Cyanobacteria inhabiting biological soil crusts of a polar desert: Sør Rondane Mountains, Antarctica
Language English Country Germany Media print-electronic
Document type Journal Article
PubMed
29452715
DOI
10.1016/j.syapm.2018.01.006
PII: S0723-2020(18)30027-4
Knihovny.cz E-resources
- Keywords
- 454 pyrosequencing, Antarctica, BSC, Biovolume, Cyanobacteria, DGGE,
- MeSH
- Biodiversity MeSH
- DNA, Bacterial genetics MeSH
- Ecosystem MeSH
- Ice Cover microbiology MeSH
- Molecular Typing MeSH
- Soil Microbiology * MeSH
- RNA, Ribosomal, 16S genetics MeSH
- Sequence Analysis, DNA MeSH
- Cyanobacteria * classification genetics isolation & purification MeSH
- Publication type
- Journal Article MeSH
- Geographicals
- Antarctic Regions MeSH
- Names of Substances
- DNA, Bacterial MeSH
- RNA, Ribosomal, 16S MeSH
Molecular and morphological methods were applied to study cyanobacterial community composition in biological soil crusts (BSCs) from four areas (two nunataks and two ridges) in the Sør Rondane Mountains, Antarctica. The sampling sites serve as control areas for open top chambers (OTCs) that were put in place in 2010 at the time of sample collection and will be compared with BSC samples taken from the OTCs in the future. Cyanobacterial cell biovolume was estimated using epifluorescence microscopy, which revealed the dominance of filamentous cyanobacteria in all studied sites except the Utsteinen ridge, where unicellular cyanobacteria were the most abundant. Cyanobacterial diversity was studied by a combination of molecular fingerprinting methods based on the 16S rRNA gene (denaturing gradient gel electrophoresis (DGGE) and 454 pyrosequencing) using cyanobacteria-specific primers. The number of DGGE sequences obtained per site was variable and, therefore, a high-throughput method was subsequently employed to improve the diversity coverage. Consistent with previous surveys in Antarctica, both methods showed that filamentous cyanobacteria, such as Leptolyngbya sp., Phormidium sp. and Microcoleus sp., were dominant in the studied sites. In addition, the studied localities differed in substrate type, climatic conditions and soil parameters, which probably resulted in differences in cyanobacterial community composition. Furthermore, the BSC growing on gneiss pebbles had lower cyanobacterial abundances than BSCs associated with granitic substrates.
References provided by Crossref.org
Marked Succession of Cyanobacterial Communities Following Glacier Retreat in the High Arctic