McMurdo LTER Publications
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The geochemistry of upland ponds, Taylor Valley, Antarctica. Antarctic Science. 2012;24(01):3 - 14. doi:10.1017/S0954102011000617.
Groundwater seeps in Taylor Valley Antarctica: An example of a subsurface melt event. Annals of Glaciology. 2005;40:200-206. doi:LTER.
Geochemical Linkages Among Glaciers, Streams, and Lakes Within the Taylor Valley, Antarctica. In: Ecosystem Processes in a Polar Desert: The McMurdo Dry Valleys, Antarctica.Vol 72. Ecosystem Processes in a Polar Desert: The McMurdo Dry Valleys, Antarctica.; 1998:77-92.
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.
. The Geochemistry of Englacial Brine From Taylor Glacier, Antarctica. Journal of Geophysical Research: Biogeosciences. 2019;124(3). doi:10.1029/2018JG004411.
Geomicrobiology of Blood Fall: An iron-rich saline discharge at the terminus of the Taylor Glacier, Antarctica. Aquatic Geochemistry. 2004;10:199-200.
. Glacial cryoconite ecosystems: a bipolar comparison of algal communities and habitats. Nova Hedwigia. 2001;123:173-197.
. Gradient analysis of cryoconite ecosystems from two Polar glaciers. Polar Biology. 2004;27:66-74.
. Groundwater and thermal legacy of a large paleolake in Taylor Valley, East Antarctica as evidenced by airborne electromagnetic and sedimentological techniques. Department of Geology and Geophysics. 2018;M.S. Available at: https://digitalcommons.lsu.edu/gradschool_theses/4776.
. Global-scale patterns of assemblage structure of soil nematodes in relation to climate and ecosystem properties. Global Ecology and Biogeography. 2014;23(9):968 - 978. doi:10.1111/geb.2014.23.issue-910.1111/geb.12177.
Geomicrobiology of sub-glacial ice above Vostok Station. Science. 1999;286(5447):2141-2144. doi:10.1126/science.286.5447.2141.
Glycerol is an osmoprotectant in two Antarctic Chlamydomonas species from an ice-covered saline lake and is synthesized by an unusual bidomain enzyme. Frontiers in Plant Science. 2020;11. doi:10.3389/fpls.2020.01259.
. The geochemistry of minor cations within Antarctic stream water: Determining the role of the hyporheic zone. . School of Earth Sciences. 2017;B.A. Available at: http://library.ohio-state.edu/record=b8218699~S7.
. Global biodiversity scenarios for the year 2100. Science. 2000;287:1770-1774. doi:LTER.
Global environmental change and the nature of aboveground net primary productivity responses: insights from long-term experiments. Oecologia. 2015;177(4):935 - 947. doi:10.1007/s00442-015-3230-9.
A global database of soil nematode abundance and functional group composition. Scientific Data. 2020;7(1). doi:10.1038/s41597-020-0437-3.
Glacial and postglacial sedimentation in the Fryxell basin, Taylor Valley, Southern Victoria Land, Antarctica. Palaeography, Palaeoclimatology, Palaeoecology. 2006;341:320. doi:LTER.
Global Change tipping points: Above- and below-ground biotic interactions in a low diversity ecosystem. Philosophical Transactions of the Royal Society B, Biological Sciences. 2007;362(1488):2291-2306. doi:10.1098/rstb.2006.1950.
. Global decomposition experiment shows soil animal impacts on decomposition are climate dependent. Global Change Biology. 2008;14(11):2661-2677. doi:10.1111/j.1365-2486.2008.01672.x.
Geochronology of high latitude lake sediments. In: Long-Term Environmental Change in Arctic and Antarctic Lakes. Long-Term Environmental Change in Arctic and Antarctic Lakes. Kluwer Academic Publishers; 2004.
. Global change effects on above and below ground biodiversity in terrestrial ecosystems: interactions and implications for ecosystem functioning. Bioscience. 2000;50:1089-1099. doi:LTER.
Genome analysis of Plectus murrayi, a nematode from continental Antarctica. G3 Genes|Genomes|Genetics. 2021. doi:10.1093/g3journal/jkaa045.
. Genomics and transcriptomics of Antarctic nematodes reveal drivers of life history evolution and genome evolution. Department of Biology. 2018;Ph.D. Available at: https://search.proquest.com/docview/2081899003.
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