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GSA TODAY • Southeastern Section Meeting, P
Vol. 5, No. 1 January 1995 INSIDE • 1995 GeoVentures, p. 4 • Environmental Education, p. 9 GSA TODAY • Southeastern Section Meeting, p. 15 A Publication of the Geological Society of America • North-Central–South-Central Section Meeting, p. 18 Stability or Instability of Antarctic Ice Sheets During Warm Climates of the Pliocene? James P. Kennett Marine Science Institute and Department of Geological Sciences, University of California Santa Barbara, CA 93106 David A. Hodell Department of Geology, University of Florida, Gainesville, FL 32611 ABSTRACT to the south from warmer, less nutrient- rich Subantarctic surface water. Up- During the Pliocene between welling of deep water in the circum- ~5 and 3 Ma, polar ice sheets were Antarctic links the mean chemical restricted to Antarctica, and climate composition of ocean deep water with was at times significantly warmer the atmosphere through gas exchange than now. Debate on whether the (Toggweiler and Sarmiento, 1985). Antarctic ice sheets and climate sys- The evolution of the Antarctic cryo- tem withstood this warmth with sphere-ocean system has profoundly relatively little change (stability influenced global climate, sea-level his- hypothesis) or whether much of the tory, Earth’s heat budget, atmospheric ice sheet disappeared (deglaciation composition and circulation, thermo- hypothesis) is ongoing. Paleoclimatic haline circulation, and the develop- data from high-latitude deep-sea sed- ment of Antarctic biota. iments strongly support the stability Given current concern about possi- hypothesis. Oxygen isotopic data ble global greenhouse warming, under- indicate that average sea-surface standing the history of the Antarctic temperatures in the Southern Ocean ocean-cryosphere system is important could not have increased by more for assessing future response of the Figure 1. -
ITEX Discoveries
Plant Response to Climate Change: Integration of ITEX Discoveries Proceedings from the 9th ITEX Meeting AEL REPORT 1 ARCTIC ECOLOGY LABORATORY DEPARTMENT OF BOTANY & PLANT PATHOLOGY MICHIGAN STATE UNIVERSITY EAST LANSING, MI 48824 Plant Response to Climate Change: Integration of ITEX Discoveries Proceedings from the 9th ITEX Meeting Compiled and edited by Robert D. Hollister Suggested Citation: Hollister, R.D. (editor). 1999. Plant Response to Climate Change: Integration of ITEX Discoveries. Proceedings from the 9th ITEX Meeting January 5-9, 1999. Arctic Ecology Laboratory Report 1, Michigan State University. East Lansing, MI. 117 p. This Report is available from: The Arctic Ecology Laboratory Department of Botany & Plant Pathology Michigan State University East Lansing, MI 48824 Telephone: 517 432-2399 i Foreword This compilation from the 1999 meeting of the International Tundra Experiment (ITEX) held at Michigan State University (MSU) demonstrates the considerable progress made since the 1990 founding meeting of ITEX which was also held at MSU. In the intervening nine years ITEX has become an established and well-known project. It has been used as a model for related endeavors. This document is intended to serve as an update on ITEX activities and an encouragement for continued integration and cooperation in the study of tundra plant response, and the linked feedback of this response, to climate change. The ITEX Steering Committee and I wish to thank Bob Hollister for his unflagging efforts as Conference Coordinator and compiler and editor of this report. The meeting was made possible with funding from the United States National Science Foundation Office of Polar Programs (grant number OPP 9714103). -
Department of Sustainability, Environment, Water, Population and Communities; Formerly from Department of Primary Industries, Parks, Water and Environment (Tasmania)
The Minister included this species in the critically endangered category, effective from 26/02/2013. Advice to the Minister for Sustainability, Environment, Water, Population & Communities from the Threatened Species Scientific Committee (the Committee) on amendment to the list of Threatened Species under the Environment Protection and Biodiversity Conservation Act 1999 (EPBC Act) 1. Reason for Conservation Assessment by the Committee This advice follows assessment of information gathered through the Commonwealth’s partnership agreement with Tasmania, which is aimed at systematically reviewing species that are inconsistently listed under the EPBC Act and relevant Tasmanian legislation. The Committee provides the following assessment of the appropriateness of this species’ inclusion in the EPBC Act list of threatened species: Corybas sulcatus (grooved helmet-orchid) 2. Summary of Species Details Taxonomy Conventionally accepted as Corybas sulcatus (M.A.Clem. & D.L.Jones) G.N.Backh. Formerly Nematoceras sulcatum M.A.Clem. & D.L.Jones. State/Territory Listing This species is listed as endangered (as Nematoceras Status sulcatum) under the Tasmanian Threatened Species Protection Act 1995. Description A small, deciduous, tuberous terrestrial orchid that forms small clonal colonies. Leaves are solitary, circular (12–20 mm diameter) and flat to shallowly concave. They are light green above and silvery green beneath, with a thick-textured blade and fleshy leaf stalk 12–16 mm long. Flowers are 25–30 mm long and 10–14 mm wide, mostly dark red and held erect on a fleshy, green stalk that is 5–7 mm long (Clements and Jones, 2007). Distribution The grooved helmet-orchid is endemic to Macquarie Island (Tasmania). -
Subantarctic and Polar Fronts of the Antarctic Circumpolar Current and Southern 1 Ocean Heat and Freshwater Content Variability: a View from Argo*
MARCH 2016 G I G L I O A N D J O H N S O N 749 Subantarctic and Polar Fronts of the Antarctic Circumpolar Current and Southern 1 Ocean Heat and Freshwater Content Variability: A View from Argo*, DONATA GIGLIO Joint Institute for the Study of the Atmosphere and Ocean, University of Washington, Seattle, Washington GREGORY C. JOHNSON NOAA/Pacific Marine Environmental Laboratory, Seattle, Washington (Manuscript received 17 July 2015, in final form 6 November 2015) ABSTRACT Argo profiling floats initiated a revolution in observational physical oceanography by providing nu- merous, high-quality, global, year-round, in situ (0–2000 dbar) temperature and salinity observations. This study uses Argo’s unprecedented sampling of the Southern Ocean during 2006–13 to describe the position of the Antarctic Circumpolar Current’s Subantarctic and Polar Fronts, comparing and contrasting two different methods for locating fronts using the same dataset. The first method locates three fronts along dynamic height contours, each corresponding to a local maximum in vertically integrated shear. The second approach locates the fronts using specific features in the potential temperature field, following Orsi et al. Results from the analysis of Argo data are compared to those from Orsi et al. and other more recent studies. Argo spatial resolution is not adequate to resolve annual and interannual movements of the fronts on a circumpolar scale since they are on the order of 18 latitude (Kim and Orsi), which is smaller than the resolution of the gridded product analyzed. Argo’s four-dimensional coverage of the Southern Ocean equatorward of ;608S is used to quantify variations in heat and freshwater content there with respect to the time-mean front locations. -
Impacts of Climate Change on Antarctic Ecosystems
IP 56 ! ! ! ! "#$%&'!()$*+ ",-.!/01! -23!45'6 ! 37$8$%)$&!9:+ ";<- ! <7=#=%'>+ 2%#>=8? ! ! Impacts of Climate Change on Antarctic Ecosystems ! ! ! ! ! / IP 56 ! ! Impacts of Climate Change on Antarctic Ecosystems Information paper submitted by ASOC to the XXXI ATCM, Kiev, 2-14 June 2008 ATCM item 13 and CEP item 9a Summary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
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 -
Climate and Deep Water Formation Regions
Cenozoic High Latitude Paleoceanography: New Perspectives from the Arctic and Subantarctic Pacific by Lindsey M. Waddell A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Oceanography: Marine Geology and Geochemistry) in The University of Michigan 2009 Doctoral Committee: Assistant Professor Ingrid L. Hendy, Chair Professor Mary Anne Carroll Professor Lynn M. Walter Associate Professor Christopher J. Poulsen Table of Contents List of Figures................................................................................................................... iii List of Tables ......................................................................................................................v List of Appendices............................................................................................................ vi Abstract............................................................................................................................ vii Chapter 1. Introduction....................................................................................................................1 2. Ventilation of the Abyssal Southern Ocean During the Late Neogene: A New Perspective from the Subantarctic Pacific ......................................................21 3. Global Overturning Circulation During the Late Neogene: New Insights from Hiatuses in the Subantarctic Pacific ...........................................55 4. Salinity of the Eocene Arctic Ocean from Oxygen Isotope -
The Intergovernmental Panel on Climate Change: a Synthesis of the Fourth Assessment Report Harvey Stern* Bureau of Meteorology, Melbourne, Vic., Australia
The Intergovernmental Panel on Climate Change: A Synthesis of the Fourth Assessment Report Harvey Stern* Bureau of Meteorology, Melbourne, Vic., Australia 1. Introduction The World Meteorological Organisation (WMO) and the United Nations Environment Programme (UNEP) established the Intergovernmental Panel on Climate Change (IPCC). The IPCC’s primary goal was to assess scientific, technical and socio-economic information relevant for the understanding of climate change, its potential impact and options for adaptation and mitigation. The purpose of the current paper is to provide a synthesis of the IPCC’s Fourth Assessment Report, which was released early in 2007. Much of the material presented is drawn directly from the summaries for policy makers prepared by the IPCC’s three Working Groups, namely: I. The Physical Science Basis (released February 2007); II. Impacts, Adaptation and Vulnerability (released April 2007); and, Fig A.1 The Rising Cost of Protection III. Mitigation (released May 2007). ___________________________________________ *Corresponding author address: Box 1636, Melbourne, Vic., 3001, Australia; email: [email protected] Dr Harvey Stern is a meteorologist with the Australian Bureau of Meteorology, holds a Ph. D. from the University of Melbourne (Earth Sciences), and currently heads the Climate Services Centre of the Bureau's Victorian Regional Office. Dr Stern's research into climate change includes evaluating costs associated with climate change and managing associated risks (Stern, 1992, 2005, 2006) – Fig A.1, and analysis of climate trends (Stern, 1980, 2000; Stern et al, 2004, 2005) – Fig A.2. His work has received praise in the Fig A.2 Trend in Melbourne’s annual extreme Victorian State Parliament (Hansard, Legislative minimum temperature (strong upward trend) Council, pp 1940-1941, 16 Nov., 2005). -
The Vegetation Communities Macquarie Island Vegetation
Edition 2 From Forest to Fjaeldmark The Vegetation Communities Macquarie Island vegetation Pleurophyllum hookeri Edition 2 From Forest to Fjaeldmark 1 Macquarie Island vegetation Community (Code) Page Coastal slope complex (QCS) 4 Coastal terrace mosaic (QCT) 6 Kelp beds (QKB) 8 Macquarie alpine mosaic (QAM) 10 Mire (QMI) 12 Short tussock grassland/rushland with herbs (QST) 14 Tall tussock grassland with megaherbs (QTT) 16 General description the surface and is part of its identified value as a World Heritage Area. The vegetation mapping of Macquarie Island was prepared by P.M. Selkirk and D.A. Adamson in 1998 All of the vegetation of Macquarie Island is and is based on vegetation structure rather than herbaceous, with no woody species present. community composition. Vegetation categories Megaherbs are a distinctive and unique feature of indicate foliage density and foliage height, similar to the sub-Antarctic, occurring nowhere else in the scheme of Specht (Specht et al. 1995). Using Tasmania. There are two megaherbs on Macquarie Specht’s classes, ‘closed vegetation’ equates to Island – Stilbocarpa polaris (Macquarie Island foliage projective cover >70%; and ‘open vegetation’ cabbage) and Pleurophyllum hookeri. In tall tussock equates to foliage projective cover <70%. ‘Tall grasslands dominated by Poa foliosa, there are often vegetation’ describes vegetation where the foliage swathes of Stilbocarpa polaris. stands higher than 0.4 to 0.5m above the ground, The vegetation communities that make up the while ‘short vegetation’ has foliage <0.4m high. Coastal terrace mosaic are much more widespread Seven structural vegetation types have been than currently mapped. Components of this mosaic identified in the mapping of Macquarie Island (mire, herbland, tall grassland, bryophytes, lakes, vegetation. -
Rapid Acidification of Mode and Intermediate Waters in the Southwestern Atlantic Ocean Lesley A
Rapid acidification of mode and intermediate waters in the southwestern Atlantic Ocean Lesley A. Salt, S. M. A. C. Heuven, M. E. Claus, E. M. Jones, H. J. W. Baar To cite this version: Lesley A. Salt, S. M. A. C. Heuven, M. E. Claus, E. M. Jones, H. J. W. Baar. Rapid acidification of mode and intermediate waters in the southwestern Atlantic Ocean. Biogeosciences, European Geosciences Union, 2015, 12 (5), pp.1387-1401. 10.5194/bg-12-1387-2015. hal-01251672 HAL Id: hal-01251672 https://hal.archives-ouvertes.fr/hal-01251672 Submitted on 6 Jan 2016 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. Distributed under a Creative Commons Attribution| 4.0 International License Biogeosciences, 12, 1387–1401, 2015 www.biogeosciences.net/12/1387/2015/ doi:10.5194/bg-12-1387-2015 © Author(s) 2015. CC Attribution 3.0 License. Rapid acidification of mode and intermediate waters in the southwestern Atlantic Ocean L. A. Salt1,*, S. M. A. C. van Heuven2,**, M. E. Claus3, E. M. Jones4, and H. J. W. de Baar1,3 1Royal Netherlands Institute for Sea Research, Landsdiep 4, -
Enhanced Marine Sulphur Emissions Offset Global Warming and Impact Rainfall Received: 22 January 2015 1 1,2 Accepted: 13 July 2015 B
www.nature.com/scientificreports OPEN Enhanced marine sulphur emissions offset global warming and impact rainfall Received: 22 January 2015 1 1,2 Accepted: 13 July 2015 B. S. Grandey & C. Wang Published: 21 August 2015 Artificial fertilisation of the ocean has been proposed as a possible geoengineering method for removing carbon dioxide from the atmosphere. The associated increase in marine primary productivity may lead to an increase in emissions of dimethyl sulphide (DMS), the primary source of sulphate aerosol over remote ocean regions, potentially causing direct and cloud-related indirect aerosol effects on climate. This pathway from ocean fertilisation to aerosol induced cooling of the climate may provide a basis for solar radiation management (SRM) geoengineering. In this study, we investigate the transient climate impacts of two emissions scenarios: an RCP4.5 (Representative Concentration Pathway 4.5) control; and an idealised scenario, based on RCP4.5, in which DMS emissions are substantially enhanced over ocean areas. We use mini-ensembles of a coupled atmosphere-ocean configuration of CESM1(CAM5) (Community Earth System Model version 1, with the Community Atmosphere Model version 5). We find that the cooling effect associated with enhanced DMS emissions beneficially offsets greenhouse gas induced warming across most of the world. However, the rainfall response may adversely affect water resources, potentially impacting human livelihoods. These results demonstrate that changes in marine phytoplankton activity may lead to a mixture of positive and negative impacts on the climate. DMS is a product of dimethylsulfoniopropionate produced by many species of phytoplankton1. Much of the DMS emitted to the atmosphere is oxidised to sulphur dioxide then to sulphuric acid to form sulphate aerosol. -
South, Tasmania
Biodiversity Summary for NRM Regions Guide to Users Background What is the summary for and where does it come from? This summary has been produced by the Department of Sustainability, Environment, Water, Population and Communities (SEWPC) for the Natural Resource Management Spatial Information System. It highlights important elements of the biodiversity of the region in two ways: • Listing species which may be significant for management because they are found only in the region, mainly in the region, or they have a conservation status such as endangered or vulnerable. • Comparing the region to other parts of Australia in terms of the composition and distribution of its species, to suggest components of its biodiversity which may be nationally significant. The summary was produced using the Australian Natural Natural Heritage Heritage Assessment Assessment Tool Tool (ANHAT), which analyses data from a range of plant and animal surveys and collections from across Australia to automatically generate a report for each NRM region. Data sources (Appendix 2) include national and state herbaria, museums, state governments, CSIRO, Birds Australia and a range of surveys conducted by or for DEWHA. Limitations • ANHAT currently contains information on the distribution of over 30,000 Australian taxa. This includes all mammals, birds, reptiles, frogs and fish, 137 families of vascular plants (over 15,000 species) and a range of invertebrate groups. The list of families covered in ANHAT is shown in Appendix 1. Groups notnot yet yet covered covered in inANHAT ANHAT are are not not included included in the in the summary. • The data used for this summary come from authoritative sources, but they are not perfect.