1. Ice shelf microbial ecosystems in the high arctic and implications for life on snowball earth.
- Author
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Vincent WF, Gibson JA, Pienitz R, Villeneuve V, Broady PA, Hamilton PB, and Howard-Williams C
- Subjects
- Animals, Arctic Regions, Canada, Ciliophora isolation & purification, Cyanobacteria isolation & purification, Eukaryota isolation & purification, Nematoda isolation & purification, Rotifera isolation & purification, Viruses isolation & purification, Ecosystem, Ice, Water parasitology, Water Microbiology
- Abstract
The Ward Hunt Ice Shelf (83 degrees N, 74 degrees W) is the largest remaining section of thick (> 10 m) land-fast sea ice along the northern coastline of Ellesmere Island, Canada. Extensive meltwater lakes and streams occur on the surface of the ice and are colonized by photosynthetic microbial mat communities. This High Arctic cryo-ecosystem is similar in several of its physical, biological and geochemical features to the McMurdo Ice Shelf in Antarctica. The ice-mats in both polar regions are dominated by filamentous cyanobacteria but also contain diatoms, chlorophytes, flagellates, ciliates, nematodes, tardigrades and rotifers. The luxuriant Ward Hunt consortia also contain high concentrations (10(7)-10(8) cm-2) of viruses and heterotrophic bacteria. During periods of extensive ice cover, such as glaciations during the Proterozoic, cryotolerant mats of the type now found in these polar ice shelf ecosystems would have provided refugia for the survival, growth and evolution of a variety of organisms, including multicellular eukaryotes.
- Published
- 2000
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