Factors and mechanisms of soil salinization under vineyards of southern Taman

The spatial distribution of saline soils under vineyards in the south of Taman Peninsular is discussed. The Paleogene–Neogene clays of the Komendantskaya Mount serve as the source of salts. Vineyards were planted on an inclined plain at the foot of this mount. At present, their state on salt-affected soils worsens. In the upper part of the plain, solonchakous or deep-solonchakous slightly saline and nonsaline (within the upper 2 m) dark quasigley vertic soils (Vertisols) are formed. The salts are of the sulfate–sodium composition. Their vertical distribution has an eluvial pattern with a quick rise in the salt content from the surface layer to the depth of 50–100 cm and with a gradual increase in the salt content in the deeper layers. The absence of chlorides in the soils of flat areas within the slope attests to the predominance of lateral leaching of salts down the slope over their vertical leaching in the soil profiles. In the lower part of the slope, soil salinization mainly takes place in the hollow crossing the plain and the vineyard from the north to the south. In the middle part of the slope, nonsaline (to a depth of 2 m) agrohumus quasigley soils (Haplic Chernozems (Clayic, Aric, Stagnic)) are formed. Slight chloride–sulfate sodium salinization is only seen in the soils of the hollow, which contain fine-crystalline gypsum in the solid phase and display the accumulation of sodium chlorides in the middle part of the soil profile (in the 60–150-cm-thick layer). Heavy loamy agrochernozems with migrational and segregational forms of carbonates (Haplic Chernozems (Loamic, Aric, Pachic) are developed in the lower part of the slope; they are nonsaline to the depth of 2.5 m. In the area of transition from the humusquasigley soils to chernozems, specific horizons are formed in the hollow at the depth of more than 250 cm. Their soil solutions contain sodium, calcium, and magnesium chlorides against the background of the presence of fine-crystalline gypsum in the solid phase, which is typical of secondary salinization.     

Identification and Characterization of a Novel Lectin from the Clam Glycymeris yessoensis and Its Functional Characterization under Microbial Stimulation and Environmental Stress

Lectin from the bivalve Glycymeris yessoensis (GYL) was purified by affinity chromatography on porcine stomach mucin–Sepharose. GYL is a dimeric protein with a molecular mass of 36 kDa, as established by SDS-PAGE and MALDI-TOF analysis, consisting of 18 kDa subunits linked by a disulfide bridge. According to circular dichroism data, GYL is a β/α-protein with the predominance of β-structure. GYL preferentially agglutinates enzyme-treated rabbit erythrocytes and recognizes glycoproteins containing O-glycosidically linked glycans, such as porcine stomach mucin (PSM), fetuin, thyroglobulin, and ovalbumin. The amino acid sequences of five segments of GYL were acquired via mass spectrometry. The sequences have no homology with other known lectins. GYL is Ca²⁺-dependent and stable over a range above a pH of 8 and temperatures up to 20 °C for 30 min. GYL is a pattern recognition receptor, as it binds common pathogen-associated molecular patterns, such as peptidoglycan, LPS, β-1,3-glucan and mannan. GYL possesses a broad microbial-binding spectrum, including Gram-positive (Bacillus subtilis, Staphylococcus aureus) and Gram-negative bacteria (Escherichia coli, Vibrio proteolyticus), but not the fungus Candida albicans. Expression levels of GYL in the hemolymph were significantly upregulated after bacterial challenge by V. proteolyticus plus environmental stress (diesel fuel). Results indicate that GYL is probably a new member of the C-type lectin family, and may be involved in the immune response of G. yessoensis to bacterial attack.     

Erratum to: A Study of Soil Organic Matter Stability Using Derivatography and Long-Term Incubation Methods

Eurasian Soil Science - An Erratum to this paper has been published: https://doi.org/10.1134/S1064229321770015     

Effect of Chemical Amelioration on the Physicochemical Properties of Chernozem Soils in Irrigated Fruit Nurseries

This paper presents the results of a study on the effects of long-term use of drip irrigation with mineralized or, in other words, saline waters on the physicochemical properties of black chernozem soils in a fruit nursery. Irrigation induced local accumulation of water-soluble salts in the main wetted zone, alkalinization of the soil, and saturation of the soil-absorbing complex with Na⁺ and Mg²⁺ cations and Ca²⁺ depletion. The introduction of phosphogypsum in a dose of 2 t/ha for chemical reclamation reduced high alkalinity of the soil and increased the content of exchangeable calcium in the soil-absorbing complex. The application of phosphogypsum seems to be an effective method to restore the fertility of chernozem soils under conditions of long-term use of drip irrigation with mineralized waters.     

Structure of the Cell-Wall-Associated Polysaccharides from the Deep-Sea Marine Bacterium Devosia submarina KMM 9415T

Two cell-wall-associated polysaccharides were isolated and purified from the deep-sea marine bacterium Devosia submarina KMM 9415^T, purified by ultracentrifugation and enzymatic treatment, separated by chromatographic techniques, and studied by sugar analyses and NMR spectroscopy. The first polysaccharide with a molecular weight of about 20.7 kDa was found to contain d-arabinose, and the following structure of its disaccharide repeating unit was established: →2)-α-d-Araf-(1→5)-α-d-Araf-(1→. The second polysaccharide was shown to consist of d-galactose and a rare component of bacterial glycans-d-xylulose: →3)-α-d-Galp-(1→3)-β-d-Xluf-(1→.     

Effect of Long-Term Drip Irrigation of Fruit Orchard on the Transformation of Properties of Chernozems

Eurasian Soil Science - The impact of long-term drip irrigation of apple plantations with low-saline water on the transformation of typical chernozems (Haplic Chernozems) on the Kuban Lowland...