Many of the world's peatlands have been affected by water table drawdown and subsequent loss of organic matter. Rewetting has been proposed as a measure to restore peatland functioning and to halt carbon loss, but its effectiveness is subject to debate. An important prerequisite for peatland recovery is a return of typical microbial communities, which drive key processes. To evaluate the effect of rewetting, we investigated 13 fen peatland areas across a wide (>1500 km) longitudinal gradient in Europe, in which we compared microbial communities between drained, undrained, and rewetted sites. There was a clear difference in microbial communities between drained and undrained fens, regardless of location. Community recovery upon rewetting was substantial in the majority of sites, and predictive functional profiling suggested a concomitant recovery of biogeochemical peatland functioning. However, communities in rewetted sites were only similar to those of undrained sites when soil organic matter quality (as expressed by cellulose fractions) and quantity were still sufficiently high. We estimate that a minimum organic matter content of ca. 70% is required to enable microbial recovery. We conclude that peatland recovery after rewetting is conditional on the level of drainage-induced degradation: severely altered physicochemical peat properties may preclude complete recovery for decades.

• MeSH
• mikrobiota * MeSH
• mokřady * MeSH
• půda MeSH
• uhlík analýza   MeSH
• Publikační typ
• časopisecké články MeSH
• práce podpořená grantem MeSH
• Geografické názvy
• Evropa MeSH

Climate change and human pressures are changing the global distribution and the extent of intermittent rivers and ephemeral streams (IRES), which comprise half of the global river network area. IRES are characterized by periods of flow cessation, during which channel substrates accumulate and undergo physico-chemical changes (preconditioning), and periods of flow resumption, when these substrates are rewetted and release pulses of dissolved nutrients and organic matter (OM). However, there are no estimates of the amounts and quality of leached substances, nor is there information on the underlying environmental constraints operating at the global scale. We experimentally simulated, under standard laboratory conditions, rewetting of leaves, riverbed sediments, and epilithic biofilms collected during the dry phase across 205 IRES from five major climate zones. We determined the amounts and qualitative characteristics of the leached nutrients and OM, and estimated their areal fluxes from riverbeds. In addition, we evaluated the variance in leachate characteristics in relation to selected environmental variables and substrate characteristics. We found that sediments, due to their large quantities within riverbeds, contribute most to the overall flux of dissolved substances during rewetting events (56%-98%), and that flux rates distinctly differ among climate zones. Dissolved organic carbon, phenolics, and nitrate contributed most to the areal fluxes. The largest amounts of leached substances were found in the continental climate zone, coinciding with the lowest potential bioavailability of the leached OM. The opposite pattern was found in the arid zone. Environmental variables expected to be modified under climate change (i.e. potential evapotranspiration, aridity, dry period duration, land use) were correlated with the amount of leached substances, with the strongest relationship found for sediments. These results show that the role of IRES should be accounted for in global biogeochemical cycles, especially because prevalence of IRES will increase due to increasing severity of drying events.

• MeSH
• biofilmy růst a vývoj   MeSH
• biologická dostupnost MeSH
• dusičnany analýza   MeSH
• geologické sedimenty chemie   MeSH
• klimatické změny MeSH
• listy rostlin chemie   MeSH
• organické látky analýza   MeSH
• podnebí MeSH
• řeky chemie   MeSH
• živiny analýza   MeSH
• Publikační typ
• časopisecké články MeSH
• práce podpořená grantem MeSH

Zygnema is a genus of filamentous green algae belonging to the class of Zygnematophyceae (Streptophyta). In the Arctic, it typically forms extensive mats in habitats that regularly dry out during summer, and therefore, mechanisms of stress resistance are expected. We investigated its natural populations with respect to production of specialized desiccation-resistant cells and osmotic acclimation. Six populations in various stages of natural desiccation were selected, from wet biomass floating in water to dried paper-like crusts. After rewetting, plasmolysis and osmotic stress effects were studied using hypertonic sorbitol solutions, and the physiological state was estimated using chlorophyll a fluorescence parameters. All populations of Zygnema sp. formed stationary-phase cells filled with storage products. In green algal research, such cells are traditionally called akinetes. However, the populations differed in their reaction to osmotic stress. Whereas the wet-collected samples were strongly impaired, the osmotic stress resistance of the naturally dried samples was comparable to that of true aeroterrestrial algae. We showed that arctic populations of Zygnema acclimate well to natural desiccation via hardening that is mediated by slow desiccation. As no other types of specialized cells were observed, we assume that the naturally hardened akinetes also play a key role in winter survival.

• MeSH
• chlorofyl metabolismus   MeSH
• ekosystém MeSH
• fluorescenční mikroskopie MeSH
• fyziologická adaptace MeSH
• fyziologický stres * MeSH
• osmotický tlak MeSH
• vysoušení MeSH
• Zygnematales fyziologie   MeSH
• Publikační typ
• časopisecké články MeSH
• práce podpořená grantem MeSH
• Geografické názvy
• Arktida MeSH
• Svalbard MeSH

Soil aggregates between 2 and 5 mm from 35- and 45-year-old unreclaimed post-mining sites near Sokolov (Czech Republic) were divided into two groups: spherical and prismatic. X-ray tomography indicated that prismatic aggregates consisted of fragments of claystone bonded together by amorphous clay and roots while spherical aggregates consisted of a clay matrix and organic fragments of various sizes. Prismatic aggregates were presumed to be formed by plant roots and physical processes during weathering of Tertiary mudstone, while earthworms were presumed to contribute to the formation of spherical aggregates. The effects of drying and rewetting and glucose addition on microbial respiration, microbial biomass, and counts of bacteria in these aggregates were determined. Spherical aggregates contained a greater percentage of C and N and a higher C-to-N ratio than prismatic ones. The C content of the particulate organic matter was also higher in the spherical than in the prismatic aggregates. Although spherical aggregates had a higher microbial respiration and biomass, the growth of microbial biomass in spherical aggregates was negatively correlated with initial microbial biomass, indicating competition between bacteria. Specific respiration was negatively correlated with microbial biomass. Direct counts of bacteria were higher in spherical than in prismatic aggregates. Bacterial numbers were more stable in the center than in the surface layers of the aggregates. Transmission electron microscopy indicated that bacteria often occurred as individual cells in prismatic aggregates but as small clusters of cells in spherical aggregates. Ratios of colony forming units (cultivatable bacteria) to direct counts were higher in spherical than in prismatic aggregates. Spherical aggregates also contained faster growing bacteria.

• MeSH
• biomasa MeSH
• fyziologie bakterií MeSH
• hornictví MeSH
• Oligochaeta fyziologie   MeSH
• půda chemie   MeSH
• půdní mikrobiologie MeSH
• zvířata MeSH
• Check Tag
• zvířata MeSH
• Publikační typ
• časopisecké články MeSH
• práce podpořená grantem MeSH

Cyanobacteria form extensive macroscopic mats in shallow freshwater environments in the High Arctic and Antarctic. In these habitats, the communities are exposed to seasonal freezing and desiccation as well as to freeze-thawing and drying-rewetting cycles. Here, we characterized the annual cycles of two Phormidium communities in very shallow seepages located in central Svalbard. We observed the structure of the communities and the morphology, ultrastructure, metabolic activity, and viability of filaments and single cells. The communities overwintered as frozen mats, which were formed by long filaments enclosed in thick multilayered polysaccharide sheaths. No morphologically and/or ultrastructurally distinct spore-like cells were produced for surviving the winter, and the winter survival of the communities was not provided by a few resistant cells, which did not undergo visible morphological and ultrastructural transformations. Instead, a high proportion of cells in samples (85%) remained viable after prolonged freezing. The sheaths were the only morphological adaption, which seemed to protect the trichomes from damage due to freezing and freeze-associated dehydration. The cells in the overwintering communities were not dormant, as all viable cells rapidly resumed respiration after thawing, and their nucleoids were not condensed. During the whole vegetative season, defined by the presence of water in a liquid state, the communities were constantly metabolically active and contained <1% of dead and injured cells. The morphology and ultrastructure of the cells remained unaltered during observations throughout the year, except for light-induced changes in thylakoids. The dissemination events are likely to occur in spring as most of the trichomes were split into short fragments (hormogonia), a substantial proportion of which were released into the environment by gliding out of their sheaths, as well as by cracking and dissolving their sheaths. The short fragments subsequently grew longer and gradually produced new polysaccharide sheaths.

• MeSH
• ekosystém * MeSH
• mikrobiální viabilita MeSH
• mikrobiologie vody MeSH
• roční období MeSH
• sinice růst a vývoj   metabolismus   fyziologie   ultrastruktura   MeSH
• sladká voda chemie   mikrobiologie   MeSH
• teplota MeSH
• zmrazování MeSH
• Publikační typ
• časopisecké články MeSH
• práce podpořená grantem MeSH
• Geografické názvy
• Antarktida MeSH
• Arktida MeSH
• Svalbard MeSH

The textbook focuses on basic and clinical science, ophthalmology, optics, refraction, and contact lenses. Intended for professional public and for university students.

• MeSH
• klinické lékařství MeSH
• kontaktní čočky MeSH
• oftalmologie MeSH
• optika a fotonika MeSH
• refrakce oka MeSH
• věda MeSH

• Konspekt
• Ortopedie. Chirurgie. Oftalmologie
• Učební osnovy. Vyučovací předměty. Učebnice
• NLK Obory
• oftalmologie
• věda a výzkum
• NLK Publikační typ
• učebnice vysokých škol

A quantitative real-time PCR (qPCR) marker Ta0 with hydrolysis probe ("TaqMan"), targeted to the internal transcribed spacer region of the ribosomal DNA, has been developed for quantification of summer truffle (Tuber aestivum) mycelium. Gene copy concentrations determined by the qPCR were calibrated against pure culture mycelium of T. aestivum, enabling quantification of the mycelium in soil and in host roots from the fields. Significant concentrations of the fungus were observed not only in the finest roots with ectomycorrhizae but also in other root types, indicating that the fungus is an important component of the microbial film at the root surface. The concentration of T. aestivum in soil is relatively high compared to other ectomycorrhizal fungi. To evaluate the reliability of the measurement of the soil mycelium density using qPCR, the steady basal extracellular concentration of the stabilized T. aestivum DNA should be known and taken into account. Therefore, we addressed the stability of the qPCR signal in soil subjected to different treatments. After the field soil was sieved, regardless of whether it was dried/rewetted or not, the T. aestivum DNA was quickly decomposed. It took just about 4 days to reach a steady concentration. This represents a conserved pool of T. aestivum DNA and determines detection limit of the qPCR quantification in our case. When the soil was autoclaved and recolonized by saprotrophic microorganisms, this conserved DNA pool was eliminated and the soil became free of T. aestivum DNA.

• MeSH
• Ascomycota genetika   růst a vývoj   izolace a purifikace   MeSH
• DNA fungální genetika   MeSH
• kořeny rostlin mikrobiologie   MeSH
• kvantitativní polymerázová řetězová reakce metody   MeSH
• mycelium genetika   růst a vývoj   izolace a purifikace   MeSH
• mykorhiza genetika   růst a vývoj   izolace a purifikace   MeSH
• půdní mikrobiologie MeSH
• Publikační typ
• časopisecké články MeSH
• hodnotící studie MeSH
• práce podpořená grantem MeSH