1 September 2015 Project Update Volume 96, Issue 16
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Geochemistry of Subglacial Lake Whillans, West Antarctica: Implications for Microbial Activity
5th International Conference on Polar & Alpine Microbiology, Big Sky, MT, USA, 2013 Geochemistry of subglacial Lake Whillans, West Antarctica: Implications for microbial activity. Mark Skidmore1, Andrew Mitchell2, Carlo Barbante3, Alex Michaud4, Trista Vick-Majors4, John Priscu4 1Earth Sciences, Montana State University, Bozeman, MT, USA, 2Geography and Earth Sciences, Aberystwyth University, Aberystwyth, UK, 3Institute for the Dynamics of Environmental Processes-CNR, University of Venice, Venice, Italy. 4Land Resources and Environmental Sciences, Montana State University, Bozeman, MT, USA. Subglacial Lake Whillans is located beneath the Whillans Ice Stream in West Antarctica. The lake is situated beneath 800 m of ice and ~ 70 km upstream of the grounding line where Whillans Ice Stream terminates into the Ross Sea. Water and sediment samples were recovered from the lake, using clean access drilling technologies, in January, 2013. Isotopic analysis of the lake waters indicates basal meltwater from the ice sheet as the dominant water source. Geochemical analysis of the lake waters reveal it is freshwater with total dissolved solids concentrations about 1/70th that of sea water. However, mineral weathering is a significant source of solute to the lake water with a contribution also from sea water. Nutrients N and P are present at micromolar concentrations. The sediment porewaters from shallow cores (~ 40 cm depth) of the subglacial lake sediments indicate increasing solute concentration with depth, with up to ~ five times greater solute concentrations than in the lake waters. Collectively the aqueous geochemistry indicates an environment favorable for microbial activity. Thus, microbially-driven mineral weathering appears likely beneath the Whillans Ice Stream, as has been demonstrated in other subglacial systems, including in subglacial sediments of the neighboring Kamb Ice Stream. -
7Th Grade February Break Packet.Pdf
__________________ ___________________ _________________ Read this story. Then answer questions 15 through 21. e narrator, Holling Hoodhood, has a crush on Meryl Lee Kowalski. Holling’s father has been honored earlier in the story by a local business group as the best businessman of 1967. Excerpt from e Wednesday Wars by Gary D. Schmidt 1 e following week the school board met to decide on the model for the new junior high school—which was probably why Mr. Kowalski had been spending all his time muttering “classical, classical, classical.” e meeting was to be at four o’clock in the high school administration building. Mr. Kowalski would present his plan and model, and then my father would present his plan and model, and then the school board would meet in private session to decide whether Kowalski and Associates or Hoodhood and Associates would be the architect for the new junior high school. 2 I know all of this because my father was making me come. It was time I started to learn the business, he said. I needed to see firsthand how competitive bidding worked. I needed to experience architectural presentations. I needed to see architecture as the blood sport that it truly was. 3 e meeting was in the public conference room, and when I got there aer school, the school board members were all sitting at the head table, studying the folders with architectural bids. Mr. Kowalski and my father were sitting at two of the high school desks—which made the whole thing seem a little weirder than it needed to be. -
Antarctic Primer
Antarctic Primer By Nigel Sitwell, Tom Ritchie & Gary Miller By Nigel Sitwell, Tom Ritchie & Gary Miller Designed by: Olivia Young, Aurora Expeditions October 2018 Cover image © I.Tortosa Morgan Suite 12, Level 2 35 Buckingham Street Surry Hills, Sydney NSW 2010, Australia To anyone who goes to the Antarctic, there is a tremendous appeal, an unparalleled combination of grandeur, beauty, vastness, loneliness, and malevolence —all of which sound terribly melodramatic — but which truly convey the actual feeling of Antarctica. Where else in the world are all of these descriptions really true? —Captain T.L.M. Sunter, ‘The Antarctic Century Newsletter ANTARCTIC PRIMER 2018 | 3 CONTENTS I. CONSERVING ANTARCTICA Guidance for Visitors to the Antarctic Antarctica’s Historic Heritage South Georgia Biosecurity II. THE PHYSICAL ENVIRONMENT Antarctica The Southern Ocean The Continent Climate Atmospheric Phenomena The Ozone Hole Climate Change Sea Ice The Antarctic Ice Cap Icebergs A Short Glossary of Ice Terms III. THE BIOLOGICAL ENVIRONMENT Life in Antarctica Adapting to the Cold The Kingdom of Krill IV. THE WILDLIFE Antarctic Squids Antarctic Fishes Antarctic Birds Antarctic Seals Antarctic Whales 4 AURORA EXPEDITIONS | Pioneering expedition travel to the heart of nature. CONTENTS V. EXPLORERS AND SCIENTISTS The Exploration of Antarctica The Antarctic Treaty VI. PLACES YOU MAY VISIT South Shetland Islands Antarctic Peninsula Weddell Sea South Orkney Islands South Georgia The Falkland Islands South Sandwich Islands The Historic Ross Sea Sector Commonwealth Bay VII. FURTHER READING VIII. WILDLIFE CHECKLISTS ANTARCTIC PRIMER 2018 | 5 Adélie penguins in the Antarctic Peninsula I. CONSERVING ANTARCTICA Antarctica is the largest wilderness area on earth, a place that must be preserved in its present, virtually pristine state. -
A Climate of Change? the Facts Are on the Table – Now It’S the Politicians’ Turn
3-15 effzettFORSCHUNGSZENTRUM JÜLICH’S MAGAZINE Jülich researcher Martin Riese investigates climate processes in the stratosphere. A climate of change? The facts are on the table – now it’s the politicians’ turn TIDY BUSY MESSY Living cells What our brain and roads Crystals don’t clean themselves have in common have to be perfect 2 AS WE SEE IT A filter for oxygen A snowy landscape with spruces and jagged rocks? No. The picture shows a 15 x 15 micrometre section of a ceramic material from the perovskite group – imaged with an electron microscope. Jülich researchers from the Institute of Energy and Climate Research investigate these ceramics, for example to separate oxygen from the ambient air. This is only possible so far using a great deal of energy. One potential application is the oxyfuel process, which is one way of reducing the emissions of conventional power plants – ideally to water and CO2. The latter could then be separated and stored or reused. TOPICS 3 NEWS IN BRIEF Home Learning from 5 improvement for mistakes the worse Viruses modify bacteria to COVER STORY suit their own needs. Small glimmers 18 of hope Researchers provide Measuring with scientific basis A measuring error for decisions Thor’s hammer shows how cell on international membranes oscillate. climate policy. 23 8 Staying clean RESEARCH Cells have their own garbage All in good disposal system. (dis)order Magnetic resonance 24 spectrometers don’t have to be large and expensive. 20 SECTIONS Editorial Massive 4 difference Publication details 4 In crystals, flaws can be useful. What’s your research 14 all about? 19 2.2 plus Rush hour Roots, leaves, and stem – how plants distribute 26 in the brain their biomass. -
When Winter Was Still Winter. the History of a Season by Bernd Brunner
Sample Translation When Winter was still Winter. The History of a Season by Bernd Brunner Translated by Lori Lantz, Ph.D © 2016, Verlag Kiepenheuer & Witsch GmbH & Co. KG, Köln/ Verlag Galiani Berlin Translation © 2016, Lori Lantz Publication: October 2016 (Hardcover) 160 pages Including illustrations Foreign rights with: Verlag Kiepenheuer & Witsch GmbH & Co. KG Iris Brandt [email protected] Aleksandra Erakovic [email protected] Sample translation from „When Winter was still Winter“ by Bernd Brunner © 2016, Verlag Kiepenheuer & Witsch/ Galiani Berlin I have been here for about ten days – and attempting to stay warm is my only occupation. The houses are shoddily built, and the iron stoves are useless. Ivan Turgenev to Gustave Flaubert, February 20, 1870, from the Hôtel de Russie in Weimar, Germany. 2 Sample translation from „When Winter was still Winter“ by Bernd Brunner © 2016, Verlag Kiepenheuer & Witsch/ Galiani Berlin Contents The world in winter – defining a season Winter is coming: the first signs Winter weather Winter around the world Is it ever winter in the ocean? The four seasons: a natural principle? Snow crunching underfoot – the characteristics of winter What does cold feel like? About snow: properties of a material Measuring the depths Tracks and the tales they tell Why is snow white? Michelangelo’s snowman and snow festivals The magic and the horror of snow Santa without snow? Feeling winter Past precautions against the cold The long evolution of heating systems Traveling in winter John Milton’s -
Hollywoodland Text.Pdf
HOLLYWOODLAND HOLLYWOODLAND an american fairy tale JENNIFER BANASH Impetus Press PO Box 10025 Iowa City, IA 52240 www.impetuspress.com [email protected] Publisher Note: This book is a work of fiction. Names, characters, businesses, organizations, places, events, and incidents either are the product of the author’s imagination or are used fictitiously. Any resemblance to actual persons, living or dead, events, or locales is entirely coincidental. ISBN 0-9776693-0-0 September 2006 Copyright © 2006 Impetus Press. All rights reserved. for my father I’m going to be in the movies if I have to fuck Bela Lugosi to get there. Actresses are a little like race horses. It’s difficult for us when the race is cancelled. This is an attempt at the ultimate motion picture. ••• 2:00 AM, 82 ° She is in her car when it happens, the black roads around Mulholland winding and twisting, unrolling like the soft dark fabric of a magic carpet. Her eyes blur and she squints them repeatedly, leaning forward to see. The needle on the speedometer flies up past eighty, then ninety, the tendons in her right arm straining, muscles burning as she grips the wheel one-handed. Sierra loves to drive more than anything, the feeling of weightlessness, careening through the air, unstoppable. She was fucking unstoppable. She could feel the kid in the seat next to her getting nervous, moving back and forth in his seat, one hand clutching the belt that cut across his skinny frame. His jeans make a harsh scraping sound. The rasp of denim on leather annoys her, and she closes her eyes. -
Spor E Pr I N Ts
SPOR E PR I N TS BULLETIN OF THE PUGET SOUND MYCOLOGICAL SOCIETY Number 514 September 2015 52nd ANNUAL WILD MUSHROOM SHOW PHOTOGRAPHY EXHIBIT ADDED TO FALL October 10–11, Bellevue College Kim Traverse MUSHROOM SHOW Paul Hill Before she was Governor With so many great photographers out in the of the State of Washington, woods taking great photographs of mushrooms, before she was Chair of the we have decided to add a photography exhibit to Atomic Energy Commis- the Fall Show. Start looking through your photo- sion, Dixie Lee Ray, PhD, graphs and thinking was Director of The Pacific about what you might Science Center. And one of like to see hanging at the many things she was in- the fall show. Contact terested in was Citizen Sci- Paul Hill, [email protected], if you ence. With UW colleague have questions or want details. Dr. Daniel Stuntz, she sent out an appeal for those interested in mushrooms to attend a founding meeting at the center. This was the beginning of PSMS. By the end of that first year, 1964, there were seventy-five fami- GOA’S APPETITE FOR WILD MUSHROOMS IS lies signed up, and they had already held their first two-day Wild HURTING THE ECOLOGY OF WESTERN GHATS Mushroom Show! Particularly interesting in exhibit pictures Chryselle D’Silva Dias from those early days (Dixie was the photographer) are a couple http://scroll.in/, Aug. 13, 2015 of photos of Hollywood’s Ginger Rogers looking over trays of mushrooms with Dr. Stuntz. Every July and August, Every show since then, PSMS has tried to make it “just a little Goa becomes a vibrant better.” Every show has its own personality, but every show is an marketplace for muddy exciting experience. -
Race Is on to Find Life Under Antarctic Ice Russia, U.S., and Britain Drill to Discover Microbes in Subglacial Lakes
Race Is On to Find Life Under Antarctic Ice Russia, U.S., and Britain drill to discover microbes in subglacial lakes. A person works at the drilling site atop Lake Ellsworth, Antarctica. Photograph courtesy Pete Bucktrout, British Antarctic Survey Marc Kaufman for National Geographic News Published December 18, 2012 A hundred years ago, two teams of explorers set out to be the first people ever to reach the South Pole. The race between Roald Amundsen of Norway and Robert Falcon Scott of Britain became the stuff of triumph, tragedy, and legend. (See rare pictures of Scott's expedition.) Today, another Antarctic drama is underway that has a similar daring and intensity—but very different stakes. Three unprecedented, major expeditions are underway to drill deep through the ice covering the continent and, researchers hope, penetrate three subglacial lakes not even known to exist until recently. The three players—Russia, Britain, and the United States—are all on the ice now and are in varying stages of their preparations. The first drilling was attempted last week by the British team at Lake Ellsworth, but mechanical problems soon cropped up in the unforgiving Antarctic cold, putting a temporary hold on their work. The key scientific goal of the missions: to discover and identify living organisms in Antarctica's dark, pristine, and hidden recesses. (See"Antarctica May Contain 'Oasis of Life.'") Scientists believe the lakes may well be home to the kind of "extreme" life that could eke out an existence on other planets or moons of our solar system, so finding them on Earth could help significantly in the search for life elsewhere. -
Environment and Processes of Subglacial Lake Whillans, West Antarctica
Environment and Processes of Subglacial Lake Whillans, West Antarctica Ross Powell1, Tim Hodson1, Jeremy Wei1, Slawek Tulaczyk2, Stefanie Brachfeld3, Isla Castañeda4, Rebecca Putkammer1, Reed Scherer1, and the WISSARD Science Team 1Department of Geology and Environmental Geosciences, Northern Illinois University 2Department of Earth and Planetary Sciences, University of California Santa Cruz 3Earth and Environmental Studies, Montclair State University 4Department of Geosciences, University of Massachusetts, Amherst Subglacial Lake Whillans (SLW) lies 800m below the low gradient, Whillans Ice Plain West Antarctica, upstream from where Whillans Ice Stream goes afloat into the Ross Ice Shelf. During 2013-14 season the WISSARD project made measurements in, and collected water and sediment samples from SLW. Sediment is typical subglacial till; a homogenized, structureless diamicton. Debris from local basal ice is likely not contributed to SLW by rainout because ice is theoretically below pressure melting. So lake floor diamicton likely was transported to SLW by deformation while the ice stream was grounded at the drill site both prior to lake formation and during lake “lowstands”. Satellite altimetry has shown SLW experiences short (~7 month) discharge events, lowering the ice surface and lake water level by between 1- 4m. Lake lowstands are separated by longer periods of gradual recharge, but over the period of many lowstands the ice stream is suspected to touch down and couple with the lake floor, potentially shearing new till into SLW. Subglacial hydrological diversions also may play a role in SLW history; if water is captured by another drainage basin, then the bed at SLW will also act as a till. The lack of sorted sediment (apart from a lamina of mud at the sediment-water interface) and erosional lags within sediment cores indicate water flow during discharge/recharge events has had a low current velocity with quiescent conditions in the lake. -
1 Big Thing: the Lake at the Bottom of the Ice Sheet
1/21/2019 Axios Science - January 17, 2019 - Axios Axios Science Subscribe By Andrew Freedman Welcome back, and thanks for subscribing to Axios Science. Please consider inviting your friends, family and colleagues to sign up. I appreciate any tips, scoops and feedback — simply reply to this email or send me a message at [email protected]. 1 big thing: The lake at the bottom of the ice sheet https://www.axios.com/newsletters/axios-science-616ee9dd-0f6e-411f-9994-e78368d62cd5.html 1/10 1/21/2019 Axios Science - January 17, 2019 - Axios The UV collar and borehole, showing the water of Subglacial Lake Mercer, from the SALSA Project. Photo: Billy Collins, SALSA Science Team A research team drilling thousands of feet under the Antarctic ice sheet has found new evidence of microbial life there — life forms that live in an environment devoid of sunlight and are not known to exist elsewhere. Why it matters: Subglacial Lake Mercer is only the second subglacial lake in Antarctica to be explored, in an area as vast as twice the continental United States. That means scientists have to draw a lot of conclusions from just two holes — but it's the only way to learn about what kind of life exists in the mysterious world of lakes and rivers deep beneath the ice. In addition, researchers think the water moving underneath the ice sheet could further destabilize portions of it, adding to the already quickening pace of sea level rise. Details: Researchers sampled Subglacial Lake Whillans in 2013, finding abundant microbial life. Now we have much more data collected from Subglacial Lake Mercer. -
Did Holocene Climate Changes Drive West Antarctic Grounding Line Retreat and Re-Advance?
https://doi.org/10.5194/tc-2020-308 Preprint. Discussion started: 19 November 2020 c Author(s) 2020. CC BY 4.0 License. Did Holocene climate changes drive West Antarctic grounding line retreat and re-advance? Sarah U. Neuhaus1, Slawek M. Tulaczyk1, Nathan D. Stansell2, Jason J. Coenen2, Reed P. Scherer2, Jill 5 A. Mikucki3, Ross D. Powell2 1Earth and Planetary Sciences, University oF CaliFornia Santa Cruz, Santa Cruz, CA, 95064, USA 2Department oF Geology and Environmental Geosciences, Northern Illinois University, DeKalb, IL, 60115, USA 3Department oF Microbiology, University oF Tennessee Knoxville, Knoxville, TN, 37996, USA 10 Correspondence to: Sarah U. Neuhaus ([email protected]) Abstract. Knowledge oF past ice sheet conFigurations is useFul For informing projections of Future ice sheet dynamics and For calibrating ice sheet models. The topology oF grounding line retreat in the Ross Sea Sector oF Antarctica has been much debated, but it has generally been assumed that the modern ice sheet is as small as it has been for more than 100,000 years 15 (Conway et al., 1999; Lee et al., 2017; Lowry et al., 2019; McKay et al., 2016; Scherer et al., 1998). Recent findings suggest that the West Antarctic Ice Sheet (WAIS) grounding line retreated beyond its current location earlier in the Holocene and subsequently re-advanced to reach its modern position (Bradley et al., 2015; Kingslake et al., 2018). Here, we further constrain the post-LGM grounding line retreat and re-advance in the Ross Sea Sector using a two-phase model of radiocarbon input and decay in subglacial sediments From six sub-ice sampling locations. -
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wood, aided by the presence of the Exidiopsis The Outside Story effusa fungus. Scientists believe that as the fungus breaks down the wood of a broad-leafed tree species, it produces complex molecules that mix with the water in the stem. Moisture near the surface of the dead branch or log is extruded from the pores of the wood and freezes into thin hairs of ice, which build up overnight into what looks like a tuft of wool or a white, shiny beard. Frost flowers are similar, but occur on the stems of certain plants. They may resemble white ribbon candy, flowing curtains, swanlike sculptures, serpentine swirls, silky spirals, or glossy fans. Despite the name, they’re not flowers, nor frost. While true frost occurs when moisture in the air condenses on a cold surface, these fanciful shapes result when sap, augmented by water drawn up from the roots, slowly pushes through the stem of an herbaceous plant and freezes on contact with the cold. They form most often near the base of the stem, but may extend further up. Hair Ice and Frost Flowers: Frost flowers occur so infrequently that many Ephemeral Frozen Forms woods walkers never see them. Their rarity is By: Laurie D. Morrissey largely due to the limited circumstances that create them. The ground must be warm enough If you are out walking on an early winter morning, for the plant’s root system to be active and the air you might be lucky enough to see some of nature’s must be cold enough to freeze the water flowing most beautiful and ephemeral sights: hair ice and up its conductive tissues.