Biogeochemical Evolution of Cryoconite Holes on Canada Glacier, Taylor Valley, Antarctica
The cryoconite holes of the McMurdo Dry Valleys are simple, closed biogeochemical systems involving water, ice, mineral and organic debris, which serve as ecosystems for consortia of microorganisms. This study is the first to document the seasonal and annual chemical evolution of solutes in cryoconi...
Main Authors: | , , , , , |
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Format: | Text |
Language: | unknown |
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PDXScholar
2007
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Online Access: | https://pdxscholar.library.pdx.edu/geog_fac/15 https://pdxscholar.library.pdx.edu/cgi/viewcontent.cgi?article=1014&context=geog_fac |