The Hybrid Skua: a Southern Ocean Enigma
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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, -
Variability in Krill Biomass Links Harvesting and Climate Warming to Penguin Population Changes in Antarctica
Variability in krill biomass links harvesting and climate warming to penguin population changes in Antarctica Wayne Z. Trivelpiecea,1, Jefferson T. Hinkea,b, Aileen K. Millera, Christian S. Reissa, Susan G. Trivelpiecea, and George M. Wattersa aAntarctic Ecosystem Research Division, Southwest Fisheries Science Center, National Marine Fisheries Service, National Oceanic and Atmospheric Administration, La Jolla, CA, 92037; and bScripps Institution of Oceanography, University of California at San Diego, La Jolla, CA 92093 Edited by John W. Terborgh, Duke University, Durham, NC, and approved March 11, 2011 (received for review November 5, 2010) The West Antarctic Peninsula (WAP) and adjacent Scotia Sea terns of population change observed before and after 1986 are support abundant wildlife populations, many of which were nearly explained by recruitment trends. During the first decade of our extirpated by humans. This region is also among the fastest- studies, 40–60% of the penguins banded as fledglings recruited warming areas on the planet, with 5–6 °C increases in mean winter back to natal colonies, and first-time breeders constituted 20– air temperatures and associated decreases in winter sea-ice cover. 25% of the breeding population annually (Fig. 1 C and D). These biological and physical perturbations have affected the eco- Subsequently, survival to first breeding dropped precipitously in system profoundly. One hypothesis guiding ecological interpreta- the 1980s, and the recruitment rates of both species have de- tions of changes in top predator populations in this region, the clined (7). Less than 10% of Adélie penguins banded as chicks “sea-ice hypothesis,” proposes that reductions in winter sea ice survive to breed (Fig. -
Thirty Years of Marine Debris in the Southern Ocean Annual
Environment International 136 (2020) 105460 Contents lists available at ScienceDirect Environment International journal homepage: www.elsevier.com/locate/envint Thirty years of marine debris in the Southern Ocean: Annual surveys of two island shores in the Scotia Sea T ⁎ Claire M. Waludaa, , Iain J. Stanilanda, Michael J. Dunna, Sally E. Thorpea, Emily Grillyb, Mari Whitelawa, Kevin A. Hughesa a British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge CB3 0ET, UK b Commission for the Conservation of Antarctic Marine Living Resources, 181 Macquarie Street, Hobart 7000, Tasmania, Australia ARTICLE INFO ABSTRACT Handling Editor: Adrian Covaci We report on three decades of repeat surveys of beached marine debris at two locations in the Scotia Sea, in the Keywords: Southwest Atlantic sector of the Southern Ocean. Between October 1989 and March 2019 10,112 items of Marine debris beached debris were recovered from Main Bay, Bird Island, South Georgia in the northern Scotia Sea. The total Plastic mass of items (data from 1996 onwards) was 101 kg. Plastic was the most commonly recovered item (97.5% by Scotia Sea number; 89% by mass) with the remainder made up of fabric, glass, metal, paper and rubber. Mean mass per − − Antarctic item was 0.01 kg and the rate of accumulation was 100 items km 1 month 1. Analyses showed an increase in South Georgia the number of debris items recovered (5.7 per year) but a decline in mean mass per item, suggesting a trend South Orkney towards more, smaller items of debris at Bird Island. At Signy Island, South Orkney Islands, located in the southern Scotia Sea and within the Antarctic Treaty area, debris items were collected from three beaches, during the austral summer only, between 1991 and 2019. -
The Antarctic Treaty
The Antarctic Treaty Measures adopted at the Thirty-ninth Consultative Meeting held at Santiago, Chile 23 May – 1 June 2016 Presented to Parliament by the Secretary of State for Foreign and Commonwealth Affairs by Command of Her Majesty November 2017 Cm 9542 © Crown copyright 2017 This publication is licensed under the terms of the Open Government Licence v3.0 except where otherwise stated. To view this licence, visit nationalarchives.gov.uk/doc/open-government-licence/version/3 Where we have identified any third party copyright information you will need to obtain permission from the copyright holders concerned. 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 Commonwealth Office, King Charles Street, London, SW1A 2AH ISBN 978-1-5286-0126-9 CCS1117441642 11/17 Printed on paper containing 75% recycled fibre content minimum Printed in the UK by the APS Group on behalf of the Controller of Her Majestyʼs Stationery Office MEASURES ADOPTED AT THE THIRTY-NINTH ANTARCTIC TREATY CONSULTATIVE MEETING Santiago, Chile 23 May – 1 June 2016 The Measures1 adopted at the Thirty-ninth 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. -
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. -
Eastern Dallmann Bay
Measure 11 (2009) - Annex Management Plan for Antarctic Specially Protected Area No. 153 EASTERN DALLMANN BAY Introduction This marine ASPA lies off the western and northern coasts of Brabant Island, Palmer Archipelago, between 64°00'S and 64°20'S; 62°50'W and the western coast of Brabant Island. Approximate area: 676km2. Designation on the grounds that the shallow shelf in this region near Brabant Island is one of only two known sites in the vicinity of Palmer Station (US) that are suitable for bottom trawling for fish and other benthic organisms (see also ASPA No 152 Western Bransfield Strait). The benthic fauna of the site is of exceptional scientific interest and the area provides an important habitat for juvenile fish. Proposed by the United States of America: adopted by Recommendation XVI-3 (Bonn, 1991: SSSI No 36); date of expiry extended by Measure 3 (2001); renamed and renumbered by Decision 1 (2002); revised management plan adopted by Measure 2 (2003). 1. Description of values to be protected Eastern Dallmann Bay (between latitudes 64°00'S and 64°20'S and from longitude 62°50'W eastward to the western shore of Brabant Island, approximately 676km2) was originally designated as a Site of Special Scientific Interest through Recommendation XVI-3 (1991, SSSI No 36) after a proposal by the United States of America. It was designated on the grounds that “the shallow shelf west of East Dallmann Bay is one of only two known sites near Palmer Station that are suitable for bottom trawling for fish and other benthic organisms. -
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. -
A New High-Latitude Record for the Macaroni Penguin (Eudyptes Chrysolophus) at Avian Island, Antarctica
Polar Biol DOI 10.1007/s00300-010-0795-y SHORT NOTE A new high-latitude record for the macaroni penguin (Eudyptes chrysolophus) at Avian Island, Antarctica K. B. Gorman • E. S. Erdmann • B. C. Pickering • P. J. Horne • J. R. Blum • H. M. Lucas • D. L. Patterson-Fraser • W. R. Fraser Received: 11 December 2009 / Revised: 10 March 2010 / Accepted: 13 March 2010 Ó Springer-Verlag 2010 Abstract On 20 and 22 January 2007, we observed observations are important for developing a better under- macaroni penguins (Eudyptes chrysolophus) on Avian standing of the natural history of the species along the Island, Antarctica, approximately 1° south of the Antarctic WAP. Circle along the Western Antarctic Peninsula (WAP) near Adelaide Island, a new high-latitude observational record Keywords Bio-geographic range shift Á for the species within this region of the continent. Addi- Climate warming Á Eudyptes chrysolophus Á tionally, we report several extra-limital sightings of mac- Western Antarctic Peninsula Á Vagrancy aroni penguins over the last decade at relatively lower latitudes along the WAP near Anvers Island, including observations of breeding attempts. Although vagrancy Introduction cannot be ruled out as a possible causal factor in our observations, we hypothesize that a climate-induced shift The macaroni penguin (Eudyptes chrysolophus) is cir- in the species’ bio-geographic range may be in progress. In cumpolar and sub-Antarctic in its breeding distribution this context, our observations are similar to the well-doc- (Parmelee 1992; Williams 1995). Breeding populations in umented range shifts and eventual establishment of the core of the species range occur on islands near the breeding populations by other sub-Antarctic penguin spe- Antarctic convergence in the southwest Atlantic and south cies along the WAP, over the last three decades, in Indian sectors of the Southern Ocean such as South response to regional climate warming. -
The Sediments of Lake on the Ardley Island , Antarctica:Identi
Chinese Journal of Polar Science , Vol .12 , No .1 , 1 8 , June 2001 The sediments of lake on the Ardley Island , Antarctica :Identi- fication of penguin-dropping soil Sun Liguang (孙立广)1 , Xie Zhouqing (谢周清)1 and Zhao Junlin (赵俊琳)2 1 Instituteof Polar Environment , University of Science and Technology of China , Hefei 230026 , China 2 Instituteof Environmental Science , Beijing Normal University , Beijing 100875 , China Received January 10 , 2001 Abstract During CHINARE-15 (Dec .1998 Mar .1999), a lake core 67 .5 cm in length , w as sampled in Y2 lake, which is located on the Ardley Island , Antarctica.The concentrations of some chemical elements in Y2 lake sediments were analyzed .According to comparative research on elementary characters of sediments in Antarctic West Lake, fresh penguin dropping as well as guano soil on the Ardley Island and Pacific Island in South China Sea , it presents that the Y2 lake sediments were ameliorated by penguin dropping .The result of element cluster analysis show s that the type elements in the sedi- ment impacted by penguin dropping include Sr , F , S , P , Ca, Se, Cu , Zn and Ba.This can provide a base for further interpreting the climatic and environmental event recorded in the sediment . Key words Antarctica, Ardley Island , penguin dropping soil , type element . 1 Introduction The ice-free area surrounding Antarctica appeared following the climate warming-up and ice regression .The sediment profile of lake formed during this period might com- pletely record the course of the glacial advance and retreat as well as environmental change since Holocene .Therefore, many researchers have made researches on the Holocene lake sediment in Antarctica , especially the lake on the South Sheltland Island (Hodgson and Johnston 1997 ;Appleby et al .1995 ;Xie et al .1992 ;Yu et al .1992 ;Bjorck et a l . -
Limosa Haemastica (Linnaeus, 1758): First Record from South Istributio
ISSN 1809-127X (online edition) © 2010 Check List and Authors Chec List Open Access | Freely available at www.checklist.org.br Journal of species lists and distribution N Aves, Charadriiformes, Scolopacidae, Limosa haemastica (Linnaeus, 1758): First record from South ISTRIBUTIO D Shetland Islands and Antarctic Peninsula, Antarctica 1,2* 1 1 1, 2 3 RAPHIC Mariana A. Juáres , Marcela M. Libertelli , M. Mercedes Santos , Javier Negrete , Martín Gray , G 1 1,2 4 1 1 EO Matías Baviera , M. Eugenia Moreira , Giovanna Donini , Alejandro Carlini and Néstor R. Coria G N O 1 Instituto Antártico Argentino, Departmento Biología, Aves, Cerrito 1248, C1010AAZ. Buenos Aires, Argentina. OTES 3 Administración de Parques Nacionales (APN). Avenida Santa Fe 690, C1059ABN. Buenos Aires, Argentina. N 4 2 JarConsejodín Zoológico Nacional de de Buenos Investigaciones Aires. República Científicas de lay TécnicasIndia 2900, (CONICET). C1425FCF. Rivadavia Buenos Aires,1917, Argentina.C1033AAJ. Buenos Aires, Argentina. * Corresponding author. E-mail: [email protected] Abstract: We report herein the southernmost record of the Hudsonian Godwit (Limosa haemastica), at two localities in the Antarctic: Esperanza/Hope Bay (January 2005) and 25 de Mayo/King George Island (October 2008). On both occasions a pair of specimens with winter plumage was observed. The Hudsonian Godwit Limosa haemastica (Linnaeus tide and each time birds were feeding in the intertidal 1758) is a neartic migratory species that breeds in Alaska zone. These individuals showed the winter plumage and Canada during summer and spends its non-breeding pattern: dark reddish chest and white ventral region, black period in the southernmost regions of South America primaries and tail feathers, a long upturned bill pink at during the boreal winter. -
Litchfield Island, Arthur Harbor Anvers Island, Palmer Archipelago
Measure 4 (2009) – Annex Management Plan for Antarctic Specially Protected Area No. 113 LITCHFIELD ISLAND, ARTHUR HARBOR ANVERS ISLAND, PALMER ARCHIPELAGO Introduction Litchfield Island lies within Arthur Harbor, SW Anvers Island, at 64°46'S, 64°06'W. Approximate area: 2.7km2. Designation on the grounds that Litchfield Island, together with its littoral zone, possesses an unusually high collection of marine and terrestrial life, is unique amongst the neighboring islands as a breeding place for six species of native birds and provides an outstanding example of the natural ecological system of the Antarctic Peninsula area. In addition, Litchfield Island possesses rich growths of vegetation and has the most varied topography and the greatest diversity of terrestrial habitats of the islands in Arthur Harbor. Proposed by the United States of America. Adopted through Recommendation VIII-1 (1975, SPA No. 17); renamed and renumbered by Decision 1 (2002); original management plan adopted through Measure 2 (2004). 1. Description of values to be protected Litchfield Island (Latitude 64°46'S, Longitude 64°06'W, 2.7km2), Arthur Harbor, Anvers Island, Antarctic Peninsula was originally designated as a Specially Protected Area through Recommendation VIII-1 (1975, SPA No. 17) after a proposal by the United States of America. It was designated on the grounds that “Litchfield Island, together with its littoral, possesses an unusually high collection of marine and terrestrial life, is unique amongst the neighboring islands as a breeding place for six species of native birds and provides an outstanding example of the natural ecological system of the Antarctic Peninsula area”. The current management plan reaffirms the original reasons for designation associated with the bird communities. -
Glacial History of the Antarctic Peninsula Since the Last Glacial Maximum—A Synthesis
Glacial history of the Antarctic Peninsula since the Last Glacial Maximum—a synthesis Ólafur Ingólfsson & Christian Hjort The extent of ice, thickness and dynamics of the Last Glacial Maximum (LGM) ice sheets in the Antarctic Peninsula region, as well as the pattern of subsequent deglaciation and climate development, are not well constrained in time and space. During the LGM, ice thickened considerably and expanded towards the middle–outer submarine shelves around the Antarctic Peninsula. Deglaciation was slow, occurring mainly between >14 Ky BP (14C kilo years before present) and ca. 6 Ky BP, when interglacial climate was established in the region. After a climate optimum, peaking ca. 4 - 3 Ky BP, a cooling trend started, with expanding glaciers and ice shelves. Rapid warming during the past 50 years may be causing instability to some Antarctic Peninsula ice shelves. Ó. Ingólfsson, The University Courses on Svalbard, Box 156, N-9170 Longyearbyen, Norway; C. Hjort, Dept. of Quaternary Geology, Lund University, Sölvegatan 13, SE-223 63 Lund, Sweden. The Antarctic Peninsula (Fig. 1) encompasses one Onshore evidence for the LGM ice of the most dynamic climate systems on Earth, extent where the natural systems respond rapidly to climatic changes (Smith et al. 1999; Domack et al. 2001a). Signs of accelerating retreat of ice shelves, Evidence of more extensive ice cover than today in combination with rapid warming (>2 °C) over is present on ice-free lowland areas along the the past 50 years, have raised concerns as to the Antarctic Peninsula and its surrounding islands, future stability of the glacial system (Doake et primarily in the form of glacial drift, erratics al.