草皮-腐殖质土壤的腐烂程度对真菌和放线菌数量和多样性的影响

V. V. Demidov, T. A. Gracheva, P. M. Perebasova, A. V. Golovchenko, A. L. Stepanov, O. A. Makarov
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摘要

摘要 在年周期的不同季节评估了土壤侵蚀程度对栽培真菌和放线菌的数量和多样性的影响。研究对象是不同侵蚀程度的草皮膏状土壤(翁布里亚网状土壤(Abruptic)),这些土壤位于东南部的斜坡上(莫斯科州索尔涅奇诺戈尔斯克区),长期以来一直用于种植农作物。微生物数量指标采用平板法测定,根据表型特征进行鉴定。结果表明,土壤侵蚀过程导致的土壤物理和农业化学参数的下降会引起微生物参数的变化。土壤侵蚀程度的增加导致真菌和放线菌的数量和物种多样性减少。未侵蚀土壤和侵蚀土壤微生物群落的分类组成存在显著差异(真菌和放线菌的物种相似性索伦森系数分别不超过 0.42 和 0.30)。菌丝微生物的分类单元已经确定。在真菌中,其代表菌种为曲霉(Aspergillus)、梭菌(Cladosporium)和帚霉(Scopulariopsis);在放线菌中,其代表菌种为链霉菌(Streptomyces malachitospinus)、念珠菌(S. candidus)和枳小孢子菌(Micromonospora aurantiaca)。
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The Influence of Erodibility Degree of Sod-Podzolic Soil on the Abundance and Diversity of Fungi and Actinomycetes

Abstract

The influence of soil erodibility degree on the abundance and diversity of cultivated fungi and actinomycetes have been assessed for different seasons of the annual cycle. The objects of the study are sod-podzolic soils (Umbric Retisols (Abruptic)) with different erodibility degree, located on the slope of the southeastern exposure (Solnechnogorsk raion, Moscow oblast), which have been used for a long time for the cultivation of agricultural crops. The indicators of microbial abundance have been determined by the plate method, identification has been carried out on the basis of phenotypic characters. It is shown that the decline in physical and agrochemical parameters of the soil resulted from the erosion processes, leads to a change in microbiological parameters. An increase in the degree of soil erosion leads to a decrease in the abundance and species diversity of fungi and actinomycetes. Significant differences in the taxonomic composition of microbial communities of noneroded and eroded soils have been found (the Sørensen coefficient of species similarity does not exceed 0.42 and 0.30 for fungi and actinomycetes, respectively). Taxonomic units of mycelial microorganisms have been identified. Among fungi, they are represented by the species Aspergillus, Cladosporium, and Scopulariopsis, and among actinomycetes, by Streptomyces malachitospinus, S. candidus, and Micromonospora aurantiaca.

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