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Sherwell SS, Kalra I, Li W, McKnight DM, Priscu JC, Morgan-Kiss RM. Antarctic lake phytoplankton and bacteria from near?surface waters exhibit high sensitivity to climate?driven disturbance. Environmental Microbiology. 2022. doi:10.1111/1462-2920.16113.\par \par Diaz MA, Adams B, Welch KA, et al. Aeolian material transport and its role in landscape connectivity in the McMurdo Dry Valleys, Antarctica. Journal of Geophysical Research: Earth Surface. 2018;123(12):3323 - 3337. doi:10.1029/2017JF004589.\par \par W. Lyons B, Dailey KR, Welch KA, Deuerling KM, Welch S, McKnight DM. Antarctic streams as a potential source of iron for the Southern Ocean: Figure 1. Geology. 2015;43(11):1003 - 1006. doi:10.1130/G36989.1.\par \par Gooseff MN, McKnight DM, Carr MH, Baeseman J. Antarctic McMurdo Dry Valley stream ecosystems as analog to fluvial systems on Mars. In: Doran PT, W. Lyons B, McKnight DM Life in Antarctic Deserts and other Cold Dry Environments. Life in Antarctic Deserts and other Cold Dry Environments. Cambridge: Cambridge University Press; 2010:139 - 159. doi:10.1017/CBO9780511712258.005.\par \par Esposito RMM, Horn S, McKnight DM, et al. Antarctic Climate Cooling and Response of Diatoms in Glacial Meltwater Streams. Geophysical Research Letters. 2006;33:L07406. doi:10.1029/2006GL025903.\par \par Doran PT, Priscu JC, W. Lyons B, et al. Antarctic climate cooling and terrestrial ecosystem response. Nature. 2002;415(6871):517-520. doi:10.1038/nature710.\par \par Conovitz PA. Active layer dynamics and hyporheic zone storage in three streams in the McMurdo Dy Valleys, Antarctica.  2000;M.S. doi:LTER.\par \par Runkel RL, McKnight DM, Andrews ED. Analysis of transient storage subject to unsteady flow:  diel flow variation in an Antarctic stream. Journal of the North American Benthological Society. 1998;17(2):143-154. Available at: http://www.jstor.org/stable/1467958.\par \par McKnight DM, Andrews ED, Spaulding SA, Aiken GR. Aquatic fulvic acids in algal-rich antarctic ponds. Limnology and Oceanography. 1994;39(8):1972-1979.\par \par }