In:
Hydrological Processes, Wiley, Vol. 18, No. 2 ( 2004-02-15), p. 379-387
Abstract:
Cryoconite holes are near‐vertical tubes that form in the surface of glaciers when solar‐heated debris melts into the ice. Those that form in the McMurdo Dry Valleys of Antarctica are distinctive, in that they have ice lids and are closed to the atmosphere for periods of years to decades. Photoautotrophs and heterotrophs grow within this closed environment, perturbing the poorly buffered water chemistry, yet maintaining the potential for photosynthesis. Microbial excretion and decomposition of organic matter produces dissolved organic carbon (DOC): dissolved inorganic carbon ratios of ∼1:2. Much of the dissolved nitrogen pool (80–100%) exists as dissolved organic nitrogen (DON). The DON:DOC ratio is ∼1:11 (mol/mol), typical of organic particulate material at the Earth's surface. The combination of photoautotrophy, heterotrophy and weak chemical buffering within these microcosms promotes values of pH, p CO 2 , O 2 saturation and percentage total dissolved nitrogen as DON that reach 10·99, 10 −7·6 atm, 160% and 100% respectively, which are a unique combination among the surface waters on Earth. These ice‐sealed cryoconite holes could be important analogues of refugia on Snowball Earth and other icy planets. Copyright © 2004 John Wiley & Sons, Ltd.
Type of Medium:
Online Resource
ISSN:
0885-6087
,
1099-1085
Language:
English
Publisher:
Wiley
Publication Date:
2004
detail.hit.zdb_id:
1479953-4
SSG:
14
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