{"title":"[Microbial communities of frozen soils of the Tuimaada Valley in Central Sakha].","authors":"T I Ivanova, N P Kuz'mina, D D Savvinov","doi":"","DOIUrl":null,"url":null,"abstract":"<p><p>This study determined the characteristic features of microbial communities inhabiting frozen soils of Central Sakha. All groups of microorganisms were present in high numbers comparable with the microbial densities in steppe soils of Transbaikalia; their distribution along soil profiles followed a specific pattern with no decrease in abundance with depth. In summer, the dominant groups of the microbial pool were actinomycetes and oligonitrophilic bacteria, while in autumn it was heterotrophic bacteria. A typical feature of the frozen soils of Central Sakha was the gradual penetration of microorganisms into deeper soil horizons during the vegetation season and their accumulation in the suprapermafrost horizon by autumn.</p>","PeriodicalId":77187,"journal":{"name":"Izvestiia Akademii nauk. Seriia biologicheskaia","volume":" ","pages":"573-85"},"PeriodicalIF":0.0000,"publicationDate":"2014-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Izvestiia Akademii nauk. Seriia biologicheskaia","FirstCategoryId":"1085","ListUrlMain":"","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
This study determined the characteristic features of microbial communities inhabiting frozen soils of Central Sakha. All groups of microorganisms were present in high numbers comparable with the microbial densities in steppe soils of Transbaikalia; their distribution along soil profiles followed a specific pattern with no decrease in abundance with depth. In summer, the dominant groups of the microbial pool were actinomycetes and oligonitrophilic bacteria, while in autumn it was heterotrophic bacteria. A typical feature of the frozen soils of Central Sakha was the gradual penetration of microorganisms into deeper soil horizons during the vegetation season and their accumulation in the suprapermafrost horizon by autumn.