Lignocellulosic polysaccharides and lignin degradation by wood decay fungi: the relevance of nonenzymatic Fenton-based reactions

The brown rot fungus Wolfiporia cocos and the selective white rot fungus Perenniporia medulla-panis produce peptides and phenolate-derivative compounds as low molecular weight Fe³⁺-reductants. Phenolates were the major compounds with Fe³⁺-reducing activity in both fungi and displayed Fe³⁺-reducing activity at pH 2.0 and 4.5 in the absence and presence of oxalic acid. The chemical structures of these compounds were identified. Together with Fe³⁺ and H₂O₂ (mediated Fenton reaction) they produced oxygen radicals that oxidized lignocellulosic polysaccharides and lignin extensively in vitro under conditions similar to those found in vivo. These results indicate that, in addition to the extensively studied Gloeophyllum trabeum—a model brown rot fungus—other brown rot fungi as well as selective white rot fungi, possess the means to promote Fenton chemistry to degrade cellulose and hemicellulose, and to modify lignin. Moreover, new information is provided, particularly regarding how lignin is attacked, and either repolymerized or solubilized depending on the type of fungal attack, and suggests a new pathway for selective white rot degradation of wood. The importance of Fenton reactions mediated by phenolates operating separately or synergistically with carbohydrate-degrading enzymes in brown rot fungi, and lignin-modifying enzymes in white rot fungi is discussed. This research improves our understanding of natural processes in carbon cycling in the environment, which may enable the exploration of novel methods for bioconversion of lignocellulose in the production of biofuels or polymers, in addition to the development of new and better ways to protect wood from degradation by microorganisms.     

Degradation of 14C-labelled lignin and dehydropolymer of coniferyl alcohol by ericoid and ectomycorrhizal fungi

The ability of ericoid and ectomycorrhizal fungi to utilize ¹⁴C-labelled lignin and O¹⁴CH₃-labelled dehydropolymer of coniferyl alcohol as sole C sources has been assessed in pure culture studies. The results indicate that ericoid mycorrhizal fungi are more effective in degrading lignin than ectomycorrhizal fungi. Amongst the ectomycorrhizal fungi the facultative mycorrhizal fungus Paxillus involutus degraded lignin more readily than those which are normally considered to be obligately mycorrhizal fungi such as Suillus bovinus and Rhizopogon roseolus. The importance of these lignin degrading capabilities is discussed in relation to the predominance of specific mycorrhiza forms along a gradient of increasing organic matter and hence lignin content of soil.     

Pathways for Extracellular Fenton Chemistry in the Brown Rot Basidiomycete Gloeophyllum trabeum

The brown rot fungus Gloeophyllum trabeum uses an extracellular hydroquinone-quinone redox cycle to reduce Fe³⁺ and produce H₂O₂. These reactions generate extracellular Fenton reagent, which enables G. trabeum to degrade a wide variety of organic compounds. We found that G. trabeum secreted two quinones, 2,5-dimethoxy-1,4-benzoquinone (2,5-DMBQ) and 4,5-dimethoxy-1,2-benzoquinone (4,5-DMBQ), that underwent iron-dependent redox cycling. Experiments that monitored the iron- and quinone-dependent cleavage of polyethylene glycol by G. trabeum showed that 2,5-DMBQ was more effective than 4,5-DMBQ in supporting extracellular Fenton chemistry. Two factors contributed to this result. First, G. trabeum reduced 2,5-DMBQ to 2,5-dimethoxyhydroquinone (2,5-DMHQ) much more rapidly than it reduced 4,5-DMBQ to 4,5-dimethoxycatechol (4,5-DMC). Second, although both hydroquinones reduced ferric oxalate complexes, the predominant form of Fe³⁺ in G. trabeum cultures, the 2,5-DMHQ-dependent reaction reduced O₂ more rapidly than the 4,5-DMC-dependent reaction. Nevertheless, both hydroquinones probably contribute to the extracellular Fenton chemistry of G. trabeum, because 2,5-DMHQ by itself is an efficient reductant of 4,5-DMBQ.     

Linoleic acid peroxidation initiated by Fe-reducing compounds recovered from Eucalyptus grandis biotreated with Ceriporiopsis subvermispora

This work evaluates linoleic acid peroxidation reactions initiated by Fe³⁺-reducing compounds recovered from Eucalyptus grandis, biotreated with the biopulping fungus Ceriporiopsis subvermispora. The aqueous extracts from biotreated wood had the ability to reduce Fe³⁺ ions from freshly prepared solutions. The compounds responsible for the Fe³⁺-reducing activity corresponded to UV-absorbing substances with apparent molar masses from 3 kDa to 5 kDa. Linoleic acid peroxidation reactions conducted in the presence of Fe³⁺ ions and the Fe³⁺-reducing compounds showed that the rate of O₂ consumption during peroxidation was proportional to the Fe³⁺-reducing activity present in each extract obtained from biotreated wood. This peroxidation reaction was coupled with in-vitro treatment of ball-milled E. grandis wood. Ultraviolet data showed that the reaction system released lignin fragments from the milled wood. Size exclusion chromatography data indicated that the solubilized material contained a minor fraction representing high-molar-mass molecules excluded by the column and a main low-molar-mass peak. Overall evaluation of the data suggested that the Fe³⁺-reducing compounds formed during wood biodegradation by C. subvermispora can mediate lignin degradation through linoleic acid peroxidation.     

First evidences that the ectomycorrhizal fungus Paxillus involutus mobilizes nitrogen and carbon from saprotrophic fungus necromass

Fungal succession in rotting wood shows a surprising abundance of ectomycorrhizal (EM) fungi during the late decomposition stages. To better understand the links between EM fungi and saprotrophic fungi, we investigated the potential capacities of the EM fungus Paxillus involutus to mobilize nutrients from necromass of Postia placenta, a wood rot fungus, and to transfer these elements to its host tree. In this aim, we used pure cultures of P. involutus in the presence of labelled Postia necromass (¹⁵N/¹³C) as nutrient source, and a monoxenic mycorrhized pine experiment composed of labelled Postia necromass and P. involutus culture in interaction with pine seedlings. The isotopic labelling was measured in both experiments. In pure culture, P. involutus was able to mobilize N, but C as well, from the Postia necromass. In the symbiotic interaction experiment, we measured high ¹⁵N enrichments in all plant and fungal compartments. Interestingly, ¹³C remains mainly in the mycelium and mycorrhizas, demonstrating that the EM fungus transferred essentially N from the necromass to the tree. These observations reveal that fungal organic matter could represent a significant N source for EM fungi and trees, but also a C source for mycorrhizal fungi, including in symbiotic lifestyle.     

In vitro weathering of phlogopite by ectomycorrhizal fungi

The ways in which ectomycorrhizal fungi benefit tree growth and nutrition have not been fully elucidated. Whilst it is most probably due to improved soil colonization, it is also likely that ectomycorrhizal fungi could be directly involved in nutrient cycling of soil reserves. This study assessed access by two species of ectomycorrhizal fungi to soil nonexchangeable K⁺ reserves. The incubation of ectomycorrhizal fungi in bi-compartment Petri dishes with phlogopite led to cation exchange reactions and to crystal lattice weathering. Paxillus involutus COU led to irreversible phlogopite transformations, while Pisolithus tinctorius 441 led to reversible ones. Simultaneous depletion in K⁺ and Mg²⁺ led to an enhanced weathering of phlogopite by P. tinctorius 441. The observation of phlogopite evolution shows that some specific Al³⁺ immobilization occurred under P. tinctorius 441. The data suggest that these bio-weathering mechanisms could be related to the release of fungal organic acids or other complex forming molecules.     

In vitro anti- and pro-oxidative effects of natural polyphenols

The anti- and pro-oxidative effects of phenolic compounds and antioxidants were studied in two different in vitro model systems utilizing ethyl linoleate and 2′-deoxyguanosine (2′-dG) as oxidative substrates, and a Fenton reaction (H₂O₂, Fe²⁺) to initiate oxidation. Oxidation of the biomolecules in both model systems exhibited dose dependency. In the 2′-dG assay, oxidation was closely related to H₂O₂ generation, which occurred during autoxidation of the phenolics. Hydroxylating activity was greatly enhanced by Mn²⁺ and Cu²⁺, but not by Zn²⁺ or Co²⁺. Ethyl linoleate peroxidation was inhibited by low concentrations of catechol, quercitin, and instant coffee. However, peroxidation was promoted by high concentrations of the same compounds, probably by recycling of chelated inactive Fe³⁺ to the active Fe²⁺ state.     

Mechanisms of Saccharomyces Cerevisiae PMA1 H+-ATPase inactivation by Fe2+, H2O2 and Fenton reagents

Although considerably more oxidation-resistant than other P-type ATPases, the yeast PMA1 H⁺-ATPase of Saccharomyces cerevisiae SY4 secretory vesicles was inactivated by H₂O₂, Fe²⁺, Fe- and Cu-Fenton reagents. Inactivation by Fe²⁺ required the presence of oxygen and hence involved auto-oxidation of Fe²⁺ to Fe³⁺. The highest Fe^2- (100 μM) and H₂O₂ (100 mM) concentrations used produced about the same effect. Inactivation by the Fenton reagent depended more on Fe²⁺ content than on H₂O₂ concentration, occurred only when Fe²⁺ was added to the vesicles first and was only slightly reduced by scavengers (mannitol, Tris, NaN₃, DMSO) and by chelators (EDTA, EGTA, DTPA, BPDs, bipyridine, 1, 10-phenanthroline). Inactivation by Fe- and Cu- Fenton reagent was the same; the identical inactivation pattern found for both reagents under anaerobic conditions showed that both reagents act via OH^·. The lipid peroxidation blocker BHT prevented Fenton-induced rise in lipid peroxidation in both whole cells and in isolated membrane lipids but did not protect the H⁺-ATPase in secretory vesicles against inactivation. ATP partially protected the enzyme against peroxide and the Fenton reagent in a way resembling the protection it afforded against SH-specific agents. The results indicate that Fe²⁺ and the Fenton reagent act via metal-catalyzed oxidation at specific metal-binding sites, very probably SH-containing amino acid residues. Deferrioxamine, which prevents the redox cycling of Fe²⁺, blocked H⁺-ATPase inactivation by Fe²⁺ and the Fenton reagent but not that caused by H₂O₂, which therefore seems to involve a direct non-radical attack. Fe-Fenton reagent caused fragmentation of the H⁺-ATPase molecule, which, in Western blots, did not give rise to defined fragments bands but merely to smears.     

Ectomycorrhizal Fungal Protein Degradation Ability Predicted by Soil Organic Nitrogen Availability

In temperate and boreal forest ecosystems, nitrogen (N) limitation of tree metabolism is alleviated by ectomycorrhizal (ECM) fungi. As forest soils age, the primary source of N in soil switches from inorganic (NH₄⁺ and NO₃⁻) to organic (mostly proteins). It has been hypothesized that ECM fungi adapt to the most common N source in their environment, which implies that fungi growing in older forests would have greater protein degradation abilities. Moreover, recent results for a model ECM fungal species suggest that organic N uptake requires a glucose supply. To test the generality of these hypotheses, we screened 55 strains of 13 Suillus species with different ecological preferences for their in vitro protein degradation abilities. Suillus species preferentially occurring in mature forests, where soil contains more organic matter, had significantly higher protease activity than those from young forests with low-organic-matter soils or species indifferent to forest age. Within species, the protease activities of ecotypes from soils with high or low soil organic N content did not differ significantly, suggesting resource partitioning between mineral and organic soil layers. The secreted protease mixtures were strongly dominated by aspartic peptidases. Glucose addition had variable effects on secreted protease activity; in some species, it triggered activity, but in others, activity was repressed at high concentrations. Collectively, our results indicate that protease activity, a key ectomycorrhizal functional trait, is positively related to environmental N source availability but is also influenced by additional factors, such as carbon availability.     

The lactate-dependent enhancement of hydroxyl radical generation by the Fenton reaction

The effect of lactic acid (lactate) on Fenton based hydroxyl radical (^·OH) production was studied by spin trapping, ESR, and fluorescence methods using DMPO and coumarin-3-carboxylic acid (3-CCA) as the ^·OH traps respectively. The ^·OH adduct formation was inhibited by lactate up to 0.4mM (lactate/iron stoichiometry = 2) in both experiments, but markedly enhanced with increasing concentrations of lactate above this critical concentration. When the H₂O₂ dependence was examined, the DMPO-OH signal was increased linearly with H₂O₂ concentration up to 1 mM and then saturated in the absence of lactate. In the presence of lactate, however, the DMPO-OH signal was increased further with higher H₂O₂ concentration than 1 mM, and the saturation level was also increased dependent on lactate concentration. Spectroscopic studies revealed that lactate forms a stable colored complex with Fe³⁺ at lactate/Fe³⁺ stoichiometry of 2, and the complex formation was strictly related to the DMPO-OH formation. The complex formation did not promote the H₂O₂ mediated Fe³⁺ reduction. When the Fe³⁺-lactate (1:2) complex was reacted with H₂O₂, the initial rate of hydroxylated 3-CCA formation was linearly increased with H₂O₂ concentrations. All the data obtained in the present experiments suggested that the Fe³⁺-lactate (1:2) complex formed in the Fenton reaction system reacts directly with H₂O₂ to produce additional ^·OH in the Fenton reaction by other mechanisms than lactate or lactate/Fe³⁺ mediated promotion of Fe³⁺/Fe²⁺ redox cycling.     

Removal of H₂O₂ and generation of superoxide radical: role of cytochrome c and NADH

In cells, mitochondria, endoplasmic reticulum, and peroxisomes are the major sources of reactive oxygen species (ROS) under physiological and pathophysiological conditions. Cytochrome c (cyt c) is known to participate in mitochondrial electron transport and has antioxidant and peroxidase activities. Under oxidative or nitrative stress, the peroxidase activity of Fe³⁺cyt c is increased. The level of NADH is also increased under pathophysiological conditions such as ischemia and diabetes and a concurrent increase in hydrogen peroxide (H₂O₂) production occurs. Studies were performed to understand the related mechanisms of radical generation and NADH oxidation by Fe³⁺cyt c in the presence of H₂O₂. Electron paramagnetic resonance (EPR) spin trapping studies using 5,5-dimethyl-1-pyrroline-N-oxide (DMPO) were performed with NADH, Fe³⁺cyt c, and H₂O₂ in the presence of methyl-β-cyclodextrin. An EPR spectrum corresponding to the superoxide radical adduct of DMPO encapsulated in methyl-β-cyclodextrin was obtained. This EPR signal was quenched by the addition of the superoxide scavenging enzyme Cu,Zn-superoxide dismutase (SOD1). The amount of superoxide radical adduct formed from the oxidation of NADH by the peroxidase activity of Fe³⁺cyt c increased with NADH and H₂O₂ concentration. From these results, we propose a mechanism in which the peroxidase activity of Fe³⁺cyt c oxidizes NADH to NAD^•, which in turn donates an electron to O₂, resulting in superoxide radical formation. A UV-visible spectroscopic study shows that Fe³⁺cyt c is reduced in the presence of both NADH and H₂O₂. Our results suggest that Fe³⁺cyt c could have a novel role in the deleterious effects of ischemia/reperfusion and diabetes due to increased production of superoxide radical. In addition, Fe³⁺cyt c may play a key role in the mitochondrial “ROS-induced ROS-release” signaling and in mitochondrial and cellular injury/death. The increased oxidation of NADH and generation of superoxide radical by this mechanism may have implications for the regulation of apoptotic cell death, endothelial dysfunction, and neurological diseases. We also propose an alternative electron transfer pathway, which may protect mitochondria and mitochondrial proteins from oxidative damage.     

Electron acceptor availability alters carbon and energy metabolism in a thermoacidophile

The thermoacidophilic Acidianus strain DS80 displays versatility in its energy metabolism and can grow autotrophically and heterotrophically with elemental sulfur (S°), ferric iron (Fe³⁺) or oxygen (O₂) as electron acceptors. Here, we show that autotrophic and heterotrophic growth with S° as the electron acceptor is obligately dependent on hydrogen (H₂) as electron donor; organic substrates such as acetate can only serve as a carbon source. In contrast, organic substrates such as acetate can serve as electron donor and carbon source for Fe³⁺ or O₂ grown cells. During growth on S° or Fe³⁺ with H₂ as an electron donor, the amount of CO₂ assimilated into biomass decreased when cultures were provided with acetate. The addition of CO₂ to cultures decreased the amount of acetate mineralized and assimilated and increased cell production in H₂/Fe³⁺ grown cells but had no effect on H₂/S° grown cells. In acetate/Fe³⁺ grown cells, the presence of H₂ decreased the amount of acetate mineralized as CO₂ in cultures compared to those without H₂. These results indicate that electron acceptor availability constrains the variety of carbon sources used by this strain. Addition of H₂ to cultures overcomes this limitation and alters heterotrophic metabolism.     

N concentration controls decomposition rates of different strains of ectomycorrhizal fungi

The decomposition of soil organic matter in forest ecosystems is important in two ways. First, soil organic matter is the largest pool of C in terrestrial ecosystems, so understanding global carbon cycling requires an appreciation of the factors that control the size of that pool and the fluxes through it. Among these factors are those that control the rate of organic matter decomposition. Second, organic matter decomposition is the major process controlling the supply of nutrients to plants. In some ecosystems ectomycorrhizal fungi comprise a surprisingly large fraction of soil organic matter. However, little is known of the rates of decomposition of ectomycorrhizal fungi, or of the factors that control those rates. Therefore, we set out to examine the relationship between N concentrations and decomposition rates of ectomycorrhizal fungi using a wide variety of strains isolated from a Pinus resinosa plantation. We found that substantial variation among strains existed in decomposition rate, and that decomposition rate was highly correlated with tissue N concentration. We conclude, therefore, that the structures of ectomycorrhizal fungal communities may be ecologically important in terms of ecosystem C and N dynamics.     

Inactivation of the plasma membrane ATPase ofSchizosaccharomyces pombe by hydrogen peroxide and by the fenton reagent (Fe2+/H2O2): Nonradicalvs. Radical-induced oxidation

In the absence of added Fe²⁺, the ATPase activity of isolatedSchizosaccharomyces pombe plasma membranes (5–7 μmolP _i per mg protein per min) is moderately inhibited by H₂O₂ in a concentration-dependent manner. Sizable inactivation occurs only at 50–80 mmol/L H₂O₂. The process, probably a direct oxidative action of H₂O₂ on the enzyme, is not induced by the indigenous membrane-bound iron (19.3 nmol/mg membrane protein), is not affected by the radical scavengers mannitol and Tris, and involves a decrease of both theK _m of the enzyme for ATP and theV of ATP splitting. On exposing the membranes to the Fenton reagent (50 μmol/L Fe²⁺ +20 mmol/L H₂O₂), which causes a fast production of HO⁻ radicals, the ATPase is 50–60% inactivated and 90% of added Fe²⁺ is oxidized to Fe³⁺ within 1 min. The inactivation occurs only when Fe²⁺ is added before H₂O₂ and can thus bind to the membranes. The lack of effect of radical scavengers (mannitol, Tris) indicates that HO⁻ radicals produced in the bulk phase play no role in inactivation. Blockage of the inactivation by the iron chelator deferrioxamine implies that the process requires the presence of Fe²⁺ ions bound to binding sites on the enzyme molecules. Added catalase, which competes with Fe²⁺ for H₂O₂, slows down the inactivation but in some cases increases its total extent, probably due to the formation of the superoxide radical that gives rise to delayed HO⁻ production.     

Induction of Extracellular Hydroxyl Radical Production by White-Rot Fungi through Quinone Redox Cycling

A simple strategy for the induction of extracellular hydroxyl radical (OH) production by white-rot fungi is presented. It involves the incubation of mycelium with quinones and Fe³⁺-EDTA. Succinctly, it is based on the establishment of a quinone redox cycle catalyzed by cell-bound dehydrogenase activities and the ligninolytic enzymes (laccase and peroxidases). The semiquinone intermediate produced by the ligninolytic enzymes drives OH production by a Fenton reaction (H₂O₂ + Fe²⁺ → OH + OH⁻ + Fe³⁺). H₂O₂ production, Fe³⁺ reduction, and OH generation were initially demonstrated with two Pleurotus eryngii mycelia (one producing laccase and versatile peroxidase and the other producing just laccase) and four quinones, 1,4-benzoquinone (BQ), 2-methoxy-1,4-benzoquinone (MBQ), 2,6-dimethoxy-1,4-benzoquinone (DBQ), and 2-methyl-1,4-naphthoquinone (menadione [MD]). In all cases, OH radicals were linearly produced, with the highest rate obtained with MD, followed by DBQ, MBQ, and BQ. These rates correlated with both H₂O₂ levels and Fe³⁺ reduction rates observed with the four quinones. Between the two P. eryngii mycelia used, the best results were obtained with the one producing only laccase, showing higher OH production rates with added purified enzyme. The strategy was then validated in Bjerkandera adusta, Phanerochaete chrysosporium, Phlebia radiata, Pycnoporus cinnabarinus, and Trametes versicolor, also showing good correlation between OH production rates and the kinds and levels of the ligninolytic enzymes expressed by these fungi. We propose this strategy as a useful tool to study the effects of OH radicals on lignin and organopollutant degradation, as well as to improve the bioremediation potential of white-rot fungi.White-rot fungi are unique in their ability to degrade a wide variety of organopollutants (36, 47), mainly due to the secretion of a low-specificity enzyme system whose natural function is the degradation of lignin (11). Components of this system include laccase and/or one or two types of peroxidase, such as lignin peroxidase (LiP), manganese peroxidase (MnP), and versatile peroxidase (VP) (31). Besides acting directly, the ligninolytic enzymes can bring about lignin and pollutant degradation through the generation of low-molecular-weight extracellular oxidants, including (i) Mn³⁺, (ii) free radicals from some fungal metabolites and lignin depolymerization products (7, 22), and (iii) oxygen free radicals, mainly hydroxyl radicals (OH) and lipid peroxidation radicals (21). Although OH radicals are the strongest oxidants found in cultures of white-rot fungi (1), studies of their involvement in pollutant degradation are scarce. One of the reasons is that the mechanisms proposed for OH production still await in vivo validation.Several potential sources of extracellular OH based on the Fenton reaction (H₂O₂ + Fe²⁺ → OH + OH⁻ + Fe³⁺) have been postulated for white-rot fungi. In one case, an extracellular fungal glycopeptide has been shown to reduce O₂ and Fe³⁺ to H₂O₂ and Fe²⁺ (45). Enzymatic sources include cellobiose dehydrogenase, LiP, and laccase. Among these, only cellobiose dehydrogenase is able to directly catalyze the formation of Fenton''s reagent (33). The ligninolytic enzymes, however, act as an indirect source of OH through the generation of Fe³⁺ and O₂ reductants, such as formate (CO₂⁻) and semiquinone (Q⁻) radicals. The first time evidence was provided that a ligninolytic enzyme was involved in OH production, oxalate was used to generate CO₂⁻ in a LiP reaction mediated by veratryl alcohol (4). The proposed mechanism consisted of the following cascade of reactions: production of veratryl alcohol cation radical (Valc⁺) by LiP, oxidation of oxalate to CO₂⁻ by Valc⁺, reduction of O₂ to O₂⁻ by CO₂⁻, and a superoxide-driven Fenton reaction (Haber-Weiss reaction) in which Fe³⁺ was reduced by O₂⁻. The OH production mechanism assisted by Q⁻ was inferred from the oxidation of 2-methoxy-1,4-benzohydroquinone (MBQH₂) and 2,6-dimethoxy-1,4-benzohydroquinone (DBQH₂) by Pleurotus eryngii laccase in the presence of Fe³⁺-EDTA. The ability of Q⁻ radicals to reduce both Fe³⁺ to Fe²⁺ and O₂ to O₂⁻, which dismutated to H₂O₂, was demonstrated (14). In this case, OH radicals were generated by a semiquinone-driven Fenton reaction, as Q⁻ radicals were the main agents accomplishing Fe³⁺ reduction. The first evidence of the likelihood of this OH production mechanism being operative in vivo had been obtained from incubations of P. eryngii with 2-methyl-1,4-naphthoquinone (menadione [MD]) and Fe³⁺-EDTA (15). Extracellular OH radicals were produced on a constant basis through quinone redox cycling, consisting of the reduction of MD by a cell-bound quinone reductase (QR) system, followed by the extracellular oxidation of the resulting hydroquinone (MDH₂) to its semiquinone radical (MD⁻). The production of extracellular O₂⁻ and H₂O₂ by P. eryngii via redox cycling involving laccase was subsequently confirmed using 1,4-benzoquinone (BQ), 2-methyl-1,4-benzoquinone, and 2,3,5,6-tetramethyl-1,4-benzoquinone (duroquinone), in addition to MD (16). However, the demonstration of OH production based on the redox cycling of quinones other than MD was still required.In the present paper, we describe the induction of extracellular OH production by P. eryngii upon its incubation with BQ, 2-methoxy-1,4-benzoquinone (MBQ), 2,6-dimethoxy-1,4-benzoquinone (DBQ), and MD in the presence of Fe³⁺-EDTA. The three benzoquinones were selected because they are oxidation products of p-hydroxyphenyl, guaiacyl, and syringyl units of lignin (MD was included as a positive control). Along with laccase, the involvement of P. eryngii VP in the production of O₂⁻ and H₂O₂ from hydroquinone oxidation has also been reported (13). Since hydroquinones are substrates of all known ligninolytic enzymes, quinone redox cycling catalysis could involve any of them. Here, we demonstrate OH production by P. eryngii under two different culture conditions, leading to the production of laccase or laccase and VP. We also show that quinone redox cycling is widespread among white-rot fungi by using a series of well-studied species that produce different combinations of ligninolytic enzymes.     

The mechanism of (+) taxifolin’s protective antioxidant effect for •OH-treated bone marrow-derived mesenchymal stem cells

The natural dihydroflavonol (+) taxifolin was investigated for its protective effect on Fenton reagent-treated bone marrow-derived mesenchymal stem cells (bmMSCs). Various antioxidant assays were used to determine the possible mechanism. These included ?OH-scavenging, 2-phenyl-4, 4, 5, 5-tetramethylimidazoline-1-oxyl-3-oxide radical-scavenging (PTIO?-scavenging), 1, 1-diphenyl-2-picryl-hydrazl radical-scavenging (DPPH?-scavenging), 2, 2′-azino-bis (3-ethylbenzo-thiazoline-6-sulfonic acid) radical-scavenging (ABTS⁺?-scavenging), Fe³⁺-reducing, and Cu²⁺-reducing assays. The Fe²⁺-binding reaction was also investigated using UV-Vis spectra. The results revealed that cell viability was fully restored, even increasing to 142.9?±?9.3% after treatment with (+) taxifolin. In the antioxidant assays, (+) taxifolin was observed to efficiently scavenge ?OH, DPPH? and ABTS⁺? radicals, and to increase the relative Cu²⁺- and Fe³⁺-reducing levels. In the PTIO?-scavenging assay, its IC₅₀ values varied with pH. In the Fe²⁺-binding reaction, (+) taxifolin was found to yield a green solution with two UV-Vis absorbance peaks: λ_max =?433 nm (ε =5.2?×?10² L mol^?1 cm ^?1) and λ_max =?721 nm (ε?=?5.1?×?10² L mol^?1 cm ^?1). These results indicate that (+) taxifolin can act as an effective ?OH-scavenger, protecting bmMSCs from ?OH-induced damage. Its ?OH-scavenging action consists of direct and indirect antioxidant effects. Direct antioxidation occurs via multiple pathways, including ET, PCET or HAT. Indirect antioxidation involves binding to Fe²⁺.     

In vitro weathering of phlogopite by ectomycorrhizal fungi

Oxalate accumulation in external medium under hyphal mats of two ectomycorrhizal species is strongly stimulated (1.7 to 35 fold) by a simultaneous depletion of available K⁺ and Mg²⁺. Pisolithus tinctorius strain 441 accumulates oxalate both on NH₄–N and on NO₃–N whereas Paxillus involutus strain COU only accumulates oxalate on NO₃–N. On NO₃–N, under a simultaneous K⁺ and Mg²⁺ deficiency, P. involutus COU is a very active oxalate producer compared to P. tinctorius 441. The present results could explain the various mineralogical evolutions of a phlogopite mica previously recorded under P. involutus COU or P. tinctorius 441 and suggest a key role for fungal oxalic acid during mineral weathering in response to nutrient deficiency.     

Degradation and Mineralization of Phenol Compounds with Goethite Catalyst and Mineralization Prediction Using Artificial Intelligence

The efficiency of phenol degradation via Fenton reaction using mixture of heterogeneous goethite catalyst with homogeneous ferrous ion was analyzed as a function of three independent variables, initial concentration of phenol (60 to 100 mg /L), weight ratio of initial concentration of phenol to that of H₂O₂ (1: 6 to 1: 14) and, weight ratio of initial concentration of goethite catalyst to that of H₂O₂ (1: 0.3 to 1: 0.7). More than 90 % of phenol removal and more than 40% of TOC removal were achieved within 60 minutes of reaction. Two separate models were developed using artificial neural networks to predict degradation percentage by a combination of Fe³⁺ and Fe²⁺ catalyst. Five operational parameters were employed as inputs while phenol degradation and TOC removal were considered as outputs of the developed models. Satisfactory agreement was observed between testing data and the predicted values (R² _Phenol = 0.9214 and R²TOC= 0.9082).     

The influence of pH on OH scavenger inhibition of damage to deoxyribose by Fenton reaction

Summary Hydroxyl radicals (OH') can be formed in aqueous solution by direct reaction of hydrogen peroxide (H₂O₂) with ferrous salt (Fenton reaction). OH' damage to deoxyribose, measured as formation of thiobarbituric acid-reactive material, was evaluated at different pHs to study the mechanism of action of classical OH' scavengers. OH' scavenger effect on Fe²⁺ oxidation was also evaluated in the same experimental conditions. In the absence of OH' scavengers, OH' damage to deoxyribose is higher at acidic compared to neutral and moderately basic pH. At acidic pH deoxiribose is per se able to inhibit Fe²⁺ oxidation by H₂0₂. Most of OH' scavengers tested inhibit deoxyribose damage and Fe²⁺ oxidation in a similar manner: both inhibitions are most relevant at acidic pH and decrease by increasing the pH. These results are not due to OH' scavenger inhibition of Fenton reaction. The influence of pH on the parameters studied appears to be due to the competition of deoxyribose and OH' scavengers for iron. These results suggest the prominent role of iron binding in the degradation of deoxyribose and in the OH' scavenging ability of different compounds. Results obtained with triethylenetetramine, a iron chelator with a low rate constant with OH', confirm that both deoxyribose and the OH' scavengers interact with iron bringing about a site specific Fenton reaction; that the OH' formed at these sites oxidize these molecules to their radical forms which in turn reduce the Fe^3– produced by Fenton reaction. The results presented indicate that most of classical OH' scavengers exert their effect predominantly by preventing the site specific reaction between Fe²⁺ and H₂0₂ on the deoxyribose molecule.