Due to their small size, microorganisms directly experience only a tiny portion of the environmental heterogeneity manifested in the soil. The microscale variations in soil properties constrain the distribution of fungi and bacteria, and the extent to which they can interact with each other, thereby directly influencing their behavior and ecological roles. Thus, to obtain a realistic understanding of bacterial–fungal interactions, the spatiotemporal complexity of their microenvironments must be accounted for. The objective of this review is to further raise awareness of this important aspect and to discuss an overview of possible methodologies, some of easier applicability than others, that can be implemented in the experimental design in this field of research. The experimental design can be rationalized in three different scales, namely reconstructing the physicochemical complexity of the soil matrix, identifying and locating fungi and bacteria to depict their physical interactions, and, lastly, analyzing their molecular environment to describe their activity. In the long term, only relevant experimental data at the cell-to-cell level can provide the base for any solid theory or model that may serve for accurate functional prediction at the ecosystem level. The way to this level of application is still long, but we should all start small.

Background and Aims: Pinus cembra represent a typical and important tree species growing in European subalpine and alpine habitats. The ectomycorrhizal (ECM) fungal communities associated to this tree under natural conditions are largely unknown. Methods: In this study, we investigated the ECM fungal abundance and composition at four high-altitude sites (two northern-exposed and two southern-exposed habitats) in South Tyrol (Italy), and included also two different age classes of P. cembra. The ECM partners were characterized morphologically, and identified by rDNA ITS sequence analysis. Results: The degree of mycorrhization in adult P. cembra was typically 100% in these natural habitats, with a total species diversity of 20 ECM species. The four high-altitude sites were similar concerning their species richness and mycobiont diversity, but they differed significantly in ECM species composition. Young P. cembra had a mycorrhization degree of 100% and a total of 10 species were observed. All mycorrhizal partners of naturally regenerated young P. cembra were only detected in one specific location, with the exception of Cenococcum sp. and Amphinema sp. which were detected at two sites. Young trees harbour a distinct ectomycorrhizal fungal diversity, which is clearly lower than the diversity detected in adult P. cembra trees. The P. cembra bolete (Suillus plorans) is the most important symbiotic partner of P. cembra at Southern Tyrolean high-altitude sites and is known for its strict, species-specific host association. Conclusions: The ectomycorrhizal fungal community composition strongly depends on geographic region and on the slope exposure (north or south) of the site.

Fervidobacterium pennivorans subsp. keratinolyticus subsp. nov. strain T was isolated from a terrestrial, high-altitude hot spring in Tajikistan. This strain is an obligate anaerobic rod and their cells occur singly, in pairs, or as short chains under the optimal growth conditions of a temperature of 65 °C and pH 6.5, with peptone, glucose, and galactose as the preferred substrates. The minimum generation time of this strain is 150 min. Strain T can efficiently degrade feather keratin at 65–75 °C; this unusual feature is also exhibited by a few other members of the Fervidobacterium genus. The total genome size of this bacterial strain is 2,002,515 base pairs, with a C + G content of 39.0%. The maximum digital DNA–DNA hybridization (dDDH) value of 76.9% was observed on comparing the genome of this strain with that of Fervidobacterium pennivorans type strain DSM9078. This study describes the physiological and genomic properties of strain T, with an emphasis on its keratinolytic power and differences from other members of the genus Fervidobacterium.

Calcareous glacier forefields challenge prevailing ecological frameworks on microbial biodiversity and community assembly due to their unique bedrock. Early stages of soil development in these environments are notorious for their high turnover rates, demanding a high degree of replication for obtaining conclusive data. However, studies across different calcareous glaciers are still missing. Here, we robustly investigated both bacterial and fungal diversity, association networks, and assembly processes in four calcareous glacier forefields of the Alps, focusing on the earliest soil developmental stages (<25 years) early in the snow-free season. We found a diverse community of bacteria and fungi, potentially involved in P and N nutrient cycling. A core microbiome existing across all four locations suggests that certain microbes might be more successful colonizers of these ecosystems than others. Nearest taxon index revealed phylogenetically clustered microbial communities. These findings suggest that the distribution and colonization of some microbes were influenced by selective forces such as geography and climate during the early stages of soil development in calcareous glaciers. Interestingly, there were no common bacterial-fungal associations across the four locations, indicating that this habitat does not select for specific bacterial-fungal associations and that associations were driven by neutral processes. We discuss microbial communities and their interactions in these special calcareous glacier forefield habitats. Moreover, we present innovative approaches for studying microbial assembly that address both deterministic, intrinsic drivers, like specific microbial traits, and stochastic, extrinsic drivers, such as the opportunistic behavior of microbes. IMPORTANCE: Our study is based on three fundamental and unique approaches: (i) we utilize the early stages of soil development in four glacier forefields across the Alpine range. This design implies high replicability in a natural setting, which is crucial for drawing general conclusions. (ii) Our study investigates glacier forefields with calcareous bedrock directly after snowmelt. These habitats and periods remain surprisingly underexplored. (iii) Our results underline the relevance of bacterial-fungal associations in microbial community assembly alongside dispersal, drift, and natural selection. Taken together, our study provides new insights into the development of complex microbial communities, their stabilization and predictability, including ecological implications.

This atlas aims to provide an overview of the picocyanobacteria cultures hold by the CNR-IRSA collection. These are monoclonal strains mostly of the genera Synechococcus and Cyanobium. These strains were mainly isolated from lakes of different trophic status around the globe and, so far, they are not available in other collections of algae and (pico)cyanobacteria. Here we summarise the main characteristics of these strains, including some previously published data, and offer most of the strains as material available for research to every scientists upon request.