Actinomycetal complexes in drained peat soils of the taiga zone upon pyrogenic succession View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2008-04

AUTHORS

G. M. Zenova, N. A. Glushkova, M. V. Bannikov, A. P. Shvarov, A. I. Pozdnyakov, D. G. Zvyagintsev

ABSTRACT

The number and diversity of actinomycetes in peat soils vary in dependence on the stage of pyrogenic succession. In the cultivated peat soil, the number of actinomycetes after fires decreases by three-four times, mainly at the expense of acidophilic and neutrophilic groups. An increase in the number of mycelial prokaryotes (at the expense of alkaliphilic forms) is seen on the fifth year of functioning of the pyrogenic peat soil. The species diversity of streptomycetes in peat soils also decreases after fires. An increase in the range of streptomycetal species at the expense of neutrophilic and alkaliphilic forms takes place on the fifth year of the pyrogenic succession. Parameters of the actinomycetal complex—the population density, species composition, and ecological features—are the criteria whose changes allow us to judge the state of peat soils in the course of their pyrogenic succession. More... »

PAGES

394-399

References to SciGraph publications

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s1064229308040054

DOI

http://dx.doi.org/10.1134/s1064229308040054

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1006090928


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