Abstract

Abstract. During the spring of 2009, as part of the Ocean–Atmosphere–Sea Ice–Snowpack (OASIS) campaign in Barrow, Alaska, USA, we examined the identity, population diversity, freezing nucleation ability of the microbial communities of five different snow types and frost flowers. In addition to the culturing and gene-sequence-based identification approach, we utilized a state-of-the-art genomic next-generation sequencing (NGS) technique to examine the diversity of bacterial communities in Arctic samples. Known phyla or candidate divisions were detected (11–18) with the majority of sequences (12.3–83.1%) belonging to one of the five major phyla: Proteobacteria, Actinobacteria, Bacteroidetes, Firmicutes, and Cyanobacteria. The number of genera detected ranged from, 101–245. The highest number of cultivable bacteria was observed in frost flowers (FFs) and accumulated snow (AS) with 325 ± 35 and 314 ± 142 CFU m L−1, respectively; and for cultivable fungi 5 ± 1 CFU m L−1 in windpack (WP) and blowing snow (BS). Morphology/elemental composition and ice-nucleating abilities of the identified taxa were obtained using high resolution electron microscopy with energy-dispersive X-ray spectroscopy and ice nucleation cold-plate, respectively. Freezing point temperatures for bacterial isolates ranged from −20.3 ± 1.5 to −15.7 ± 5.6 °C, and for melted snow samples from −9.5 ± 1.0 to −18.4 ± 0.1 °C. An isolate belonging to the genus Bacillus (96% similarity) had ice nucleation activity of −6.8 ± 0.2 °C. Comparison with Montreal urban snow, revealed that a seemingly diverse community of bacteria exists in the Arctic with some taxa possibly originating from distinct ecological environments. We discuss the potential impact of snow microorganisms in the freezing and melting process of the snowpack in the Arctic.

Highlights

  • The snowpack has been shown to act as an important matrix for chemical and biological reactions of organic compounds (Ariya et al, 2011)

  • Recent observations have indicated that snowpack is a complex microhabitat that permits the growth of diverse microorganisms allowing for photo-chemical and biological reactions to occur (Amoroso et al, 2010)

  • A largely diverse community of bacteria exists in the Arctic with many originating from remote ecological environments such as dust storms

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Summary

Introduction

The snowpack has been shown to act as an important matrix for (photo) chemical and biological reactions of organic compounds (Ariya et al, 2011). Trace gas exchange, scavenging, photolysis, adsorption (Kos et al, 2014), and more recently, biological transformations in snowpack have been considered (Amoroso et al, 2010, 2009; Fujii et al, 2010; Segawa et al, 2005). Climate change has been linked to changes in snow and ice patterns in the Arctic, potentially impacting the Earth’s albedo and atmospheric energy balance (Grenfell and Maykut, 1977; Grenfell and Perovich, 1984, 2004; Hanesiak, 2001). Atmospheric transport events such as dust storms initiated long distances away have been considered to influence the Arctic climate. In 1976, an Asian dust storm was responsible for bringing as much as 4000 t

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