4.6 Article

Microbial diversity on Icelandic glaciers and ice caps

期刊

FRONTIERS IN MICROBIOLOGY
卷 6, 期 -, 页码 -

出版社

FRONTIERS MEDIA SA
DOI: 10.3389/fmicb.2015.00307

关键词

snow algae; Iceland; glaciers; microbial diversity; bacteria; archaea; sequencing; albedo

资金

  1. University of Leeds grant
  2. Royal Geographical Society
  3. Society for General Microbiology granted
  4. [NE/J02399X/1]
  5. [NE/K000942/1]
  6. Natural Environment Research Council [NE/J02399X/1, NE/K000942/1, NE/J022365/1] Funding Source: researchfish
  7. NERC [NE/K000942/1, NE/J02399X/1, NE/J022365/1] Funding Source: UKRI

向作者/读者索取更多资源

Algae are important primary colonizers of snow and glacial ice, but hitherto little is known about their ecology on Iceland's glaciers and ice caps. Due do the close proximity of active volcanoes delivering large amounts of ash and dust, they are special ecosystems. This study provides the first investigation of the presence and diversity of microbial communities on all major Icelandic glaciers and ice caps over a 3 year period. Using high-throughput sequencing of the small subunit ribosomal RNA genes (16S and 18S), we assessed the snow community structure and complemented these analyses with a comprehensive suite of physical-, geo-, and biochemical characterizations of the aqueous and solid components contained in snow and ice samples. Our data reveal that a limited number of snow algal taxa (Chloromonas polyptera, Raphidonema sempervirens and two uncultured Chlamydomonadaceae) support a rich community comprising of other micro-eukaryotes, bacteria and archaea. Proteobacteria and Bacteroidetes were the dominant bacterial phyla. Archaea were also detected in sites where snow algae dominated and they mainly belong to the Nitrososphaerales, which are known as important ammonia oxidizers. Multivariate analyses indicated no relationships between nutrient data and microbial community structure. However, the aqueous geochemical simulations suggest that the microbial communities were not nutrient limited because of the equilibrium of snow with the nutrient-rich and fast dissolving volcanic ash. Increasing algal secondary carotenoid contents in the last stages of the melt seasons have previously been associated with a decrease in surface albedo, which in turn could potentially have an impact on the melt rates of Icelandic glaciers.

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