<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Jackson, Abigail C.</style></author><author><style face="normal" font="default" size="100%">Jorna, Jesse</style></author><author><style face="normal" font="default" size="100%">Chaston, J</style></author><author><style face="normal" font="default" size="100%">Adams, Byron J.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Glacial legacies: Microbial communities of Antarctic refugia</style></title><secondary-title><style face="normal" font="default" size="100%">Biology</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Antarctica</style></keyword><keyword><style  face="normal" font="default" size="100%">McMurdo Dry Valleys</style></keyword><keyword><style  face="normal" font="default" size="100%">metabarcoding</style></keyword><keyword><style  face="normal" font="default" size="100%">microbial communities</style></keyword><keyword><style  face="normal" font="default" size="100%">refugia</style></keyword><keyword><style  face="normal" font="default" size="100%">soil biodiversity</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2022</style></year><pub-dates><date><style  face="normal" font="default" size="100%">10/2022</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.mdpi.com/2079-7737/11/10/1440</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">11</style></volume><pages><style face="normal" font="default" size="100%">1440</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;In the cold deserts of the McMurdo Dry Valleys (MDV) the suitability of soil for microbial life is determined by both contemporary processes and legacy effects. Climatic changes and accompanying glacial activity have caused local extinctions and lasting geochemical changes to parts of these soil ecosystems over several million years, while areas of refugia may have escaped these disturbances and existed under relatively stable conditions. This study describes the impact of historical glacial and lacustrine disturbance events on microbial communities across the MDV to investigate how this divergent disturbance history influenced the structuring of microbial communities across this otherwise very stable ecosystem. Soil bacterial communities from 17 sites representing either putative refugia or sites disturbed during the Last Glacial Maximum (LGM) (22&amp;ndash;17 kya) were characterized using 16 S metabarcoding. Regardless of geographic distance, several putative refugia sites at elevations above 600 m displayed highly similar microbial communities. At a regional scale, community composition was found to be influenced by elevation and geographic proximity more so than soil geochemical properties. These results suggest that despite the extreme conditions, diverse microbial communities exist in these putative refugia that have presumably remained undisturbed at least through the LGM. We suggest that similarities in microbial communities can be interpreted as evidence for historical climate legacies on an ecosystem-wide scale.&lt;/p&gt;</style></abstract><issue><style face="normal" font="default" size="100%">10</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Xue, Xia</style></author><author><style face="normal" font="default" size="100%">Suvorov, Anton</style></author><author><style face="normal" font="default" size="100%">Fujimoto, Stanley</style></author><author><style face="normal" font="default" size="100%">Dilman, Adler R.</style></author><author><style face="normal" font="default" size="100%">Byron Adams</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Genome analysis of &lt;I&gt;Plectus murrayi&lt;/I&gt;, a nematode from continental Antarctica</style></title><secondary-title><style face="normal" font="default" size="100%">G3 Genes|Genomes|Genetics</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">gene loss</style></keyword><keyword><style  face="normal" font="default" size="100%">genome architecture</style></keyword><keyword><style  face="normal" font="default" size="100%">genome assembly</style></keyword><keyword><style  face="normal" font="default" size="100%">genome decay</style></keyword><keyword><style  face="normal" font="default" size="100%">Plectus murrayi</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2021</style></year><pub-dates><date><style  face="normal" font="default" size="100%">01/2021</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://academic.oup.com/g3journal/advance-article/doi/10.1093/g3journal/jkaa045/6044189</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;&lt;em&gt;Plectus murrayi&lt;/em&gt; is one of the most common and locally abundant invertebrates of continental Antarctic ecosystems. Because it is readily cultured on artificial medium in the laboratory and highly tolerant to an extremely harsh environment, &lt;em&gt;Plectus murrayi&lt;/em&gt; is emerging as a model organism for understanding the evolutionary origin and maintenance of adaptive responses to multiple environmental stressors, including freezing and desiccation. The de novo assembled genome of &lt;em&gt;Plectus murrayi&lt;/em&gt; contains 225.741 million base pairs and a total of 14,689 predicted genes. Compared to &lt;em&gt;Caenorhabditis elegans&lt;/em&gt;, the architectural components of &lt;em&gt;Plectus murrayi&lt;/em&gt; are characterized by a lower number of protein-coding genes, fewer transposable elements, but more exons, than closely related taxa from less harsh environments. We compared the transcriptomes of lab-reared &lt;em&gt;Plectus murrayi&lt;/em&gt; with wild-caught &lt;em&gt;Plectus murrayi&lt;/em&gt; and found genes involved in growth and cellular processing were up-regulated in lab-cultured &lt;em&gt;Plectus murrayi&lt;/em&gt;, while a few genes associated with cellular metabolism and freeze tolerance were expressed at relatively lower levels. Preliminary comparative genomic and transcriptomic analyses suggest that the observed constraints on &lt;em&gt;P. murrayi&lt;/em&gt; genome architecture and functional gene expression, including genome decay and intron retention, may be an adaptive response to persisting in a biotically simplified, yet consistently physically harsh environment.&lt;/p&gt;</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Melisa A. Diaz</style></author><author><style face="normal" font="default" size="100%">Christopher B. Gardner</style></author><author><style face="normal" font="default" size="100%">Welch, Susan A.</style></author><author><style face="normal" font="default" size="100%">W. Andrew Jackson</style></author><author><style face="normal" font="default" size="100%">Adams, Byron J.</style></author><author><style face="normal" font="default" size="100%">Diana H. Wall</style></author><author><style face="normal" font="default" size="100%">Hogg, Ian D.</style></author><author><style face="normal" font="default" size="100%">Noah Fierer</style></author><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geochemical zones and environmental gradients for soils from the central Transantarctic Mountains, Antarctica</style></title><secondary-title><style face="normal" font="default" size="100%">Biogeosciences</style></secondary-title><short-title><style face="normal" font="default" size="100%">Biogeosciences</style></short-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year><pub-dates><date><style  face="normal" font="default" size="100%">03/2021</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://bg.copernicus.org/articles/18/1629/2021/</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">18</style></volume><pages><style face="normal" font="default" size="100%">1629 - 1644</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;Previous studies have established links between biodiversity and soil geochemistry in the McMurdo Dry Valleys, Antarctica, where environmental gradients are important determinants of soil biodiversity. However, these gradients are not well established in the central Transantarctic Mountains, which are thought to represent some of the least hospitable Antarctic soils. We analyzed 220 samples from 11 ice-free areas along the Shackleton Glacier (~85&amp;deg;S), a major outlet glacier of the East Antarctic Ice Sheet. We established three zones of distinct geochemical gradients near the head of the glacier (upper), its central part (middle), and at the mouth (lower). The upper zone had the highest water-soluble salt concentrations with total salt concentrations exceeding 80 000 &amp;micro;g g&lt;sup&gt;-1&lt;/sup&gt;, while the lower zone had the lowest water-soluble N:P ratios, suggesting that, in addition to other parameters (such as proximity to water and/or ice), the lower zone likely represents the most favorable ecological habitats. Given the strong dependence of geochemistry on geographic parameters, we developed multiple linear regression and random forest models to predict soil geochemical trends given latitude, longitude, elevation, distance from the coast, distance from the glacier, and soil moisture (variables which can be inferred from remote measurements). Confidence in our random forest model predictions was moderately high with &lt;i&gt;R&lt;/i&gt;&lt;sup&gt;2&lt;/sup&gt; values for total water-soluble salts, water-soluble N:P, ClO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;-&lt;/sup&gt;, and ClO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;-&lt;/sup&gt; of 0.81, 0.88, 0.78, and 0.74, respectively. These modeling results can be used to predict geochemical gradients and estimate salt concentrations for other Transantarctic Mountain soils, information that can ultimately be used to better predict distributions of soil biota in this remote region.&lt;/p&gt;</style></abstract><issue><style face="normal" font="default" size="100%">5</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Harmon, Russell S.</style></author><author><style face="normal" font="default" size="100%">Leslie, Deborah L.</style></author><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author><author><style face="normal" font="default" size="100%">Kathleen A. Welch</style></author><author><style face="normal" font="default" size="100%">Diane M. McKnight</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geochemistry of contrasting stream types, Taylor Valley, Antarctica</style></title><secondary-title><style face="normal" font="default" size="100%">GSA Bulletin</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2021</style></year><pub-dates><date><style  face="normal" font="default" size="100%">01/2021</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://pubs.geoscienceworld.org/gsa/gsabulletin/article/133/1-2/425/587799/Geochemistry-of-contrasting-stream-types-Taylor</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">133</style></volume><pages><style face="normal" font="default" size="100%">425-448</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;The McMurdo Dry Valley region is the largest ice-free area of Antarctica. Ephemeral streams flow here during the austral summer, transporting glacial meltwater to perennially ice-covered, closed basin lakes. The chemistry of 24 Taylor Valley streams was examined over the two-decade period of monitoring from 1993 to 2014, and the geochemical behavior of two streams of contrasting physical and biological character was monitored across the seven weeks of the 2010&amp;ndash;2011 flow season. Four species dominate stream solute budgets: HCO&lt;sub&gt;3&lt;/sub&gt;&lt;sup&gt;&amp;ndash;&lt;/sup&gt;, Ca&lt;sub&gt;2&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;, Na&lt;sup&gt;+&lt;/sup&gt;, and Cl&lt;sup&gt;&amp;ndash;&lt;/sup&gt;, with SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2&amp;ndash;&lt;/sup&gt;, Mg&lt;sup&gt;2+&lt;/sup&gt;, and K&lt;sup&gt;+&lt;/sup&gt; present in significantly lesser proportions. All streams contain dissolved silica at low concentrations. Across Taylor Valley, streams are characterized by their consistent anionic geochemical fingerprint of HCO&lt;sub&gt;3&lt;/sub&gt; &amp;gt; Cl &amp;gt; SO&lt;sub&gt;4&lt;/sub&gt;, but there is a split in cation composition between 14 streams with Ca &amp;gt; Na &amp;gt; Mg &amp;gt; K and 10 streams with Na &amp;gt; Ca &amp;gt; Mg &amp;gt; K.&lt;/p&gt;&lt;p&gt;&lt;br /&gt;Andersen Creek is a first-order proglacial stream representative of the 13 short streams that flow &amp;lt;1.5 km from source to gage. Von Guerard is representative of 11 long streams 2&amp;ndash;7 km in length characterized by extensive hyporheic zones. Both streams exhibit a strong daily cycle for solute load, temperature, dissolved oxygen, and pH, which vary in proportion to discharge. A well-expressed diurnal co-variation of pH with dissolved oxygen is observed for both streams that reflects different types of biological control. The relative consistency of Von Guerard composition over the summer flow season reflects chemostatic regulation, where water in transient storage introduced during times of high streamflow has an extended opportunity for water-sediment interaction, silicate mineral dissolution, and pore-water exchange.&lt;/p&gt;</style></abstract><issue><style face="normal" font="default" size="100%">1/2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Gemma E. Collins</style></author><author><style face="normal" font="default" size="100%">Hogg, Ian D.</style></author><author><style face="normal" font="default" size="100%">Convey, Peter</style></author><author><style face="normal" font="default" size="100%">Sancho, Leopoldo G.</style></author><author><style face="normal" font="default" size="100%">Cowan, Don A.</style></author><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author><author><style face="normal" font="default" size="100%">Byron Adams</style></author><author><style face="normal" font="default" size="100%">Diana H. Wall</style></author><author><style face="normal" font="default" size="100%">Allan Green, T. G.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Genetic diversity of soil invertebrates corroborates timing estimates for past collapses of the West Antarctic Ice Sheet</style></title><secondary-title><style face="normal" font="default" size="100%">Proceedings of the National Academy of Sciences</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">climate change</style></keyword><keyword><style  face="normal" font="default" size="100%">microarthropods</style></keyword><keyword><style  face="normal" font="default" size="100%">molecular clock</style></keyword><keyword><style  face="normal" font="default" size="100%">phylogeography</style></keyword><keyword><style  face="normal" font="default" size="100%">terrestrial biodiversity</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2020</style></year><pub-dates><date><style  face="normal" font="default" size="100%">08/2020</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.pnas.org/content/early/2020/08/19/2007925117</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;During austral summer field seasons between 1999 and 2018, we sampled at 91 locations throughout southern Victoria Land and along the Transantarctic Mountains for six species of endemic microarthropods (Collembola), covering a latitudinal range from 76.0&amp;deg;S to 87.3&amp;deg;S. We assembled individual mitochondrial cyto-chrome &lt;em&gt;c&lt;/em&gt; oxidase subunit 1 (COI) sequences (&lt;em&gt;n&lt;/em&gt; = 866) and found high levels of sequence divergence at both small (&amp;lt;10 km) and large (&amp;gt;600 km) spatial scales for four of the six Collembola species. We applied molecular clock estimates and assessed genetic divergences relative to the timing of past glacial cycles, including collapses of the West Antarctic Ice Sheet (WAIS). We found that genetically distinct lineages within three species have likely been isolated for at least 5.54 My to 3.52 My, while the other three species diverged more recently (&amp;lt;2 My). We suggest that Collembola had greater dispersal opportunities under past warmer climates, via flotation along coastal margins. Similarly increased opportunities for dispersal may occur under contemporary climate warming scenarios, which could influence the genetic structure of extant populations. As Collembola are a living record of past landscape evolution within Antarctica, these findings provide biological evidence to support geological and glaciological estimates of historical WAIS dynamics over the last ca. 5 My.&lt;/p&gt;</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Melisa A. Diaz</style></author><author><style face="normal" font="default" size="100%">Welch, Susan A.</style></author><author><style face="normal" font="default" size="100%">Sheets, J. M.</style></author><author><style face="normal" font="default" size="100%">Kathleen A. Welch</style></author><author><style face="normal" font="default" size="100%">Khan, Alia L.</style></author><author><style face="normal" font="default" size="100%">Byron Adams</style></author><author><style face="normal" font="default" size="100%">Diane M. McKnight</style></author><author><style face="normal" font="default" size="100%">Craig S Cary</style></author><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geochemistry of aeolian material from the McMurdo Dry Valleys, Antarctica: Insights into Southern Hemisphere dust sources</style></title><secondary-title><style face="normal" font="default" size="100%">Earth and Planetary Science Letters</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">aeolian material</style></keyword><keyword><style  face="normal" font="default" size="100%">Antarctica</style></keyword><keyword><style  face="normal" font="default" size="100%">major oxides</style></keyword><keyword><style  face="normal" font="default" size="100%">mineralogy</style></keyword><keyword><style  face="normal" font="default" size="100%">rare earth elements</style></keyword><keyword><style  face="normal" font="default" size="100%">trace elements</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2020</style></year><pub-dates><date><style  face="normal" font="default" size="100%">10/2020</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.sciencedirect.com/science/article/pii/S0012821X20304040</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">547</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;In the Southern Hemisphere, the major sources of dust and other aeolian materials are from Patagonia, South Africa, Australia, and New Zealand. Dust from Patagonia and New Zealand has been identified in ice cores throughout Antarctica, suggesting that during arid and windy periods, such as glacial periods, dust can be entrained and transported onto the continent. However, little information exists on modern Antarctic dust sources, transport, and its role in the Southern Hemisphere dust cycle. We present the first geochemical characterization of aeolian materials collected at five heights (between 5 cm and 100 cm) above the surface in four valleys within the McMurdo Dry Valleys, the largest ice-free area in Antarctica. Our mineralogy data indicate that these materials are primarily derived from local rocks of the McMurdo Volcanics, Ferrar Dolerite, Beacon Sandstone and Granite Harbor Intrusives, with varying contributions of each rock type dependent on the valley location. While major oxide, trace element and rare earth element data show that low elevation and coastal locations (with respect to the Ross Sea) are dominated by local sources, high elevation and inland locations have accumulated both local materials and dust from other distant Southern Hemisphere sources. This far-traveled material may not be accumulating today, but represents a paleo source that is resuspended from the soils. By geochemically &amp;ldquo;fingerprinting&amp;rdquo; aeolian materials from the MDV, we can better inform future studies on the transport of materials within Antarctica and between Southern Hemisphere land masses.&lt;/p&gt;</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Acosta, Dimitri R.</style></author><author><style face="normal" font="default" size="100%">Peter T. Doran</style></author><author><style face="normal" font="default" size="100%">Myers, Madeline</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">GIS tool to predict photosynthetically active radiation in a Dry Valley</style></title><secondary-title><style face="normal" font="default" size="100%">Antarctic Science</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">ArcMap</style></keyword><keyword><style  face="normal" font="default" size="100%">automated weather station</style></keyword><keyword><style  face="normal" font="default" size="100%">digital elevation model</style></keyword><keyword><style  face="normal" font="default" size="100%">ice-covered lakes</style></keyword><keyword><style  face="normal" font="default" size="100%">McMurdo Dry Valleys</style></keyword><keyword><style  face="normal" font="default" size="100%">R model</style></keyword><keyword><style  face="normal" font="default" size="100%">Taylor Valley</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2020</style></year><pub-dates><date><style  face="normal" font="default" size="100%">04/2020</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.cambridge.org/core/journals/antarctic-science/article/gis-tool-to-predict-photosynthetically-active-radiation-in-a-dry-valley/BD0BE4FF6A8F3DAAF32D698797287078</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;Understanding primary productivity is a core research area of the National Science Foundation&amp;#39;s Long-Term Ecological Research Network. This study presents the development of the GIS-based Topographic Solar Photosynthetically Active Radiation (T-sPAR) toolbox for Taylor Valley. It maps surface photosynthetically active radiation using four meteorological stations with ~20 years of data. T-sPAR estimates were validated with ground-truth data collected at Taylor Valley&amp;#39;s major lakes during the 2014&amp;ndash;15 and 2015&amp;ndash;16 field seasons. The average daily error ranges from 0.13 mol photons m&lt;sup&gt;-2&lt;/sup&gt; day&lt;sup&gt;-1&lt;/sup&gt; (0.6%) at Lake Fryxell to 3.8 mol photons m&lt;sup&gt;-2&lt;/sup&gt; day&lt;sup&gt;-1&lt;/sup&gt; (5.8%) at Lake Hoare. We attribute error to variability in terrain and sun position. Finally, a user interface was developed in order to estimate total daily surface photosynthetically active radiation for any location and date within the basin. T-sPAR improves upon existing toolboxes and models by allowing for the inclusion of a statistical treatment of light attenuation due to cloud cover. The T-sPAR toolbox could be used to inform biological sampling sites based on radiation distribution, which could collectively improve estimates of net primary productivity, in some cases by up to 25%.&lt;/p&gt;</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Cross, Julian M.</style></author><author><style face="normal" font="default" size="100%">Andrew G Fountain</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Glacial meltwater modeling to simulate lake water budget (1996-2013) in Taylor Valley, Antarctica</style></title><secondary-title><style face="normal" font="default" size="100%">Department of Geography</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2020</style></year><pub-dates><date><style  face="normal" font="default" size="100%">01/2020</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://archives.pdx.edu/ds/psu/30806</style></url></web-urls></urls><publisher><style face="normal" font="default" size="100%">Portland State University</style></publisher><pub-location><style face="normal" font="default" size="100%">Portland, OR</style></pub-location><volume><style face="normal" font="default" size="100%">M.S.</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;The McMurdo Dry Valleys (MDV), the largest ice-free region (4,500 km2) in Antarctica, are a polar desert with an average annual temperature of -18 ̊C. In Taylor Valley, one of the MDV, closed-basin, perennially ice-covered lakes occupy the valley floor. Their water balance is controlled by inflow from glacial meltwater runoff and loss due to sublimation, making them sensitive indicators of climate. In this study, a physically-based model of glacier meltwater and lake ice sublimation is adapted to explain modern (1996 to 2013) lake-level variations. Meltwater model results were improved by the inclusion of MODIS remotely-sensed albedo measurements (E = 0.47; nRMSE = 0.73). After 2008 the meltwater model significantly under-predicted streamflow and only through decreasing albedo by -30% (equivalent to a decrease of -0.18 on average) did the results match observations (E = 0.79; nRMSE = 0.45). This study provides the first estimate of direct (unmeasured) glacier inflow to the lakes, 69%, 73% and 28%, and sublimation loss rates, 0.37 m yr&lt;sup&gt;-1&lt;/sup&gt;, 0.24 m yr&lt;sup&gt;-1&lt;/sup&gt; and 0.16 m yr&lt;sup&gt;-1&lt;/sup&gt;, for Lakes Bonney, Hoare and Fryxell, respectively. Despite similar meltwater volumes entering Lakes Bonney and Fryxell, the difference in basin hypsometry results in a much faster lake rise at Bonney from 2002-13. If future climate conditions match current (1996-2013) conditions, all lakes will rise through the end of the century.&lt;/p&gt;</style></abstract><work-type><style face="normal" font="default" size="100%">masters</style></work-type></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">van den Hoogen, Johan</style></author><author><style face="normal" font="default" size="100%">Geisen, Stefan</style></author><author><style face="normal" font="default" size="100%">Diana H. Wall</style></author><author><style face="normal" font="default" size="100%">Wardle, D</style></author><author><style face="normal" font="default" size="100%">Traunspurger, Walter</style></author><author><style face="normal" font="default" size="100%">de Goede, Ron G. M.</style></author><author><style face="normal" font="default" size="100%">Byron Adams</style></author><author><style face="normal" font="default" size="100%">Ahmad, Wasim</style></author><author><style face="normal" font="default" size="100%">Ferris, Howard</style></author><author><style face="normal" font="default" size="100%">Richard D. Bardgett</style></author><author><style face="normal" font="default" size="100%">Bonkowski, Michael</style></author><author><style face="normal" font="default" size="100%">Campos-Herrera, Raquel</style></author><author><style face="normal" font="default" size="100%">Cares, Juvenil E.</style></author><author><style face="normal" font="default" size="100%">Caruso, Tancredi</style></author><author><style face="normal" font="default" size="100%">de Brito Caixeta, Larissa</style></author><author><style face="normal" font="default" size="100%">Chen, Xiaoyun</style></author><author><style face="normal" font="default" size="100%">Costa, Sofia R.</style></author><author><style face="normal" font="default" size="100%">Creamer, Rachel</style></author><author><style face="normal" font="default" size="100%">da Cunha e Castro, José</style></author><author><style face="normal" font="default" size="100%">Dam, Marie</style></author><author><style face="normal" font="default" size="100%">Djigal, Djibril</style></author><author><style face="normal" font="default" size="100%">Escuer, Miguel</style></author><author><style face="normal" font="default" size="100%">Griffiths, Bryan S.</style></author><author><style face="normal" font="default" size="100%">Gutiérrez, Carmen</style></author><author><style face="normal" font="default" size="100%">Hohberg, Karin</style></author><author><style face="normal" font="default" size="100%">Kalinkina, Daria</style></author><author><style face="normal" font="default" size="100%">Kardol, Paul</style></author><author><style face="normal" font="default" size="100%">Kergunteuil, Alan</style></author><author><style face="normal" font="default" size="100%">Korthals, Gerard</style></author><author><style face="normal" font="default" size="100%">Krashevska, Valentyna</style></author><author><style face="normal" font="default" size="100%">Kudrin, Alexey A.</style></author><author><style face="normal" font="default" size="100%">Li, Qi</style></author><author><style face="normal" font="default" size="100%">Liang, Wenju</style></author><author><style face="normal" font="default" size="100%">Magilton, Matthew</style></author><author><style face="normal" font="default" size="100%">Marais, Mariette</style></author><author><style face="normal" font="default" size="100%">Martín, José Antonio Rodríguez</style></author><author><style face="normal" font="default" size="100%">Matveeva, Elizaveta</style></author><author><style face="normal" font="default" size="100%">Mayad, El Hassan</style></author><author><style face="normal" font="default" size="100%">Mzough, E.</style></author><author><style face="normal" font="default" size="100%">Mulder, Christian</style></author><author><style face="normal" font="default" size="100%">Mullin, Peter</style></author><author><style face="normal" font="default" size="100%">Neilson, Roy</style></author><author><style face="normal" font="default" size="100%">Nguyen, T. A. Duong</style></author><author><style face="normal" font="default" size="100%">Uffe N. Nielsen</style></author><author><style face="normal" font="default" size="100%">Okada, Hiroaki</style></author><author><style face="normal" font="default" size="100%">Rius, Juan Emilio Palomares</style></author><author><style face="normal" font="default" size="100%">Pan, Kaiwen</style></author><author><style face="normal" font="default" size="100%">Peneva, Vlada</style></author><author><style face="normal" font="default" size="100%">Pellissier, Loïc</style></author><author><style face="normal" font="default" size="100%">Carlos Pereira da Silva, Julio</style></author><author><style face="normal" font="default" size="100%">Pitteloud, Camille</style></author><author><style face="normal" font="default" size="100%">Powers, Thomas O.</style></author><author><style face="normal" font="default" size="100%">Powers, Kirsten</style></author><author><style face="normal" font="default" size="100%">Quist, Casper W.</style></author><author><style face="normal" font="default" size="100%">Rasmann, Sergio</style></author><author><style face="normal" font="default" size="100%">Moreno, Sara Sánchez</style></author><author><style face="normal" font="default" size="100%">Scheu, Stefan</style></author><author><style face="normal" font="default" size="100%">Setälä, Heikki</style></author><author><style face="normal" font="default" size="100%">Sushchuk, Anna</style></author><author><style face="normal" font="default" size="100%">Tiunov, Alexei V.</style></author><author><style face="normal" font="default" size="100%">Trap, Jean</style></author><author><style face="normal" font="default" size="100%">Vestergård, Mette</style></author><author><style face="normal" font="default" size="100%">Villenave, Cecile</style></author><author><style face="normal" font="default" size="100%">Waeyenberge, Lieven</style></author><author><style face="normal" font="default" size="100%">Wilschut, Rutger</style></author><author><style face="normal" font="default" size="100%">Wright, Daniel G.</style></author><author><style face="normal" font="default" size="100%">Keith, Aidan M.</style></author><author><style face="normal" font="default" size="100%">Yang, Jiue-in</style></author><author><style face="normal" font="default" size="100%">Schmidt, Olaf</style></author><author><style face="normal" font="default" size="100%">Bouharroud, R.</style></author><author><style face="normal" font="default" size="100%">Ferji, Z.</style></author><author><style face="normal" font="default" size="100%">van der Putten, Wim H.</style></author><author><style face="normal" font="default" size="100%">Routh, Devin</style></author><author><style face="normal" font="default" size="100%">Crowther, Thomas Ward</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">A global database of soil nematode abundance and functional group composition</style></title><secondary-title><style face="normal" font="default" size="100%">Scientific Data</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2020</style></year><pub-dates><date><style  face="normal" font="default" size="100%">03/2020</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.nature.com/articles/s41597-020-0437-3</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">7</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;As the most abundant animals on earth, nematodes are a dominant component of the soil community. they play critical roles in regulating biogeochemical cycles and vegetation dynamics within and across landscapes and are an indicator of soil biological activity. Here,&amp;nbsp;we present a comprehensive global dataset of soil nematode abundance and functional group composition. This dataset includes 6,825 georeferenced soil samples from all continents and biomes. For geospatial mapping purposes these samples are aggregated into 1,933 unique 1-km pixels, each of which is linked to 73 global environmental covariate data layers. Altogether,&amp;nbsp;this dataset can help to gain insight into the spatial distribution patterns of soil nematode abundance and community composition, and the environmental drivers shaping these patterns.&lt;/p&gt;</style></abstract><issue><style face="normal" font="default" size="100%">1</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Raymond, James A.</style></author><author><style face="normal" font="default" size="100%">Rachael M. Morgan-Kiss</style></author><author><style face="normal" font="default" size="100%">Stahl-Rommel, Sarah</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Glycerol is an osmoprotectant in two Antarctic &lt;I&gt;Chlamydomonas&lt;/I&gt; species from an ice-covered saline lake and is synthesized by an unusual bidomain enzyme</style></title><secondary-title><style face="normal" font="default" size="100%">Frontiers in Plant Science</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Antarctica</style></keyword><keyword><style  face="normal" font="default" size="100%">Chlamydomonas</style></keyword><keyword><style  face="normal" font="default" size="100%">glycerol synthesis</style></keyword><keyword><style  face="normal" font="default" size="100%">glycerol-3-phosphate dehydrogenase</style></keyword><keyword><style  face="normal" font="default" size="100%">Lake Bonney</style></keyword><keyword><style  face="normal" font="default" size="100%">phosphoserine phosphatase</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2020</style></year><pub-dates><date><style  face="normal" font="default" size="100%">08/2020</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.frontiersin.org/articles/10.3389/fpls.2020.01259/full</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">11</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;Glycerol, a compatible solute, has previously been found to act as an osmoprotectant in some marine &lt;em&gt;Chlamydomonas&lt;/em&gt; species and several species of &lt;em&gt;Dunaliella&lt;/em&gt; from hypersaline ponds. Recently, &lt;em&gt;Chlamydomonas reinhardtii&lt;/em&gt; and &lt;em&gt;Dunaliella salina&lt;/em&gt; were shown to make glycerol with an unusual bidomain enzyme, which appears to be unique to algae, that contains a phosphoserine phosphatase and glycerol-3-phosphate dehydrogenase. Here we report that two psychrophilic species of &lt;em&gt;Chlamydomonas&lt;/em&gt; (&lt;em&gt;C.&lt;/em&gt; spp. UWO241 and ICE-MDV) from Lake Bonney, Antarctica also produce high levels of glycerol to survive in the lake&amp;rsquo;s saline waters. Glycerol concentration increased linearly with salinity and at 1.3 M NaCl, exceeded 400 mM in &lt;em&gt;C.&lt;/em&gt; sp. UWO241, the more salt-tolerant strain. We also show that both species expressed several isoforms of the bidomain enzyme. An analysis of one of the isoforms of &lt;em&gt;C.&lt;/em&gt; sp. UWO241 showed that it was strongly upregulated by NaCl and is thus the likely source of glycerol. These results reveal another adaptation of the Lake Bonney &lt;em&gt;Chlamydomonas&lt;/em&gt; species that allow them to survive in an extreme polar environment.&lt;/p&gt;</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author><author><style face="normal" font="default" size="100%">Jill A. Mikucki</style></author><author><style face="normal" font="default" size="100%">German, Laura A.</style></author><author><style face="normal" font="default" size="100%">Kathleen A. Welch</style></author><author><style face="normal" font="default" size="100%">Sue Welch</style></author><author><style face="normal" font="default" size="100%">Christopher B. Gardner</style></author><author><style face="normal" font="default" size="100%">Tulaczyk, Slawek M.</style></author><author><style face="normal" font="default" size="100%">Pettit, Erin C.</style></author><author><style face="normal" font="default" size="100%">Kowalski, Julia</style></author><author><style face="normal" font="default" size="100%">Dachwald, Bernd</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The Geochemistry of Englacial Brine From Taylor Glacier, Antarctica</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Geophysical Research: Biogeosciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">03/2019</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2018JG004411</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">124</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;Blood Falls is a hypersaline, iron‐rich discharge at the terminus of the Taylor Glacier in the McMurdo Dry Valleys, Antarctica. In November 2014, brine in a conduit within the glacier was penetrated and sampled using clean‐entry techniques and a thermoelectric melting probe called the IceMole. We analyzed the englacial brine sample for filterable iron (fFe), total Fe, major cations and anions, nutrients, organic carbon, and perchlorate. In addition, aliquots were analyzed for minor and trace elements and isotopes including δD and δ&lt;sup&gt;18&lt;/sup&gt;O of water, δ&lt;sup&gt;34&lt;/sup&gt;S and δ&lt;sup&gt;18&lt;/sup&gt;O of sulfate, &lt;sup&gt;234&lt;/sup&gt;U, &lt;sup&gt;238&lt;/sup&gt;U, δ&lt;sup&gt;11&lt;/sup&gt;B, &lt;sup&gt;87&lt;/sup&gt;Sr/&lt;sup&gt;86&lt;/sup&gt;Sr, and δ&lt;sup&gt;81&lt;/sup&gt;Br. These measurements were made in order to (1) determine the source and geochemical evolution of the brine and (2) compare the chemistry of the brine to that of nearby hypersaline lake waters and previous supraglacially sampled collections of Blood Falls outflow that were interpreted as end‐member brines. The englacial brine had higher Cl&amp;minus; concentrations than the Blood Falls end‐member outflow; however, other constituents were similar. The isotope data indicate that the water in the brine is derived from glacier melt. The H&lt;sub&gt;4&lt;/sub&gt;SiO&lt;sub&gt;4&lt;/sub&gt; concentrations and U and Sr isotope suggest a high degree of chemical weathering products. The brine has a low N:P ratio of ~7.2 with most of the dissolved inorganic nitrogen in the form of NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt;. Dissolved organic carbon concentrations are similar to end‐member outflow values. Our results provide strong evidence that the original source of solutes in the brine was ancient seawater, which has been modified with the addition of chemical weathering products.&lt;/p&gt;</style></abstract><issue><style face="normal" font="default" size="100%">3</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Carolyn Dowling</style></author><author><style face="normal" font="default" size="100%">Sue Welch</style></author><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The geochemistry of glacial deposits in Taylor Valley, Antarctica: Comparison to upper continental crustal abundances</style></title><secondary-title><style face="normal" font="default" size="100%">Applied Geochemistry</style></secondary-title><short-title><style face="normal" font="default" size="100%">Applied Geochemistry</style></short-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Antarctica</style></keyword><keyword><style  face="normal" font="default" size="100%">geochemistry</style></keyword><keyword><style  face="normal" font="default" size="100%">glacial deposits</style></keyword><keyword><style  face="normal" font="default" size="100%">polar dry-based glaciers</style></keyword><keyword><style  face="normal" font="default" size="100%">Taylor Valley</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2019</style></year><pub-dates><date><style  face="normal" font="default" size="100%">05/2019</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.sciencedirect.com/science/article/pii/S0883292719301246</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;Wet-based glacial deposits have been used traditionally as an analog for upper continental crust (UCC) abundances. To provide more information on the validity of using glacial deposits from wet-based glaciers, samples deposited by the dry-based polar glaciers located in Taylor Valley, Antarctica, were collected. Stream channel sediments, comprised of igneous, metamorphic, and sedimentary rocks initially deposited as glacial tills by polar glaciers, were analyzed by XRF, ICP-MS, and SEM. Based on the Chemical Index of Alteration values and A&amp;ndash;CN&amp;ndash;K ternary diagram, there are low levels of chemical weathering in these tills. Additionally, major and trace element geochemical data are compared to the average UCC values. The observed discrepancies between the mean UCC and Antarctic samples develop from the existence of mafic components, most likely the McMurdo Volcanic Group and Ferrar Dolerite, being present in the Taylor Valley tills. Even though the mafic material typically comprises 3&amp;ndash;7% of the till, the volcanic rocks have a significant influence on the tills&amp;rsquo; bulk geochemistry. The existence of this mafic fraction in the dry-based glacial tills results from the reduced rate of weathering, as compared to wet-based glaciers. Geochemical analyses of the dry-based glacial tills in polar deserts, such as those found in Taylor Valley, may provide a better representative composition of the original material than wet-based glaciers and need to be incorporated into upper continental crust calculations.&lt;/p&gt;</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Xue, Xia</style></author><author><style face="normal" font="default" size="100%">Byron Adams</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Genomics and transcriptomics of Antarctic nematodes reveal drivers of life history evolution and genome evolution</style></title><secondary-title><style face="normal" font="default" size="100%">Department of Biology</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Antarctic nematodes</style></keyword><keyword><style  face="normal" font="default" size="100%">Caenorhabditis elegans</style></keyword><keyword><style  face="normal" font="default" size="100%">genome evolution</style></keyword><keyword><style  face="normal" font="default" size="100%">growth rate hypothesis</style></keyword><keyword><style  face="normal" font="default" size="100%">Plectus murrayi</style></keyword><keyword><style  face="normal" font="default" size="100%">Scottnema lindsayae</style></keyword><keyword><style  face="normal" font="default" size="100%">transcriptome</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2018</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://search.proquest.com/docview/2081899003</style></url></web-urls></urls><publisher><style face="normal" font="default" size="100%">Brigham Young University</style></publisher><pub-location><style face="normal" font="default" size="100%">Provo, UT</style></pub-location><volume><style face="normal" font="default" size="100%">Ph.D.</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;Elemental stoichiometry defines a critical understanding of the relationship between&amp;nbsp;nutrient availability and usage throughout different levels of the biological community. We&amp;nbsp;found there is a link between available phosphorus (P), cellular phosphorus, and nematode development as postulated by the growth rate hypothesis (GRH). I predicted that in a P-poor environment, cellular RNA concentrations would be lower than they are in P-rich environment, and thus the 18srRNA expression level will have reduced. To most efficiently regulate the&amp;nbsp;uptake of limited P, I predicted that nematodes in P-poor environments would decrease the number of copies of the 18s rRNA gene in their genome. I measured life history traits as well as rRNA gene expression and gene copy number. We found that elemental stoichiometry predicts evolutionary changes consistent with the Growth Rate Hypothesis. We sequenced and assembled a draft genome of &lt;em&gt;P. murrayi&lt;/em&gt;. Although we expected to find genes responsible for stress tolerance, we hypothesized that in response to strong selection pressure associated with living in&amp;nbsp;a simplified ecosystem, over time the genome of &lt;em&gt;P. murrayi&lt;/em&gt; should have undergone significant decay (gene loss) relative to species in ecosystems structured more strongly by biotic interactions. We found significantly fewer genes in &lt;em&gt;P. murrayi&lt;/em&gt;. To compare patterns of gene expression between two highly divergent Antarctic nematode species, we sequenced and assembled the transcriptomes of &lt;em&gt;S. lindsayae&lt;/em&gt; and &lt;em&gt;P. murrayi&lt;/em&gt;. Under laboratory conditions at 4&amp;nbsp; ̊C, &lt;em&gt;S. lindsayae&lt;/em&gt; had significantly lower rates of gene expression but expressed a significantly larger number of genes. We speculate that the differences in gene expression are correlated with life history traits (developmental rates) while the differences in the number of genes expressed can be explained&amp;nbsp;by their different genetic systems (&lt;em&gt;S. lindsayae&lt;/em&gt; is amphimictic, &lt;em&gt;P. murrayi&lt;/em&gt; is parthenogenic) and the soil environments to which they are adapted. Since we previously showed that differences in available P content can influence the evolution of gene expression via gene copy number, and that this ultimately influences growth rate, we wondered how much of this response is driven by genetics versus how strongly these patterns are driven by temperature. To better understand this, we maintained wild type populations of P. murrayi in P-rich and P-poor conditions at 5&amp;nbsp; ̊C, 10&amp;nbsp; ̊C and 15 ̊C in the laboratory for over 40 generations and sequenced the transcriptomes prepared from each treatment group. We found that nutrient levels played an important role in gene expression when the temperature is optimal for P. murrayi culturing and that temperature is more important in gene expression when the available P is limited. This work underscores the utility of using principles of elemental stoichiometry coupled with genomic and transcriptomics research tools to make and test predictions about life history evolution. The results of my work also&amp;nbsp;inform inferences about the ways in which nutrient availability also drives the organization of trophic interactions and ultimately ecosystems.&lt;/p&gt;</style></abstract><work-type><style face="normal" font="default" size="100%">doctoral</style></work-type></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Myers, Krista F.</style></author><author><style face="normal" font="default" size="100%">Peter T. Doran</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Groundwater and thermal legacy of a large paleolake in Taylor Valley, East Antarctica as evidenced by airborne electromagnetic and sedimentological techniques</style></title><secondary-title><style face="normal" font="default" size="100%">Department of Geology and Geophysics</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2018</style></year><pub-dates><date><style  face="normal" font="default" size="100%">07/2018</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://digitalcommons.lsu.edu/gradschool_theses/4776</style></url></web-urls></urls><publisher><style face="normal" font="default" size="100%">Louisiana State University</style></publisher><pub-location><style face="normal" font="default" size="100%">Baton Rouge, LA</style></pub-location><volume><style face="normal" font="default" size="100%">M.S.</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;During the Last Glacial Maximum, grounded ice in the Ross Sea extended into the otherwise ice-free McMurdo Dry Valleys, creating a series of large ice dammed paleolakes. Grounded ice within the mouth of Taylor Valley allowed for lake levels to reach elevations not possible at modern day and formed what is known as Glacial Lake Washburn (GLW). GLW extended from the eastern portion of Taylor Valley roughly 20 km west to a level ~300 m higher than modern day Lake Fryxell. The formation and existence of GLW has been debated, though previous studies correlate the timing of GLW with early Holocene grounded ice. Evidence of GLW has largely been constrained to the interpretation of glacial deposits and fluvial features such as lacustrine deposits, strandlines, and preserved paleodeltas. GIS and remote sensing techniques paired with regional resistivity data provide new insight into the paleohydrology of the region.&lt;/p&gt;&lt;p&gt;To quantify the extent of GLW, paleodelta locations were mapped using high resolution LiDAR digital elevation models and satellite imagery. Delta topset elevations were correlated between three streams in Fryxell basin to determine paleolake levels. Additionally, mean resistivity maps generated from airborne electromagnetic survey data (SkyTEM) reveal an extensive groundwater system within Fryxell basin which is interpreted as a legacy groundwater signal from GLW. Resistivity data suggests that active permafrost formation has been ongoing since onset of lake drainage, and that lake levels were over 60 m higher than modern only 1,000 &amp;ndash; 2,000 yr BP. This coincides with a warmer than modern paleoclimate inferred by ice core records, indicating a dynamic hydrological system that is highly sensitive to small changes in climate. As global temperatures increase, Lake Fryxell will continue to experience highly variable lake levels. Lakes and groundwater within the McMurdo Dry Valleys are critical to understanding impacts on the broader ecosystem which is largely driven by the availability of liquid water.&lt;/p&gt;</style></abstract><work-type><style face="normal" font="default" size="100%">masters</style></work-type></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Saelens, Elsa D.</style></author></authors><secondary-authors><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author></secondary-authors></contributors><titles><title><style face="normal" font="default" size="100%">The geochemistry of minor cations within Antarctic stream water: Determining the role of the hyporheic zone</style></title><secondary-title><style face="normal" font="default" size="100%">School of Earth Sciences</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2017</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://library.ohio-state.edu/record=b8218699~S7</style></url></web-urls></urls><publisher><style face="normal" font="default" size="100%">The Ohio State University</style></publisher><pub-location><style face="normal" font="default" size="100%">Columbus, OH</style></pub-location><volume><style face="normal" font="default" size="100%">B.A.</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">bachelors</style></work-type></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Clare R. Beet</style></author><author><style face="normal" font="default" size="100%">Hogg, Ian D.</style></author><author><style face="normal" font="default" size="100%">Gemma E. Collins</style></author><author><style face="normal" font="default" size="100%">Cowan, Don A.</style></author><author><style face="normal" font="default" size="100%">Diana H. Wall</style></author><author><style face="normal" font="default" size="100%">Byron Adams</style></author><author><style face="normal" font="default" size="100%">John-James Wilson</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Genetic diversity among populations of Antarctic springtails (Collembola) within the Mackay Glacier ecotone &lt;sup&gt;1&lt;/sup&gt;</style></title><secondary-title><style face="normal" font="default" size="100%">Genome</style></secondary-title><short-title><style face="normal" font="default" size="100%">Genome</style></short-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year><pub-dates><date><style  face="normal" font="default" size="100%">Jan-09-2016</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.nrcresearchpress.com/doi/10.1139/gen-2015-0194</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">59</style></volume><pages><style face="normal" font="default" size="100%">762 - 770</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">9</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Andrew G Fountain</style></author><author><style face="normal" font="default" size="100%">Hassan J. Basagic</style></author><author><style face="normal" font="default" size="100%">Niebuhr, Spencer</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Glaciers in equilibrium, McMurdo Dry Valleys, Antarctica</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Glaciology</style></secondary-title><short-title><style face="normal" font="default" size="100%">J. Glaciol.</style></short-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Antarctica</style></keyword><keyword><style  face="normal" font="default" size="100%">glaciers</style></keyword><keyword><style  face="normal" font="default" size="100%">mass balance</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2016</style></year><pub-dates><date><style  face="normal" font="default" size="100%">07/2016</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143016000861</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">62</style></volume><pages><style face="normal" font="default" size="100%">976 - 989</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;The McMurdo Dry Valleys are a cold, dry polar desert and the alpine glaciers therein exhibit small annual and seasonal mass balances, often &amp;lt;&amp;plusmn;0.06 m w.e. Typically, winter is the accumulation season, but significant snow storms can occur any time of year occasionally making summer the accumulation season. The yearly equilibrium line altitude is poorly correlated with mass balance because the elevation gradient of mass balance on each glacier can change dramatically from year to year. Most likely, winds redistribute the light snowfall disrupting the normal gradient of increasing mass balance with elevation. Reconstructed cumulative mass balance shows that the glaciers have lost &amp;lt;2 m w.e. over the past half century and area changes show minimal retreat. In most cases these changes are less than the uncertainty and the glaciers are considered in equilibrium. Since 2000, however, the glaciers have lost mass despite relatively stable summer air temperatures suggesting a different mechanism in play. Whether this trend is a harbinger of future changes or a temporary excursion is unclear.&lt;/p&gt;</style></abstract><issue><style face="normal" font="default" size="100%">235</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Ian Hawes</style></author><author><style face="normal" font="default" size="100%">Jungblut, Anne D.</style></author><author><style face="normal" font="default" size="100%">Maciek K. Obryk</style></author><author><style face="normal" font="default" size="100%">Peter T. Doran</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Growth dynamics of a laminated microbial mat in response to variable irradiance in an Antarctic lake</style></title><secondary-title><style face="normal" font="default" size="100%">Freshwater Biology</style></secondary-title><short-title><style face="normal" font="default" size="100%">Freshw Biol</style></short-title></titles><dates><year><style  face="normal" font="default" size="100%">2016</style></year><pub-dates><date><style  face="normal" font="default" size="100%">02/2016</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://doi.wiley.com/10.1111/fwb.12715</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">61</style></volume><pages><style face="normal" font="default" size="100%">396 - 410</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;ol class=&quot;o-list--numbered o-list--paragraph&quot; id=&quot;fwb12715-list-0001&quot; style=&quot;margin-top: 0px; margin-bottom: 3em; margin-left: 6em; outline: 0px; font-size: 10px; list-style-position: outside; color: rgb(51, 51, 51); font-family: 'Open Sans', Arial, Helvetica, 'Lucida Sans Unicode', sans-serif; line-height: 14px; background: 0px 0px rgb(249, 249, 249);&quot;&gt;&lt;li style=&quot;margin-bottom: 0.8em; padding-left: 0.5em; outline: 0px; font-size: 1.6em; background: 0px 0px;&quot;&gt;Laminated microbial mats are important ecosystem components of perennially ice-covered Antarctic dry valley lakes. In order to understand better their response to changing environment, we made observations and carried out a manipulation experiment to determine their response to variations in irradiance in Lake Hoare (77&amp;deg;38&amp;prime; S, 162&amp;deg;53&amp;prime; E).&lt;/li&gt;&lt;li style=&quot;margin-bottom: 0.8em; padding-left: 0.5em; outline: 0px; font-size: 1.6em; background: 0px 0px;&quot;&gt;Ice transparency was the most variable parameter that affected benthic light dose, both spatially and between years. Patterns of lamina accrual corresponded to irradiance history, with laminae that were initiated in high transmission years thicker than those from low transmission years.&lt;/li&gt;&lt;li style=&quot;margin-bottom: 0.8em; padding-left: 0.5em; outline: 0px; font-size: 1.6em; background: 0px 0px;&quot;&gt;A shading experiment confirmed that accrual of lamina thickness, calcite precipitation and ash-free dry mass were determined by irradiance, but photosynthetic biomass and phototrophic species composition were less affected.&lt;/li&gt;&lt;li style=&quot;margin-bottom: 0.8em; padding-left: 0.5em; outline: 0px; font-size: 1.6em; background: 0px 0px;&quot;&gt;Buried laminae decomposed only slowly over time, with potentially viable phototrophs many laminae down into the microbial mat. Decay rate increased only slightly with shading.&lt;/li&gt;&lt;li style=&quot;margin-bottom: 0.8em; padding-left: 0.5em; outline: 0px; font-size: 1.6em; background: 0px 0px;&quot;&gt;We conclude that the microbial mats in Lake Hoare are characterised by remarkable stability, with slow accumulation rates and turnover of biomass over time. Photosynthetic biomass and species composition appeared to be stable across long time periods, with interannual variation in lamination pattern due to differential accumulation of extracellular polysaccharide and representing the visible expression of annual growth conditions.&lt;/li&gt;&lt;/ol&gt;</style></abstract><issue><style face="normal" font="default" size="100%">4</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Tyler J. Kohler</style></author><author><style face="normal" font="default" size="100%">Kopalová, Kateřina</style></author><author><style face="normal" font="default" size="100%">Bart Van de Vijver</style></author><author><style face="normal" font="default" size="100%">J. Patrick Kociolek</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The genus Luticola D.G.Mann (Bacillariophyta) from the McMurdo Sound Region, Antarctica, with the description of four new species</style></title><secondary-title><style face="normal" font="default" size="100%">Phytotaxa</style></secondary-title><short-title><style face="normal" font="default" size="100%">Phytotaxa</style></short-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year><pub-dates><date><style  face="normal" font="default" size="100%">10/2015</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://www.biotaxa.org/Phytotaxa/article/view/phytotaxa.208.2.1</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">208</style></volume><pages><style face="normal" font="default" size="100%">103</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">2</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Smith, Melinda D.</style></author><author><style face="normal" font="default" size="100%">La Pierre, Kimberly J.</style></author><author><style face="normal" font="default" size="100%">Collins, SL</style></author><author><style face="normal" font="default" size="100%">Knapp, Alan K.</style></author><author><style face="normal" font="default" size="100%">Gross, Katherine L.</style></author><author><style face="normal" font="default" size="100%">John E. Barrett</style></author><author><style face="normal" font="default" size="100%">Frey, Serita D.</style></author><author><style face="normal" font="default" size="100%">Gough, Laura</style></author><author><style face="normal" font="default" size="100%">Miller, Robert J.</style></author><author><style face="normal" font="default" size="100%">Morris, James T.</style></author><author><style face="normal" font="default" size="100%">Rustad, Lindsey E.</style></author><author><style face="normal" font="default" size="100%">Yarie, John</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Global environmental change and the nature of aboveground net primary productivity responses: insights from long-term experiments</style></title><secondary-title><style face="normal" font="default" size="100%">Oecologia</style></secondary-title><short-title><style face="normal" font="default" size="100%">Oecologia</style></short-title></titles><dates><year><style  face="normal" font="default" size="100%">2015</style></year><pub-dates><date><style  face="normal" font="default" size="100%">04/2015</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://link.springer.com/10.1007/s00442-015-3230-9http://link.springer.com/content/pdf/10.1007/s00442-015-3230-9</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">177</style></volume><pages><style face="normal" font="default" size="100%">935 - 947</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">4</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hilary A. Dugan</style></author></authors><secondary-authors><author><style face="normal" font="default" size="100%">Peter T. Doran</style></author></secondary-authors></contributors><titles><title><style face="normal" font="default" size="100%">Geophysics, Water Balance, and History of Thick Perennial Ice Covers on Antarctic Lakes</style></title><secondary-title><style face="normal" font="default" size="100%">Department of Earth and Environmental Sciences</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Antarctica</style></keyword><keyword><style  face="normal" font="default" size="100%">brine</style></keyword><keyword><style  face="normal" font="default" size="100%">lake ice</style></keyword><keyword><style  face="normal" font="default" size="100%">McMurdo Dry Valleys</style></keyword><keyword><style  face="normal" font="default" size="100%">polar lakes</style></keyword><keyword><style  face="normal" font="default" size="100%">sublimation</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2014</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://hdl.handle.net/10027/19407</style></url></web-urls></urls><publisher><style face="normal" font="default" size="100%">University of Illinois</style></publisher><pub-location><style face="normal" font="default" size="100%">Chicago, IL</style></pub-location><volume><style face="normal" font="default" size="100%">Ph.D.</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;Antarctic lakes are studied as sentinels of future change, for paleolimnological records contained in the sediments, and as habitats for the simple food webs that can exist in inhospitable environments. Understanding how lakes are formed and are sustained in response to landscape and climate conditions is critical in addressing the aforementioned research themes. This thesis is governed by the overarching hypothesis that an understanding of hydrologic and sediment transport processes associated with lake ice formation and preservation can be used to reveal past climatic changes, and further our awareness of current changes in climate and water balance in the McMurdo Dry Valleys of Antarctica. The first chapter focuses on water loss from closed basin lakes in Taylor Valley, Antarctica, and presents updated estimates of sublimation and ablation rates from long-term empirical measurements. The second and third chapters address the formation of Lake Vida, Antarctica. The former investigates the accretion of a 27 m ice cover, and considers the origin of thick sediment layers in the ice cover, and the latter uses two geophysical methods to quantify the extent and volume of the brine network in the subsurface beneath the lake. The results presented herein advance the study of hydrogeology in continuous permafrost, provide additional evidence for fluctuating climate states in the McMurdo Dry Valleys throughout the mid to late Holocene, and provide a case study for the preservation of water in a cold, desert environment analogous to neighboring planets.&lt;/p&gt;</style></abstract><work-type><style face="normal" font="default" size="100%">doctoral</style></work-type></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Uffe N. Nielsen</style></author><author><style face="normal" font="default" size="100%">Edward Ayres</style></author><author><style face="normal" font="default" size="100%">Diana H. Wall</style></author><author><style face="normal" font="default" size="100%">Li, Grace</style></author><author><style face="normal" font="default" size="100%">Richard D. Bardgett</style></author><author><style face="normal" font="default" size="100%">Wu, Tiehang</style></author><author><style face="normal" font="default" size="100%">James R. Garey</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Global-scale patterns of assemblage structure of soil nematodes in relation to climate and ecosystem properties</style></title><secondary-title><style face="normal" font="default" size="100%">Global Ecology and Biogeography</style></secondary-title><short-title><style face="normal" font="default" size="100%">Global Ecology and Biogeography</style></short-title></titles><dates><year><style  face="normal" font="default" size="100%">2014</style></year><pub-dates><date><style  face="normal" font="default" size="100%">01/2014</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://doi.wiley.com/10.1111/geb.12177</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">23</style></volume><pages><style face="normal" font="default" size="100%">968 - 978</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">9</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Joseph S. Levy</style></author><author><style face="normal" font="default" size="100%">Andrew G Fountain</style></author><author><style face="normal" font="default" size="100%">O'Connor, J. E.</style></author><author><style face="normal" font="default" size="100%">Kathleen A. Welch</style></author><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Garwood Valley, Antarctica: A new record of Last Glacial Maximum to Holocene glaciofluvial processes in the McMurdo Dry Valleys</style></title><secondary-title><style face="normal" font="default" size="100%">Geological Society of America Bulletin</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2013</style></year><pub-dates><date><style  face="normal" font="default" size="100%">09/2013</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://bulletin.geoscienceworld.org/content/early/2013/06/07/B30783.1.abstract</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">125</style></volume><pages><style face="normal" font="default" size="100%">1484 - 1502</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">9-10</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author><author><style face="normal" font="default" size="100%">Kathleen A. Welch</style></author><author><style face="normal" font="default" size="100%">Christopher B. Gardner</style></author><author><style face="normal" font="default" size="100%">Chris Jaros</style></author><author><style face="normal" font="default" size="100%">Daryl L. Moorhead</style></author><author><style face="normal" font="default" size="100%">Knoepfle, J</style></author><author><style face="normal" font="default" size="100%">Peter T. Doran</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The geochemistry of upland ponds, Taylor Valley, Antarctica</style></title><secondary-title><style face="normal" font="default" size="100%">Antarctic Science</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2012</style></year><pub-dates><date><style  face="normal" font="default" size="100%">2/2012</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://journals.cambridge.org/action/displayAbstract?fromPage=online&amp;aid=8483351</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">24</style></volume><pages><style face="normal" font="default" size="100%">3 - 14</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">01</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hogg, Ian D.</style></author><author><style face="normal" font="default" size="100%">Diana H. Wall</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Global change and Antarctic terrestrial biodiversity</style></title><secondary-title><style face="normal" font="default" size="100%">Polar Biology</style></secondary-title><short-title><style face="normal" font="default" size="100%">Polar Biol</style></short-title></titles><dates><year><style  face="normal" font="default" size="100%">2011</style></year><pub-dates><date><style  face="normal" font="default" size="100%">11/2011</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://link.springer.com/10.1007/s00300-011-1108-9</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">34</style></volume><pages><style face="normal" font="default" size="100%">1625 - 1627</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">11</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Bishwo N. Adhikari</style></author><author><style face="normal" font="default" size="100%">Byron Adams</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Genomic analysis of nematode-environment interaction</style></title><secondary-title><style face="normal" font="default" size="100%">Department of Biology</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">anhydrobiosis</style></keyword><keyword><style  face="normal" font="default" size="100%">Antarctic nematode</style></keyword><keyword><style  face="normal" font="default" size="100%">comparative transcriptomics</style></keyword><keyword><style  face="normal" font="default" size="100%">complementary DNA library</style></keyword><keyword><style  face="normal" font="default" size="100%">desiccation</style></keyword><keyword><style  face="normal" font="default" size="100%">functional analysis</style></keyword><keyword><style  face="normal" font="default" size="100%">Heterorhabditis bacteriophora</style></keyword><keyword><style  face="normal" font="default" size="100%">McMurdo Dry Valleys</style></keyword><keyword><style  face="normal" font="default" size="100%">microarray analysis</style></keyword><keyword><style  face="normal" font="default" size="100%">Plectus murrayi</style></keyword><keyword><style  face="normal" font="default" size="100%">quantative real-time polymerase chain reaction</style></keyword><keyword><style  face="normal" font="default" size="100%">Scottnema lindsayae</style></keyword><keyword><style  face="normal" font="default" size="100%">stoichiometry</style></keyword><keyword><style  face="normal" font="default" size="100%">stress survival</style></keyword><keyword><style  face="normal" font="default" size="100%">subtractive hybridization</style></keyword><keyword><style  face="normal" font="default" size="100%">trait deterioration</style></keyword><keyword><style  face="normal" font="default" size="100%">transcriptional profiling</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2010</style></year><pub-dates><date><style  face="normal" font="default" size="100%">08/2010</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">https://scholarsarchive.byu.edu/etd/2578</style></url></web-urls></urls><publisher><style face="normal" font="default" size="100%">Brigham Young University</style></publisher><pub-location><style face="normal" font="default" size="100%">Provo, UT</style></pub-location><volume><style face="normal" font="default" size="100%">Ph.D.</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;The natural environments of organisms present a multitude of biotic and abiotic challenges that require both short-term ecological and long-term evolutionary responses. Though most environmental response studies have focused on effects at the ecosystem, community and organismal levels, the ultimate controls of these responses are located in the genome of the organism. Soil nematodes are highly responsive to, and display a wide variety of responses to changing environmental conditions, making them ideal models for the study of organismal interactions with their environment. In an attempt to examine responses to environmental stress (desiccation and freezing), genomic level analyses of gene expression during anhydrobiosis of the Antarctic nematode &lt;em&gt;Plectus murrayi&lt;/em&gt; was undertaken. An EST library representative of the desiccation induced transcripts was established and the transcripts differentially expressed during desiccation stress were identified. The expressed genome of &lt;em&gt;P. murrayi&lt;/em&gt; showed that desiccation survival in nematodes involves differential expression of a suite of genes from diverse functional areas, and constitutive expression of a number of stress related genes. My study also revealed that exposure to slow desiccation and freezing plays an important role in the transcription of stress related genes, improves desiccation and freezing survival of nematodes. Deterioration of traits essential for biological control has been recognized in diverse biological control agents including insect pathogenic nematodes. I studied the genetic mechanisms behind such deterioration using expression profiling. My results showed that trait deterioration of insect pathogenic nematode induces substantial overall changes in the nematode transcriptome and exhibits a general pattern of metabolic shift causing massive changes in metabolic and other processes. Finally, through field observations and molecular laboratory experiments the validity of the growth rate hypothesis in natural populations of Antarctic nematodes was tested. My results indicated that elemental stoichiometry influences evolutionary adaptations in gene expression and genome evolution. My study, in addition to providing immediate insight into the mechanisms by which multicellular animals respond to their environment, is transformative in its potential to inform other fundamental ecological and evolutionary questions, such as the evolution of life-history patterns and the relationship between community structure and ecological function in ecosystems.&lt;/p&gt;</style></abstract><work-type><style face="normal" font="default" size="100%">doctoral</style></work-type></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>32</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Sarah Fortner</style></author></authors><tertiary-authors><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author></tertiary-authors></contributors><titles><title><style face="normal" font="default" size="100%">The geochemistry of glacier snow and melt: The Oregon Cascades and Taylor Valley, Antarctica.</style></title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><publisher><style face="normal" font="default" size="100%">The Ohio State University</style></publisher><volume><style face="normal" font="default" size="100%">Ph.D.</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><work-type><style face="normal" font="default" size="100%">doctoral</style></work-type></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Hodson, A</style></author><author><style face="normal" font="default" size="100%">Alexandre M. Anesio</style></author><author><style face="normal" font="default" size="100%">Martyn Tranter</style></author><author><style face="normal" font="default" size="100%">Andrew G Fountain</style></author><author><style face="normal" font="default" size="100%">Osborn, M</style></author><author><style face="normal" font="default" size="100%">John C. Priscu</style></author><author><style face="normal" font="default" size="100%">Johanna Laybourn-Parry</style></author><author><style face="normal" font="default" size="100%">Sattler, B</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Glacial ecosystems</style></title><secondary-title><style face="normal" font="default" size="100%">Ecological Monographs</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Biggie</style></keyword><keyword><style  face="normal" font="default" size="100%">snow ecology</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2008</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1890/07-0187.1</style></url></web-urls></urls><edition><style face="normal" font="default" size="100%">1</style></edition><volume><style face="normal" font="default" size="100%">78</style></volume><pages><style face="normal" font="default" size="100%">41-67</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;div&gt;There is now compelling evidence that microbially mediated reactions impart a significant effect upon the dynamics, composition, and abundance of nutrients in glacial melt water. Consequently, we must now consider ice masses as ecosystem habitats in their own right and address their diversity, functional potential, and activity as part of alpine and polar environments. Although such research is already underway, its fragmentary nature provides little basis for developing modern concepts of glacier ecology. This paper therefore provides a much-needed framework for development by reviewing the physical, biogeochemical, and microbiological characteristics of microbial habitats that have been identified within glaciers and ice sheets. Two key glacial ecosystems emerge, one inhabiting the glacier surface (the supraglacial ecosystem) and one at the ice-bed interface (the subglacial ecosystem). The supraglacial ecosystem is characterized by a diverse consortium of microbes (usually bacteria, algae, phytoflagellates, fungi, viruses and occasional rotifers, tardigrades, and diatoms) within the snowpack, supraglacial streams, and melt pools (cryoconite holes). The subglacial system is dominated by aerobic/anaerobic bacteria and most probably viruses in basal ice/till mixtures and subglacial lakes. A third, so-called englacial ecosystem is also described, but it is demonstrated that conditions within glacier ice are sufficient to make metabolic activity and its impact upon nutrient dynamics negligible at the glacier scale.&lt;/div&gt;&lt;div&gt;&amp;nbsp;&lt;/div&gt;&lt;div&gt;Consideration of the surface and internal heat balances of the glacier show that all glacial ecosystems are sensitive to climate change, although at different timescales. Thus, while rapid, melt-driven habitat changes lead to melt-out, resuscitation, and redistribution of microorganisms in many supraglacial ecosystems, much slower climatic and glacial mass-balance processes effect such changes in the subglacial ecosystem. Paradoxically, it is shown that these forces have brought about net refreezing and the onset of cryostasis in the subglacial ecosystems of many Arctic glaciers subject to thinning in recent decades.&lt;/div&gt;</style></abstract></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Diana H. Wall</style></author><author><style face="normal" font="default" size="100%">Mark A. Bradford</style></author><author><style face="normal" font="default" size="100%">Mark G. StJohn</style></author><author><style face="normal" font="default" size="100%">John A. Trofymow</style></author><author><style face="normal" font="default" size="100%">Valerie Behan-Pelletier</style></author><author><style face="normal" font="default" size="100%">David E. Bignell</style></author><author><style face="normal" font="default" size="100%">J. Mark Dangerfield</style></author><author><style face="normal" font="default" size="100%">William J. Parton</style></author><author><style face="normal" font="default" size="100%">Josef Rusek</style></author><author><style face="normal" font="default" size="100%">Winfried Voigt</style></author><author><style face="normal" font="default" size="100%">Volkmar Wolters</style></author><author><style face="normal" font="default" size="100%">Holley Zadeh Gardel</style></author><author><style face="normal" font="default" size="100%">Fred O. Ayuke</style></author><author><style face="normal" font="default" size="100%">Richard Bashford</style></author><author><style face="normal" font="default" size="100%">Olga I. Beljakova</style></author><author><style face="normal" font="default" size="100%">Patrick J. Bohlen</style></author><author><style face="normal" font="default" size="100%">Alain Brauman</style></author><author><style face="normal" font="default" size="100%">Stephen Flemming</style></author><author><style face="normal" font="default" size="100%">Joh R. Henschel</style></author><author><style face="normal" font="default" size="100%">Dan L. Johnson</style></author><author><style face="normal" font="default" size="100%">T. Hefin Jones</style></author><author><style face="normal" font="default" size="100%">Marcela Kovarova</style></author><author><style face="normal" font="default" size="100%">J. Marty Kranabetter</style></author><author><style face="normal" font="default" size="100%">Les Kutny</style></author><author><style face="normal" font="default" size="100%">Kuo-Chuan Lin</style></author><author><style face="normal" font="default" size="100%">Mohamed Maryati</style></author><author><style face="normal" font="default" size="100%">Dominique Masse</style></author><author><style face="normal" font="default" size="100%">Andrei Pokarzhevskii</style></author><author><style face="normal" font="default" size="100%">Homathevi Rahman</style></author><author><style face="normal" font="default" size="100%">Millor G. Sabara</style></author><author><style face="normal" font="default" size="100%">Joerg-Alfred Salamon</style></author><author><style face="normal" font="default" size="100%">Michael J. Swift</style></author><author><style face="normal" font="default" size="100%">Amanda Varela</style></author><author><style face="normal" font="default" size="100%">Heraldo L. Vasconcelos</style></author><author><style face="normal" font="default" size="100%">Don White</style></author><author><style face="normal" font="default" size="100%">Xiaming Zou</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Global decomposition experiment shows soil animal impacts on decomposition are climate dependent</style></title><secondary-title><style face="normal" font="default" size="100%">Global Change Biology</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2008</style></year><pub-dates><date><style  face="normal" font="default" size="100%">11/2008</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://onlinelibrary.wiley.com/doi/10.1111/j.1365-2486.2008.01672.x/full</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">14</style></volume><pages><style face="normal" font="default" size="100%">2661-2677</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">11</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Diana H. Wall</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Global Change tipping points: Above- and below-ground biotic interactions in a low diversity ecosystem</style></title><secondary-title><style face="normal" font="default" size="100%">Philosophical Transactions of the Royal Society B, Biological Sciences</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Biggie</style></keyword><keyword><style  face="normal" font="default" size="100%">soil</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2007</style></year><pub-dates><date><style  face="normal" font="default" size="100%">12/2007</style></date></pub-dates></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://rstb.royalsocietypublishing.org/content/362/1488/2291.full</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">362</style></volume><pages><style face="normal" font="default" size="100%">2291-2306</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;&lt;span style=&quot;color: rgb(51, 49, 50); font-family: Arial, Helvetica, sans-serif; font-size: 14px; line-height: 26.04px;&quot;&gt;Low diversity ecosystems are expected to be more vulnerable to global changes although they have received less attention than high diversity ecosystems. Addressing the present state of the Antarctic Dry Valley region by focusing on the potential global changes that may alter the coupling of above- and below-ground species and ecosystem processes is a realistic and critical need that has value beyond the Antarctic community. Presented here are suggested implications of global change on the Dry Valley terrestrial systems and how these effects might be manifested in the future.&lt;/span&gt;&lt;/p&gt;</style></abstract><issue><style face="normal" font="default" size="100%">1488</style></issue><work-type><style face="normal" font="default" size="100%">Journal</style></work-type></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Wagner, B</style></author><author><style face="normal" font="default" size="100%">Melles, M</style></author><author><style face="normal" font="default" size="100%">Peter T. Doran</style></author><author><style face="normal" font="default" size="100%">Kenig, Fabien</style></author><author><style face="normal" font="default" size="100%">Forman, S</style></author><author><style face="normal" font="default" size="100%">Pierau, R</style></author><author><style face="normal" font="default" size="100%">Allan, P</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Glacial and postglacial sedimentation in the Fryxell basin, Taylor Valley, Southern Victoria Land, Antarctica</style></title><secondary-title><style face="normal" font="default" size="100%">Palaeography, Palaeoclimatology, Palaeoecology</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><volume><style face="normal" font="default" size="100%">341</style></volume><pages><style face="normal" font="default" size="100%">320</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Andrew G Fountain</style></author><author><style face="normal" font="default" size="100%">Thomas H. Nylen</style></author><author><style face="normal" font="default" size="100%">MacClune, K</style></author><author><style face="normal" font="default" size="100%">Gayle L. Dana</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Glacier mass balances (1993-2001) Taylor Valley, McMurdo Dry Valleys, Antarctica</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Glaciology</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2006</style></year></dates><volume><style face="normal" font="default" size="100%">52</style></volume><pages><style face="normal" font="default" size="100%">451</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Sarah Fortner</style></author><author><style face="normal" font="default" size="100%">Martyn Tranter</style></author><author><style face="normal" font="default" size="100%">Andrew G Fountain</style></author><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author><author><style face="normal" font="default" size="100%">Kathleen A. Welch</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The Geochemistry of Supraglacial Streams of Canada Glacier, Taylor Valley (Antarctica), and their Evolution into Proglacial Waters</style></title><secondary-title><style face="normal" font="default" size="100%">Aquatic Geochemistry</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><volume><style face="normal" font="default" size="100%">11</style></volume><pages><style face="normal" font="default" size="100%">391-412</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><accession-num><style face="normal" font="default" size="100%">LTER63390</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Brent C. Christner</style></author><author><style face="normal" font="default" size="100%">Jill A. Mikucki</style></author><author><style face="normal" font="default" size="100%">Christine M. Foreman</style></author><author><style face="normal" font="default" size="100%">Denson, J</style></author><author><style face="normal" font="default" size="100%">John C. Priscu</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Glacial ice cores: a model system for developing extraterrestrial decontamination protocols</style></title><secondary-title><style face="normal" font="default" size="100%">Icarus</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">/reports/lakes/ChristnerEtAl2005Decontamination.pdf</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">174</style></volume><pages><style face="normal" font="default" size="100%">572-584</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author><author><style face="normal" font="default" size="100%">Kathleen A. Welch</style></author><author><style face="normal" font="default" size="100%">Anne E. Carey</style></author><author><style face="normal" font="default" size="100%">Diana H. Wall</style></author><author><style face="normal" font="default" size="100%">Ross A. Virginia</style></author><author><style face="normal" font="default" size="100%">Andrew G Fountain</style></author><author><style face="normal" font="default" size="100%">Peter T. Doran</style></author><author><style face="normal" font="default" size="100%">Csatho, B</style></author><author><style face="normal" font="default" size="100%">Tremper, C</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Groundwater seeps in Taylor Valley Antarctica: An example of a subsurface melt event</style></title><secondary-title><style face="normal" font="default" size="100%">Annals of Glaciology</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><volume><style face="normal" font="default" size="100%">40</style></volume><pages><style face="normal" font="default" size="100%">200-206</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Wolf, A</style></author><author><style face="normal" font="default" size="100%">Miller, G</style></author><author><style face="normal" font="default" size="100%">Olsen, C</style></author><author><style face="normal" font="default" size="100%">Forman, S</style></author><author><style face="normal" font="default" size="100%">Peter T. Doran</style></author><author><style face="normal" font="default" size="100%">Holmgren, S</style></author></authors><secondary-authors><author><style face="normal" font="default" size="100%">Pienitz, R</style></author><author><style face="normal" font="default" size="100%">Douglas, Marianne S. V.</style></author><author><style face="normal" font="default" size="100%">J.P. Smol</style></author></secondary-authors></contributors><titles><title><style face="normal" font="default" size="100%">Geochronology of high latitude lake sediments</style></title><secondary-title><style face="normal" font="default" size="100%">Long-Term Environmental Change in Arctic and Antarctic Lakes</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2004</style></year></dates><publisher><style face="normal" font="default" size="100%">Kluwer Academic Publishers</style></publisher><language><style face="normal" font="default" size="100%">eng</style></language><accession-num><style face="normal" font="default" size="100%">LTER63387</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Jill A. Mikucki</style></author><author><style face="normal" font="default" size="100%">Christine M. Foreman</style></author><author><style face="normal" font="default" size="100%">Sattler, B</style></author><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author><author><style face="normal" font="default" size="100%">John C. Priscu</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geomicrobiology of Blood Fall: An iron-rich saline discharge at the terminus of the Taylor Glacier, Antarctica</style></title><secondary-title><style face="normal" font="default" size="100%">Aquatic Geochemistry</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2004</style></year></dates><volume><style face="normal" font="default" size="100%">10</style></volume><pages><style face="normal" font="default" size="100%">199-200</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><accession-num><style face="normal" font="default" size="100%">LTER63375</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Derek R. Mueller</style></author><author><style face="normal" font="default" size="100%">Pollard, W</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Gradient analysis of cryoconite ecosystems from two Polar glaciers</style></title><secondary-title><style face="normal" font="default" size="100%">Polar Biology</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2004</style></year></dates><volume><style face="normal" font="default" size="100%">27</style></volume><pages><style face="normal" font="default" size="100%">66-74</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><accession-num><style face="normal" font="default" size="100%">LTER49873</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Karen J. Lewis</style></author><author><style face="normal" font="default" size="100%">Andrew G Fountain</style></author><author><style face="normal" font="default" size="100%">Kargel, J</style></author><author><style face="normal" font="default" size="100%">MacAyeal, D</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Glaciers of the McMurdo Dry Valleys: terrestrial analog for Martian polar sublimation</style></title><secondary-title><style face="normal" font="default" size="100%">Journal of Geophysical Research</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2003</style></year></dates><volume><style face="normal" font="default" size="100%">108</style></volume><pages><style face="normal" font="default" size="100%">5031</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><accession-num><style face="normal" font="default" size="100%">LTER49870</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Derek R. Mueller</style></author><author><style face="normal" font="default" size="100%">Warwick F. Vincent</style></author><author><style face="normal" font="default" size="100%">Pollard, W</style></author><author><style face="normal" font="default" size="100%">Christian H. Fritsen</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Glacial cryoconite ecosystems: a bipolar comparison of algal communities and habitats</style></title><secondary-title><style face="normal" font="default" size="100%">Nova Hedwigia</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2001</style></year></dates><volume><style face="normal" font="default" size="100%">123</style></volume><pages><style face="normal" font="default" size="100%">173-197</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><accession-num><style face="normal" font="default" size="100%">LTER49829</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Osvaldo E. Sala</style></author><author><style face="normal" font="default" size="100%">Kinzig, A</style></author><author><style face="normal" font="default" size="100%">Leemans, R</style></author><author><style face="normal" font="default" size="100%">Lodge, D</style></author><author><style face="normal" font="default" size="100%">Mooney, H</style></author><author><style face="normal" font="default" size="100%">Oesterheld, M</style></author><author><style face="normal" font="default" size="100%">Poff, N</style></author><author><style face="normal" font="default" size="100%">Sykes, M</style></author><author><style face="normal" font="default" size="100%">Walker, B</style></author><author><style face="normal" font="default" size="100%">Walkder, M</style></author><author><style face="normal" font="default" size="100%">Diana H. Wall</style></author><author><style face="normal" font="default" size="100%">F. S. Chapin</style></author><author><style face="normal" font="default" size="100%">Armesto, J</style></author><author><style face="normal" font="default" size="100%">Berlow, E</style></author><author><style face="normal" font="default" size="100%">Bloomfield, J</style></author><author><style face="normal" font="default" size="100%">Dirzo, R</style></author><author><style face="normal" font="default" size="100%">Huber-Sanwald, E</style></author><author><style face="normal" font="default" size="100%">Huenneke, L</style></author><author><style face="normal" font="default" size="100%">Jackson, R</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Global biodiversity scenarios for the year 2100</style></title><secondary-title><style face="normal" font="default" size="100%">Science</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2000</style></year></dates><volume><style face="normal" font="default" size="100%">287</style></volume><pages><style face="normal" font="default" size="100%">1770-1774</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Wolters, V</style></author><author><style face="normal" font="default" size="100%">Wardle, D</style></author><author><style face="normal" font="default" size="100%">Brussaard, L</style></author><author><style face="normal" font="default" size="100%">J. Mark Dangerfield</style></author><author><style face="normal" font="default" size="100%">Brown, V</style></author><author><style face="normal" font="default" size="100%">Giller, K</style></author><author><style face="normal" font="default" size="100%">Hooper, D</style></author><author><style face="normal" font="default" size="100%">Osvaldo E. Sala</style></author><author><style face="normal" font="default" size="100%">Tiedje, J</style></author><author><style face="normal" font="default" size="100%">van Veen, J</style></author><author><style face="normal" font="default" size="100%">Silver, W</style></author><author><style face="normal" font="default" size="100%">Bignell, D</style></author><author><style face="normal" font="default" size="100%">David C.  Coleman</style></author><author><style face="normal" font="default" size="100%">Lavelle, P</style></author><author><style face="normal" font="default" size="100%">van der Putten, W</style></author><author><style face="normal" font="default" size="100%">DeRuiter, P</style></author><author><style face="normal" font="default" size="100%">Josef Rusek</style></author><author><style face="normal" font="default" size="100%">Diana H. Wall</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Global change effects on above and below ground biodiversity in terrestrial ecosystems: interactions and implications for ecosystem functioning</style></title><secondary-title><style face="normal" font="default" size="100%">Bioscience</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2000</style></year></dates><volume><style face="normal" font="default" size="100%">50</style></volume><pages><style face="normal" font="default" size="100%">1089-1099</style></pages><language><style face="normal" font="default" size="100%">eng</style></language></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">John C. Priscu</style></author><author><style face="normal" font="default" size="100%">Edward E. Adams</style></author><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author><author><style face="normal" font="default" size="100%">Mary A. Voytek</style></author><author><style face="normal" font="default" size="100%">David W. Mogk</style></author><author><style face="normal" font="default" size="100%">Robert L. Brown</style></author><author><style face="normal" font="default" size="100%">Christopher P. McKay</style></author><author><style face="normal" font="default" size="100%">Cristina D. Takacs-Vesbach</style></author><author><style face="normal" font="default" size="100%">Kathleen A. Welch</style></author><author><style face="normal" font="default" size="100%">Craig F.  Wolf</style></author><author><style face="normal" font="default" size="100%">Julie D. Kirshtein</style></author><author><style face="normal" font="default" size="100%">Recep Avci</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geomicrobiology of sub-glacial ice above Vostok Station</style></title><secondary-title><style face="normal" font="default" size="100%">Science</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1999</style></year></dates><volume><style face="normal" font="default" size="100%">286</style></volume><pages><style face="normal" font="default" size="100%">2141-2144</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><issue><style face="normal" font="default" size="100%">5447</style></issue></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author><author><style face="normal" font="default" size="100%">Kathleen A. Welch</style></author><author><style face="normal" font="default" size="100%">Klaus Neumann</style></author><author><style face="normal" font="default" size="100%">Jeffrey K. Toxey</style></author><author><style face="normal" font="default" size="100%">Robyn McArthur</style></author><author><style face="normal" font="default" size="100%">Changela Williams</style></author><author><style face="normal" font="default" size="100%">Diane M. McKnight</style></author><author><style face="normal" font="default" size="100%">Daryl L. Moorhead</style></author></authors><tertiary-authors><author><style face="normal" font="default" size="100%">John C. Priscu</style></author></tertiary-authors></contributors><titles><title><style face="normal" font="default" size="100%">Geochemical Linkages Among Glaciers, Streams, and Lakes Within the Taylor Valley, Antarctica</style></title><secondary-title><style face="normal" font="default" size="100%">Ecosystem Processes in a Polar Desert: The McMurdo Dry Valleys, Antarctica</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1998</style></year></dates><volume><style face="normal" font="default" size="100%">72</style></volume><pages><style face="normal" font="default" size="100%">77-92</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><accession-num><style face="normal" font="default" size="100%">LTER12885</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Andrew G Fountain</style></author><author><style face="normal" font="default" size="100%">Gayle L. Dana</style></author><author><style face="normal" font="default" size="100%">Karen J. Lewis</style></author><author><style face="normal" font="default" size="100%">Bruce H. Vaughn</style></author><author><style face="normal" font="default" size="100%">Diane M. McKnight</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Glaciers of the McMurdo Dry Valleys, Southern Victoria Land, Antarctica</style></title><secondary-title><style face="normal" font="default" size="100%">Ecosystem Processes in a Polar Desert: The McMurdo Dry Valleys, Antarctica</style></secondary-title><tertiary-title><style face="normal" font="default" size="100%">Antarctic Research Series</style></tertiary-title></titles><dates><year><style  face="normal" font="default" size="100%">1998</style></year></dates><volume><style face="normal" font="default" size="100%">72</style></volume><pages><style face="normal" font="default" size="100%">65-75</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><accession-num><style face="normal" font="default" size="100%">LTER12831</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">George R. Aiken</style></author><author><style face="normal" font="default" size="100%">Diane M. McKnight</style></author><author><style face="normal" font="default" size="100%">Richard A. Harnish</style></author><author><style face="normal" font="default" size="100%">Robert Wershaw</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Geochemistry of aquatic humic substances in the Lake Fryxell Basin, Antarctica</style></title><secondary-title><style face="normal" font="default" size="100%">Biogeochemistry</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1996</style></year></dates><volume><style face="normal" font="default" size="100%">34</style></volume><pages><style face="normal" font="default" size="100%">157-188</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><accession-num><style face="normal" font="default" size="100%">LTER12782</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">W. Berry Lyons</style></author><author><style face="normal" font="default" size="100%">Paul A. Mayewski</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The geochemical evolution of terrestrial waters in the antarctic:  the role of rock-water interactions, in Physical and Biogeochemical Processes in Antarctic Lakes</style></title></titles><dates><year><style  face="normal" font="default" size="100%">1993</style></year></dates><volume><style face="normal" font="default" size="100%">59</style></volume><pages><style face="normal" font="default" size="100%">135-143</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><accession-num><style face="normal" font="default" size="100%">LTER12879</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>5</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Andrew G Fountain</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Glaciers of the southern hemisphere</style></title><secondary-title><style face="normal" font="default" size="100%">Global and Planetary Change</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">1990</style></year></dates><volume><style face="normal" font="default" size="100%">22</style></volume><language><style face="normal" font="default" size="100%">eng</style></language></record></records></xml>