In Situ Nitrogen(C2h2)-Fixation in Lakes Of
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Ice Caves of Terra Nova Bay (Victoria Land, Antarctica)
SPECIALE GLACIER CAVES NIMBUS 23-24 Ice Caves of Terra Nova Bay (Victoria Land, Antarctica) Mirco Meneghel - Dipartimento di Geografia, University of Padova, Italy Giovanni Badino - Dipartimento di Fisica Generale, University of Torino, Italy Associazione La Venta Abstract Baia Terra Nova, sulla costa occi- wider Terra Nova Bay, on the we- In the 2000/2001 expedition of dentale del Mare di Ross. Sono stern coast of the Ross Sea, at 74° the Italian Programme of Resear- state esplorate tre grotte nella 41' 42" S lat. and 164° 07' 23" E ch in Antarctica (PNRA) an inve- fronte dei ghiacciai al contatto col long. The Transantarctic Mts, stigation on the presence of ca- mare e un'altra sulla sommità del whose relief is often higher than ves in ice has been carried out monte Melbourne, un cono vulca- 3000 m, fringe the coast. South near the Italian Station of Terra nico di 2700 metri di altezza. Le of the Base the mountain chaine Nova Bay, on the western coast of grotte sulla costa sono crepacci is crossed by outlet glaciers that the Ross Sea (Northern Victoria ampliati dalla sublimazione del drain the ice of the inlandsis. On Land). Three caves have been ex- ghiaccio a causa della differenza the north huge valley glaciers plored at the snout of glaciers di temperatura fra il ghiaccio e flow from the mountains to the reaching the sea and an other l'acqua marina. La grotta subgla- sea. The Italian Base is placed one on the summit of Mt Mel- ciale sul monte Melbourne è ge- between the region of the Dry bourne, a volcanic cone 2700 m nerata dal calore delle rocce vul- Valleys to the south, where broad 1 - Below - high. -
Federal Register/Vol. 84, No. 78/Tuesday, April 23, 2019/Rules
Federal Register / Vol. 84, No. 78 / Tuesday, April 23, 2019 / Rules and Regulations 16791 U.S.C. 3501 et seq., nor does it require Agricultural commodities, Pesticides SUPPLEMENTARY INFORMATION: The any special considerations under and pests, Reporting and recordkeeping Antarctic Conservation Act of 1978, as Executive Order 12898, entitled requirements. amended (‘‘ACA’’) (16 U.S.C. 2401, et ‘‘Federal Actions to Address Dated: April 12, 2019. seq.) implements the Protocol on Environmental Justice in Minority Environmental Protection to the Richard P. Keigwin, Jr., Populations and Low-Income Antarctic Treaty (‘‘the Protocol’’). Populations’’ (59 FR 7629, February 16, Director, Office of Pesticide Programs. Annex V contains provisions for the 1994). Therefore, 40 CFR chapter I is protection of specially designated areas Since tolerances and exemptions that amended as follows: specially managed areas and historic are established on the basis of a petition sites and monuments. Section 2405 of under FFDCA section 408(d), such as PART 180—[AMENDED] title 16 of the ACA directs the Director the tolerance exemption in this action, of the National Science Foundation to ■ do not require the issuance of a 1. The authority citation for part 180 issue such regulations as are necessary proposed rule, the requirements of the continues to read as follows: and appropriate to implement Annex V Regulatory Flexibility Act (5 U.S.C. 601 Authority: 21 U.S.C. 321(q), 346a and 371. to the Protocol. et seq.) do not apply. ■ 2. Add § 180.1365 to subpart D to read The Antarctic Treaty Parties, which This action directly regulates growers, as follows: includes the United States, periodically food processors, food handlers, and food adopt measures to establish, consolidate retailers, not States or tribes. -
Fault Kinematic Studies in the Transantarctic Mountains, Southern Victoria Land TERRY J
studies. Together these data will be used to develop a model to plate tectonic modeling. In R.A. Hodgson, S.P. Gay, Jr., and J.Y. of the structural architecture and motion history associated Benjamins (Eds.), Proceedings of the First International Conference with the Transantarctic Mountains in southern Victoria Land. on the New Basement Tectonics (Publication number 5). Utah Geo- logical Association. We thank Jane Ferrigno for cooperation and advice on Lucchita, B.K., J. Bowell, K.L. Edwards, E.M. Eliason, and H.M. Fergu- image selection; John Snowden, David Cunningham, and son. 1987. Multispectral Landsat images of Antarctica (U.S. Geo- Tracy Douglass at the Ohio State University Center for Map- logical Survey bulletin 1696). Washington, D.C.: U.S. Government ping for help with computer processing; and Carolyn Merry, Printing Office. Gary Murdock, and Ralph von Frese for helpful discussions Wilson, T.J. 1992. Mesozoic and Cenozoic kinematic evolution of the Transantarctic Mountains. In Y. Yoshida, K. Kaminuma, and K. concerning image analysis. This research was supported by Shiraishi (Eds.), Recent progress in antarctic earth science. Tokyo: National Science Foundation grant OPP 90-18055 and by the Terra Scientific. Byrd Polar Research Center of Ohio State University. Wilson, T.J. 1993. Jurassic faulting and magmatism in the Transantarctic Mountains: Implication for Gondwana breakup. In R.H. Findlay, M.R. Banks, R. Unrug, and J. Veevers (Eds.), Gond- References wana 8—Assembly, evolution, and dispersal. Rotterdam: A.A. Balkema. Wilson, T.J., P. Braddock, R.J. Janosy, and R.J. Elliot. 1993. Fault kine- Isachsen, Y.W. 1974. -
Terra Nova Bay, Ross Sea
MEASURE 14 - ANNEX Management Plan for Antarctic Specially Protected Area No 161 TERRA NOVA BAY, ROSS SEA 1. Description values to be protected A coastal marine area encompassing 29.4km2 between Adélie Cove and Tethys Bay, Terra Nova Bay, is proposed as an Antarctic Specially Protected Area (ASPA) by Italy on the grounds that it is an important littoral area for well-established and long-term scientific investigations. The Area is confined to a narrow strip of waters extending approximately 9.4km in length immediately to the south of the Mario Zucchelli Station (MZS) and up to a maximum of 7km from the shore. No marine resource harvesting has been, is currently, or is planned to be, conducted within the Area, nor in the immediate surrounding vicinity. The site typically remains ice-free in summer, which is rare for coastal areas in the Ross Sea region, making it an ideal and accessible site for research into the near-shore benthic communities of the region. Extensive marine ecological research has been carried out at Terra Nova Bay since 1986/87, contributing substantially to our understanding of these communities which had not previously been well-described. High diversity at both species and community levels make this Area of high ecological and scientific value. Studies have revealed a complex array of species assemblages, often co-existing in mosaics (Cattaneo-Vietti, 1991; Sarà et al., 1992; Cattaneo-Vietti et al., 1997; 2000b; 2000c; Gambi et al., 1997; Cantone et al., 2000). There exist assemblages with high species richness and complex functioning, such as the sponge and anthozoan communities, alongside loosely structured, low diversity assemblages. -
Downloaded 10/01/21 04:29 PM UTC 224 MONTHLY WEATHER REVIEW
APRIL, 1914. MONTHLY WEATHER REWW. 223 of no direct consequence to lants, its importance being ordinary weather stations. Therefore it would be of urely meteorological, the reP ative huniiclit affects them great advantage to students of plant life if such deter- Zirectly, since it so largely determines t i! e amount of minations could be made at agricultural and forest exper- transpiration. The monthly , mean relative humidity iment stations.' and its minimum, and particularly the average relative Sunshine. humidity with its minimum during periods of different wind direction, are things important to know. In local- Light is another important factor in t-he development ities with a humid climate and wit,hout n, distinct hot of plants. The amount avdable for plants in a given eriod, where fogs are frequent, observations upon the 1oc.alit-y depends upon cloudiness and geographic lati- fatter should, of course, Gve all the information as to tude. For this reason, the avera. e monthly cloudi- humidit of the air necessary for the purposes of botanical ness, tjhe average cloudiness for win as of different direc- geograpE y.a tions, and the number of clear, semicloudy, and cloudy Precipitation. days should be computed. Some simple sunshine record, especially for winds of different directions, is The important part which precipitation, especially also necessary. The occurrence of days with sunshine total precipitation, plays in plant life, needs no discussion. should be given in per cent of the total number of obser- The maximum precipitation for any day during the month va tions. and the number of da s of precipitation are also inipor- Bammetric pressure. -
Ice-Sheet Flow in the Vicinity of Southern Victoria Land, Antarctica: Implications for Glacial Chronology
ABSTRACTS OF PAPERS PRESENTED ICE-SHEET FLOW IN THE VICINITY OF SOUTHERN VICTORIA LAND, ANTARCTICA: IMPLICATIONS FOR GLACIAL CHRONOLOGY By DAVID J. DREWRY (Scott Polar Research Institute, Lensfield Road, Cambridge CB2 IER, England) ABSTRACT. Systematic radio echo-sounding during three seasons since 1971-72 has produced data on the configuration of the ice sheet in East Antarctica. In the sector extending inland from southern Victoria Land, the ice sheet exhibits a large ridge which drives ice towards David Glacier in the north and Mulock and Byrd Glaciers to the south. Within 100 km of the McMurdo dry-valley region soundings along ten sub-parallel lines (c. 10 km apart) provides detail on ice surface and flow patterns at the ridge tip. A small surface dome lies just inland of Taylor Glacier. The surface drops by 100 m or more before rising to join the major ridge in East Antarctica. Only Mawson and Mulock Glaciers in this area currently discharge any ice from central East Antarctica. The small outlet glaciers including Taylor, Wright Upper, and Victoria Upper are nourished by local ice originating within a few tens of kilometres of the exposed Transantarctic Mountains. Oxygen and deuterium isotope determinations on samples taken from Taylor Glacier snout in January 1978 corroborate this hypothesis of a nearby source. 0180 values between -38 and -41%0 are isotopically much heavier than we would anticipate for ice derived from central East Antarctic ic~ sheets (-45 to -55%0). Minimum o-values for Taylor Glacier, predicted from elevation- temperature considerations close to the local ice divide based on a measured mean annual surface temperature of - 41 .S oC are in the order of -42 to -43%0. -
The Transantarctic Mountains These Watercolor Paintings by Dee Molenaar Were Originally Published in 1985 with His Map of the Mcmurdo Sound Area of Antarctica
The Transantarctic Mountains These watercolor paintings by Dee Molenaar were originally published in 1985 with his map of the McMurdo Sound area of Antarctica. We are pleased to republish these paintings with the permission of the artist who owns the copyright. Gunter Faure · Teresa M. Mensing The Transantarctic Mountains Rocks, Ice, Meteorites and Water Gunter Faure Teresa M. Mensing The Ohio State University The Ohio State University School of Earth Sciences School of Earth Sciences and Byrd Polar Research Center and Byrd Polar Research Center 275 Mendenhall Laboratory 1465 Mt. Vernon Ave. 125 South Oval Mall Marion, Ohio 43302 Columbus, Ohio 43210 USA USA [email protected] [email protected] ISBN 978-1-4020-8406-5 e-ISBN 978-90-481-9390-5 DOI 10.1007/978-90-481-9390-5 Springer Dordrecht Heidelberg London New York Library of Congress Control Number: 2010931610 © Springer Science+Business Media B.V. 2010 No part of this work may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, microfilming, recording or otherwise, without written permission from the Publisher, with the exception of any material supplied specifically for the purpose of being entered and executed on a computer system, for exclusive use by the purchaser of the work. Cover illustration: A tent camp in the Mesa Range of northern Victoria Land at the foot of Mt. Masley. Printed on acid-free paper Springer is part of Springer Science+Business Media (www.springer.com) We dedicate this book to Lois M. Jones, Eileen McSaveny, Terry Tickhill, and Kay Lindsay who were the first team of women to conduct fieldwork in the Transantarctic Mountains during the 1969/1970 field season. -
Draft Comprehensive Environmental Evaluation
Proposed Construction and Operation of a New Chinese Research Station, Victoria Land, Antarctica DRAFT COMPREHENSIVE ENVIRONMENTAL EVALUATION January 2014 Polar Research Institute of China Tongji University Contents CONTACT DETAILS ..................................................................................................................... 1 NON-TECHNICAL SUMMARY .................................................................................................. 2 1. Introduction ............................................................................................................................. 9 1.1 Purpose of a new station in Victoria Land................................................................................................... 9 1.2 History of Chinese Antarctic activities ...................................................................................................... 13 1.3 Scientific programs for the new station ..................................................................................................... 18 1.4 Preparation and submission of the Draft CEE ........................................................................................... 22 1.5 Laws, standards and guidelines ................................................................................................................. 22 1.5.1 International laws, standards and guidelines ................................................................................. 23 1.5.2. Chinese laws, standards and guidelines ...................................................................................... -
Expedition to the South Pole
Framheim, National Library of Norway. Roald Amundsen Expedition to the South Pole E&T P 29 Roald Amundsen -2- Expedition to the South Pole by Roald Amundsen -1- Lecture delivered in German by Roald Amundsen before the Berlin Geographical Society on October 9, 1912. Translated and reprinted from the Zeitschr. der Gesell. für Erdkunde zu Berlin, 1912, No.7, pp. 481-498. Reprinted in the Annual Report of the Board of Regents of The Smithsonian Institution, Washington D.C., 1912, by permission from the Bulletin of the American Geographical Society, vol. 44, No. 11, November, 1912, New York, pp. 822-838. This edition of 100 copies was issued by The Erebus & Terror Press, Jaffrey, New Hampshire, for those attending the SouthPole-sium v.3 Oslo, Norway 12-14 May 2017. Certain images and footnotes were not included. Printed at Savron Graphics Jaffrey, New Hampshire May 2017 ❦ -2- Expedition to the South Pole HE PLAN of the third Fram expedition was twofold: First, the attainment Tof the South Pole, and, second, the exploration of the north polar regions. This evening I have the honor to report to you on the accomplishment of the first part of this plan. I can only briefly mention here the expeditions which have worked in the region which we had selected for our starting point. As we wished to reach the South Pole, our first problem was to go south as far as possible with our ship and there establish our station. Even so, the sled journeys would be long enough. I knew that the English expedition would again choose their old winter quarters in McMurdo Sound, South Victoria Land, as their starting point. -
National Science Foundation § 670.29
National Science Foundation § 670.29 the unique natural ecological system ASPA 115 Lagotellerie Island, Mar- in that area; and guerite Bay, Graham Land (c) Where a management plan exists, ASPA 116 New College Valley, information demonstrating the consist- Caughley Beach, Cape Bird, Ross Is- ency of the proposed actions with the land management plan. ASPA 117 Avian Island, Marguerite Bay, Antarctic Peninsula § 670.29 Designation of Antarctic Spe- ASPA 118 Summit of Mount Mel- cially Protected Areas, Specially bourne, Victoria Land Managed Areas and Historic Sites ASPA 119 Davis Valley and Forlidas and Monuments. Pond, Dufek Massif, Pensacola Moun- (a) The following areas have been tains designated by the Antarctic Treaty ASPA 120 Pointe-Geologie Parties for special protection and are Archipelego, Terre Adelie hereby designated as Antarctic Spe- ASPA 121 Cape Royds, Ross Island cially Protected Areas (ASPA). The ASPA 122 Arrival Heights, Hut Point Antarctic Conservation Act of 1978, as Peninsula, Ross Island amended, prohibits, unless authorized ASPA 123 Barwick and Balham Val- by a permit, any person from entering leys, Southern Victoria Land or engaging in activities within an ASPA 124 Cape Crozier, Ross Island ASPA. Detailed maps and descriptions ASPA 125 Fildes Peninsula, King of the sites and complete management George Island (25 de Mayo) plans can be obtained from the Na- ASPA 126 Byers Peninsula, Living- tional Science Foundation, Office of ston Island, South Shetland Islands Polar Programs, National Science ASPA 127 Haswell Island Foundation, Room 755, 4201 Wilson ASPA 128 Western shore of Admiralty Boulevard, Arlington, Virginia 22230. Bay, King George Island, South Shet- ASPA 101 Taylor Rookery, Mac. -
Federal Register/Vol. 81, No. 175/Friday, September 9, 2016
Federal Register / Vol. 81, No. 175 / Friday, September 9, 2016 / Notices 62543 banding. The principal avian predators ASPA 132, Potter Peninsula, King Division of Polar Programs, National of the penguins (skuas, gulls, giant George Island, South Shetland Islands Science Foundation, 4201 Wilson petrels and sheathbills) are also ASPA 133, Harmony Point, Nelson Boulevard, Arlington, Virginia 22230. monitored and, when possible, adults Island, South Shetland Island FOR FURTHER INFORMATION CONTACT: and chicks will be banded, weighed and ASPA 134, Cierva Point Offshore Nature McGinn, ACA Permit Officer, at measured for behavioral and Islands, Danco Coast, Antarctic the above address or ACApermits@ demographic studies. In addition, the Peninsula nsf.gov or (703) 292–7149. applicant may census, band and ASPA 139, Biscoe Point, Anvers Island SUPPLEMENTARY INFORMATION: The measure cape petrels and blue-eyed ASPA 140, Shores of Port Foster, National Science Foundation, as shags. The applicant may collect Deception Island, South Shetland directed by the Antarctic Conservation samples of penguin and skua blood from Islands Act of 1978 (Pub. L. 95–541), as adults of each species. The number of ASPA 144, Chile Bay amended by the Antarctic Science, takes per annum of each avian species ASPA 145, Port Foster, Deception Tourism and Conservation Act of 1996, will be as follows: chinstrap penguin, Island, South Shetland Islands ASPA 146, South Bay, Doumer Island, has developed regulations for the 3320; Adelie penguin, 2880; Gentoo Palmer Archipelago establishment of a permit system for penguin, 3020; brown skua, 600; south ASPA 148, Mount Flora, Hope Bay, various activities in Antarctica and polar skua, 600; giant petrel, 600; kelp Antarctic Peninsula designation of certain animals and gull, 100; blue-eyed shag, 150; snowy ASPA 149, Cape Shirreff, Livingston certain geographic areas a requiring sheathbill, 45; cape petrel, 200. -
Spatial Variations in the Geochemistry of Glacial Meltwater Streams in the Taylor Valley, Antarctica KATHLEEN A
Antarctic Science 22(6), 662–672 (2010) & Antarctic Science Ltd 2010 doi:10.1017/S0954102010000702 Spatial variations in the geochemistry of glacial meltwater streams in the Taylor Valley, Antarctica KATHLEEN A. WELCH1, W. BERRY LYONS1, CARLA WHISNER1, CHRISTOPHER B. GARDNER1, MICHAEL N. GOOSEFF2, DIANE M. MCKNIGHT3 and JOHN C. PRISCU4 1The Ohio State University, Byrd Polar Research Center, 1090 Carmack Rd, 108 Scott Hall, Columbus, OH 43210, USA 2Department of Civil and Environmental Engineering, Pennsylvania State University, University Park, PA 16802, USA 3University of Colorado, INSTAAR, Boulder, CO 80309-0450, USA 4Dept LRES, 334 Leon Johnson Hall, Montana State University, Bozeman, MT 59717, USA [email protected] Abstract: Streams in the McMurdo Dry Valleys, Antarctica, flow during the summer melt season (4–12 weeks) when air temperatures are close to the freezing point of water. Because of the low precipitation rates, streams originate from glacial meltwater and flow to closed-basin lakes on the valley floor. Water samples have been collected from the streams in the Dry Valleys since the start of the McMurdo Dry Valleys Long-Term Ecological Research project in 1993 and these have been analysed for ions and nutrient chemistry. Controls such as landscape position, morphology of the channels, and biotic and abiotic processes are thought to influence the stream chemistry. Sea-salt derived ions tend to be higher in streams that are closer to the ocean and those streams that drain the Taylor Glacier in western Taylor Valley. Chemical weathering is an important process influencing stream chemistry throughout the Dry Valleys. Nutrient availability is dependent on landscape age and varies with distance from the coast.