Research Highlights

Total Page:16

File Type:pdf, Size:1020Kb

Research Highlights Vol 452|13 March 2008 RESEARCH HIGHLIGHTS Nosing around J. Exp. Biol. 211, 921–934 (2008) The elephant nose fish uses its eponymous if misnamed adaptation — actually a protuberant chin appendage — as an electrical ‘flashlight’, and Jacob Engelmann PIXONNET.COM/ALAMY at the University of Bonn in Germany and his colleagues have shown how. Gnathonemus petersii senses objects through the distortions they cause in an electric field that it creates. The researchers confirm that elephant noses have two different high-acuity sensory regions, known as foveae. One is the actual nasal region, and the other is in its characteristic chin, called a Schnauzenorgan. The highest density of electrical receptors is at the tip of this appendage. EVOLUTION Astronomers expect that many stars THEORETICAL PHYSICS periodically reverse their magnetic polarity, Streetwise weeds but so far only about 20 stars have had Holographic memory Proc. Natl Acad. Sci. USA 105, 3796–3799 (2008) magnetic polarization measurements taken Phys. Rev. A 77, 020302 (2008) City weeds are adapting to their urban more than once. A special type of hologram may provide a environment at a staggering rate, suggests Jean-François Donati of France’s CNRS way to store light’s quantum information. a research team in France. and his colleagues, who made the discovery, Regular holograms store three-dimensional Pierre-Olivier Cheptou and his colleagues estimate that Tau Bootis’s poles flip every information in an interference pattern, often at the CNRS, France’s basic-research agency, year or so. etched on a glass surface. But such a system in Montpellier analysed the dispersal of the won’t work for quantum information, which weed Crepis sancta, which produces two types CHEMISTRY includes fundamental uncertainties that of seed — a light, feathery, wind-dispersed cannot be held in a classical medium. one and a heavy one. The researchers A ring-side seat for chloride Eugene Polzik of the Danish Research found that feathery seeds dispersed along Angew. Chem. Int. Edn doi:10.1002/anie.200704717 Center for Quantum Optics in Copenhagen Montpellier’s city streets have a 55% lower (2008) and his colleagues at St Petersburg University chance of successfully settling in their parent’s Normally, opposites attract, but chemists in Russia determined a way to store light’s local patch than heavy seeds. In patchy, at Indiana University in Bloomington have quantum properties in a cloud of atoms. pavement-dense habitats, weeds release a designed an uncharged organic molecule By entangling the light with atoms at a significantly higher proportion of heavy seeds that can nevertheless attract and hold temperature close to absolute zero, it should than do their country counterparts. negatively charged ions. be possible to store the quantum features of Genetic evaluations suggest that short- Amar Flood and Yongjun Li the light in the atoms’ collective spins. The term evolution has taken place during a made a doughnut-shaped information can then be read from the atoms mere 5–12 generations. molecule from a number of by reversing the process. small building-block ASTRONOMY molecules, using a CHEMICAL BIOLOGY technique called Magnetic flux ‘click chemistry’. Fixing fragile flies Mon. Not. R. Astron. Soc. doi:10.1111/j.1365- The doughnut’s Nature Chem. Biol. doi:10.1038/nchembio.78 (2008) 2966.2008.12946.x (2008) hole snugly fits a A fruitfly model of fragile X syndrome, a The Sun’s magnetic poles are known to chloride (pictured left), and common cause of mental retardation in reverse their polarity every 11 years, but could potentially hold other anions such as humans, has unveiled possible therapeutic it is not alone — another ‘flip-flopper’ has fluoride, depending on building-block size. targets to combat the condition. been identified. Recent mapping of the Anions are held in place by hydrogen Flies lacking a gene called Fmr1 exhibit magnetic field around nearby star Tau bonds. These were thought to be too weak some physical and behavioural features Bootis shows that its polarity to provide a strong attractive pull, but of fragile X syndrome. Stephen Warren at has reversed since the last nitrogen atoms in the doughnut draw Emory University School of Medicine in observation in 2006. some electron density out of the Atlanta, Georgia, and his colleagues found Measurements of C–H bonds, making it more that food enriched with glutamate, which the polarization of attractive to a negative ion. functions as an excitatory neurotransmitter, the light emitted by Tau These molecules could kills mutant embryos. Bootis allow its complicated provide a new regime for The researchers screened a library of 2,000 magnetic structure to be calculated. removing unwanted anions from solution. compounds and characterized nine that 130 NATURE|Vol 452|13 March 2008 RESEARCH HIGHLIGHTS JOURNAL CLUB John Church Centre for Australian Weather and Climate Research, allowed Fmr1 mutants to survive a high- STRUCTURAL BIOLOGY Tasmania, Australia glutamate diet. Three of the compounds Into the groove An oceanographer ponders affect the inhibitory neurotransmitter, the difficulty of accurately GABA. Treating mutants with GABA Mol. Cell 29, 525–531 (2008) estimating abyssal-ocean relieved glutamate toxicity, and restored Genes are often marked for silencing by warming. several features, including normal courtship the addition of methyl groups to DNA. behaviour and some brain morphology. This type of modification is recognized Estimating how much oceans are by transcriptional regulators such as the warming and where within them FOOD SCIENCE repressor MeCP2, but not in the way heat is stored is a fascinating generally predicted, according to research challenge for me and my fellow The origins of la louche by Adrian Bird and Malcolm Walkinshaw at oceanographers. So far, most Langmuir 24, 1701–1706 (2008) the University of Edinburgh, UK, and their studies comparing observations Part of the allure of aniseed-flavoured spirits collaborators. and models of changing ocean such as absinthe (pictured below), ouzo Previous studies predicted that a temperatures have focused on the and pastis is the mysterious ‘louche’ — their hydrophobic patch in the MeCP2 protein upper 1 kilometre of water. But what transformation from clear to cloudy and made contact with methylated DNA. However, about the abyssal depths, from opalescent with the addition of water. The structural analysis of how the two molecules about 3,000 metres to the bottom? effect comes from the formation of insoluble, bind together suggests that hydrogen bonding Are changes in those waters milky droplets of anise-flavoured oil. of MeCP2 with the water-containing groove in really so slow as to be essentially Details of the process are murky, however. the DNA double helix is crucial. irrelevant to atmospheric warming? Erik van der Linden of Wageningen The research also reveals how a mutation The most comprehensive University in the Netherlands and his common in Rett syndrome, an autism surface-to-bottom measurements colleagues made the first direct measurement spectrum disorder, might disrupt this binding. of ocean temperature were of the oil droplets’ interfacial collected by research ships over tension, which determines how many months during the World fast they grow. These rates, and Ocean Circulation Experiment in their dependence on ethanol the 1990s. By comparing these concentration, differ from those observations with more recent ones predicted by conventional theory. from the World Climate Research PIXONNET.COM/ALAMY Because this ‘spontaneous Programme’s CLIVAR Project, Greg emulsification’ is being explored Johnson and his colleagues have for various purposes, including shown that the Pacific Ocean’s the production of drug-loaded abyssal waters have warmed during nanoparticles and microcapsules, the past two decades (G. C. Johnson the discrepancy is more than just a et al. J. Clim. 20, 5365–5375; 2007). puzzle for barflies. Although the temperature increase is small — up to about GEOLOGY 0.01 °C — compared with the much larger changes in the upper Glacier slimming 1,000 metres of the ocean, it has Geology 36, 223–226 (2008) OPTICS occurred over a thickness of several Satellites have documented the rapid decline kilometres, implying a huge quantity of the West Antarctic ice sheet during the How to make a black hole of heat storage. The deep warming past two decades, with thinning of more than Science 319, 1367–1370 (2008) is strongest in the south-west a metre per year. But pre-satellite — let alone Researchers have created an analogue of a Pacific, where newly ventilated prehistoric — data are harder to come by. black hole in a lab, using light trapped in an abyssal waters enter from the south. Joanne Johnson from the British Antarctic optical fibre. This optical black hole affects The Pacific warming, and abyssal Survey in Cambridge, UK, and her colleagues light in ways equivalent to the intense gravity warming elsewhere, means that we used rocks to gain insight into the history of at a black hole’s ‘event horizon’, beyond which should start considering abyssal glaciers by the Amundsen Sea Embayment. no light can escape. waters when estimating sea-level They suggest that, for most of the past Pulses of light travelling down the fibre rise and the climate’s sensitivity 10,000 years, these glaciers have been thinning affect the fibre’s light-carrying properties to increasing greenhouse-gas at rates of just a few centimetres per year. in a manner analogous to the bending of concentrations. There is plenty to The team took samples from nunataks space-time by gravity. The leading edge of a find out: how does the heat reach — rocky peaks that poke through the ice and pulse then acts like an event horizon when abyssal waters? Is the warming sometimes, like dipsticks, contain evidence of it catches up with slower light up ahead. human-induced? Designing historical glacier heights. The thinning rates, Meanwhile, the pulse’s trailing edge becomes and implementing an adequate which the researchers established by isotopic equivalent to a white-hole event horizon, abyssal-water-observing system is dating of quartz grains from within seven where no light can enter.
Recommended publications
  • Jörg M. Schäfer
    JÖRG M. SCHÄFER LAMONT-DOHERTY EARTH OBSERVATORY • THE EARTH INSTITUTE AT COLUMBIA UNIVERSITY ROUTE 9W • PALISADES, NY 10964 • USA PHONE: 1 845 365 8756 • FAX: 1 845 365 8155 • EMAIL: [email protected] Personal Born 1968 in Stuttgart, Germany Citizenship: German Language: german, english, french 90 Morningside Drive • Apt. 2G New York • NY-10027 Education Lamont Research Professor Lamont-Doherty Earth Observatory of Columbia University Adjunct Professor Dept. of Earth and Environmental Sciences, Columbia University Doherty Associate Research Scientist (September 2003-November 2008) Lamont-Doherty Earth Observatory of Columbia University Postdoctoral Research Fellow (January 2001-August 2003) Lamont-Doherty Earth Observatory of Columbia University Postdoctoral Researcher (February 2000-October 2000) Dept. of Earth Sciences, Swiss Federal Institute of Technology (ETH) Zürich Ph.D. (March 1996-June 2000) Swiss Federal Institute of Technology (ETH) Zürich. Dissertation: Reconstruction of landscape evolution and continental paleoglaciations using in-situ cosmogenic nuclides. Jointly supervised by Profs. R. Wieler, C. Schlüchter, A.N. Halliday at the Department of Earth Sciences, ETH Zürich Masters Degree (“Diplom”) in Physics (1995) Institute of Environmental Physics, University of Heidelberg, Germany. Reconstruction of bio-geochemical trace substance cycles from an alpine ice- core. Supervisors: Dr. D. Wagenbach, Prof. U. Platt. Exchange student • ERASMUS program (1991-92) Department of Physics, University of Aix- Marseille III,
    [Show full text]
  • Proposal Description: Cenozoic Formation of the Antarctic Glacial Landscape Investigated by Low-Temperature Thermochronometry
    PROPOSAL DESCRIPTION: CENOZOIC FORMATION OF THE ANTARCTIC GLACIAL LANDSCAPE INVESTIGATED BY LOW-TEMPERATURE THERMOCHRONOMETRY Summary: This pre-proposal outlines a drilling program aimed at investigating the origin of the present glacial landscape in the fjord system of the western Antarctic Peninsula by applying novel methods of low-temperature thermochronometry. This, in turn, is important in understanding the Cenozoic geologic history of Antarctica and, more broadly, in understanding the role of glaciation in climate-solid Earth interactions. Accomplishing this requires samples of the present bedrock surface in the location of maximum Cenozoic erosion, that is, glacial valley bottoms. Thus, the major challenge is the inherent inaccessibility of the Antarctic landscape: the only significant regions of Antarctica that are not now covered by ice are below present sea level. To overcome this challenge, we propose to employ an IODP mission-specific platform, specifically, a semiautonomous seabed drill suitable for short coring of crystalline bedrock in formerly glaciated and now submarine fjord bottoms. In the following sections: i) we explain why understanding Cenozoic glacial erosion in Antarctica is important; ii) we describe how we propose to develop this understanding; and iii) we outline criteria for a drilling program necessary to implement this strategy. 1. The when and how of Cenozoic glacial erosion: why is it important? Understanding how and when glacial landscapes form is broadly important for two reasons. First, formation of geomorphic features diagnostic of glaciation, e.g., cirques, U-shaped valleys, and landscapes of selective linear erosion (localized glacial troughs incised into an otherwise low-relief landscape; Sugden, 1978) requires the presence of glaciers.
    [Show full text]
  • Antarctic Peninsula Exhumation and Landscape Development Investigated by Low-Temperature Detrital Thermochronometry
    PROJECT DESCRIPTION: ANTARCTIC PENINSULA EXHUMATION AND LANDSCAPE DEVELOPMENT INVESTIGATED BY LOW-TEMPERATURE DETRITAL THERMOCHRONOMETRY I. Overview and introduction. We propose to apply methods of low-temperature thermochronometry based on the (U-Th)/He system in apatite to investigate the exhumation history, the development of the present topography, and the pattern of glacial erosion in the central Antarctic Peninsula. Recent studies have used this approach to study the dramatic, high-relief landscapes formed by Pleistocene alpine glaciation in temperate latitudes, for example in New Zealand, The Alps, British Columbia, Alaska and Patagonia (Shuster et al, 2011; Valla et al., 2011; Shuster et al., 2005; Thomson et al., 2010; Berger et al., 2008; Ehlers et al., 2006). This research has revealed not only when the glacial valleys in these landscapes formed -- which is important in understanding the relationship between Plio-Pleistocene climate change, landscape evolution, and tectonics -- but also provided new insights into the pattern and physical processes of glacial erosion. In this work, we aim to apply this approach to the similarly dramatic glacial landscape of the Antarctic Peninsula. The Antarctic Peninsula is broadly similar to alpine glacial landscapes formed in temperate latitudes during the Pleistocene in that the dominant landforms are deep, steep-sided glacial troughs. Because of the contrast in glacial history between Antarctica and temperate regions, however, we expect the timing and history of its formation to be very different. Specifically, the Antarctic Peninsula has most likely been glaciated since the Eocene (Anderson et al., 2011; Davies et al., 2012 and references therein), and Pleistocene cooling is hypothesized to have suppressed, rather than enhanced, glacial erosion by establishment of polar conditions (e.g., Rebesco et al., 2005).
    [Show full text]
  • UKNCAR Reporting Template Provide up to Two
    UKNCAR Reporting Template Provide up to two pages of information following the structure below, only filling out those sections where there is new information to report. 1. Principal UK Researchers Claire Allen (BAS); Mike Bentley (Durham); Alex Burton-Johnson (BAS); Julian Dowdeswell (SPRI); Tina van De Flierdt (Imperial); Jane Francis (BAS); Jenny Gales (Plymouth); Kate Hendry (Bristol); Sian Henley (Edinburgh); Javier Hernandez-Molina (RHUL); Claus-Dieter Hillenbrand (BAS); Jo Johnson (BAS); Rob Larter (BAS); Erin McLymont (Durham); Keir Nichols (Imperial); Vicky Peck (BAS); Tim van Peer (Southampton); Clive Oppenheimer (Cambridge); Teal Riley (BAS); Steve Roberts (BAS); Laura Robinson (Bristol); Dylan Rood (Imperial); Richard Sanders (NOCS); Daniela Schmidt (Bristol); John Smellie (Leicester); James Smith (BAS); Pippa Whitehouse (Durham); John Woodward (Northumbria). 2. Major activities and International Thwaites Glacier Collaboration (ITGC): progress since previous Following the first ITGC field season in Hudson Mountains year involving UK in 2019-20, Joanne Johnson (BAS) and John Woodward personnel/infrastructure (Northumbria), with support from Dylan Rood and Keir Nichols (Imperial), have been preparing rock samples for 10Be dating and processing radar data. The GHC team (co- led by Johnson) have chosen a site for subglacial bedrock recovery drilling in the Hudson Mountains, currently scheduled for the 2021-22 season (postponed from 2020- 21 due to covid). The GHC team have also constructed a Holocene relative sea-level curve for Pine Island Bay. ANiSEED project (NERC-funded): Joanne Johnson & Steve Roberts (BAS), Pippa Whitehouse (Durham) and Dylan Rood (Imperial) published a paper showing Holocene thinning of Pope Glacier, in the Amundsen Sea Embayment, which implies widespread early Holocene ice sheet thinning coinciding with enhanced upwelling of warm ocean water onto the continental shelf in this important area.
    [Show full text]
  • 2018-19 Science Planning Summary
    Cover Palmer Station graces the cover of this year's Science Planning Summary. March 2018 marked the fiftieth anniversary of this USAP station located on Anvers Island in the Antarctic Peninsula region. Shaun O'Boyle, an Antarctic Artists and Writers participant to both McMurdo Station (2015-16) and Palmer Station (2017-18), took the photo in October 2017. This Science Planning Summary was prepared by Leidos ASC under contract to the National Science Foundation Support Contract #NSFDACS1219442 2018 - 2019 Science Planning Summary United States Antarctic Program This Science Planning Summary is also available online via the USAP web site at www.usap.gov/sps or by scanning the QR code below with a smart phone or other mobile device. Table of Contents Planning and On-Ice Support Points of Contact . ii Science Event Numbering System . iii Station and Vessel Schedules . iv Staffed Field Camps . v Air Operations . vii Antarctic Astrophysics and Geospace Sciences. 1 Antarctic Organisms and Ecosystems. 30 Antarctic Integrated System Science . 55 Antarctic Instrumentation and Research Facilities . 77 Antarctic Earth Sciences . 80 Antarctic Glaciology. 93 Antarctic Ocean and Atmospheric Sciences . 101 Antarctic Technical Events . 114 Antarctic Artists and Writers. 126 Other Science Events. 131 Antarctic Education and Outreach . 135 Table of Contents to Indexes . 138 Principal Investigators (by Science Event Number) . 139 Principal Investigators (Alphabetical) . 143 Principal Investigators (by Institution) . 148 ARSV Laurence M. Gould Projects . 153 RV/IB Nathaniel B. Palmer Projects. 154 McMurdo Station Projects . 155 Palmer Station Projects . 158 South Pole Station Projects . 159 Projects Not Supported by a USAP Station or Vessel. 160 Antarctic Astrophysics and Geospace Sciences .
    [Show full text]
  • Making the Paper: Joanne Johnson
    AUTHORS Making the Paper: Joanne Johnson Exposed boulders on the harsh terrain of west Antarctica harbour a warning that the region’s glaciers could collapse. Joanne Johnson’s fi rst chance to explore of bedrock outcrops dotted with lumps the fastest-melting glaciers of the West of pinkish granite. She planned landing Antarctic Ice Sheet came unexpectedly, sites in advance, but “When you get there, nearly two years ahead of schedule. But it you look at it and you think, it’s too steep was also overdue. or too icy, we can’t land here — then Satellite data and ground-based you have to start making decisions,” measurements had raised alarms that she recalls. fast-fl owing glaciers near Pine Island Bay Having made it to the ground, they could disintegrate completely, raising fought winds that limited their ability to global sea levels by a metre. Yet Johnson, collect data, and sometimes even to stand whose work has now validated concerns upright. One area reached with diffi culty that the glaciers there are melting rapidly, had to be abandoned suddenly when was the fi rst to set foot on the region’s the wind changed and ice began to close rocky bluff s in four decades. in behind the waiting ship. Meanwhile, Th e trip represented not only a the metre-wide boulders whose surfaces challenge for Johnson, a geologist with Johnson expected to sample were nowhere the British Antarctic Survey (BAS), to be found. Instead, she scooped up six but a change in her scientifi c direction. football-sized substitutes.
    [Show full text]
  • Ice Survived the Lateglacial Interstadial in Scotland
    LICHENOMETRY ON ADELAIDE ISLAND, ANTARCTIC PENINSULA: SIZE-FREQUENCY STUDIES, GROWTH RATES AND SNOWPATCHES BY GOLLEDGE, N.R1,2, EVEREST, J.D.1, BRADWELL, T. 1 & JOHNSON, J.S.3 1British Geological Survey, Murchison House, Edinburgh, UK 2Antarctic Research Centre, Victoria University of Wellington, New Zealand 3British Antarctic Survey, Cambridge, UK Golledge, N.R., Everest, J.D., Bradwell, T. and Johnson, J.S., 2010: Lichenometry on Adelaide Island, Antarctic Peninsula: size-frequency studies, growth rates and snowpatches. Geogr. Ann., 92A: xx-xx. ABSTRACT This paper presents new lichenometric population data from the Antarctic Peninsula (67°S), and describes a new approach to lichen growth-rate calibration in locations where dated surfaces are extremely rare. We use historical aerial photography and field surveys to identify sites of former perennial snowpatches where lichen populations now exist. As an independent check on lichen mortality by snowkill, and the timing of snow patch disappearance, we use a positive-degree day (PDD) approach based on monthly climate data from Rothera Research Station. We find that maximum growth rates for lichens <40 mm in diameter on Adelaide Island are around 0.8 mm/yr. Furthermore, we propose that our combined methodology may be more widely applicable to the Polar regions where the construction of lichenometric dating (age-size) curves remains a problem. Key words: glaciation, snow patches, Rhizocarpon, positive degree day, photogrammetry Introduction Lichenometric dating is a valuable dating tool for geoscientists. The combination of extremely slow growth in certain species together with their common occurrence in widely ranging environments has been a key factor in most lichenometric dating studies.
    [Show full text]
  • Science Planning Summary 2019-20
    Cover The Phoenix Airfield at McMurdo Station appears on the cover of this year's Science Planning Summary. The photo captures a southbound C-17 landing behind the waiting Kress personnel carrier that will transport arriving scientists and support personnel to McMurdo Station. Photo by Colin M. Harnish, December 2018. The Science Planning Summary was prepared by Leidos ASC under contract to the National Science Foundation Support Contract #NSFDACS1219442 2019 - 2020 Science Planning Summary United States Antarctic Program This Science Planning Summary is subject to change based on project funding allocation, Antarctic operational considerations, and other factors. For the lat- est 2019-2020 information, please consult the online Science Planning Summary via the USAP web site at www.usap.gov/sps or by scanning the QR code below. Editor’s Note: To submit a comment about how to improve the Science Plan- ning Summary or to report an error, please email PlanningCoords.Sci- [email protected]. Table of Contents Planning and On-Ice Support Points of Contact . ii Science Event Numbering System . iii Station and Vessel Schedules . iv Staffed Field Camps. v Air Operations . viii Antarctic Astrophysics and Geospace Sciences. 1 Antarctic Organisms and Ecosystems . 27 Antarctic Integrated System Science. 45 Antarctic Instrumentation and Research Facilities. 66 Antarctic Earth Sciences . 70 Antarctic Glaciology . 79 Antarctic Ocean and Atmospheric Sciences . 86 Antarctic Technical Events . 101 Antarctic Artists and Writers . 116 Other Science Events . 121 Antarctic Education and Outreach. 129 Table of Contents to Indexes . 132 Principal Investigators (by Science Event Number) . 133 Principal Investigators (Alphabetical). 137 Principal Investigators (by Institution) . 141 ARSV Laurence M.
    [Show full text]
  • This Article Appeared in a Journal Published by Elsevier. the Attached
    (This is a sample cover image for this issue. The actual cover is not yet available at this time.) This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Quaternary Science Reviews 59 (2013) 101e111 Contents lists available at SciVerse ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Exposure-age record of Holocene ice sheet and ice shelf change in the northeast Antarctic Peninsula Greg Balco a,*, Joerg M. Schaefer b, LARISSA group1 a Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709, USA b Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9W, Palisades, NY 10964, USA article info abstract Article history: This paper describes glacialegeologic observations and cosmogenic-nuclide exposure ages from ice-free Received 13 March 2012 areas adjacent to the Sjögren, Boydell, and Drygalski Glaciers of the northeast Antarctic Peninsula. These Received in revised form provide a record of Holocene glacier and ice shelf change in this region. Early Holocene ice surface 12 October 2012 elevation near the present coastline was locally at least 500 m above present sea level, but our obser- Accepted 18 October 2012 vations do not constrain the maximum thickness of Last Glacial Maximum (LGM) ice or the time at which Available online it was attained.
    [Show full text]
  • Timing of the Northern Prince Gustav Ice Stream Retreat and the Deglaciation of Northern James Ross Island, Antarctic Peninsula
    Quaternary Research 82 (2014) 441–449 Contents lists available at ScienceDirect Quaternary Research journal homepage: www.elsevier.com/locate/yqres Timing of the Northern Prince Gustav Ice Stream retreat and the deglaciation of northern James Ross Island, Antarctic Peninsula during the last glacial–interglacial transition Daniel Nývlt a,b,⁎, Régis Braucher c,ZbyněkEngeld,e,Bedřich Mlčoch e, ASTER Team c,1 a Department of Geography, Faculty of Science, Masaryk University, Kotlářská 2, 611 37 Brno, Czechia b Czech Geological Survey, Brno branch, Leitnerova 22, 658 69 Brno, Czechia c Aix-Marseille Université, CNRS-IRD-Collège de France, UM 34 CEREGE, Technopôle de l'Arbois, BP80, 13545 Aix-en-Provence, France d Faculty of Science, Charles University in Prague, Albertov 6, 128 43 Praha, Czechia e Czech Geological Survey, Klárov 3, 118 21 Praha, Czechia article info abstract Article history: The Northern Prince Gustav Ice Stream located in Prince Gustav Channel, drained the northeastern portion of the Received 13 September 2013 Antarctic Peninsula Ice Sheet during the last glacial maximum. Here we present a chronology of its retreat based Available online 27 June 2014 on in situ produced cosmogenic 10Be from erratic boulders at Cape Lachman, northern James Ross Island. Schmidt hammer testing was adopted to assess the weathering state of erratic boulders in order to better interpret excess Keywords: cosmogenic 10Be from cumulative periods of pre-exposure or earlier release from the glacier. The weighted mean Northern Prince Gustav Ice Stream exposure age of five boulders based on Schmidt hammer data is 12.9 ± 1.2 ka representing the beginning of the Antarctic Peninsula Ice Sheet b Be-10 exposure dating deglaciation of lower-lying areas ( 60 m a.s.l.) of the northern James Ross Island, when Northern Prince Gustav Schmidt hammer testing Ice Stream split from the remaining James Ross Island ice cover.
    [Show full text]
  • Jörg M. Schäfer
    JÖRG M. SCHÄFER LAMONT-DOHERTY EARTH OBSERVATORY • THE EARTH INSTITUTE AT COLUMBIA UNIVERSITY ROUTE 9W • PALISADES, NY 10964 • USA PHONE: 1 845 365 8756 • FAX: 1 845 365 8155 • EMAIL: [email protected] Personal Born 1968 in Stuttgart, Germany Citizenship: German Language: german, english, french 90 Morningside Drive • Apt. 2G New York • NY-10027 Education Adjunct Associate Professor Dept. of Earth and Environmental Sciences, Columbia University Lamont Research Professor Lamont-Doherty Earth Observatory of Columbia University Doherty Associate Research Scientist (September 2003-November 2008) Lamont-Doherty Earth Observatory of Columbia University Postdoctoral Research Fellow (January 2001-August 2003) Lamont-Doherty Earth Observatory of Columbia University Postdoctoral Researcher (February 2000-October 2000) Dept. of Earth Sciences, Swiss Federal Institute of Technology (ETH) Zürich Ph.D. (March 1996-June 2000) Swiss Federal Institute of Technology (ETH) Zürich. Dissertation: Reconstruction of landscape evolution and continental paleoglaciations using in-situ cosmogenic nuclides. Jointly supervised by Profs. R. Wieler, C. Schlüchter, A.N. Halliday at the Department of Earth Sciences, ETH Zürich Masters Degree (“Diplom”) in Physics (1995) Institute of Environmental Physics, University of Heidelberg, Germany. Reconstruction of bio-geochemical trace substance cycles from an alpine ice- core. Supervisors: Dr. D. Wagenbach, Prof. U. Platt. Exchange student • ERASMUS program (1991-92) Department of Physics, University of Aix- Marseille
    [Show full text]
  • THWAITES WILD CARD This Unstable Glacier—With Its Potentially Disastrous Effect on Sea Levels—Is Starting to Show Its Hand
    VOL. 101 | NO. 3 Ancient Assyrian Aurorae MARCH 2020 A Ski Resort Report New AGU Medalists THE THWAITES WILD CARD This unstable glacier—with its potentially disastrous effect on sea levels—is starting to show its hand. FROM THE EDITOR Editor in Chief Heather Goss, AGU, Washington, D.C., USA; [email protected] Editorial Manager, News and Features Editor Caryl-Sue Micalizio The Threat at Thwaites Science Editor Timothy Oleson Senior News Writer Randy Showstack News Writer and Production Associate Kimberly M. S. Cartier he best—or at least most entertaining—thing I learned News and Production Fellow Jenessa Duncombe from this issue is that glaciers tend to behave “like Production & Design pancake batter on a frying pan.” Ted Scambos offers T Manager, Production and Operations Faith A. Ishii that description in this month’s cover story, “Diagnosing Senior Production Specialist Melissa A. Tribur Thwaites” (page 18). Editorial and Production Coordinator Liz Castenson Scambos is the lead scientific coordinator for the U.S. side Assistant Director, Design & Branding Beth Bagley of the International Thwaites Glacier Collaboration (ITGC). Senior Graphic Designer Valerie Friedman Graphic Designer J. Henry Pereira Launched in 2018, this large research initiative hosts eight teams studying the past, present, and future of Thwaites, one Marketing of Antarctica’s most unstable glaciers. The problem with Director, Marketing, Branding & Advertising Jessica Latterman Thwaites, and the West Antarctic region generally, is that it’s Assistant Director, Marketing & Advertising Liz Zipse Marketing Program Manager like pancake batter sliding around in too much oil—as it loses Angelo Bouselli Senior Specialist, Digital Marketing Nathaniel Janick mass from both above and below, ocean water is creeping in Digital Marketing Coordinator Ashwini Yelamanchili underneath and reducing the friction between the ice and the bedrock, allowing it to slide freely over the water.
    [Show full text]