Lignocellulose Degradation during Solid-State Fermentation: Pleurotus ostreatus versus Phanerochaete chrysosporium

Effect of manganese on preferential degradation of lignin by Pleurotus ostreatus during solid-state fermentation

Practical utilization of the polysaccharides in the lignocellulosic complex is limited because of the high lignin content of the complex. In this study we focused on the effect of Mn on lignin and cellulose biodegradation during solid-state fermentation by the edible mushroom Pleurotus ostreatus. Preferential degradation of lignin was enhanced by the addition of Mn(II) to cotton stalks at concentrations ranging from 30 to 620 micrograms of Mn per g. This effect was most apparent when we compared mineralization rates of [14C] lignin with mineralization rates of [14C] cellulose. Enhanced selectivity was also observed when we analyzed residual organic matter at the end of the fermentation period by using crude fiber analysis. The cellulose fraction in the original material was 1.8 times larger than the cellulose fraction of lignin. The cellulose/lignin ratio increased during 32 days of solid-state fermentation from 2.5 in the control to 3.3 following the addition of Mn to the medium. The in vitro digestibility value for fermented cotton stalks was 53% of the dry matter. Addition of 600 micrograms of Mn per g to the cotton stalks resulted in a digestibility value of 65.4%. Enhancement of preferential lignin degradation could be result of either increased activity of the ligninolytic enzymes or production of Mn (III), which might preferentially degrade aromatic structures in the lignocellulosic complex.

Effect of Manganese on Lignin Degradation by Pleurotus ostreatus during Solid-State Fermentation

Lignin degradation by Pleurotus ostreatus was studied under solid-state fermentation (SSF) in chemically defined medium containing various levels of Mn. Degradation of [ 14 C]lignin prepared from cotton branches to soluble products, as well as its mineralization to 14 CO 2 , was enhanced by the addition of Mn. The effect of malonate on lignin mineralization was most marked during the first 10 days of SSF, in a treatment amended with 73 μM Mn. A high concentration of Mn (4.5 mM) caused inhibition of both fungal growth and mineralization rates during the first 2 weeks of incubation. Addition of malonate reversed this effect because of chelation of Mn. Mn was found to precipitate in all treatments, with or without the addition of malonate. α-Keto-γ-methiolbutyric acid cleavage to ethylene, an indication of . OH production, was observed as early as 3 days of incubation in all treatments.

Overproduction of lignin peroxidase by Phanerochaete chrysosporium (BKM-F-1767) under nonlimiting nutrient conditions

The ligninolytic enzymes synthesized by Phanerochaete chrysosporium BKM-F-1767 immobilized on polyurethane foam were characterized under limiting, sufficient, and excess nutrient conditions. The fungus was grown in a nonimmersed liquid culture system under conditions close to those occurring in nature, with nitrogen concentrations ranging from 2.4 to 60 mM. This nonimmersed liquid culture system consisted of fungal mycelium immobilized on porous pieces of polyurethane foam saturated with liquid medium and highly exposed to gaseous oxygen. Lignin peroxidase (LIP) activity decreased to almost undetectable levels as the initial NH4+ levels were increased over the range from 2.4 to 14 mM and then increased with additional increases in initial NH4+ concentration. At 45 mM NH4+, LIP was overproduced, reaching levels of 800 U/liter. In addition, almost simultaneous secretion of LIP and secretion of manganese-dependent lignin peroxidase were observed on the third day of incubation. Manganese-dependent lignin peroxidase activity was maximal under nitrogen limitation conditions (2.4 mM NH4+) and then decreased to 40 to 50% of the maximal level in the presence of sufficient or excess initial NH4+ concentrations. Overproduction of LIP in the presence of a sufficient nitrogen level (24 mM NH4+) and excess nitrogen levels (45 to 60 mM NH4+) seemed to occur as a response to carbon starvation after rapid glucose depletion. The NH4+ in the extracellular fluid reappeared as soon as glucose was depleted, and an almost complete loss of CO2 was observed, suggesting that an alternative energy source was generated by self-proteolysis of cell proteins.(ABSTRACT TRUNCATED AT 250 WORDS)