normally repressive concentrations of Fe³⁺. There was a limited effect on the pyoverdin siderophore, azotobactin, where low concentrations of Fe³⁺ were rendered less repressive, but the repression by higher concentrations of Fe³⁺ was normal. These drugs did not induce high-molecular-mass iron-repressible outer-membrane proteins and similar effects on the regulation of catechol siderophore synthesis were not produced by novobiocin, coumermycin, or ethidium bromide. The timing of nalidixic acid and Fe³⁺ addition to iron-limited cells was critical. Nalidixic acid had to be added before iron-repression of catechol siderophore synthesis and before the onset of iron-sufficient growth. Continued production of the catechol siderophores, however, was not due to interference with normal iron uptake. These data indicated that nalidixic acid prevented normal iron-repression of catechol siderophore synthesis but could not reverse iron repression once it had ocurred. The possible roles of DNA gyrase activity in the regulation of catechol siderophore synthesis is discussed.     

Differential Siderophore Utilization and Iron Uptake by Soil and Rhizosphere Bacteria

The differential availabilities of the hydroxamate siderophores ferrioxamine B (FOB) and ferrichrome (FC) and the pseudobactin siderophores St3, 7NSK₂, and WCS 358 as sources of Fe for soil and rhizosphere bacteria were studied. About 20% of the total bacterial CFU from the rhizospheres of four plant species were able to use FOB as the sole Fe source in an Fe-deficient medium, while about 12, 10, 2, and > 1% were able to use FC and pseudobactins 7NSK₂, St3, and WCS 358, respectively. Of the 165 colonies isolated from plates containing pseudobactins, 64 were able to use the pseudobactin on which they were isolated as the sole Fe source in pure culture. Cross-feeding tests showed that almost all of these 64 strains were also able to use at least one of the other siderophores studied (pseudobactin, FOB, or FC). Pseudomonas putida StS2, Pseudomonas maltophilia 7NM1, and Vibrio fluvialis WS1, which were originally isolated on pseudobactins St3, 7NSK₂, and WCS 358, respectively, were selected for their ability to grow with pseudobactin St3 as the sole Fe source. They incorporated ⁵⁵Fe³⁺ mediated by pseudobactin St3 at various rates (71.5, 4, and 23 pmol/min/mg [dry weight] of cells, respectively). Similarly, P. putida St3 was shown to incorporate ⁵⁵Fe³⁺ mediated by FOB and FC. We suggest that the ability of bacteria to utilize a large variety of siderophores confers an ecological advantage.     

The Fe2+ Chelator Proferrorosamine A Is Essential for the Siderophore-Mediated Uptake of Iron by Pseudomonas roseus fluorescens

Pseudomonas roseus fluorescens produces, besides the Fe²⁺ chelator proferrorosamine A, Fe³⁺ -chelating compounds, called siderophores. The production of proferrorosamine A and siderophores by P. roseus fluorescens appears to be controlled in a similar way by the concentration of available iron and by the concentration of dissolved oxygen. The higher the concentration of iron available for the microorganism, the lower the production of both chelating compounds. However, the production of siderophores was much more sensitive to iron availability than was proferrorosamine A production. Proferrorosamine A and siderophores were only produced in minimal medium C if the concentration of dissolved oxygen ranged from 4.5 to 2.0 ppm. At higher or lower concentrations, none of the iron-chelating compounds were produced. Furthermore, it has been shown that proferrorosamine-negative Tn5 mutants of P. roseus fluorescens were able to form siderophores only under iron-limiting conditions when proferrorosamine A was added to the medium. Our data suggest that proferrorosamine A production is essential for siderophore synthesis by P. roseus fluorescens; the production of siderophores occurred only when proferrorosamine A was present.     

Iron Uptake in Ustilago maydis: Tracking the Iron Path

In this study, we monitored and compared the uptake of iron in the fungus Ustilago maydis by using biomimetic siderophore analogs of ferrichrome, the fungal native siderophore, and ferrioxamine B (FOB), a xenosiderophore. Ferrichrome-iron was taken up at a higher rate than FOB-iron. Unlike ferrichrome-mediated uptake, FOB-mediated iron transport involved an extracellular reduction mechanism. By using fluorescently labeled siderophore analogs, we monitored the time course, as well as the localization, of iron uptake processes within the fungal cells. A fluorescently labeled ferrichrome analog, B9-lissamine rhodamine B, which does not exhibit fluorescence quenching upon iron binding, was used to monitor the entry of the compounds into the fungal cells. The fluorescence was found intracellularly 4 h after the application and later was found concentrated in two to three vesicles within each cell. The fluorescence of the fluorescently labeled FOB analog CAT18, which is quenched by iron, was visualized around the cell membrane after 4 h of incubation with the ferrated (nonfluorescent) compounds. This fluorescence intensity increased with time, demonstrating fungal iron uptake from the siderophores, which remained extracellular. We here introduce the use of fluorescent biomimetic siderophores as tools to directly track and discriminate between different pathways of iron uptake in cells.