Caffeine metabolism during cultivation of oyster mushroom (Pleurotus ostreatus) with spent coffee grounds.

In coffee-producing countries, waste products from coffee production are useful substrates for cultivation of Pleurotus ostreatus. This species is relatively easy to grow, coffee waste substrates are readily available and the mushroom fruiting bodies are a valuable source of nutrition and income. In developed countries, cultivation of P. ostreatus on spent coffee grounds (SCG) from coffee consumption is a novel way to recycle this urban waste product. Here, we studied the effect of SCG and caffeine on growth of a commercial strain of P. ostreatus in liquid and solid cultures, and on a commercial scale. The presence of caffeine inhibited mycelial growth on agar and in liquid culture in the laboratory. Increased levels of SCG in an SCG/sawdust substrate also delayed mycelial growth and delayed or prevented fruiting during commercial cultivation. Despite growth inhibition, partial degradation of caffeine to xanthine by P. ostreatus mycelium was observed in all SCG-containing substrate mixtures. Degradation of caffeine proceeded mainly via sequential N-demethylation to theophylline (1,3-dimethylxanthine) and 3-methylxanthine, although both paraxanthine and theobromine also accumulated in the substrate. Caffeine and its demethylated metabolites were also detected in fruiting bodies, but it was not clear whether caffeine metabolism occurred in the fruiting bodies themselves or whether caffeine metabolites were translocated there from the mycelium. Based on the caffeine concentrations measured in fruiting bodies after growth with SCG, it would be necessary to consume ~ 250 kg of fresh oyster mushrooms to obtain the amount of caffeine equivalent to one cup of espresso coffee, suggesting that the health impact of caffeine in these mushrooms is low. However, the ability of P. ostreatus to degrade caffeine indicates that this and other species in this genus may have potential applications in detoxification of coffee production wastes.

Phosphorus forms affect the hyphosphere bacterial community involved in soil organic phosphorus turnover.

Interactions between bacteria and arbuscular mycorrhizal (AM) fungi play a significant role in mediating organic phosphorus (P) transformations and turnover in soil. The bacterial community in soil is largely responsible for mobilization of the soil organic P pool, and the released P is taken up by extraradical AM hyphae, which mediate its use for plant growth. However, the functional microbiome involved in organic P mineralization in the hyphosphere remains poorly understood. The aim of this study was to determine how AM hyphae-associated bacterial communities related to P turnover in the hyphosphere of leek (Allium porrum) respond to different forms of soil P. Using a compartmented microcosm, leek was grown with the AM fungus Funneliformis mosseae, and the extraradical mycelium of F. mosseae was allowed to grow into a separate hyphal compartment containing either no added P, or P as KH2PO4 or phytin. High-throughput sequencing showed that the alkaline phosphatase (ALP)-harboring bacterial community associated with the AM hyphae was dominated by Sinorhizobium, Bradyrhizobium, Pseudomonas, and Ralstonia and was significantly changed in response to different P treatments, with Pseudomonas showing higher relative abundance in organic P treatments than in control and inorganic P treatments. Pseudomonas was also the major genus harboring the ß-propeller phytase (BPP) gene in the hyphosphere, but the BPP-harboring community structure was not affected by the presence of different P forms. These results demonstrate the profound differences in ALP- and BPP-harboring bacterial communities in the hyphosphere at bacterial genus level, providing new insights to link bacteria and biogeochemical P cycling driven in association with mycorrhizal hyphae.

Soil phoD and phoX alkaline phosphatase gene diversity responds to multiple environmental factors.

Alkaline phosphatases such as PhoD and PhoX are important in organic phosphorus cycling in soil. We identified the key organisms harboring the phoD and phoX genes in soil and explored the relationships between environmental factors and the phoD- and phoX-harboring community structures across three land uses located in arid to temperate climates on two continents using 454-sequencing. phoD was investigated using recently published primers, and new primers were designed to study phoX in soil. phoD was found in 1 archaeal, 13 bacterial and 2 fungal phyla, and phoX in 1 archaeal and 16 bacterial phyla. Dominant phoD-harboring phyla were Actinobacteria, Cyanobacteria, Deinococcus-Thermus, Firmicutes, Gemmatimonadetes, Planctomycetes and Proteobacteria, while abundant phoX-harboring phyla were Acidobacteria, Actinobacteria, Chloroflexi, Planctomycetes, Proteobacteria and Verrucomicrobia. Climate, soil group, land use and soil nutrient concentrations were the common environmental drivers of both community structures. In addition, the phoX-harboring community structure was affected by pH. Despite differences in environmental factors, the dominant phyla in the phoD-harboring community remained similar in all samples, while the composition of phoX differed substantially between the samples. This study shows that the composition of phoD and phoX is governed by the same environmental drivers but that phoD and phoX occur partly in different phyla.