@article {3012,
	title = {Deep groundwater and potential subsurface habitats beneath an Antarctic dry valley},
	journal = {Nature Communications},
	volume = {6},
	year = {2015},
	month = {Apr-04-2017},
	pages = {6831},
	abstract = {The occurrence of groundwater in Antarctica, particularly in the ice-free regions and along the coastal margins is poorly understood. Here we use an airborne transient electromagnetic (AEM) sensor to produce extensive imagery of resistivity beneath Taylor Valley. Regional-scale zones of low subsurface resistivity were detected that are inconsistent with the high resistivity of glacier ice or dry permafrost in this region. We interpret these results as an indication that liquid, with sufficiently high solute content, exists at temperatures well below freezing and considered within the range suitable for microbial life. These inferred brines are widespread within permafrost and extend below glaciers and lakes. One system emanates from below Taylor Glacier into Lake Bonney and a second system connects the ocean with the eastern 18 km of the valley. A connection between these two basins was not detected to the depth limitation of the AEM survey (~350 m).},
	keywords = {LTER-MCM},
	doi = {10.1038/ncomms7831},
	url = {http://www.nature.com/doifinder/10.1038/ncomms7831},
	author = {Jill A. Mikucki and Auken, E. and Tulaczyk, S and Ross A. Virginia and Schamper, C. and S{\o}rensen, K. I. and Peter T. Doran and Hilary A. Dugan and Foley, N.}
}
@inbook {1206,
	title = {Antarctic subglacial water: origin, evolution, and ecology},
	booktitle = {Polar Lakes and Rivers: Limnology of Arctic and Antarctic Aquatic Ecosystems},
	year = {2008},
	publisher = {Oxford University Press},
	organization = {Oxford University Press},
	address = {Oxford},
	keywords = {LTER-MCM},
	author = {John C. Priscu and Tulaczyk, S and Studinger, M and Kenicutt, M and Brent C. Christner and Christine M. Foreman}
}
