The spatial structure of Antarctic biodiversity. Ecological Monographs 84, 203 - 244 (2014).
Spring thaw ionic pulses boost nutrient availability and microbial growth in entombed Antarctic Dry Valley cryoconite holes. Frontiers in Microbiology 5, (2014).
Accelerated thermokarst formation in the McMurdo Dry Valleys, Antarctica. Scientific Reports 3, (2013).
Antarctic Thresholds - Ecosystem Resilience and Adaptation (AnT-ERA), a new SCAR-biology programme. Polarforschung 82, 147-150. (2013).
Are the Dry Valleys getting wetter? A preliminary assessment of wetness across the McMurdo Dry Valleys landscape. Department of Civil & Environmental Engineering M.S., (2013).
Carbon Sequestration and Release from Antarctic Lakes: Lake Vida and West Lake Bonney (McMurdo Dry Valleys). Aquatic Geochemistry 19, 135 - 145 (2013).
The carbon stable isotope biogeochemistry of streams, Taylor Valley, Antarctica. Applied Geochemistry 32, 26 - 36 (2013).
Characterization of fulvic acid fractions of dissolved organic matter during ice-out in a hyper-eutrophic, coastal pond in Antarctica. Environmental Research Letters 8, 045015 (2013).
Characterization of IHSS Pony Lake fulvic acid dissolved organic matter by electrospray ionization Fourier transform ion cyclotron resonance mass spectrometry and fluorescence spectroscopy. Organic Geochemistry 65, 19 - 28 (2013).
CORRIGENDUM: Don Juan Pond, Antarctica: Near-surface CaCl2-brine feeding Earth’s most saline lake and implications for Mars. Scientific Reports 3, (2013).
Distribution of Siliceous-Walled Algae in Taylor Valley, Antarctica Lakes. International Journal of Geosciences 04, 688 - 699 (2013).
Do Cryoconite Holes have the Potential to be Significant Sources of C, N, and P to Downstream Depauperate Ecosystems of Taylor Valley, Antarctica?. Arctic, Antarctic, and Alpine Research 45, 440 - 454 (2013).
Don Juan Pond, Antarctica: Near-surface CaCl2-brine feeding Earth's most saline lake and implications for Mars. Scientific Reports 3, (2013).
Environmental controls over bacterial communities in polar desert soils. Ecosphere 4, art127 (2013).
Environmental factors influencing diatom communities in Antarctic cryoconite holes. Environmental Research Letters 8, 045006 (2013).
Factors Controlling Soil Microbial Biomass and Bacterial Diversity and Community Composition in a Cold Desert Ecosystem: Role of Geographic Scale. PLoS ONE 8, e66103 (2013).
The future of soil invertebrate communities in polar regions: different climate change responses in the Arctic and Antarctic?. Ecology Letters 16, 409 - 419 (2013).
Garwood Valley, Antarctica: A new record of Last Glacial Maximum to Holocene glaciofluvial processes in the McMurdo Dry Valleys. Geological Society of America Bulletin 125, 1484 - 1502 (2013).
How big are the McMurdo Dry Valleys? Estimating ice-free area using Landsat image data. Antarctic Science 25, 119 - 120 (2013).
The influence of stream thermal regimes and preferential flow paths on hyporheic exchange in a glacial meltwater stream. Water Resources Research 49, 5552 - 5569 (2013).
Lake ice ablation rates from permanently ice-covered Antarctic lakes. Journal of Glaciology 59, (2013).
The Life Cycle of the Antarctic Nematode Plectus murrayi Under Laboratory Conditions. Journal of nematology 45, 39-42 (2013).
Local and regional influences over soil microbial metacommunities in the Transantarctic Mountains. Ecosphere 4, art136 (2013).
Microbial growth under humic-free conditions in a supraglacial stream system on the Cotton Glacier, Antarctica. Environmental Research Letters 8, 035022 (2013).
Micro-hole and multigrain quartz luminescence dating of Paleodeltas at Lake Fryxell, McMurdo Dry Valleys (Antarctica), and relevance for lake history. Quaternary Geochronology 18, 119 - 134 (2013).