Microbial diversity on Icelandic glaciers and ice caps

• Published in: Frontiers in Microbiology
• Main Authors: Stefanie eLutz, Alexandre M Anesio, Arwyn eEdwards, Liane G Benning
• Format: Article in Journal/Newspaper
• Language: English
• Published: Frontiers Media S.A. 2015
• Subjects: Archaea; Bacteria; Iceland; Sequencing; Microbial Diversity; glaciers; Microbiology; QR1-502
• Online Access: https://doi.org/10.3389/fmicb.2015.00307; https://doaj.org/article/915123243c3f49f89436ec471e8d57e1

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 three 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.