Plant induced alteration in the rhizosphere and the utilisation of soil heterogeneity

Plant-soil interactions result in a special rhizosphere soil chemistry, differing from that of the bulk soil found only a few mm from the root. The aim of this study was to investigate adaptation mechanisms of herbs growing in acid soils through studying their rhizosphere chemistry in a greenhouse experiment and in a field study. Ten herbs were grown in acid soil (pH 4.2 in the soil solution) in the greenhouse. The concentrations of NO₃ ^-, SO₄ ^2-, phosphates, Ca²⁺, Mg²⁺, Mn²⁺, K⁺, Na⁺, NH₄ ⁺ and pH were analysed in soil solutions obtained by centrifugation. The general pattern found was a depletion of nutrients in the rhizosphere compared with their concentrations in the bulk soil. The pH increase (up to 0.7 units) in the rhizosphere soil appeared to be caused by plant uptake of NO₃ ^- (r²=0.88). The ion concentrations in the soil solution of the rhizosphere were dependent on plant species and biomass increase. Although species with a larger biomass and higher growth rates showed a higher degree of ion depletion (except for Na⁺, SO₄ ^2-) in the rhizosphere, there were also species specific responses. A field study of five herbs at five oak forest sites in Southern Sweden (Scania) was also carried out. In addition to the soil solution concentrations, the loss on ignition (LOI) and the concentrations of 0.1 M BaCl₂ extractable K⁺, Mg²⁺, Mn²⁺, Ca²⁺, and Al ions were measured. The amount of soil solution Al was determined as free ionic (quickly reacting) Al. For all species and sites, the LOI and the concentrations of exchangeable cations were higher in the rhizosphere than in the bulk soil, apparently due to the roots preferably growing at organic-rich microsites. The concentrations of the ions as measured in the centrifuged soil solution, were either higher in the rhizosphere than in the bulk soil or were the same in both, except for NO₃ ^- and quickly reacting Al. The lower concentrations of quickly reacting Al in the rhizosphere, compared with the bulk soil could indicate the uptake of Al by the plant or the exudation of complexing substances. The pH differences were only small and mostly non-significant. Plant-soil interactions and the ability of plants to utilise heterogeneity of the soil appear to be more important for plant growth in acid soils than recognised heretofore. Rhizosphere studies provide an important means of understanding plant strategies in acid soils. This revised version was published online in June 2006 with corrections to the Cover Date.     

Influence of Certain Cations on Activity of Succinyl CoA Synthetase From Tobacco

Succinyl CoA synthetase from Nicotiana tabacum exhibited a requirement for univalent and divalent cations. Mn²⁺ replaced Mg²⁺ in the assay medium and Co²⁺ and Ca²⁺ partially replaced Mg²⁺. Addition of Zn²⁺ resulted in no enzyme activity. The enzyme was activated by univalent cations K⁺, Rb⁺, NH₄⁺, and Na⁺; Li⁺ showed little or no activation. Maximum enzyme activity varied significantly with potassium salts of different anions. Greatest activation was obtained with K₃PO₄ and, respectively, KCl, KNO₃, K₂SO₄ and KF exhibited steadily decreasing enzyme activation.     

盐分胁迫对啤酒大麦幼苗生长、离子平衡和根际pH变化的影响

盐分胁迫不仅影响植物的生长,而且会影响植物根际微域环境。根际pH的改变对土壤养分的有效性和微生物群落组成的变化有重要影响。为了探究啤酒大麦幼苗对不同类型盐分胁迫的生理生态响应机制和根际pH变化影响的生理机制,采用水培法,通过不同类型盐分(对照、混合Na盐、混合Cl盐和NaCl)胁迫处理啤酒大麦幼苗,对其生长、离子平衡和根际pH变化进行了研究。结果表明,1)在3种不同类型盐分胁迫下,啤酒大麦幼苗地上部干重、含水量均有所降低,而根冠比增加,尤其在NaCl胁迫下啤酒大麦幼苗地上部干重较对照显著降低了17.88%,而根干重和根冠比则分别增加了19.12%和43.86%。不同类型盐分胁迫抑制了啤酒大麦幼苗根长的生长,尤其在混合Na盐胁迫下根长降低明显(P0.05),但促进了根表面积和根体积的增加,尤其在混合Cl盐胁迫下,根表面积和根体积分别增加了41.76%和84.38%。2)不同类型盐分胁迫下啤酒大麦幼苗地上部离子平衡发生改变,在混合Na盐和NaCl胁迫下啤酒大麦幼苗主要吸收Na~+,地上部K~+/Na~+、Ca~(2+)/Na~+和Mg~(2+)/Na~+显著降低;混合Cl盐和NaCl胁迫下则过量吸收Cl~-,抑制了H_2PO_4~-、NO_3~-和SO_4~(2-)的吸收。3)在混合Na盐、混合Cl盐和NaCl盐分胁迫下,啤酒大麦幼苗对阴离子的吸收总量高于对阳离子的吸收总量,离子平衡计算结果表明根际呈碱化现象,与原位显色结果一致,且在混合Cl盐胁迫下根际碱化程度最大。     

Multiphasic accumulation of nutrients by plants

Seedlings of rice (Oryza sativa), soybean (Glycine max) and sour orange (Citrus aurantium) were grown for 20 to 125 days under controlled conditions in nutrient solutions wiht up to 16 different concentrations of NH⁴₊, H₂PO₄^-, K⁺, Ca²⁺, Mg²⁺ or Zn²⁺. Nutrient concentrations differed by up to 4 orders of magnitude (H₂PO₄^- and Zn²⁺) and were kept constant or within certain limits by changing solutions daily. Dry weights and concentrations of N, P, K, Ca, Mg or Zn were determined for roots and tops (or roots, stems and leaves). The relationship between tissue concentration of an element and external concentration of the corresponding nutient ion was invariably multiphasic, with phases separated by sharp breaks or jumps. The kinetics of accumulation were similar to those of short-term uptake of the same ions. Reanalysis of previously published data (including data for Mn²⁺) for other plants yielded, similarly, bi- or multiphasic isotherms for accumulation. Accumulation patterns and growth were in several instances correlated, with separate phases coinciding with regions of poverty adjustment, luxury consumption and toxicity. Implications of multiphasic kinetics of long-term nutrient accumulation for membrane properties, fluxes and regulation include: (i) Membranes and uptake mechanisms must remain relatively constant throughout the life of the plant with respect to affinities for ions and concentrations at which transitions occur. (ii) Rate-limitation occurs at the plasmalemma of the root cortical cells. (iii) Uptake is at all times under multiphasic control by the external solution.     

Toxicity of chromium and tin toAnabaena doliolum Interaction with bivalent cations

Summary The toxicity of chromium and tin on growth, photosynthetic carbon-fixation, oxygen evolution, heterocyst differentiation and nitrogenase activity ofAnabaena doliolum and its interaction with bivalent cations has been studied. Some interacting cations, viz. Ca²⁺, Mg²⁺ and Mn²⁺, substantially antagonised the toxic effects of chromium and tin with reference to growth, heterocyst differentiation and nitrogenase activity in the following hierarchal sequence: Ca²⁺ > Mg²⁺ > Mn²⁺. However, the sequence of hierarchy was Mg²⁺ > Ca²⁺ > Mn²⁺ for carbon fixation and Mn²⁺ > Mg²⁺ > Ca²⁺ for photosynthetic oxygen evolution. Synergistically inhibitory patterns were noticed for all the parameters, viz. growth,¹⁴CO₂ uptake, oxygen evolution, heterocyst differentiation and nitrogenase activity ofA. doliolum when Ni²⁺, Co²⁺ and Zn²⁺ were combined with the test metals in the growth medium. These cations followed the following sequence of synergistic inhibition: Ni²⁺ > Co²⁺ > Zn²⁺. Among all the interacting cations, Ca²⁺, Mg²⁺ and Mn²⁺ exhibited antagonistic effects which relieved the test cyanobacterium from metal toxicity. In contrast to this, Ni²⁺, CO²⁺ and Zn²⁺ showed synergistic inhibition which potentiating the toxicity of test metals in the N₂-fixing cyanobacteriumA. doliolum. It is evident from the present study that bivalent cations, viz. Ca²⁺, Mg²⁺, Mn²⁺, Ni²⁺, Co²⁺ and Zn²⁺, may appreciably regulate the toxicity of heavy metals in N₂-fixing cyanobacteria if present in aquatic media.     

Characterization of Mg2+-ATPase from sheep kidney medulla: purification.

Magnesium-dependent adenosine triphosphatase has been purified from sheep kidney medulla plasma membranes. The purification, which is based on treatment of a kidney plasma membrane fraction with 0.5% digitonin in 3 mm MgCl₂, effectively separates the Mg²⁺-ATPase from (Na⁺ + K⁺)-ATPase present in the same tissue and yields the Mg²⁺-ATPase in soluble form. The purified enzyme is activated by a variety of divalent cations and trivalent cations, including Mg²⁺, Mn²⁺, Ca²⁺, Co²⁺, Fe²⁺, Zn²⁺, Eu³⁺, Gd³⁺, and VO²⁺. Sodium dodecyl sulfate-polyacrylamide gel electrophoresis of the purified enzyme shows two bands with R_f values corresponding to molecular weights of 150,000 and 77,000. The larger peptide is phosphorylated by [γ-³²P]ATP, suggesting that this peptide may contain the active site of the Mg²⁺-ATPase. The Mg²⁺-ATPase activity is unaffected by the specific (Na⁺ + K⁺)-ATPase inhibitor ouabain.     

Comparison of 4-hydroxynzoate decarboxylase and phenol carboxylase activities in cell-free extracts of a defined, 4-hydroxybenzoate and phenol-degrading anaerobic consortium

Summary Two 4-hydroxybenzoate decarboxylase activities and a phenol carboxylase activity were found in cell-free extracts of a defined, 4-hydroxybenzoate- or phenol-grown consortium. Both decarboxylase activities were loosely membrane-associated and required K⁺ but a different pH and ion strength. Loss of activity of both decarboxylases by EDTA could be compensated by Zn²⁺ ions. The K _m values for 4-hydroxybenzoate and K⁺ of the decarboxylase activities with pH optima at 6.4 or 7.8 were 0.02 and 2.5 or 0.004 and 0.5 mm, respectively. 3,4-Dihydroxybenzoate, 3,4,5-tridydroxybenzoate, 3,5-dimethoxy-4-hydroxybenzoate and 3-chloro-4-hydroxybenzoate were also decarboxylated by both enzyme activities. The phenol carboxylase was a soluble enzyme with its pH optimum at 6.5. It required K⁺, Rb⁺ or NH _inf4 ^sup+ as monovalent, Zn²⁺, Mg²⁺, Mn²⁺ or Ni²⁺ as divalent cations and catalysed the carboxylation of phenol if 2,4-,2,3,4- or 2,4,6-hydroxybezoates were absent. The three enzyme activities were not influenced by Avidin and thus were probably not biotin-dependent enzymes. Offprint requests to: J. Winter     

The phosphate-pyrophosphate exchange and hydrolytic reactions of the membrane-bound pyrophosphatase ofRhodospirillum rubrum: Effects of pH and divalent cations

The relation that exist between the Pi-PPi exchange reaction and pyrophosphate hydrolysis by the membrane-bound pyrophosphatase of chromatophores ofRhodospirillum rubrum was studied. The two reactions have a markedly different requirement for pH. The optimal pH for hydrolysis was 6.5 while the Pi-PPi exchange reaction was at 7.5; the pH affects mainly theK _m of Mg²⁺ or Pi for the enzyme; Mn²⁺ and Co²⁺ support the Pi-PPi exchange reaction partially (50%), but the reaction is slower than with Mg²⁺; other divalent cations like Zn²⁺ or Ca²⁺ do not support the exchange reaction. In the hydrolytic reaction, Zn²⁺, at low concentration, substitutes for Mg²⁺ as substrate, and Co²⁺ also substitutes in limited amount (50%). Other cations (Ca²⁺, Cu²⁺, Fe²⁺, etc.) do not act as substrates in complex with PPi. The Zn²⁺ at high concentrations inhibited the hydrolytic reaction, probably due to uncomplexed free Zn²⁺. In the presence of high concentration of substrate for the hydrolysis (Mg-PPi) the divalent cations are inhibitory in the following order: Zn²⁺>Mn²⁺>Ca²⁺Co²⁺>Fe²⁺>Cu²⁺>Mg²⁺. The data in this work suggest that H⁺ and divalent cations in their free form induced changes in the kinetic properties of the enzyme.     

Physical and kinetic properties of sheep liver pyridoxine kinase

Pyridoxine kinase purified from sheep liver was found to consist of a single polypeptide chain with a molecular weight of 60,000 as determined by gel filtration, sedimentation equilibrium ultracentrifugation, and sodium dodecyl sulfate-polyacrylamide gel electrophoresis. The isoelectric pH of the enzyme was 5.1, and the pH optimum was between 5.5 and 6.0. The enzyme required divalent cations for activity. At cation concentrations of 80 μm, the enzyme activity with each cation was in the order of Zn²⁺ > Mn²⁺ > Mg²⁺. At cation concentrations of 400 μm, the enzyme activity with each cation was in the order of Mn²⁺ > Zn²⁺ > Mg²⁺. Excess free divalent cation inhibited the enzyme. Pyridoxine kinase also required monovalent cations. The enzyme activation was greatest with K⁺, then Rb⁺ and NH₄⁺, whereas the enzyme had very little activity with Na⁺, Li⁺, or Cs⁺. Na⁺ did not interfere with the activation by K⁺. The activation of the kinase by K⁺, NH₄⁺, and Rb⁺ followed Michaelis-Menten kinetics, and the apparent K_m values for the cations were 8.9, 3.7, and 5.3 mm, respectively. Increasing the potassium concentration lowered the apparent K_m value of the enzyme for pyridoxine and had little or no effect on the K_m for ZnATP^2? or the V of the kinase-catalyzed reaction.     

Effect of nitrogen form and phosphorus source on the growth,nutrient uptake and rhizosphere soil property of Camellia sinensis L.

The effects of nitrogen form and phosphorus source on the growth, nutrient uptake and rhizosphere soil property of tea (Camellia sinensis L.) were investigated in a pot experiment. The experiment was performed with a compartmental cropping device, which enables the collection of rhizosphere soil at defined distances from the root of tea plant. Nitrogen was supplied as nitrate or ammonium in combination with soluble phosphorus as Ca(H₂PO₄)₂ or insoluble P as rock phosphate. The leaf dry matter production of tea was significantly greater in the treatments with NH₄ ⁺ than NO₃ ^-, whereas dry matter production of root and stem was not significantly affected. Addition of phosphorus as either source did not influence the dry matter production. The concentrations of K in root, Mg and Ca in both the shoot and root supplied with NO₃ ^- were significantly higher than in NH₄ ⁺ and influence of P sources was minor. On the contrary, Al and Mn concentrations were significantly larger in NH₄ ^--fed plants which could be attributed to remarkably increased availability of Al and Mn caused by acidification of the rhizosphere soil (the first 1-mm soil section from the root surface) with NH₄–N nutrition. The concentration of N in shoot was also significantly higher in NH₄- than in NO₃-fed plants, indicating higher use efficiency of NH₄–N. Whatever the phosphate source, rhizosphere pH declined in ammonium compared to in nitrate treatment. The pH decrease was much larger when no P or soluble P were applied and reached 0.85–1.30 units which extended to 3–5 mm away from the root surface. Exchangeable acidity, content of exchangeable Al and Mn were also considerably higher in the rhizosphere soils of NH₄ ⁺ fed tea plants. Significant amounts of P dissolved from rock phosphate accumulated in rhizosphere of NH₄ ⁺, not NO₃ ^-, suggesting that the dissolution of rock phosphate was induced by the proton excreted by tea root fed with ammonium. With soluble P addition, shoot and root P concentrations were greater in NH₄ ⁺ than in NO₃ ^- treatment and it appeared that this difference could not be sufficiently explained by the available P content in soil which was only slightly higher in NH₄ ⁺ treatment. With rock phosphate addition, the shoot and root P concentrations were hardly affected by nitrogen form, although the available P content was much higher and accumulated in the rhizosphere soil supplied with ammonium. The reason for this was discussed with regard to the inter-relationship of Al with P uptake. This revised version was published online in June 2006 with corrections to the Cover Date.     

Closure of the yeast mitochondria unspecific channel (YMUC) unmasks a Mg2+ and quinine sensitive K+ uptake pathway in Saccharomyces cerevisiae

The K⁺ uptake pathways in yeast mitochondria are still undefined. Nonetheless, the K⁺-mediated mitochondrial swelling observed in the absence of phosphate (PO₄) and in the presence of a respiratory substrate has led to propose that large K⁺ movements occur in yeast mitochondria. Thus, the uptake of K⁺ by isolated yeast mitochondria was evaluated. Two parallel experiments were conducted to evaluate K⁺ transport; these were mitochondrial swelling and the uptake of the radioactive K⁺ analog ⁸⁶Rb⁺. The opening of the yeast mitochondrial unspecific channel (YMUC) was regulated by different PO₄ concentrations. The high protein concentrations used to measure ⁸⁶Rb⁺ uptake resulted in a slight stabilization of the transmembrane potential at 0.4 mM PO₄ but not at 0 or 4 mM PO₄. At 4 mM PO₄ swelling was inhibited while, in contrast, ⁸⁶Rb⁺ uptake was still observed. The results suggest that an energy-dependent K⁺ uptake mechanism was unmasked when the YMUC was closed. To further analyze the properties of this K⁺ uptake system, the Mg²⁺ and quinine sensitivity of both swelling and ⁸⁶Rb⁺ uptake were evaluated. Under the conditions where the unspecific pore was closed, K⁺ transport sensitivity to Mg²⁺ and quinine increased. In addition, when Zn²⁺ was added as an antiport inhibitor, uptake of ⁸⁶Rb⁺ increased. It is suggested that in yeast mitochondria, the K⁺ concentration is highly regulated by the equilibrium of uptake and exit of this cation through two specific transporters.     

Characterization of a partially purified adenosine triphosphatase from a corn root plasma membrane fraction

The (K⁺,Mg²⁺)-ATPase was partially purified from a plasma membrane fraction from corn roots (WF9 × Mol7) and stored in liquid N₂ without loss of activity. Specific activity was increased 4-fold over that of the plasma membrane fraction. ATPase activity resembled that of the plasma membrane fraction with certain alterations in cation sensitivity. The enzyme required a divalent cation for activity (Co²⁺ > Mg²⁺ > Mn²⁺ > Zn²⁺ > Ca²⁺) when assayed at 3 millimolar ATP and 3 millimolar divalent cation at pH 6.3. When assayed in the presence of 3 millimolar Mg²⁺, the enzyme was further activated by monovalent cations (K⁺, NH₄⁺, Rb⁺ Na⁺, Cs⁺, Li⁺). The pH optima were 6.5 and 6.3 in the absence and presence of 50 millimolar KCl, respectively. The enzyme showed simple Michaelis-Menten kinetics for the substrate ATP-Mg, with a K_m of 1.3 millimolar in the absence and 0.7 millimolar in the presence of 50 millimolar KCl. Stimulation by K⁺ approached simple Michaelis-Menten kinetics, with a K_m of approximately 4 millimolar KCl. ATPase activity was inhibited by sodium orthovanadate. Half-maximal inhibition was at 150 and 35 micromolar in the absence and presence of 50 millimolar KCl. The enzyme required the substrate ATP. The rate of hydrolysis of other substrates, except UDP, IDP, and GDP, was less than 20% of ATP hydrolysis. Nucleoside diphosphatase activity was less than 30% of ATPase activity, was not inhibited by vanadate, was not stimulated by K⁺, and preferred Mn²⁺ to Mg²⁺. The results demonstrate that the (K⁺,Mg²⁺)-ATPase can be clearly distinguished from nonspecific phosphohydrolase and nucleoside diphosphatase activities of plasma membrane fractions prepared from corn roots.     

Absorption of copper, zinc, and manganese by sugarcane leaf tissue

The absorption of Cu²⁺, Zn²⁺, and Mn²⁺ by leaf tissue of 4-month old sugarcane plants (Saccharum officinarum L., var. H53-263) has been investigated. After the “apparent free space” fraction was desorbed, the absorption of Cu²⁺, Mn²⁺, and Zn²⁺ yielded a curve typical of many ion uptake processes when measured as a function of the external concentration. However, only 1 absorption mechanism was evident for each cation. The pH optimum for Cu²⁺ and Zn²⁺ uptake was 5.0 to 6.0, whereas that for Mn²⁺ absorption was 4.5 to 6.0. Absorption was competitively inhibited by H⁺, and this inhibition was reversible when 0.5 mm Ca²⁺ was present. Cu²⁺ and Zn²⁺ were absorbed through the same carrier sites, as concluded from their mutually competitive activities. Mn²⁺ was absorbed through a second, independent mechanism. Uptake of each cation was strongly inhibited by uncouplers of oxidative phosphorylation, by Amytal and Nembutal², by 5 × 10⁻²m succinate, and by ADP and P_i. Absorption of Cu²⁺, Zn²⁺, and Mn²⁺ was concluded to be coupled to oxidative phosphorylation, and specifically to energy-conservation Site I.     

Production and partial characterization of two types of phytase from Aspergillus niger NCIM 563 under submerged fermentation conditions

Novel extracellular phytase was produced by Aspergillus niger NCIM 563 under submerged fermentation conditions at 30 °C in medium containing dextrin and glucose as carbon sources along with sodium nitrate as nitrogen source. Maximum phytase activity (41.47 IU/mL at pH 2.5 and 10.71 IU/mL at pH 4.0) was obtained when dextrin was used as carbon source along with glucose and sodium nitrate as nitrogen source. Nearly 13 times increase in phytase activity was observed when phosphate in the form of KH₂PO₄ (0.004 g/100 mL) was added in the fermentation medium. Physic-chemical properties of partially purified enzyme indicate the possibility of two distinct forms of phytases, Phy I and Phy II. Optimum pH and temperature for Phy I was 2.5 and 60 °C while Phy II was 4.0 and 60 °C, respectively. Phy I was stable in the pH range 1.5–3.5 while Phy II was stable in the wider pH range, 2.0–7.0. Molecular weight of Phy I and Phy II on Sephacryl S-200 was approximately 304 kDa and 183 kDa, respectively. Phy I activity was moderately stimulated in the presence of 1 mM Mg²⁺, Mn²⁺, Ca²⁺ and Fe³⁺ ions and inhibited by Zn²⁺ and Cd²⁺ ions while Phy II activity was moderately stimulated by Fe³⁺ ions and was inhibited by Hg²⁺, Mn²⁺ and Zn²⁺ ions at 1 mM concentration in reaction mixture. The Km for Phy I and II was 3.18 and 0.514 mM while Vmax was 331.16 and 59.47 μmols/min/mg protein, respectively.     

Uptake of Metal Ions by Rhizopus arrhizus Biomass

Rhizopus arrhizus biomass was found to absorb a variety of different metal cations and anions but did not absorb alkali metal ions. The amount of uptake of the cations was directly related to ionic radii of La³⁺, Mn²⁺, Cu²⁺, Zn²⁺, Cd²⁺, Ba²⁺, Hg²⁺, Pb²⁺, UO₂²⁺, and Ag⁺. The uptake of all the cations is consistent with absorption of the metals by sites in the biomass containing phosphate, carboxylate, and other functional groups. The uptake of the molybdate and vanadate anions was strongly pH dependent, and it is proposed that the uptake mechanism involves electrostatic attraction to positively charged functional groups.     

Novel function of eubacterial flagella: role in aggregation of a marine bacterium

Pseudomonas marina (ATCC 27 129) rapidly aggregates when suspended in buffered artificial seawater (ASW). Light microscopic observations of stained preparations, showed that flagella-flagella contact was responsible for this phenomenon. Aggregation did not occur if flagella were sheared off, or if motility was inhibited with NaN₃. Aggregates were not observed when Mg²⁺ was omitted from ASW, even though the bacteria remained motile. Other divalent cations, including Ca²⁺, Mn²⁺, and Ba²⁺ could replace Mg²⁺. However, there is no absolute requirement for divalent cations, since aggregation occurred in ASW containing Cs⁺ or Li⁺ instead of Mg²⁺. P. marina aggregates developed from pH 5.8–8.4, but not below pH 5.8 even though motility continued unimpaired to pH 4.5.Abbreviation ASW artificial seawater     

Genes for all metals—a bacterial view of the Periodic Table

Bacterial chromosomes have genes for transport proteins for inorganic nutrient cations and oxyanions, such as NH₄ ⁺, K⁺, Mg²⁺, Co²⁺, Fe³⁺, Mn²⁺, Zn²⁺ and other trace cations, PO₄ ^3-, SO₄ ^2- and less abundant oxyanions. Together these account for perhaps a few hundred genes in many bacteria. Bacterial plasmids encode resistance systems for toxic metal and metalloid ions including Ag⁺ AsO₂ ^-, AsO₄ ^3-, Cd²⁺, Co²⁺, CrO₄ ²⁻, Cu²⁺, Hg²⁺, Ni²⁺, Pb²⁺, TeO₃ ²⁻, TI⁺ and Zn²⁺. Most resistance systems function by energy-dependent efflux of toxic ions. A few involve enzymatic (mostly redox) transformations. Some of the efflux resistance systems are ATPases and others are chemiosmotic ion/proton exchangers. The Cd²⁺-resistance cation pump of Gram-positive bacteria is membrane P-type ATPase, which has been labeled with ³²P from [γ-³²P]ATP and drives ATP-dependent Cd²⁺ (and Zn²⁺) transport by membrane vesicles. The genes defective in the human hereditary diseases of copper metabolism, Menkes syndrome and Wilson’s disease, encode P-type ATPases that are similar to bacterial cadmium ATPases. The arsenic resistance system transports arsenite [As(III)], alternatively with the ArsB polypeptide functioning as a chemiosmotic efflux transporter or with two polypeptides, ArsB and ArsA, functioning as an ATPase. The third protein of the arsenic resistance system is an enzyme that reduces intracellular arsenate [As(V)] to arsenite [As(III)], the substrate of the efflux system. In Gram-negative cells, a three polypeptide complex functions as a chemiosmotic cation/protein exchanger to efflux Cd²⁺, Zn²⁺ and Co²⁺. This pump consists of an inner membrane (CzcA), an outer membrane (CzcC) and a membrane-spanning (CzcB) protein that function together. Received 08 August 1997/ Accepted in revised form 01 November 1997     

Raman spectroscopic studies on the interaction between divalent counterion and polyion

The nature of the interaction between polyacrylalc ion and several divalent cations, such as Cu²⁺, Mn²⁺, Zn²⁺, Ba²⁺ and Mg²⁺, was investigated using Raman spectroscopy. A specific Raman band characteristic of a carboxyl group is shifted upon addition of Cu²⁺. Zn²⁺ and Mn²⁺ to partially neutralized poly(acrylic acid). On the other hand. no frequency shift of the specific Raman band is observed on addition of Mg²⁺ and Ba²⁺*, though the intensity of the specific Raman band decreases with concentration of MgCl₂. It is concluded from these Raman data that the interaction between polyacrylatc ion and Cu²⁺. Zn²⁺ or Mn²⁺ includes a specific interaction with bond formation, whereas in the case of Mg²⁺ and Ba²⁺, the electrostatic interaction is dominant.     

Effects of divalent metal ions on the fluorescence and glucose-quenching of yeast hexokinase isozymes

Titrations of the quenching of the tryptophan fluorescence of yeast hexokinase isozymes P-I and P-II by Mg²⁺, Mn²⁺, Ca²⁺, Cd²⁺, and Zn²⁺ ions and by glucose in the presence of each of these ions (10mM) were performed at pH 5.5 and 6.5 at 20°C. At the higher pH there was a reversal of the type of glucose-binding cooperativity for P-II from negative to positive when either Mn²⁺ or Ca²⁺ was present in the buffered isozyme solution before the glucose titration, whereas Mg²⁺ caused the glucose binding to become noncooperative. Zn²⁺ and Cd²⁺ decreased the glucose quenching of P-II fluorescence drastically at pH 5.5, from a value of 15% in buffer to only 4%. Thus, only these two ions, of the five studied, cause the conformation change that results in quenching of the glucose-quenchable cleft tryptophan of P-II. Glucose binding to the P-I isozyme exhibited positive cooperativity in the presence of either Ca²⁺, Mg²⁺, or Mn²⁺, as well as in buffer alone, at both pH's. At the lower pH, Ca²⁺ enhanced the efficiency of glucose quenching of P-I fluorescence several-fold, while Mn²⁺ increased it only about 40% and Mg²⁺ not at all. Further, Ca²⁺ raised the degree of cooperativity (Hill coefficient) of glucose binding to P-I at this pH from the value of 1.42 in buffer and in the presence of Mg²⁺ and Mn²⁺ to 1.94, i.e., almost up to the highest possible value, 2, for dimeric hexokinase. However, at pH 6.5 the Ca²⁺ effect on the cooperativity was negligible, while Mg²⁺ and Mn²⁺ decreased the coefficient from 1.6 in buffer to about 1.4. The biological implications of these diverse metal ion effects are discussed.     

Iron transport by proteoliposomes containing mitochondrial F1Fo ATP synthase isolated from rat heart

In this work, we present evidence of Fe²⁺ transport by rat heart mitochondrial F₁F_o ATP synthase. Iron uptake by the vesicles containing the enzyme was concentration- and temperature-dependent, with an optimum temperature of 37 °C. Both ATP and ADP stimulated iron uptake in a concentration-dependent manner, whereas AMP, AMPPCP, and mADP did not. Inhibitors of the enzyme, oligomycin, and resveratrol similarly blocked iron transport. The iron uptake was confirmed by inhibition using specific antibodies against the α, β, and c subunits of the enzyme. Interestingly, slight transport of common divalent and trivalent metal ions such as Mg⁺², Ca⁺², Mn⁺², Zn⁺², Cu⁺², Fe⁺³, and Al⁺³ was observed. Moreover, Cu⁺², even in the nM range, inhibited iron uptake and attained maximum inhibition of approximately 56%. Inorganic phosphate (Pi) in the medium exerted an opposite effect depending on the type of adenosine nucleotide, which was suppressed with ATP, but enhanced with ADP. A similarly stimulating effect of ATP and ADP with an inverse effect of Pi suggests that the activity of ATPase and ATP synthase may be associated with iron uptake in a different manner, probably via antiport of H⁺.