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A Vegetation Map of South America
A VEGETATION MAP OF SOUTH AMERICA MAPA DE LA VEGETACIÓN DE AMÉRICA DEL SUR MAPA DA VEGETAÇÃO DA AMÉRICA DO SUL H.D.Eva E.E. de Miranda C.M. Di Bella V.Gond O.Huber M.Sgrenzaroli S.Jones A.Coutinho A.Dorado M.Guimarães C.Elvidge F.Achard A.S.Belward E.Bartholomé A.Baraldi G.De Grandi P.Vogt S.Fritz A.Hartley 2002 EUR 20159 EN A VEGETATION MAP OF SOUTH AMERICA MAPA DE LA VEGETACIÓN DE AMÉRICA DEL SUR MAPA DA VEGETAÇÃO DA AMÉRICA DO SUL H.D.Eva E.E. de Miranda C.M. Di Bella V.Gond O.Huber M.Sgrenzaroli S.Jones A.Coutinho A.Dorado M.Guimarães C.Elvidge F.Achard A.S.Belward E.Bartholomé A.Baraldi G.De Grandi P.Vogt S.Fritz A.Hartley 2002 EUR 20159 EN A Vegetation Map of South America I LEGAL NOTICE Neither the European Commission nor any person acting on behalf of the Commission is responsible for the use which might be made of the following information. A great deal of additional information on the European Union is available on the Internet. It can be accessed through the Europa server (http://europa.eu.int) Cataloguing data can be found at the end of this publication Luxembourg: Office for Official Publications of the European Communities, 2002 ISBN 92-894-4449-5 © European Communities, 2002 Reproduction is authorized provided the source is acknowledged Printed in Italy II A Vegetation Map of South America A VEGETATION MAP OF SOUTH AMERICA prepared by H.D.Eva* E.E. -
The Physical Oceanography of the Gulf of Thailand, Naga Expedition; Bathythermograph (BT) Temperature Observations in the Timor Sea, Naga Expedition, Cruise S11
UC San Diego Naga Report Title The physical oceanography of the Gulf of Thailand, Naga Expedition; Bathythermograph (BT) temperature observations in the Timor sea, Naga Expedition, Cruise S11 Permalink https://escholarship.org/uc/item/4mf3d0b7 Author Robinson, Margaret K Publication Date 1974 eScholarship.org Powered by the California Digital Library University of California NAGA REPORT Volume 3, Part 1 Scientific Results of Marine Investigations of the South China Sea and the Gulf of Thailand 1959-1961 Sponsored by South Viet Nam, Thailand and the United States of America The University of California Scripps Institution of Oceanography La Jolla, California 1974 EDITORS: EDWARD BRINTON, WILLIAM A. NEWMAN ASSISTANT EDITOR: NANCE F. NORTH Printing of this volume was made possible through the National Science Foundation Grant GN-32570. The NAGA Expedition was supported by the International Cooperation Administration Contract ICAc-1085. Library of Congress Catalog Card Number: 74-620121 2 CONTENTS 3 THE PHYSICAL OCEANOGRAPHY OF THE GULF OF THAILAND, NAGA EXPEDITION by Margaret K. Robinson* *Scripps Institution of Oceanography, University of California, La Jolla, California 5 Chart of the Gulf of Thailand showing Cruise Track Lines 6 THE PHYSICAL OCEANOGRAPHY OF THE GULF OF THAILAND, NAGA EXPEDITION CONTENTS 7 LIST OF TABLES AND FIGURES 8 9 INTRODUCTION AND ACKNOWLEDGMENTS The Research Vessel Stranger of the Scripps Institution of Oceanography, University of California, San Diego, was engaged in the Naga Expedition in the Gulf of Thailand and the South China Sea during the period of October, 1959, to December, 1960. The expedition was jointly sponsored by the Governments of South Viet Nam, Thailand and the United States of America. -
South China Sea Overview
‹ Countries South China Sea Last Updated: February 7, 2013 (Notes) full report Overview The South China Sea is a critical world trade route and a potential source of hydrocarbons, particularly natural gas, with competing claims of ownership over the sea and its resources. Stretching from Singapore and the Strait of Malacca in the southwest to the Strait of Taiwan in the northeast, the South China Sea is one of the most important trade routes in the world. The sea is rich in resources and holds significant strategic and political importance. The area includes several hundred small islands, rocks, and reefs, with the majority located in the Paracel and Spratly Island chains. Many of these islands are partially submerged land masses unsuitable for habitation and are little more than shipping hazards. For example, the total land area of the Spratly Islands encompasses less than 3 square miles. Several of the countries bordering the sea declare ownership of the islands to claim the surrounding sea and its resources. The Gulf of Thailand borders the South China Sea, and although technically not part of it, disputes surround ownership of that Gulf and its resources as well. Asia's robust economic growth boosts demand for energy in the region. The U.S. Energy Information Administration (EIA) projects total liquid fuels consumption in Asian countries outside the Organization for Economic Cooperation and Development (OECD) to rise at an annual growth rate of 2.6 percent, growing from around 20 percent of world consumption in 2008 to over 30 percent of world consumption by 2035. Similarly, non-OECD Asia natural gas consumption grows by 3.9 percent annually, from 10 percent of world gas consumption in 2008 to 19 percent by 2035. -
Active Faulting Geometry and Stress
Tectonics RESEARCH ARTICLE Active Faulting Geometry and Stress Pattern Near Complex 10.1029/2018TC004983 Strike-Slip Systems Along the Maghreb Region: Special Section: Constraints on Active Convergence Geodynamics, Crustal and Lithospheric Tectonics, and in the Western Mediterranean active deformation in the Mediterranean Regions Abdelkader Soumaya1,2 , Noureddine Ben Ayed3, Mojtaba Rajabi4 , Mustapha Meghraoui5, (A tribute to Prof. Renato Damien Delvaux6, Ali Kadri3, Moritz Ziegler7,8 , Said Maouche9, and Ahmed Braham2 Funiciello) 1Faculty of Sciences Tunis, University of Manar, Tunis, Tunisia, 2National Office of Mines, Tunisia, 3Faculty of Sciences Bizerte, 4 Key Points: University of Carthage, Tunis, Tunisia, Australian School of Petroleum, University of Adelaide, Adelaide, South Australia, • Maghreb region is characterized by Australia, 5Institut de Physique du Globe de Strasbourg (UMR 7516), Strasbourg, France, 6Earth Sciences Department, Royal different geometries of active Museum for Central Africa, Tervuren, Belgium, 7Helmholtz Centre Potsdam, German Research Centre for Geosciences GFZ, strike-slip faults Potsdam, Germany, 8Institute of Earth and Environmental Science, University of Potsdam, Potsdam, Germany, 9CRAAG, • Present-day active contraction on western Africa-Eurasia boundary is Bouzareah-Alger, Algeria accommodated by a combination of strike-slip and thrust faulting • Second-order tectonic regime across Abstract The Maghreb region (from Tunisia to Gibraltar) is a key area in the western Mediterranean to Maghreb varies with clockwise study the active tectonics and stress pattern across the Africa-Eurasia convergent plate boundary. In the rotation of S from east to west Hmax present study, we compile comprehensive data set of well-constrained crustal stress indicators (from single focal mechanism solutions, formal inversion of focal mechanism solutions, and young geologic fault slip data) based on our and published data analyses. -
Rent Drain Estimation of the Thai Fisheries in the Gulf of Thailand
IIFET 2008 Vietnam Proceedings RENT DRAIN ESTIMATION OF THE THAI FISHERIES IN THE GULF OF THAILAND Pongpat Boonchuwong, Department of Fisheries, [email protected] Waraporn Dechboon, Department of Fisheries, [email protected] ABSTRACT The fishery resources in the Gulf of Thailand have been subjected to excessive levels of fishing effort since perhaps as long as two to three decades. This has caused a change in catch composition with a higher share of short-lived species. The influence of this change on the value of the catch has not been unambiguously negative because some short-lived species fetch a good price. This notwithstanding, the paper shows significant rent losses associated with overfishing and greatly excessive fleet sizes in the Gulf of Thailand for all three of the studied fisheries, namely for demersal resources, Indo-Pacific mackeral and anchovy. Keywords: Rent Drain, Demersal Resources, Indo-Pacific Mackerel, Anchovy, Gulf of Thailand OVERVIEW OF THAI FISHERIES Thailand is one of the top fish producing nations in the world. During 2000-2004, annual fish production was 3.7-4.1 million tonnes. Geographical advantage is one factor attributed to the relative high annual fish production. Thailand has a total land area of about 540,000 km.2 and a coastline of 2,614 km. Marine fishing grounds that fall within Thailand’s Exclusive Economic Zones lie in part of the Gulf of Thailand and part of the Andaman Sea cover the total area of about 316,000 km.2 The area of inland waters is approximately 3,750 km.2 . Besides, over one million hectares of her coastal areas have a potential for coastal aquaculture. -
Global Seagrass Distribution and Diversity: a Bioregional Model ⁎ F
Journal of Experimental Marine Biology and Ecology 350 (2007) 3–20 www.elsevier.com/locate/jembe Global seagrass distribution and diversity: A bioregional model ⁎ F. Short a, , T. Carruthers b, W. Dennison b, M. Waycott c a Department of Natural Resources, University of New Hampshire, Jackson Estuarine Laboratory, Durham, NH 03824, USA b Integration and Application Network, University of Maryland Center for Environmental Science, Cambridge, MD 21613, USA c School of Marine and Tropical Biology, James Cook University, Townsville, 4811 Queensland, Australia Received 1 February 2007; received in revised form 31 May 2007; accepted 4 June 2007 Abstract Seagrasses, marine flowering plants, are widely distributed along temperate and tropical coastlines of the world. Seagrasses have key ecological roles in coastal ecosystems and can form extensive meadows supporting high biodiversity. The global species diversity of seagrasses is low (b60 species), but species can have ranges that extend for thousands of kilometers of coastline. Seagrass bioregions are defined here, based on species assemblages, species distributional ranges, and tropical and temperate influences. Six global bioregions are presented: four temperate and two tropical. The temperate bioregions include the Temperate North Atlantic, the Temperate North Pacific, the Mediterranean, and the Temperate Southern Oceans. The Temperate North Atlantic has low seagrass diversity, the major species being Zostera marina, typically occurring in estuaries and lagoons. The Temperate North Pacific has high seagrass diversity with Zostera spp. in estuaries and lagoons as well as Phyllospadix spp. in the surf zone. The Mediterranean region has clear water with vast meadows of moderate diversity of both temperate and tropical seagrasses, dominated by deep-growing Posidonia oceanica. -
Data Structure
Data structure – Water The aim of this document is to provide a short and clear description of parameters (data items) that are to be reported in the data collection forms of the Global Monitoring Plan (GMP) data collection campaigns 2013–2014. The data itself should be reported by means of MS Excel sheets as suggested in the document UNEP/POPS/COP.6/INF/31, chapter 2.3, p. 22. Aggregated data can also be reported via on-line forms available in the GMP data warehouse (GMP DWH). Structure of the database and associated code lists are based on following documents, recommendations and expert opinions as adopted by the Stockholm Convention COP6 in 2013: · Guidance on the Global Monitoring Plan for Persistent Organic Pollutants UNEP/POPS/COP.6/INF/31 (version January 2013) · Conclusions of the Meeting of the Global Coordination Group and Regional Organization Groups for the Global Monitoring Plan for POPs, held in Geneva, 10–12 October 2012 · Conclusions of the Meeting of the expert group on data handling under the global monitoring plan for persistent organic pollutants, held in Brno, Czech Republic, 13-15 June 2012 The individual reported data component is inserted as: · free text or number (e.g. Site name, Monitoring programme, Value) · a defined item selected from a particular code list (e.g., Country, Chemical – group, Sampling). All code lists (i.e., allowed values for individual parameters) are enclosed in this document, either in a particular section (e.g., Region, Method) or listed separately in the annexes below (Country, Chemical – group, Parameter) for your reference. -
Invading the Mediterranean Sea: Biodiversity Patterns Shaped by Human Activities
ORIGINAL RESEARCH ARTICLE published: 30 September 2014 MARINE SCIENCE doi: 10.3389/fmars.2014.00032 Invading the Mediterranean Sea: biodiversity patterns shaped by human activities Stelios Katsanevakis 1*, Marta Coll 2, Chiara Piroddi 1, Jeroen Steenbeek 3, Frida Ben Rais Lasram 4, Argyro Zenetos 5 and Ana Cristina Cardoso 1 1 Water Resources Unit, Institute for Environment and Sustainability, Joint Research Centre, Ispra, Italy 2 Institut de Recherche pour le Développement, UMR EME 212, Centre de Recherche Halieutique Méditerranéenne et Tropicale, Sète, France 3 Ecopath International Initiative Research Association, Barcelona, Spain 4 Unité de Recherche Ecosystèmes et Ressources Aquatiques UR03AGRO1, Institut National Agronomique de Tunisie, Tunis, Tunisia 5 Institute of Marine Biological Resources and Inland Waters, Hellenic Centre for Marine Research, Agios Kosmas, Greece Edited by: Human activities, such as shipping, aquaculture, and the opening of the Suez Canal, Christos Dimitrios Arvanitidis, have led to the introduction of nearly 1000 alien species into the Mediterranean Sea. Hellenic Centre for Marine We investigated how human activities, by providing pathways for the introduction of alien Research, Greece species, may shape the biodiversity patterns in the Mediterranean Sea. Richness of Red Reviewed by: Melih Ertan Çinar, Ege University, Sea species introduced through the Suez Canal (Lessepsian species) is very high along the 2 Turkey eastern Mediterranean coastline, reaching a maximum of 129 species per 100 km ,and Salud Deudero, Instituto Español de declines toward the north and west. The distribution of species introduced by shipping is Oceanografia, Spain strikingly different, with several hotspot areas occurring throughout the Mediterranean Christos Dimitrios Arvanitidis, Hellenic Centre for Marine basin. -
Africa-Arabia-Eurasia Plate Interactions and Implications for the Dynamics of Mediterranean Subduction and Red Sea Rifting
This page added by the GeoPRISMS office. Africa-Arabia-Eurasia plate interactions and implications for the dynamics of Mediterranean subduction and Red Sea rifting Authors: R. Reilinger, B. Hager, L. Royden, C. Burchfiel, R. Van der Hilst Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA USA, [email protected], Tel: (617)253 -7860 This page added by the GeoPRISMS office. Our proposed GeoPRISMS Initiative is based on the premise that understanding the mechanics of plate motions (i.e., the force balance on the plates) is necessary to develop realistic models for plate interactions, including processes at subduction and extensional (rifting) plate boundaries. Important advances are being made with new geologic and geophysical techniques and observations that are providing fundamental insights into the dynamics of these plate tectonic processes. Our proposed research addresses directly the following questions identified in the GeoPRISMS SCD Draft Science Plan: 4.2 (How does deformation across the subduction plate boundary evolve in space and time, through the seismic cycle and beyond?), 4.6 (What are the physical and chemical conditions that control subduction zone initiation and the development of mature arc systems?), and 4.7 (What are the critical feedbacks between surface processes and subduction zone mechanics and dynamics?). It has long been recognized that the Greater Mediterranean region provides a natural laboratory to study a wide range of geodynamic processes (Figure 1) including ocean subduction and continent- continent collision (Hellenic arc, Arabia-Eurasia collision), lithospheric delamination (E Turkey High Plateau, Alboran Sea/High Atlas), back-arc extension (Mediterranean basins, including Alboran, Central Mediterranean, Aegean), “escape” tectonics and associated continental transform faulting (Anatolia, North and East Anatolian faults), and active continental and ocean rifting (East African and northern Red Sea rifting, central Red Sea and Gulf of Aden young ocean rifting). -
Marine Mammals and Sea Turtles of the Mediterranean and Black Seas
Marine mammals and sea turtles of the Mediterranean and Black Seas MEDITERRANEAN AND BLACK SEA BASINS Main seas, straits and gulfs in the Mediterranean and Black Sea basins, together with locations mentioned in the text for the distribution of marine mammals and sea turtles Ukraine Russia SEA OF AZOV Kerch Strait Crimea Romania Georgia Slovenia France Croatia BLACK SEA Bosnia & Herzegovina Bulgaria Monaco Bosphorus LIGURIAN SEA Montenegro Strait Pelagos Sanctuary Gulf of Italy Lion ADRIATIC SEA Albania Corsica Drini Bay Spain Dardanelles Strait Greece BALEARIC SEA Turkey Sardinia Algerian- TYRRHENIAN SEA AEGEAN SEA Balearic Islands Provençal IONIAN SEA Syria Basin Strait of Sicily Cyprus Strait of Sicily Gibraltar ALBORAN SEA Hellenic Trench Lebanon Tunisia Malta LEVANTINE SEA Israel Algeria West Morocco Bank Tunisian Plateau/Gulf of SirteMEDITERRANEAN SEA Gaza Strip Jordan Suez Canal Egypt Gulf of Sirte Libya RED SEA Marine mammals and sea turtles of the Mediterranean and Black Seas Compiled by María del Mar Otero and Michela Conigliaro The designation of geographical entities in this book, and the presentation of the material, do not imply the expression of any opinion whatsoever on the part of IUCN concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The views expressed in this publication do not necessarily reflect those of IUCN. Published by Compiled by María del Mar Otero IUCN Centre for Mediterranean Cooperation, Spain © IUCN, Gland, Switzerland, and Malaga, Spain Michela Conigliaro IUCN Centre for Mediterranean Cooperation, Spain Copyright © 2012 International Union for Conservation of Nature and Natural Resources With the support of Catherine Numa IUCN Centre for Mediterranean Cooperation, Spain Annabelle Cuttelod IUCN Species Programme, United Kingdom Reproduction of this publication for educational or other non-commercial purposes is authorized without prior written permission from the copyright holder provided the sources are fully acknowledged. -
The Seasonal Variability of Sea Surface Temperature and Chlorophyll-A Concentration in the South of Makassar Strait
Available online at www.sciencedirect.com ScienceDirect Procedia Environmental Sciences 33 ( 2016 ) 583 – 599 The 2nd International Symposium on LAPAN-IPB Satellite for Food Security and Environmental Monitoring 2015, LISAT-FSEM 2015 The seasonal variability of sea surface temperature and chlorophyll-a concentration in the south of Makassar Strait Bisman Nababan*, Novilia Rosyadi, Djisman Manurung, Nyoman M. Natih, and Romdonul Hakim Department of Marine Science and Technology, Bogor Agricultural University, Jl. Lingkar Akademik, Kampus IPB Darmaga, Bogor 16680, Indonesia Abstract The sea surface temperature (SST) and chlorophyll-a (Chl-a) variabilities in the south of Makassar Strait were mostly affected by monsoonal wind speed/directions and riverine freshwater inflows. The east-southeast (ESE) wind (May-October) played a major role in an upwelling formation in the region starting in the southern tip of the southern Sulawesi Island. Of the 17 years time period, the variability of the SST values ranged from 25.7°C (August 2004) - 30.89°C (March 2007). An upwelling initiation typically occurred in early May when ESE wind speed was at <5 m/s, a fully developed upwelling event usually occurred in June when ESE wind speed reached >5 m/s, whereas the largest upwelling event always occurred in August of each year. Upwelling event generally diminished in September and terminated in October. At the time of the maximum upwelling events (August), the formation of upwelling could be observed up to about 330 km toward the southwest of the southern tip of the Sulawesi island. Interannually, El Niño Southern Oscillation (ENSO) intensified the upwelling event during the east season through an intensification of the ESE wind speed. -
DEEP SEA LEBANON RESULTS of the 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project
DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project March 2018 DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project Citation: Aguilar, R., García, S., Perry, A.L., Alvarez, H., Blanco, J., Bitar, G. 2018. 2016 Deep-sea Lebanon Expedition: Exploring Submarine Canyons. Oceana, Madrid. 94 p. DOI: 10.31230/osf.io/34cb9 Based on an official request from Lebanon’s Ministry of Environment back in 2013, Oceana has planned and carried out an expedition to survey Lebanese deep-sea canyons and escarpments. Cover: Cerianthus membranaceus © OCEANA All photos are © OCEANA Index 06 Introduction 11 Methods 16 Results 44 Areas 12 Rov surveys 16 Habitat types 44 Tarablus/Batroun 14 Infaunal surveys 16 Coralligenous habitat 44 Jounieh 14 Oceanographic and rhodolith/maërl 45 St. George beds measurements 46 Beirut 19 Sandy bottoms 15 Data analyses 46 Sayniq 15 Collaborations 20 Sandy-muddy bottoms 20 Rocky bottoms 22 Canyon heads 22 Bathyal muds 24 Species 27 Fishes 29 Crustaceans 30 Echinoderms 31 Cnidarians 36 Sponges 38 Molluscs 40 Bryozoans 40 Brachiopods 42 Tunicates 42 Annelids 42 Foraminifera 42 Algae | Deep sea Lebanon OCEANA 47 Human 50 Discussion and 68 Annex 1 85 Annex 2 impacts conclusions 68 Table A1. List of 85 Methodology for 47 Marine litter 51 Main expedition species identified assesing relative 49 Fisheries findings 84 Table A2. List conservation interest of 49 Other observations 52 Key community of threatened types and their species identified survey areas ecological importanc 84 Figure A1.