Glacier-fed streams (GFSs) serve as headwaters to many of the world's largest river
networks. Although being characterized by extreme environmental conditions (ie, low water …

Nearly 60% of the world's glaciers are predicted to be lost by the end of the century because
of global warming1. The impacts of this environmental change on the glacier-fed stream …

Glacier-fed streams are the cold, ultra-oligotrophic, and unstable streams that are fed by
glacial meltwater. Despite these extreme conditions, they harbour a diverse and abundant …

Glacier-fed streams (GFSs) are extreme and rapidly vanishing ecosystems, and yet they
harbor diverse microbial communities. Although our understanding of the GFS microbiome …

High‐mountain streams are particularly vulnerable to climate change because they
intimately interface with the cryosphere. As glaciers shrink and snowpack diminishes …

While glaciers become increasingly recognised as a habitat for diverse and active microbial
communities, effects of their climate change-induced retreat on the microbial ecology of …

Glaciers are receding worldwide because of climate change, and as a consequence, glacier-
fed streams are expected to undergo deep physical and chemical changes in the future …

Owing to climate changes, glaciers and ice sheets are rapidly shrinking worldwide, altering
the geophysical properties of many ecosystems. In this context, glacier-fed streams are …

Microdiversity, the organization of microorganisms into groups with closely related but
ecologically different sub-types, is widespread and represents an important linchpin …

Mountain glaciers are frequently assessed for their hydrological connectivity from glaciers to
proglacial lakes. Ecological process on glacier surfaces and downstream ecosystems have …