<p>Photosynthetic and heterotrophic prokaryotes and eukaryotes inhabit the supraglacial ecosystem, which receives sunlight and has abundant liquid water. Organic matter is slowly transferred to englacial organisms and more rapidly transferred via hydrological processes to subglacial bacteria. The subglacial surface may be till or water, as in the case of subglacial lakes.</p
Water exported from Alpine and polar glaciers is often concentrated in a range of major ions, and mi...
Photoautotrophic microorganisms, i.e. cyanobacteria and microalgae, are ubiquitous in the glacial ec...
The debris-rich basal ice layers of a high Arctic glacier were shown to contain metabolically divers...
Subglacial environments are located at the interface of glacier ice and bedrock. They represent one ...
There is now compelling evidence that microbially mediated reactions impart a significant effect upo...
Subglacial environments harbor active microbial communities. The composition of these communities is...
Glaciers and ice sheets, like other biomes, occupy a significant area of the planet and harbour biol...
Supraglacial environments occupy 11% of Earth’s surface area and represent a critical interface betw...
Microorganisms have a crucial role to play in the cycling of nutrients within glacial environments. ...
Glaciers are melting rapidly. The concurrent export of microbial assemblages alongside glacial meltw...
Liquid water occurs below glaciers and ice sheets globally, enabling the existence of an array of aq...
Glaciological processes under ice sheets provide sustainable ecosystems for microbes, forming an aqu...
The supraglacial environment is an integral part of the glacial ecosystem. It is known to harbour an...
Liquid water has been known to occur beneath the Antarctic ice sheet for more than 40 years, but onl...
Alpine glacial loss is resulting in the rapid change and even emergence of downstream lakes; however...
Water exported from Alpine and polar glaciers is often concentrated in a range of major ions, and mi...
Photoautotrophic microorganisms, i.e. cyanobacteria and microalgae, are ubiquitous in the glacial ec...
The debris-rich basal ice layers of a high Arctic glacier were shown to contain metabolically divers...
Subglacial environments are located at the interface of glacier ice and bedrock. They represent one ...
There is now compelling evidence that microbially mediated reactions impart a significant effect upo...
Subglacial environments harbor active microbial communities. The composition of these communities is...
Glaciers and ice sheets, like other biomes, occupy a significant area of the planet and harbour biol...
Supraglacial environments occupy 11% of Earth’s surface area and represent a critical interface betw...
Microorganisms have a crucial role to play in the cycling of nutrients within glacial environments. ...
Glaciers are melting rapidly. The concurrent export of microbial assemblages alongside glacial meltw...
Liquid water occurs below glaciers and ice sheets globally, enabling the existence of an array of aq...
Glaciological processes under ice sheets provide sustainable ecosystems for microbes, forming an aqu...
The supraglacial environment is an integral part of the glacial ecosystem. It is known to harbour an...
Liquid water has been known to occur beneath the Antarctic ice sheet for more than 40 years, but onl...
Alpine glacial loss is resulting in the rapid change and even emergence of downstream lakes; however...
Water exported from Alpine and polar glaciers is often concentrated in a range of major ions, and mi...
Photoautotrophic microorganisms, i.e. cyanobacteria and microalgae, are ubiquitous in the glacial ec...
The debris-rich basal ice layers of a high Arctic glacier were shown to contain metabolically divers...