Australian Antarctic Magazine — Issue 7
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2016 Heard Island Expedition Project Description
2016 Heard Island Expedition Project Description Definition TITLE BIOGEOCHEMICAL COMPOSITION OF THE SUBGLACIAL REGIME ON HEARD ISLAND USING GLACIAL STREAMS AS REMOTE SAMPLING PROBES Abstract We plan to examine the chemical composition and particulate loads of glacial streams at Heard Island as a probe of the geochemical and geophysical composition of the parent rocks, and the microbiological activity of the subglacial till. Given the impressive size and discharge of many of these streams, and their deposition of large amounts of fine sediment in various lagoons and the ocean, these streams are obviously transporting large amounts of material from underneath the glaciers. Lixiviation and direct solution will add solutes to the meltwater, providing a clear chemical signature in samples taken downstream. In addition, subglacial till is a refugium for microbial life which will be carried in the runoff. This work will consist of collecting samples from as many streams as possible, followed by laboratory characterization of the particulates, solutes, and bioactive components. Principal Investigator Fred Belton Cordell Expeditions Principal Investigator Robert Schmieder Cordell Expeditions Co-Investigator Gavin Marshall Tangaroa Blue Foundation Co-Investigator William Mitchell Cordell Expeditions Co-Investigator Staff U. S. Geological Survey Co-Investigator Carlos Nascimento Biochemist Co-Investigator Patrick Quilty University of Tasmania Co-Investigator Maria Hauger Consultant Co-Investigator Onsite team members Cordell Expeditions Context Background Satellite images of Heard Island taken in 2014 have sufficient resolution to exhibit many glacial melt streams, clearly seen as they approach the shoreline and disappear into the ocean, some entering lagoons depositing large amounts of fine sediment. Most of these streams, especially the longer ones (descending up to 3 km) show classic meanders with periods ca. -
49°S, 69°E) Between 1963 and 2006 Etienne Berthier, Raymond Le Bris, Laure Mabileau, L
Ice wastage on the Kerguelen Islands (49°S, 69°E) between 1963 and 2006 Etienne Berthier, Raymond Le Bris, Laure Mabileau, L. Testut, Frédérique Rémy To cite this version: Etienne Berthier, Raymond Le Bris, Laure Mabileau, L. Testut, Frédérique Rémy. Ice wastage on the Kerguelen Islands (49°S, 69°E) between 1963 and 2006. Journal of Geophysical Research, American Geophysical Union, 2009, 114, pp.F03005. 10.1029/2008JF001192. hal-00406745 HAL Id: hal-00406745 https://hal.archives-ouvertes.fr/hal-00406745 Submitted on 23 Jul 2009 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Ice wastage on the Kerguelen Islands (49°S, 69°E) between 1963 and 2006. Berthier E. 1*, Le Bris R. 2, Mabileau L. 1, Testut L. 3 & Rémy F. 1 1 LEGOS, CNRS, 14 avenue Edouard Belin, F-31400 Toulouse, CEDEX 9, France. 2 Department of Geography, University of Zurich, Winterthurerstrasse 190, CH-8057 Zurich, Switzerland. 3 Université de Toulouse; UPS (OMP-PCA); LEGOS; 14 Av. Edouard Belin, F-31400 Toulouse, France. * corresponding author [email protected] Citation : Berthier, E., Le Bris, R., Mabileau, L., Testut, L., & Rémy, F. -
State of the Antarctic and Southern Ocean Climate System Paul Andrew Mayewski University of Maine, [email protected]
The University of Maine DigitalCommons@UMaine Earth Science Faculty Scholarship Earth Sciences 1-2009 State of the Antarctic and Southern Ocean Climate System Paul Andrew Mayewski University of Maine, [email protected] M. P. Meredith C. P. Summerhayes J. Turner A. Worby See next page for additional authors Follow this and additional works at: https://digitalcommons.library.umaine.edu/ers_facpub Part of the Climate Commons, Glaciology Commons, Hydrology Commons, and the Meteorology Commons Repository Citation Mayewski, Paul Andrew; Meredith, M. P.; Summerhayes, C. P.; Turner, J.; Worby, A.; Barrett, P. J.; Casassa, G.; Bertler, Nancy; Bracegirdle, T.; Naveira Garabato, A. C.; Bromwich, D.; Campbell, H.; Hamilton, Gordon S.; Lyons, W. B.; Maasch, Kirk A.; Aoki, S.; Xiao, C.; and van Ommen, Tas, "State of the Antarctic and Southern Ocean Climate System" (2009). Earth Science Faculty Scholarship. 272. https://digitalcommons.library.umaine.edu/ers_facpub/272 This Article is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Earth Science Faculty Scholarship by an authorized administrator of DigitalCommons@UMaine. For more information, please contact [email protected]. Authors Paul Andrew Mayewski, M. P. Meredith, C. P. Summerhayes, J. Turner, A. Worby, P. J. Barrett, G. Casassa, Nancy Bertler, T. Bracegirdle, A. C. Naveira Garabato, D. Bromwich, H. Campbell, Gordon S. Hamilton, W. B. Lyons, Kirk A. Maasch, S. Aoki, C. Xiao, and Tas van Ommen This article is available at DigitalCommons@UMaine: https://digitalcommons.library.umaine.edu/ers_facpub/272 STATE OF THE ANTARCTIC AND SOUTHERN OCEAN CLIMATE SYSTEM P. -
Heard and Mcdonald Islands Australia
HEARD AND MCDONALD ISLANDS AUSTRALIA Heard Island and the McDonald Islands are in the Southern Ocean, approximately 4,100 km south- west of Perth and 1,700 km from the Antarctic continent. Their distinctive conservation value is as one of the world’s rare pristine island ecosystems which have virtually no record of alien species and minimal human impact; also as the only volcanically active subantarctic islands they provide a window into ongoing tectonic activity, geomorphic processes and glacial dynamics. COUNTRY Australia NAME Heard and McDonald Islands NATURAL WORLD HERITAGE SERIAL SITE 1997: Inscribed on the World Heritage List under Natural Criteria viii and ix. STATEMENT OF OUTSTANDING UNIVERSAL VALUE [pending] The UNESCO World Heritage Committee issued the following statement at the time of inscription: Justification for Inscription The Committee inscribed this property under criteria (viii) and (ix). It noted that this site is the only volcanically active sub-Antarctic island and illustrates ongoing geomorphic processes and glacial dynamics in the coastal and submarine environment and sub-Antarctic flora and fauna, with no record of alien species. The Committee repeated its request by the sixteenth session for further documentation on the marine resources of the site. IUCN MANAGEMENT CATEGORY 1a Strict Nature Reserve BIOGEOGRAPHICAL PROVINCE Insulantarctica (7.4.9) GEOGRAPHICAL LOCATION Located in the southern Indian Ocean 4,100 km south-west of Australia and 1,700 km north of Mawson Base, Antarctica. Heard Island is at 53°06'S by 73°30'E with the McDonald Islands 43.5 km west of it at 53°03'S by 72°36'E. -
Origin and Evolution of the Sub-Antarctic Islands: the Foundation
Papersnd a Proceedings of the Royal Society of Tasmania, Volume 141 (1), 2007 35 ORIGIN AND EVOLUTION OF THE SUB-ANTARCTIC ISLANDS: THE FOUNDATION by Patrick G. Quilty (with 23 text-figures and two tables) Quilty, P.G. 2007 (23:xi): Origin and evolution of the sub-Antarctic islands: the foundation.Papers and Proceedings of the Royal Society of Tasmania 141 (1): 35-58. https://doi.org/10.26749/rstpp.141.1.35 ISSN 0080-4703. School of Earth Sciences, University of Tasmania, Private Bag 79, Hobart, Tasmania 7001, Australia. Email: P.Quil [email protected] Sub-Antarctic islands have a diversity of origins in detail but most are volcanic and very young suggesting that they are short-lived and that the distribution would have been very differenta few million years ago. 'They contrast with the common tourist brochure concept of oceanic islands. As the Antarctic Plate is virtually static, the islands seldom show signs of association with long-lived linear island chains and most thus stand alone. Longer-lived islands are either on submarine plateaux or are continental remnants of the dispersion of Gondwana. The islands are classified in relation to raised sea-floor, transform fault, triple junction, subduction zone, submarine plateau, submerged continent or continental. Many are difficult of access and poorly known geologically. Their geological history controls their many other roles such as sites as observatories, or for study of colonisation, evolution and speciation rates. Key Words: Sub-Antarctic islands, geological evolution, Macquarie Island, Balleny Islands, Scott Island, Campbell Island, Antipodes Island, Auckland Islands, Enderby Island, Peter I Island, Islas Diego Ramirez, South Georgia, South Sandwich Islands, Bouvetoya, Gough Island, Marion Island, Prince Edward Island, Iles Crozet, Amsterdam Island, St Paul Island, Kerguelen Plateau, Iles Kerguelen, Heard Island, McDonald Island. -
CHANGES in HEARD ISLAND GLACIERS, KING PENGUINS and Furby SEALS G
Papers and Proceedings of the Royal Society of Tasmania, Volume 133(2), 2000 47 CHANGES IN HEARD ISLAND GLACIERS, KING PENGUINS AND FURby SEALS G. M. Budd SINCE 1947 (with two tables, three text-figures and one plate) BUDD, G.M., 2000 (30:vi): Changes in Heard Island glaciers, king penguins and fur seals since 1947. In Banks M.R. & Brown, M.]. (Eds): HEARD ISLAND Pap. Proc. R. Soc. Tasm. 133 (2): 47-60. https://doi.org/10.26749/rstpp.133.2.47 ISSN 0080-4703. School of Exercise and RS. Sport Science, The University of Sydney, PO Box 170, Lidcombe, NSW, Australia 2141. The purpose of this paper is to summarise and discuss the changes in glaciers, king penguins and fur seals reported by the nine wintering parties and 11 summer expeditions that have visited Heard Island since 1947, with emphasis upon those of the years between 1947 and 1971. These early years were notable for an initial period (1947-55) of minimal change, and a subsequent period(1963-71) of rapid change in which a complex pattern of asynchronous glacier retreat and readvance was observed and the main features of the island's recolonisation by king penguins and fur seals were established. Subsequent expeditions (1980-93) have reported continuing glacier recession, evidently in response to warmer air temperatures, and a continuing exponential increase in king penguins and fur seals. The glacier observations show that the Heard Island glaciers are sensitive indicators of climate change in the Southern Ocean, and of the interactions between climate and glacier topography. The island's recolonisation by king penguins and fur seals is attributed mainly to an improved food supply which may itself, like the glacier recession, be a response to changes in atmospheric and oceanic circulation. -
Heard Island and Mcdonald Islands Australia
HEARD ISLAND AND MCDONALD ISLANDS AUSTRALIA McDonald Island with Meyer Aock in background(G. Johnstone) Heard Island and McDonald Islands (Australia) 11 WORLD HERITAGE NOMINATION - IUCN TECHNICAL EVALUATION HEARD ISLAND AND MCDONALD ISLANDS (AUSTRALIA) 1. DOCUMENTATION (i) IUCNAVCMC Data Sheet(25 references) (ii) Additional Literature Consulted: Keage, P. 1987. Additional Protective Measures for Heard Island and the McDonald Islands. b Conserving the Natural Heritage of the Antarctic Realm. IUCN. 1991. A Strategy for Antarctic Conservation. 85 p; IUCN/SCAR. 1994. Developing The Antarctic Protected Area System. 137~. Clarke, M.R. and P. Dingwall. 1995. Conservation of Islands in the Southern Ocean. IUCN. 18Op.; Thorsell, J. 1993. Which Islands Merit World Heritage Status? Insula No 2; Dingwall, P. 1995. Ranking the World Heritage Values of Islands in the Southern Ocean. Report to IUCN 8p. (iii) Consultations: (1992 evaluation) 7 external reviewers. (Second evaluation) 5 external reviewers including members of the IUCN Antarctic Advisory Committee. (iv) Field Visit: None 2. SUMMARY OF NATURAL VALUES The Territory of Heard Island and McDonald Islands (HIMI), an external territory of Australia, consists of a remote group of islands in the Southern Ocean. The nominated property comprises the islands and all offshore rocks and shoals, out to the 12 nautical mile limit for a total area of 6,734 km’. HIM1 are limestone and volcanic accumulations located on the submarine Kerguelen Plateau. Heard Island is dominated by the Big Ben massif, with the volcanically active 2,745m Mawson Peak (the only active volcano in Australia territory). Heard Island is heavily glaciated, with ice cliffs forming a high percentageof the coastline. -
HEARD ISLAND and the Mcdonald ISLANDS: a WINDOW INTO the KERGUELEN PLATEAU
Papers and Proceedings of the Royal Society of Tasmania, Vulurne 2000 1 HEARD ISLAND AND THE McDONALD ISLANDS: A WINDOW INTO THE KERGUELEN PLATEAU by Patrick G. Quilty and Graeme Wheller (with four text.·flgures) QUILTY, P.G. & WHELLER, G.E., 2000 (30:vi): Heard Island and the McDonald Islands: a window into the Kerguelen Plateau. In Banks, MR & Brown, M.J. (Eds); HEARD ISLAND PAPERS. Pap. Proc. R. Soc. Tasm. 133(2): 1~12. ISSN 0080~4703. School of Earth Sciences, University of Tasmania, GPO Box 252-79, Hobart, Tasmania, Australia 7001 (PGQ); Volcanex International Pty Ltd, Suite 4,286 Macquarie St, South Hobart, Tasmania, Australia 7004 (GW). The modem phase of volcanism on Heard Island probably is younger than one million years and is responsible for building Big Ben, the bulk of the island. The nearby McDonald Islands are less than 100 000 years old and are volcanically active. Big Ben sits on (he Drygalski Formation, a Late Miocenc~Early Pliocene volcanic/marine sediment with glacial influence, which occurs as a generally fiat-lying, diff forming unit over most of Heard Island. The "basement" of Palaeogene limestone crops out mainly on Laurens Peninsula but also sporadically heneath Big Ben and occurs as clasts in volcanics. Historical eruptions of Heard Island, most recently from 1985 to at least 1992 and probahly later, have occurred from Mawson Peak, the summit cone built upon Big Ben, bur young lavas and ash cones afe widespread around the island. Recent volcanic activity is summarised. Heard Island and the McDonald Islands, with the Kerguelen Islands, are exposed parts of the Kerguelen Plateau, possibly the largest submarine plateau on earth, and provide geochemical and isotopic insights into the formation of oceanic plateaux, mantle plume development and the separation of Australia, India and Africa from Antarctica. -
Glaciers on Heard Island
2016 Heard Island Expedition Project Description Definition TITLE MACROSCOPIC INCLUSIONS IN RETREATING GLACIERS ON HEARD ISLAND Abstract The termini, margins, and immediate vicinity of selected glaciers on Heard Island will be examined for macroscopic inclusions. Significant items exposed due to retreat of the glacier will be documented and collected for laboratory analysis. Principal Investigator Fred Belton Cordell Expeditions Co-Investigator Robert Schmieder Cordell Expeditions Co-Investigator Gavin Marshall Tangaroa Blue Foundation Co-Investigator William Mitchell Cordell Expeditions Co-Investigator Grahame Budd University of Sydney Co-Investigator Nezamoddin Nezamoddini-Kachouie Florida Institute of Technology Co-Investigator Onsite team members Cordell Expeditions Context Background Besides the episodic volcanic activity of Big Ben, perhaps the most obvious dynamic process occurring on Heard Island is the retreat of the glaciers. The extraordinarily high rates of retreat, especially of the Stephenson Glacier (up to 100 m/y), are among the highest in the world. The following map shows historical changes between 1947 and 2009. There is, however, evidence that retreat since 2009 has continued, and even accelerated. Source: Lucieer, et al. 2009. Kiernan and McConnell (2002) provide the following: Rates of both glacier retreat and melt-lake enlargement have increased by about one order 2016 Heard Island Expedition Project GLACIERS Updated 1/12/2016 4:18 PM Page 1 of 16 of magnitude during the last two decades. Precise ice-volume loss cannot presently be calculated, but about 30% of the cross-sectional area of the terminal zone of Stephenson Glacier above sea level has vanished in the past three decades. That accelerated melting of older ice-cored moraines is contributing so significantly to melt-lake expansion rather than it being the product solely of glacier recession perhaps emphasizes the significance of temperature increases in causing environmental change on Heard Island. -
Heard Island and Mcdonald Islands Marine Reserve Management Plan 2014–2024
Australian Antarctic Division Heard Island and McDonald Islands Marine Reserve Management Plan 2014-2024 ISBN: 978-1876934-255 This publication is available on the internet at: http://heardisland.antarctica.gov.au/ It is also available from the Department of Environment at [email protected] or freecall 1800 803 772. This publication should be cited as: Commonwealth of Australia (2014). Heard Island and McDonald Islands Marine Reserve Management Plan 2014-2024, Department of the Environment, Canberra. © Commonwealth of Australia 2014 This work is copyright. You may download, display, print and reproduce this material in unaltered form only (retaining this notice) for your personal, non-commercial use or use within your organisation. Apart from any use as permitted under the Copyright Act 1968, all other rights are reserved. Requests and enquiries concerning reproduction and rights should be addressed to Department of the Environment, Public Affairs, GPO Box 787, Canberra ACT 2601 or email [email protected]. Disclaimer The contents of this document have been compiled using a range of source materials and are valid as at October 2014. The Australian Government is not liable for any loss or damage that may be occasioned directly or indirectly through the use of or reliance on the contents of the document. All images in this publication by: Dr. Matt Curnock Contents Part 1 Foreword and acknowledgements iii Part 2 A description of the Reserve 3 Part 3 Management plan for the Reserve 13 1. Introductory Background 14 1.1 Proclamation of the Reserve 14 1.2 Conservation significance of the Reserve 14 1.3 Previous management plans 16 1.4 Structure of this management plan 16 2. -
Final Report of the Twenty-Ninth Antarctic Treaty Consultative Meeting
Final Report of the Twenty-ninth Antarctic Treaty Consultative Meeting ANTARCTIC TREATY CONSULTATIVE MEETING Final Report of the Twenty-ninth Antarctic Treaty Consultative Meeting Edinburgh, United Kingdom 12 – 23 June 2006 Secretariat of the Antarctic Treaty Buenos Aires 2006 Antarctic Treaty Consultative Meeting (29th : 2006 : Edinburgh) Final Report of the Twenty-ninth Antarctic Treaty Consultative Meeting. Edinburgh, United Kingdom, 12-23 June 2006. Buenos Aires : Secretariat of the Antarctic Treaty, 2006. 564 p. ISBN 987-23163-0-9 1. International law – Environmental issues. 2. Antarctic Treaty System. 3. Environmental law – Antarctica. 4. Environmental protection – Antarctica. DDC 341.762 5 ISBN-10: 987-23163-0-9 ISBN-13: 978-987-23163-0-3 CONTENTS Acronyms and Abbreviations 9 I. FINAL REPORT 11 II. MEASURES, DECISIONS AND RESOLUTIONS 49 A. Measures 51 Measure 1 (2006): Antarctic Specially Protected Areas: Designations and Management Plans 53 Annex A: ASPA No. 116 - New College Valley, Caughley Beach, Cape Bird, Ross Island 57 Annex B: ASPA No. 127 - Haswell Island (Haswell Island and Adjacent Emperor Penguin Rookery on Fast Ice) 69 Annex C: ASPA No. 131 - Canada Glacier, Lake Fryxell, Taylor Valley, Victoria Land 83 Annex D: ASPA No. 134 - Cierva Point and offshore islands, Danco Coast, Antarctic Peninsula 95 Annex E: ASPA No. 136 - Clark Peninsula, Budd Coast, Wilkes Land 105 Annex F: ASPA No. 165 - Edmonson Point, Wood Bay, Ross Sea 119 Annex G: ASPA No. 166 - Port-Martin, Terre Adélie 143 Annex H: ASPA No. 167 - Hawker Island, Vestfold Hills, Ingrid Christensen Coast, Princess Elizabeth Land, East Antarctica 153 Measure 2 (2006): Antarctic Specially Managed Area: Designation and Management Plan: Admiralty Bay, King George Island 167 Annex: Management Plan for ASMA No. -
Conserving Antarctic Biodiversity in the Anthropocene
Conserving Antarctic biodiversity in the Anthropocene Jasmine Lee A thesis submitted for the degree of Doctor of Philosophy at The University of Queensland in 2018 School of Biological Sciences Centre for Biodiversity and Conservation Science Abstract Anthropogenic activity threatens biodiversity worldwide, with the species and ecosystems of even the most remote and largest remaining wilderness at risk. In Antarctica, human activity is growing, barriers to invasive species establishment are being lowered, pollution is pervasive, and climate change directly and indirectly threatens taxa across the region. This has the potential to impact some of the world’s most unusual, isolated, and highly-adapted species. Evolving in isolation for long periods, a number of specialised lower plants and invertebrates dominate Antarctic ecosystems, with mosses, lichens, microbes, arthropods and soil microfauna present across the continent. Seals and seabirds breed in coastal regions and two flowering plants survive in the milder conditions of the Antarctic Peninsula. In this thesis I provide crucial impact assessments for some of the key processes threatening Antarctic biodiversity, and produce the first inclusive, continent-wide prioritisation of management strategies for conserving Antarctic biodiversity in the face of multiple threats, which will help to inform decision makers in identifying cost-effective conservation strategies. The vast majority of Antarctic life survives only in the less than 1% of the Antarctic continent that is permanently ice-free, where soils and rocks areas emerge as nunataks, dry valleys, cliffs, fellfields, and coastal oases. Despite being crucial habitat, we have limited understanding of how ice-free areas will be impacted by climate change. In Chapter 2 I use temperature-index melt modelling to determine the potential impacts of climate change on Antarctic biodiversity habitat.