Extinction: It's Not Just for Polar Bears
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
North America Other Continents
Arctic Ocean Europe North Asia America Atlantic Ocean Pacific Ocean Africa Pacific Ocean South Indian America Ocean Oceania Southern Ocean Antarctica LAND & WATER • The surface of the Earth is covered by approximately 71% water and 29% land. • It contains 7 continents and 5 oceans. Land Water EARTH’S HEMISPHERES • The planet Earth can be divided into four different sections or hemispheres. The Equator is an imaginary horizontal line (latitude) that divides the earth into the Northern and Southern hemispheres, while the Prime Meridian is the imaginary vertical line (longitude) that divides the earth into the Eastern and Western hemispheres. • North America, Earth’s 3rd largest continent, includes 23 countries. It contains Bermuda, Canada, Mexico, the United States of America, all Caribbean and Central America countries, as well as Greenland, which is the world’s largest island. North West East LOCATION South • The continent of North America is located in both the Northern and Western hemispheres. It is surrounded by the Arctic Ocean in the north, by the Atlantic Ocean in the east, and by the Pacific Ocean in the west. • It measures 24,256,000 sq. km and takes up a little more than 16% of the land on Earth. North America 16% Other Continents 84% • North America has an approximate population of almost 529 million people, which is about 8% of the World’s total population. 92% 8% North America Other Continents • The Atlantic Ocean is the second largest of Earth’s Oceans. It covers about 15% of the Earth’s total surface area and approximately 21% of its water surface area. -
Northern Sea Route Cargo Flows and Infrastructure- Present State And
Northern Sea Route Cargo Flows and Infrastructure – Present State and Future Potential By Claes Lykke Ragner FNI Report 13/2000 FRIDTJOF NANSENS INSTITUTT THE FRIDTJOF NANSEN INSTITUTE Tittel/Title Sider/Pages Northern Sea Route Cargo Flows and Infrastructure – Present 124 State and Future Potential Publikasjonstype/Publication Type Nummer/Number FNI Report 13/2000 Forfatter(e)/Author(s) ISBN Claes Lykke Ragner 82-7613-400-9 Program/Programme ISSN 0801-2431 Prosjekt/Project Sammendrag/Abstract The report assesses the Northern Sea Route’s commercial potential and economic importance, both as a transit route between Europe and Asia, and as an export route for oil, gas and other natural resources in the Russian Arctic. First, it conducts a survey of past and present Northern Sea Route (NSR) cargo flows. Then follow discussions of the route’s commercial potential as a transit route, as well as of its economic importance and relevance for each of the Russian Arctic regions. These discussions are summarized by estimates of what types and volumes of NSR cargoes that can realistically be expected in the period 2000-2015. This is then followed by a survey of the status quo of the NSR infrastructure (above all the ice-breakers, ice-class cargo vessels and ports), with estimates of its future capacity. Based on the estimated future NSR cargo potential, future NSR infrastructure requirements are calculated and compared with the estimated capacity in order to identify the main, future infrastructure bottlenecks for NSR operations. The information presented in the report is mainly compiled from data and research results that were published through the International Northern Sea Route Programme (INSROP) 1993-99, but considerable updates have been made using recent information, statistics and analyses from various sources. -
Beaufort Sea Monitoring Program
Outer Continental Shelf Environmental Assessment Program Beaufort Sea Monitoring Program: Proceedings of a Workshop and Sampling Design Recommendations Beaufort Sea Monitoring Program: Proceedings of a Workshop (September 1983) and Sampling Design Recommendations ; Prepared for the Outer Continental Shelf Environmental Assessment Program Juneau, Alaska by J. P. Houghton Dames & Moore 155 N.E. lOOth Street Seattle, WA 98125 with D. A Segar J. E. Zeh SEAM Ocean Inc. Department of Statistics Po. Box 1627 University of Washington Wheaton, MD 20902 Seattle, WA 98195 April 1984 UNITED STATES UNITED STATES DEPARTMENT OF COMMERCE DEPARTMENT OF THE INTERIOR Malcolm Baldridge, Secretary William P Clark, Secretary NATIONAL OCEANIC AND MINERALS MANAGEMENT SERVICE ATMOSPHERIC ADMINISTRATION William D. Bettenberg, Director John V. Byrne, Administrator r. NOTICES i? I This report has been reviewed by the US. Department of Commerce, National Oceanic and Atmospheric Administration's Outer Continental Shelf Environmental Assessment Program office, and approved for publication. The interpretation of data and opinions expressed in this document are those of the authors and workshop participants. Approval does not necessarily signify that the contents reflect the views and policies of the Department of Commerce or those of the Department of the Interior. The National Oceanic and Atmospheric Administration (NOAA) does not approve, recommend, or endorse any proprietary product or proprietary material mentioned in this publica tion. No reference shall be made to NOAA or to this publication in any advertising or sales promotion which would indicate or imply that NOAA approves, recommends, or endorses any proprietary'product or proprietary material mentioned herein, or which has as its purpose an intent to cause directly or indirectly the advertised product to be used or purchas'ed because of this publication. -
REDEFINING EUROPE-AFRICA RELATIONS Contents
The European Union’s relations with the African continent are facing distinct challenges, with the impact of the Covid-19 pandemic making it all the more evident that the prevail- ing asymmetry is no longer REDEFINING acceptable as we move into the future. EUROPE-AFRICA This analysis takes a closer RELATIONS look at economic relations between the European Union Robert Kappel and Africa, which for some time now have been on a January 2021 downward trajectory, and addresses the impact of the global pandemic at the same time. Additionally, the paper outlines the current political cooperation between the two continents and evaluates the EU’s recent strategy pro- posal. Lastly, the key aspects of more comprehensive stra- tegic cooperation between Europe and Africa are iden tified. REDEFINING EUROPE-AFRICA RELATIONS Contents Summary 2 1 EU-AFRICAN ECONOMIC RELATIONS 3 2 EFFECTS OF THE COVID-19 PANDEMIC ON AFRICAN ECONOMIES 14 3 COOPERATION WITH AFRICA: FROM LOMÉ TO A COMPREHENSIVE STRATEGY WITH AFRICA 18 4 FORGING A STRATEGIC PARTNERSHIP: RECOMMENDATIONS FOR ACTION 20 Résumé: Paving the Way for a New Africa-Europe Partnership 28 Literature 30 1 FRIEDRICH-EBERT-STIFTUNG – REDEFINING EUROPE-AFRICA RELATIONS Summary The European Union’s (EU) relations with the African conti- This paper begins by describing the EU’s current economic nent are facing a distinct set of challenges. Contrary to the relations with Africa (Chapter 1), which have been on a expectations of both African and European governments, downward trajectory for quite some time already. The ef- the pending negotiations between the partners are now fects of the Covid-19 pandemic are then outlined in Chap- being put to the test like never before. -
Respiratory Turbinates of Canids and Felids: a Quantitative Comparison
J. Zool., Lond. (2004) 264, 281–293 C 2004 The Zoological Society of London Printed in the United Kingdom DOI:10.1017/S0952836904005771 Respiratory turbinates of canids and felids: a quantitative comparison Blaire Van Valkenburgh1*, Jessica Theodor 2, Anthony Friscia1, Ari Pollack1 and Timothy Rowe3 1 Department of Ecology and Evolutionary Biology, University of California, Los Angeles, CA 90095-1606, U.S.A. 2 Department of Geology, Illinois State Museum, 1011 East Ash Street, Springfield, IL 62703, U.S.A. 3 Department of Geological Sciences, University of Texas, Austin, TX 78712, U.S.A. (Accepted 31 March 2004) Abstract The respiratory turbinates of mammals are complex bony plates within the nasal chamber that are covered with moist epithelium and provide an extensive surface area for the exchange of heat and water. Given their functional importance, maxilloturbinate size and structure are expected to vary predictably among species adapted to different environments. Here the first quantitative analysis is provided of maxilloturbinate structure based on high-resolution computed tomography (CT) scans of the skulls of eight canid and seven felid species. The key parameters examined were the density of the maxilloturbinate bones within the nasal chamber and how that density varied along the air pathway. In both canids and felids, total maxilloturbinate chamber volume and bone volume increased with body size, with canids having c. 1.5–2.0 times the volume of maxilloturbinate than felids of similar size. In all species, the volume of the maxilloturbinates varies from rostral to caudal, with the peak volume occurring approximately midway, close to where airway cross-sectional area is greatest. -
Asteroid Impact, Not Volcanism, Caused the End-Cretaceous Dinosaur Extinction
Asteroid impact, not volcanism, caused the end-Cretaceous dinosaur extinction Alfio Alessandro Chiarenzaa,b,1,2, Alexander Farnsworthc,1, Philip D. Mannionb, Daniel J. Luntc, Paul J. Valdesc, Joanna V. Morgana, and Peter A. Allisona aDepartment of Earth Science and Engineering, Imperial College London, South Kensington, SW7 2AZ London, United Kingdom; bDepartment of Earth Sciences, University College London, WC1E 6BT London, United Kingdom; and cSchool of Geographical Sciences, University of Bristol, BS8 1TH Bristol, United Kingdom Edited by Nils Chr. Stenseth, University of Oslo, Oslo, Norway, and approved May 21, 2020 (received for review April 1, 2020) The Cretaceous/Paleogene mass extinction, 66 Ma, included the (17). However, the timing and size of each eruptive event are demise of non-avian dinosaurs. Intense debate has focused on the highly contentious in relation to the mass extinction event (8–10). relative roles of Deccan volcanism and the Chicxulub asteroid im- An asteroid, ∼10 km in diameter, impacted at Chicxulub, in pact as kill mechanisms for this event. Here, we combine fossil- the present-day Gulf of Mexico, 66 Ma (4, 18, 19), leaving a crater occurrence data with paleoclimate and habitat suitability models ∼180 to 200 km in diameter (Fig. 1A). This impactor struck car- to evaluate dinosaur habitability in the wake of various asteroid bonate and sulfate-rich sediments, leading to the ejection and impact and Deccan volcanism scenarios. Asteroid impact models global dispersal of large quantities of dust, ash, sulfur, and other generate a prolonged cold winter that suppresses potential global aerosols into the atmosphere (4, 18–20). These atmospheric dinosaur habitats. -
Trapping Regulations You May Trap Wildlife for Subsistence Uses Only Within the Seasons and Harvest Limits in These Unit Trapping Regulations
Trapping Regulations You may trap wildlife for subsistence uses only within the seasons and harvest limits in these unit trapping regulations. Trapping wildlife out of season or in excess of harvest limits for subsistence uses is illegal and prohibited. However, you may trap unclassified wildlife (such as all squirrel and marmot species) in all units, without harvest limits, from July 1, 2014 through June 30, 2016. Subsistence Trapping Restrictions When taking wildlife for subsistence purposes, ● Take (or assist in the taking of) furbearers by firearm trappers may not: before 3:00 a.m. on the day following the day on which airborne travel occurred. This does not apply to a ● Disturb or destroy a den (except any muskrat pushup trapper using a firearm to dispatch furbearers caught in or feeding house that may be disturbed in the course of a trap or snare. trapping). ● Use a net or fish trap (except a blackfish or fyke trap). ● Disturb or destroy any beaver house. ● Use a firearm other than a shotgun, muzzle-loaded ● Take beaver by any means other than a steel trap or rifle, rifle or pistol using center-firing cartridges, for the snare, except certain times of the year when firearms taking of a wolf or wolverine, except that: may be used to take beaver in Units 9, 12, 17, 18, 20E, ■ You may use a firearm that shoots rimfire 21E, 22 and 23. See Unit-specific regulations. cartridges to take wolf and wolverine under a ● Under a trapping license, take a free-ranging furbearer trapping license. You may sell the raw fur or tanned with a firearm on NPS lands. -
Introduction to Astronomy from Darkness to Blazing Glory
Introduction to Astronomy From Darkness to Blazing Glory Published by JAS Educational Publications Copyright Pending 2010 JAS Educational Publications All rights reserved. Including the right of reproduction in whole or in part in any form. Second Edition Author: Jeffrey Wright Scott Photographs and Diagrams: Credit NASA, Jet Propulsion Laboratory, USGS, NOAA, Aames Research Center JAS Educational Publications 2601 Oakdale Road, H2 P.O. Box 197 Modesto California 95355 1-888-586-6252 Website: http://.Introastro.com Printing by Minuteman Press, Berkley, California ISBN 978-0-9827200-0-4 1 Introduction to Astronomy From Darkness to Blazing Glory The moon Titan is in the forefront with the moon Tethys behind it. These are two of many of Saturn’s moons Credit: Cassini Imaging Team, ISS, JPL, ESA, NASA 2 Introduction to Astronomy Contents in Brief Chapter 1: Astronomy Basics: Pages 1 – 6 Workbook Pages 1 - 2 Chapter 2: Time: Pages 7 - 10 Workbook Pages 3 - 4 Chapter 3: Solar System Overview: Pages 11 - 14 Workbook Pages 5 - 8 Chapter 4: Our Sun: Pages 15 - 20 Workbook Pages 9 - 16 Chapter 5: The Terrestrial Planets: Page 21 - 39 Workbook Pages 17 - 36 Mercury: Pages 22 - 23 Venus: Pages 24 - 25 Earth: Pages 25 - 34 Mars: Pages 34 - 39 Chapter 6: Outer, Dwarf and Exoplanets Pages: 41-54 Workbook Pages 37 - 48 Jupiter: Pages 41 - 42 Saturn: Pages 42 - 44 Uranus: Pages 44 - 45 Neptune: Pages 45 - 46 Dwarf Planets, Plutoids and Exoplanets: Pages 47 -54 3 Chapter 7: The Moons: Pages: 55 - 66 Workbook Pages 49 - 56 Chapter 8: Rocks and Ice: -
Taltheilei Houses, Lithics, and Mobility
University of Calgary PRISM: University of Calgary's Digital Repository Graduate Studies The Vault: Electronic Theses and Dissertations 2012-09-06 Taltheilei houses, lithics, and mobility Pickering, Sean Joseph Pickering, S. J. (2012). Taltheilei houses, lithics, and mobility (Unpublished master's thesis). University of Calgary, Calgary, AB. doi:10.11575/PRISM/27975 http://hdl.handle.net/11023/177 master thesis University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. Downloaded from PRISM: https://prism.ucalgary.ca UNIVERSITY OF CALGARY Taltheilei Houses, Lithics, and Mobility by Sean J. Pickering A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS DEPARTMENT OF ARCHAEOLOGY CALGARY, ALBERTA SEPTEMBER, 2012 © Sean J. Pickering 2012 Abstract The precontact subsistence-settlement strategy of Taltheilei tradition groups has been interpreted by past researchers as representing a high residential mobility forager system characterized by ephemeral warm season use of the Barrenlands environment, while hunting barrenground caribou. However, the excavation of four semi-subterranean house pits at the Ikirahak site (JjKs-7), in the Southern Kivalliq District of Nunavut, has challenged these assumptions. An analysis of the domestic architecture, as well as the morphological and spatial attributes of the excavated lithic artifacts, has shown that some Taltheilei groups inhabited the Barrenlands environment during the cold season for extended periods of time likely subsisting on stored resources. -
Recent Declines in Warming and Vegetation Greening Trends Over Pan-Arctic Tundra
Remote Sens. 2013, 5, 4229-4254; doi:10.3390/rs5094229 OPEN ACCESS Remote Sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Recent Declines in Warming and Vegetation Greening Trends over Pan-Arctic Tundra Uma S. Bhatt 1,*, Donald A. Walker 2, Martha K. Raynolds 2, Peter A. Bieniek 1,3, Howard E. Epstein 4, Josefino C. Comiso 5, Jorge E. Pinzon 6, Compton J. Tucker 6 and Igor V. Polyakov 3 1 Geophysical Institute, Department of Atmospheric Sciences, College of Natural Science and Mathematics, University of Alaska Fairbanks, 903 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 2 Institute of Arctic Biology, Department of Biology and Wildlife, College of Natural Science and Mathematics, University of Alaska, Fairbanks, P.O. Box 757000, Fairbanks, AK 99775, USA; E-Mails: [email protected] (D.A.W.); [email protected] (M.K.R.) 3 International Arctic Research Center, Department of Atmospheric Sciences, College of Natural Science and Mathematics, 930 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 4 Department of Environmental Sciences, University of Virginia, 291 McCormick Rd., Charlottesville, VA 22904, USA; E-Mail: [email protected] 5 Cryospheric Sciences Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mail: [email protected] 6 Biospheric Science Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mails: [email protected] (J.E.P.); [email protected] (C.J.T.) * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-907-474-2662; Fax: +1-907-474-2473. -
Opening up Europe's Public Data
The European Data Portal: Opening up Europe’s public data data.europa.eu/europeandataportal it available in the first place? What we do And in what domains, or A third of European across domains and across More and more volumes of countries are leading the countries? Also in what data are published every day, way with solid policies, language should the data be every hour, every minute, every licensing norms, good available? second. In every domain. portal traffic and many local Across every geography, small initiatives and events Value focuses on purpose, or big. The amount of data re-use and economic gains of across the world is increasing Open Data. Is there a societal exponentially. A substantial gain? Or perhaps a demo- amount of this data is cratic gain? How many new collected by governments. Public Sector Information jobs are created? What is the is information held by the critical mass? Value is there. The European Data Portal public sector. The EU Directive The question is how big? harvests the metadata on the re-use of Public (data about the data) of Sector Information provides Public Sector Information a common legal framework The Portal available on public data and for a European market for geospatial portals across government-held data. It is The first official version of European countries. Portals built around the key pillars of the European Data Portal is can be national, regional, the internal market: free flow available since February 2016. local or domain specific. of data, transparency and fair Within the Portal, sections are They cover the EU Member competition. -
New Siberian Islands Archipelago)
Detrital zircon ages and provenance of the Upper Paleozoic successions of Kotel’ny Island (New Siberian Islands archipelago) Victoria B. Ershova1,*, Andrei V. Prokopiev2, Andrei K. Khudoley1, Nikolay N. Sobolev3, and Eugeny O. Petrov3 1INSTITUTE OF EARTH SCIENCE, ST. PETERSBURG STATE UNIVERSITY, UNIVERSITETSKAYA NAB. 7/9, ST. PETERSBURG 199034, RUSSIA 2DIAMOND AND PRECIOUS METAL GEOLOGY INSTITUTE, SIBERIAN BRANCH, RUSSIAN ACADEMY OF SCIENCES, LENIN PROSPECT 39, YAKUTSK 677980, RUSSIA 3RUSSIAN GEOLOGICAL RESEARCH INSTITUTE (VSEGEI), SREDNIY PROSPECT 74, ST. PETERSBURG 199106, RUSSIA ABSTRACT Plate-tectonic models for the Paleozoic evolution of the Arctic are numerous and diverse. Our detrital zircon provenance study of Upper Paleozoic sandstones from Kotel’ny Island (New Siberian Island archipelago) provides new data on the provenance of clastic sediments and crustal affinity of the New Siberian Islands. Upper Devonian–Lower Carboniferous deposits yield detrital zircon populations that are consistent with the age of magmatic and metamorphic rocks within the Grenvillian-Sveconorwegian, Timanian, and Caledonian orogenic belts, but not with the Siberian craton. The Kolmogorov-Smirnov test reveals a strong similarity between detrital zircon populations within Devonian–Permian clastics of the New Siberian Islands, Wrangel Island (and possibly Chukotka), and the Severnaya Zemlya Archipelago. These results suggest that the New Siberian Islands, along with Wrangel Island and the Severnaya Zemlya Archipelago, were located along the northern margin of Laurentia-Baltica in the Late Devonian–Mississippian and possibly made up a single tectonic block. Detrital zircon populations from the Permian clastics record a dramatic shift to a Uralian provenance. The data and results presented here provide vital information to aid Paleozoic tectonic reconstructions of the Arctic region prior to opening of the Mesozoic oceanic basins.