McMurdo LTER Publications
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Diversity and Distribution of Freshwater Aerobic Anoxygenic Phototrophic Bacteria across a Wide Latitudinal Gradient. Frontiers in Microbiology. 2017;8. doi:10.3389/fmicb.2017.00175.
. High-resolution elevation mapping of the McMurdo Dry Valleys, Antarctica, and surrounding regions. Earth System Science Data. 2017;9:435 - 443. doi:10.5194/essd-9-435-2017.
High-resolution elevation mapping of the McMurdo Dry Valleys, Antarctica, and surrounding regions. Earth System Science Data. 2017;9:435 - 443. doi:10.5194/essd-9-435-2017.
Impacts of permafrost degradation on a stream in Taylor Valley, Antarctica. Geomorphology. 2017;285:205 - 213. doi:10.1016/j.geomorph.2017.02.009.
. Glaciers in equilibrium, McMurdo Dry Valleys, Antarctica. Journal of Glaciology. 2016;62(235):976 - 989. doi:10.1017/jog.2016.86.
. The Impact of a Large-Scale Climate Event on Antarctic Ecosystem Processes. BioScience. 2016;66(10):848 - 863. doi:10.1093/biosci/biw110.
The Impact of a Large-Scale Climate Event on Antarctic Ecosystem Processes. BioScience. 2016;66(10):848 - 863. doi:10.1093/biosci/biw110.
Responses of Antarctic Marine and Freshwater Ecosystems to Changing Ice Conditions. BioScience. 2016;66(10):864 - 879. doi:10.1093/biosci/biw109.
Deep groundwater and potential subsurface habitats beneath an Antarctic dry valley. Nature Communications. 2015;6:6831. doi:10.1038/ncomms7831.
Experimental formation of pore fluids in McMurdo Dry Valleys soils. Antarctic Science. 2015;27(02):163 - 171. doi:10.1017/S0954102014000479.
. 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.
Patterns and processes of salt efflorescences in the McMurdo region, Antarctica. Artic, Antarctic and Alpine Research. 2015. Available at: http://aaarjournal.org/doi/abs/10.1657/AAAR0014-024.
A roadmap for Antarctic and Southern Ocean science for the next two decades and beyond. Antarctic Science. 2015;27(01):3 - 18. doi:10.1017/S0954102014000674.
A roadmap for Antarctic and Southern Ocean science for the next two decades and beyond. Antarctic Science. 2015;27(01):3 - 18. doi:10.1017/S0954102014000674.
A roadmap for Antarctic and Southern Ocean science for the next two decades and beyond. Antarctic Science. 2015;27(01):3 - 18. doi:10.1017/S0954102014000674.
Elemental Cycling in a Flow-Through Lake in the McMurdo Dry Valleys, Antarctica: Lake Miers. . Earth Sciences. 2014;Master Thesis:122. Available at: https://etd.ohiolink.edu/!etd.send_file?accession=osu1413291502&disposition=inline.
. Forum: Climate Change and Environmental History. Environmental History. 2014;19(2):281 - 364. doi:10.1093/envhis/emu004.
Hyperspectral measurements of wet, dry and saline soils from the McMurdo Dry Valleys: soil moisture properties from remote sensing. Antarctic Science. 2014;26(05):565 - 572. doi:10.1017/S0954102013000977.
. The McMurdo Dry Valleys: A landscape on the threshold of change. Geomorphology. 2014;225:25 - 35. doi:10.1016/j.geomorph.2014.03.044.
. Near-Surface Internal Melting - a Substantial Mass Loss on Antarctic Dry Valley Glaciers. Journal of Glaciology. 2014;60:361-374. doi:10.3189/2014JoG13J095.
. The spatial structure of Antarctic biodiversity. Ecological Monographs. 2014;84(2):203 - 244. doi:10.1890/12-2216.1.
Spring thaw ionic pulses boost nutrient availability and microbial growth in entombed Antarctic Dry Valley cryoconite holes. Frontiers in Microbiology. 2014;5. doi:10.3389/fmicb.2014.00694.
Accelerated thermokarst formation in the McMurdo Dry Valleys, Antarctica. Scientific Reports. 2013;3. doi:10.1038/srep02269.
Carbon Sequestration and Release from Antarctic Lakes: Lake Vida and West Lake Bonney (McMurdo Dry Valleys). Aquatic Geochemistry. 2013;19(2):135 - 145. doi:10.1007/s10498-012-9184-1.
. Characterization of fulvic acid fractions of dissolved organic matter during ice-out in a hyper-eutrophic, coastal pond in Antarctica. Environmental Research Letters. 2013;8(4):045015. doi:10.1088/1748-9326/8/4/045015.