EXPERT/GOVERNMENT REVIEW IPCC Technical Paper Do Not Cite Or Quote 1 Climate Change and Biodiversity IPCC Technical Paper On
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Mitt. Münch. Ent. Ges. 106 Suppl. S2 1-10 München, 15.02.2016 Systematische, revidierte und kommentierte Checkliste der Schmetterlinge Bayerns (Insecta: Lepidoptera) Alfred HASLBERGER & Andreas H. SEGERER Supplementmaterial S2 Zusammenstellung der in vorliegender Arbeit publizierten regionalen Neu- und Wiederfunde. S2.1 Neufunde für die Bayerischen Alpen und/oder das Alpenvorland (AVA) Nr. FauEu Überfamilie Familie Art 0016 431725 Eriocranioidea Eriocraniidae Dyseriocrania subpurpurella (HAWORTH, 1828) 0026 431739 Eriocranioidea Eriocraniidae Eriocrania semipurpurella (STEPHENS, 1835) 0058 431808 Nepticuloidea Nepticulidae Stigmella aceris (FREY, 1857) 0080 431900 Nepticuloidea Nepticulidae Stigmella myrtillella (STAINTON, 1857) 0089 431932 Nepticuloidea Nepticulidae Stigmella splendidissimella (HERRICH-SCHÄFFER, 1855) 0125 432021 Nepticuloidea Nepticulidae Ectoedemia decentella (HERRICH-SCHÄFFER, 1855) 0133 432060 Nepticuloidea Nepticulidae Ectoedemia hannoverella (GLITZ, 1872) 0158 432282 Adeloidea Heliozelidae Heliozela resplendella (STAINTON, 1851) 0182 432335 Adeloidea Adelidae Adela cuprella (DENIS & SCHIFFERMÜLLER, 1775) 0202 432387 Adeloidea Incurvariidae Incurvaria pectinea HAWORTH, 1828 0230 432437 Tischerioidea Tischeriidae Coptotriche marginea (HAWORTH, 1828) 0331 433122 Tineoidea Tineidae Nemapogon granella (LINNAEUS, 1758) 0355 432916 Tineoidea Tineidae Monopis weaverella (SCOTT, 1858) 0371 433010 Tineoidea Tineidae Tinea columbariella WOCKE, 1877 0373 433015 Tineoidea Tineidae Tinea trinotella THUNBERG, 1794 0394 433489 -
Motyle (Lepidoptera) Parku Krajobrazowego Cysterskie Kompozycje Krajobrazowe Rud Wielkich
ROCZNIK MUZEUM GÓRNOŚLĄSKIEGO W BYTOMIU PRZYRODA Vol. 26 (online 001): 1–40 ISSN 0068-466X, eISSN 2451-0467 (online) Bytom, 10.04.2020 Jacek Maroń1, Adam Larysz2 Motyle (Lepidoptera) Parku Krajobrazowego Cysterskie Kompozycje Krajobrazowe Rud Wielkich http://doi.org/10.5281/zenodo.3747209 1 ul. Kuglera 9, 44-207 Rybnik, Polska, e-mail: [email protected] 2 Dział Przyrody, Muzeum Górnośląskie w Bytomu, pl. Jana III Sobieskiego 2, 41-902 Bytom, Polska, e-mail: [email protected] Abstract: The Butterflies and Moths (Lepidoptera) of the Cysterskie Kompozycje Krajobrazowe Rud Wielkich Landscape Park. The paper presents the research on Lepidoptera in Cysterskie Kompozycje Krajobrazowe Rud Wielkich Landscape Park between 1982 and 2019. The material was collected at nine selected sites, mainly in various forest environments. Overall, 1162 species in 66 families were recorded and listed, including 26 species new to the Province of Silesia. Key words: Lepidoptera, list of species, Cysterskie Kompozycje Krajobrazowe Rud Wielkich Landscape Park, biodiversity. WSTĘP Park Krajobrazowy Cysterskie Kompozycje Krajobrazowe Rud Wielkich (PK CKKRW) położony jest w południowo-zachodniej części województwa śląskiego i zajmuje wschodnią część Kotliny Raciborskiej oraz północne fragmenty Płaskowyżu Rybnickiego. Powstał na mocy Rozporządzenia Wojewody Katowickiego Nr 181/93 z dnia 23 listopada 1993 roku. Powierzchnia Parku wynosi 493,87 km², a strefa ochronna to obszar 140,10 km². Dominują tu drzewostany sosnowe, rosnące na siedliskach borowych, wykształconych na glebach bielicowych, a także wprowadzone sztucznie na siedliska żyznych lasów liściastych. Najbogatszym przyrodniczo terenem w obrębie Parku jest kompleks leśno-stawowy Łężczok w okolicach Raciborza, będący jedynym rezerwatem w granicach Parku. MATERIAŁ I METODY PROWADZENIA BADAŃ Stopień poznania entomofauny PK CKKRW jest niezadawalający, a dane dotyczące występowania poszczególnych gatunków są fragmentaryczne i rozproszone. -
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. -
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 -
Additions, Deletions and Corrections to An
Bulletin of the Irish Biogeographical Society No. 36 (2012) ADDITIONS, DELETIONS AND CORRECTIONS TO AN ANNOTATED CHECKLIST OF THE IRISH BUTTERFLIES AND MOTHS (LEPIDOPTERA) WITH A CONCISE CHECKLIST OF IRISH SPECIES AND ELACHISTA BIATOMELLA (STAINTON, 1848) NEW TO IRELAND K. G. M. Bond1 and J. P. O’Connor2 1Department of Zoology and Animal Ecology, School of BEES, University College Cork, Distillery Fields, North Mall, Cork, Ireland. e-mail: <[email protected]> 2Emeritus Entomologist, National Museum of Ireland, Kildare Street, Dublin 2, Ireland. Abstract Additions, deletions and corrections are made to the Irish checklist of butterflies and moths (Lepidoptera). Elachista biatomella (Stainton, 1848) is added to the Irish list. The total number of confirmed Irish species of Lepidoptera now stands at 1480. Key words: Lepidoptera, additions, deletions, corrections, Irish list, Elachista biatomella Introduction Bond, Nash and O’Connor (2006) provided a checklist of the Irish Lepidoptera. Since its publication, many new discoveries have been made and are reported here. In addition, several deletions have been made. A concise and updated checklist is provided. The following abbreviations are used in the text: BM(NH) – The Natural History Museum, London; NMINH – National Museum of Ireland, Natural History, Dublin. The total number of confirmed Irish species now stands at 1480, an addition of 68 since Bond et al. (2006). Taxonomic arrangement As a result of recent systematic research, it has been necessary to replace the arrangement familiar to British and Irish Lepidopterists by the Fauna Europaea [FE] system used by Karsholt 60 Bulletin of the Irish Biogeographical Society No. 36 (2012) and Razowski, which is widely used in continental Europe. -
Predicting Forest Insect Disturbance Under Climate Change
PREDICTING FOREST INSECT DISTURBANCE UNDER CLIMATE CHANGE Allan L. Carroll University of British Columbia Department of Forest Sciences 2424 Main Mall, Vancouver, BC Canada V6T 1Z4 Tel: 1-604-822-3360 Fax: 1-604-822-9102 Email: [email protected] 1 ABSTRACT This paper comprises a review of literature regarding climate change impacts to forest insect disturbances. Its primary objectives were three-fold. First, commonalities were sought among systems regarding the effects associated with altered temperature and/or precipitation patterns on forest insect herbivores, the proximate and ultimate form of the response by the insects, and the outcome in terms of forest disturbance. Second, a general framework within which to assess future disturbances to temperate and boreal forests by insect herbivores was constructed. Finally, uncertainty regarding predictions of the extent/severity of forest insect disturbances under climate change into the future was discussed. 2 INTRODUCTION There is now ample evidence that recent climatic changes have affected a broad range of organisms in a manner consistent with expectations from a warming environment (reviewed by Walther et al. 2002, Parmesan and Yohe 2003, Root et al. 2003, Hickling et al. 2006, Post et al. 2009, Robinet and Roques 2010, Wolken et al. 2011). In fact, evidence has accumulated indicating direct effects of anthropogenic climate change on every continent, in every ocean and in most major taxonomic groups (Parmesan 2006). Among the major taxonomic groups in which impacts of global warming have been most frequently documented are the insects. Terrestrial insects are sensitive indicators of changes to the condition of abiotic and biotic systems (McGeoch 1998). -
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). -
Vorarlbergs (Österreich) - Erkenntnisse Und Rückschlüsse : Supplement 2 1-29 Huemer, P
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Inatura Forschung online Jahr/Year: 2015 Band/Volume: 15_Supp2 Autor(en)/Author(s): Huemer Peter, Hebert Paul D. N. Artikel/Article: DNA-Barcoding der Schmetterlinge (Lepidoptera) Vorarlbergs (Österreich) - Erkenntnisse und Rückschlüsse : Supplement 2 1-29 Huemer, P. & Hebert, P.D.N. (2015): «DNA-Barcoding der Schmetterlinge (Lepidoptera) Vorarlbergs (Österreich) - Erkenntnisse und Rückschlüsse». inatura – Forschung online, Nr. 15, Suppl. 2: 29 S. DNA-Barcoding der Schmetterlinge (Lepidoptera) Nr. 15 - 2015 Vorarlbergs (Österreich) - Erkenntnisse und Suppl. 2 Rückschlüsse : Supplement 2 Peter Huemer1 & Paul D. N. Hebert2 1 Dr. Peter Huemer, Naturwissenschaftliche Sammlungen, Tiroler Landesmuseen Betriebsges.m.b.H., Feldstr. 11a, A-6020 Innsbruck. E-Mail: [email protected] 2 Prof. Dr. Paul D. N. Hebert, Biodiversity Institute of Ontario, University of Guelph, Guelph, ON, N1G 2W1, Canada. Anhangstabelle 2 Minimale genetische Distanzen zum jeweils Nächsten Nachbarn für 1497 Schmetterlingsarten aus Vorarlberg Familie Art Nächster Nachbar (NN) Distanz NN Adelidae Adela albicinctella Adela cuprella 2,51 Adelidae Adela cuprella Adela albicinctella 2,51 Adelidae Adela reaumurella Adela cuprella 7,15 Adelidae Cauchas rufimitrella Adela reaumurella 9,91 Adelidae Nematopogon metaxella Nematopogon schwarziellus 7,78 Adelidae Nematopogon pilella Nematopogon robertella 8,1 Adelidae Nematopogon -
Climate Change Effects on Eruptive Forest Insects: a R Eview and Synthesis of Empirical Evidence
CLIMATE CHANGE EFFECTS ON ERUPTIVE FOREST INSECTS: A REVIEW AND SYNTHESIS OF EMPIRICAL EVIDENCE FRST 498 AMBERLY MARCINIAK ABSTRACT Global climate change is affecting ecosystems through warming temperatures, changing precipitation, and increasing climatic variability. One of the major impacts is the alteration of forest disturbance regimes, including forest insect outbreaks that cause landscape-scale tree mortality and significantly affect the composition, function, and socioeconomic value of forests. Many studies have been conducted and models created to predict how future climate change may affect forest insects, but it may also be useful to determine how insects have already responded in order to detect where knowledge may be lacking and which species may be of most concern in future forest management. For this thesis, research papers providing empirical evidence to show a definitive climate change effect on an eruptive forest insect were identified and reviewed. The selected papers were then synthesized into a predictive framework for the likely responses of specific forest insect groups or species to changes in temperature or precipitation. Bark beetles and defoliators were the two functional groups for which evidence was found. All evidence pointed to bark beetle species responding positively to warming temperatures and decreasing precipitation through range expansion and increases in outbreak extent and severity. Evidence was less straightforward for defoliators, as some species, but not all, showed a negative response to warmer