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Much research dealing with the processing of milk by-products in heat exchangers has noted the key role of calcium in β-lactoglobulin (β-LG) fouling behavior. Nevertheless, the manner by which Ca affects β-LG denaturation has rarely been quantified using reliable kinetic and thermodynamic data. To this end, the influence of Ca on β-LG denaturation mechanisms in simulated lactoserum concentrates was studied on the laboratory-scale under 100°C by HPLC analysis. The heat-treated solutions were composed of 53.3g/L β-LG and were enriched in Ca at various concentrations (0, 66, 132, and 264 mg/kg). The kinetic parameters (reaction order, activation energy, and frequency factor) associated with β-LG denaturation, along with the unfolding and aggregation thermodynamic parameters were deduced from these experiments and discussed with respect to Ca content. We found that the multistage process characterizing β-LG thermal denaturation is not greatly affected by Ca addition. In fact, the general model subdividing β-LG denaturation mechanisms in 2 steps, namely, unfolding and aggregation, remained valid for all tested Ca concentrations. The change in the predominant mechanism from unfolding to aggregation was observed at 80°C across the entire Ca concentration range. Moreover, the classical 1.5 reaction order value was unaffected by the presence of Ca. Interpretation of the acquired kinetic data showed that Ca addition led to a significant increase in kinetic rate, and more so in the aggregation temperature range. This indicates that Ca principally catalyzes β-LG aggregation, by lowering the Coulombian repulsion between the negatively charged β-LG reactive species, bridging β-LG proteins, or via an ion-specific conformational change. To a lesser extent, Ca favors β-LG unfolding, probably by disturbing the noncovalent binding network of native β-LG. Simultaneously, Ca has a slight protective role on the native and unfolded β-LG species, as shown by the increase in activation energy with Ca concentration. The calculation of thermodynamic parameters related to β-LG denaturation confirmed this observation. A threshold effect in Ca influence was noted in this study: no further significant kinetic rate change was observed above 132 mg/kg of Ca; at this concentration, the studied solution was an almost equimolar mixture of β-LG and Ca. Finally, we simulated the temporal evolution of β-LG species concentrations at diverse Ca contents at 3 holding temperatures. The simulations were based on the acquired kinetic parameters. This permitted us to highlight the greater effect of Ca on β-LG denaturation at high Ca content or for short-time heat treatments at temperatures near 100°C, as in heat exchangers.

The basidiomycete Marasmius quercophilus is commonly found during autumn on the decaying litter of the evergreen oak (Quercus ilex L.), a plant characteristic of Mediterranean forest. This white-rot fungus colonizes the leaf surface with rhizomorphs, causing a total bleaching of the leaf. In synthetic liquid media, this white-rot fungus has strong laccase activity. From a three-step chromatographic procedure, we purified a major isoform to homogeneity. The gene encodes a monomeric glycoprotein of approximately 63 kDa, with a 3.6 isoelectric point, that contains 12% carbohydrate. Spectroscopic analysis of the purified enzyme (UV/visible and electron paramagnetic resonance, atomic absorption) confirmed that it belongs to the "blue copper oxidase" family. With syringaldazine as the substrate, the enzyme's pH optimum was 4.5, the optimal temperature was 75°C, and the K m was 7.1 M. The structural gene, lac1, was cloned and sequenced. This gene encodes a 517-aminoacid protein 99% identical to a laccase produced by PM1, an unidentified basidiomycete previously isolated from wastewater from a paper factory in Spain. This similarity may be explained by the ecological distribution of the evergreen oak in Mediterranean forest.Litter mineralization is an important component of biogeochemical cycles in terrestrial environments. Lignin is the most difficult litter polymer to degrade, and the only organisms known to completely mineralize lignin are white-rot fungi (6,17). In the last two decades, several such organisms have been studied. At present, three main enzymes (i.e., manganese and lignin peroxidases and laccases) (15, 30) are implicated in the biodegradation of lignin. In addition to fundamental studies on lignin mineralization, these enzymes also have potential uses in industrial processes such as the bleaching of paper pulp (1) or the remediation of xenobiotics in effluents (3). There is no clear relationship between the distribution of ligninolytic enzymes and lignin degradation, since white-rot fungi with only one, with a combination of two, or with all three enzymes are known and can degrade lignin (15,27,34).The role of laccases in lignin degradation has only recently become well established (38). Laccases (p-diphenol oxidase, EC 1.10.3.2) are polyphenol oxidases that catalyze the reduction of oxygen to water with a concomitant oxidation of phenolic compounds. They are typically glycoproteins containing 2 to 4 atoms of copper per molecule and are found in plants and fungi (25,33,35).The evergreen oak (Quercus ilex) forms a characteristic forest climax common in the Western Mediterranean area (22,28). The leaf of Q. ilex, highly lignous and covered by a thick and waxy upper cuticle, is typical of sclerous plants exposed to dryness, particularly during the summer. The white-rot fungus Marasmius quercophilus colonizes dead leaves of Quercus ilex (32). Under favorable temperature and humidity conditions, i.e., in autumn and sometimes in May and June, this fungus becomes predominant among litter fungi and produces ma...