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This article presents the results of microscopic fungi complexes in the areas of five Russian polar stations in East Antarctica and the Subantarctic. A total of 104 microfungal species have been identified. Seventyseven fungal species have been detected in samples of soils and anthropogenic materials from polar stations of East Antarctica (Progress, Mirny, Molodezhnaya, and Druzhnaya 4) using mycological methods while, in the Bellingshausen station (Subantarctic), we have isolated 87 micromycete species. The number of fungi in soils varies from individual propagules in control soils to 94000 per 1 g of soil in contaminated areas. The largest number of species is represented by the genus Penicillium (26 species). Fungal species that form the core of mycobiota in most of the studied habitats have been identified. For soils of East Antarctica, it is formed by species of the genera Aureobasidium, Cadophora, Pseudogymnoascus (Geomyces), Thelebolus, and Phoma. Significant differences are established between the mycobiota of East Antarctica and that of the Subantarctic. At the same time, a general trend towards an increase in fungal species diversity and number in the areas of polar stations compared to the control (clean) sites for all studied areas is recorded. These data indicate that a significant part of micromycetes is introduced into the Antarctic by humans (anthropogenic invasion).

Soil fungal pathogens are the most common cause of diseases in commercial strawberry crops worldwide. Since simultaneous infections by different pathogens can severely damage the crop, understanding the associated fungal communities can be helpful to mitigate crop loss. Herein, we used Illumina metabarcoding to assess the structure of fungal communities in five strawberry production areas in Estonia. Our analysis revealed 990 to 1430 operational taxonomic units (OTUs) per soil sample (pools of eight soil samples per production area). Based on our analyses, Ascomycota (55.5%) and Basidiomycota (25.0%) were the most OTUs-rich. Amongst the 24 most abundant OTUs, Geomyces, Rhodotorula, Verticillium and Microdochium were the most abundant genera, which were found across nearly all the soil samples. The OTUs were also clustered into three distinct groups, corresponding to different functional guilds of fungi. In addition, Fusarium solani, V. dahliae, Rhizoctonia solani and Colletotrichum truncatum were enormously abundant in the fields with disease symptoms, whereas arbuscular mycorrhizal fungi especially Rhizophagus irregularis were considerably more abundant in the fields with healthy plants. These findings provide support that mycorrhizal fungi may play an important role in suppressing pathogens. Our study for the first time shows the usefulness of Illumina technology in surveying the communities of soil fungi in strawberry fields effectively, which may improve available disease management strategies against strawberry diseases.

Original Russian Text © K.A. Kravchenko, A.S. Vlashchenko, O.V. Prilutskii, A.S. Prilutskaya, 2015, published in Ekologiya, 2015, No. 5, pp. 397–400.

Comparative characterization of Geomyces isolates was performed. The isolates were obtained from Arctic cryopegs and the surrounding ancient marine deposits, from nonsaline permafrost soils, and from temperate environments. Microbiological (cultural and morphological) and molecular criteria were used to confirm the identification of the isolates as Geomyces pannorum. The isolates from cryopegs and surrounding marine deposits were shown to differ from those obtained from nonsaline soils and temperate environments in their ability to grow at negative temperatures (−2°C) under increased salt concentration (10%). The results are discussed in relation to the possible inheritance of the adaptive characteristics acquired in specific environments.

The difference between fungal communities in the cultural layer of a medieval settlement and in the background soddy calcareous soil is shown. In the cultural layer, the portion of spores, especially large spores (d > 6 µ m), in the total fungal biomass is increased, whereas the portion of mycelium, especially with a thick- ness of > 4 µ m, is decreased. The species composition of micromycetes in the cultural layer is also transformed; species from the Aspergillus and Fusarium genera predominate. The frequency and diversity of Penicillium rep- resentatives decreases, whereas the fungal species from the Phoma, Doratomyces, Geomyces , and Verticillium genera, which are not typical of the background soil horizons, increases. The diversity of the minor fungal spe- cies also increases in the cultural layer. An increased content of keratin-decomposing soil fungi is found in the cultural layer. It is argued that the use of the entire set of these characteristics makes it possible to perform mycological indication of the parts of the cultural layer that served different purposes (ancient streets, house floors, backing of the walls, etc.) within the settlement.