Variation in bacterial composition, diversity, and activity across different subglacial basal ice types

Abstract

ABSTRACTGlaciers and ice sheets possess layers of basal ice characterized by high amounts of entrained debris that can serve as sources of nutrients and organic matter, providing habitat for microorganisms adapted to the frozen conditions. Basal ice forms through various mechanisms and is classified based on its ice and debris content; however, little is known about variation in microbial composition, diversity, and activity across different basal ice types. We investigated these parameters in four different types of basal ice from a cold-based and temperate glacier and used a meta-analysis to compare our findings with microbiome studies from other frozen environments. We found basal ice environments harbor a diverse range of microbiomes whose composition and activity can vary significantly between basal ice types, even within adjacent facies from the same glacier. In some debris-rich basal ices, elevated ATP concentrations, isotopic gas signatures, and high ratios of amplified sequences for 16S rRNA relative to that for 16S rRNA genes implicated certain bacterial taxa (e.g., Paenisporosarcina, Desulfocapsa, Syntrophus, Desulfosporosinus) as being potentially active, with ice temperature appearing to be an important predictor for the diversity of taxa inferred to be active. Compared to those of other sympagic environments, these microbiomes often resembled those found in permafrost or perennial cave ice rather than other glacial ice environments. In contrast, debris-poor basal ices harbored microbiomes more like those found in oligotrophic englacial ice. Collectively, these results suggest that different basal ice types contain distinct microbiomes that are actively structured by the diagenesis of their habitat.IMPORTANCEThe discharge of material from the basal ice zones of glaciers and ice sheets is an important source of dissolved organic matter, nutrients, and trace metals to downstream environments. Microorganisms with the ability to remain metabolically active while frozen have the potential to alter these substrates before they are released and may thus be a vital biogeochemical component of proglacial environments. However, basal ice environments are among the least explored areas of the cryosphere and information on their microbiology is limited. Here, we examine several basal ice types that were collected from different glaciers to investigate how their microbiomes varied. Our results indicate that sediment-rich basal ice from cold-based and temperate glaciers harbor microbiomes that conduct biogeochemical transformations at subzero temperatures and raises the intriguing possibility that subsurface regions of the cryosphere may be more biogeochemically active than previously thought.