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Antarctic Hydrologic Margin Microbiology and Biogeochemistry Project Title:Collaborative Research: Hydrologic controls over biogeochemistry and microbial community structure and function across terrestrial/aquatic interfaces in a polar desert Project Duration: 1-Jul-2004 - 30-Jun-2007 Principal Investigators: John E. Barrett (Virginia Tech) Michael Gooseff (Penn State University) Cristina Takacs-Vesbach (University of New Mexico) |
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| Overview: It is generally held that "where there is water, there is life". We are investigating the control of hydrology on microbial structure and biogeochemical cycling in terrestrial-aquatic interfaces in the McMurdo Dry Valleys, Antarctica. These transition zones are easily delineated as wetted sediment bounding lakes and streams in the Dry Valleys. Because there is little precipitation and permafrost is shallow (< 1 m), the water in these interfaces comes from the adjoining water body. We expect that a gradient of soil moisture exists across these transition zones, from wet near the water body to dry, within several meters. |
![]() Example of a lentic hydrologic margin, Lake Joyce, Pearse Valley, Antarctica. |
![]() Expected pattern of subsurface moisture and microbial diversity in dry valley hydrologic margins. |
We propose that hydrologic margins are unique locations of biogeochemical cycling and soil microbial habitat in the dry valleys landscape. We will test the hypothesis that the presence of and proximity to liquid water influences the structure and functioning of sub-surface microbial populations and consequently biogeochemical conditions in hydrologic margins of the dry valleys with coordinated hydrologic, biogeochemical, and molecular microbial studies. Further, we expect that lentic (i.e. lake) hydrologic margins have biogeochemical functions that will influence only local sub-surface environments, but that lotic (i.e. stream) hydrologic margin biogeochemical functions influence a much broader portion of the dry valleys landscape, including stream water, downstream hydrologic margins, and ultimately lakes. |
Location: Our field sites will be within Taylor Valley, Antarctica. Numerous plot-scale investigation sites will be selected adjacent various streams and lakes within Taylor Valley.
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This project is
funded through the National Science Foundation's Office of Polar Programs.
This material is based upon work supported by the National Science Foundation under Grant No. 0338267. 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 |