Pulse radiolytically determined superoxide dismutase mimicking activity of copper-putrescine-pyridine,a diSchiff base coordinated copper complex

In order to exclude possible interferences in the many indirect superoxide dismutase (SOD) activity measurements using the copper-putrescine-pyridine complex (Cu-PuPy) a pulse radiolytic study on this diSchiff base copper complex has been devised and sucessfully performed. The reaction kinetics and rate constants of pulse radiolytically generated superoxide in the presence of Cu-PuPy reveal pseudo first-order characteristics. The rate constant (k ₂ = 6 ± 1 × 10⁸ m ^–1 s ^–1) is comparable to that of an Fe-SOD and is approximately a factor of 3 lower than that of bovine Cu₂Zn₂-SOD. The superoxide dismutating activity of Cu-PuPy shows a more pronounced temperature dependence compared with that of Cu₂Zn₂-SOD. Arrhenius analyses yielded activation energies of 7.8 ±0.3 and 4.6 ± 0.2 kcal mol^–1 for Cu-PuPy and Cu₂Zn₂-SOD, respectively. The rate constant of the reaction of superoxide and Cu-PuPy is highest at pH 5.0. The possible application of Cu-PuPy for new therapeutic strategies on all types of inflammatory diseases appears to be promising.     

Interactions of growth inhibitory factor with hydroxyl and superoxide radicals

To show the effects of growth inhibitory factor (Cu₄Zn₃MT-III) involved in the scavenging of reactive oxygen species (ROS), a pulse radiolytic study was employed using N₂O-saturated Cu₄Zn₃MT-III aqueous solutions. It was demonstrated that the oxidizing OH radical efficiently reacted with Cu₄Zn₃MT-III by forming a thiyl radical RS with a second-order constant of 1.46×10¹¹ mol l^–1s^–1, which was determined by competition kinetics against KSCN. The thiyl radical RS reacted rapidly and reversibly with a thiolate in Cu₄Zn₃MT-III to form radical anion RSSR ^– with a constant of 1.65×10⁹ mol lL^–1s^–1 per thiolate, while the constant of the decay of this radical anion was 2.72×10⁵ s^–1, and the equilibrium constant of the formation for RSSR ^– was 6.08×10³ mol^–1 l. These values were close to those of Cd₅Zn₂MT-II. The SOD activity of Cu₄Zn₃MT-III to quench O₂ ^–was assayed by the riboflavine-methionine-nitrobluetetrazolium (NBT) method which catalyzed the dismutation of superoxide (O₂ ^–) at pH 7.8 with an IC₅₀ value of 1.50×10^–6 M for Cu₄Zn₃MT-III and 1.62×10^–6 M for Cd₅Zn₂MT-II. Additionally, the down-regulation of GIF may be a main factor in the decrease of the scavenging ability for the free OH and O₂ ^–radicals, which is possibly associated with the pathogenesis of neurodegenerative disease.     

Spatial variability of NO and NO2 flux rates from soil of spruce and beech forest ecosystems

In order to evaluate differences in the magnitude of NO and NO₂ flux rates between soil areas in direct vicinity to tree stems and areas of increasing distance to tree stems, we followed in 1997 at the Höglwald Forest site with a fully automated measuring system a complete annual cycle of NO and NO₂ fluxes from soils of an untreated spruce stand, a limed spruce strand, and a beech stand using at each stand measuring chambers which were installed onto the soils in such a way that they formed a stem to stem gradient. Flux data obtained since the end of 1993 from measuring chambers placed at the interstem areas of the stands, which had been used for the calculation of the long year annual mean of NO and NO₂ flux rates from soils of the stands, are compared to both (a) those obtained from the interstem chambers in 1997 and (b) those from the stem to stem gradient chambers. Daily mean NO fluxes obtained in 1997 were in a range of 0.3 – 280.1 g NO-N m^–2 h^–1 at the untreated spruce stand, 0.5 – 273.2 g NO-N m^–2 h^–1 at the limed spruce stand and 0.5 - 368.8 g NO-N m^–2 h^–1 at the beech stand, respectively. Highest NO emission rates were observed during summer, lowest during winter. Daily mean NO₂ fluxes were in a range of –83.1 – 7.6 g NO₂-N m^–2 h^–1 at the untreated spruce stand, -85.1 – 2.1 g NO₂-N m^–2 h^–1 at the limed spruce stand and –77.9 to –2.0 g NO₂-N m^–2 h^–1 at the beech site, respectively. As had been observed for the years 1994–1996, also in 1997 NO emission rates were highest at the untreated spruce stand and lowest at the beech stand and liming of a spruce stand resulted in a significant decrease in NO emission rates. For NO₂ no marked differences in the magnitude of flux rates were found between the three different stands. Results obtained from the stem to stem gradient experiments revealed that at all stands studied NO emission rates were significantly higher (between 1.6- and 2.6-fold) from soil areas close to the tree stems and decreased – except at the beech stand - with increasing distance from the stems, while for NO₂ deposition no marked differences were found. Including the contribution of soil areas in direct vicinity to the beech stems in the estimation of the annual mean NO source strength revealed that the source strength has been underestimated by 40% in the past.     

Influence of chelators and iron ions on the production and degradation of H2O2 by β-amyloid–copper complexes

β-Amyloid peptide (Aβ) 1–42, involved in the pathogenesis of Alzheimer’s disease, binds copper ions to form Aβ · Cu_n complexes that are able to generate H₂O₂ in the presence of a reductant and O₂. The production of H₂O₂ can be stopped with chelators. More reactive than H₂O₂ itself, hydroxyl radicals HO (generated when a reduced redox active metal complex interacts with H₂O₂) are also probably involved in the oxidative stress that creates brain damage during the disease. We report in the present work a method to monitor the effect of chelating agents on the production of hydrogen peroxide by metallo-amyloid peptides. The addition of H₂O₂ associated to a pre-incubation step between ascorbate and Aβ · Cu_n allows to study the formation of H₂O₂ but also, at the same time, its transformation by the copper complexes. Aβ · Cu_n peptides produce but do not efficiently degrade H₂O₂. The reported analytic method, associated to precipitation experiments of copper-containing amyloid peptides, allows to study the inhibition of H₂O₂ production by chelators. The action of a ligand such as EDTA is probably due to the removal of the copper ions from Aβ · Cu_n, whereas bidentate ligands such as 8-hydroxyquinolines probably act via the formation of ternary complexes with Aβ · Cu_n. The redox activity of these bidentate ligands can be modulated by the incorporation or the modification of substituents on the quinoline heterocycle.     

Influence of acid rain and liming on fluxes of NO and NO2 from forest soil

Flux measurements of nitric oxide (NO) and nitrogen dioxide (NO₂) were performed in a coniferous forest (Höglwald) in southern Germany using a fully automated measuring system based on the dynamic chamber method. The forest soil was predominately a source of NO, but mean flux rates of NO ranged from –26.3 (deposition) to 55 g N m^-2 h_-1 (emission). NO₂ was deposited on the forest soil with mean flux rates ranging from –4 to –72 g N m^-2 h_-1 . Removal of forest floor vegetation did not influence NO or NO₂ fluxes. Apparently, forest floor vegetation was neither a source of NO nor a significant sink of NO₂. When the organic layer of the forest soil was removed, net NO flux changed from emission to deposition. Thus NO emitted to the atmosphere was produced almost exclusively in the organic layer of the forest soil. Liming caused a significant decrease in the rate of NO emission by 43 to 100%, whereas irrigation with simulated acid rain increased the emission of NO by a factor of 3.1. Irrigation with simulated normal rain decreased the emission of NO by 35 to 100%. No such effects could be detected for the deposition of NO₂.     

Losses of inorganic carbon and nitrous oxide from a temperate freshwater wetland in relation to nitrate loading

We studied the export of inorganic carbon and nitrous oxide (N₂O) from a Danish freshwater wetland. The wetland is situated in an agricultural catchment area and is recharged by groundwater enriched with nitrate (NO₃ ^–) (1000 M). NO₃ ^– in recharging groundwater was reduced (57.5 mol NO₃ ^– m^–2 yr^–) within a narrow zone of the wetland. Congruently, the annual efflux of carbon dioxide (CO₂) from the sediment was 19.1 mol C m^–2 when estimated from monthly in situ measurements. In comparison the CO₂ efflux was 4.8 mol C m^–2 yr^–1 further out in the wetland, where no NO₃ ^– reduction occurred. Annual exports of inorganic carbon in groundwater and surface water was 78.4 mol C m^–2 and 6.1 mol C m^–2 at the two sites, respectively. N₂O efflux from the sedimenst was detectable on five out of twelve sampling dates and was significantly (P < 0.0001) higher in the NO₃ ^– reduction zone (0.35–9.40 mol m^–2 h^–1, range of monthly means) than in the zone without NO₃ ^– reduction (0.21–0.41 mol m^–2 h^–1). No loss of dissolved N₂O could be measured. Total annual export of N₂O was not estimated. The reduction of oxygen (O₂) in groundwater was minor throughout the wetland and did not exceed 0.2 mol 0₂ m^–2yr^–1. Sulfate (SO₄ ^––) was reduced in groundwater (2.1 mol SO₄ ^–– m^–2 yr^–1) in the zone without NO₃ ^– reduction. Although the NO₃ ^– in our wetland can be reduced along several pathways our results strongly suggest that NO₃ ^– loading of freshwater wetlands disturb the carbon balance of such areas, resulting in an accelerated loss of inorganic carbon in gaseous and dissolved forms.     

Isolation of a highly copper-tolerant yeast, Cryptococcus sp., from the Japan Trench and the induction of superoxide dismutase activity by Cu2+

Thirteen yeast strains were isolated from deep-sea sediment samples collected at a depth of 4500 m to 6500 m in the Japan Trench. Amongst them, strain N6 possessed high tolerance against Cu²⁺ and could grow on yeast extract/peptone/dextrose/agar containing 50 mM CuSO₄. Analysis of the 18S rDNA sequence indicates strain N6 belongs to the genus Cryptococcus. In contrast, the type strain of C. albidus, a typical marine yeast Rhodotorula ingeniosa and Saccharomyces cerevisiae did not grow at high concentrations of CuSO₄. Superoxide dismutase (SOD) catalyzes the scavenging of superoxide radicals. The activity of SOD in cell extract of strain N6 was very weak (<1 mU g^–1 total protein) when the strain was grown in the absence of CuSO₄. However, the activity was stimulated (25.8 mU g^–1 total protein) when cells were grown with 1 mM CuSO₄ and further enhanced to 110 mU g^–1 total protein with 10 mM CuSO₄. Catalase activity was increased only 1.4 or 1.1-fold with 1 mM or 10 mM CuSO₄ in the growth medium, respectively. These results suggest that SOD may have a role in the defensive mechanisms against high concentrations of CuSO₄ in strain N6.     

Hg2+-induced leakage of electrolytes and inhibition of NO3 − utilization inNostoc calcicola

Summary The effect of mercury (Hg²⁺) in the absence and presence of methylmercury (CH₃Hg⁺), cadmium (Cd²⁺), copper (Cu²⁺), nickel (Ni²⁺) and calcium (Ca²⁺) on Nostoc calcicola Bréb. has been studied in terms of electrolyte leakage, NO₃ ^– uptake and in vivo nitrate reductase (NR) activity to discover any possible correlation among such parameters under Hg²⁺ stress. Leakage of electrolytes from Hg²⁺-treated cyanobacterial cells was directly proportional to Hg²⁺ concentrations and exposure time. In comparison to NO₃ ^– uptake, an about 60-fold slower rate of NR activity was observed in the untreated cultures, the former being five times more Hg²⁺-sensitive. A non-competitive synergistic interaction of Hg²⁺ with CH₃Hg⁺ or Cd²⁺ and antagonistic with that of Ni²⁺ or Ca²⁺ has been observed for both the processes of NO₃ ^– utilization. The antagonistic interaction of Cu²⁺ with Hg²⁺ in terms of NO₃ ^– uptake and synergistic with respect to NR activity, has been attributed to the dual bonding preference of Cu²⁺ for cellular ligands. These findings suggest that (a) a statistically significant correlation exists among such parameters; (b) Hg²⁺ predominantly attacks the cyanobacterial cell membrane; (c) Hg²⁺ inhibits NO₃ ^– utilization; (d) the presence of other cations increases or decreases the inhibitory actions of Hg²⁺.     

Exchange of N-gases at the Höglwald Forest – A summary

During 4 years continuous measurements of N-trace gas exchange were carried out at the forest floor-atmosphere interface at the Höglwald Forest that is highly affected by atmospheric N-deposition. The measurements included spruce control, spruce limed and beech sites. Based on these field measurements and on intensive laboratory measurements of N₂-emissions from the soils of the beech and spruce control sites, a total balance of N-gas emissions was calculated. NO₂-deposition was in a range of –1.6 –2.9 kg N ha^–1 yr^–1 and no huge differences between the different sites could be demonstrated. In contrast to NO₂-deposition, NO- and N₂O-emissions showed a huge variability among the different sites. NO emissions were highest at the spruce control site (6.4–9.1 kg N ha^–1 yr^–1), lowest at the beech site (2.3–3.5 kg N ha^–1 yr^–1) and intermediate at the limed spruce site (3.4–5.4 kg N ha^–1 yr^–1). With regard to N₂O-emissions, the following ranking between the sites was found: beech (1.6–6.6 kg N ha^–1 yr^–1) >> spruce limed (0.7–4.0 kg N ha^–1 yr^–1) > spruce control (0.4–3.1 kg N ha^–1 yr^–1). Average N-trace gas emissions (NO, NO₂, N₂O) for the years 1994–1997 were 6.8 kg N ha^–1 yr^–1 at the spruce control site, 3.6 kg N ha^–1 yr^–1 at the limed spruce site and 4.5 kg N ha^–1 yr^–1 at the beech site. Considering N₂-losses, which were significantly higher at the beech (12.4 kg N ha^–1 yr^–1) than at the spruce control site (7.2 kg N ha^–1 yr^–1), the magnitude of total gaseous N losses, i.e. N₂-N + NO-N + NO₂-N + N₂O-N, could be calculated for the first time for a forest ecosystem. Total gaseous N-losses were 14.0 kg N ha^–1 yr^–1 at the spruce control site and 15.5 kg N ha^–1 yr^–1 at the beech site, respectively. In view of the huge interannual variability of N-trace gas fluxes and the pronounced site differences in N-gas emissions it is concluded that more research is needed in order to fully understand patterns of microbial N-cycling and N-gas production/emission in forest ecosystems and mechanisms of reactions of forest ecosystems to the ecological stress factor of atmospheric N-input.     

Inhibitory effects of copper on bacteria related to the free ion concentration

Cu²⁺ ion determinations were carried out in complex and in inorganic salts-glycerol media, to which increasing amounts of Cu(II) had been added, with the ion-specific Cu(II)-Selectrode. Likewise, complexing capacity of bacterial suspensions was estimated by titration with CuSO₄.Copper-sensitive bacteria, e.g.,Klebsiella aerogenes, were inhibited in their growth and survival in the range of 10^–8–10^–6 M Cu²⁺ ion concentrations. In copper-buffered complex media, high copper loads could be tolerated, as growth proceeded with most of the copper bound to medium components. In low-complexing mineral salts media, in which high Cu²⁺ ion concentrations exist at low copper loads, there was competition of Cu²⁺ for binding sites of the cells. Total allowed copper was then determined by the ratio of copper to biomass.Copper-resistant bacteria could be isolated from a stock solution of CuSO₄, containing 100 ppm Cu(II). They were of thePseudomonas type and showed a much higher tolerance towards Cu²⁺, up to 10^–3 M.     

Influence of cis-[Re2GABA2Cl4]Cl2 on the antioxidant defense system parameters of normal human blood

The effect of the rhenium complex cis-[Re₂GABA₂Cl₄]Cl₂ on the antioxidant parameters of normal human blood in vitro have been studied. The results suggest that the complex influences various enzymes in the cascade of reactions utilizing active oxygen metabolites. However, the manifestation of this activity varies over the studied concentration range of the complex in the preincubation medium (10^–12-10^–4 M), so the effects appear to be concentration-dependent. The largest differences in antioxidant parameters in comparison with control were observed for the concentrations 10^–8, 10^–5, and 10^–4 M. Thus, correlations between the peroxidation level, superoxide dismutase (SOD) activity, antioxidant factor (F), and indexes of resistance of erythrocytes for hemolysis (TR) were found.     

Denitrification in a seashore sandy deposit influenced by groundwater discharge

The chemical compositions of ground water and organic matter in sediments were investigated at a sandy shore of Tokyo Bay, Japan to determine the fate of ground water NO₃ ^–. On the basis of Cl^– distribution in ground water, the beach was classified into freshwater (FR)-, transition (TR)-, and seawater (SW)-zones from the land toward the shoreline. The NO₃ ^– and N₂O did not behave conservatively with respect to Cl^– during subsurface mixing of freshwater and seawater, suggesting NO₃ ^– consumption and N₂O production in the TR-zone. Absence of beach vegetation indicated that NO₃ ^– assimilation by higher plants was not as important as NO₃ ^– sink. Low NH₄ ⁺ concentrations in ground water revealed little reduction of NO₃ ^– to NH₄ ⁺. These facts implied that microbial denitrification and assimilation were the likely sinks for ground water NO₃ ^–. The potential activity and number of denitrifiers in water-saturated sediment were highest in the low-chlorinity part of the TR-zone. The location of the highest potential denitrification activity (DN-zone) overlapped with that of the highest NO₃ ^– concentration. The C/N ratio and carbon isotope ratio (¹³C) of organic matter in sediment (< 100 -m) varied from 12.0 to 22.5 and from –22.5 to –25.5, respectively. The ¹³C value was inversely related to the C/N ratio (r ² = 0.968, n = 11), which was explained by the mixing of organic matters of terrestrial and marine origins. In the DN-zone, the fine sediments were rich in organic matters with high C/N ratios and low ¹³C values, implying that dissolved organic matters of terrestrial origin might have been immobilized under slightly saline conditions. A concurrent supply of NO₃ ^– and organic matter to the TR-zone by ground water discharge probably generates favorable conditions for denitrifiers. Ground water NO₃ ^– discharged to the beach is thus partially denitrified and fixed as microbial biomass before it enters the sea. Further studies are necessary to determine the relative contribution of these processes for NO₃ ^– removal.     

Chemiluminescence Assays of Cu2Zn2 Superoxide Dismutase Mimicking Cu-Complexes

The aqueous decay of K₃CrO₈ was used to compare the reactivity of Cu₂Zn₂ superoxide dismutase and two active centre analogues where the first shell atoms around the copper are four unsaturated nitrogens. Unlike the acetate or biuret type Cu(II) chelates these di-Schiff-base complexes had an identical reactivity compared to that of the intact enzyme. Nanomolar concentrations of copper coordinated in these complexes were sufficient to inhibit the K₃CrO₈ induced chemiluminescence by 50%.

Furthermore, a lucigenin amplified chemiluminescence assay based on isolated polymorph nuclear leucocytes in the absence and presence of whole, unseparated blood was developed and successfully employed. CuPu(Im), and CuPu(Py), equivalent to 0.5 and 0.8 SOD units. only, were required to inhibit the photon emission by 50% in the absence of bovine serum albumin. Even in the presence of 600 μM albumin mimicking the competitive copper chelation in biological fluids Cu-Pu(Py)₂ and CuPu(lm)₂ remained active, whereas the carboxylate-and biuret type chelates Cu(Sal)₂ and Cu(Ser)₂ reacted like CuSO₄ The same reactivity of these low M, SOD mimics was seen in human blood.     

Ca2+ and Cu2+ supplementation augments vancomycin production by Amycolatopsis orientalis

Supplementation with CaCl₂2H₂O (40 mg l^–1) or CuSO₄5H₂O (10 mg l^–1) improved vancomycin production by Amycolatopsis orientalis by 12 and 11%, respectively; used in combination, they acted synergistically. Ca²⁺ decreased the intracellular concentration of vancomycin 36%, whereas Cu²⁺ increased the intracellular activity of TDP-glucose:aglycosylvancomycin glucosyltransferase 3 times more than control. Ca²⁺ probably works by altering the permeability of cells to vancomycin, whereas Cu²⁺ increases the activity of an enzyme responsible for vancomycin biosynthesis.     

The mechanism of nitrate transport across the tonoplast of barley root cells

Nitrate-selective microelectrodes were used to measure not only nitrate activity in the cytoplasm and vacuole of barley (Hordeum vulgare L.) root cells, but also the tonoplast electrical membrane potential. For epidermal cells, the mean cytoplasmic and vacuolar pNO₃ (-log₁₀ [NO₃]) values were 2.3±0.04 (n=19) and 1.41±0.03 (n=35), respectively, while for cortical cells, the mean cytoplasmic and vacuolar nitrate values were 2.58±0.18 (n=4) and 1.17±0.06 (n=13), respectively. These results indicate that the accumulation of nitrate in the vacuole must be an active process. Proton-selective microelectrodes were used to measure the proton gradient across the tonoplast to assess the possibility that nitrate transport into the vacuole is mediated by an H⁺/NO ₃ ^– antiport mechanism. For epidermal cells, the mean cytoplasmic and vacuolar pH values were 7.12±0.06 (n=10) and 4.93±0.11 (n=22), respectively, while for cortical cells, the mean cytoplasmic and vacuolar pH values were 7.24±0.07 (n=3) and 5.09±0.17 (n=7), respectively. Calculations of the energetics for this mechanism indicate that the observed gradient of nitrate across the tonoplast of both epidermal and cortical cells could be achieved by an H⁺/NO ₃ ^– antiport with a 11 stoichiometry.Abbreviations and Symbols G/F free-energy change for H⁺/NO ₃ ^– antiport - F Faraday constant - pH_c cytoplasmic pH - pH_v vacuolar pH - p[NO₃]_c log₁₀ (cytoplasmic [NO ₃ ^– ]) - P[NO₃]_v -log₁₀ (vacuolar [NO₃]) We wish to thank Dr. K. Moore for assistance with statistical analysis.     

Nitrate and chloride ions have different permeation pathways in skeletal muscle fibers ofRana pipiens

Summary The effects of pH on the permeability and conductance of the membranes to nitrate and to chloride of semitendinosus and lumbricalis muscle fibers were examined.Membrane potential responses to quick solution changes were recorded in semitendinosus fibers initially equilibrated in isotonic, high K₂SO₄ solutions. External solutions were first changed to ones in which either Rb⁺ or Cs⁺ replaced K⁺ and then to solutions containing either NO ₃ ^– or Cl^– to replace SO ₄ ^2– . The hyperpolarizations produced by Cl^– depend on external pH, being smaller in acid than in alkaline solutions. By contrast, hyperpolarizations produced by NO ₃ ^– were independent of external pH over a pH range from 5.5 to 9.0.In addition, voltage-clamp measurements were made on short lumbricalis muscle fibers. Initially they were equilibrated in isotonic solutions containing mainly K₂SO₄ plus Na₂SO₄. KCl or KNO₃ were added to the sulfate solutions and the fibers were equilibrated in these new solutions. When finally equilibrated the fibers had the same volume they had in the sulfate solutions before the additions. Constant hyperpolarizing voltage pulses of 0.6-sec duration were applied when all external K⁺ was replaced by TEA⁺. For these conditions, inward currents flowing during the voltage pulses were largely carried by Cl^– or NO ₃ ^– depending on the final equilibrating solution. Cl^– currents during voltage pulses were both external pH and time dependent. By contrast, NO ₃ ^– currents were independent of both external pH and time.The voltage dependence of NO ₃ ^– currents could be fit by constant field equations with aP _{NO 3} of 3.7·10^–6 cm/sec. The voltage dependence of the initial or instantaneous Cl^– currents at pH 7.5 and 9.0 could also be fit by constant field equations with P_Cl of 5.8·10^–6 and 7.9·10^–6 cm/sec, respectively. At pH 5.0, no measurable instantaneous Cl^– currents were found.From these results we conclude that NO ₃ ^– does not pass through the pH, time-dependent Cl^– channels but rather passes through a distinct set of channels. Furthermore, Cl^– ions do not appear to pass through the channels which allow NO ₃ ^– through. Consequently, the measured ratio ofP _Cl/P _{NO 3} based on membrane potential changes to ionic changes made on intact skeletal muscle fibers is not a measure of the selectivity of a single anion channel but rather is a measure of the relative amounts of different channel types.     

Effects of Zn2+ and Cu2+ on growth,lignin degradation and ligninolytic enzymes in Phanerochaete chrysosporium

The influence of Zn²⁺ (6.0 × 10^–3 –18.0 × 10^–3 M) and Cu²⁺ (4 × 10^–4 –1.2 × 10^–4 M) in the basal medium on mycelial growth (dry weight), activities of lignin peroxidase (Lip), manganese peroxidase (Mnp), solubilization, and mineralization (¹⁴CO₂ evolution) of lignin during a period of 3 weeks was studied in Phanerochaete chrysosporium strain MTCC-787. Highest mycelial growth was obtained at 0.6 M Zn²⁺ and 0.4 M Cu²⁺ levels. Enzyme activities were found to increase up to the highest levels of both the trace elements. However, Zn²⁺ had a relatively more stimulatory effect on Lip production and the reverse was true in case of Cu²⁺. [¹⁴C]Lignin solubilization was also promoted by higher levels of both trace elements. Mineralization of [¹⁴C]lignin was optimal at 6.0 M Zn²⁺ and 1.2 M Cu²⁺. The stimulatory effect of Zn²⁺ on Lip production was correlated with higher rates of [¹⁴C]lignin mineralization.     

Effects of defoliation and atmospheric CO2 depletion on nitrate acquisition,and exudation of organic compounds by roots of Festuca rubra

The aim of this study was to investigate the physiological basis of increased root exudation from Festuca rubra, in response to defoliation. The hypothesis, that assimilate supply to roots is a key determinant of the response of root exudation to defoliation was tested by imposing CO₂-deplete (< 50 mol mol^–1) atmospheres to F. rubra. This was done as a non-destructive means of preventing supply of new assimilate to roots of intact and defoliated plants. F. rubra was grown in axenic sand systems, with defoliation and CO₂-depletion treatments applied to plants at 14 and 35 days after planting. Root exudation and NO₃ ^– uptake were quantified throughout, and post-treatment uptake and allocation of N were determined from the distribution of ¹⁵N label, supplied as ¹⁵NO₃ ^–. Defoliation of F. rubra resulted in significantly (P <0.01) increased root exudation, CO₂-depletion did not result in increased exudation from plants of either age. When treatments were applied to F. rubra after 14 days, defoliation and CO₂-depletion each reduced NO₃ ^– uptake significantly (P <0.05). However, in older plants, uptake of NO₃ ^– was less sensitive to defoliation and CO₂-depletion. The results indicate that increased root exudation following defoliation is not related directly to reduced assimilate supply to roots. This was evident from the lack of effect of CO₂-depletion on root exudation, and the absence of correlation between root-C efflux and the rate of NO₃ ^– uptake. The physiological basis of increased exudation following defoliation remains uncertain, but may be dependent on physical damage, either directly or as a consequence of systemic responses to wounding.     

Leaf cavity CO2 concentrations and CO2 exchange in onion,Allium cepa L.

Onion (Allium cepa L.) plants were examined to determine the photosynthetic role of CO₂ that accumulates within their leaf cavities. Leaf cavity CO₂ concentrations ranged from 2250 L L^–1 near the leaf base to below atmospheric (<350 L L^–1) near the leaf tip at midday. There was a daily fluctuation in the leaf cavity CO₂ concentrations with minimum values near midday and maximum values at night. Conductance to CO₂ from the leaf cavity ranged from 24 to 202 mol m^–2 s^–1 and was even lower for membranes of bulb scales. The capacity for onion leaves to recycle leaf cavity CO₂ was poor, only 0.2 to 2.2% of leaf photosynthesis based either on measured CO₂ concentrations and conductance values or as measured directly by ¹⁴CO₂ labeling experiments. The photosynthetic responses to CO₂ and O₂ were measured to determine whether onion leaves exhibited a typical C₃-type response. A linear increase in CO₂ uptake was observed in intact leaves up to 315 L L^–1 of external CO₂ and, at this external CO₂ concentration, uptake was inhibited 35.4±0.9% by 210 mL L^–1 O₂ compared to 20 mL L^–1 O₂. Scanning electron micrographs of the leaf cavity wall revealed degenerated tissue covered by a membrane. Onion leaf cavity membranes apparently are highly impermeable to CO₂ and greatly restrict the refixation of leaf cavity CO₂ by photosynthetic tissue.Abbreviations C_a external CO₂ concentration - C_i intercellular CO₂ concentration - CO₂ compensation concentration - PPFR photosynthetic photon fluence rate     

Quantification of N2-fixation and survival of inoculated diazotrophs associated with roots of Kallar grass

White clover plants were grown for 97 days under two temperature regimes (20/15°C and 8/5°C day/night temperatures) and were supplied with either small amounts (a total of 80 mg N pot^–1) of ammonium (NH ₄ ⁺ ) or nitrate (NO ₃ ^– ) nitrogen, or received no mineral N and relied on N₂ fixation. Greatest growth and total leaf area of clover plants occurred in N₂ fixing and NO ₃ ^– -fed plants grown at 20/15°C and poorest growth occurred in NH ₄ ⁺ -fed plants grown at 8/5°C. Nodule mass per plant was greater at 8/5°C due to increased nodule numbers rather than increased dry weight per nodule. This compensated to some extent for the reduced N₂-fixing activity per unit dry weight of nodule tissue found at the low growth temperature up to 116 d after sowing, but thereafter both activity per nodule dry weight and activity per plant were greater at the low temperature. Highest nitrate reductase activity (NRA) per g fresh weight and total activity per leaf, petiole or root occurred in NO ₃ ^– -fed plants at 8/5°C. Low growth temperature resulted in a greater partitioning of total plant NRA to the roots of NO ₃ ^– -fed plants. The results are considered in relation to the use of N fertiliser in the spring under field conditions.