Bibliographic Introduction to Antarctic- Subantarctic Entomology
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Meteorology Climate
Meteorology: Climate • Climate is the third topic in the B-Division Science Olympiad Meteorology Event. • Topics rotate annually so a middle school participant may receive a comprehensive course of instruction in meteorology during this three-year cycle. • Sequence: 1. Climate (2006) 2. Everyday Weather (2007) 3. Severe Storms (2008) Weather versus Climate Weather occurs in the troposphere from day to day and week to week and even year to year. It is the state of the atmosphere at a particular location and moment in time. http://weathereye.kgan.com/cadet/cl imate/climate_vs.html http://apollo.lsc.vsc.edu/classes/me t130/notes/chapter1/wea_clim.html Weather versus Climate Climate is the sum of weather trends over long periods of time (centuries or even thousands of years). http://calspace.ucsd.edu/virtualmuseum/ climatechange1/07_1.shtml Weather versus Climate The nature of weather and climate are determined by many of the same elements. The most important of these are: 1. Temperature. Daily extremes in temperature and average annual temperatures determine weather over the short term; temperature tendencies determine climate over the long term. 2. Precipitation: including type (snow, rain, ground fog, etc.) and amount 3. Global circulation patterns: both oceanic and atmospheric 4. Continentiality: presence or absence of large land masses 5. Astronomical factors: including precession, axial tilt, eccen- tricity of Earth’s orbit, and variable solar output 6. Human impact: including green house gas emissions, ozone layer degradation, and deforestation http://www.ecn.ac.uk/Education/factors_affecting_climate.htm http://www.necci.sr.unh.edu/necci-report/NERAch3.pdf http://www.bbm.me.uk/portsdown/PH_731_Milank.htm Natural Climatic Variability Natural climatic variability refers to naturally occurring factors that affect global temperatures. -
Interactions of Patagonian Toothfish Fisheries With
CCAMLR Science, Vol. 17 (2010): 179–195 INTERACTIONS OF PATAGONIAN TOOTHFISH FISHERIES WITH KILLER AND SPERM WHALES IN THE CROZET ISLANDS EXCLUSIVE ECONOMIC ZONE: AN ASSESSMENT OF DEPREDATION LEVELS AND INSIGHTS ON POSSIBLE MITIGATION STRATEGIES P. Tixier1, N. Gasco2, G. Duhamel2, M. Viviant1, M. Authier1 and C. Guinet1 1 Centre d’Etudes Biologiques de Chizé CNRS, UPR 1934 Villiers-en-Bois, 79360 France Email – [email protected] 2 MNHN Paris, 75005 France Abstract Within the Crozet Islands Exclusive Economic Zone (EEZ), the Patagonian toothfish (Dissostichus eleginoides) longline fishery is exposed to high levels of depredation by killer (Orcinus orca) and sperm whales (Physeter macrocephalus). From 2003 to 2008, sperm whales alone, killer whales alone, and the two species co-occurring were observed on 32.6%, 18.6% and 23.4% respectively of the 4 289 hauled lines. It was estimated that a total of 571 tonnes (€4.8 million) of Patagonian toothfish were lost due to depredation by killer whales and both killer and sperm whales. Killer whales were found to be responsible for the largest part of this loss (>75%), while sperm whales had a lower impact (>25%). Photo-identification data revealed 35 killer whales belonging to four different pods were involved in 81.3% of the interactions. Significant variations of interaction rates with killer whales were detected between vessels suggesting the influence of operational factors on depredation. When killer whales were absent at the beginning of the line hauling process, short lines (<5 000 m) provided higher yield and were significantly less impacted by depredation than longer lines. -
Climate Change and Human Health: Risks and Responses
Climate change and human health RISKS AND RESPONSES Editors A.J. McMichael The Australian National University, Canberra, Australia D.H. Campbell-Lendrum London School of Hygiene and Tropical Medicine, London, United Kingdom C.F. Corvalán World Health Organization, Geneva, Switzerland K.L. Ebi World Health Organization Regional Office for Europe, European Centre for Environment and Health, Rome, Italy A.K. Githeko Kenya Medical Research Institute, Kisumu, Kenya J.D. Scheraga US Environmental Protection Agency, Washington, DC, USA A. Woodward University of Otago, Wellington, New Zealand WORLD HEALTH ORGANIZATION GENEVA 2003 WHO Library Cataloguing-in-Publication Data Climate change and human health : risks and responses / editors : A. J. McMichael . [et al.] 1.Climate 2.Greenhouse effect 3.Natural disasters 4.Disease transmission 5.Ultraviolet rays—adverse effects 6.Risk assessment I.McMichael, Anthony J. ISBN 92 4 156248 X (NLM classification: WA 30) ©World Health Organization 2003 All rights reserved. Publications of the World Health Organization can be obtained from Marketing and Dis- semination, World Health Organization, 20 Avenue Appia, 1211 Geneva 27, Switzerland (tel: +41 22 791 2476; fax: +41 22 791 4857; email: [email protected]). Requests for permission to reproduce or translate WHO publications—whether for sale or for noncommercial distribution—should be addressed to Publications, at the above address (fax: +41 22 791 4806; email: [email protected]). The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the World Health Organization concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. -
(Acari: Mesostigmata) Raphael De Campos Castilho
Universidade de São Paulo Escola Superior de Agricultura “Luiz de Queiroz” Taxonomy of Rhodacaroidea mites (Acari: Mesostigmata) Raphael de Campos Castilho Thesis submitted in partial fulfillment of the requirements for the degree of Doctor in Science. Area of concentration: Entomology Piracicaba 2012 2 Raphael de Campos Castilho Engenheiro Agrônomo Taxonomy of Rhodacaroidea mites (Acari: Mesostigmata) Adviser: Prof. Dr. GILBERTO JOSÉ DE MORAES Thesis submitted in partial fulfillment of the requirements for the degree of Doctor in Science. Area of concentration: Entomology Piracicaba 2012 Dados Internacionais de Catalogação na Publicação DIVISÃO DE BIBLIOTECA - ESALQ/USP Castilho, Raphael de Campos Taxonomy of Rhodacaroidea mites (Acari: Mesostigmata) / Raphael de Campos Castilho. - - Piracicaba, 2012. 579 p. : il. Tese (Doutorado) - - Escola Superior de Agricultura “Luiz de Queiroz”, 2012. 1. Ácaros predadores 2. Classificação 3. Ácaros de solo 4. Controle biológico I. Título CDD 595.42 C352t “Permitida a cópia total ou parcial deste documento, desde que citada a fonte – O autor” 3 To GOD Source of perseverance and life, To my mother Sonia Regina de Campos For her love, tenderness and comprehension. To my partner Karina Cezarete Semençato for her love, patience and unfailing support to me Offer To Prof. Dr. Gilberto José de Moraes For his valuable guidance, friendship and recognition of my work Special thanks 4 5 Ackanowledgements To Escola Superior de Agricultura ―Luiz de Queiroz‖ (ESALQ), Universidade de São Paulo (USP), and especially to ―Departamento de Entomologia e Acarologia‖ for providing all intellectual and material support necessary for the proper development of this work; I am especially grateful to Carlos H. W. -
Office of Polar Programs
DEVELOPMENT AND IMPLEMENTATION OF SURFACE TRAVERSE CAPABILITIES IN ANTARCTICA COMPREHENSIVE ENVIRONMENTAL EVALUATION DRAFT (15 January 2004) FINAL (30 August 2004) National Science Foundation 4201 Wilson Boulevard Arlington, Virginia 22230 DEVELOPMENT AND IMPLEMENTATION OF SURFACE TRAVERSE CAPABILITIES IN ANTARCTICA FINAL COMPREHENSIVE ENVIRONMENTAL EVALUATION TABLE OF CONTENTS 1.0 INTRODUCTION....................................................................................................................1-1 1.1 Purpose.......................................................................................................................................1-1 1.2 Comprehensive Environmental Evaluation (CEE) Process .......................................................1-1 1.3 Document Organization .............................................................................................................1-2 2.0 BACKGROUND OF SURFACE TRAVERSES IN ANTARCTICA..................................2-1 2.1 Introduction ................................................................................................................................2-1 2.2 Re-supply Traverses...................................................................................................................2-1 2.3 Scientific Traverses and Surface-Based Surveys .......................................................................2-5 3.0 ALTERNATIVES ....................................................................................................................3-1 -
Potential Regime Shift in Decreased Sea Ice Production After the Mertz Glacier Calving
ARTICLE Received 27 Jan 2012 | Accepted 3 Apr 2012 | Published 8 May 2012 DOI: 10.1038/ncomms1820 Potential regime shift in decreased sea ice production after the Mertz Glacier calving T. Tamura1,2,*, G.D. Williams2,*, A.D. Fraser2 & K.I. Ohshima3 Variability in dense shelf water formation can potentially impact Antarctic Bottom Water (AABW) production, a vital component of the global climate system. In East Antarctica, the George V Land polynya system (142–150°E) is structured by the local ‘icescape’, promoting sea ice formation that is driven by the offshore wind regime. Here we present the first observations of this region after the repositioning of a large iceberg (B9B) precipitated the calving of the Mertz Glacier Tongue in 2010. Using satellite data, we find that the total sea ice production for the region in 2010 and 2011 was 144 and 134 km3, respectively, representing a 14–20% decrease from a value of 168 km3 averaged from 2000–2009. This abrupt change to the regional icescape could result in decreased polynya activity, sea ice production, and ultimately the dense shelf water export and AABW production from this region for the coming decades. 1 National Institute of Polar Research, Tachikawa, Japan. 2 Antarctic Climate & Ecosystem Cooperative Research Centre, University of Tasmania, Hobart, Australia. 3 Institute of Low Temperature of Science, Sapporo, Japan. *These authors contributed equally to this work. Correspondence and requests for materials should be addressed to T.T. (email: [email protected]) or to G.D.W. (email: [email protected]). NATURE COMMUNICATIONS | 3:826 | DOI: 10.1038/ncomms1820 | www.nature.com/naturecommunications © 2012 Macmillan Publishers Limited. -
Download the Presentation Here
Photo 1 4.2” x 10.31” Position x: 8.74”, y: .18” Jean-Philippe Palasi Director for European policy Averting global biodiversity loss Photo 1 4.2” x 10.31” Position x: 8.74”, y: .18” Can we avert global biodiversity loss ? That means addressing 5 direct causes: • Habitat destruction • Over exploitation • Pollution • Invasive species • Climate change Photo 1 4.2” x 10.31” Position x: 8.74”, y: .18” Can we avert global biodiversity loss ? That means addressing 5 direct causes: • Habitat destruction • Over exploitation • Pollution • Invasive species • Climate change Photo 1 4.2” x 10.31” Position x: 8.74”, y: .18” Can we avert global biodiversity loss ? That means addressing 5 direct causes: • Habitat destruction • Over exploitation • Pollution • Invasive species • Climate change And several root causes: • Demographic growth • Poverty • Poor governance, corruption and conflicts • Unsustainable economic models (production, Photo 1 consumption and supply chains) 4.2” x 10.31” • Lack of awareness & adequate accounting Position x: 8.74”, y: .18” Habitat destruction Climate change species confined to high altitude At 520 ppm (mid-century?) most of coral species in warm waters would scarcely support further growth. Increased droughts in the Amazon basin 2010 vegetation anomalies, Nasa Earth Observatory CC impact on species Chris Thomas (Leeds univ), Nature, 2004 « We predict, on the basis of mid-range climate-warming scenarios for 2050, that 15-37% of species (…) will be committed to exctinction » = 1 million terrestrial species by 2050 Mitigation is key: - Lower climate projections: ~18% - Mid-range: ~24% Photo 1 4.2” x 10.31” - Maximum: ~35% Position x: 8.74”, y: .18” Biodiversity loss …is a defining issues of our time …is closely linked to climate change …will carry on for decades, probably centuries …can be mitigated through profound changes in our economic and social systems Photo 1 4.2” x 10.31” Position x: 8.74”, y: .18” EU action for global biodiversity Photo 1 4.2” x 10.31” Position x: 8.74”, y: .18” EU action for global biodiversity 1. -
Amazing Antarctica – Lesson 6
Year 8 GEOGRAPHY – Ecosystems – Amazing Antarctica – Lesson 6 Title: Ecosystems – Amazing Antarctica TASK 1: write down the following WOW words. As you go through the information, write the definition for each word (you might find some of the definitions as you work through the booklet). • Precipitation = • Albedo = • Ice sheet = • Glaciers = • Food chain = TASK 2: where is Antarctica? Use the following sentence starters and complete them to explain where Antarctica is located around the world. • Antarctica is located at the _________________ pole. • Antarctica is a country/continent/city. • Nearby countries include ______________________. • The oceans that surround Antarctica are __________________________. TASK 3: watch the video and write down facts about Antarctica https://www.youtube.com/watch?v=X3uT89xoKuc Antarctica TASK 4: what is the climate like in Antarctica? Read through the information below and answer the questions in red. Climate of Antarctica Antarctica can be called a desert because of its low levels of precipitation, which is mainly snow. In coastal regions, about 200 mm can fall annually. In mountainous regions and on the East Antarctica plateau, the amount is less than 50 mm annually. Evaporation is not as high as other desert regions because it is so cold, so the snow gradually builds up year after year. There are also strong winds, with recordings of up to 200 mph being made. Antarctica's seasons are opposite to the seasons that we're familiar with in the UK. Antarctic summers happen at the same time as UK winters. This is because Antarctica is in the Southern Hemisphere, which faces the Sun during our winter time. -
Educator's Guide
SOUTH POLE Amundsen’s Route Scott’s Route Roald Amundsen EDUCATOR’S GUIDE amnh.org/education/race Robert Falcon Scott INSIDE: • Suggestions to Help You Come Prepared • Essential Questions for Student Inquiry • Strategies for Teaching in the Exhibition • Map of the Exhibition • Online Resources for the Classroom • Correlation to Standards • Glossary ESSENTIAL QUESTIONS Who would be fi rst to set foot at the South Pole, Norwegian explorer Roald Amundsen or British Naval offi cer Robert Falcon Scott? Tracing their heroic journeys, this exhibition portrays the harsh environment and scientifi c importance of the last continent to be explored. Use the Essential Questions below to connect the exhibition’s themes to your curriculum. What do explorers need to survive during What is Antarctica? Antarctica is Earth’s southernmost continent. About the size of the polar expeditions? United States and Mexico combined, it’s almost entirely covered Exploring Antarc- by a thick ice sheet that gives it the highest average elevation of tica involved great any continent. This ice sheet contains 90% of the world’s land ice, danger and un- which represents 70% of its fresh water. Antarctica is the coldest imaginable physical place on Earth, and an encircling polar ocean current keeps it hardship. Hazards that way. Winds blowing out of the continent’s core can reach included snow over 320 kilometers per hour (200 mph), making it the windiest. blindness, malnu- Since most of Antarctica receives no precipitation at all, it’s also trition, frostbite, the driest place on Earth. Its landforms include high plateaus and crevasses, and active volcanoes. -
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. -
Henderson Island Expedition June 2019 Henderson Island Expedition June 2019
Henderson Island Expedition June 2019 Henderson Island Expedition June 2019 Overview Overarching objectives of the expedition: A) Study the plastic pollution on Henderson Island and raise awareness of the waste in the context of the global problem of ocean plastics; B) Study and raise awareness of the Henderson marine environment – promoting the Pitcairn Island Marine Reserve and the benefits of large, fully protected marine protected areas. A 2015 analysis (published in 2017) found that one of the Pitcairn archipelago’s four islands, Henderson, has >18 tonnes of plastic on its beaches: “the highest density of plastic debris recorded anywhere in the world”. The 38km2 island has >38 million pieces of plastic upon its shores. Conservative estimates suggest that 3,500-13,500 new plastic items wash up on Henderson each day. One of its beaches, the 2 km long East Beach, is polluted by 30 million plastic items. The 2015 work served as a reminder that the long-term protection of large areas of ocean needs to be partnered by science and messaging capable of changing attitudes towards the way we live, consume, and discard on land. The Pitcairn Island Council has sanctioned an expedition to Henderson in June 2019 which provides an opportunity for key Pitcairn and ocean stakeholders to effectively communicate the source, scale, range and impacts of ocean debris on Henderson and the Pacific Ocean through on-site science, art and media. The initiative also provides the team an opportunity to study and showcase the beauty and ambition of the Pitcairn Island Marine Reserve Henderson Island Expedition June 2019 MEXICO Timings PACIFIC OCEAN 1 02/06 Arrive at Tahiti Team briefing Tahiti 2 04/06 PERU Depart Tahiti 07:30 a.m. -
Diptera: Sphaeroceridae: Limosininae), an Almost Entirely
A review of the Archiceroptera Papp genus complex (Diptera: Sphaeroceridae: Limosininae) by Steven Mark Paiero A Thesis presented to The University of Guelph In partial fulfilment of requirements for the degree of Doctor of Philosophy in Environmental Sciences Guelph, Ontario, Canada © Steven Mark Paiero, December, 2017 ABSTRACT: A review of the Archiceroptera Papp genus complex (Diptera: Sphaeroceridae: Limosininae) Steven Mark Paiero Advisor: University of Guelph, 2017 Dr. S.A. Marshall This thesis has two parts. The first part investigates the relationships between the Archiceroptera genus complex and other members of the Limosininae (Diptera: Sphaeroceridae). A focus is placed on the relationships within the larger epandrial process group, which contains Bitheca, Bromeloecia, Pterogramma, Aptilotella, and Robustagramma, along with Archiceroptera, Rudolfina and several previously unplaced species groups. Molecular and morphological data sets provide the first phylogeny of the group, and were used to support the inclusion of several unplaced species groups within Rudolfina and Archiceroptera, while one new genus is described. Pectinosina gen. nov. includes two species: P. prominens (Duda), previously placed in Rudolfina, and P. carro n. sp. The second part of the thesis deals with revisions of Archiceroptera Papp and Rudolfina Roháček. Rudolfina now includes 13 described species, nine of which are newly described here (R. bucki, R. exuberata, R. howdeni, R. megepandria, R. pauca, R. pilosa, R. newtoni, R. remiforma, and R. tumida). Archiceroptera now includes 29 species, of which 27 are newly described here (A. adamas, A. addenda, A. barberi, A. basilia, A. bilobata, A. bisetosus, A. braziliensis, A. brevivilla, A. browni, A. caliga, A. calligraphia, A. cobolorum, A.