Chilean Antarctic Science Program and Related Activities
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Detrital Zircon Geochronology of Palaeozoic Siliciclastic Rocks from the Ellsworth Mountains, West Antarctica
O EOL GIC G A D D A E D C E I H C I L E O S F u n 2 d 6 la serena octubre 2015 ada en 19 Detrital zircon geochronology of Palaeozoic siliciclastic rocks from the Ellsworth Mountains, West Antarctica Paula Castillo* and C. Mark Fanning Research School of Earth Sciences, The Australian National University, Canberra, Australia. Rodrigo Fernández University of Texas Institute for Geophysics, The University of Texas at Austin, Austin, Texas, USA. Fernando Poblete Geosciences Rennes, Université de Rennes 1, Rennes, France. Departamento de Geología, Universidad de Chile, Santiago, Chile. *Contact email: [email protected] Abstract. In the Ellsworth Mountains there is an extensive record of sedimentation from early Cambrian to Permian times. However, the tectonic history and the palaeogeographic significance remain enigmatic. Nine sandstone samples were analysed for their U-Pb detrital zircon age spectra using SHRIMPII and RG. They belong to the early Cambrian to Carboniferous-Permian sequences and record typical Gondwana margin signatures. Variations up section/sequence in zircon provenance suggest restricted basinal deposition during the Cambrian,! with likely sources in the Namaqua-Natal and Mozambique/Maud Belts. There are little or no contributions from older cratons and so the Ellsworth basin evolved as a separate basin to that in the Transantarctic Mountains.! This basin configuration changed after the Devonian and deposition continued Figure 1. Reconstruction of part of Gondwana at ca. 500 Ma. during the late Palaeozoic, when the Ellsworth Mountains South America: SFC - Sao Francisco craton; PPC - basin only received detritus from the Ross/Pan-African Paranapanema craton; RPC - Río de la Plata craton. -
Fig. Ap. 2.1. Denton Tending His Fairy Shrimp Collection
Fig. Ap. 2.1. Denton tending his fairy shrimp collection. 176 Appendix 1 Hatching and Rearing Back in the bowels of this book we noted that However, salts may leach from soils to ultimately if one takes dry soil samples from a pool basin, make the water salty, a situation which commonly preferably at its deepest point, one can then "just turns off hatching. Tap water is usually unsatis- add water and stir". In a day or two nauplii ap- factory, either because it has high TDS, or because pear if their cysts are present. O.K., so they won't it contains chlorine or chloramine, disinfectants always appear, but you get the idea. which may inhibit hatching or kill emerging If your desire is to hatch and rear fairy nauplii. shrimps the hi-tech way, you should get some As you have read time and again in Chapter 5, guidance from Brendonck et al. (1990) and temperature is an important environmental cue for Maeda-Martinez et al. (1995c). If you merely coaxing larvae from their dormant state. You can want to see what an anostracan is like, buy some guess what temperatures might need to be ap- Artemia cysts at the local aquarium shop and fol- proximated given the sample's origin. Try incu- low directions on the container. Should you wish bation at about 3-5°C if it came from the moun- to find out what's in your favorite pool, or gather tains or high desert. If from California grass- together sufficient animals for a study of behavior lands, 10° is a good level at which to start. -
Review of the Geology and Paleontology of the Ellsworth Mountains, Antarctica
U.S. Geological Survey and The National Academies; USGS OF-2007-1047, Short Research Paper 107; doi:10.3133/of2007-1047.srp107 Review of the geology and paleontology of the Ellsworth Mountains, Antarctica G.F. Webers¹ and J.F. Splettstoesser² ¹Department of Geology, Macalester College, St. Paul, MN 55108, USA ([email protected]) ²P.O. Box 515, Waconia, MN 55387, USA ([email protected]) Abstract The geology of the Ellsworth Mountains has become known in detail only within the past 40-45 years, and the wealth of paleontologic information within the past 25 years. The mountains are an anomaly, structurally speaking, occurring at right angles to the Transantarctic Mountains, implying a crustal plate rotation to reach the present location. Paleontologic affinities with other parts of Gondwanaland are evident, with nearly 150 fossil species ranging in age from Early Cambrian to Permian, with the majority from the Heritage Range. Trilobites and mollusks comprise most of the fauna discovered and identified, including many new genera and species. A Glossopteris flora of Permian age provides a comparison with other Gondwana floras of similar age. The quartzitic rocks that form much of the Sentinel Range have been sculpted by glacial erosion into spectacular alpine topography, resulting in eight of the highest peaks in Antarctica. Citation: Webers, G.F., and J.F. Splettstoesser (2007), Review of the geology and paleontology of the Ellsworth Mountains, Antarctica, in Antarctica: A Keystone in a Changing World – Online Proceedings of the 10th ISAES, edited by A.K. Cooper and C.R. Raymond et al., USGS Open- File Report 2007-1047, Short Research Paper 107, 5 p.; doi:10.3133/of2007-1047.srp107 Introduction The Ellsworth Mountains are located in West Antarctica (Figure 1) with dimensions of approximately 350 km long and 80 km wide. -
Final Report of the Thirty-Second Antarctic Treaty Consultative Meeting
Final Report of the Thirty-second Antarctic Treaty Consultative Meeting ANTARCTIC TREATY CONSULTATIVE MEETING Final Report of the Thirty-second Antarctic Treaty Consultative Meeting Baltimore, United States 6–17 April 2009 Secretariat of the Antarctic Treaty Buenos Aires 2009 Antarctic Treaty Consultative Meeting (32nd : 2009 : Baltimore) Final Report of the Thirtieth Antarctic Treaty Consultative Meeting. Baltimore, United States, 6–17 April 2009. Buenos Aires : Secretariat of the Antarctic Treaty, 2009. 292 p. ISBN 978-987-1515-08-0 1. International law – Environmental issues. 2. Antarctic Treaty system. 3. Environmental law – Antarctica. 4. Environmental protection – Antarctica. DDC 341.762 5 ISBN 978-987-1515-08-0 Contents VOLUME 1 (in hardcopy and CD) Acronyms and Abbreviations 11 PART I. FINAL REPORT 13 1. Final Report 15 2. CEP XII Report 85 3. Appendices 159 Declaration on the 50th Anniversary of the Antarctic Treaty 161 Declaration on the International Polar Year and Polar Science 163 Preliminary Agenda for ATCM XXXIII 165 PART II. MEASURES, DECISIONS AND RESOLUTIONS 167 1. Measures 169 Measure 1 (2009): ASMA No 3 – Cape Denison, Commonwealth Bay, George V Land, East Antarctica 171 Measure 2 (2009): ASMA No 7 – South-west Anvers Island and Palmer Basin 173 Measure 3 (2009): ASPA No 104 – Sabrina Island, Balleny Islands 175 Measure 4 (2009): ASPA No 113 – Litchfi eld Island, Arthur Harbour, Anvers Island, Palmer Archipelago 177 Measure 5 (2009): ASPA No 121 – Cape Royds, Ross Island 179 Measure 6 (2009): ASPA No 125 – Fildes Peninsula, -
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. -
Visualizing the Quality of Scientific Production
Research Journal of Applied Sciences, Engineering and Technology 10(12): 1435-1440, 2015 DOI: 10.19026/rjaset.10.1845 ISSN: 2040-7459; e-ISSN: 2040-7467 © 2015 Maxwell Scientific Publication Corp. Submitted: April 17, 2015 Accepted: May 10, 2015 Published: August 25, 2015 Research Article Sweet Spots for Manuscripts: Visualizing the Quality of Scientific Production 1Patricio Ramírez-Correa, 2Jorge Alfaro-Pérez, 3F. Javier Rondan-Cataluña and 3Jorge Arenas-Gaitán 1Escuela de Ciencias Empresariales, 2Escuela de Ingeniería, Universidad Católica del Norte, Chile 3Departamento de Administración de Empresas y Marketing, Universidad de Sevilla, España Abstract: This study presents a visual approach to analyze scientific activity in indexed journals based on bibliometric indicators. The result of this analysis approach supports the process of choosing a journal to submit a manuscript, especially in knowledge domains where the author, whether novice or not, has failed to follow in detail the evolution of the domain. Moreover, the same approach can be used to an overall assessment of the production of researchers, research groups, institutions and countries. The conceptual foundations of the approach are volume and citation indicators of scientific journals articles. In particular, the proposed approach is based on SCImago Journal Rank index, the h-index and the annual number of articles published. The above indicators are transformed into percentiles and then displayed on a graph, integrating in this diagram the set of articles to be analyzed. The analysis approach was implemented in Sweet Spots for Manuscripts, online software based on open source components. As an example of its potential, an analysis of the 2014 research activity of the institutions belonging to the Council of Rectors of Chilean Universities is presented. -
South America Cryonet Meeting, 27-29 October 2014, Santiago De
TECHNICAL REPORT No. 2013- xx Insert title of report ....... WORLD METEOROLOGICAL ORGANIZATION GLOBAL CRYOSPHERE WATCH REPORT No. 8 CryoNet South America Workshop First Session Santiago de Chile, Chile 27-29 October 2014 © World Meteorological Organization, 2014 The right of publication in print, electronic and any other form and in any language is reserved by WMO. Short extracts from WMO publications may be reproduced without authorization, provided that the complete source is clearly indicated. Editorial correspondence and requests to publish, reproduce or translate this publication in part or in whole should be addressed to: Chair, Publications Board World Meteorological Organization (WMO) 7 bis, avenue de la Paix Tel.: +41 (0) 22 730 8403 P.O. Box 2300 Fax: +41 (0) 22 730 8040 CH-1211 Geneva 2, Switzerland E-mail: [email protected] NOTE The designations employed in WMO publications and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of WMO concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products does not imply that they are endorsed or recommended by WMO in preference to others of a similar nature which are not mentioned or advertised. The findings, interpretations and conclusions expressed in WMO publications with named authors are those of the authors alone and do not necessarily reflect those of WMO or its Members. FINAL -
Ch. 3. Ecology of Fairy Shrimps Life Stage and Species (Mertens Et Al
Ch. 3. Ecology of fairy shrimps life stage and species (Mertens et al. 1991). As face of the fused 12th and 13th segments of the appendages return forward from a beat, a low thorax (Fig. 1.2, p. 2). Yes, you read correctly, pressure is created between them causing water to males actually have two penes. Each lateral testis flow in (be "sucked" in) with its dead particles, empties through only the penis on its side of the and living organisms too if they are unable to body. swim against the flow. When the phyllopodia In females, oviducts extend from the ovaries beat once more, whether in graceful swimming or and enlarge at their distal ends into what are bottom scraping, increased pressure forces water called lateral pouches. These join one even through the setal meshwork and particles too large larger structure called an ovisac which also re- to pass through its pores are sieved out, whether ceives ducts from several shell glands. The living or dead, plant, animal, or mineral, nutri- ovisac expands within the brood pouch which is a tious or not. These particles are moved to a food centrally placed and posteriorly directed protru- groove between the bases of the phyllopodia, then sion from the ventral body wall of the fused geni- passed along to the jaws and mouth by specialized tal segments (Fig. 1.3, p. 3). The opening of the spiny lobes at the base of each appendage. For an ovisac to the outside is the female's genital pore, excellent discussion of anostracan feeding mech- the site that male sexual behavior is aimed at en- anisms, see Fryer (1983). -
Download Factsheet
Antarctic Factsheet Geographical Statistics May 2005 AREA % of total Antarctica - including ice shelves and islands 13,829,430km2 100.00% (Around 58 times the size of the UK, or 1.4 times the size of the USA) Antarctica - excluding ice shelves and islands 12,272,800km2 88.74% Area ice free 44,890km2 0.32% Ross Ice Shelf 510,680km2 3.69% Ronne-Filchner Ice Shelf 439,920km2 3.18% LENGTH Antarctic Peninsula 1,339km Transantarctic Mountains 3,300km Coastline* TOTAL 45,317km 100.00% * Note: coastlines are fractal in nature, so any Ice shelves 18,877km 42.00% measurement of them is dependant upon the scale at which the data is collected. Coastline Rock 5,468km 12.00% lengths here are calculated from the most Ice coastline 20,972km 46.00% detailed information available. HEIGHT Mean height of Antarctica - including ice shelves 1,958m Mean height of Antarctica - excluding ice shelves 2,194m Modal height excluding ice shelves 3,090m Highest Mountains 1. Mt Vinson (Ellsworth Mts.) 4,892m 2. Mt Tyree (Ellsworth Mts.) 4,852m 3. Mt Shinn (Ellsworth Mts.) 4,661m 4. Mt Craddock (Ellsworth Mts.) 4,650m 5. Mt Gardner (Ellsworth Mts.) 4,587m 6. Mt Kirkpatrick (Queen Alexandra Range) 4,528m 7. Mt Elizabeth (Queen Alexandra Range) 4,480m 8. Mt Epperly (Ellsworth Mts) 4,359m 9. Mt Markham (Queen Elizabeth Range) 4,350m 10. Mt Bell (Queen Alexandra Range) 4,303m (In many case these heights are based on survey of variable accuracy) Nunatak on the Antarctic Peninsula 1/4 www.antarctica.ac.uk Antarctic Factsheet Geographical Statistics May 2005 Other Notable Mountains 1. -
Glaciological Investigations on Union Glacier, Ellsworth Mountains, West Antarctica
Annals of Glaciology 51(55) 2010 91 Glaciological investigations on Union Glacier, Ellsworth Mountains, West Antarctica Andre´s RIVERA,1,2,3 R. ZAMORA,1 Camilo RADA,1 Jonathan WALTON,4 Stuart PROCTOR5 1Centro de Estudios Cientı´ficos, Av. Arturo Prat 514, Casilla 1469, Valdivia, Chile E-mail: [email protected] 2Departamento de Geografı´a, Universidad de Chile, Portugal 84, Casilla 3387, Santiago, Chile 3Centro de la Ingenierı´a de la Innovacio´n del CECS (CIN), Av. Arturo Prat 514, Casilla 1469, Valdivia, Chile 4Antarctic Logistics and Expeditions (ALE), LLC 4376 South 700 East, Suite 226 Salt Lake City, UT 84107-3006, USA 5Topcon Europe Positioning B.V., Essebaan 11, Capelle aan den IJssel, 2908LJ, The Netherlands ABSTRACT. Union Glacier, West Antarctica, was intensively mapped in December 2008, when an over- snow traverse was conducted by CECS and ALE, with the aim to determine the ice-dynamical characteristics of the glacier, through mapping the crevasse fields and by providing a glaciological baseline for future studies. A mean ice thickness of 1450 m was measured, confirming the presence of a deep subglacial topography (~900 m below sea level), much deeper than previously estimated. Ice velocities were also measured at 21 stakes drilled into the ice at the narrowest gate of the glacier between December 2007 and December 2008, yielding a mean value of 22.6 m a–1. These velocities, combined with the measured ice thicknesses and a numerical model, yielded an ice flux of 0.10 Æ 0.03 km3 a–1 w.e. Considering the ice basin above this gate, a mean surface mass balance of 0.18 Æ 0.05 m a–1 was estimated, a value consistent with a mean snow accumulation for nearby ice streams. -
Mem170-Bm.Pdf by Guest on 30 September 2021 452 Index
Index [Italic page numbers indicate major references] acacamite, 437 anticlines, 21, 385 Bathyholcus sp., 135, 136, 137, 150 Acanthagnostus, 108 anticlinorium, 33, 377, 385, 396 Bathyuriscus, 113 accretion, 371 Antispira, 201 manchuriensis, 110 Acmarhachis sp., 133 apatite, 74, 298 Battus sp., 105, 107 Acrotretidae, 252 Aphelaspidinae, 140, 142 Bavaria, 72 actinolite, 13, 298, 299, 335, 336, 339, aphelaspidinids, 130 Beacon Supergroup, 33 346 Aphelaspis sp., 128, 130, 131, 132, Beardmore Glacier, 429 Actinopteris bengalensis, 288 140, 141, 142, 144, 145, 155, 168 beaverite, 440 Africa, southern, 52, 63, 72, 77, 402 Apoptopegma, 206, 207 bedrock, 4, 58, 296, 412, 416, 422, aggregates, 12, 342 craddocki sp., 185, 186, 206, 207, 429, 434, 440 Agnostidae, 104, 105, 109, 116, 122, 208, 210, 244 Bellingsella, 255 131, 132, 133 Appalachian Basin, 71 Bergeronites sp., 112 Angostinae, 130 Appalachian Province, 276 Bicyathus, 281 Agnostoidea, 105 Appalachian metamorphic belt, 343 Billingsella sp., 255, 256, 264 Agnostus, 131 aragonite, 438 Billingsia saratogensis, 201 cyclopyge, 133 Arberiella, 288 Bingham Peak, 86, 129, 185, 190, 194, e genus, 105 Archaeocyathidae, 5, 14, 86, 89, 104, 195, 204, 205, 244 nudus marginata, 105 128, 249, 257, 281 biogeography, 275 parvifrons, 106 Archaeocyathinae, 258 biomicrite, 13, 18 pisiformis, 131, 141 Archaeocyathus, 279, 280, 281, 283 biosparite, 18, 86 pisiformis obesus, 131 Archaeogastropoda, 199 biostratigraphy, 130, 275 punctuosus, 107 Archaeopharetra sp., 281 biotite, 14, 74, 300, 347 repandus, 108 Archaeophialia, -
1 Compiled by Mike Wing New Zealand Antarctic Society (Inc
ANTARCTIC 1 Compiled by Mike Wing US bulldozer, 1: 202, 340, 12: 54, New Zealand Antarctic Society (Inc) ACECRC, see Antarctic Climate & Ecosystems Cooperation Research Centre Volume 1-26: June 2009 Acevedo, Capitan. A.O. 4: 36, Ackerman, Piers, 21: 16, Vessel names are shown viz: “Aconcagua” Ackroyd, Lieut. F: 1: 307, All book reviews are shown under ‘Book Reviews’ Ackroyd-Kelly, J. W., 10: 279, All Universities are shown under ‘Universities’ “Aconcagua”, 1: 261 Aircraft types appear under Aircraft. Acta Palaeontolegica Polonica, 25: 64, Obituaries & Tributes are shown under 'Obituaries', ACZP, see Antarctic Convergence Zone Project see also individual names. Adam, Dieter, 13: 6, 287, Adam, Dr James, 1: 227, 241, 280, Vol 20 page numbers 27-36 are shared by both Adams, Chris, 11: 198, 274, 12: 331, 396, double issues 1&2 and 3&4. Those in double issue Adams, Dieter, 12: 294, 3&4 are marked accordingly. Adams, Ian, 1: 71, 99, 167, 229, 263, 330, 2: 23, Adams, J.B., 26: 22, Adams, Lt. R.D., 2: 127, 159, 208, Adams, Sir Jameson Obituary, 3: 76, A Adams Cape, 1: 248, Adams Glacier, 2: 425, Adams Island, 4: 201, 302, “101 In Sung”, f/v, 21: 36, Adamson, R.G. 3: 474-45, 4: 6, 62, 116, 166, 224, ‘A’ Hut restorations, 12: 175, 220, 25: 16, 277, Aaron, Edwin, 11: 55, Adare, Cape - see Hallett Station Abbiss, Jane, 20: 8, Addison, Vicki, 24: 33, Aboa Station, (Finland) 12: 227, 13: 114, Adelaide Island (Base T), see Bases F.I.D.S. Abbott, Dr N.D.