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Responses of Antarctic Tundra Ecosystem to Climate Change and Human Activity
PAPERS on GLOBAL CHANGE, 17, 43–52, 2010 DOI: 10.2478/v10190-010-0004-4 RESPONSES OF ANTARCTIC TUNDRA ECOSYSTEM TO CLIMATE CHANGE AND HUMAN ACTIVITY MARIA OLECH Institute of Botany, Jagiellonian University, Kopernika 27, 31-501 Cracow, Poland, Department of Antarctic Biology, Polish Academy of Sciences, Ustrzycka 10/12, 02-141 Warsaw, Poland e-mail: [email protected] ABSTRACT: Over the last couple of years the Antarctic Peninsula region has been one of the fastest warming regions on the Earth. Rapidly proceeding deglaciation uncovers new areas for colonisation and formation of Antarctic tundra communities. The most evi- dent dynamics, i.e. changes in both biodiversity and structure of tundra communities, are observed in the forefi elds of retreating glaciers. This paper presents examples of changes in biodiversity and in the direction and rate of succession changes taking place due to climate warming compounded by synanthropization in the maritime Antarctic. KEY WORDS: Antarctic, climate change, colonisation, tundra ecosystem, bio- diversity, alien species. INTRODUCTION Development of vegetation in the Antarctic is limited to ice-free surfaces of the land, which account for only a few percent (2–5%) of the total area. The Antarctic tundra ecosystem is mainly made up of cryptogams, i.e. lichens, bryophytes, algae and fungi, while at the same time it is extremely defi cient in vascular plants, of which only two species are found: a grass Deschampsia antarctica Desv. (Poace- ae) and Colobanthus quitensis (Kunth). Bartl. (Caryophyllaceae). Occurrence of both species is limited to the climatically favourable sites in the maritime Antarctic (Olech 2002). -
(2011). AB Dobrowolski–The First Cryospheric Scientist–And
CMYK RGB Hist. Geo Space Sci., 2, 75–79, 2011 History of www.hist-geo-space-sci.net/2/75/2011/ Geo- and Space doi:10.5194/hgss-2-75-2011 © Author(s) 2011. CC Attribution 3.0 License. Access Open Sciences Advances in Science & Research Review article Open Access Proceedings A. B. Dobrowolski – the first cryospheric scientist – Drinking Water Drinking Water and the subsequent development of cryosphericEngineering science and Science Engineering and Science Open Access Access Open Discussions R. G. Barry1, J. Jania2, and K. Birkenmajer3 1National Snow and Ice Data Center, CIRES, University of Colorado, Boulder, CO, 80309-0449, USA 2 Discussions Faculty of Earth Sciences University of Silesia, Bedzinska 60, 41-200 Sosnowiec, Poland Earth System Earth System 3Institute of Geological Sciences, Polish Academy of Sciences, Senacka 1, 31-002, Krakow,´ Poland Science Science Received: 8 November 2010 – Revised: 17 March 2011 – Accepted: 17 March 2011 – Published: 18 April 2011 Open Access Open Abstract. The origin of the term “cryosphere” has been traced to the Polish scientist A. B. DobrowolskiAccess Open Data in Data his 1923 book on “The Natural History of Ice” written in Polish. This note commemorates his little recognized contribution to the science, outside of his native country, and summarizes the recent organization of cryospheric Discussions research. Social Social Open Access Open Geography 1 A. B. Dobrowolski this time and Dobrowolski was contractedAccess Open Geography as a simple sailor. Later, in the middle of the cruise and during overwintering in Antoni Bolesław Dobrowolski (1872–1954) was born into an the Antarctic, he became a formal member of the scientific indigent family, but with a high regard for education as a val- group (Dobrowolski, 1958). -
Cumulated Bibliography of Biographies of Ocean Scientists Deborah Day, Scripps Institution of Oceanography Archives Revised December 3, 2001
Cumulated Bibliography of Biographies of Ocean Scientists Deborah Day, Scripps Institution of Oceanography Archives Revised December 3, 2001. Preface This bibliography attempts to list all substantial autobiographies, biographies, festschrifts and obituaries of prominent oceanographers, marine biologists, fisheries scientists, and other scientists who worked in the marine environment published in journals and books after 1922, the publication date of Herdman’s Founders of Oceanography. The bibliography does not include newspaper obituaries, government documents, or citations to brief entries in general biographical sources. Items are listed alphabetically by author, and then chronologically by date of publication under a legend that includes the full name of the individual, his/her date of birth in European style(day, month in roman numeral, year), followed by his/her place of birth, then his date of death and place of death. Entries are in author-editor style following the Chicago Manual of Style (Chicago and London: University of Chicago Press, 14th ed., 1993). Citations are annotated to list the language if it is not obvious from the text. Annotations will also indicate if the citation includes a list of the scientist’s papers, if there is a relationship between the author of the citation and the scientist, or if the citation is written for a particular audience. This bibliography of biographies of scientists of the sea is based on Jacqueline Carpine-Lancre’s bibliography of biographies first published annually beginning with issue 4 of the History of Oceanography Newsletter (September 1992). It was supplemented by a bibliography maintained by Eric L. Mills and citations in the biographical files of the Archives of the Scripps Institution of Oceanography, UCSD. -
List of Place-Names in Antarctica Introduced by Poland in 1978-1990
POLISH POLAR RESEARCH 13 3-4 273-302 1992 List of place-names in Antarctica introduced by Poland in 1978-1990 The place-names listed here in alphabetical order, have been introduced to the areas of King George Island and parts of Nelson Island (West Antarctica), and the surroundings of A. B. Dobrowolski Station at Bunger Hills (East Antarctica) as the result of Polish activities in these regions during the period of 1977-1990. The place-names connected with the activities of the Polish H. Arctowski Station have been* published by Birkenmajer (1980, 1984) and Tokarski (1981). Some of them were used on the Polish maps: 1:50,000 Admiralty Bay and 1:5,000 Lions Rump. The sheet reference is to the maps 1:200,000 scale, British Antarctic Territory, South Shetland Islands, published in 1968: King George Island (sheet W 62 58) and Bridgeman Island (Sheet W 62 56). The place-names connected with the activities of the Polish A. B. Dobrowolski Station have been published by Battke (1985) and used on the map 1:5,000 Antarctic Territory — Bunger Oasis. Agat Point. 6211'30" S, 58'26" W (King George Island) Small basaltic promontory with numerous agates (hence the name), immediately north of Staszek Cove. Admiralty Bay. Sheet W 62 58. Polish name: Przylądek Agat (Birkenmajer, 1980) Ambona. 62"09'30" S, 58°29' W (King George Island) Small rock ledge, 85 m a. s. 1. {ambona, Pol. = pulpit), above Arctowski Station, Admiralty Bay, Sheet W 62 58 (Birkenmajer, 1980). Andrzej Ridge. 62"02' S, 58° 13' W (King George Island) Ridge in Rose Peak massif, Arctowski Mountains. -
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. -
Western Shore of Admiralty Bay, King George Island, South Shetland Islands
Measure 4 (2014) Annex Management Plan for Antarctic Specially Protected Area No 128 WESTERN SHORE OF ADMIRALTY BAY, KING GEORGE ISLAND, SOUTH SHETLAND ISLANDS Introduction The Western Shore of Admiralty Bay is located on King George Island, South Shetland Islands, ~125 kilometers from the northern Antarctic Peninsula. Approximate area and coordinates: 16.8 km2 (centered at 58° 27' 40" W, 62° 11' 50" S). The Area is wholly terrestrial, and the primary reasons for designation are its diverse avian and mammalian fauna and locally rich vegetation, providing a representative sample of the maritime Antarctic ecosystem. Long term scientific research has been conducted on the animals within the Area. The Area is relatively accessible to nearby research stations and tourist ships regularly visit Admiralty Bay, and the ecological and scientific values of the area need protection from potential disturbance. The Area was originally designated as Site of Special Scientific Interest (SSSI) No. 8 in Recommendation X-5 (1979, SSSI No. 8) after a proposal by Poland. The SSSI designation was extended through Recommendation XII-5 (1983), Recommendation XIII-7 (1985) and Resolution 7 (1995). A revised Management Plan was adopted through Measure 1 (2000). The site was renamed and renumbered as Antarctic Specially Protected Area (ASPA) No 128 by Decision 1 (2002). The Area lies within Antarctic Specially Managed Area (ASMA) No. 1 Admiralty Bay, King George Island, South Shetland Islands, designated under Measure 2 (2006). The biological and scientific values of the Area are vulnerable to human disturbance (e.g. oversampling, disturbance to wildlife, introduction of non-native species). Therefore, it is important that human activities in the Area are managed to minimize the risk of impacts. -
Grain Size Distribution of Bedload Transport in a Glaciated Catchment (Baranowski Glacier, King George Island, Western Antarctica)
water Article Grain Size Distribution of Bedload Transport in a Glaciated Catchment (Baranowski Glacier, King George Island, Western Antarctica) Joanna Sziło 1,* and Robert Józef Bialik 2 1 Institute of Geophysics, Polish Academy of Sciences, 01-452 Warsaw, Poland 2 Institute of Biochemistry and Biophysics, Polish Academy of Sciences, 02-106 Warsaw, Poland; [email protected] * Correspondence: [email protected]; Tel.: +48-504-595-266 Received: 20 February 2018; Accepted: 20 March 2018; Published: 23 March 2018 Abstract: The relationships among grain size distribution (GSD), water discharge, and GSD parameters are investigated to identify regularities in the evolution of two gravel-bed proglacial troughs: Fosa Creek and Siodło Creek. In addition, the potential application of certain parameters obtained from the GSD analysis for the assessment of the formation stage of both creeks is comprehensively discussed. To achieve these goals, River Bedload Traps (RBTs) were used to collect the bedload, and a sieving method for dry material was applied to obtain the GSDs. Statistical comparisons between both streams showed significant differences in flow velocity; however, the lack of significant differences in bedload transport clearly indicated that meteorological conditions are among the most important factors in the erosive process for this catchment. In particular, the instability of flow conditions during high water discharge resulted in an increase in the proportion of medium and coarse gravels. The poorly sorted fine and very fine gravels observed in Siodło Creek suggest that this trough is more susceptible to erosion and less stabilized than Fosa Creek. The results suggest that GSD analyses can be used to define the stage of development of riverbeds relative to that of other riverbeds in polar regions. -
Variabilidade Da Cobertura De Gelo Marinho E As Colônias De Pygoscelidae Na Costa Oeste Da Baia Do Almirantado, Ilha Rei George, Antártica
UNIVERSIDADE FEDERAL DO RIO GRANDE DO SUL INSTITUTO DE GEOCIÊNCIAS PROGRAMA DE PÓS-GRADUAÇÃO EM GEOCIÊNCIAS Variabilidade da cobertura de gelo marinho e as colônias de Pygoscelidae na costa oeste da baia do Almirantado, ilha Rei George, Antártica Ricardo Burgobraga Orientador: Prof. Dr. Jefferson Cardia Simões Banca examinadora: Prof. Dr. Elírio Toldo Júnior (UFRGS) Profa. Dr. Larissa de Oliveira Rosa (UNISINOS) Prof. Dr. Jean Carlos Budke (URI) Porto Alegre, janeiro de 2010 UNIVERSIDADE FEDERAL DO RIO GRANDE DO SUL INSTITUTO DE GEOCIÊNCIAS Programa de Pós-Graduação em Geociências Variabilidade da cobertura de gelo marinho e as colônias de Pygoscelidae na costa oeste da baía do Almirantado, ilha Rei George, Antártica Ricardo Burgobraga Orientador: Prof. Dr. Jefferson Cardia Simões Banca examinadora: Prof. Dr. Elírio Toldo Júnior (UFRGS) Profa. Dra. Larissa de Oliveira Rosa (UNISINOS) Prof. Dr. Jean Carlos Budke (URI) Dissertação de Mestrado submetida como requisito para obtenção do título de Mestre em Geociências. Porto Alegre, janeiro de 2010 ii Foto da capa: Anne Frolich (novembro de 2004) Um Pygoscelis antarctica descansando sobre um grunhão encalhado na ponta Demay, costa oeste da baía do Almirantado - ASPA 128. Dedico este trabalho à minha esposa Eloísa, que faz tudo isso ter mais sentido; aos meus pais, Rebeca e José e ao meu irmão, Regis. Todos ofertaram todo o amor, paciência e apoio durante esse projeto. Estes são os meus esteios. iii AGRADECIMENTOS Agradeço muitíssimo ao meu orientador, o Prof. Dr. Jefferson Cardia Simões, por ter me delegado toda a liberdade de conduzir este projeto, além das inúmeras oportunidades de treinamento e colaboração no Núcleo de Pesquisas Antárticas e Climáticas – NUPAC. -
Antarctic.V14.4.1996.Pdf
Antarctic Contents Foreword by Sir Vivian Fuchs Forthcoming Events Cover Story Scott Base 40 Years Ago by Margaret Bradshaw... Cover: Main: How Scott Base looks International today. Three Attempt a World Record Photo — Courtesy of Antarctica New Zealand Library. Solo-Antarctic Crossing National Programmes New Zealand United States of America France Australia Insert: Scott Base during its South Africa final building stage 1957. Photo — Courtesy of Guy on Warren. Education December 1996, Tourism Volume 1 4, No. 4, Echoes of the Past Issue No.l 59 Memory Moments Relived. ANTARCTIC is published quar terly by the New Zealand Antarctic Society Inc., ISSN Historical 01)03-5327, Riddles of the Antarctic Peninsula by D Yelverton. Editor: Shelley Grell Please address all editorial Tributes inquiries and contributions to the Editor, P O Box -104, Sir Robin Irvine Christchurch or Ian Harkess telephone 03 365 0344, facsimile 03 365 4255, e-mail Book Reviews [email protected]. DECEMBER 1996 Antargic Foreword By Sir Vivian Fuchs All the world's Antarcticians will wish to congratulate New Zealand on maintaining Scott Base for the last forty years, and for the valuable scientific work which has been accom plished. First established to receive the Crossing Party of the Commonwealth Trans- Antarctic Expedition 1955-58, it also housed the New Zealand P a r t y w o r k i n g f o r t h e International Geophysical Year. Today the original huts have been replaced by a more modern„. , j . , Sir andEdmund Hillaryextensive and Dr. V E.base; Fuchs join •'forces at. -
How the Western Frontiers Were Won with the Help of Geophysics
1 Controls on microalgal community structures in cryoconite 2 holes upon high Arctic glaciers, Svalbard 3 4 T.R. Vonnahme1,2,*, M. Devetter1,3, J. D. Žárský1,4, M. Šabacká1,5, J. Elster1,6 5 [1] {Centre for Polar Ecology, Faculty of Science, University of South Bohemia, České 6 Budějovice, Czech Republic} 7 [2] {University of Konstanz, Constance, Germany} 8 [3] {Biology Centre of the Academy of Science of the Czech Republic, Institute of Soil Biology, 9 České Budějovice, Czech Republic} 10 [4] {Department of Ecology, Charles University, Prague, Czech Republic} 11 [5] {British Antarctic Survey, Cambridge, UK} 12 [6] {Institute of Botany, Academy of the Science of the Czech Republic, Třeboň, Czech Republic} 13 [*] {now at: Max Planck Institute for Marine Microbiology, Bremen, Germany} 14 Correspondence to: J. Elster ([email protected]) 15 16 Abstract 17 Glaciers are known to harbor surprisingly complex ecosystems. On their surface, distinct 18 cylindrical holes filled with meltwater and sediments are considered as hot spots for microbial life. 19 The present paper addresses possible biological interactions within the community of prokaryotic 20 cyanobacteria and eukaryotic microalgae (microalgae) and relations to their potential grazers, such 21 as tardigrades and rotifers, additional to their environmental controls. Svalbard glaciers with 22 substantial allochthonous input of material from local sources reveal high microalgal densities. 23 Small valley glaciers with high sediment coverages and high impact of birds show high biomasses 24 and support a high biological diversity. Invertebrate grazer densities do not show any significant 25 negative correlation with microalgal abundances, but a positive correlation with eukaryotic 26 microalgae. -
An Analysis of Fungal Propagules Transported to the Henryk Arctowski Antarctic Station
vol. 34, no. 3, pp. 269–278, 2013 doi: 10.2478/popore−2013−0015 An analysis of fungal propagules transported to the Henryk Arctowski Antarctic Station Anna AUGUSTYNIUK−KRAM 1,2, Katarzyna J. CHWEDORZEWSKA3, Małgorzata KORCZAK−ABSHIRE 3, Maria OLECH 3,4 and Maria LITYŃSKA−ZAJĄC 5 1 Centrum Badań Ekologicznych PAN w Dziekanowie Leśnym, ul. M. Konopnickiej 1, 05−092 Łomianki, Poland <aaugustyniuk−kram@cbe−pan.pl> 2 Instytut Ekologii i Bioetyki, Uniwersytet Kardynała Stefana Wyszyńskiego w Warszawie, ul. Dewajtis 5, 01−815 Warszawa, Poland 3 Instytut Biochemii i Biofizyki PAN, Zakład Biologii Antarktyki, ul. Pawińskiego 5a, 02−106 Warszawa, Poland 4 Instytut Botaniki, Uniwersytet Jagielloński, ul. Kopernika 27, 31−512 Kraków, Poland 5 Instytut Archeologii i Etnologii PAN w Krakowie, ul. Sławkowska 17, 31−016 Kraków, Poland Abstract: During three austral summer seasons, dust and soil from clothes, boots and equip− ment of members of scientific expeditions and tourists visiting the Polish Antarctic Station Henryk Arctowski were collected and analysed for the presence of fungal propagules. Of a to− tal of 60 samples, 554 colonies of fungi belonging to 19 genera were identified. Colonies of the genus Cladosporium, Penicillium and non−sporulating fungus (Mycelia sterilia) domi− nated in the examined samples. The microbiological assessment of air for the presence of fungi was also conducted at two points in the station building and two others outside the sta− tion. A total of 175 fungal colonies belonging to six genera were isolated. Colonies of the ge− nus Penicillium were the commonest in the air samples. The potential epidemiological conse− quences for indigenous species as a result of unintentional transport of fungal propagules to the Antarctic biome are discussed in the light of rapid climate change in some parts of the Ant− arctic and adaptation of fungi to extreme conditions. -
Em Áreas Livres De Gelo Nas Ilhas Nelson E Rei George, Antártica Marítima
Revista Brasileira de Geomorfologia v. 22, nº 3 (2021) http://lsie.unb.br/ugb/ ISSN 2236-5664 http://dx.doi.org/10.20502/rbg.v22i3.1911 Artigo de Pesquisa Mudanças recentes (1988-2018) em áreas livres de gelo nas ilhas Nelson e Rei George, Antártica Marítima Recent changes (1988-2018) in ice-marginal environments of the King George and Nelson Island ice-free land areas, Maritime Antarctica Manoela Araujo Gonçalves de Oliveira(1), Kátia Kellem da Rosa(2), Carina Petsch(3), Rosemary Vieira(4), Felipe Casanova(5), Jefferson Cardia Simões (6) 1 Centro Polar e Climático, Programa de Pós-Graduação em Geografia - UFRGS, Porto Alegre, RS, Brasil. [email protected] ORCID: https://orcid.org/0000-0003-4661-7316 2 Departamento de Geografia, Centro Polar e Climático, Programa de Pós-Graduação em Geografia - UFRGS, Porto Alegre, RS, Brasil. [email protected] ORCID: https://orcid.org/0000-0003-0977-9658 3 Departamento de Geociências – UFSM, Santa Maria, RS, Brasil. Centro Polar e Climático, UFRGS, Porto Alegre, RS, Brasil. [email protected] ORCID: http://orcid.org/0000-0002-1079-0080 4 Laboratório de Processos Sedimentares e Ambientais, Depto de Geografia – UFF, Niterói, RJ, Brasil [email protected] ORCID: https://orcid.org/0000-0003-0312-2890 5 Centro Polar e Climático, UFRGS, Porto Alegre, RS, Brasil, [email protected] ORCID: https://orcid.org/0000-0002-3626-7853 6 Departamento de Geografia, Centro Polar e Climático, Programa de Pós-Graduação em Geografia - UFRGS, Porto Alegre, RS, Brasil. jefferson.simõ[email protected] ORCID: https://orcid.org/0000-0001-5555-3401 Recebido: 11/12/2020; Aceito: 17/05/2021; Publicado: 01/07/2021 Resumo: O objetivo deste trabalho é comparar as variações dos lagos e geleiras apresentadas por diferentes setores de áreas livres de gelo nas ilhas Rei George (IRG) e Nelson (IN) no período 1988-2018.