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The research team tested samples from the ice 3,590 meters below Vostok Station, and found diverse colonies of microbes. Scientists say this is significant because the lake has been isolated from the usual sources of atmospheric-derived energy, such as photosynthesis, for millions of years. "How the bacteria get energy (to survive) is an important question," McKay said. "The lake could be an analog to sub-ice Europa or subsurface Mars where conditions are similar."
Scientists believe ice is a good environment for primitive bacteria. The bacteria need less food because it's cold, and its metabolism slows down, somewhat like a hibernating bear's. Another finding was that DNA extracted from the microbes present in the team's Lake Vostok sample indicated the presence of only a few subgroups of known bacteria, coupled with low overall microbial diversity. "It's what you'd expect, not teeming with rich life," McKay said. The team also found signs of bacterial life in the ice core and detected metabolic activity in some of the bacteria by measuring the bacteria's respiration rates during incubation.
Although the thickness of the ice on Europa is not known, scientists think that tidal forces could form cracks extending to the surface. Under the thin ice, conditions may be similar to the conditions at Lake Vostok. "If a similar ice layer is present under the surface of Europa's icy oceans, it may also harbor life," said McKay. Left: Fragmented chunks of ice on Europa, similar in appearance to those seen in Earth polar seas during a springtime thaw. It's possible that Europa and Lake Vostok share a number of remarkable properties, including a kilometers-thick covering of ice over liquid water and an environment where life may have developed along unique evolutionary paths, [more information] The research team included the paper's lead author, Dr. John Priscu, and others from the departments of Biology, Earth Science and Physics at Montana State University, Bozeman, MT. Other researchers were from the department of Geology, the University of Alabama, Tuscaloosa, AL, and the U. S. Geological Survey, Reston, VA. |
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