TY - JOUR T1 - Causes and characteristics of electrical resistivity variability in shallow (<4 m) soils in Taylor Valley, East Antarctica JF - Journal of Geophysical Research: Earth Surface Y1 - 2023 A1 - Gutterman, William S. A1 - Peter T. Doran A1 - Ross A. Virginia A1 - John E. Barrett A1 - Myers, Krista F. A1 - Tulaczyk, Slawek M. A1 - Foley, Neil T. A1 - Jill A. Mikucki A1 - Hilary A. Dugan A1 - Grombacher, Denys A1 - Bording, Thue S. A1 - Auken, E. KW - active layer KW - airborne electromagnetic surveys KW - McMurdo Dry Valleys KW - permafrost dynamics AB -

Airborne electromagnetic surveys collected in December 2011 and November 2018 and three soil sampling transects were used to analyze the spatial heterogeneity of shallow (<4 m) soil properties in lower Taylor Valley (TV), East Antarctica. Soil resistivities from 2011 to 2018 ranged from ∼33 Ωm to ∼3,500 Ωm with 200 Ωm assigned as an upper boundary for brine-saturated sediments. Elevations below ∼50 m above sea level (masl) typically exhibit the lowest resistivities with resistivity increasing at high elevations on steeper slopes. Soil water content was empirically estimated from electrical resistivities using Archie's Law and range from ∼<1% to ∼68% by volume. An increase in silt- and clay-sized particles at low elevations increases soil porosity but decreases hydraulic conductivity, promoting greater residence times of soil water at low elevations near Lake Fryxell. Soil resistivity variability between 2011 and 2018 shows soils at different stages of soil freeze-thaw cycles, which are caused predominantly by solar warming of soils as opposed to air temperature. This study furthers the understanding of the hydrogeologic structure of the shallow subsurface in TV and identifies locations of soils that are potentially prone to greater rates of thaw and resulting ecosystem homogenization of soil properties from projected increases in hydrological connectivity across the region over the coming decades.

VL - 128 UR - https://onlinelibrary.wiley.com/doi/10.1029/2022JF006696 IS - 2 JO - JGR Earth Surface ER - TY - JOUR T1 - Thermal legacy of a large paleolake in Taylor Valley, East Antarctica, as evidenced by an airborne electromagnetic survey JF - The Cryosphere Y1 - 2021 A1 - Myers, Krista F. A1 - Peter T. Doran A1 - Tulaczyk, Slawek M. A1 - Foley, Neil T. A1 - Bording, Thue S. A1 - Auken, Esben A1 - Hilary A. Dugan A1 - Jill A. Mikucki A1 - Foged, Nikolaj A1 - Grombacher, Denys A1 - Ross A. Virginia AB -

Previous studies of the lakes of the McMurdo Dry Valleys have attempted to constrain lake level history, and results suggest the lakes have undergone hundreds of meters of lake level change within the last 20 000 years. Past studies have utilized the interpretation of geologic deposits, lake chemistry, and ice sheet history to deduce lake level history; however a substantial amount of disagreement remains between the findings, indicating a need for further investigation using new techniques. This study utilizes a regional airborne resistivity survey to provide novel insight into the paleohydrology of the region. Mean resistivity maps revealed an extensive brine beneath the Lake Fryxell basin, which is interpreted as a legacy groundwater signal from higher lake levels in the past. Resistivity data suggest that active permafrost formation has been ongoing since the onset of lake drainage and that as recently as 1500–4000 years BP, lake levels were over 60 m higher than present. This coincides with a warmer-than-modern paleoclimate throughout the Holocene inferred by the nearby Taylor Dome ice core record. Our results indicate Mid to Late Holocene lake level high stands, which runs counter to previous research finding a colder and drier era with little hydrologic activity throughout the last 5000 years.

VL - 15 UR - https://tc.copernicus.org/articles/15/3577/2021/ IS - 8 JO - The Cryosphere ER - TY - JOUR T1 - Picocyanobacterial cells in near‐surface air above terrestrial and freshwater substrates in Greenland and Antarctica JF - Environmental Microbiology Reports Y1 - 2020 A1 - Trout‐Haney, Jessica V. A1 - Heindel, Ruth C A1 - Ross A. Virginia AB -

Bioaerosols are an important component of the total atmospheric aerosol load, with implications for human health, climate feedbacks, and the distribution and dispersal of microbial taxa. Bioaerosols are sourced from marine, freshwater, and terrestrial surfaces, with different mechanisms potentially responsible for releasing biological particles from these substrates. Little is known about the production of freshwater and terrestrial bioaerosols in polar regions. We used portable collection devices to test for the presence of picocyanobacterial aerosols above freshwater and soil substrates in the southwestern Greenland tundra and the McMurdo Dry Valleys of Antarctica. We show that picocyanobacterial cells are present in the near‐surface air at concentrations ranging from 2,431 to 28,355 cells m^−3 of air, with no significant differences among substrates or between polar regions. Our concentrations are lower than those measured using the same methods in temperate ecosystems. We suggest that aerosolization is an important process linking terrestrial and aquatic ecosystems in these polar environments, and that future work is needed to explore aerosolization mechanisms and taxon‐specific aerosolization rates. Our study is a first step toward understanding the production of bioaerosols in extreme environments dominated by microbial life.

UR - https://onlinelibrary.wiley.com/doi/abs/10.1111/1758-2229.12832 ER - TY - JOUR T1 - The hydroecology of an ephemeral wetland in the McMurdo Dry Valleys, Antarctica JF - Journal of Geophysical Research: Biogeosciences Y1 - 2019 A1 - Wlostowski, Adam A1 - Schulte, Nicholas O. A1 - Byron Adams A1 - Ball, Becky A1 - Rhea M.M. Esposito A1 - Michael N. Gooseff A1 - W. Berry Lyons A1 - Uffe N. Nielsen A1 - Ross A. Virginia A1 - Diana H. Wall A1 - Kathleen A. Welch A1 - Diane M. McKnight KW - Antarctica KW - desert hydrology KW - diatom biodiversity KW - hyporheic interactions KW - wetlands AB -

The McMurdo Dry Valleys (MDV) is a polar desert on the coast of East Antarctica where ephemeral wetlands become hydrologically active during warm and sunny summers when sub‐surface flows are generated from melting snowfields. To understand the structure and function of polar wetland ecosystems, we investigated the hydroecology of one such wetland, the Wormherder Creek wetland, during the warm and sunny summer of 2008 – 2009, when the wetland was hydrologically reactivated. Conservative tracer (LiCl) was injected for a 2‐hour period into a stream above the wetland to determine flow path orientations and hydrologic residence times. Tracer results indicated that surface water is rapidly exchanged with wetland groundwater and wetland residence times may exceed two austral summers. Major ion concentrations were uniform in samples from surface water and shallow groundwater throughout the wetland. Microbial mats in the wetland had high autotrophic index values (the ratios of chlorophyll a [Chl‐a]/ash‐free dry mass [AFDM]), ranging from 9‐38 μg Chl‐a/mg AFDM, indicative of actively photosynthesizing mat communities. The diatom communities in the mats were relatively uniform compared to those in mats from regularly flowing MDV streams, with four endemic and one widespread diatom taxa of the genus Luticola accounting for an average of 86% of the community. These results indicate that the hydrologic characteristics of the wetland contribute to uniform geochemical conditions. In turn, uniform geochemical conditions may explain the high autotrophic index values of the microbial mats and relatively low spatial variation of the diatom community.

UR - https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2019JG005153 ER - TY - JOUR T1 - The polar regions in a 2°C warmer world JF - Science Advances Y1 - 2019 A1 - Post, Eric A1 - Alley, Richard B. A1 - Christensen, Torben R. A1 - Macias-Fauria, Marc A1 - Forbes, Bruce C. A1 - Michael N. Gooseff A1 - Iler, Amy A1 - Kerby, Jeffrey T. A1 - Laidre, Kristin L. A1 - Mann, Michael E. A1 - Olofsson, Johan A1 - Stroeve, Julienne C. A1 - Ulmer, Fran A1 - Ross A. Virginia A1 - Wang, Muyin AB -

Over the past decade, the Arctic has warmed by 0.75°C, far outpacing the global average, while Antarctic tem- peratures have remained comparatively stable. As Earth approaches 2°C warming, the Arctic and Antarctic may reach 4°C and 2°C mean annual warming, and 7°C and 3°C winter warming, respectively. Expected consequences of increased Arctic warming include ongoing loss of land and sea ice, threats to wildlife and traditional human livelihoods, increased methane emissions, and extreme weather at lower latitudes. With low biodiversity, Antarctic ecosystems may be vulnerable to state shifts and species invasions. Land ice loss in both regions will contribute substantially to global sea level rise, with up to 3 m rise possible if certain thresholds are crossed. Mitigation efforts can slow or reduce warming, but without them northern high latitude warming may accelerate in the next two to four decades. International cooperation will be crucial to foreseeing and adapting to expected changes.

VL - 5 UR - http://advances.sciencemag.org/lookup/doi/10.1126/sciadv.aaw9883 IS - 12 JO - Sci. Adv. ER - TY - JOUR T1 - Biogeochemical weathering of soil apatite grains in the McMurdo Dry Valleys, Antarctica JF - Geoderma Y1 - 2018 A1 - Heindel, Ruth C A1 - W. Berry Lyons A1 - Sue Welch A1 - Spickard, Angela M A1 - Ross A. Virginia AB -

The biogeochemical weathering of the mineral apatite links the lithosphere to the biosphere by releasing the essential nutrient phosphorus (P) into the soil ecosystem. In Taylor Valley, Antarctica, faster rates of apatite weathering may be responsible for the higher concentrations of bioavailable soil P that exist in the Fryxell Basin as compared to the Bonney Basin. In this study, we use scanning electron microscopy to quantify the morphology and surface etching of individual apatite grains to determine whether the degree of apatite weathering differs between the Fryxell and Bonney Basins as well as saturated and dry soil sediments. We show that apatite grains from the Fryxell Basin are rounder, have fewer intact crystal faces, and are more chemically etched than grains from the Bonney Basin. In the Bonney Basin, apatite grains from dry soils show few signs of chemical dissolution, suggesting that soil moisture is a stronger control on the rate of apatite weathering in the Bonney Basin than in the Fryxell Basin. In addition, etch-pit morphologies in the Bonney Basin are more clearly controlled by the hexagonal crystal structure of apatite, while in the Fryxell Basin, etch pits demonstrate a wide range of morphologies without clear crystallographic control. Higher rates of apatite weathering in the Fryxell Basin may be due to the legacy of the physical abrasion of apatite grains during transport by a warm-based ice sheet, as well as the higher levels of precipitation and soil moisture closer to the coast. Our grain-scale approach provides a new perspective on P cycling in the McMurdo Dry Valleys and has implications for apatite weathering and P dynamics in the early stages of soil development.

VL - 320 UR - https://www.sciencedirect.com/science/article/pii/S0016706117320694 JO - Geoderma ER - TY - JOUR T1 - Observed trends of soil fauna in the Antarctic Dry Valleys: early signs of shifts predicted under climate change JF - Ecology Y1 - 2018 A1 - Andriuzzi, Walter S. A1 - Byron Adams A1 - John E. Barrett A1 - Ross A. Virginia A1 - Diana H. Wall AB -

Long-term observations of ecological communities are necessary for generating and testing predictions of ecosystem responses to climate change. We investigated temporal trends and spatial patterns of soil fauna along similar environmental gradients in three sites of the McMurdo Dry Valleys, Antarctica, spanning two distinct climatic phases: a decadal cool- ing trend from the early 1990s through the austral summer of February 2001, followed by a shift to the current trend of warming summers and more frequent discrete warming events. After February 2001, we observed a decline in the dominant species (the nematode Scottnema lindsayae) and increased abundance and expanded distribution of less common taxa (rotifers, tardigrades, and other nematode species). Such diverging responses have resulted in slightly greater evenness and spatial homogeneity of taxa. However, total abundance of soil fauna appears to be declining, as positive trends of the less common species so far have not compen- sated for the declining numbers of the dominant species. Interannual variation in the propor- tion of juveniles in the dominant species was consistent across sites, whereas trends in abundance varied more. Structural equation modeling supports the hypothesis that the observed biological trends arose from dissimilar responses by dominant and less common spe- cies to pulses of water availability resulting from enhanced ice melt. No direct effects of mean summer temperature were found, but there is evidence of indirect effects via its weak but signif- icant positive relationship with soil moisture. Our findings show that combining an under- standing of species responses to environmental change with long-term observations in the field can provide a context for validating and refining predictions of ecological trends in the abun- dance and diversity of soil fauna. 

VL - 99 UR - http://doi.wiley.com/10.1002/ecy.2090/full IS - 2 JO - Ecology ER - TY - JOUR T1 - Soil biological responses to C, N and P fertilization in a polar desert of Antarctica JF - Soil Biology and Biochemistry Y1 - 2018 A1 - Ball, Becky A1 - Byron Adams A1 - John E. Barrett A1 - Diana H. Wall A1 - Ross A. Virginia AB -

 

In the polar desert ecosystem of the McMurdo Dry Valleys of Antarctica, biology is constrained by available liquid water, low temperatures, as well as the availability of organic matter and nutrient elements. These soil ecosystems are climate-sensitive, where projected future warming may have profound effects on biological communities and biogeochemical cycling. Warmer temperatures will mobilize meltwater from permafrost and glaciers, may increase precipitation and may be accompanied by pulses of nutrient availability. Enhanced water and nutrient availability have the potential to greatly influence desert soil biology and ecosystem processes. The objectives of this 5-year study were to determine which nutrient elements (C, N, P) are most limiting to dry valley soil communities and whether landscape history (i.e., in situ soil type and stoichiometry) influences soil community response to nutrient additions. After 3 years of no noticeable response, soil CO2 flux was significantly higher under addition of C+ N than the other treatments, regardless of in situ soil stoichiometry, but microbial biomass and invertebrate abundance were variable and not influenced in the same manner. A stable isotope incubation suggests that fertilization increases C and N mineralization from organic matter via stimulating microbial activity, with loss of both the applied treatments as well in situ C and N. However, these responses are relatively short-lived, suggesting long-term impacts on C and N cycling would only occur if meltwater and nutrient pulses are sustained over time, a scenario that is increasingly likely for the dry valleys.

 

VL - 122 UR - http://linkinghub.elsevier.com/retrieve/pii/S0038071718301081 JO - Soil Biology and Biochemistry ER - TY - JOUR T1 - Stable C and N isotope ratios reveal soil food web structure and identify the nematode Eudorylaimus antarcticus as an omnivore–predator in Taylor Valley, Antarctica JF - Polar Biology Y1 - 2018 A1 - Shaw, E. Ashley A1 - Byron Adams A1 - John E. Barrett A1 - W. Berry Lyons A1 - Ross A. Virginia A1 - Diana H. Wall AB -

Soil food webs of the McMurdo Dry Valleys, Antarctica are simple. These include primary trophic levels of mosses, algae, cyanobacteria, bacteria, archaea, and fungi, and their protozoan and metazoan consumers (including relatively few species of nematodes, tardigrades, rotifers, and microarthropods). These biota are patchily distributed across the landscape, with greatest faunal biodiversity associated with wet soil. Understanding trophic structure is critical to studies of biotic interactions and distribution; yet, McMurdo Dry Valley soil food web structure has been inferred from limited laboratory culturing and micro- scopic observations. To address this, we measured stable isotope natural abundance ratios of C (13C/12C) and N (15N/14N) for di erent metazoan taxa (using whole body biomass) to determine soil food web structure in Taylor Valley, Antarctica. Nitrogen isotopes were most useful in di erentiating trophic levels because they fractionated predictably at higher trophic levels. Using 15N/14N, we found that three trophic levels were present in wet soil habitats. While cyanobacterial mats were the primary trophic level, the nematode Plectus murrayi, tardigrade Acutuncus antarcticus, and rotifers composed a secondary trophic level of grazers. Eudorylaimus antarcticus had a 15N/14N ratio that was 2–4‰ higher than that of grazers, indicating that this species is the sole member of a tertiary trophic level. Understanding the trophic positions of soil fauna is critical to predictions of current and future species interactions and their distributions for the McMurdo Dry Valleys, Antarctica.

VL - 41 UR - http://link.springer.com/10.1007/s00300-017-2243-8 IS - 5 JO - Polar Biol ER - TY - JOUR T1 - Stoichiometric Shifts in Soil C:N:P Promote Bacterial Taxa Dominance, Maintain Biodiversity, and Deconstruct Community Assemblages JF - Frontiers in Microbiology Y1 - 2018 A1 - Aanderud, Zachary T. A1 - Saurey, Sabrina D. A1 - Ball, Becky A1 - Diana H. Wall A1 - John E. Barrett A1 - Muscarella, Mario E. A1 - Griffin, Natasha A. A1 - Ross A. Virginia A1 - Byron Adams KW - ecological stoichiometry KW - Lake Fryxell Basin KW - McMurdo Dry Valleys KW - network community modeling KW - nutrient colimitation KW - Solirubrobacteriaceae AB -

Imbalances in C:N:P supply ratios may cause bacterial resource limitations and constrain biogeochemical processes, but the importance of shifts in soil stoichiometry are complicated by the nearly limitless interactions between an immensely rich species pool and a multiple chemical resource forms. To more clearly identify the impact of soil C:N:P on bacteria, we evaluated the cumulative effects of single and coupled long-term nutrient additions (i.e., C as mannitol, N as equal concentrations NH4 + and NO3 − , and P as Na3PO4) and water on communities in an Antarctic polar desert, Taylor Valley. Untreated soils possessed relatively low bacterial diversity, simplified organic C sources due to the absence of plants, limited inorganic N, and excess soil P potentially attenuating links between C:N:P. After 6 years of adding resources, an alleviation of C and N colimitation allowed one rare Micrococcaceae, an Arthrobacter species, to dominate, comprising 47% of the total community abundance and elevating soil respiration by 136% relative to untreated soils. The addition of N alone reduced C:N ratios, elevated bacterial richness and diversity, and allowed rare taxa relying on ammonium and nitrite for metabolism to become more abundant [e.g., nitrite oxidizing Nitrospira species (Nitrosomonadaceae), denitrifiers utilizing nitrite (Gemmatimonadaceae) and members of Rhodobacteraceae with a high affinity for ammonium]. Based on community co-occurrence networks, lower C:P ratios in soils following P and CP additions created more diffuse and less connected communities by disrupting 73% of species interactions and selecting for taxa potentially exploiting abundant P. Unlike amended nutrients, water additions alone elicited no lasting impact on communities. Our results suggest that as soils become nutrient rich a wide array of outcomes are possible from species dominance and the deconstruction of species interconnectedness to the maintenance of biodiversity.

VL - 9 UR - https://www.frontiersin.org/article/10.3389/fmicb.2018.01401/full JO - Front. Microbiol. ER - TY - JOUR T1 - Decadal ecosystem response to an anomalous melt season in a polar desert in Antarctica JF - Nature Ecology & Evolution Y1 - 2017 A1 - Michael N. Gooseff A1 - John E. Barrett A1 - Byron Adams A1 - Peter T. Doran A1 - Andrew G Fountain A1 - W. Berry Lyons A1 - Diane M. McKnight A1 - John C. Priscu A1 - Eric R. Sokol A1 - Cristina D. Takacs-Vesbach A1 - Martijn L. Vandegehuchte A1 - Ross A. Virginia A1 - Diana H. Wall VL - 1 UR - https://www.nature.com/articles/s41559-017-0253-0 IS - 9 JO - Nat Ecol Evol ER - TY - JOUR T1 - Landscape-scale soil phosphorus variability in the McMurdo Dry Valleys, Antarctica JF - Antarctic Science Y1 - 2017 A1 - Heindel, Ruth C A1 - Spickard, Angela M A1 - Ross A. Virginia VL - 29 UR - https://www.cambridge.org/core/product/identifier/S0954102016000742/type/journal_article IS - 3 ER - TY - JOUR T1 - The Impact of a Large-Scale Climate Event on Antarctic Ecosystem Processes JF - BioScience Y1 - 2016 A1 - Andrew G Fountain A1 - Saba, Grace A1 - Byron Adams A1 - Peter T. Doran A1 - Fraser, William A1 - Michael N. Gooseff A1 - Maciek K. Obryk A1 - John C. Priscu A1 - Sharon E. Stammerjohn A1 - Ross A. Virginia AB -

Extreme climate and weather events, such as a drought, hurricanes, or ice storms, can strongly imprint ecosystem processing and may alter ecosystem structure. Ecosystems in extreme environments are particularly vulnerable because of their adaptation to severe limitations in energy, water, or nutrients. The vulnerability can be expressed as a relatively long-lasting ecosystem response to a small or brief change in environmental conditions. Such an event occurred in Antarctica and affected two vastly different ecosystems: a marine-dominated coastal system and a terrestrial polar desert. Both sites experienced winds that warmed air temperatures above the 0°C threshold, resulting in extensive snow and ice melt and triggering a series of cascading effects through the ecosystems that are continuing to play out more than a decade later. This highlights the sensitivity of Antarctic ecosystems to warming events, which should occur more frequently in the future with global climate warming.

VL - 66 UR - http://academic.oup.com/bioscience/article-pdf/66/10/848/7510601/biw110.pdf IS - 10 ER - TY - JOUR T1 - Impact of diurnal freeze–thaw cycles on the soil nematode Scottnema lindsayae in Taylor Valley, Antarctica JF - Polar Biology Y1 - 2016 A1 - Matthew Knox A1 - Diana H. Wall A1 - Ross A. Virginia A1 - Martijn L. Vandegehuchte A1 - Inigo San Gil A1 - Byron Adams VL - 39 UR - https://link.springer.com/article/10.1007/s00300-015-1809-6 IS - 4 JO - Polar Biol ER - TY - JOUR T1 - Controls on diel soil CO2 flux across moisture gradients in a polar desert JF - Antarctic Science Y1 - 2015 A1 - Ball, Becky A1 - Ross A. Virginia AB -

The McMurdo Dry Valleys of Antarctica are a climate-sensitive ecosystem, where future projected climate warming will increase liquid water availability to release soil biology from physical limitations and alter ecosystem processes. For example, many studies have shown that CO2 flux, an important aspect of the carbon cycle, is controlled by temperature and moisture, which often overwhelm biotic contributions in desert ecosystems. However, these studies used either single-point measurements during peak times of biological activity or diel cycles at individual locations. Here, we present diel cycles of CO2 flux from a range of soil moisture conditions and a variety of locations and habitats to determine how diel cycles of CO2 flux vary across gradients of wet-to-dry soil and whether the water source influences the diel cycle of moist soil. Soil temperature, water content and microbial biomass significantly influenced CO2 flux. Soil temperature explained most of the variation. Soil CO2 flux moderately increased with microbial biomass, demonstrating a sometimes small but significant role of biological fluxes. Our results show that over gradients of soil moisture, both geochemical and biological fluxes contribute to soil CO2 flux, and physical factors must be considered when estimating biological CO2 flux in systems with low microbial biomass.

UR - http://journals.cambridge.org/action/displayAbstract?fromPage=online&aid=9776001&fileId=S0954102015000255 ER - TY - JOUR T1 - Deep groundwater and potential subsurface habitats beneath an Antarctic dry valley JF - Nature Communications Y1 - 2015 A1 - Jill A. Mikucki A1 - Auken, E. A1 - Tulaczyk, S A1 - Ross A. Virginia A1 - Schamper, C. A1 - Sørensen, K. I. A1 - Peter T. Doran A1 - Hilary A. Dugan A1 - Foley, N. AB - The occurrence of groundwater in Antarctica, particularly in the ice-free regions and along the coastal margins is poorly understood. Here we use an airborne transient electromagnetic (AEM) sensor to produce extensive imagery of resistivity beneath Taylor Valley. Regional-scale zones of low subsurface resistivity were detected that are inconsistent with the high resistivity of glacier ice or dry permafrost in this region. We interpret these results as an indication that liquid, with sufficiently high solute content, exists at temperatures well below freezing and considered within the range suitable for microbial life. These inferred brines are widespread within permafrost and extend below glaciers and lakes. One system emanates from below Taylor Glacier into Lake Bonney and a second system connects the ocean with the eastern 18 km of the valley. A connection between these two basins was not detected to the depth limitation of the AEM survey (~350 m). VL - 6 UR - http://www.nature.com/doifinder/10.1038/ncomms7831 JO - Nat Comms ER - TY - JOUR T1 - Ecological Biogeography of the Terrestrial Nematodes of Victoria Land, Antarctica JF - ZooKeys Y1 - 2014 A1 - Byron Adams A1 - Diana H. Wall A1 - Ross A. Virginia A1 - Broos, Emma A1 - Matthew Knox VL - 419 UR - http://zookeys.pensoft.net/articles.php?id=3899 JO - ZK ER - TY - JOUR T1 - The ecological role of moss in a polar desert: implications for aboveground- belowground and terrestrial -aquatic linkages. JF - Polar Biology Y1 - 2014 A1 - Ball, Becky A1 - Ross A. Virginia VL - 37 UR - http://link.springer.com/article/10.1007/s00300-014-1465-2 IS - 5 ER - TY - JOUR T1 - Microbial biomass and respiration responses to nitrogen fertilization in a polar desert JF - Polar Biology Y1 - 2014 A1 - Ball, Becky A1 - Ross A. Virginia UR - http://link.springer.com/article/10.1007%2Fs00300-014-1459-0 ER - TY - JOUR T1 - Aeolian flux of biotic and abiotic material in Taylor Valley, Antarctica JF - Geomorphology Y1 - 2012 A1 - Marie Šabacká A1 - John C. Priscu A1 - Hassan J. Basagic A1 - Andrew G Fountain A1 - Diana H. Wall A1 - Ross A. Virginia A1 - Mark C. Greenwood VL - 155-156 UR - http://www.sciencedirect.com/science/article/pii/S0169555X11006222 ER - TY - JOUR T1 - The ecology of pulse events: insights from an extreme climatic event in a polar desert ecosystem JF - Ecosphere Y1 - 2012 A1 - Uffe N. Nielsen A1 - Diana H. Wall A1 - Byron Adams A1 - Ross A. Virginia A1 - Ball, Becky A1 - Michael N. Gooseff A1 - Diane M. McKnight VL - 3 UR - http://www.esajournals.org/doi/abs/10.1890/ES11-00325.1 IS - 2 ER - TY - JOUR T1 - Meltwater seep patches increase heterogeneity of soil geochemistry and therefore habitat suitability JF - Geoderma Y1 - 2012 A1 - Ball, Becky A1 - Ross A. Virginia VL - 189-190 ER - TY - JOUR T1 - Thawing permafrost alters nematode populations and soil habitat characteristics in an Antarctic polar desert ecosystem JF - Pedobiologia Y1 - 2012 A1 - Smith, T.E. A1 - Diana H. Wall A1 - Hogg, I A1 - Byron Adams A1 - Uffe N. Nielsen A1 - Ross A. Virginia VL - 55 UR - http://www.sciencedirect.com/science/article/pii/S0031405611001156 IS - 2 ER - TY - JOUR T1 - Antarctic nematode communities: observed and predicted responses to climate change JF - Polar Biology Y1 - 2011 A1 - Uffe N. Nielsen A1 - Diana H. Wall A1 - Byron Adams A1 - Ross A. Virginia VL - 34 UR - http://www.springerlink.com/content/v588t5671p1w1323/ IS - 11 ER - TY - JOUR T1 - Implications of meltwater pulse events for soil biology and biogeochemical cycling in a polar desert JF - Polar Research Y1 - 2011 A1 - Ball, Becky A1 - John E. Barrett A1 - Michael N. Gooseff A1 - Ross A. Virginia A1 - Diana H. Wall VL - 3081281030352511340 UR - http://www.polarresearch.net/index.php/polar/article/view/14555 JO - Polar Research ER - TY - JOUR T1 - Nematode communities of Byers Peninsula, Livingston Island, maritime Antarctica JF - Antarctic Science Y1 - 2011 A1 - Uffe N. Nielsen A1 - Diana H. Wall A1 - Li, Grace A1 - Toro, Manuel A1 - Byron Adams A1 - Ross A. Virginia VL - 23 IS - 04 ER - TY - JOUR T1 - Experimentally increased snow accumulation alters soil moisture and animal community structure in a polar desert JF - Polar Biology Y1 - 2010 A1 - Edward Ayres A1 - Johnson N. Nkem A1 - Diana H. Wall A1 - Byron Adams A1 - John E. Barrett A1 - Breana L. Simmons A1 - Ross A. Virginia A1 - Andrew G Fountain VL - 33 IS - 7 ER - TY - JOUR T1 - Interactions between physical and biotic factors influence CO_2 flux in Antarctic dry valley soils JF - Soil Biology and Biochemistry Y1 - 2009 A1 - Ball, Becky A1 - Ross A. Virginia A1 - John E. Barrett A1 - Andrew N. Parsons A1 - Diana H. Wall VL - 41 IS - 7 ER - TY - JOUR T1 - Long-term experimental warming reduces soil nematode populations in the McMurdo Dry Valleys, Antarctica JF - Soil Biology & Biochemistry Y1 - 2009 A1 - Breana L. Simmons A1 - Diana H. Wall A1 - Byron Adams A1 - Edward Ayres A1 - John E. Barrett A1 - Ross A. Virginia VL - 41 ER - TY - JOUR T1 - Terrestrial mesofauna in above- and below-ground habitats: Taylor Valley, Antarctica JF - Polar Biology Y1 - 2009 A1 - Breana L. Simmons A1 - Diana H. Wall A1 - Byron Adams A1 - Edward Ayres A1 - John E. Barrett A1 - Ross A. Virginia VL - 32 ER - TY - JOUR T1 - Decline in a dominant invertebrate species contributes to altered carbon cycling in a low-diversity soil ecosystem JF - Global Change Biology Y1 - 2008 A1 - John E. Barrett A1 - Ross A. Virginia A1 - Diana H. Wall A1 - Byron Adams VL - 14 ER - TY - JOUR T1 - Effects of Human Trampling on Populations of Soil Fauna in the McMurdo Dry Valleys, Antarctica. JF - Conservation Biology Y1 - 2008 A1 - Edward Ayres A1 - Johnson N. Nkem A1 - Diana H. Wall A1 - Byron Adams A1 - John E. Barrett A1 - Broos, E A1 - Andrew N. Parsons A1 - Powers, Laura E. A1 - Breana L. Simmons A1 - Ross A. Virginia AB -

Antarctic ecosystems are often considered nearly pristine because levels of anthropogenic disturbance are extremely low there. Nevertheless, over recent decades there has been a rapid increase in the number of people, researchers and tourists, visiting Antarctica. We evaluated, over 10 years, the direct impact of foot traffic on the abundance of soil animals and soil properties in Taylor Valley within the McMurdo Dry Valleys region of Antarctica. We compared soils from minimally disturbed areas with soils from nearby paths that received intermediate and high levels of human foot traffic (i.e., up to approximately 80 passes per year). The nematodes Scottnema lindsayae and Eudorylaimus sp. were the most commonly found animal species, whereas rotifers and tardigrades were found only occasionally. On the highly trampled footpaths, abundance of S. lindsayae and Eudorylaimus sp. was up to 52 and 76% lower, respectively, than in untrampled areas. Moreover, reduction in S. lindsayae abundance was more pronounced after 10 years than 2 years and in the surface soil than in the deeper soil, presumably because of the longer period of disturbance and the greater level of physical disturbance experienced by the surface soil. The ratio of living to dead Eudorylaimus sp. also declined with increased trampling intensity, which is indicative of increased mortality or reduced fecundity. At one site there was evidence that high levels of trampling reduced soil CO2 fluxes, which is related to total biological activity in the soil. Our results show that even low levels of human traffic can significantly affect soil biota in this ecosystem and may alter ecosystem processes, such as carbon cycling. Consequently, management and conservation plans for Antarctic soils should consider the high sensitivity of soil fauna to physical disturbance as human presence in this ecosystem increases.

VL - 22 IS - 6 ER - TY - JOUR T1 - The influence of soil geochemistry on nematode distribution, McMurdo Dry Valleys, Antarctica JF - Arctic, Antarctic, and Alpine Research Y1 - 2008 A1 - Poage, M A1 - John E. Barrett A1 - Ross A. Virginia A1 - Diana H. Wall VL - 40 IS - 1 ER - TY - JOUR T1 - Persistent effects of a discrete climate event on a polar desert ecosystem JF - Global Change Biology Y1 - 2008 A1 - John E. Barrett A1 - Ross A. Virginia A1 - Diana H. Wall KW - Climate Response KW - nematodes VL - 14 IS - 10 ER - TY - JOUR T1 - Soil phosphorus cycling in an Antarctic polar desert JF - Geochimica et Cosmochimica Acta Y1 - 2008 A1 - D. Brad Bate A1 - John E. Barrett A1 - Poage, M A1 - Ross A. Virginia VL - 144 ER - TY - JOUR T1 - Biogeochemical stoichiometry of Antarctic Dry Valley ecosystems JF - Journal of Geophysical Research Y1 - 2007 A1 - John E. Barrett A1 - Ross A. Virginia A1 - W. Berry Lyons A1 - Diane M. McKnight A1 - John C. Priscu A1 - Andrew G Fountain A1 - Diana H. Wall A1 - Daryl L. Moorhead A1 - Peter T. Doran KW - Biggie AB -

Among aquatic and terrestrial landscapes of the McMurdo Dry Valleys, Antarctica, ecosystem stoichiometry ranges from values near the Redfield ratios for C:N:P to nutrient concentrations in proportions far above or below ratios necessary to support balanced microbial growth. This polar desert provides an opportunity to evaluate stoichiometric approaches to understand nutrient cycling in an ecosystem where biological diversity and activity are low, and controls over the movement and mass balances of nutrients operate over 10–106 years. The simple organisms (microbial and metazoan) comprising dry valley foodwebs adhere to strict biochemical requirements in the composition of their biomass, and when activated by availability of liquid water, they influence the chemical composition of their environment according to these ratios. Nitrogen and phosphorus varied significantly in terrestrial and aquatic ecosystems occurring on landscape surfaces across a wide range of exposure ages, indicating strong influences of landscape development and geochemistry on nutrient availability. Biota control the elemental ratio of stream waters, while geochemical stoichiometry (e.g., weathering, atmospheric deposition) evidently limits the distribution of soil invertebrates. We present a conceptual model describing transformations across dry valley landscapes facilitated by exchanges of liquid water and biotic processing of dissolved nutrients. We conclude that contemporary ecosystem stoichiometry of Antarctic Dry Valley soils, glaciers, streams, and lakes results from a combination of extant biological processes superimposed on a legacy of landscape processes and previous climates.

VL - 112 ER - TY - THES T1 - Ecotoxicity and microbial biogeochemistry of Fluoride in Antarctic soils Y1 - 2007 A1 - Collins, Pamela M. PB - Dartmouth College VL - B.S. ER - TY - JOUR T1 - A mathematical model for variation in water-retention curves among sandy soils JF - Antarctic Science Y1 - 2007 A1 - Hunt , H A1 - Amy M Treonis A1 - Diana H. Wall A1 - Ross A. Virginia VL - 19 ER - TY - THES T1 - Soil organic matter sources and quality in the McMurdo Dry Valleys, Antarctica Y1 - 2007 A1 - D. Brad Bate PB - Dartmouth College VL - M.S. ER - TY - JOUR T1 - Unique similarity of faunal communities across aquatic terrestrial interfaces in a polar desert ecosystem JF - Ecosystems Y1 - 2007 A1 - Edward Ayres A1 - Diana H. Wall A1 - Byron Adams A1 - John E. Barrett A1 - Ross A. Virginia ER - TY - CHAP T1 - Biogeochemistry, terrestrial T2 - Encyclopedia of the Antarctic Vol 1 Y1 - 2006 A1 - John E. Barrett A1 - Ross A. Virginia ED - B. Riffenburgh JF - Encyclopedia of the Antarctic Vol 1 PB - Routledge Press CY - New York VL - 1 ER - TY - JOUR T1 - Co-variation in soil biodiversity and biogeochemistry in Northern and Southern Victoria Land, Antarctica JF - Antarctic Science Y1 - 2006 A1 - John E. Barrett A1 - Ross A. Virginia A1 - Diana H. Wall A1 - Craig S Cary A1 - Byron Adams A1 - Hacker, A A1 - Aislabie, J VL - 18 UR - https://www.cambridge.org/core/journals/antarctic-science/article/covariation-in-soil-biodiversity-and-biogeochemistry-in-northern-and-southern-victoria-land-antarctica/C3514C28DB75F3A19DB5F266D4B1B56E ER - TY - CHAP T1 - Pedogenic carbonate distribution within glacial till in Taylor Valley, Southern Victoria Land, Antarctica T2 - Paleoenvironmental Record and Applications of Calcretes and Palustrine Carbonates Y1 - 2006 A1 - Foley, K A1 - W. Berry Lyons A1 - John E. Barrett A1 - Ross A. Virginia JF - Paleoenvironmental Record and Applications of Calcretes and Palustrine Carbonates PB - Geological Society of America ER - TY - JOUR T1 - Phosphorus fractions in soils of Taylor Valley, Antarctica JF - Soil Science Society of America Journal Y1 - 2006 A1 - Blecker, S A1 - Ippolito, J A1 - John E. Barrett A1 - Diana H. Wall A1 - Ross A. Virginia A1 - Norvell, K VL - 70 ER - TY - JOUR T1 - Salt tolerance and survival thresholds for two species of Antarctic soil nematodes JF - Polar Biology Y1 - 2006 A1 - Johnson N. Nkem A1 - Ross A. Virginia A1 - John E. Barrett A1 - Diana H. Wall A1 - Li, G VL - 29 ER - TY - JOUR T1 - Soil carbon turnover model for the McMurdo Dry Valleys, Antarctica JF - Soil Biology and Biochemistry Y1 - 2006 A1 - John E. Barrett A1 - Ross A. Virginia A1 - Andrew N. Parsons A1 - Diana H. Wall VL - 38 ER - TY - THES T1 - Soil nitrogen cycling in cold desert (McMurdo Dry Valleys) and hot desert ecosystems Y1 - 2006 A1 - Stucker, A PB - Dartmouth College VL - M.S. ER - TY - JOUR T1 - Terrestrial ecosystem processes of Victoria Land, Antarctica JF - Soil Biology and Biochemistry Y1 - 2006 A1 - John E. Barrett A1 - Johnson N. Nkem A1 - Sletten, R A1 - Steltzer, H A1 - Diana H. Wall A1 - Wallenstein, M A1 - Ross A. Virginia A1 - D. W. Hopkins A1 - Aislabie, J A1 - Bargagli, R A1 - Bockheim, J A1 - Campbell, I A1 - W. Berry Lyons A1 - Daryl L. Moorhead VL - 38 ER - TY - JOUR T1 - Wind dispersal of soil invertebrates in the McMurdo Dry Valleys, Antarctica JF - Polar Biology Y1 - 2006 A1 - Johnson N. Nkem A1 - Diana H. Wall A1 - Ross A. Virginia A1 - John E. Barrett A1 - Broos, E A1 - Porazinska, D A1 - Byron Adams KW - Biggie AB -

Dispersal of soil organisms is crucial for their spatial distribution and adaptation to the prevailing conditions of the Antarctic Dry Valleys. This study investigated the possibility of wind dispersal of soil invertebrates within the dry valleys. Soil invertebrates were evaluated in (1) pockets of transported sediments to lake ice and glacier surfaces, (2) wind-transported dust particles in collection pans (Bundt pans) 100 cm above the soil surface, and (3) sediments transported closer to the surface (<50 cm) and collected in open top chambers (OTCs). Invertebrates were extracted and identified. Nematodes were identified to species and classified according to life stage and sex. Three species of nematodes were recovered and Scottnema lindsayae was the most dominant. There were more juveniles (∼71%) in the transported sediments than adults (29%). Tardigrades and rotifers were more abundant in sediments on lake and glacier surfaces while nematodes were more abundant in the dry sediment collections of Bundt pans and OTCs. The abundance of immobile (dead) nematodes in the Bundt pans and OTCs was three times greater than active (live) nematodes. Anhydrobiosis constitutes a survival mechanism that allows wind dispersal of nematodes in the McMurdo Dry Valleys. Our results show that soil invertebrates are dispersed by wind in the Dry Valleys and are viable in ice communities on lake surfaces and glaciers.

VL - 29 UR - http://link.springer.com/content/pdf/10.1007%2Fs00300-005-0061-x ER - TY - JOUR T1 - Comment on ``El Niño suppresses Antarctic warming'' by N. Bertler et al. JF - Geophysical Research Letters Y1 - 2005 A1 - Peter T. Doran A1 - Gary D. Clow A1 - Christian H. Fritsen A1 - Christopher P. McKay A1 - Andrew N. Parsons A1 - John C. Priscu A1 - W. Berry Lyons A1 - Walsh, J A1 - Andrew G Fountain A1 - Diane M. McKnight A1 - Daryl L. Moorhead A1 - Ross A. Virginia A1 - Diana H. Wall KW - Tropical meteorology VL - 32 IS - 7 ER - TY - JOUR T1 - Distribution and diversity of soil protozoa in the McMurdo Dry Valleys of Antarctica JF - Polar Biology Y1 - 2005 A1 - Bamforth, S A1 - Diana H. Wall A1 - Ross A. Virginia VL - 28 ER - TY - JOUR T1 - Groundwater seeps in Taylor Valley Antarctica: An example of a subsurface melt event JF - Annals of Glaciology Y1 - 2005 A1 - W. Berry Lyons A1 - Kathleen A. Welch A1 - Anne E. Carey A1 - Diana H. Wall A1 - Ross A. Virginia A1 - Andrew G Fountain A1 - Peter T. Doran A1 - Csatho, B A1 - Tremper, C VL - 40 ER - TY - JOUR T1 - Invertebrate diversity in Taylor Valley soils and sediments JF - Antarctic Journal of the United States Y1 - 2005 A1 - Amy M Treonis A1 - Diana H. Wall A1 - Ross A. Virginia VL - 33 ER - TY - CHAP T1 - Polar Systems T2 - Millennium Ecosystem Assessment. Current State and Trends: Findings of the Condition and Trends Working Group Y1 - 2005 A1 - F. S. Chapin A1 - McGuire, A A1 - Nuttall, M A1 - Ross A. Virginia A1 - Young, O A1 - Zimov, S A1 - Christensen, T A1 - Godduhn, A A1 - Murphy, E A1 - Diana H. Wall A1 - Zockler, C A1 - Berman, M A1 - Callaghan, T A1 - Peter Convey A1 - A. S. Crepin A1 - Danell, K A1 - Hugh W. Ducklow A1 - Forbes, B A1 - Kofinas, G ED - R. Hassan ED - R. Scholes ED - N. Ash JF - Millennium Ecosystem Assessment. Current State and Trends: Findings of the Condition and Trends Working Group PB - Island Press ER - TY - JOUR T1 - Potential soil organic matter turnover in Taylor Valley, Antarctica JF - Arctic, Antarctic, and Alpine Research Y1 - 2005 A1 - John E. Barrett A1 - Ross A. Virginia A1 - Andrew N. Parsons A1 - Diana H. Wall KW - Biggie AB -

Antarctic Dry Valley ecosystems are among the most inhospitable soil ecosystems on earth with simple food webs and nearly undetectable fluxes of carbon (C) and nitrogen (N). Due to the lack of vascular plants, soil organic matter concentrations are extremely low, and it is unclear how much of the contemporary soil C budget is actively cycling or a legacy of paleolake production and sedimentation. While recent work indicates multiple sources of organic matter for dry valley soils, the composition and kinetics of organic pools remain poorly characterized. We examined soil organic matter pools and potential C and N turnover in soils from within six sites located across three hydrological basins of Taylor Valley, Antarctica that differed in surface age, microclimate and proximity to legacy (paleolake) sources of organic matter. We estimated potential C and N mineralization, and rate kinetics using gas exchange and repeated leaching techniques during 90-d incubations of surface soils collected from valley basin and valley slope positions in three basins of Taylor Valley. Soil organic C content was negatively correlated with the ages of underlying tills, supporting previous descriptions of legacy organic matter. Carbon and N mineralization generally followed 1st order kinetics and were well described by exponential models. Labile pools of C (90 d) were 10% of the total organic C in the upper 5 cm of the soil profile. Labile N was 50% of the total N in surface soils of Taylor Valley. These results show that a large proportion of soil C and particularly N are mineralizable under suitable conditions and suggest that a kinetically defined labile pool of organic matter is potentially active in the field during brief intervals of favorable microclimate. Climate variation changing the duration of these conditions may have potentially large effects on the small pools of C and N in these soils.

VL - 37 UR - http://instaar.metapress.com/content/e653225425230175/ IS - 1 ER - TY - JOUR T1 - The Biodiversity and Biogeochemistry of Cryoconite Holes from McMurdo Dry Valley Glaciers, Antarctica JF - Arctic, Antarctic, and Alpine Research Y1 - 2004 A1 - Porazinska, D A1 - Andrew G Fountain A1 - Thomas H. Nylen A1 - Martyn Tranter A1 - Ross A. Virginia A1 - Diana H. Wall VL - 36 IS - 1 ER - TY - JOUR T1 - Soil carbon dioxide flux from Antarctic Dry Valley soils JF - Ecosystems Y1 - 2004 A1 - Andrew N. Parsons A1 - John E. Barrett A1 - Diana H. Wall A1 - Ross A. Virginia VL - 7 IS - 3 ER - TY - THES T1 - Soil phosphorus dynamics in Taylor Valley, Antarctica Y1 - 2004 A1 - D. Brad Bate PB - Dartmouth College VL - B.S. ER - TY - JOUR T1 - Variation in biogeochemistry and soil biodiversity across spatial scales in a polar desert JF - Ecology Y1 - 2004 A1 - John E. Barrett A1 - Ross A. Virginia A1 - Diana H. Wall A1 - Andrew N. Parsons A1 - Powers, Laura E. A1 - Melody B. Burkins AB -
Desert ecosystems are characterized by distinct spatial patterning in soil
biogeochemistry and biodiversity. In the Antarctic Dry Valleys, soil polygons are prominent
features of the landscape and may be key units for scaling local ecological information to
the greater region. We examined polygon soils in each of the three basins of Taylor Valley,
Antarctica. Our objectives were to characterize variability in soil biogeochemistry and
biodiversity at local to regional scales, and to test the influence of soil properties upon
invertebrate communities. We found that soil biogeochemical properties and biodiversity
vary over multiple spatial scales from fine (,10 m) to broad (.10 km) scales. Differences
in biogeochemistry were most pronounced at broad scales among the major lake basins of
Taylor Valley corresponding to differences in geology and microclimate, while variation
in invertebrate biodiversity and abundance occurred at landscape scales of 10–500 m, and
within individual soil polygons. Variation in biogeochemistry and invertebrate communities
across these scales reflects the influence of physical processes and landscape development
over ecosystem structure in the dry valleys. The development of soil polygons influences
the spatial patterning of soil properties such as soil organic matter, salinity, moisture, and
invertebrate habitat suitability. Nematode abundance and life history data indicate that
polygon interiors are more suitable habitats than soils in the troughs at the edges of polygons.
These data suggest that physical processes (i.e., polygon development) and biogeochemistry
are important influences on the spatial variability of biotic communities in dry valley soil
ecosystems.
VL - 85 IS - 11 ER - TY - JOUR T1 - Organic matter and soil biota of upland wetlands in Taylor Valley, Antarctica JF - Polar Biology Y1 - 2003 A1 - Daryl L. Moorhead A1 - John E. Barrett A1 - Ross A. Virginia A1 - Diana H. Wall A1 - Porazinska, D VL - 26 ER - TY - JOUR T1 - Antarctic climate cooling and terrestrial ecosystem response JF - Nature Y1 - 2002 A1 - Peter T. Doran A1 - John C. Priscu A1 - W. Berry Lyons A1 - John E. Walsh A1 - Andrew G Fountain A1 - Diane M. McKnight A1 - Daryl L. Moorhead A1 - Ross A. Virginia A1 - Diana H. Wall A1 - Gary D. Clow A1 - Christian H. Fritsen A1 - Christopher P. McKay A1 - Andrew N. Parsons KW - Climate Response VL - 415 IS - 6871 ER - TY - JOUR T1 - Distribution and life cycle of Scottnema lindsayae (Nematoda) in Antarctic soils: A modeling analysis of tempaerature responses JF - Polar Biology Y1 - 2002 A1 - Daryl L. Moorhead A1 - Diana H. Wall A1 - Ross A. Virginia A1 - Andrew N. Parsons VL - 25 ER - TY - JOUR T1 - Field and microcosm studies of decomposition and soil biota in a cold dessert soil JF - Ecosystems Y1 - 2002 A1 - Amy M Treonis A1 - Diana H. Wall A1 - Ross A. Virginia VL - 5 IS - 159-170 ER - TY - JOUR T1 - Invertebrates in ornithogenic soils at Ross Island, Antarctica. JF - Polar Biology Y1 - 2002 A1 - Porazinska, D A1 - Diana H. Wall A1 - Ross A. Virginia VL - 25 ER - TY - JOUR T1 - Population age structure of nematodes in the Antarctic Dry Valleys: perspectives on time, space, and habitat suitability JF - Arctic,Antarctic, and Alpine Research Y1 - 2002 A1 - Porazinska, D A1 - Diana H. Wall A1 - Ross A. Virginia VL - 34 ER - TY - JOUR T1 - Recent Temperature Trends in the Antarctic JF - Nature Y1 - 2002 A1 - John E. Walsh A1 - Gary D. Clow A1 - Christian H. Fritsen A1 - Christopher P. McKay A1 - Andrew N. Parsons A1 - Peter T. Doran A1 - John C. Priscu A1 - W. Berry Lyons A1 - Andrew G Fountain A1 - Diane M. McKnight A1 - Daryl L. Moorhead A1 - Ross A. Virginia A1 - Diana H. Wall VL - 418 ER - TY - JOUR T1 - Snow patch influence on soil biogeochemical processes and invertebrate distribution in the McMurdo Dry Valleys, Antarctica JF - Arctic, Antarctic, and Alpine Research Y1 - 2002 A1 - Michael N. Gooseff A1 - John E. Barrett A1 - Peter T. Doran A1 - Andrew G Fountain A1 - W. Berry Lyons A1 - Andrew N. Parsons A1 - Porazinska, D A1 - Ross A. Virginia A1 - Diana H. Wall KW - Biggie VL - 35 UR - http://instaar.metapress.com/content/r086455ju7213711/ IS - 1 ER - TY - JOUR T1 - Trends in resin and KCl-extractable soil nitrogen across landscape gradients in Taylor Valley, Antarctica JF - Ecosystems Y1 - 2002 A1 - John E. Barrett A1 - Ross A. Virginia A1 - Diana H. Wall VL - 5 ER - TY - CHAP T1 - Basic Principles in ecosystem functioning T2 - Encyclopedia of Biodiversity Y1 - 2001 A1 - Ross A. Virginia A1 - Diana H. Wall ED - S. Levin JF - Encyclopedia of Biodiversity PB - Academic Press VL - 2 ER - TY - JOUR T1 - Determining habitat suitability for soil invertebrates in an extreme environment: The McMurdo Dry Valleys, Antarctica. JF - Antarctic Science Y1 - 2001 A1 - Courtright, E A1 - Diana H. Wall A1 - Ross A. Virginia VL - 13 ER - TY - JOUR T1 - Organic carbon cycling in Taylor Valley, Antarctica: Quantifying soil reservoirs and soil respiration JF - Global Change Biology Y1 - 2001 A1 - Melody B. Burkins A1 - Ross A. Virginia A1 - Diana H. Wall VL - 7 ER - TY - JOUR T1 - Nuclear and mitochondrial DNA sequence diversity in the Antarctic nematode Scottnema lindsayae JF - Journal of Nematology Y1 - 2000 A1 - Courtright, E A1 - Diana H. Wall A1 - Ross A. Virginia A1 - Vida, J A1 - Frisse, L A1 - Thomas, W VL - 322 ER - TY - JOUR T1 - The Origin of Soil Organic Matter in Taylor Valley, Antarctica: A Legacy of Climate Change JF - Ecology Y1 - 2000 A1 - Melody B. Burkins A1 - Ross A. Virginia A1 - C. Page Chamberlain A1 - Diana H. Wall KW - legacy VL - 81 ER - TY - JOUR T1 - The use of anhydrobiosis by soil nematodes in the Antarctic Dry Valleys JF - Functional Ecology Y1 - 2000 A1 - Amy M Treonis A1 - Diana H. Wall A1 - Ross A. Virginia KW - Biggie KW - survival strategies VL - 14 UR - http://onlinelibrary.wiley.com/doi/10.1046/j.1365-2435.2000.00442.x/full IS - 4 ER - TY - JOUR T1 - Controls on soil biodiversity: insight s from extreme environments JF - Applied Soil Ecology Y1 - 1999 A1 - Diana H. Wall A1 - Ross A. Virginia VL - 13 ER - TY - JOUR T1 - Invertebrate biodiversity in Antarctic Dry Valley soils and sediments JF - Ecosystems Y1 - 1999 A1 - Amy M Treonis A1 - Diana H. Wall A1 - Ross A. Virginia VL - 2 ER - TY - JOUR T1 - Physical controls on the Taylor Valley Ecosystem, Antarctica JF - BioScience Y1 - 1999 A1 - Andrew G Fountain A1 - W. Berry Lyons A1 - Melody B. Burkins A1 - Gayle L. Dana A1 - Peter T. Doran A1 - Karen J. Lewis A1 - Diane M. McKnight A1 - Daryl L. Moorhead A1 - Andrew N. Parsons A1 - John C. Priscu A1 - Diana H. Wall A1 - Robert A. Wharton Jr. A1 - Ross A. Virginia KW - Water availability VL - 49 IS - 12 ER - TY - CHAP T1 - The world beneath our feet: Soil biodiversity and ecosystem functioning T2 - Nature and Human Society: The Quest for a Sustainable World Y1 - 1999 A1 - Diana H. Wall A1 - Ross A. Virginia JF - Nature and Human Society: The Quest for a Sustainable World PB - National Academy of Sciences Press ER - TY - JOUR T1 - Distribution, Community Structure, and Microhabitats of Soil Invertebrates along an Elevational Gradient in Taylor Valley JF - Alpine and Alpine Research Y1 - 1998 A1 - Powers, Laura E. A1 - Mengchi Ho A1 - Diana W. Freckman A1 - Ross A. Virginia VL - 30 IS - 2 ER - TY - JOUR T1 - McMurdo Dry Valleys LTER: Genetic diversity of soil nematodes in the McMurdo Dry Valleys of Antarctica JF - Antarctic Journal of the United States - 1996 Review Issue (NSF 98-28) Y1 - 1998 A1 - Courtright, Ericha M A1 - Diana W. Freckman A1 - Ross A. Virginia A1 - W. Kelley Thomas VL - 31 IS - 2 ER - TY - JOUR T1 - Natural abundance of carbon and nitrogen isotopes in potential sources of organic matter to soils of Taylor Valley, Antarctica JF - Antarctic Journal of the United States - 1996 Review Issue (NSF 98-28) Y1 - 1998 A1 - Melody B. Burkins A1 - C. Page Chamberlain A1 - Ross A. Virginia A1 - Diana W. Freckman VL - 31 IS - 2 ER - TY - JOUR T1 - Soil Biodiversity and Community Structure in the McMurdo Dry Valleys, Antarctica, in Ecosystem Processes in a Polar Desert: The McMurdo Dry Valleys, Antarctica JF - Antarctic Research Series Y1 - 1998 A1 - Diana W. Freckman A1 - Ross A. Virginia VL - 72 ER - TY - JOUR T1 - Carbon cycling in soils of the McMurdo Dry Valley region, Antarctica JF - Bulletin of the Ecological Society of America Supplement Y1 - 1997 A1 - Melody B. Burkins A1 - Ross A. Virginia A1 - Diana W. Freckman A1 - C. Page Chamberlain VL - 78 IS - 4 ER - TY - JOUR T1 - Low-diversity Antarctic soil nematode communities: distribution and response to disturbance JF - Ecology Y1 - 1997 A1 - Diana W. Freckman A1 - Ross A. Virginia VL - 78 IS - 2 ER - TY - JOUR T1 - Open-top Designs for Manipulating Field Temperature in High-Latitude Ecosystems JF - Global Change Biology Y1 - 1997 A1 - G. M. Marion A1 - G.H.R. Henry A1 - Diana W. Freckman A1 - J. Johnstone A1 - G. Jones A1 - M.H. Jones A1 - E. Levesque A1 - U. Molau A1 - P. MØLGAARD A1 - Andrew N. Parsons A1 - J. Svoboda A1 - Ross A. Virginia VL - 3 IS - S1 ER - TY - JOUR T1 - Effects of human disturbance on soil nematode populations in Taylor Valley, Antarctica JF - Bulletin of the Ecological Society of America Supplement Y1 - 1996 A1 - Powers, Laura E. A1 - Diana W. Freckman A1 - Ross A. Virginia VL - 77 IS - 3 ER - TY - JOUR T1 - Soil spatial variation along a toposequence in Taylor Valley, Antarctica JF - Bulletin of the Ecological Society of America Supplement Y1 - 1996 A1 - Mengchi Ho A1 - Ross A. Virginia A1 - Diana W. Freckman VL - 77 IS - 3 ER - TY - JOUR T1 - Sources and distribution of abundance of organic matter in the Dry Valley soils of southern Victoria Land, Antarctica JF - Bulletin of the Ecological Society of America Supplement Y1 - 1996 A1 - Melody J. Brown A1 - Ross A. Virginia A1 - C. Page Chamberlain VL - 77 IS - 3 ER - TY - JOUR T1 - McMurdo LTER: Soil properties associated with nematode distribution along an elevational transect in Taylor Valley, Antarctica JF - Antarctic Journal of the U.S. Y1 - 1995 A1 - Powers, Laura E. A1 - Diana W. Freckman A1 - Mengchi Ho A1 - Ross A. Virginia VL - 30 IS - 5 ER - TY - JOUR T1 - Soil chemistry along a glacial chronosequence on Andrews Ridge, Taylor Valley JF - Antarctic Journal of the U.S. Y1 - 1995 A1 - Mengchi Ho A1 - Ross A. Virginia A1 - Powers, Laura E. A1 - Diana W. Freckman VL - 30 IS - 5 ER - TY - JOUR T1 - Spatial Distribution of Nematodes in Polar Desert Soils of Antarctica JF - Polar Biology Y1 - 1995 A1 - Powers, Laura E. A1 - Diana W. Freckman A1 - Ross A. Virginia VL - 15 IS - 5 ER - TY - JOUR T1 - Depth distribution of soil nematodes in Taylor Valley, Antarctica JF - Antarctic Journal of the U.S. Y1 - 1994 A1 - Powers, Laura E. A1 - Diana W. Freckman A1 - Ross A. Virginia VL - 29 IS - 5 ER - TY - JOUR T1 - McMurdo LTER:Soil and nematode distribution along an elevational gradient in Taylor Valley, Antarctica JF - Antarctic Journal of the U.S. Y1 - 1994 A1 - Powers, Laura E. A1 - Diana W. Freckman A1 - Mengchi Ho A1 - Ross A. Virginia VL - 29 IS - 5 ER - TY - JOUR T1 - Nematode biodiversity and community structure in Antarctic Polar Desert Soils JF - Bulletin of the Ecological Society of America Y1 - 1994 A1 - Powers, Laura E. A1 - Diana W. Freckman A1 - Ross A. Virginia KW - Biggie VL - 75 ER - TY - CHAP T1 - Nematode biodiversity and survival in Antarctic Dry Valley soils T2 - SCAR 6th Biology Symposium Y1 - 1994 A1 - Diana W. Freckman A1 - Ross A. Virginia A1 - Powers, Laura E. JF - SCAR 6th Biology Symposium CY - Venice, Italy ER - TY - JOUR T1 - Survival of Scottnema lindsayae under extreme osmotic conditions JF - Society of Nematologists Y1 - 1994 A1 - Powers, Laura E. A1 - Diana W. Freckman A1 - Ross A. Virginia ER - TY - JOUR T1 - The ecology of nematodes in Antarctic Dry Valley soils JF - Antarctic Journal of the U.S. Y1 - 1993 A1 - Diana W. Freckman A1 - Ross A. Virginia VL - 28 ER - TY - JOUR T1 - Extraction of nematodes from Dry Valley Antarctic soils JF - Polar Biology Y1 - 1993 A1 - Diana W. Freckman A1 - Ross A. Virginia VL - 13 IS - 7 ER - TY - JOUR T1 - Life Cycle of the Microbivorous Antarctic Dry Valley Nematode Scottnema lindsaye Timm 1971 JF - Polar Biology Y1 - 1993 A1 - A. Overhoff A1 - Diana W. Freckman A1 - Ross A. Virginia VL - 13 IS - 3 ER - TY - JOUR T1 - Nematodes and soil properties in the Dry Valleys of southern Victoria Land, Antarctica JF - Bulletin of the Ecological Society of America Y1 - 1992 A1 - Diana W. Freckman A1 - Ross A. Virginia VL - 73 IS - 2 ER - TY - JOUR T1 - Nematodes in Antarctic Dry Valley soils: extraction and distribution JF - Journal of Nematology Y1 - 1992 A1 - Diana W. Freckman A1 - Ross A. Virginia VL - 24 ER - TY - JOUR T1 - Nematodes in the McMurdo Dry Valleys of Southern Victoria Land JF - Antarctic Journal of the United States Y1 - 1991 A1 - Diana W. Freckman A1 - Ross A. Virginia VL - 26 ER - TY - JOUR T1 - Nematode Ecology of the McMurdo Dry Valley Ecosystems JF - Antarctic Journal of the United States Y1 - 1990 A1 - Diana W. Freckman A1 - Ross A. Virginia VL - 25 ER -