The effect of leaf exudates on the spore germination of phylloplane mycoflora of chilli (Capsicum annuum L.) cultivars

Summary Ninetten aminoacids, twelve sugars, eleven organic acids and ten phenols were detected in the leaf exudates of three cultivars of chilli. The number of aminoacids, sugars, organic acids and phenols increased as the plants grew older. More aminoacids and sugars were detected in the exudate from the susceptible cultivar (Malwa). More organic acids and phenols were detected from the resistant cultivar (Simla). The leaf exudate of the resistant cultivar (Simla) inhibited spore germination of the pathogen (Alternaria solani) while that of susceptible (Malwa) stimulated spore germination. The cultivar ‘Patna’ which is moderately resistant, occupied an intermediate position. Spore germination of the isolated fungi was enhanced in leaf exudate of susceptible cultivar (Malwa), while leaf exudates of the moderately resistant (Patna) and resistant (Simla) inhibited spore germination of the majority of fungi isolated. Most of the antagonistic fungi were not isolated from the susceptible cultivar and the percentage spore germination of these fungi was less in leaf exudate of the susceptible cultivar, while leaf exudates of resistant cultivars enhanced the percentage spore germination of antagonistic fungi,viz Aspergillus flavus, A. fumigatus, A. versicolor, Penicillium citrinum, P. restrictum andTrichoderma viride.     

A study of the growth condition and solubilization of phosphate from hydroxyapatite byPantoea agglomerans

The growth conditions ofPantoea agglomerans, a phosphate solubilizing organism, were studied in our laboratory to determine the optimal conditions.Pantoea agglomerans showed the highest growth rate at 30°C, pH 7.0 and 2 vvm, after 50 h cultivation. A certain relationship between pH and phosphate concentration, was evident when the glucose concentration in the medium was changed. Increasing glucose concentration increased the pH buffer action of the broth. At glucose concentrations higher than the optimum concentration of 0.2 M, the cell growth was retarded.P. agglomerans consumed glucose as a substrate to produce organic acids which caused the pH decrease in the culture medium. The phosphate concentration in the medium was increased by the presence of the organic acids, which solubilized insoluble phosphates such as hydroxyapatite.     

Fungal degradation of calcium-, lead- and silicon-bearing minerals

The aim of this study was to examine nutritional influence on the ability of selected filamentous fungi to mediate biogenic weathering of the minerals, apatite, galena and obsidian in order to provide further understanding of the roles of fungi as biogeochemical agents, particularly in relation to the cycling of metals and associated elements found in minerals. The impact of three organic acid producing fungi (Aspergillus niger, Serpula himantioides and Trametes versicolor) on apatite, galena and obsidian was examined in the absence and presence of a carbon and energy source (glucose). Manifestation of fungal weathering included corrosion of mineral surfaces, modification of the mineral substrate through transformation into secondary minerals (i.e. crystal formation) and hyphal penetration of the mineral substrate. Physicochemical interactions of fungal metabolites, e.g. H⁺ and organic acids, with the minerals are thought to be the primary driving forces responsible. All experimental fungi were capable of mineral surface colonization in the absence and presence of glucose but corrosion of the mineral surface and secondary mineral formation were affected by glucose availability. Only S. himantioides and T. versicolor were able to corrode apatite in the absence of glucose but none of the fungi were capable of doing so with the other minerals. In addition, crystal formation with galena was entirely dependent on the availability of glucose. Penetration of the mineral substrates by fungal hyphae occurred but this did not follow any particular pattern. Although the presence of glucose in the media appeared to influence positively the mineral penetrating abilities of the fungi, the results obtained also showed that some geochemical change(s) might occur under nutrient-limited conditions. It was, however, unclear whether the hyphae actively penetrated the minerals or were growing into pre-existing pores or cracks.     

Decreased mineral availability enhances rock phosphate solubilization efficiency in <Emphasis Type="Italic">Aspergillus niger</Emphasis>

Microbial solubilization of rock phosphate (RP) is mainly achieved by the production of organic acids and medium acidification through H⁺ release. During RP solubilization, mineral nutrient availability is likely to be critical for determining how much carbon is channeled either for metabolite synthesis or for microbial growth, influencing organic acid release by microorganisms. Thus, the objective of this work was to study the relationships between the concentration of mineral nutrients in the growth medium and the efficiency of RP solubilization by Aspergillus niger FS1. For this, the fungus was grown in Czapek medium containing 0, 1, 2, 10, 50, and 100 % of its original concentration of mineral nutrients. Decreasing mineral availability in the growth medium led to decreases in fungal biomass and solubilized P, and increases in titratable acidity and solubilization efficiency as expressed by mg solubilized P per g fungal biomass (Y_P/B), indicating a shift in fungal metabolism from biomass production to organic acid release. The transfer of pre-grown biomass to media with or without added minerals confirmed that lower mineral availability increases Y_P/B and led to the solubilization of 76 % of P present in Patos RP. These observations open new perspectives on improving RP solubilization systems by manipulating mineral nutrient availability in the medium, with consequent gains in cost reduction.     

不同碳源对三种溶磷真菌溶解磷矿粉能力的影响

通过液体培养法 ,对 3种溶磷真菌利用葡萄糖、果糖、蔗糖、麦芽糖、淀粉和纤维素等碳源溶解宜昌产磷矿粉的试验 ,结果表明 ,菌株P2 3在供给葡萄糖时的溶磷能力最高 ,并在一定程度上能够利用长链碳源淀粉和纤维素为营养而溶磷 ;而高效溶磷菌株P6 6和P39溶磷的最佳碳源是果糖和麦芽糖 ,该两菌株利用淀粉和纤维素的溶磷效果很小 ,甚至不溶磷。 3种溶磷真菌培养滤液 pH值、可滴定酸含量与其溶磷量之间的相关性因菌株而异 ,差别很大。菌株P2 3培养滤液pH值、可滴定酸含量与其溶磷量之间相关性很低 ,但菌株P6 6和P39培养滤液pH值、可滴定酸含量与其溶磷量之间相关性却达到极显著水平 (P <0 0 1)。结果表明 ,不同碳源对溶磷菌溶解磷矿粉能力影响很大 ,分析推断 3种菌株产生的有机酸活化磷矿粉能力为P6 6>P39>P2 3。     

一株节杆菌溶解磷矿粉的动态

磷矿粉用量明显地影响节杆菌1TCRi7菌株对其溶解,随着磷矿粉用量的增加,溶磷率急剧下降,超过5 g/L,溶磷率不到0.1%,培养液的pH也随磷矿粉用量增加而升高,但菌体生长繁殖几乎不受磷矿粉用量的影响。振荡培养时,第1 d菌体繁殖量就达到高峰,pH也降至最低,同时表现出强烈的溶磷活力,但菌株的溶磷量并不与其生长量吻合,溶磷量第9 d才达到高峰,以后逐渐下降。培养过程中有机酸分泌发生交替变化,主要分泌乙酸和丙二酸。第1 d、第9 d和第15 d出现3个峰值,说明微生物利用了所分泌出来的有机酸,并发生了有机酸代谢的变化。     

The ability of filamentous fungi to produce acids on indoor building materials

Sixty two filamentous fungi isolated from paint coatings, wallpaper, carton-gypsum board, and indoor air in buildings were screened for acid activity. It was found that 64.5% of strains produce acids on medium with bromo-cresol purple, where 18% of the strains were distinguished by very high acid activity (acid activity coefficient Q = 1.32–2.83), including the species:Aspergillus niger, Aspergillus versicolor, Penicillium expansum, Penicillium brevicom pactum, Penicillium chrysogenum, Cladosporium cladosporioides, Stachybotrys chartarum, Mucor globosus, Ulocladium chartarum andAlternaria alternata. Research indicated that filamentous fungi considerably decrease the pH of the medium when that medium containing building material. The greatest acid production and pH decrease of the medium was observed during the growth of filamentous fungi in a medium with mortar, while the production of acids was less in a medium with cartongypsum board, gypsum, and wallpaper. Filamentous fungi produced succinic, oxalic, malic and fumaric acids in the medium with indoor building materials. It was stated that the type of building material affects the spectrum and quantity of organic acids produced by filamentous fungi.     

微生物溶解磷矿粉能力与pH及分泌有机酸的关系

从玉米根际和非根际土壤中分离得到的 74株溶解磷矿粉的微生物 ,发现它们的溶磷能力差异很大 ,主要决定于菌株本身的特性 ,与其来源无关 ,真菌普遍比细菌要强。真菌的溶磷能力与其培养介质的 pH之间呈显著的负相关 ,但细菌的这种关系非常弱。二者都产生多种有机酸 ,真菌主要分泌草酸、丙二酸和乳酸 ,而细菌主要分泌草酸、酒石酸、丙二酸、乳酸和乙酸 ,不同菌株分泌有机酸的数量和种类差异很大 ,但溶磷量与有机酸总量或单个有机酸浓度之间 ,没有发现显著的相关性 ,唯独柠檬酸与真菌的溶磷量之间存在显著的相关性。说明不同菌株有完全不同的溶磷机理 ,可能多种机理并存。     

Biodeterioration of Mayan buildings at uxmal and tulum,Mexico

Uxmal and Tulum are two important Mayan sites in the Yucatan peninsula. The buildings are mainly composed of limestone and grey/black discoloration is seen on exposed walls and copious greenish biofilms on inner walls. The principal microorganisms detected on interior walls at both Uxmal and Tulum were cyanobacteria; heterotrophic bacteria and filamentous fungi were also present. A dark‐pigmented mitosporic fungus and Bacillus cereus, both isolated from Uxmal, were shown to be acidogenic in laboratory cultures. Cyanobacteria belonging to rock‐degrading genera Synechocystis and Gloeocapsa were identified at both sites. Surface analysis previously showed that calcium ions were present in the biofilms on buildings at Uxmal and Tulum, suggesting the deposition of biosolubilized stone. Apart from their potential to degrade the substrate, the coccoid cyanobacteria supply organic nutrients for bacteria and fungi, which can produce organic acids, further increasing stone degradation.     

Nitrogen fixation in lichens is important for improved rock weathering

It is known that cyanobacteria in cyanolichens fix nitrogen for their nutrition. However, specific uses of the fixed nitrogen have not been examined. The present study shows experimentally that a mutualistic interaction between a heterotrophic N₂ fixer and lichen fungi in the presence of a carbon source can contribute to enhanced release of organic acids, leading to improved solubilization of the mineral substrate. Three lichen fungi were isolated fromXanthoparmelia mexicana, a foliose lichen, and they were cultured separately or with a heterotrophic N₂ fixer in nutrient broth media in the presence of a mineral substrate. Cells of the N₂-fixing bacteria attached to the mycelial mats of all fungi, forming biofilms. All biofilms showed higher solubilizations of the substrate than cultures of their fungi alone. This finding has bearing on the significance of the origin and existence of N₂-fixing activity in the evolution of lichen symbiosis. Further, our results may explain why there are N₂-fixing photobionts even in the presence of non-fixing photobionts (green algae) in some remarkable lichens such asPlacopsis gelida. Our study sheds doubt on the idea that the establishment of terrestrial eukaryotes was possible only through the association between a fungus and a phototroph.     

菌根真菌对酸铝胁迫的响应

酸性环境中活性铝浓度升高可能抑制菌根真菌生长,为探讨酸性条件下菌根真菌对活性铝的响应机制,以拟青霉(Simplicillium sp.,Si)、细长孢霉(Mortierella elongate,Me)、木霉菌(Trichoderma spp.,Tr)、瓶头霉(Phialocephala,Ph)和葡萄状穗霉(Stachybotrys chartarum,Sc)5种菌根真菌为供试材料,采用PDA液体培养基单种纯培养以pH值为5.5设定3个Al3+浓度梯度,分别为对照(0 mmol·L^-1)、低铝(0.2 mmol·L^-1)和高铝(1.0 mmol·L^-1),研究酸性条件下不同活性铝浓度对菌根真菌的生物量、有机酸分泌以及N、P、K含量等的影响。结果表明:(1)除拟青霉(Si)外,其他菌株均不同程度受活性铝浓度影响,Si生物量随活性铝浓度增加而增加,低铝时比对照增加了238%(P<0.05),而细长孢霉(Me)、木霉菌(Tr)、瓶头霉(Ph)和葡萄状穗霉(Sc)生物量均降低,其中,Ph和Sc分别比对照降低了38.1%和72.5%(P<0.05)。(2)5种菌根真菌分泌有机酸存在显著性差异,Si、Me、Tr和Sc的H+分泌量在高铝浓度时均低于对照,对Si产生显著性差异(P<0.05);仅Me分泌草酸,对照的分泌量是高铝时的1.12倍。(3)5种菌根真菌N、P、K含量随不同活性铝浓度胁迫存在显著性差异,Si和Sc的P、K含量随活性铝浓度增加而显著增加(P<0.05);Me和Ph的N含量随活性铝浓度增加而显著降低(P<0.05),Me的P、K含量分别在低铝和高铝时达到峰值,Tr和Ph的N、P、K含量在低铝时达到峰值而在高铝时受到抑制。(4)Si、Me和Tr受酸铝影响不显著,属耐酸铝型菌株,Ph和Sc属酸铝敏感型菌株。本工作可为天山雪岭云杉森林更新与幼苗存活问题研究的深入开展提供基础依据。     

Substrate specificity of glucose dehydrogenase (GDH) of Enterobacter asburiae PSI3 and rock phosphate solubilization with GDH substrates as C sources

Enterobacter asburiae PSI3 is a rhizospheric isolate that solubilizes mineral phosphates by the action of a phosphate starvation-inducible GDH (EC 1.1.5.2). We report here that GDH activity of this isolate shows broad substrate range, being able to act on mono and disaccharides. Enterobacter asburiae PSI3 was proficient at bringing about a drop in pH and solubilization of RP with the use of 75 mmol/L of each of the GDH substrate sugars tested as the sole C source. It liberated amounts of P ranging from 450 micromol/L (on arabinose) to 890 micromol/L (on glucose). When grown on a mixture of 7 GDH substrates at concentrations of 15 mmol/L each, the bacterium solubilized RP equivalent to 46% of the value when 75 mmol glucose/L was the C source. HPLC analysis of the culture supernatant under these conditions showed that the acidification of the media is primarily due to the production of organic acids. The significance of these results on the efficacy of E. asburiae PSI3 at solubilizing phosphates under rhizospheric conditions is discussed.     

Transformation of rock phosphate during composting and the effect of humic acid

Summary Phosphorus from Mussoorie rock phosphate (MRP) was solubilized and transformed into available forms when MRP was incorporated during composting of organic wastes. Clusterbean and redgram utilized phosphorus efficiently from the phosphorus enriched compost containing 3.1% P when added in the soil of pH 7.6 to 7.8. The solubilization of phosphorus during composting has been attributed to the formation of humic substances.     

Urea-lysine method for recovery of enteroviruses from sludge.

Enteroviruses added to sludge and indigenous viruses present in sludge were recovered by treating the sludge flocs with a 4 M urea solution buffered at pH 9 with 0.5 M lysine. Eluted viruses were absorbed to aluminum hydroxide flocs and collected by centrifugation. The flocs were solubilized with 0.1 M ethylenediaminetetraacetic acid-3% beef extract at pH 9. After dialysis to remove the ethylenediaminetraacetic acid, viruses were further concentrated by organic flocculation. Approximately 40% of poliovirus and coxsackievirus B-3 added to 500 to 1,000 ml of sludge could be recovered in final sample volumes of less than 10 ml. Polioviruses, echoviruses, and coxsackieviruses were recovered from different samples of wastewater sludge.     

Chemical and microbiological solubilization of silicates

The solubilization of silicates was investigated using kaolin and quartz sand as model substances. The mineral solubilization was studied in the concentration of solubilized Si and Al. The chemical leaching of the silicates was carried out using inorganic and organic acids as well as sodium hydroxide. The process was more effective in the alkine than in the acid pH range. In the acid medium, oxalic acid showed maximum acidity and a tendency to form complex structures, especially with aluminium, and was most effective in leaching. The microbiological influence on solubilization reactions was tested using a number of microorganisms among them acid, alkali and slime-forming species. The highest leaching activity was observed in the case of Thiobacillus thiooxidans, whereas the heterotrophic microorganisms (among them Bacillus mucilaginosus) did not exercise a sollubilizing effect on the silicates. X-ray phase analysis of leached kaolin samples did not show any differences from the non-leached mineral.     

Surface iron polymers and hydroxy acids. A model of iron supply in sideramine-free fungi

Biochemical and electron microscopic evidence is presented that sideramine-free fungi form iron hydroxide polymer layers on the cell surface when grown in an iron containing medium.Iron hydroxide polymer formation on the cell surface is completely prevented in sideramine producing strains of Neurospora crassa. After feeding a sideramine-free mutant of Neurospora crassa with ornithine in order to restore the sideramine synthesis the iron hydroxide coat is gradually dissolved.The addition of excess citrate and malate to the incubation medium also prevents iron polymer adsorption, suggesting that hydroxy acids may be involved in iron supply, when sideramine-free organisms are grown in iron containing media.In order to study the interaction between iron hydroxide polymer deposition upon the cell surface and iron chelating acids in Neurospora crassa, the amount and the proportion of excreted acids was studied under various experimental conditions. Gas chromatographic analysis of the acids produced under iron deficient conditions revealed that succinate, malate and citrate were present within the cells in the early growth phase. The acids were sequentially excreted into the medium in the order succinate, malate and citrate. The amount of succinate decreased after 2 days of cultivation, whereas the amount of malate and citrate continually increased. Although citrate was present within the cells from the 1st day, excretion occurred very late, generally after the 3rd day.It is suggested that sideramine-free fungi first adsorb iron as a hydroxide polymer on the cell surface, and that it is gradually solubilized by excreted hydroxy acids such as citrate or malate. Thus high local concentrations of iron chelated by hydroxy acids provide sideramine-free fungi with a continuous iron supply.Abbreviations BSTFA N,O-Bis(trimethylsilyl)-trifluoracetamide - GC Gaschromatography - EGTA Ethylenglykol-bis(2-aminoethylether) N,N-tetraacetic acid - TMS Trimethylsilyl     

Growth engineering of Propionibacterium freudenreichii shermanii for organic acids and other value-added products formation

Propionic acid production from glucose was studied using Propionibacterium freudenreichii shermanii. Conditions were optimized for high yields of propionic acid and total organic acids by sequential optimization of parameters like pH, inoculum age, inoculum volume and substrate concentration. Near-theoretical yield (0.54?±?0.023?g/g) was achieved for propionic acid with fermentation of 1% glucose using 20% (v/v) of 48?hr old P. shermanii at 30°C, pH maintained at 5.5. Total organic acid yield under these conditions was 0.74?±?0.06?g/g. The study resulted in achieving 98% and 95% theoretical yields of propionic acid and total organic acids, respectively. Under optimized conditions, along with organic acids, P. shermanii also produced vitamin B12 and trehalose intracellularly, showing its potential to be used as a cell factory.     

Ionization and phase behavior of fatty acids in water: application of the Gibbs phase rule

The phase behavior of several medium-chain (10- and 12-carbon) and long-chain (18-carbon) fatty acids in water was examined as a function of the ionization state of the carboxyl group. Equilibrium titration curves were generated above and below fatty acid and acid-soap chain melting temperatures and critical micelle concentrations, and the phases formed were characterized by X-ray diffraction, 13C NMR spectroscopy, and phase-contrast and polarized light microscopy. The resulting titration curves were divided into five regions: (i) at pH values less than 7, a two-phase region containing oil or fatty acid crystals and an aqueous phase; (ii) at pH approximately 7, a three-phase region containing oil, lamellar, and aqueous (or fatty acid crystals, 1:1 acid-soap crystals, and aqueous) phases; (iii) between pH 7 and 9, a two-phase region containing a lamellar fatty acid/soap (or crystalline 1:1 acid-soap) phase in an aqueous phase; (iv) at pH approximately 9, a three-phase region containing lamellar fatty acid-soap (or crystalline 1:1 acid-soap), micellar, and aqueous phases; and (v) at pH values greater than 9, a two-phase region containing micellar and aqueous phases. Interpretation of the results using the Gibbs phase rule indicated that, for oleic acid/potassium oleate, the composition of the lamellar fatty acid/soap phase varied from approximately 1:1 to 1:3 un-ionized to ionized fatty acid species. In addition, constant pH regions observed in titration curves were a result of thermodynamic invariance (zero degrees of freedom) rather than buffering capacity. The results provide insights into the physical states of fatty acids in biological systems.(ABSTRACT TRUNCATED AT 250 WORDS)     

Fungal Diversity in Rock Beneath a Crustose Lichen as Revealed by Molecular Markers

Lichen-forming fungi have been assumed to be more or less restricted to the surface of the substrate on which they grow, Conclusive identification of hyphae or an assessment of the fungal diversity inside lichen-covered rock has not been possible using methods based on direct observation. We circumvented this problem by using a DNA sequencing approach. Cores were drilled from a Devonian arcosic sandstone rock harboring the crustose lichen Ophioparma ventosa (L.) Norman on the surface. The cores were cut vertically, and DNA was extracted from the pulverized rock slices. A series of polymerase chain reactions using fungal-specific primers as well as Ophioparma ventosa specific primers were employed to amplify the internal transcribed spacer region of the nuclear ribosomal DNA. The results show that hyphae of O. ventosa penetrate approximately 10–12 mm into the rock. Consequently, the hyphal layer formed by the lichen fungus inside the rock could be 7–12 times as thick as the symbiotic thallus at the surface of the rock. In addition, eight non-lichenized fungal taxa and five that could not be identified to species were encountered. One fungal species in the order Helotiales occurs in six of the eight cores. The significance of these results to the colonization and weathering of rock by lichenized fungi is discussed.