| Geochemistry and Microbiology of the Extreme Aquatic Environment in Lake Vida, East Antarctica |
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Lake Vida III: Developing a comprehensive understanding of Lake Vida – from the past to the present – life, biogeochemical function, geochemical composition and paleohistory of its microbial inhabitants. Lake Vida, in the McMurdo Dry Valleys of East Antarctica, is one of the largest lakes in the region. It was originally thought to be an ice block lake - frozen solid. However, in 1995, ground penetrating radar surveys revealed a very salty liquid layer (a brine) underlying a 20 m (66 foot) ice cover. This started a series of investigations on the history and physics behind the formation of this unusual lake, as well as on the potential for life in the brine, and how it survives. Lake Vida is not a lake like those of Wisconsin or Michigan. Unlike those lakes, Vida has an ice cover year round. In fact, the ice cover is so thick that water trapped under the ice is completely isolated from other environments. In the summer, new water coming in from glacial streams cannot get under the ice and so it flows on top and freezes. This leads to a unique situation where a thick ice cover on Lake Vida requires occurrence of warm summers (and therefore more stream flow). We’ve created these pages for you to learn about our research and follow our adventures as they unfold. Enjoy. |
This material is based upon work supported by the National Science Foundation. Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation.