The permanent ice covers of Antarctic lakes in the McMurdo Dry Valleys
develop liquid water inclusions in response to solar heating of inter
nal aeolian-derived sediments. The ice sediment particles serve as nut
rient (inorganic and organic)-enriched microzones for the establishmen
t of a physiologically and ecologically complex microbial consortium c
apable of contemporaneous photosynthesis,.nitrogen fixation, and decom
position. The consortium is capable of physically and chemically estab
lishing and modifying a relatively nutrient- and organic matter-enrich
ed microbial ''oasis'' embedded in the lake ice cover.