Minimizing Tourist Impact on the Argentine Islands Ecosystem, Antarctic Peninsula, Using Visitor Site Guidelines Approach
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Management Plan for Antarctic Specially Protected Area No
Management Plan for Antarctic Specially Protected Area No. 108 GREEN ISLAND, BERTHELOT ISLANDS, ANTARCTIC PENINSULA 1. Description of values to be protected Green Island (Latitude 65°19' S, Longitude 64°09' W, approximately 0.2 km2), Berthelot Islands, Grandidier Channel, Antarctic Peninsula, was originally designated as a Specially Protected Area through Recommendation IV-9 (1966, SPA No. 9) after a proposal by the United Kingdom. It was designated on the grounds that the vegetation “is exceptionally rich, [and] is probably the most luxuriant anywhere on the west side of the Antarctic Peninsula”. The Recommendation noted: “in some places the humus is 2 metres thick and that this area, being of outstanding scientific interest, should be protected because it is probably one of the most diverse Antarctic ecosystems”. A Management Plan for the site was prepared by the United Kingdom and adopted through Recommendation XVI-6 (1991). The original reasons for designation were extended and elaborated, although following comparisons to other sites in the vicinity, Green Island was no longer considered to be particularly diverse. The vegetation on the island was described as extensive on the north-facing slopes, with well-developed continuous banks of moss turf formed by Chorisodontium aciphyllum and Polytrichum strictum that, over much of their extent, overlie peat of more than one metre in depth. Antarctic hair grass (Deschampsia antarctica), one of only two native vascular plants that grow south of 56°S, was noted as frequent in small patches near a blue-eyed cormorant (Phalacrocorax atriceps) colony. The colony of blue- eyed cormorants, located on the steep, rocky northwestern corner of the island, was noted as being possibly one of the largest along the Antarctic 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. -
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. -
Geoterrace-2020-001
GeoTerrace-2020-001 Volume changes of glacier frontal parts on Galindez and Winter islands in 2013-2019 *Kh. Marusazh (Lviv Polytechnic National University) SUMMARY The results of glacier monitoring on Galindez Island and Winter Island (the Argentine Islands in the Wilhelm Archipelago, Antarctic Peninsula) in 2013-2019 are presents. The main objective of research was to determine how the volumes of glaciers changed in 2013-2019 in the course of a complex study. The materials of the Ukrainian seasonal expedition of 2013-2019 was used: terrestrial laser scanning data of 2013, 2014, 2018, terrestrial digital photography of 2013, 2014, 2018, 2019 and an unmanned aerial vehicle survey of 2019. The technique was used to determine changes in the volumes of glaciers can significantly improve both the speed and accuracy of the measurements. It included complementary processing of scanning data and digital photography of 2013-2018, and digital photography and aerial survey of 2019. Changes in the volumes of glaciers were calculated for the western and southern parts of the glacier on Galindez Island and the southern part of the glacier on Winter Island. The results demonstrate significant changes since 2002. This is confirmed quantitatively by independent studies of the West of the peninsula. Monitoring of the dynamics of glacier volumes enables detection of climatic and glaciological changes in the Antarctic region. GeoTerrace-2020 07-09 December 2020, Lviv, Ukraine Introduction The Antarctic ice cover is a complex natural system whose internal dynamics is sensitive to both atmospheric and oceanic influences. A deeper understanding of the underlying processes may have a profound impact on the development of prognostic models. -
Antarctic Treaty Handbook
Annex Proposed Renumbering of Antarctic Protected Areas Existing SPA’s Existing Site Proposed Year Annex V No. New Site Management Plan No. Adopted ‘Taylor Rookery 1 101 1992 Rookery Islands 2 102 1992 Ardery Island and Odbert Island 3 103 1992 Sabrina Island 4 104 Beaufort Island 5 105 Cape Crozier [redesignated as SSSI no.4] - - Cape Hallet 7 106 Dion Islands 8 107 Green Island 9 108 Byers Peninsula [redesignated as SSSI no. 6] - - Cape Shireff [redesignated as SSSI no. 32] - - Fildes Peninsula [redesignated as SSSI no.5] - - Moe Island 13 109 1995 Lynch Island 14 110 Southern Powell Island 15 111 1995 Coppermine Peninsula 16 112 Litchfield Island 17 113 North Coronation Island 18 114 Lagotellerie Island 19 115 New College Valley 20 116 1992 Avian Island (was SSSI no. 30) 21 117 ‘Cryptogram Ridge’ 22 118 Forlidas and Davis Valley Ponds 23 119 Pointe-Geologic Archipelago 24 120 1995 Cape Royds 1 121 Arrival Heights 2 122 Barwick Valley 3 123 Cape Crozier (was SPA no. 6) 4 124 Fildes Peninsula (was SPA no. 12) 5 125 Byers Peninsula (was SPA no. 10) 6 126 Haswell Island 7 127 Western Shore of Admiralty Bay 8 128 Rothera Point 9 129 Caughley Beach 10 116 1995 ‘Tramway Ridge’ 11 130 Canada Glacier 12 131 Potter Peninsula 13 132 Existing SPA’s Existing Site Proposed Year Annex V No. New Site Management Plan No. Adopted Harmony Point 14 133 Cierva Point 15 134 North-east Bailey Peninsula 16 135 Clark Peninsula 17 136 North-west White Island 18 137 Linnaeus Terrace 19 138 Biscoe Point 20 139 Parts of Deception Island 21 140 ‘Yukidori Valley’ 22 141 Svarthmaren 23 142 Summit of Mount Melbourne 24 118 ‘Marine Plain’ 25 143 Chile Bay 26 144 Port Foster 27 145 South Bay 28 146 Ablation Point 29 147 Avian Island [redesignated as SPA no. -
The Antarctic Treaty Cm 8841
The Antarctic Treaty Measures adopted at the Thirty-sixth Consultative Meeting held at Brussels, 20 – 29 May 2013 Presented to Parliament by the Secretary of State for Foreign and Commonwealth Affairs by Command of Her Majesty March 2014 Cm 8841 © Crown copyright 2014 You may re-use this information (excluding logos) free of charge in any format or medium, under the terms of the Open Government Licence v.2. To view this licence visit www.nationalarchives.gov.uk/doc/open-government-licence/version/2/ or email [email protected] This publication is available at www.gov.uk/government/publications Any enquiries regarding this publication should be sent to us at Treaty Section, Foreign and Commo nwealth Office, King Charles Street, London, SW1A 2AH Print ISBN 9781474101134 Web ISBN 9781474101141 Printed in the UK by the Williams Lea Group on behalf of the Controller of Her Majesty’s Stationery Office ID P002631486 03/14 Printed on paper containing 30% recycled fibre content minimum MEASURES ADOPTED AT THE THIRTY-SIXTH ANTARCTIC TREATY CONSULTATIVE MEETING Brussels, Belgium, 20-29 May 2013 The Measures1 adopted at the Thirty-sixth Antarctic Treaty Consultative Meeting are reproduced below from the Final Report of the Meeting. In accordance with Article IX, paragraph 4, of the Antarctic Treaty, the Measures adopted at Consultative Meetings become effective upon approval by all Contracting Parties whose representatives were entitled to participate in the meeting at which they were adopted (i.e. all the Consultative Parties). The full text of the Final Report of the Meeting, including the Decisions and Resolutions adopted at that Meeting and colour copies of the maps found in this command paper, is available on the website of the Antarctic Treaty Secretariat at www.ats.aq/documents. -
Bacterial Diversity Is Strongly Associated with Historical Penguin Activity in an Antarctic Lake Sediment Profile
www.nature.com/scientificreports OPEN Bacterial diversity is strongly associated with historical penguin activity in an Antarctic lake Received: 27 July 2015 Accepted: 27 October 2015 sediment profile Published: 25 November 2015 Renbin Zhu1, Yu Shi2, Dawei Ma1, Can Wang1, Hua Xu2 & Haiyan Chu2 Current penguin activity in Antarctica affects the geochemistry of sediments and their microbial communities; the effects of historical penguin activity are less well understood. Here, bacterial diversity in ornithogenic sediment was investigated using high-throughput pyrosequencing. The relative abundances of dominant phyla were controlled by the amount of historical penguin guano deposition. Significant positive correlations were found between both the bacterial richness and diversity, and the relative penguin number (p < 0.01); this indicated that historical penguin activity drove the vertical distribution of the bacterial communities. The lowest relative abundances of individual phyla corresponded to lowest number of penguin population at 1,800–2,300 yr BP during a drier and colder period; the opposite was observed during a moister and warmer climate (1,400–1,800 yr BP). This study shows that changes in the climate over millennia affected penguin populations and the outcomes of these changes affect the sediment bacterial community today. Antarctic freshwater lakes are relatively simple aquatic ecosystems, with low species richness and diversity, low biomass, short food chains and limited trophic complexity1,2. However, benthic sediments represent one of the most complex microbial habitats on Earth3. Microorganisms in sediments play a significant role in biogeochemical cycles and the remineralisation of organic matter within aquatic ecosystems. For example, bacterial populations are major contributors in the transformation of organic carbon, sulphur, nitrogenous compounds, and metals, and have an important role in ecosystem food webs and nutrient cycling2,4. -
Groundwater Characteristics at Seabee Hook, Cape Hallett, Antarctica ERICA H
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Research Commons@Waikato Antarctic Science 18 (4), 487–495 (2006) © Antarctic Science Ltd Printed in the UK DOI: 10.1017/S0954102006000538 Groundwater characteristics at Seabee Hook, Cape Hallett, Antarctica ERICA H. HOFSTEE1, DAVE I. CAMPBELL1*, MEGAN R. BALKS1 and JACKIE AISLABIE2 1Department of Earth and Ocean Sciences, The University of Waikato, Private Bag 3105, Hamilton, New Zealand 2Landcare Research, Private Bag 3127, Hamilton, New Zealand *corresponding author: [email protected] Abstract: Seabee Hook is a low lying gravel spit adjacent to Cape Hallett, northern Victoria Land, in the Ross Sea region of Antarctica and hosts an Adélie penguin (Pygoscelis adeliae) rookery. Dipwells were inserted to monitor changes in depth to, and volume of, groundwater and tracer tests were conducted to estimate aquifer hydraulic conductivity and groundwater velocity. During summer (November–February), meltwater forms a shallow, unconfined, aquifer perched on impermeable ice cemented soil. Groundwater extent and volume depends on the amount of snowfall as meltwater is primarily sourced from melting snow drifts. Groundwater velocity through the permeable gravel and sand was up to 7.8 m day-1, and hydraulic conductivities of 4.7 × 10-4 m s-1 to 3.7 × 10-5 m s-1 were measured. The presence of the penguin rookery, and the proximity of the sea, affects groundwater chemistry with elevated concentrations of salts (1205 mg L-1 sodium, 332 mg L-1 potassium) and nutrients (193 mg L-1 nitrate, 833 mg L-1 ammonia, 10 mg L-1 total phosphorus) compared with groundwater sourced away from the rookery, and with other terrestrial waters in Antarctica. -
Fln.Tflrcit.IC
flN.TflRCiT.IC A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) A New Zealand Ministry of Works and Development surveyor, Steven Currie, carries out a triangulation survey on the main crater rim of Mt Erebus, the active volcano on Ross Island. Some of the hazards of last season's programme were average temperatures of minus 30deg Celsius and 23 eruptions which hurled lava bombs from the inner crater up to 200m in the air. - Antarctic Division photo , , _, ., -. ,, p- Registered at Post Office Headquarters, Marrh 1 QRd VOL 1U, NO. O Wellington, New Zealand, as a magazine. ivlaluii, I30t SOUTH GEORGIA •. SOUTH SANDWICH It SOUTH ORKNEY It / \ S^i^j^voiMarevskaya7 6SignyloK ,'' / / o O r c a d a s a r g SOUTHTH AMERICAAMERICA ' /''' / .\ J'Borgal ^7^]Syowa japan \ Kr( SOUTH , .* /WEDDELL \ U S* I / ^ST^Moiodwhnaya \^' SHETLAND U / x Ha|| J^tf ORONN NG MAUD LAND ^D£RBY \\US*> \ / " W ' \ / S f A u k y C O A T S L d / l a n d J ^ ^ \ Lw*M#^ ^te^B.«,ranoW >dMawson \ /PENINSUtA'^SX^^^Rpnnep^J "<v MAC ROKRTSON LAND^ \ aust \ |s« map below) 1^=^ A <ce W?dSobralARG \/^ ^7 '• Davis Aust /_ Siple _ USA ! ELLSWORTH ^ Amundsen-Scon / queen MARY LAND {MimV ') LAND °VosloJc ussr MARIE BYRD^S^ »« She/f\'r - ..... 1 y * \ WIL KES U N O Y' ROSS|N'l?SEA I J«>ryVICTORIA \VandaN' .TERRE / gf ,f 7.W ^oV IAN0 y/ADEliu/ /» I ( GEORGE V l4_,„-/'r^ •^^Sa^/^r .uumont d'Urville iranc i L e n i n g r a d j k a Y a V > ussr.-' \ / - - - - " ' " ' " B A I L E N Y l t \ / ANTARCTIC PENINSULA 1 Teniente Matien?o arc 2 Esp*ran:a arc 3 Almiranie Brown arg 4 Petrel arg 5 Decepcion arg 6 V i c e c o m o d o r o M a r a m b i o a r g ' ANTARCTICA 7 AMuro Prat chili 8 Bernardo O'Higgins chile 500 1000 Milts 9 Presidente Frei chili WOO K.kxnnna 10 Stonington I. -
Interglacial Heterogeneities in the Ice Caps of the Argentine Islands and Their Dynamics During first 2 Years of GPR Investigations
Geophysical Research Abstracts Vol. 21, EGU2019-1633, 2019 EGU General Assembly 2019 © Author(s) 2018. CC Attribution 4.0 license. Interglacial heterogeneities in the ice caps of the Argentine islands and their dynamics during first 2 years of GPR investigations Anatolii Chernov (1), Denis Pishniak (2), Kristaps Lamsters (3), Janis¯ Karušs (3), and Maris¯ Krievans¯ (3) (1) Institute of geology, Taras Shevchenko National University of Kyiv, Kyiv, Ukraine ([email protected]), (2) Department of Atmospheric Physics, National Antarctic Scientific Center of Ukraine, Kyiv, Ukraine ([email protected]), (3) Faculty of Geography and Earth Sciences, University of Latvia, Riga, Latvia ([email protected]) First information about glaciological observations in the area of the Antarctic Peninsula is dated by the beginning of the 20-th century (French Antarctic Expedition 1904-1907). In 1960-th, Thomas and Sadler (British Antarctic Survey) noted that the ice cap of Galindez Island like the other Argentine Archipelago islands is a relict of the shelf glacier, which subsequent evolution needs further studies. Therefore, during several Ukrainian short-term researches (video-impulse radiolocation method in 1998, vertical electric-resonance sounding in 2004) of island’s glaciers on Galindez and Winter islands (the Argentine Archipelago) were organized. These researches reveal that monitoring of glaciers on the Argentine islands is important and should be done regularly. Furthermore, informa- tion about changes in island’s glaciers movement, deformation and geometrical parameters is considered to be an indicator of worldwide climate changes. In this paper, results of ground-penetrating radar surveying, drilling with photo-video recording and core sampling, which were done on the glaciers around the station Akademik Vernadsky since April 2017, are described. -
Antarctic Peninsula) Under the Antarctic Treaty System, Суспільно-Географічні Ukrainian Antarctic Journal, 1, 111—119, 2020
Fedchuk, A., Sinna, O., Milinevsky, G., Utevsky, A.: The harmonization of small-scale marine spatial protection in the Argentine Islands area Міжнародне співробітництво: (Antarctic Peninsula) under the Antarctic Treaty System, суспільно-географічні Ukrainian Antarctic Journal, 1, 111—119, 2020. та політико-правові аспекти doi:10.33275/1727-7485.1.2020.384 освоєння Антарктики International Co-Operation: Socio-Economic, Political and Legal Issues of Antarctic Exploration A. Fedchuk 1, *, O. Sinna 2, G. Milinevsky 1, 3, 4, A. Utevsky 1, 2 1 State Institution National Antarctic Scientific Center, Ministry of Education and Science of Ukraine, Kyiv, 01601, Ukraine 2 V.N. Karazin Kharkiv National University, Kharkiv, 61022, Ukraine 3 Taras Shevchenko National University of Kyiv, Kyiv, 01601, Ukraine 4 College of Physics, International Center of Future Science, Jilin University, Changchun, 130012, China * Corresponding author: [email protected] The harmonization of small-scale marine spatial protection in the Argentine Islands area (Antarctic Peninsula) under the Antarctic Treaty System Abstract. The purpose of the article is to summarize the results of field studies carried out in the framework of the State Antarc- tic Research Program for 2011–2020 and undertaken to identify areas of special interest for small-scale marine spatial protec- tion in the Argentine Islands water area. The scientific results reported in the publications and relevant meetings’ documents officially presented by the Ukrainian delegation in 2012–2019 were summarized and interpreted in view of the Antarctic Treaty System (ATS) provisions on marine spatial protection. GIS analysis was applied to field data. It is shown that the development of protection regime for small-scale underwater landscape is based on systematic biogeographical data collected during sea- sonal and year-round Ukrainian Antarctic expeditions in 2011–2019. -
Mineral Resources of Antarctica
GEOLOGICAL SURVEY CIRCULAR 705 Mineral Resources of Antarctica Mineral Resources of Antarctica Compiled ancl eclitecl &y N. A. Wright ancl P. L. Williams GEOLOGICAL SURVEY CIRCULAR 705 1974 United States Department of the Interior ROGERS C. B. MORTON, Secretary Geological Survey V. E. McKelvey, Director Free on application to the U.S. Geological Survey, National Center, Reston, Va. 22092 CONTENTS Page )Lbstract ---------------------------------------------------------------- 1 Introduction ------------------------------------------------------------ 1 ldineral occurrences ------------------------------------------------------ 3 Sand and gravel ---------------------------------------------------- 3 Other nonmetals ---------------------------------------------------- 3 Iron ---------------------------------------------------------------- 10 Copper --------_____ -.- ____ - __ - _________ - ___ - ___ - --__ ----------------- 11 Gold and silver ------------------------------------------------------ 11 ldolybdenum ___________________________________ ---_ -~- --------------- 11 Other metals -------------------------------------------------------- 11 Potential resources _--- _-_________ - ________ - ____ ---_----__ ---------------- 11 ldanganese nodules _____________________________ ---____ --------------- 11 Geothermal energy --------------------------------------------------- 12 VVater (as ice) ------------------------------------------------------ 15 Coal ---------------------------------------------------------------- 15 Oil and natural gas