The Greenland Ice Sheet harbours a wealth of microbial life, yet the total biomass stored or exported from its surface to downstream environments is unconstrained. Here, we quantify microbial abundance and cellular biomass flux within the near-surface weathering crust photic zone of the western sector of the ice sheet. Using groundwater techniques, we demonstrate that interstitial water flow is slow (~10−2 m d−1), while flow cytometry enumeration reveals this pathway delivers 5 × 108 cells m−2 d−1 to supraglacial streams, equivalent to a carbon flux up to 250 g km−2 d−1. We infer that cellular carbon accumulation in the weathering crust exceeds fluvial export, promoting biomass sequestration, enhanced carbon cycling, and biological albedo r...
The melting of the Greenland Ice Sheet provides direct connections between atmospheric, supraglacial...
Uncertainty surrounds estimates of microbial cell and organic detritus fluxes from glacier surfaces....
Runoff from small glacier systems contains dissolved organic carbon (DOC) rich in protein-like, low ...
The Greenland Ice Sheet harbours a wealth of microbial life, yet the total biomass stored or exporte...
Melting glacier ice surfaces host active microbial communities that enhance glacial melt, contribute...
Microbially mediated carbon fluxes on the surface of the Greenland ice sheet (GrIS) were recently qu...
This paper presents an assessment of biological activity associated with ice surface debris (cryocon...
The Greenland Ice Sheet (GrIS) exports approximately 400 km3 of freshwater annually to downstream fr...
Microorganisms are flushed from the Greenland Ice Sheet (GrIS) where they may contribute towards the...
Greenland's Dark Zone is the largest contiguous region of bare terrestrial ice in the Northern Hemis...
Meltwater runoff from the Greenland Ice Sheet (GrIS) has increased by more than 50% in the last 50 y...
Measurements from Austre Brøggerbreen (Svalbard, 2009) and the Greenland Ice Sheet (GrIS, near Kange...
Current research into bacterial dynamics on the Greenland Ice Sheet (GrIS) is biased toward cryoconi...
Current research into bacterial dynamics on the Greenland Ice Sheet (GrIS) is biased toward cryoconi...
Measurements from Austre Brøggerbreen (Svalbard, 2009) and the Greenland Ice Sheet (GrIS, near Kange...
The melting of the Greenland Ice Sheet provides direct connections between atmospheric, supraglacial...
Uncertainty surrounds estimates of microbial cell and organic detritus fluxes from glacier surfaces....
Runoff from small glacier systems contains dissolved organic carbon (DOC) rich in protein-like, low ...
The Greenland Ice Sheet harbours a wealth of microbial life, yet the total biomass stored or exporte...
Melting glacier ice surfaces host active microbial communities that enhance glacial melt, contribute...
Microbially mediated carbon fluxes on the surface of the Greenland ice sheet (GrIS) were recently qu...
This paper presents an assessment of biological activity associated with ice surface debris (cryocon...
The Greenland Ice Sheet (GrIS) exports approximately 400 km3 of freshwater annually to downstream fr...
Microorganisms are flushed from the Greenland Ice Sheet (GrIS) where they may contribute towards the...
Greenland's Dark Zone is the largest contiguous region of bare terrestrial ice in the Northern Hemis...
Meltwater runoff from the Greenland Ice Sheet (GrIS) has increased by more than 50% in the last 50 y...
Measurements from Austre Brøggerbreen (Svalbard, 2009) and the Greenland Ice Sheet (GrIS, near Kange...
Current research into bacterial dynamics on the Greenland Ice Sheet (GrIS) is biased toward cryoconi...
Current research into bacterial dynamics on the Greenland Ice Sheet (GrIS) is biased toward cryoconi...
Measurements from Austre Brøggerbreen (Svalbard, 2009) and the Greenland Ice Sheet (GrIS, near Kange...
The melting of the Greenland Ice Sheet provides direct connections between atmospheric, supraglacial...
Uncertainty surrounds estimates of microbial cell and organic detritus fluxes from glacier surfaces....
Runoff from small glacier systems contains dissolved organic carbon (DOC) rich in protein-like, low ...