厚壁菌
拟杆菌
蛋白质细菌
生物
放线菌门
生态学
雪
酸杆菌
浮霉菌门
蓝藻
植物
北极的
塔玛丘塔
16S核糖体RNA
细菌
地质学
地貌学
遗传学
作者
Annette K. Møller,Ditte Andreasen Søborg,Waleed Abu Al‐Soud,Søren J. Sørensen,Niels Kroer
出处
期刊:Polar Research
[Norwegian Polar Institute]
日期:2013-01-01
卷期号:32 (1): 17390-17390
被引量:79
标识
DOI:10.3402/polar.v32i0.17390
摘要
The bacterial community structures in High-Arctic snow over sea ice and an ice-covered freshwater lake were examined by pyrosequencing of 16S rRNA genes and 16S rRNA gene sequencing of cultivated isolates. Both the pyrosequence and cultivation data indicated that the phylogenetic composition of the microbial assemblages was different within the snow layers and between snow and freshwater. The highest diversity was seen in snow. In the middle and top snow layers, Proteobacteria, Bacteroidetes and Cyanobacteria dominated, although Actinobacteria and Firmicutes were relatively abundant also. High numbers of chloroplasts were also observed. In the deepest snow layer, large percentages of Firmicutes and Fusobacteria were seen. In freshwater, Bacteroidetes, Actinobacteria and Verrucomicrobia were the most abundant phyla while relatively few Proteobacteria and Cyanobacteria were present. Possibly, light intensity controlled the distribution of the Cyanobacteria and algae in the snow while carbon and nitrogen fixed by these autotrophs in turn fed the heterotrophic bacteria. In the lake, a probable lower light input relative to snow resulted in low numbers of Cyanobacteria and chloroplasts and, hence, limited input of organic carbon and nitrogen to the heterotrophic bacteria. Thus, differences in the physicochemical conditions may play an important role in the processes leading to distinctive bacterial community structures in High-Arctic snow and freshwater.Keywords: Taxonomic diversity; microbial assemblages; bacterial density; DOC(Published: 25 April 2013)To access the supplementary material for this article, please see supplementary files in the column to the right (under Article Tools).Citation: Polar Research 2013, 32, 17390, http://dx.doi.org/10.3402/polar.v32i0.17390
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