Heard Island and Mcdonald Islands Australia
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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. -
Iucn Summary Gough Island (United Kingdom) 2
WORLD HERITAGE NOMINATION - IUCN SUMMARY GOUGH ISLAND (UNITED KINGDOM) Summary prepared by IUCN/WCMC (March 1995) based on the original nomination supplied by the Government of the United Kingdom. This original and all documents in support of this nomination will be available for consultation at the meetings of the Bureau and the Committee. 1. LOCATION Located southeast of Tristan da Cunha Island in the south Atlantic Ocean, midway between Africa and South America. 2. JURIDICAL DATA The island and surrounding territorial waters were designated a wildlife area in 1976 under the Tristan da Cunha Conservation Ordinance. 3. IDENTIFICATION The island of Gough (6500ha) represents the eroded core of a Late Tertiary volcano. The east side of the island is dissected by a series of deep steep-sided valleys, which are separated by narrow serrated ridges. Along the west side of the island, rounded slopes extend from the central plateau to the western sea cliffs. Many offshore stacks and rocks are present, mostly within 100m of the main island. Vegetation comprises tussock grass around the coast and wet heath with moss and feldmark, and bog and swamp communities at higher elevations. Knowledge of the flora is incomplete but consists of some 35 native flowering plant and 28 native fern species. Over 30 of Gough's vascular plant taxa are endemic to the Tristan de Cunha islands. A total of 146 bryophytes have been recorded, eight of which are endemic, together with 20 fungi and 24 lichens. Invertebrate fauna also remains poorly known, but comprises 100 species, eight of which are endemic. -
A Global Overview of Protected Areas on the World Heritage List of Particular Importance for Biodiversity
A GLOBAL OVERVIEW OF PROTECTED AREAS ON THE WORLD HERITAGE LIST OF PARTICULAR IMPORTANCE FOR BIODIVERSITY A contribution to the Global Theme Study of World Heritage Natural Sites Text and Tables compiled by Gemma Smith and Janina Jakubowska Maps compiled by Ian May UNEP World Conservation Monitoring Centre Cambridge, UK November 2000 Disclaimer: The contents of this report and associated maps do not necessarily reflect the views or policies of UNEP-WCMC or contributory organisations. The designations employed and the presentations do not imply the expressions of any opinion whatsoever on the part of UNEP-WCMC or contributory organisations concerning the legal status of any country, territory, city or area or its authority, or concerning the delimitation of its frontiers or boundaries. TABLE OF CONTENTS EXECUTIVE SUMMARY INTRODUCTION 1.0 OVERVIEW......................................................................................................................................................1 2.0 ISSUES TO CONSIDER....................................................................................................................................1 3.0 WHAT IS BIODIVERSITY?..............................................................................................................................2 4.0 ASSESSMENT METHODOLOGY......................................................................................................................3 5.0 CURRENT WORLD HERITAGE SITES............................................................................................................4 -
The Adaptations of Antarctic Dinosaurs "Exploration Is the Physical Expression of the Intellectual Passion
The Adaptations of Antarctic Dinosaurs "Exploration is the physical expression of the Intellectual Passion. And I tell you, if you have the desire for knowledge and the power to give it physical expression, go out and explore. If you are a brave man you will do nothing: if you are fearful you may do much, for none but cowards have need to prove their bravery. Some will tell you that you are mad, and nearly all will say, "What is the use?" For we are a nation of shopkeepers, and no shopkeeper will look at research which does not promise him a financial return within a year. And so you will sledge nearly alone, but those with whom you sledge will not be shopkeepers: that is worth a good deal. If you march your Winter Journeys you will have your reward, so long as all you want is a penguin's egg." —Apsley Cherry-Garrard, "The Worst Journey in the World" Life Long Ago in the Antarctic Long ago during the age of the dinosaurs the basics of life and survival were not so different from today. Life was in great abundance and creatures of all sizes walked, stomped, crept and slunk all over the earth. Although many of the animals have changed and disappeared, the way all animals live have remained the same. They still need to eat, sleep and be safe. They still all strive to find way to raise a family and be happy. This was true even 185 million years ago in the continent we now call Antarctica. -
New Zealand Subantarctic Islands Research Strategy
New Zealand Subantarctic Islands Research Strategy SOUTHLAND CONSERVANCY New Zealand Subantarctic Islands Research Strategy Carol West MAY 2005 Cover photo: Recording and conservation treatment of Butterfield Point fingerpost, Enderby Island, Auckland Islands Published by Department of Conservation PO Box 743 Invercargill, New Zealand. CONTENTS Foreword 5 1.0 Introduction 6 1.1 Setting 6 1.2 Legal status 8 1.3 Management 8 2.0 Purpose of this research strategy 11 2.1 Links to other strategies 12 2.2 Monitoring 12 2.3 Bibliographic database 13 3.0 Research evaluation and conditions 14 3.1 Research of benefit to management of the Subantarctic islands 14 3.2 Framework for evaluation of research proposals 15 3.2.1 Research criteria 15 3.2.2 Risk Assessment 15 3.2.3 Additional points to consider 16 3.2.4 Process for proposal evaluation 16 3.3 Obligations of researchers 17 4.0 Research themes 18 4.1 Theme 1 – Natural ecosystems 18 4.1.1 Key research topics 19 4.1.1.1 Ecosystem dynamics 19 4.1.1.2 Population ecology 20 4.1.1.3 Disease 20 4.1.1.4 Systematics 21 4.1.1.5 Biogeography 21 4.1.1.6 Physiology 21 4.1.1.7 Pedology 21 4.2 Theme 2 – Effects of introduced biota 22 4.2.1 Key research topics 22 4.2.1.1 Effects of introduced animals 22 4.2.1.2 Effects of introduced plants 23 4.2.1.3 Exotic biota as agents of disease transmission 23 4.2.1.4 Eradication of introduced biota 23 4.3 Theme 3 – Human impacts and social interaction 23 4.3.1 Key research topics 24 4.3.1.1 History and archaeology 24 4.3.1.2 Human interactions with wildlife 25 4.3.1.3 -
Is It All Going South? Four Future Scenarios for Antarctica
Polar Record 53 (5): 459–478 (2017). © Cambridge University Press 2017. This is an Open Access article, 459 distributed under the terms of the Creative Commons Attribution licence (http:// creativecommons.org/ licenses/ by/ 4.0/ ), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. doi:10.1017/S0032247417000390 Is it all going south? Four future scenarios for Antarctica Daniela Liggett Gateway Antarctica, University of Canterbury, Private Bag 4800, 8140 Christchurch, New Zealand Bob Frame Landcare Research, PO Box 69040, Lincoln 7640, New Zealand ([email protected]) Neil Gilbert Constantia Consulting, 310 Papanui Road, Christchurch 8052, New Zealand Fraser Morgan Landcare Research, Private Bag 92170, Auckland Mail Centre, Auckland 1142, New Zealand Received December 2016; first published online 11 September 2017 ABSTRACT. The future is uncertain for Antarctica, with many possibilities – some more plausible, others more preferable. Indeed, the region and its governance regime may be reaching (or may have reached) a crossroads moment as a result of a series of challenges, including the changing Antarctic climate and environment, increasing human activity, shifting values among Antarctic states and a low-cost, somewhat benign governance regime (the Antarctic Treaty System). Within this context there are a number of interdependent drivers that are likely to influence Antarctica’s future over, say, 25 years: global environmental and socio-economic developments; Antarctic governance; Antarctic research, including national Antarctic programme operations; and Antarctic tourism. The research presented here involved a thorough examination of Antarctic literature on current Antarctic developments and challenges, and an assessment of global trends. -
Climate Change and Southern Ocean Resilience REPORT from an INTERDISCIPLINARY SCIENTIFIC WORKSHOP
POLAR PERSPECTIVES No. 5 Summary l June 2021 Icebergs with adélie penguins on top flow near Antarctic peninsula. ©Jo Crebbin/Shutterstock Climate Change and Southern Ocean Resilience REPORT FROM AN INTERDISCIPLINARY SCIENTIFIC WORKSHOP Introduction and Executive Summary for Policymakers I. INTRODUCTION BY EVAN T. BLOOM1 the Antarctic ice sheets and shelves. New research on the Antarctic Ice Sheet indicates that rapid sea- As the world prepares for the Glasgow Climate level rise from Antarctica will be triggered if Paris Change Conference in November 2021, there is Agreement targets (2°C warming in the twenty-first considerable focus on the Southern Ocean. The century) are exceeded. A recent article notes that, if international community has come to realize that the current emissions rates continue and put the world polar regions hold many of the keys to unlocking our on course towards 3°C warming, this tipping point understanding of climate-related phenomena - and will be reached by 2060, and no human intervention, thus polar science will influence policy decisions on including geoengineering, would be able to stop 17 to which our collective futures depend. 21 centimeters (cm) of sea-level rise from Antarctic ice melt alone by 21002. Global sea-level rise is linked to future melting of 2. R.M. DeConto, D. Pollard, R.B. Alley, I. Velicogna, E. Gasson, N. Gomez, S. Sadai, A. Condron, 1. Senior Fellow, Wilson Center Polar Institute and former U.S. Commissioner to D.M. Gilford, E.L. Ashe, R.E. Kopp, D. Li, A. Dutton, The Paris Climate Agreement and future sea-lev- CCAMLR. -
A Global Overview of Wetland and Marine Protected Areas on the World Heritage List
A GLOBAL OVERVIEW OF WETLAND AND MARINE PROTECTED AREAS ON THE WORLD HERITAGE LIST A Contribution to the Global Theme Study of World Heritage Natural Sites Prepared by Jim Thorsell, Renee Ferster Levy and Todd Sigaty Natural Heritage Programme lUCN Gland, Switzerland September 1997 WORLD CONSERVATION MONITORING CENTRE lUCN The World Conservation Union 530S2__ A GLOBAL OVERVIEW OF WETLAND AND MARINE PROTECTED AREAS ON THE WORLD HERITAGE LIST A Contribution to the Global Theme Study of Wodd Heritage Natural Sites Prepared by Jim Thorsell. Renee Ferster Levy and Todd Sigaty Natural Heritage Program lUCN Gland. Switzerland September 1997 Working Paper 1: Earth's Geological History - A Contextual Framework Assessment of World Heritage Fossil Site Nominations Working Paper 2: A Global Overview of Wetland and Marine Protected Areas on the World Heritage List Working Paper 3; A Global Overview of Forest Protected Areas on the World Heritage List Further volumes (in preparation) on biodiversity, mountains, deserts and grasslands, and geological features. Digitized by tine Internet Arciiive in 2010 witii funding from UNEP-WCIVIC, Cambridge littp://www.arcliive.org/details/globaloverviewof97glob . 31 TABLE OF CONTE>rrS PAGE I. Executive Summary (e/f) II. Introduction 1 III. Tables & Figures Table 1 . Natural World Heritage sites with primary wetland and marine values 1 Table 2. Natural World Heritage sites with secondary wetland and marine values 12 Table 3. Natural World Heritage sites inscribed primarily for their freshwater wetland values 1 Table 4. Additional natural World Heritage sites with significant freshwater wetland values 14 Tables. Natural World Heritage sites with a coastal/marine component 15 Table 6. -
And Registration Tea/Coffee Welcome Address
Wednesday 4th November 09:00 Welcome and registration Tea/Coffee David Vaughan : 09:15 Welcome address Director of Science Session 1: Land 09:30 Jennifer Brown Seasonal penguin colony colour change at Signy, Antarctica 09:50 Elise Biersma First evidence of long-term persistence of mosses in Antarctica 10:10 Tun Jan Young Resolving flow and deformation of store glacier, west Greenland using FMCW radar 10:30 Tea/Coffee Session 2: Air 10:50 Ian White Dynamical response to the equatorial QBO in the northern winder extratropical stratosphere 11:20 Michelle McCrystall Modelling the influence of remote teleconnection on Arctic climate variability 11:40 Jenny Turton Spatial and temporal characteristics of foehn winds over the Larsen ice shelf 12:00 Hoi Ga Chan Modelling nitrogen oxide emission from snow 12:20 Lunch 13:30 Hayley Allison Tracey Dornan Irene Malmierca Zoe Roseby First year welcome Jesamine Bartlett Rebecca Frew Christine McKenna Felipe Lorenz Simoes David Buchanan Tom Hudson Emily Potter Rebecca Vignols Harriet Clewlow Amy King 13:45 David Vaughan Keynote talk 1: “Ice sheets, climate and sea-level” Session 3: Water: Circulation 14.15 Lewis Drysdale The seasonal distribution of freshwater from meteoric sources and sea ice melt in Svalbard fjords 14.35 Heather Regan Sources and fate of freshwater in the ocean west of the Antarctic Peninsula 14.55 Ewa Karczewska 3-D transport pathways from the southern ocean 15:15 Tea/Coffee 15.45 Ryan Patmore Making a gyre, the southern ocean way 16.05 Erik Mackie Has Antarctica ice loss altered the -
Quaternary Colonization of Sub-Antarctic Marion Island by the Limpet Genus Nacella (Patellogastropoda: Nacellidae)
CORE Metadata, citation and similar papers at core.ac.uk Provided by HAL-uB Polar Biol (2016) 39:77–89 DOI 10.1007/s00300-014-1620-9 ORIGINAL PAPER Out of Antarctica: quaternary colonization of sub-Antarctic Marion Island by the limpet genus Nacella (Patellogastropoda: Nacellidae) Claudio A. Gonza´lez-Wevar • Steven L. Chown • Simon Morley • Nestor Coria • Thomas Sauce´de • Elie Poulin Received: 29 January 2014 / Revised: 3 November 2014 / Accepted: 12 November 2014 / Published online: 29 November 2014 Ó Springer-Verlag Berlin Heidelberg 2014 Abstract The distribution of the Southern Ocean near- Nacella concinna and its sub-Antarctic relative Nacella shore marine benthic fauna is the consequence of major delesserti from Marion Island stands against this tenet. geologic, oceanographic, and climatic changes during the Here, we performed new phylogenetic reconstructions in last 50 Ma. As a result, a main biogeographic principle in Nacella with special emphasis on the relationship between the Southern Ocean is the clear distinction of the Antarctic N. concinna and N. delesserti. Similarly, we performed biota. The Antarctic Polar Front (APF) represents an population-based analyses in N. concinna and N. delesserti important barrier between Antarctica and other sub-Ant- to further understand the genetic legacy of the Quaternary arctic provinces. However, the high degree of genetic glacial cycles. Phylogenetic reconstructions recognized N. affinity between populations of the Antarctic limpet concinna and N. delesserti as two closely but distinct monophyletic entities and therefore as valid evolutionary units. The cladogenetic process separating them occurred This article is an invited contribution on Life in Antarctica: *0.35 Ma and is consistent with the origin of Marion Boundaries and Gradients in a Changing Environment as the main Island (*0.45 Ma). -
Concepts & Synthesis
CONCEPTS & SYNTHESIS EMPHASIZING NEW IDEAS TO STIMULATE RESEARCH IN ECOLOGY Ecology, 89(3), 2008, pp. 682–692 Ó 2008 by the Ecological Society of America LIFE HUNG BY A THREAD: ENDURANCE OF ANTARCTIC FAUNA IN GLACIAL PERIODS 1,4 2 3 2 SVEN THATJE, CLAUS-DIETER HILLENBRAND, ANDREAS MACKENSEN, AND ROB LARTER 1National Oceanography Centre, Southampton, School of Ocean and Earth Science, University of Southampton, European Way, Southampton SO14 3ZH United Kingdom 2British Antarctic Survey, Geological Sciences Division, High Cross, Madingley Road, Cambridge CB3 0ET United Kingdom 3Alfred Wegener Institute for Polar and Marine Research, Am Alten Hafen 26, D-27568 Bremerhaven, Germany Abstract. Today, Antarctica exhibits some of the harshest environmental conditions for life on Earth. During the last glacial period, Antarctic terrestrial and marine life was challenged by even more extreme environmental conditions. During the present interglacial period, polar life in the Southern Ocean is sustained mainly by large-scale primary production. We argue that during the last glacial period, faunal populations in the Antarctic were limited to very few areas of local marine productivity (polynyas), because complete, multiannual sea-ice and ice shelf coverage shut down most of the Southern Ocean productivity within today’s seasonal sea-ice zone. Both marine sediments containing significant numbers of planktonic and benthic foraminifera and fossil bird stomach oil deposits in the adjacent Antarctic hinterland provide indirect evidence for the existence of polynyas during the last glacial period. We advocate that the existence of productive oases in the form of polynyas during glacial periods was essential for the survival of marine and most higher-trophic terrestrial fauna. -
New Zealand Sub-Antarctic Islands New Zealand
NEW ZEALAND SUB-ANTARCTIC ISLANDS NEW ZEALAND The New Zealand Sub-Antarctic Islands consist of five remote and windswept island groups in the Southern Ocean south and south-east of New Zealand. The islands, lying between the Antarctic and Subtropical Convergences, are oases of high productivity, biodiversity, dense populations and endemism for birds, ocean life, plants and invertebrates. Of the 126 species of birds, 40 are seabirds of which 5 breed nowhere else in the world. They have among the most southerly forests in the world, an unusual flora of megaherbs and some small islands never colonised by man. COUNTRY New Zealand NAME New Zealand Sub-Antarctic Islands NATURAL WORLD HERITAGE SERIAL SITE 1998: Inscribed on the World Heritage List under Natural Criteria ix and x. STATEMENT OF OUTSTANDING UNIVERSAL VALUE [pending] The UNESCO World Heritage Committee issued the following statement at the time of inscription: Justification for Inscription Criterion (ix): The New Zealand Sub-Antarctic Islands display a pattern of immigration of species, diversifications and emergent endemism, offering particularly good opportunities for research into the dynamics of island ecology. Criterion (x): The New Zealand Sub-Antarctic Islands are remarkable for their high level of biodiversity, population densities,and for endemism in birds, plants and invertebrates. The bird and plant life, especially the endemic albatrosses, cormorants, landbirds and “megaherbs” are unique to the islands. IUCN MANAGEMENT CATEGORY Auckland Islands National Nature Reserve