Influence of clay minerals on sorption of bacteriolytic enzymes

Myxobacteria presumably produce extracellular bacteriolytic enzymes when they are growing in soil. In order to study their ecological significance, adsorption experiments were performed with lytic enzymes produced byMyxococcus virescens in casitone media. Different soils as well as montmorillonite and kaolinite can rapidly adsorb the bacteriolytic but not the proteolytic enzymes. About 1 gm of montmorillonite per liter of cell-free culture solution is enough for the adsorption of 97% of the bacteriolytic enzymes. The adsorption per unit weight is about 100 times greater on montmorillonite than on kaolinite. About 40% of the adsorbed enzymes can be eluted with solutions of high pH or high ionic strength. The only desorbed bacteriolytic enzyme is the alanyl-∈-N-lysine endopeptidase.     

Binding of the protoxin and toxin proteins ofBacillus thuringiensis subsp.kurstaki on clay minerals

The equilibrium adsorption and binding of the delta-endotoxin proteins, i.e., the protoxins (M_r=132 kDa) and toxins (M_r=66 kDa), fromBacillus thuringiensis subsp.kurstaki were greater on montmorillonite than on kaolinite (five-fold more protoxin and three-fold more toxin were adsorbed on montmorillonite). Approximately two- to three-fold more toxin than protoxin was adsorbed on these clay minerals. Maximum adsorption occurred within 30 min (the shortest interval measured), and adsorption was not significantly affected by temperatures between 7° and 50°C. The proteins were more easily desorbed from kaolinite than from montmorillonite; they could not be desorbed from montmorillonite with water or 0.2% Na₂CO₃, but they could be removed with Tris-SDS (sodium dodecyl sulfate) buffer. Adsorption was higher at low pH and decreased as the pH increased. Adsorption on kaolinite was also dependent on the ionic nature of the buffers. The molecular mass of the proteins was unaltered after adsorption on montmorillonite, as shown by SDS-PAGE (polyacrylamide gel electrophoresis) of the desorbed proteins; no significant modifications occurred in their structure as the result of binding on the clay, as indicated by infrared analysis; and there was no significant expansion of the clay by the proteins, as shown by x-ray diffraction analysis. The bound proteins appeared to retain their insecticidal activity against the third instar larvae ofTrichoplusia ni.     

Activity of bacteriolytic enzymes adsorbed to clays

Myxococcus virescens is able to produce extracellular bacteriolytic enzymes that are rapidly adsorbed on montmorillonite. These adsorbed enzymes are active and can be assayed by measuring the release of UV-absorbing materials in mixtures containingMicrococcus luteus cells. The activity of the clay-adsorbed enzymes is, however, considerably lower than that of the unadsorbed enzymes. Both unadsorbed and adsorbed enzymes have their maximum activity at approximately the same pH. At lower clay-enzyme concentrations, the activity is proportional to the concentration. If, however, increasing amounts of clay are added to a fixed volume of clay-enzyme suspension, the activity remains almost unchanged until a definite limit is reached, then the activity decreases rapidly. This limit was dependent only on the ratio of the amounts of enzyme and clay and not on the absolute concentration of the enzyme. The montmorillonite-adsorbed bacteriolytic enzymes fromM. virescens were not active against gram-negative bacteria, and no activity against purified cell walls fromM. luteus could be measured. Montmorillonite-adsorbed egg white lysozyme was not active onM. luteus cells.     

Extracellular Lytic Enzymes of Myxococcus virescens II. Purification of Three Bacteriolytic Enzymes and Determination of their Molecular Weights and Isoelectric Points

The bacteriolytic enzymes produced by Myxococcus virescens and previously concentrated and separated from most of the non-bacteriolytic proteins have been further separated and purified. The bacteriolytic enzyme solution was concentrated by lyo-philization. When applied to a Sephadex G-100 column, three peaks of bacteriolytic activity were eluted. Polyacrylamide gel electrophoresis showed that all the three enzyme fractions were contaminated with at least four non-bacteriolytic proteins. In the first enzyme fraction the bacteriolytic enzymes could be freed from the contaminating proteolytic activity by adsorption on a hydroxylapatite column. The bacteriolytic enzymes could then be adsorbed on a CM-cellulose column. The remaining contaminating proteins passed the column un-adsorbed while the bacteriolytic enzymes could be eluted with a gradient of 0.02–0.10 M ammonium hydrogen carbonate solution. The second enzyme fraction was adsorbed on a CM-cellulose column and then eluted with 0.03–0.15 M NH4 HCO₃. After rechromatography on a new column under the same conditions, all of the contaminating proteins had disappeared. For purification of the third enzyme fraction chro-matography on one single CM-cellulose column was sufficient. The elution of the adsorbed enzymes was performed with a gradient of 0.15–0.30 M NH₄HCO₃. The recovery of activity for each of the ion-exchange chromatography separations was at least 90%. The purity of the enzymes was tested by polyacrylamid gel electrophoresis. Each of the purified enzymes gave only one coloured band which coincided with the enzyme activity assayed in sliced gels. The molecular weights of the enzymes were determined by electrophoresis on acryl-amide gels containing sodiumdodecylsulphate. The molecular weights determined in this way (about 40,000, 30,000 and 20,000, respectively) were about 10,000 daltons higher than those obtained by gel chromatography on Sephadex G-100. This discrepancy seems to depend on interactions between the enzymes and the dextran molecules probably caused by the strongly basic nature of the enzymes or by formation of enzyme-substrate complexes.     

Adsorption/Desorption of toluene on clay minerals

Adsorption/desorption of toluene on montmorillonite, illite, and kaolinite was studied using the batch equilibrium method. The isotherms measured fit the Freundlich equation (r² >0.95). Montmorillonite adsorbed more toluene than illite or kaolinite; the adsorption of toluene on illite and kaolinite was not significantly different. Adsorption of toluene by montmorillonite showed an exponential increase as the ratio of toluene to clay was increased from 5 to 100. The rate studies showed that 62% of the adsorption was completed within 6 h. A rapid desorption was observed initially, followed by slow desorption after 1 h. The desorption rate decreased as the time of adsorption was increased. Almost all of the adsorbed toluene was extracted with water from the clay when the adsorption time was 0.1 h, but only 61% of the toluene could be desorbed when the adsorption time was 24 h.     

Extracellular Lytic Enzymes of Myxococcus virescens

An easy and rapid method for the purification of a bacteriolytic endopeptidase produced by Myxococcus virescens is described. The bacteria were grown in casitone media and the cells were sedimented by centrifugation. About 1.2 g of montmorillonite were added per liter of cell-free culture solution. The clay was sedimented by centrifugation and the enzyme was then eluted by 0.05 M Na-phosphate buffer pH 6.0, containing 0.4 M NaCl. The enzyme was diluted with water and chromatographed on carboxymethyl-cellulose columns. The purified enzyme liberated free amino groups but no reducing sugars or N-acetylhexosamines when acting on purified N-acetylated cell walls of Micrococcus lysodeikticus. Analysis of N- and C-terminal amino acids in the digestion products showed that the enzyme had liberated about 110 nmoles of lysine ε-amino groups and 60 nmoles of alanine carboxyl groups per mg of cell wall. When it acted on a bisdisaccharide pentapeptide dimer isolated from M. lysodeikticus cell walls, it cleaved about 30% of the alanyl-lysine linkages. Consequently the enzyme was an alanyl-lysine endopeptidase. It had no muramyl-alanine amidase activity.     

Adsorption and anti-ultraviolet light characteristics of the protoxin from Bacillus thuringiensis on montmorillonite,kaolinite, zinc oxide and rectorite

The adsorption, desorption and anti-ultraviolet light characteristics of the protoxin from Bacillus thuringiensis strain WG-001 on montmorillonite, kaolinite, zinc oxide and rectorite were studied. The protoxin was easily adsorbed onto minerals and the adsorption reached equilibrium within 0.5–1.0 h (except for rectorite). The adsorption isotherms of protoxin at different concentrations in sodium carbonate buffer (pH 9) followed the Langmuir (R ² >0.97) and Freundlich (R ² >0.95) equations. The maximum amounts of protoxin adsorbed were in the order: montmorillonite>rectorite>znic oxide>kaolinite. In the range of pH from 9 to 11 (carbonate buffer), the protoxin adsorbed decreased with increasing pH. The adsorption was not significantly affected by the temperature between 5 and 45°C. Both free and adsorbed protoxin were toxic to larvae of Heliothis armigera. The LC₅₀ value of free and adsorbed protoxin on montmorillonite, rectorite, zinc oxide and kaolinite were 14±1.16, 1.76±0.31, 2.94±0.71, 4.78±2.08 and 1.91±0.91 µg mL^?1, respectively. After 1 h of ultraviolet irradiation, the LC₅₀ of the above samples increased by 41.4, 19.3, 16.3, 125.9 and 62.3%, respectively. The desorption of adsorbed protoxin in water ranged from 30.1 to 64.9% and from 18.5 to 48.7% in carbonate buffer.     

Interaction between ATP,metal ions,glycine, and several minerals

Summary The adsorption of ATP and ADP on montmorillonite, kaolinite, and A1(OH)₃ was studied as a funtion of pH and, for montmorillonite and kaolinite, as a funtion of the ionic composition of the system. The three minerals exhibit different adsorption charcteristics. Mg²⁺- and Zn²⁺-montmorillonite adsorb ATP and ADP more than Na⁺-montmorillonite, presumably because of complex formation. In kaolinite, the effect of these divalent cations is small. Pure ATP decomposes upon heating, and the rate of the decomposition is accelerated by the presence of glycine. Drying and heating glycine to 70°C under vacuum in the presence of ATP results in abiotic peptide formation with yields up to 0.25%. This peptide formation also occurs when kaolinite or montmorillonite is added to the system. The presence of kaolinite, Mg²⁺-or Zn²⁺-koalinite, or Mg²⁺-montmorillonite results in a reduction in the rate of the ATP decomposition in the abiotic peptide synthesizing system. These results suggest that one role for clays and metal ions in chemical evolution may have been the stabilization of nucleotides during prebiotic peptide synthesis.On Leave from the Hebrew University of Jerusalem, Israel     

Effects of Temperature,pH and Salt Concentrations on the Adsorption of Bacillus subtilis on Soil Clay Minerals Investigated by Microcalorimetry

Adsorption of microorganisms on minerals is a ubiquitous interfacial phenomenon in soil. Knowledge of the extent and mechanisms of bacterial adsorption on minerals is of great agronomic and environmental importance. This study examined adsorption of Bacillus subtilis on three common minerals in soils such as kaolinite, montmorillonite and goethite under various environmental conditions. Isothermal titration calorimetry (ITC) was used to investigate the effects of temperature (20, 30, and 40°C), pH (5.0, 7.0, and 9.0) and KNO₃ concentration (0.001, 0.01, and 0.1 mol L^?1) on the adsorption by direct measurement of enthalpies. The results revealed that the adsorption process in all the mineral systems were exothermic, with the enthalpy changes (ΔH_ads ) ranging from ?52 to ?137, ?33 to ?147, and ?53 to ?141 kJ kg^?1 (dry weight of adsorbed bacteria) for kaolinite, montmorillonite, and goethite, respectively. No obvious dependence of ΔH_ads on temperature was observed. The heat release for all the systems generally declined with pH and decrease of salt concentration, which can be explained by the variations of hydrophobicity and electrostatic force with pH or salt concentration. The largest decrease was found for goethite among the three minerals from pH 5.0 to 7.0, suggesting that electrostatic attraction may play a more important role in bacterial adsorption on this mineral. The ΔH_ads values for all the minerals became nearly the same at pH 9.0, indicating that the same force probably hydrophobicity governing the adsorption for the minerals in alkaline environment. It is assumed that acidic or saline soils and the associated environments favor the adsorption of B. subtilis on clay minerals. In addition, the negative enthalpies expressed as kJ kg^?1 (carbon) revealed an energy flow into the environment accompanied by the carbon adsorption on the minerals in soil.     

Effect of the clay minerals montmorillonite and kaolinite on the genetic transformation of competentBacillus subtilis cells

The effect of the clay minerals montmorillonite and kaolinite on the transformation of competentBacillus subtilis cells with chromosomal DNA was studied. Clay particles were found to substantially increase the transformation frequency of competent cells, as well as the rate of their spontaneous chromosomal and plasmid transformation. The effect was ascribed to the adsorption of bacterial cells on the surface of mineral particles.     

Influence of clay minerals,humic acid and bacterial capsular polysaccharide on the survival of Klebsiella aerogenes exposed to drying and heating in soils

The influence of clay minerals, humic acid and capsular polysaccharide on the survival of Klebsiella aerogenes exposed to drying and heating in soils was investigated. The study of three types of soils showed that the survival of the bacteria was higher in montmorillonitic than in kaolinitic soils. When a sandy soil was amended with 10 per cent montmorillonite, 10 per cent kaolinite or 0.5 per cent humic acid, the survival of K. aerogenes was increased in the presence of montmorillonite but was not affected by kaolinite or humic acid. It was suggested that montmorillinite affected the pattern of water retention by the cells during the drying process. The influence of capsular polysaccharides was also investigated and no significant difference was abserved between the survival of the encapsulated and non-capsulated strains of K. aerogenes exposed to drying and heating in soils. re]19750321     

Specificity of virus adsorption to clay minerals

Competitive adsorption studies indicated that reovirus type 3 and coliphage T1 did not share common adsorption sites on kaolinite and montmorillonite. Compounds in the minimal essential medium (e.g., fetal bovine serum, amino acids) in which the reovirus was maintained blocked adsorption of coliphage T1 to kaolinite and partially to montmorillonite in synthetic estuarine water, but they had no effect on coliphage adsorption to montmorillonite in distilled water or on the adsorption of the reovirus to either clay. The blockage of positively charged sites on kaolinite or montmorillonite by treatment of the clays with sodium metaphosphate or with the supernatants from montmorillonite or kaolinite, respectively, had no effect on adsorption of the reovirus. These data indicate that there was a specificity in adsorption sites for mixed populations of reovirus type 3 and coliphage T1 and emphasize the importance of using more than one type of virus, especially in combination, to predict virus behavior (e.g., adsorption, loss of infectivity) in soils and sediments containing clay minerals.     

Adsorption of DNA by Bacteria and Their Composites with Minerals

Previous studies revealed the thermodynamic properties of DNA adsorption on pure minerals or biomasses; however, there has been little attempt to develop such studies on bacteria–mineral composites. Equilibrium adsorption experiments, attenuated total reflectance Fourier transform infrared spectroscopy, and isothermal titration calorimetry were employed to investigate the adsorption of DNA by Bacillus subtilis, Pseudomonas putida, and their composites with minerals. Similar capacity and affinity were observed for DNA adsorption on two bacterial cells. However, different patterns were found in the adsorption of DNA by bacteria–mineral composites. The Gram-positive bacterium B. subtilis enhanced the adsorption of DNA on its mineral composites compared with their individual components, while the composites of Gram-negative bacterial cells with kaolinite and goethite bound lower amounts of DNA than the predicted values. The thermodynamic parameters and the Fourier transform infrared spectra showed that van der Waals force and hydrogen bonding are responsible for the DNA adsorption on B. subtilis–minerals and P. putida–kaolinite. By contrast, the entropy increases of excluded water rearrangement and dehydration effect play key roles in the interaction between DNA and P. putida–montmorillonite/goethite composites.     

The Mechanism of Action of the Extracellular Bacteriolytic Enzymes of Lysobacter sp. on Gram-Positive Bacteria: The Role of the Cell Wall Anionic Polymers of Target Bacteria

The study of the extracellular bacteriolytic enzymes of Lysobacter sp. showed that they can efficiently hydrolyze the peptidoglycan of gram-positive bacteria provided that there is an electrostatic interaction of these enzymes with the cell wall anionic polymers, teichoic and teichuronic acids in particular. The hydrolytic action of bacteriolytic enzymes on the cell wall largely depends on the negative charge of the teichoic and teichuronic acids rather than on their chemical composition.     

Extracellular Lytic Enzymes of Myxococcus virescens

The aim of the investigation was to obtain large amounts of the bacteriolytic enzymes of Myxococcus virescens and to separate these enzymes from the non-bactcriolytic protemases produced by this organism. The bacteria were grown in Casitone broth. When the bacteriolytic activity had reached its maximal value, the cells were removed from the culture medium by centrifugation. Polyethylene glycol 4000 (20 g/1) and potassium phosphate (about 210 g/1) were added to the cell-free solution. The additions resulted in the formation of two liquid phases. The bottom layer was removed, and polyethylene glycol was added to it at a final concentration of 10 g/1. Again two liquid phases formed. The two top phases thus obtained were pooled and 1.6 volumes of cold acetone were added to the mixture. The precipitate formed was dissolved in water and desalted on a Sephadex G-25 column. The desalted protein solution was applied to a carboxymethyl-cellulose column equilibrated with 0.025 M sodium phosphate buffer of pH 6.0. Most of the proteins and the proteinases but none of the bacteriolytic enzymes passed the column unadsorbed. The column was washed with 0.05 M glycine-NaOH buffer of pH 8.8, whereupon the adsorbed bacteriolytic enzymes together with small amounts of proteinases and other proteins were eluted with 0.2 M ammonium carbonate. The material not adsorbed on the CM-cellulose column contained 22 % of the proteolytic activity of the initial cell-free solution and had a 26-fold higher specific activity. The enzyme solution eluted with carbonate contained 24 and 0.3 %, respectively, of the initial bacteriolytic and proteolytic activities. The specific activity of the bacteriolytic enzyme system was about 5000-fold higher than that of the original solution.     

Michaelis constant (K m ) of acid phospatase as affected by montmorillonite,illite, and kaolinite clay minerals

The influence of Ca homoionic clay minerals (montmorillonite, illite, and kaolinite) on the activity,K _m , andV _m values of acid phosphatase was examined in model experiments. At each substrate (p-nitrophenyl phosphate) level tested, the addition of increasing amounts of clays (50, 100, and 150 mg, respectively) decreased the activity and increased theK _m value from 1.43×10^–3 m PNP (in the soluble state) to 82.3×10^–3M (montmorillonite), 8.02×10^–3 m (kaolinite), and 7.65×10^–3 m (illite) at the 150 mg level. The maximum enzyme reaction velocity (V _m ) remained nearly constant at different amounts of kaolinite and illite, but increased remarkably with rising quantities of montmorillonite. Apparently, the substrate affinity of sorbed acid phosphatase is significantly lower with montmorillonite than with kaolinite or illite. This may be ascribed to an intensive sorption of both substrate and enzyme to the surface as well as to interlattice sites of montmorillonite.     

Effect of proteins on reovirus adsorption to clay minerals

Organic matter in sewage, soil, and aquatic systems may enhance or inhibit the infectivity of viruses associated with particulates (e.g., clay minerals, sediments). The purpose of this investigation was to identify the mechanisms whereby organic matter, in the form of defined proteins, affects the adsorption of reovirus to the clay minerals kaolinite and montmorillonite and its subsequent infectivity. Chymotrypsin and ovalbumin reduced the adsorption of reovirus to kaolinite and montmorillonite homoionic to sodium. Lysozyme did not reduce the adsorption of the virus to kaolinite, but it did reduce adsorption to montmorillonite. The proteins apparently competed with the reovirus for sites on the clay. As lysozyme does not adsorb to kaolinite by cation exchange, it did not inhibit the adsorption of reovirus to this clay. The amount of reovirus desorbed from lysozyme-coated montmorillonite was approximately 38% less (compared with the input population) than that from uncoated or chymotrypsin-coated montmorillonite after six washings with sterile distilled water. Chymotrypsin and lysozyme markedly decreased reovirus infectivity in distilled water, whereas infectivity of the virus was enhanced after recovery from an ovalbumin-distilled water-reovirus suspension (i.e., from the immiscible pelleted fraction plus supernatant). The results of these studies indicate that the persistence of reovirus in terrestrial and aquatic environments may vary with the type of organic matter and clay mineral with which the virus comes in contact.     

Effect of proteins on reovirus adsorption to clay minerals.

Organic matter in sewage, soil, and aquatic systems may enhance or inhibit the infectivity of viruses associated with particulates (e.g., clay minerals, sediments). The purpose of this investigation was to identify the mechanisms whereby organic matter, in the form of defined proteins, affects the adsorption of reovirus to the clay minerals kaolinite and montmorillonite and its subsequent infectivity. Chymotrypsin and ovalbumin reduced the adsorption of reovirus to kaolinite and montmorillonite homoionic to sodium. Lysozyme did not reduce the adsorption of the virus to kaolinite, but it did reduce adsorption to montmorillonite. The proteins apparently competed with the reovirus for sites on the clay. As lysozyme does not adsorb to kaolinite by cation exchange, it did not inhibit the adsorption of reovirus to this clay. The amount of reovirus desorbed from lysozyme-coated montmorillonite was approximately 38% less (compared with the input population) than that from uncoated or chymotrypsin-coated montmorillonite after six washings with sterile distilled water. Chymotrypsin and lysozyme markedly decreased reovirus infectivity in distilled water, whereas infectivity of the virus was enhanced after recovery from an ovalbumin-distilled water-reovirus suspension (i.e., from the immiscible pelleted fraction plus supernatant). The results of these studies indicate that the persistence of reovirus in terrestrial and aquatic environments may vary with the type of organic matter and clay mineral with which the virus comes in contact.     

Effect of Fatty Acids on the Activity of Bacteriolytic Enzymes

The ability of fatty acids to sensitize gram-negative and gram-positive bacterial cells to the action of bacteriolytic enzymes was studied. By synergetic effects between bacteriolytic enzymes and fatty acids isolated from Myxococcus such bacteria, which were otherwise resistant to the enzymes, could be lysed. Isobranched and unbranched acids with 11–15 carbon atoms were active and could sensitize Bacillus megaterium and Aerobacter aerogenes to the action of bacteriolytic enzymes from myxobacteria and to lysozyme. The sensitizing activity of tetradecanoic acid was enhanced with increasing concentration even after the solution was saturated. Neither ethylene diaminetetraacetate (0.1 and 1 mM) nor Triton X-100 (1 0/00) could sensitize resistant bacteria to the action of bacteriolytic enzymes. However, they were active in combination and they could also increase the effect of tetradecanoic acid.     

The role of particles on the biogeochemical cycling of domoic acid and its isomers in natural water matrices

The adsorption of dissolved domoic acid (DA) and its geometrical isomers was assessed in aqueous solutions containing various types of particles. In one series of experiments carried out in coastal seawater, detectable net adsorption of 100 nM DA occurred only onto natural seawater particles (unfiltered seawater) and 0.5 g L⁻¹ chromatographic silica (18%) in 0.2 μm-filtered seawater. Some net adsorption (<5%) also occurred in the 0.5 g L⁻¹ suspension of estuarine sediment and 0.5 g L⁻¹ solution of humic acid in filtered seawater. No losses were seen in 0.5 g L⁻¹ suspensions of illite, kaolinite, montmorillonite, and silica sand. Biological degradation accounted for small losses (8–10%) in filtered seawater without particles. A second series of experiments using organic-free, <5 μm fractions of kaolinite and montmorillonite in deionized water (DIW) demonstrated that 70% of DA adsorbed onto kaolinite, but only 5% onto montmorillonite. Geometrical isomers of DA (iso-DA D, E, and F) showed negligible adsorption (0–8%) onto a variety of particles in filtered seawater, suggesting that major ions in seawater neutralize electrostatic attractions between particles and DA isomers. These results suggest that DA and its isomers are relatively hydrophilic and not particle reactive. Our data suggest that photochemical and biological degradation of dissolved DA and its isomers appears to occur in bulk surface seawater and its transport to bottom sediments must be mainly biologically driven.