McMurdo LTER Publications
Hydrological Controls on Ecosystem Dynamics in Lake Fryxell, Antarctica. . PLOS ONE. 2016;11(7):e0159038. doi:10.1371/journal.pone.015903810.1371.
Hydrological Connectivity of the Landscape of the McMurdo Dry Valleys, Antarctica. Geography Compass. 2011;5(9):666 - 681. doi:10.1111/j.1749-8198.2011.00445.x.
. The hydroecology of an ephemeral wetland in the McMurdo Dry Valleys, Antarctica. Journal of Geophysical Research: Biogeosciences. 2019. doi:10.1029/2019JG005153.
History of McMurdo Dry Valley Lakes, Antarctica, from stable chlorine isotope data. Geology. 1999;27(527-530). doi:LTER.
. Halogen geochemistry of the McMurdo Dry Valleys Lakes, Antarctica: clues to the origin of solutes and lake evolution. Geochimica et Cosmochimica Acta. 2005;69:305-323.
Groundwater seeps in Taylor Valley Antarctica: An example of a subsurface melt event. Annals of Glaciology. 2005;40:200-206. doi:LTER.
Geomicrobiology of sub-glacial ice above Vostok Station. Science. 1999;286(5447):2141-2144. doi:10.1126/science.286.5447.2141.
Geomicrobiology of Blood Fall: An iron-rich saline discharge at the terminus of the Taylor Glacier, Antarctica. Aquatic Geochemistry. 2004;10:199-200.
. The geochemistry of upland ponds, Taylor Valley, Antarctica. Antarctic Science. 2012;24(01):3 - 14. doi:10.1017/S0954102011000617.
The Geochemistry of Supraglacial Streams of Canada Glacier, Taylor Valley (Antarctica), and their Evolution into Proglacial Waters. Aquatic Geochemistry. 2005;11:391-412.
. The geochemistry of glacial deposits in Taylor Valley, Antarctica: Comparison to upper continental crustal abundances. Applied Geochemistry. 2019. doi:10.1016/j.apgeochem.2019.05.006.
. The Geochemistry of Englacial Brine From Taylor Glacier, Antarctica. Journal of Geophysical Research: Biogeosciences. 2019;124(3). doi:10.1029/2018JG004411.
Geochemistry of contrasting stream types, Taylor Valley, Antarctica. GSA Bulletin. 2021;133(1/2):425-448. doi:10.1130/B35479.1.
. Geochemistry of aeolian material from the McMurdo Dry Valleys, Antarctica: Insights into Southern Hemisphere dust sources. Earth and Planetary Science Letters. 2020;547. doi:10.1016/j.epsl.2020.116460.
Geochemical zones and environmental gradients for soils from the central Transantarctic Mountains, Antarctica. Biogeosciences. 2021;18(5):1629 - 1644. doi:10.5194/bg-18-1629-2021.
The geochemical evolution of terrestrial waters in the antarctic: the role of rock-water interactions, in Physical and Biogeochemical Processes in Antarctic Lakes. 1993;59:135-143.
. Genetic diversity of soil invertebrates corroborates timing estimates for past collapses of the West Antarctic Ice Sheet. Proceedings of the National Academy of Sciences. 2020. doi:10.1073/pnas.2007925117.
Garwood Valley, Antarctica: A new record of Last Glacial Maximum to Holocene glaciofluvial processes in the McMurdo Dry Valleys. Geological Society of America Bulletin. 2013;125(9-10):1484 - 1502. doi:10.1130/B30783.1.
. Fossil fuel burning in Taylor Valley, southern Victoria Land, Antarctica: estimating the role of scientific activities on carbon and nitrogen reservoirs and fluxes. Environmental Science and Technology. 2000;34:1659-1662.
. Fe and Nutrients in Coastal Antarctic Streams: Implications for Primary Production in the Ross Sea. Journal of Geophysical Research: Biogeosciences. 2018;123(12):3507 - 3522. doi:10.1029/2017JG004352.
. Extreme hydrochemical conditions in natural microcosms entombed within Antarctic ice. Hydrological Processes. 2004;18:379-387.
Exploring the boundaries of microbial habitability in soil. Journal of Geophysical Research: Biogeosciences. 2021;126(6). doi:10.1029/2020JG006052.
Experimental formation of pore fluids in McMurdo Dry Valleys soils. Antarctic Science. 2015;27(02):163 - 171. doi:10.1017/S0954102014000479.
. Evidence of deep circulation in two perennially ice-covered Antarctic lakes. Limnol. Oceanogr. 1998;43(4):625-635.
. Evidence for dispersal and habitat controls on pond diatom communities from the McMurdo Sound Region of Antarctica. Polar Biology. 2016. doi:10.1007/s00300-016-1901-6.