BackgroundNothing is currently known about microbial composition of saline lakes of the Novosibirsk region and its dependence on physical-chemical parameters of waters. We studied the structure of microbial communities of saline lakes of the Novosibirsk region and the effect of physical-chemical parameters of waters on microbial communities of these lakes.ResultsAccording to the ion content, the lakes were classified either as chloride or chloride-sulfate types. Water salinity ranges from 4.3 to 290 g L−1. Many diverse microbial communities were found. Filamentous and colonial Cyanobacteria of the genera Scytonema, Aphanocapsa, and/or filamentous Algae dominated in littoral communities. Spatial and temporal organization of planktonic microbial communities and the quantities of Archaea and Bacteria were investigated using fluorescent in situ hybridization. We have found that the dominant planktonic component is represented by Archaea, or, less frequently, by Bacteria. Various phylogenetic groups (Bacteria, Archaea, Algae, and Cyanobacteria) are nonuniformly distributed. The principal component analysis was used to detect environmental factors that affect microorganism abundance. We found the principal components responsible for 71.1 % of the observed variation. It was demonstrated that two-block partial least squares was a better method than principal component analysis for analysis of the data. We observed general relationships between microbial abundance and water salinity.ConclusionsWe have performed the first-ever study of the structure of the microbial communities of eleven saline lakes in the Novosibirsk region along with their physical-chemical parameters of waters. Our study demonstrates that saline lakes in the Novosibirsk region contain a unique microbial communities that may become a prolific source of microorganisms for fundamental and applied studies in various fields of ecology, microbiology, geochemistry, and biotechnology, and deserve further metagenomic investigation.
BackgroundMicrobial mats are a good model system for ecological and evolutionary analysis of microbial communities. There are more than 20 alkaline hot springs on the banks of the Barguzin river inflows. Water temperature reaches 75 °C and pH is usually 8.0–9.0. The formation of microbial mats is observed in all hot springs. Microbial communities of hot springs of the Baikal rift zone are poorly studied. Garga is the biggest hot spring in this area.ResultsIn this study, we investigated bacterial and archaeal diversity of the Garga hot spring (Baikal rift zone, Russia) using 16S rRNA metagenomic sequencing. We studied two types of microbial communities: (i) small white biofilms on rocks in the points with the highest temperature (75 °C) and (ii) continuous thick phototrophic microbial mats observed at temperatures below 70 °C. Archaea (mainly Crenarchaeota; 19.8% of the total sequences) were detected only in the small biofilms. The high abundance of Archaea in the sample from hot springs of the Baikal rift zone supplemented our knowledge of the distribution of Archaea. Most archaeal sequences had low similarity to known Archaea. In the microbial mats, primary products were formed by cyanobacteria of the genus Leptolyngbya. Heterotrophic microorganisms were mostly represented by Actinobacteria and Proteobacteria in all studied samples of the microbial mats. Planctomycetes, Chloroflexi, and Chlorobi were abundant in the middle layer of the microbial mats, while heterotrophic microorganisms represented mostly by Firmicutes (Clostridia, strict anaerobes) dominated in the bottom part. Besides prokaryotes, we detect some species of Algae with help of detection their chloroplasts 16 s rRNA.ConclusionsHigh abundance of Archaea in samples from hot springs of the Baikal rift zone supplemented our knowledge of the distribution of Archaea. Most archaeal sequences had low similarity to known Archaea. Metagenomic analysis of microbial communities of the microbial mat of Garga hot spring showed that the three studied points sampled at 70 °C, 55 °C, and 45 °C had similar species composition. Cyanobacteria of the genus Leptolyngbya dominated in the upper layer of the microbial mat. Chloroflexi and Chlorobi were less abundant and were mostly observed in the middle part of the microbial mat. We detected domains of heterotrophic organisms in high abundance (Proteobacteria, Firmicutes, Verrucomicrobia, Planctomicetes, Bacteroidetes, Actinobacteria, Thermi), according to metabolic properties of known relatives, which can form complete cycles of carbon, sulphur, and nitrogen in the microbial mat. The studied microbial mats evolved in early stages of biosphere formation. They can live autonomously, providing full cycles of substances and preventing live activity products poisoning.
Fractions of neurospecific S-100 protein were purified from bovine brain and their physicochemical properties were studied. Conformational changes caused by the binding of calcium to S-100 protein fractions were detected by means of differential and fluorescence spectroscopy. Fractions demonstrating opposite shifts of their spectra also differ in the distribution in double-phase system. The number of calcium-binding centers and their association. The nature of the differences in the interaction of various S-100 protein fractions with calcium is discussed.
1. Data on the presence of S-100 protein in synaptic endings are revised, and evidence is given in favor of its localization inside mouse brain cortex synaptosomes and on the surface of their external membrane. 2. For identification of the S-100-specific polypeptide, proteins of external synaptosomal membranes were iodinated with lactoperoxidase fixed on cyanogen bromide (CNBr)-Sepharose, and after synaptosome lysis S-100-positive material was isolated by means of affinity chromatography antibodies to S-100 protein (a-S-100)-Sepharose. The molecular weight of the polypeptide obtained corresponded to that of S-100 subunits (10 kD), and iodine incorporation pointed to its localization on the surface of synaptosomal membranes. 3. With the help of antibodies labeled with horseradish peroxidase (a-S-100-HP) or 125I (a-S-100-125I), which do not penetrate into noninjured synaptosomes, the amount of S-100 protein on synaptosomal membranes was found to be 18.5 ng/mg total protein (as assayed with a-S-100-HP) or 95.33 ng/mg (as assayed with a-S-100-125I). 4. At the same time, the total S-100 protein content in synaptosomes measured by means of radioimmune analysis after their complete lysis turned out to be 284 +/- 0.84 ng/mg, i.e., a part of S-100 seemed to be inside synaptosomes. 5. Cosedimentation of water-soluble S-100 protein with the synaptosomal fraction during isolation was insignificant. Prefixation with glutaraldehyde or paraformaldehyde decreased the amount of material reacting with antibodies, possibly due to steric effects or denaturation of active centers. This could have influenced the earlier attempts to detect S-100 protein in synapses. Treatment of nonfixed synaptosomes with a conjugate of a-S-100 with colloidal gold made it possible to detect S-100-positive material on pre- and postsynaptic membranes, which confirms the biochemical data.
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