Articles | Volume 12, issue 11
https://doi.org/10.5194/tc-12-3653-2018
https://doi.org/10.5194/tc-12-3653-2018
Research article
 | 
26 Nov 2018
Research article |  | 26 Nov 2018

Microbial processes in the weathering crust aquifer of a temperate glacier

Brent C. Christner, Heather F. Lavender, Christina L. Davis, Erin E. Oliver, Sarah U. Neuhaus, Krista F. Myers, Birgit Hagedorn, Slawek M. Tulaczyk, Peter T. Doran, and William C. Stone

Viewed

Total article views: 3,502 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,229 1,142 131 3,502 407 76 92
  • HTML: 2,229
  • PDF: 1,142
  • XML: 131
  • Total: 3,502
  • Supplement: 407
  • BibTeX: 76
  • EndNote: 92
Views and downloads (calculated since 08 Aug 2018)
Cumulative views and downloads (calculated since 08 Aug 2018)

Viewed (geographical distribution)

Total article views: 3,502 (including HTML, PDF, and XML) Thereof 3,190 with geography defined and 312 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 17 Nov 2024
Download
Short summary
Solar radiation that penetrates into the glacier heats the ice to produce nutrient-containing meltwater and provides light that fuels an ecosystem within the ice. Our analysis documents a near-surface photic zone in a glacier that functions as a liquid water oasis in the ice over half the annual cycle. Since microbial growth on glacier surfaces reduces the amount of solar radiation reflected, microbial processes at depths below the surface may also darken ice and accelerate meltwater production.