Ultrastructural and cytochemical aspects of the interaction between the ectomycorrhizal fungus Laccaria laccata and the saprotrophic fungi, Trichoderma harzianum and T. virens

Different interactions between soil fungi competing in the rhizosphere with each other are necessary to understand their influence on plant growth and health. The interactions between the ectomycorrhizal (ECM) fungus Laccaria laccata and soil saprotrophic fungi (T. harzianum, T. virens) were studied by transmission electron microscopy, and by gold cytochemistry to assess the potential role of cell wall lytic enzymes in mycoparasitism. Anti-β-1,3-glucan antibody, WGA/ovomucoid-gold complex and PATAg test were used to localize β-1,3-glucan, chitin and polysaccharides. Cytoplasm disorganisation of the saprotrophic fungi occurred concurrently with dissolution of β-1,3-glucan in walls of hyphae and conidia of the saprotrophic fungi. Then digestion of polysaccharides and chitin of colonised fungal structures occurred. The studies suggest sequential contribution of cell wall lytic enzymes and importance of disturbing the host's cell integrity during mycoparasitism. We conclude that the ECM fungus can parasitise on the saprotrophic fungi not only in dual culture on artificial medium but also in the rhizosphere of Scots pine.     

Geographical distribution ofSporidesmium goidanichii in pine forests of Japan

The geographical distribution of a saprotrophic hyphomycete,Sporidesmium goidanichii was studied in pine forests of Japan. Using the data of 282 fungal communitles of pine leaf litter collected over a wide range of climatic conditions, the relationships among two indexes of distribution of the species (constancy and abundance) and three climatic variables were analyzed by the multiple regression analysis. The results demonstrated that the mean annual air temperature and the mean annual range (the difference in monthly mean air temperatures between the coldest and warmest months at the study sites) were necessary variables for the prediction of the values of indexes ofS. goidanichii in pine forests of Japan, while the mean annual precipitation was an unimportant factor. The distribution patterns of the fungus along the gradients of two temperature variables were analyzed graphically. The fungus has an optimal climatic area with high values of indexes where is restricted to the center of the warm temperate regions of the main islands. The relationship between the life strategy of the fungus and its temperature-dependent distribution pattern in Japan was also discussed. Contributions to Sugadaira Montane Research Center No. 179.     

Phylogenetic similarity and structure of Agaricomycotina communities across a forested landscape

The Agaricomycotina are a phylogenetically diverse group of fungi that includes both saprotrophic and mycorrhizal species, and that form species – rich communities in forest ecosystems. Most species are infrequently observed, and this hampers assessment of the role that environmental heterogeneity plays in determining local community composition and in driving β‐diversity. We used a combination of phenetic (TRFLP) and phylogenetic approaches [Unifrac and Net Relatedness Index (NRI)] to examine the compositional and phylogenetic similarity of Agaricomycotina communities in forest floor and surface soil of three widely distributed temperate upland forest ecosystems (one, xeric oak – dominated and two, mesic sugar maple dominated). Generally, forest floor and soil communities had similar phylogenetic diversity, but there was little overlap of species or evolutionary lineages between these two horizons. Forest floor communities were dominated by saprotrophic species, and were compositionally and phylogenetically similar in all three ecosystems. Mycorrhizal species represented 30% to 90% of soil community diversity, and these communities differed compositionally and phylogenetically between ecosystems. Estimates of NRI revealed significant phylogenetic clustering in both the forest floor and soil communities of only the xeric oak‐dominated forest ecosystem, and may indicate that this ecosystem acts as a habitat filter. Our results suggest that environmental heterogeneity strongly influences the phylogenetic β‐diversity of soil inhabiting Agaricomycotina communities, but has only a small influence on forest floor β‐diversity. Moreover, our results suggest that the strength of community assembly processes, such as habitat filtering, may differ between temperate forest ecosystems.     

Carbon sources for the Palaeozoic giant fungus Prototaxites inferred from modern analogues

A wide range of carbon isotope values in the Devonian fossil Prototaxites has been interpreted to support heterotrophy and the classification of Prototaxites as a giant fungus. This inference remains controversial because of the huge size of Prototaxites relative to co-occurring terrestrial vegetation and the lack of existing fungal analogues that display equally broad isotopic ranges. Here, we show wide isotopic variability in the modern saprotrophic fungus Arrhenia obscurata collected adjacent to shallow meltwater pools of a sparsely vegetated glacial succession in the Washington Cascades, USA. Soils collected specifically around the edges of these pools were up to 5‰ higher in δ¹³C than adjacent soils consistent with C₃ origin. Microbial sources of primary production appear to cause these high δ¹³C values, and the environment may be analogous to that of the Early Devonian landscapes, where Prototaxites individuals with extreme isotopic variance were found. Carbon isotopes are also compared in Prototaxites, Devonian terrestrial vascular plants, and Devonian algal-derived lake sediments. Prototaxites isotopic values show little correspondence with those of contemporaneous tracheophytes, providing further evidence that non-vascular land plants or aquatic microbes were important contributors to its carbon sources. Thus, a saprotrophic fungal identity is supported for Prototaxites, which may have relied on deposits of algal-derived organic matter in floodplain environments that were less dominated by vascular plants than a straight reading of the macrofossil record might suggest.     

Carbon and nutrients of indigestible pollen are transferred to zooplankton by chytrid fungi

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