[Comparative assessment of soil microbial biomass determined by the methods of direct microscopy and substrate-induced respiration].

The content of microbial biomass (MB) was determined in samples of gray forest, chestnut, and tundra soils with different physicochemical properties (0.4-22.7% Corg; 8.4-26.8% silt particles; pH 4.3-8.4) by the methods of substrate-induced respiration (MB(SIR)) and direct microscopy (MB(M)). The samples of two upper soil layers, 0-5 and 5-10 cm (without plant litter), from different ecosystems (forest, forest shelter belt, meadow, fallow, and arable land) and elements of relief of interfluvial tundra (block/upper land plateau, depression between blocks) have been analyzed. The content of microbial biomass in the 0-5-cm soil layer was 216-8134 and 348-7513 microg C/g soil as measured by the methods of substrate-induced respiration and direct microscopy, respectively. The MB(SIR) and MB(M) values closely correlated with each other: r = 0.90 and 0.74 for 0-5 and 5-10 cm, respectively. The average MB(SIR)/MB(M) ratio was 90 and 60% for 0-5 and 5-10 cm, respectively. The portion of microbial carbon in total organic soil carbon was, on average, 4 and 3% (SIR) and 5 and 7% (direct microscopy) for 0-5 and 5-10 cm, respectively. Possible reasons for the differences between MB(SIR) and MB(M) values in the soils under study are discussed.

[The ratio of fungi and bacteria in the biomass of different types of soil determined by selective inhibition].

Tundra, chernozem (virgin and arable), sod-podzolic (coniferous forest, meadow, and arable), and grey forest (larch forest) soils were used to separate the contributions of fungi and bacteria to substrate-induced respiration (SIR) with the help of antibiotics. For soils with a high content of organic matter (tundra and chernozem: 12 and 8%, respectively), the procedure of selective inhibition of SIR has been optimized. The optimized procedure includes the application of high concentrations of streptomycin (50-120 mg/g of soil) and cycloheximide (50-80 mg/g of soil) and decreasing the weight of the analyzed soil sample. Soils under study have shown the predominant contribution of fungi (63-82%) to the total SIR. The fungal-bacterial ratio in the soils of natural ecosystems (0-5 cm, without litter) was 4.32, 2.19, 1.5, and 1.5 for tundra soil, virgin chernozem, coniferous (sod-podzolic soil), and larch (grey forest soil) forests, respectively. The lower layers of sod-podzolic (5-10 cm) and grey forest (48-58 cm) soils showed a decrease in the fungal and increase in the bacterial component in the total SIR.

[The antibiotic-aided separation of fungal and bacterial substrate-induced respiration in various soil ecosystems].

Fungal and bacterial substrate-induced respiratory activities have been distinguished in gray forest and chestnut soils in various ecosystems (forest, grassland, tillage, unused land, and shelterbelt) using the antibiotics cycloheximide and streptomycin. The optimal inhibitory concentrations of the antibiotics, added separately and in combination; the preincubation time of the antibiotics with the soil before glucose addition; and the mass of added inert material (talc) have been determined. Based on the results obtained, the inhibitor additivity ratio (IAR) has been calculated for the antibiotics. With the IAR differing from 1.0 by a value of more than 5%, the fungal and bacterial substrate-induced respiratory activities can not be distinguished reliably. Respiration measurements show that the microbial communities of natural ecosystems are dominated by fungi (81-95% on average). The smallest amount of fungi (54-59%) is found in the tillage ecosystem.