Microbial origin of phenylcarboxylic acids in the human body

In previous studies we demonstrated increased amounts of phenylcarboxylic acids (PCA) in serum of patients with sepsis. This observation prompted the present study of the ability of the human microbiome bacteria to produce PCA in vitro. PCA were detected in culture media by gas chromatography-mass spectrometry. Increased amounts of phenyllactic and p-hydroxyphenyllactic acids were produced by Klebsiella pneumonia, Escherichia coli, and Staphylococcus aureus. Certain strict anaerobes (bifidobacteria, lactobacteria, eubacteria) have also been found to actively produce these PCA, but these bacteria are not etiologically linked to sepsis. Thus our results demonstrate the ability of sepsis-related bacteria to produce PCA and provide experimental support for the theory that the accumulation of PCA in the blood of patients with sepsis results from microbial degradation of phenylalanine and tyrosine.     

Preparation and analysis of biological activity of the secreted proteins of the Noggin family

Methods for preparation of recombinant physiologically active proteins of the Noggin family (Noggin1 and Noggin2) of the clawed frog Xenopus laevis that are capable of interaction with BMP factors of the TGF-beta superfamily have been developed. Structures were designed for the expression of Noggin1 and Noggin2 proteins allowing us to produce them from the directly microinjected synthetic mRNA in the cells of developing embryos of the clawed frog, as well as in the prokaryotic expression system. Target proteins contained three Myc-epitopes at the N-terminal. Introduction of these’ tags’ allowed comparison of the expression level of the Noggin1 and Noggin2 proteins, isolation on the affinity immunosorbent, and demonstration of biological activity of the isolated Noggin-proteins through the analysis of their ability to bind the BMP4 factor of the TGF-beta superfamily with coimmunoprecipitation method.     

Microbial Processes of the Carbon and Sulfur Cycles in Lake Mogil'noe

In the beginning of the summer of 1999, complex microbiological and biogeochemical investigations of meromictic Lake Mogil'noe (Kil'din Island, Barents Sea) were carried out. The analysis of the results shows a clearly pronounced vertical zonality of the microbial processes occurring in the water column of the lake. To a depth of 8 m, the total number and activity of microorganisms was limited by the relatively low content of organic matter (OM). In the upper part of the hydrogen-sulfide zone of the lake (beginning at a depth of 8.25 m), the content of particulate OM and the microbial number sharply increased. In this zone, the daily production of OM during anaerobic photosynthesis at the expense of massive development of colored sulfur bacteria reached 620 mg C/m², which was twofold greater than the daily production of phytoplankton photosynthesis and led to a considerable change in the isotopic composition (¹³C) of the particulate OM. In the same intermediate layer, the highest rates of sulfate reduction were recorded, and fractionation of stable sulfur isotopes occurred. Below 10 m was the third hydrochemical zone, characterized by maximum concentrations of H₂S and CH₄and by a relatively high rate of autotrophic methanogenesis. The comparison of the results obtained with the results of investigations of previous years, performed in the end of summer, shows a decrease in the intensity of all microbial processes inspected. An exception was anoxygenic photosynthesis, which can utilize not only the de novo formed H₂S but also the H₂S accumulated in the lake during the winter period.     

The Process of Microbial Sulfate Reduction in Sediments of the Coastal Zone and Littoral of the Kandalaksha Bay of the White Sea

Microbiological and biogeochemical investigations of the coastal zone and the littoral of the Kandalaksha Bay of the White Sea were carried out. The material for investigations was obtained in the series of expeditions of the Institute of Microbiology, Russian Academy of Sciences, in August 1999, 2000, 2001, and in March 2003. The studies were conducted on the littoral and in the water area of the Kandalaksha Preserve, the Moscow University Belomorsk Biological Station, and the Zoological Institute Biological Station, Russian Academy of Sciences. Sediment sampling on the littoral was carried out in the typical microlandscapes differing in the sediment properties and macrobenthos distribution. The maximal sulfate reduction rate (SRR) was shown for the shallow part of the Chernorechenskaya Bay (up to 2550 g S/(dm³ day)) and in the Bab'ye More Bay (up to 3191 g S/(dm³ day)). During the winter season, at a temperature of –0.5 × 0.5°C, the SRR in the sediments of the Kartesh Bay was 7.9 × 13 g S/(dm³ day). In the widest limits, the SRR values varied in the sediment cores sampled on the littoral. The minimal values (11 g S/(dm³ day)) were obtained in the core samples on the silt–sandy littoral. The littoral finely dispersed sediments rich in organic matter were characterized by high SRR values (524–1413 g S/(dm³ day)). The maximal SRR values were shown for the sediments present within the stretch of decomposing macrophytes, in local pits at the lower littoral waterline, and in the mouth of a freshwater stream (51–159 mg S/(dm³ day)). A sharp difference in the level of H₂S production in the type microlandscapes was shown. The average hydrogen sulfide production in finely dispersed sediments constituted 125 mg S/(m² day); in stormy discharge deposits, 1950 mg S/(m² day); in depressions under stones and in silted pits, 4300 mg S/(m² day). A calculation made with regard to the area of microlandscapes with increased productivity shows that the daily H₂S production per 1 km² of the littoral (August) is 60.8 to 202 kg S/(km² day), while the organic carbon consumption for sulfate reduction per 1 km² of the littoral is 46 to 152 kg C_org/(km² day).     

The formation and role of β-amyloid peptides in neurons upon amyloidosis

The mechanism of amyloid peptide formation in normally functioning neuron and upon the development of amyloidosis resulting in neuronal death is described. Amyloid peptides are formed by enzymatic processing of a large protein precursor and participate in intermolecular interactions after conformational rearrangements resulting in the formation of pathogenic structures. They enter into the cascade of molecular and cellular events leading to amyloidosis and death of neuronal cells. These molecular events clarify the relation between the conformation and function of neuropathogenic peptides and the role of this relation in the development of pathology of differentiated neurons.     

Microbiological Explorations in the Northern Part of the Barents Sea in Early Winter

The total number of microorganisms and rates of microbial processes of the carbon cycle were determined in snow, sea ice, water, and seafloor sediments of the northern part of the Barents Sea from September to October, 1998. The explorations were carried out in two areas: along the transection from Franz Josef Land to Victoria Island and along the continental slope region covered with solid ice at latitude 81°–82° N and longitude 37°–39° E. At the time of study, the ice cover was represented by thick one-year old ice (up to 1.2 m), perennial ice (up to 1.85 m), and pack ice. The number of bacteria in the snow cover, sea ice, and seawater was 12 to 14, 50 to 110, and 10 to 240 × 10³ cells/ml, respectively. Rates of dark CO₂ assimilation, glucose utilization, and methane oxidation by bacteria were determined. The highest rate of microbial processes was found in samples of the lowermost newly formed sea ice. The lowest level of activity for all processes was observed in melted snow water. A direct relation was shown between the concentration of C_org, the bacterial biomass, and the values of ¹³C_org in mixtures of melted snow and ice. The number of microorganisms and rates of microbial processes in seafloor sediments measured at the stations on the continental slope are comparable to those in the central part of the Barents Sea and the northern part of the Kara Sea.     

Effect of phenolic acids of microbial origin on production of reactive oxygen species in mitochondria and neutrophils

Cardiovascular death is frequently associated with atherosclerosis, a chronic multifactorial disease and a leading cause of death worldwide. Genetically engineered mouse models have proven useful for the study of the mechanisms underlying cardiovascular diseases. The apolipoprotein E-deficient mouse has been the most widely used animal model of atherosclerosis because it rapidly develops severe hypercholesterolemia and spontaneous atherosclerotic lesions similar to those observed in humans. In this review, we provide an overview of the cardiac and vascular phenotypes and discuss the interplay among nitric oxide, reactive oxygen species, aging and diet in the impairment of cardiovascular function in this mouse model.     

Purification, Properties, and Localization of Two Carbonic Anhydrases from Amaranthus cruentus Leaves

The method has been developed for obtaining two purified forms of carbonic anhydrase (CA, A and B forms) from amaranth (Amaranthus cruentus L.) leaves. The method includes precipitation with ammonium sulfate, fractionation by ion-exchange chromatography on DEAE Sephadex A-50, gel filtration on AcA-34 ultragel, and ion-exchange chromatography on DEAE cellulose. The molecular weights of A and B forms were different and equaled to 151 and 251 kD, respectively. The results suggest that SH groups and zinc play important roles in the catalytic activity of both CA forms. Both forms exhibited a high hydratase activity and did not represent allosteric enzymes. However, the catalytic properties of A form, evaluated from the pH dependence of kinetic parameters, differed from those of B form, which was apparently caused by dissimilar structures of these forms. Furthermore, the A form was localized in chloroplast membranes of bundle sheath cells, whereas B form was a soluble enzyme located in the cytoplasm of mesophyll cells.