Influence of Manganese on Growth of a Sheathless Strain of Leptothrix discophora

Mn²⁺ exerted various effects on the growth of Leptothrix discophora strain SS-1 in batch cultures depending on the concentration added to the medium. Concentrations of 0.55 to 5.5 μM Mn²⁺, comparable to those in the environment from which strain SS-1 was isolated, decreased cell yield and prolonged stationary-phase survival, but did not affect growth rate. Elevated concentrations of 55 to 910 μM Mn²⁺ also decreased cell yield and prolonged survival, but growth rate was decreased as well. The addition of 1,820 μM Mn²⁺ caused a decline in cell numbers followed by an exponential rise after 80 h of incubation, indicating the development of a population of cells resistant to Mn²⁺ toxicity. When 360 μM Mn²⁺ or less was added to growth flasks, Mn²⁺ was oxidized to manganese oxide (MnO_x, where x is ~2), which appeared as brown particles in the medium. Quantification of Mn oxidation during growth of cultures to which 55 μM Mn²⁺ was added showed that nearly all of the Mn²⁺ was oxidized by the beginning of the stationary phase of growth (15 to 25 h). This result suggested that the decrease in cell yield observed at low and moderate concentrations of Mn²⁺ was related to the formation of MnO_x, which may have bound cationic nutrients essential to the growth of SS-1. The addition of excess Fe³⁺ to cultures containing 55 μM Mn²⁺ increased cell yield to levels near those found in cultures with no added Mn²⁺, indicating that iron deprivation by MnO_x was at least partly responsible for the decreased cell yield.     

Physiology and ultrastructure of Leptothrix discophora SS-1

Leptothrix discophora strain SS-1 (ATCC 43182) is a Gram-negative, Mn²⁺-oxidizing, aerobic heterotroph which lost its sheath-forming ability after 18 months of cultivation on laboratory media. SS-1 possesses high 6-phosphogluconate dehydratase and KDPG aldolase activities, and a very low level of phosphofructokinase, indicating carbohydrate catabolism by the Entner-Doudoroff pathway. The strain is polarly flagellated, accumulates PHB up to 67% of its dry weight when grown in pyruvate-containing medium, and has a G+C content of 69.8 mol%. These properties indicate that L. discophora is essentially a pseudomonad which can form a sheath and oxidize Mn²⁺. Ultrastructural observations made before SS-1 lost its sheath-forming ability indicated two cell types. Short, flagellated, non-sheathed cells seen under the electron microscope probably corresponded to swarmer cells observed under phase-contrast microscopy. These cells contained plate organelles and PHB granules, and produced extracellular blebs approx. 25–50 nm in diameter. Larger sheathed cells also contained plate organelles, PHB granules, and blebs that were often sandwiched between the outer membrane and the sheath. Cells grown in the presence of added Mn²⁺ were surrounded by an extensive fibrillar matrix, rendered electron dense by precipitation of manganic oxide. The matrix was connected to various points of the cell by outer membrane evaginations or electron dense threads. We propose that the outer membrane blebs represent vehicles for excretion of unorganized sheath material and/or Mn²⁺-oxidizing protein produced by L. discophora.Parts of this work were presented previously (W.C. Ghiorse, Abst. Annu. Meet. Am. Soc. Microbiol., 1981, N 64, p 183)     

Manganese oxidation by microbial consortia from sand filters

The role of microbial consortia on the removal of manganese (Mn) was examined on sand from three different Belgian rapid sand filters for the treatment of ground water. Microorganisms closely associated with deposits of Fe and amorphous Mn precipitates were observed by SEM and EDAX techniques on sand from the filters able to remove Mn efficiently. Bacterial counts were performed. Of the CFU enumerated on PYM-medium, 25–33% displayed Mn-oxidizing activity.Batch cultures were set up by inoculating a Mn-containing, low organic medium with sand from one of the filters. Microbial growth resulted in the formation of Mn-removing bacterial flocs and a pH increase. Suppression of microbial growth by addition of azide, kanamycin, or by autoclaving reduced removal of Mn²⁺ from 0.5 mM/day to 0.05–0.11 mM/day. Buffering the pH of the medium at 7.5 (0.1 mM Hepes) decelerated the Mn removal but did not halt it, whereas microelectrode measurements revealed a clear pH drop of about 0.7 units inside bacterial flocs. In the absence of Mn²⁺, the pH drop was only 0.4 units. The auto-catalytic removal of Mn by the Mn oxide coated filter sand was not sufficient to explain the Mn removal observed. Inactivated cells were not capable of a pronounced autocatalytic Mn removal. Experiments with enrichment cultures indicated that the Mn-removing capacity of the microbial sand filter consortia was not constitutive but was promoted by preadaptation and the presence of a substratum. These results clearly link Mn oxidation in rapid sand filters to microbial processes. Offprint requests to: W. Verstraete.     

Formation of Metallogenium-like structures by a manganese-oxiding fungus

Structures resembling Metallogenium spp. were observed in agar and in liquid cultures of a Mn-oxidizing basidiomycetous fungus only when Mn²⁺ was oxidized. Fungal viability was necessary for formation of the structures; Mn²⁺ concentration and the presence or absence of agar in the medium were important factors determining their morphology. Slide cultures revealed no identifiable cells in any stage of development. Fluorescent dyes that stained nucleic acids and polysaccharides in the fungal hyphae did not stain the Metallogenium-like structures. Likewise, Rhodamine 123, a fluorescent probe for membrane potential, stained fungal mitochondria, but did not stain the structures. Thin sections through the structures showed no biological membranes or other cellular features. Only the characteristic ultrastructure of biological Mn oxides were observed in serial thin sections. In agar, unfixed structures disappeared permanently during reduction of Mn oxides with hydroxylamine. Glutaraldehyde fixation stabilized these structures. Fixed structures lost most of their original phase density during reduction with hydroxylamine, but continuous microscopic observations showed that their phase density could be restored by staining with Coomassie blue. Structures that formed in liquid medium did not require stabilization with glutaraldehyde during reduction of Mn oxides. They, too, lost their original phase density during reduction with hydroxylamine; phase density could be restored by staining with cationic colloidal iron or Coomassie blue. The results suggest that the Metallogenium-like structures were formed as a result of Mn oxidation associated with exopolymers produced by the fungus.Non-standard abbreviations HEPES (N-hydroxyethylpiperazine-N-2-ethane sulfonic acid) - DAPI (4,6-diamidino-2-phenylindole) - PIPES (piperazine-N,N-bis[2-ethane sulfonic acid])     

Production of Biogenic Mn Oxides by Leptothrix discophora SS-1 in a Chemically Defined Growth Medium and Evaluation of Their Pb Adsorption Characteristics

Biogenic Mn oxides were produced by the bacterium Leptothrix discophora SS-1 (= ATCC 3182) in a chemically defined mineral salts medium, and the Pb binding and specific surface area of these oxides were characterized. Growth of SS-1 in the defined medium with pyruvate as a carbon and energy source required the addition of vitamin B₁₂. Complete oxidation of Mn(II) within 60 h required the addition of ≥0.1 μM FeSO₄. Pb adsorption isotherms were determined for the biogenic Mn oxides (and associated cells with their extracellular polymer) and compared to the Pb adsorption isotherms of cells and exopolymer alone, as well as to abiotic Mn oxides. The Pb adsorption to cells and exopolymer with biogenic Mn oxides (0.8 mmol of Mn per g) at pH 6.0 and 25°C was 2 orders of magnitude greater than the Pb adsorption to cells and exopolymer alone (on a dry weight basis). The Pb adsorption to the biogenic Mn oxide was two to five times greater than the Pb adsorption to a chemically precipitated abiotic Mn oxide and several orders of magnitude greater than the Pb adsorption to two commercially available crystalline MnO₂ minerals. The N₂ Brunauer-Emmet-Teller specific surface areas of the biogenic Mn oxide and fresh Mn oxide precipitate (224 and 58 m²/g, respectively) were significantly greater than those of the commercial Mn oxide minerals (0.048 and 4.7 m²/g). The Pb adsorption capacity of the biogenic Mn oxide also exceeded that of a chemically precipitated colloidal hydrous Fe oxide under similar solution conditions. These results show that amorphous biogenic Mn oxides similar to those produced by SS-1 may play a significant role in the control of trace metal phase distribution in aquatic systems.     

Biogenic Manganese Oxides Facilitate Iodide Oxidation at pH ≤ 5

Radioactive ¹²⁹I, a byproduct of nuclear power generation, can pose risks to human health if released into the environment, where its mobility is highly dependent on speciation. Based on thermodynamic principles, ¹²⁹I should exist primarily as iodide (I^?) in most terrestrial environments; however, organo-¹²⁹I and ¹²⁹iodate are also commonly detected in contaminated soils and groundwater. To investigate the capability of biogenic manganese oxides to influence iodide speciation, 17 manganese-oxidizing bacterial strains, representing six genera, were isolated from soils of the Savannah River Site, South Carolina. The isolates produced between 2.6 and 67.1 nmole Mn oxides (ml^?1 media after 25 days, pH 6.5). Results from inhibitor assays targeting extracellular enzymes and reactive oxygen species indicated that both play a role in microbe-induced Mn(II) oxidation among the strains examined. Iodide oxidation was not observed in cultures of the most active Mn-oxidizing bacteria, Chryseobacterium sp. strain SRS1 and Chromobacterium sp. strain SRS8, or the fungus, Acremonium strictum strain KR21–2. While substantial amounts of Mn(III/IV) oxides were only generated in cultures at ≥pH 6, iodide oxidation was only observed in the presence of Mn(III/IV) oxides when the pH was ≤5. Iodide oxidation was promoted to a greater extent by synthetic Mn(IV)O₂ than biogenic Mn(III/IV) oxides under these low pH conditions (≤pH 5). These results indicate that the influence of biogenic manganese oxides on iodide oxidation and immobilization is primarily limited to low pH environments.     

Fungal manganese oxidation in a reduced soil

Manganese chemistry in soils is a function of complex, competing biotic and abiotic reactions. The role of soil-borne fungi in mediating these reactions is poorly understood. The objective of this article is to document direct observation of fungal Mn oxidation in soil under near in situ conditions, and to isolate, describe and confirm the role of fungi in the observed Mn oxidation, and present a model to explain our observations. We incubated soil under different moisture contents in sample cells designed to allow us to use synchrotron microspectroscopic techniques to analyse areas as small as 38x40 microm2. Mn was redistributed and accumulated in distinct small circular shapes or in dendritic patterns near the air-soil interface when water-saturated soil was incubated for >or=7 days. Mn oxidation did not occur at 3 or 52 degrees C indicating that oxidation was caused by microbial activity. Mn-oxidizing fungi were isolated from the sample cells and cultured on agar. Reinoculation of sterile soil with the Mn-oxidizing isolates resulted in the formation of Mn oxides around fungal hyphae. A model to describe the distinct zonal distribution of Mn oxides in the sample cells is presented. We believe that our data are the first direct observation of Mn oxidation by soil-inhabiting fungi under in situ conditions. Mn-oxidizing fungi may play an underappreciated role in the cycling of Mn in soils.     

Ultrastructure and chemical composition of the sheath of Leptothrix discophora SP-6.

Light microscopy and transmission electron microscopy of thin sections and metal-shadowed specimens showed that the sheath of Leptothrix discophora SP-6 (ATCC 51168) is a tube-like extracellular polymeric structure consisting of a condensed fabric of 6.5-nm-diameter fibrils underlying a more diffuse outer capsular layer. In thin sections, outer membrane bridges seen to contact the inner sheath layer suggested that the sheath fabric was attached to the outer layer of the gram-negative cell wall. The capsular polymers showed an affinity for cationic colloidal iron and polycationic ferritin, indicating that they carry a negative charge. Cell-free sheaths were isolated by treatment with a mixture of lysozyme, EDTA, and N-lauroylsarcosine (Sarkosyl) or sodium dodecyl sulfate (SDS). Both Sarkosyl- and SDS-isolated sheaths were indistinguishable in microscopic appearance. However, the Mn-oxidizing activity of Sarkosyl-isolated sheaths was more stable than that of SDS-isolated sheaths. The Sarkosyl-isolated sheaths also contained more 2-keto-3-deoxyoctanoic acid and more outer membrane protein than SDS-isolated sheaths. The oven-dried mass of detergent-isolated sheaths represented approximately 9% of the total oven-dried biomass of SP-6 cultures; the oven-dried sheaths contained 38% C, 6.9% N, 6% H, and 2.1% S and approximately 34 to 35% carbohydrate (polysaccharide), 23 to 25% protein, 8% lipid, and 4% inorganic ash. Gas-liquid chromatography showed that the polysaccharide was an approximately 1:1 mixture of uronic acids (glucuronic, galacturonic, and mannuronic acids and at least one other unidentified uronic acid) and an amino sugar (galactosamine). Neutral sugars were not detected. Amino acid analysis showed that sheath proteins were enriched in cysteine (6 mol%). The cysteine residues in the sheath proteins probably provide sulfhydryls for disulfide bonds that play an important role in maintaining the structural integrity of the sheath (D. Emerson and W.C. Ghiorse, J. Bacteriol. 175:7819-7827, 1993).     

Mycorrhiza and soil bacteria influence extractable iron and manganese in soil and uptake by soybean

Excess manganese (Mn) in soil is toxic to crops, but in some situations arbuscular mycorrhizal fungi (AMF) alleviate the toxic effects of Mn. Besides the increased phosphorus (P) uptake, mycorrhiza may affect the balance between Mn-reducing and Mn-oxidizing microorganisms in the mycorrhizosphere and affect the level of extractable Mn in soil. The aim of this work was to compare mycorrhizal and non-mycorrhizal plants that received extra P in relation to alleviation of Mn toxicity and the balance between Mn-oxidizing and Mn-reducing bacteria in the mycorrhizosphere. A clayey soil containing 508 mg kg⁻¹ of extractable Mn was fertilized with 30 mg kg⁻¹ (P1) or 45 mg kg⁻¹ (P2) of soluble P. Soybean (Glycine max L. Merrill, cv. IAC 8-2) plants at P1 level were non-inoculated (CP1) or inoculated with either Glomus etunicatum (GeP1) or G. macrocarpum (GmP1), while plants at P2 level were left non-inoculated (CP2). Plants were grown in a greenhouse and harvested after 80 days. In the mycorrhizosphere of the GmP1 and GeP1 plants a shift from Mn-oxidizing to Mn-reducing bacteria coincided with higher soil extractability of Mn and Fe. However, the occurrence of Mn-oxidizing/reducing bacteria in the (mycor)rhizosphere was unrelated to Mn toxicity in plants. Using 16S rDNA sequence homologies, the Mn-reducing isolates were consistent with the genus Streptomyces. The Mn-oxidizers were homologous with the genera Arthrobacter, Variovorax and Ralstonia. While CP1 plants showed Mn toxicity throughout the whole growth period, CP2 plants never did, in spite of having Fe and Mn shoot concentrations as high as in CP1 plants. Mycorrhizal plants showed Mn toxicity symptoms early in the growth period that were no longer visible in later growth stages. The shoot P concentration was almost twice as high in mycorrhizal plants compared with CP1 and CP2 plants. The shoot Mn and Fe concentrations and contents were lower in GmP1 and GeP1 plants compared with the CP2 treatment, even though levels of extractable metals increased in the soil when plants were mycorrhizal. This suggests that mycorrhiza protected its host plant from excessive uptake of Mn and Fe. In addition, higher tissue P concentrations may have facilitated internal detoxification of Mn in mycorrhizal plants. The exact mechanisms acting on alleviation of Mn toxicity in mycorrhizal plants should be further investigated.     

Superoxide Production by a Manganese-Oxidizing Bacterium Facilitates Iodide Oxidation

The release of radioactive iodine (i.e., iodine-129 and iodine-131) from nuclear reprocessing facilities is a potential threat to human health. The fate and transport of iodine are determined primarily by its redox status, but processes that affect iodine oxidation states in the environment are poorly characterized. Given the difficulty in removing electrons from iodide (I⁻), naturally occurring iodide oxidation processes require strong oxidants, such as Mn oxides or microbial enzymes. In this study, we examine iodide oxidation by a marine bacterium, Roseobacter sp. AzwK-3b, which promotes Mn(II) oxidation by catalyzing the production of extracellular superoxide (O₂⁻). In the absence of Mn²⁺, Roseobacter sp. AzwK-3b cultures oxidized ∼90% of the provided iodide (10 μM) within 6 days, whereas in the presence of Mn(II), iodide oxidation occurred only after Mn(IV) formation ceased. Iodide oxidation was not observed during incubations in spent medium or with whole cells under anaerobic conditions or following heat treatment (boiling). Furthermore, iodide oxidation was significantly inhibited in the presence of superoxide dismutase and diphenylene iodonium (a general inhibitor of NADH oxidoreductases). In contrast, the addition of exogenous NADH enhanced iodide oxidation. Taken together, the results indicate that iodide oxidation was mediated primarily by extracellular superoxide generated by Roseobacter sp. AzwK-3b and not by the Mn oxides formed by this organism. Considering that extracellular superoxide formation is a widespread phenomenon among marine and terrestrial bacteria, this could represent an important pathway for iodide oxidation in some environments.     

Zinc Sorption During Bio-oxidation and Precipitation of Manganese Modifies the Layer Stacking of Biogenic Birnessite

The formation and structural evolution of fungal mediate biogenic birnessite are dynamic processes. Although the associations of Zn with the pre-formed biogenic Mn oxides are relatively well understood, the reactivity of the intermediate precipitate at the initial stage of Mn bio-oxidation appears to differ from the final precipitate. In the present work, Zn sorption during precipitation of biogenic Mn oxides was investigated contrasting Zn sorption to pre-formed biogenic Mn oxides, using the Mn-oxidizing fungus Paraconiothyrium sp. WL-2. A substantially higher Zn uptake was found during precipitation of biogenic Mn oxides compared to Zn sorption to pre-formed biogenic Mn oxides. The presence of Zn during Mn oxidation resulted in a biogenic Mn oxide with reduced ordering in the c-axis. The precipitate was identified by X-ray diffraction (XRD) as a layer-type Mn oxide with structural properties similar to hexagonal birnessite. Extended X-ray absorption fine structure (EXAFS) spectroscopy showed that Zn forms triple-corner-sharing tetrahedral coordination (^IVTCS-Zn) complexes on the surface of birnessite, which may inhibited layer stacking of birnessite in the final products. This study emphasizes the importance of the intermediate precipitates on Zn sorption, and provides insight regarding the dynamic interaction between Zn and Mn oxide in the process of microbiological oxidation. Supplemental materials are available for this article. Go to the publisher's online edition of Geomicrobiology Journal to view the supplemental file.     

A new strain of <Emphasis Type="Italic">Bjerkandera</Emphasis> sp. production,purification and characterization of versatile peroxidase

The lignin modifying enzymes (LMEs) secreted by a new white rot fungus isolated from Chile were studied in this work. This fungus has been identified as a new anamorph of Bjerkandera sp. based on the sequences of the ribosomal DNA and morphological analysis at light microscopy showing hyaline hyphae without clamp connection, cylindrical conidia and lack of sexual forms, similar to those reported in other Bjerkandera anamorphs. The characterization of the culture medium for the highest LMEs production was performed in flask cultures, with a formulation of the culture medium containing high levels of glucose and peptone. The highest Mn-oxidizing peroxidase activity (1,400 U/L) was achieved on day 6 in Erlenmeyer flasks. Four peroxidases (named R1B1, R1B2, R1B3 and R1B4), have been purified by using ion-exchange and exclusion molar chromatographies. All of them showed typical activity on Mn²⁺ and exhibited Mn-independent activity against 2,6-dimethoxyphenol. R1B4 showed also activity on veratryl alcohol (pH 3) indicating that this enzyme belongs to the versatile peroxidase family. The high VP production capacities of this strain, as well as the enzymatic characteristics of the LMEs suggest that it may be successfully used in the degradation of recalcitrant compounds.     

The solubility of manganese in some acid soils of the tropics

Summary Soil samples obtained from genetic horizons of two upland soils and an acid sulphate sub-soil of Sierra Leone West Africa, and crushed to pass a 2 mm sieve were equilibrated with 0.01M CaCl₂. Mn⁺² activity was estimated from measured total Mn, accounting where necessary for the MnSO₄ ⁰ complex specie.Mn⁺² activity was much lower than those predicted for equilibrium with a number of Mn minerals. It seems probable that known simple silicates, sulphates, phosphates, oxides and hydroxides of Mn are too soluble to persist in the fine earth fraction of these highly weathered soils of low pH. Observed Mn⁺² activity may be governed by exchangeable and/or other forms not evaluated here.     

Manganese uptake and toxicity in magnesium-supplemented and unsupplemented Saccharomyces cerevisiae

The magnesium content of Saccharomyces cerevisiae was found to vary by up to fivefold at differing␣ stages of batch growth and during growth in the presence of differing magnesium concentrations. Excess Mg was primarily sequestered in vacuoles. Mn²⁺-uptake experiments revealed that Mg-enriched cells had a markedly reduced capacity for Mn²⁺ accumulation. For example, after 6 h incubation in the presence of 50 μM Mn²⁺, Mn levels were approximately twofold higher in cells previously grown in unsupplemented medium than in those from Mg-supplemented medium. These differences were further accentuated at higher Mn²⁺ concentrations and were not attributable to altered cell-surface charge or altered cell-surface Mn²⁺ binding. Cellular Mg status also influenced Mn toxicity towards S. cerevisiae. During exposure to 5 mM Mn²⁺, 50% reductions in the viability of cells with initial Mg contents of approximately 1400 and 2700 nmol (10⁹ cells)⁻¹ occurred after approximately 1.6 h and 3.6 h respectively. In cells containing 3300 nmol Mg (10⁹ cells)⁻¹, more than 75% viability was still maintained after 7 h incubation with 5 mM Mn²⁺. It is concluded that Mn²⁺ uptake and toxicity in S. cerevisiae are strongly influenced by intracellular Mg, possibly through Mg-dependent regulation of divalent-cation transport activity. Received: 15 May 1996 / Received revision: 13 September 1996 / Accepted: 22 September 1996     

Inoculation of Fe/Mn-oxidizing bacteria enhances Fe/Mn plaque formation and reduces Cd and As accumulation in Rice Plant tissues

Plant and Soil - Iron plaques can prevent the uptake of heavy metals on the root surface of wetland plants. The Fe and Mn oxides produced by microorganisms are major Fe/Mn-oxidizing agents in the...     

锰对外生菌根真菌生长、养分吸收、有机酸分泌和菌丝体中锰分布的影响

外生菌根真菌对于酸性和锰污染土壤的植树造林和生态恢复有重要作用。采用液体培养方法,以大白菇Rd Fr(Russula delica Fr.)、彩色豆马勃Pt 715(Pisolithus tinctorius 715)、土生空团菌Cg Fr(Cenococcum geophilum Fr.)和厚环粘盖牛肝菌Sg Kl S(Suillus grevillei(Kl.)Sing)为供试对象,研究了Mn2+对外生菌根真菌生长、养分吸收、有机酸和氢离子分泌的影响,以及锰在菌丝细胞内外的分布情况。结果表明:在0—800 mg Mn2+/L的培养液中,Mn2+对Rd Fr生长无显著影响;低浓度的Mn2+刺激Sg Kl S生长,中、高浓度无抑制作用;但大幅度降低Pt 715和Cg Fr的生物量,说明Rd Fr和Sg Kl S抗(耐)锰的能力较强。在Mn2+胁迫下,供试菌株的氮、钾含量和吸收量显著降低;含磷量和吸收量,以及草酸和柠檬酸的分泌速率因菌株不同而表现出多样性,说明在减轻Mn2+毒的过程中,磷酸盐(或聚磷酸盐)对Mn2+固定作用和有机酸的络合作用因菌株不同而异。但是,Mn2+显著降低Rd Fr和Sg Kl S的氢离子分泌速率,菌丝和原生质中的含Mn量显著低于敏感性菌株,说明降低Mn2+的活性和减少吸收可能是外生菌根真菌抗(耐)Mn2+的重要机制。此外,菌丝吸收的Mn2+绝大部份存在于质外体,少量进入细胞,前者是后者的5.23—9.21倍,说明原生质膜是外生菌根真菌防御Mn2+进入细胞的重要屏障。     

Superior Therapeutic Index of Calmangafodipir in Comparison to Mangafodipir as a Chemotherapy Adjunct

Mangafodipir is a magnetic resonance imaging contrast agent with manganese superoxide dismutase (MnSOD) mimetic activity. The MnSOD mimetic activity protects healthy cells against oxidative stress-induced detrimental effects, e.g., myelosuppressive effects of chemotherapy drugs. The contrast property depends on in vivo dissociation of Mn²⁺ from mangafodipir—about 80% dissociates after injection. The SOD mimetic activity, however, depends on the intact Mn complex. Complexed Mn²⁺ is readily excreted in the urine, whereas dissociated Mn²⁺ is excreted slowly via the biliary route. Mn is an essential but also a potentially neurotoxic metal. For more frequent therapeutic use, neurotoxicity due to Mn accumulation in the brain may represent a serious problem. Replacement of 4/[5] of Mn²⁺ in mangafodipir with Ca²⁺ (resulting in calmangafodipir) stabilizes it from releasing Mn²⁺ after administration, which roughly doubles renal excretion of Mn. A considerable part of Mn²⁺ release from mangafodipir is governed by the presence of a limited amount of plasma zinc (Zn²⁺). Zn²⁺ has roughly 10³ and 10⁹ times higher affinity than Mn²⁺ and Ca²⁺, respectively, for fodipir. Replacement of 80% of Mn²⁺ with Ca²⁺ is enough for binding a considerable amount of the readily available plasma Zn²⁺, resulting in considerably less Mn²⁺ release and retention in the brain and other organs. At equivalent Mn²⁺ doses, calmangafodipir was significantly more efficacious than mangafodipir to protect BALB/c mice against myelosuppressive effects of the chemotherapy drug oxaliplatin. Calmangafodipir did not interfere negatively with the antitumor activity of oxaliplatin in CT2[6] tumor-bearing syngenic BALB/c mice, contrary calmangafodipir increased the antitumor activity.     

Sublethal nickel toxicity shuts off manganese oxidation and pellicle biofilm formation in Pseudomonas putida GB-1

In sediments, the bioavailability and toxicity of Ni are strongly influenced by its sorption to manganese (Mn) oxides, which largely originate from the redox metabolism of microbes. However, microbes are concurrently susceptible to the toxic effects of Ni, which establishes complex interactions between toxicity and redox processes. This study measured the effect of Ni on growth, pellicle biofilm formation and oxidation of the Mn-oxidizing bacteria Pseudomonas putida GB-1. In liquid media, Ni exposure decreased the intrinsic growth rate but allowed growth to the stationary phase in all intermediate treatments. Manganese oxidation was 67% less than control for bacteria exposed to 5 μM Ni and completely ceased in all treatments above 50 μM. Pellicle biofilm development decreased exponentially with Ni concentration (maximum 92% reduction) and was replaced by planktonic growth in higher Ni treatments. In solid media assays, growth was unaffected by Ni exposure, but Mn oxidation completely ceased in treatments above 10 μM of Ni. Our results show that sublethal Ni concentrations substantially alter Mn oxidation rates and pellicle biofilm development in P. putida GB-1, which has implications for toxic metal bioavailability to the entire benthic community and the environmental consequences of metal contamination.     

Mechanisms for solubilization of cobalt,copper and nickel from Indian Ocean nodules at near neutral pH by a marine isolate

Polymetallic ocean nodules offer an alternative source for extracting valuable strategic metals like Cu, Co and Ni. A novel biodissolution process was carried out, employing the cell-free spent growth medium from a marine organism (Bacillus M1) isolated from nodules; and Cu, Co and Ni solubilization from the nodules was observed to be beyond the theoretical solubility limits at near neutral pH. Different characterization techniques revealed the presence of phenolic substances in the spent growth medium, which might have formed soluble complexes with the transition metals. The low prevailing E_h redox value in the medium suggested a strong reducing environment, favoring the reductive dissolution of the oxides. A correlation study of dissolution of Cu, Co and Ni with that of Mn and Fe in the nodules was made to investigate the mechanisms of metal solubilization by the marine isolate. Under the influence of a strong reducing environment coupled with complexation by a phenolic substance present in the spent growth medium, Mn and Fe oxides were solubilized from the nodules, resulting in concomitant dissolution of Cu, Co and Ni associated with them in the nodules.     

Patterns of sheath elongation, cell proliferation, and manganese(II) oxidation in Leptothrix cholodnii

Leptothrix cholodnii is a Mn(II)-oxidizing and sheath-forming member of the class β-Proteobacteria. Its sheath is a microtube-like filament that contains a chain of cells. From a chemical perspective, the sheath can be described as a supermolecule composed of a cysteine-rich polymeric glycoconjugate, called thiopeptidoglycan. However, the mechanism that controls the increase in sheath length is unknown. In this study, we attempted to detect sheath elongation through microscopic examination by using conventional reagents. Selective fluorescent labeling of preexisting or newly formed regions of the sheath was accomplished using combinations of biotin-conjugated maleimide, propionate-conjugated maleimide, and a fluorescent antibiotin antibody. Epifluorescence microscopy indicated that the sheath elongates at the terminal regions. On the bases of this observation, we assumed that the newly secreted thiopeptidoglycan molecules are integrated into the preexisting sheath at its terminal ends. Successive phase-contrast microscopy revealed that all cells proliferate at nearly the same rate regardless of their positions within the sheath. Mn(II) oxidation in microcultures was also examined with respect to cultivation time. Results suggested that the deposition of Mn oxides is notable in the aged regions. The combined data reveal the spatiotemporal relationships among sheath elongation, cell proliferation, and Mn oxide deposition in L. cholodnii.