McMurdo LTER Publications

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Welch KA, W. Lyons B, Whisner C, et al. Spatial variations in the geochemistry of glacial meltwater streams in the Taylor Valley, Antarctica. Antarctic Science. 2010;22(06):662 - 672. doi:10.1017/S0954102010000702.
Welch KA, W. Lyons B, Whisner C, et al. Spatial variations in the geochemistry of glacial meltwater streams in the Taylor Valley, Antarctica. Antarctic Science. 2010;22(06):662 - 672. doi:10.1017/S0954102010000702.
Langford ZL, Gooseff MN, Lampkin DJ. Spatiotemporal Dynamics of Wetted Soils across a Polar Desert Landscape, McMurdo Dry Valleys Antarctica. Antarctic Science. 2015;27(2):197-209. doi:10.1017/S0954102014000601.
Gooseff MN, W. Lyons B, McKnight DM, Vaughn BH, Fountain AG, Dowling C. A stable isotopic investigation of a polar desert hydrologic system, McMurdo Dry Valleys, Antarctica. Arctic, Antarctic, and Alpine Research. 2006;38(1):60-71. doi:10.1657/1523-0430(2006)038[0060:ASIIOA]2.0.CO;2.
Aanderud ZT, Saurey SD, Ball B, et al. Stoichiometric Shifts in Soil C:N:P Promote Bacterial Taxa Dominance, Maintain Biodiversity, and Deconstruct Community Assemblages. Frontiers in Microbiology. 2018;9. doi:10.3389/fmicb.2018.01401.
Sinsabaugh R, Gallo M, Gartner T, et al. Stoichiometry of soil enzyme activity at global scale. Ecology Letters. 2008;11:1252-1264. doi:LTER.
Sinsabaugh R, Gallo M, Gartner T, et al. Stoichiometry of soil enzyme activity at global scale. Ecology Letters. 2008;11:1252-1264. doi:LTER.
Gooseff MN, Van Horn DJ, Sudman Z, McKnight DM, Welch KA, W. Lyons B. Stream biogeochemical and suspended sediment responses to permafrost degradation in stream banks in Taylor Valley, Antarctica. Biogeosciences. 2016;13(6):1723 - 1732. doi:10.5194/bg-13-1723-2016.
Singley JG. Stream corridor connectivity controls on nitrogen cycling. Hinckley E-LS, Gooseff MN. 2021;PhD. Available at: https://www.proquest.com/docview/2572593127.
Von Guerard P, McKnight DM, Harnish RA, Gartner JW, Andrews ED. Streamflow, water-temperature, and specific-conductance data for selected streams draining into Lake Fryxell, Lower Taylor Valley, Victoria Land, Antarctica, 1990-92. U.S. Geological Survey. Open-File Report 94-545. 1995.
W. Lyons B, Nezat CA, Benson L, et al. Strontium isotopic signatures of the streams and lakes of Taylor Valley, southern Victoria Land, Antarctica: chemical weathering in a polar climate. Aquatic Geochemistry. 2003;8:875-895.
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Dana GL, Davis R, Fountain AG, Wharton, Jr. RA. A Temperature area index of stream discharge in Taylor Valley, Antarctica. In: Pietroniro A, Granger R, Pultz TJ Applications of Remote Sensing in Hydrology. Applications of Remote Sensing in Hydrology. National Water Research Institute , Environment Canada; 1998:29-39.
Gutt J, Isla E, Xavier JC, et al. Ten scientific messages on risks and opportunities for life in the Antarctic. Antarctic Environments Portal; 2022. Available at: https://environments.aq/publications/ten-scientific-messages-on-risks-and-opportunities-for-life-in-the-antarctic/.
Gutt J, Isla E, Xavier JC, et al. Ten scientific messages on risks and opportunities for life in the Antarctic. Antarctic Environments Portal; 2022. Available at: https://environments.aq/publications/ten-scientific-messages-on-risks-and-opportunities-for-life-in-the-antarctic/.
Darling JP, Garland DD, Stanish LF, Esposito RMM, Sokol ER, McKnight DM. Thermal autecology describes the occurrence patterns of four benthic diatoms in McMurdo Dry Valley streams. Polar Biology. 2017;40(12):2381-2396. doi:10.1007/s00300-017-2151-y.
Ikard S, Gooseff MN, Barrett JE, Takacs-Vesbach CD. Thermal Characterisation of Active Layer Across a Soil Moisture Gradient in the McMurdo Dry Valleys, Antarctica. Permafrost and Periglacial Processes. 2009;20:27-39. doi:10.1002/ppp.634.
Myers KF, Doran PT, Tulaczyk SM, et al. Thermal legacy of a large paleolake in Taylor Valley, East Antarctica, as evidenced by an airborne electromagnetic survey. The Cryosphere. 2021;15(8):3577 - 3593. doi:10.5194/tc-15-3577-2021.
O’Brien KM, Crockett EL, Adams B, et al. The time is right for an Antarctic biorepository network. Proceedings of the National Academy of Sciences. 2022;119(50). doi:10.1073/pnas.2212800119.
Gulati S, Richmond K, Flesher C, et al. Toward autonomous scientific exploration of ice-covered lakes—Field experiments with the ENDURANCE AUV in an Antarctic Dry Valley. In: 2010 IEEE International Conference on Robotics and Automation (ICRA 2010)2010 IEEE International Conference on Robotics and Automation. 2010 IEEE International Conference on Robotics and Automation (ICRA 2010)2010 IEEE International Conference on Robotics and Automation. Anchorage, AK: IEEE; 2010:308 - 315. doi:10.1109/ROBOT.2010.5509224.
Wlostowski A, Gooseff MN, McKnight DM, W. Lyons B. Transit times and rapid chemical equilibrium explain chemostasis in glacial meltwater streams in the McMurdo Dry Valleys, Antarctica. Geophysical Research Letters. 2018;45(24):13322 - 13331. doi:10.1029/2018GL080369.
Gooseff MN, McKnight DM, Doran PT, W. Lyons B. Trends in discharge and flow season timing of the Onyx River, Wright Valley, Antarctica since 1969. Cooper A, Raymond C, Team ISAESEditorial. Antarctica; A keystone in a changing world--online proceedings for the tenth international symposium. 2007. doi:LTER.
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Geyer KM, Barrett JE. Unimodal productivity–diversity relationships among bacterial communities in a simple polar soil ecosystem. Environmental Microbiology. 2019;21(7). doi:10.1111/1462-2920.14639.
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Kepner RL, Wharton, Jr. RA, Galchenko V. Viruses in antarctic lakes: a first assessment of their distribution. Bulletin of the Ecological Society of America Supplement. 1996;77(3):230.
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Levy JS, Fountain AG, Gooseff MN, et al. Water track modification of soil ecosystems in the Lake Hoare basin, Taylor Valley, Antarctica. Antarctic Science. 2013:1 - 10. doi:10.1017/S095410201300045X.
Levy JS, Fountain AG, Gooseff MN, Welch KA, W. Lyons B. Water tracks and permafrost in Taylor Valley, Antarctica: Extensive and shallow groundwater connectivity in a cold desert ecosystem. Geological Society of America Bulletin. 2011;123(11-12):2295-2311. doi:10.1130/B30436.1.

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