Roadmap to Recovery: a Global Network of Marine Reserves
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Translation Series No.1375
FISHERIES RESEARCH BOARD OF CANADA Translation Series No. 1375 Bioebenoses and biomass of benthos of the Newfoundland-Labrador region. By Ki1N. Nesis Original title: Biotsenozy i biomassa bentosa N'yufaund- • .lendskogo-Labradorskogo raiona.. From: Trudy Vsesoyuznogo Nauchno-Issledovatel'skogo •Instituta Morskogo Rybnogo Khozyaistva Okeanografii (eNIRO), 57: 453-489, 1965. Translated by the Translation Bureau(AM) Foreign Languages Division Department of the Secretary of State of Canada Fisheries Research Board of Canada • Biological Station , st. John's, Nfld 1970 75 pages typescript 'r OEPARTMENT OF THE SECRETARY OF STATE SECRÉTARIAT D'ÉTAT TRANSLATION BUREAU BUREAU DES TRADUCTIONS FOREIGN LANGUAGES DIVISION DES LANGUES DIVISION ° CANADA ÉTRANGÈRES TRANSLATED FROM - TR,ADUCTION DE INTO - EN Russian English 'AUTHOR - AUTEUR Nesis K.N. TITLE IN ENGLISH - TITRE ; ANGLAIS Biocoenoses and biomas of benthos of the Newfolindland-Labradoriregion Title . in foreign_iangnage---(tranalitarate_foreisn -ottantatere) Biotsenozy i biomassa bentosa N i yufaundlendSkogo-Labradorskogoraiona. , .ReF5RENCE IN FOREIGN ANGUA2E (NAME OF BOOK OR PUBLICATION) IN FULL. TRANSLITERATE FOREIGN CFiA,IRACTERS. • REFERENCE' EN LANGUE ETRANGERE (NOM DU LIVRE OU PUBLICATION), AU COMPLET. TRANSCRIRE EN CARACTERES PHONETIQUEL •. Trudylesesoyuznogo nauchno-iàsledovaterskogo instituta morskogo — rybnogo khozyaistva i okeanogràfii - :REFEREN CE IN ENGLISH - RÉFÉRENCE EN ANGLAIS • Trudy of the 40.1-Union Scientific-Research Instituteof Marine . Fiseriés and Oceanography. PUBLISH ER ÉDITEUR PAGE,NUMBERS IN ORIGINAL DATE OF PUBLICATION NUMEROS DES PAGES DANS DATE DE PUBLICATION . L'ORIGINAL YE.tR ISSUE.NO . 36 VOLUME ANNEE NUMERO PLACE OF PUBLICATION NUMBER OF TYPED PAGES LIEU DE PUBLICATION NOMBRE DE PAG.ES DACTY LOGRAPHIEES 1965 5 7 REQUEr IN G• DEPA RTMENT Fisheries Research Board TRANSLATION BUREAU NO. -
Shrimp Fishing in Mexico
235 Shrimp fishing in Mexico Based on the work of D. Aguilar and J. Grande-Vidal AN OVERVIEW Mexico has coastlines of 8 475 km along the Pacific and 3 294 km along the Atlantic Oceans. Shrimp fishing in Mexico takes place in the Pacific, Gulf of Mexico and Caribbean, both by artisanal and industrial fleets. A large number of small fishing vessels use many types of gear to catch shrimp. The larger offshore shrimp vessels, numbering about 2 212, trawl using either two nets (Pacific side) or four nets (Atlantic). In 2003, shrimp production in Mexico of 123 905 tonnes came from three sources: 21.26 percent from artisanal fisheries, 28.41 percent from industrial fisheries and 50.33 percent from aquaculture activities. Shrimp is the most important fishery commodity produced in Mexico in terms of value, exports and employment. Catches of Mexican Pacific shrimp appear to have reached their maximum. There is general recognition that overcapacity is a problem in the various shrimp fleets. DEVELOPMENT AND STRUCTURE Although trawling for shrimp started in the late 1920s, shrimp has been captured in inshore areas since pre-Columbian times. Magallón-Barajas (1987) describes the lagoon shrimp fishery, developed in the pre-Hispanic era by natives of the southeastern Gulf of California, which used barriers built with mangrove sticks across the channels and mouths of estuaries and lagoons. The National Fisheries Institute (INP, 2000) and Magallón-Barajas (1987) reviewed the history of shrimp fishing on the Pacific coast of Mexico. It began in 1921 at Guaymas with two United States boats. -
Identity Crisis Or Split Personality? Trans-Ocean Distances and Not Within Individual Regions
Journal of Biogeography (J. Biogeogr.) (2007) 34, 2001–2008 GUEST Seamounts: identity crisis or split EDITORIAL personality? Craig R. McClain* Monterey Bay Aquarium Research Institute, ABSTRACT 7700 Sandholdt Road, Moss Landing, CA At present, researchers propose that over 14,000 seamounts exist and, like their 95039, USA terrestrial analogues, function like islands. In addition, seamounts are described as oases, biodiversity hotspots, and lush coral/sponge gardens. Here I discuss the extent to which these tenets regarding seamounts may be inappropriate, suffer from a lack of support, and be over-generalizations of a broad range of envi- ronmental types encountered on seamounts. Ultimately, for seamount science to progress, we need to challenge our conventional wisdom on these habitats and the extent to which all seamounts function in a similar manner. *Correspondence: Craig R. McClain, Monterey Bay Aquarium Research Institute, 7700 Keywords Sandholdt Road, Moss Landing, CA, 95039, USA. Biodiversity, conservation, coral, deep sea, ecological oasis, endemism, hotspot, E-mail: [email protected] island biogeography, isolation, seamount. biological communities that support highly unique and INTRODUCTION endemic faunas’. In ‘Toward a strategy for high seas marine There is no such things as mountains and valleys on the deep-sea protected areas’, Gjerde & Breide (2003) notes that ‘Sea- bottom. mounts are areas of high endemic biodiversity with little Mosely (1880), p. 343 overlap in community composition between seamount Less than 100 years after Mosely’s statement, Hubbs (1959) clusters’. contemplated the ‘scientific interests, particularly in respect Alternatively, others suggest that seamounts are unique to zoogeography and speciation’ of recently discovered habitats for reasons not related to their ‘islandness’. -
Cnidaria, Hydrozoa) from the Vema and Valdivia Seamounts (SE Atlantic)
European Journal of Taxonomy 758: 49–96 ISSN 2118-9773 https://doi.org/10.5852/ejt.2021.758.1425 www.europeanjournaloftaxonomy.eu 2021 · Gil M. & Ramil F. This work is licensed under a Creative Commons Attribution License (CC BY 4.0). Research article urn:lsid:zoobank.org:pub:7CA6D8AC-2312-47F9-8C17-528B94E4C8A7 Hydroids (Cnidaria, Hydrozoa) from the Vema and Valdivia seamounts (SE Atlantic) Marta GIL 1,* & Fran RAMIL 2 1,2 CIM-UVigo – Centro de Investigación Mariña, Facultade de Ciencias do Mar, Universidade de Vigo, Spain. 1 Instituto Español de Oceanografía, Centro Oceanográfi co de Vigo, Spain. * Corresponding author: [email protected] 2 Email: [email protected] 1 urn:lsid:zoobank.org:author:FFF187EB-84CE-4A54-9A01-4E4326B5CD26 2 urn:lsid:zoobank.org:author:67BAF0B6-E4D5-4A2D-8C03-D2D40D522196 Abstract. In this report, we analyse the benthic hydroids collected on the Vema and Valdivia seamounts during a survey conducted in 2015 in the SEAFO Convention Area, focused on mapping and analysing the occurrence and abundance of benthopelagic fi sh and vulnerable marine ecosystem (VMEs) indicators on selected Southeast Atlantic seamounts. A total of 27 hydroid species were identifi ed, of which 22 belong to Leptothecata and only fi ve to Anthoathecata. Monostaechoides gen. nov. was erected within the family Halopterididae to accommodate Plumularia providentiae Jarvis, 1922, and a new species, Monotheca bergstadi sp. nov., is also described. Campanularia africana is recorded for the fi rst time from the Atlantic Ocean, and the Northeast Atlantic species Amphinema biscayana, Stegopoma giganteum and Clytia gigantea are also recorded from the South Atlantic. -
Fronts in the World Ocean's Large Marine Ecosystems. ICES CM 2007
- 1 - This paper can be freely cited without prior reference to the authors International Council ICES CM 2007/D:21 for the Exploration Theme Session D: Comparative Marine Ecosystem of the Sea (ICES) Structure and Function: Descriptors and Characteristics Fronts in the World Ocean’s Large Marine Ecosystems Igor M. Belkin and Peter C. Cornillon Abstract. Oceanic fronts shape marine ecosystems; therefore front mapping and characterization is one of the most important aspects of physical oceanography. Here we report on the first effort to map and describe all major fronts in the World Ocean’s Large Marine Ecosystems (LMEs). Apart from a geographical review, these fronts are classified according to their origin and physical mechanisms that maintain them. This first-ever zero-order pattern of the LME fronts is based on a unique global frontal data base assembled at the University of Rhode Island. Thermal fronts were automatically derived from 12 years (1985-1996) of twice-daily satellite 9-km resolution global AVHRR SST fields with the Cayula-Cornillon front detection algorithm. These frontal maps serve as guidance in using hydrographic data to explore subsurface thermohaline fronts, whose surface thermal signatures have been mapped from space. Our most recent study of chlorophyll fronts in the Northwest Atlantic from high-resolution 1-km data (Belkin and O’Reilly, 2007) revealed a close spatial association between chlorophyll fronts and SST fronts, suggesting causative links between these two types of fronts. Keywords: Fronts; Large Marine Ecosystems; World Ocean; sea surface temperature. Igor M. Belkin: Graduate School of Oceanography, University of Rhode Island, 215 South Ferry Road, Narragansett, Rhode Island 02882, USA [tel.: +1 401 874 6533, fax: +1 874 6728, email: [email protected]]. -
PGCCDBS Report 2007
ICES PGCCDBS Report 2007 ICES Advisory Committee on Fisheries Management ICES CM 2007/ACFM:09 Report of the Planning Group on Commercial Catch, Discards and Biological Sampling (PGCCDBS) 5–9 March 2007 Valetta, Malta International Council for the Exploration of the Sea Conseil International pour l’Exploration de la Mer H.C. Andersens Boulevard 44-46 DK-1553 Copenhagen V Denmark Telephone (+45) 33 38 67 00 Telefax (+45) 33 93 42 15 www.ices.dk [email protected] Recommended format for purposes of citation: ICES. 2007. Report of the Planning Group on Commercial Catch, Discards and Biological Sampling (PGCCDBS), 5–9 March 2007, Valetta, Malta. ACFM:09. 115 pp. For permission to reproduce material from this publication, please apply to the General Secretary. The document is a report of an Expert Group under the auspices of the International Council for the Exploration of the Sea and does not necessarily represent the views of the Council. © 2007 International Council for the Exploration of the Sea. ICES PGCCDBS Report 2007 | i Contents Executive summary.......................................................................................................... 4 1 Introduction ............................................................................................................. 7 1.1 Terms of Reference ......................................................................................... 7 1.2 Background...................................................................................................... 7 1.3 General introductory remarks -
Ices/Nafo Wgdec Report 2015
ICES/NAFO WGDEC REPORT 2015 ICES ADVISORY COMMITTEE ICES CM 2015/ACOM:27 Report of the ICES/NAFO Joint Working Group on Deep-water Ecology (WGDEC) 16–20 February 2015 Horta, Azores, Portugal International Council for the Exploration of the Sea Conseil International pour l’Exploration de la Mer H. C. Andersens Boulevard 44–46 DK-1553 Copenhagen V Denmark Telephone (+45) 33 38 67 00 Telefax (+45) 33 93 42 15 www.ices.dk [email protected] Recommended format for purposes of citation: ICES. 2015. Report of the ICES/NAFO Joint Working Group on Deep-water Ecology (WGDEC), 16–20 February 2015, Horta, Azores, Portugal. ICES CM 2015/ACOM:27. 113 pp. For permission to reproduce material from this publication, please apply to the Gen- eral Secretary. The document is a report of an Expert Group under the auspices of the International Council for the Exploration of the Sea and does not necessarily represent the views of the Council. © 2015 International Council for the Exploration of the Sea ICES/NAFO WGDEC REPORT 2015 | i Contents Executive summary ................................................................................................................ 4 Opening of the meeting ........................................................................................................ 5 1 Adoption of the agenda ................................................................................................ 6 2 Provide all available new information on distribution of VMEs in the North Atlantic with a view to advising on any new closures to bottom fisheries or revision of existing closures to bottom fisheries (NEAFC standing request). In addition, provide new information on location of habitats sensitive to particular fishing activities (i.e. vulnerable marine ecosystems, VMEs) within EU waters (EC request) ................................... 8 2.1 Introduction ........................................................................................................... 8 2.2 Areas within the NEAFC regulatory area ........................................................ -
Prionace Glauca) Across Their Life History
Movements of Blue Sharks (Prionace glauca) across Their Life History Frederic Vandeperre1,2*, Alexandre Aires-da-Silva3, Jorge Fontes1,2, Marco Santos1,2, Ricardo Serra˜o Santos1,2, Pedro Afonso1,2 1 Centre of IMAR of the University of the Azores; Department of Oceanography and Fisheries, Horta, Portugal, 2 LARSyS Associated Laboratory, Lisboa, Portugal, 3 Inter- American Tropical Tuna Commission, La Jolla, California, United States of America Abstract Spatial structuring and segregation by sex and size is considered to be an intrinsic attribute of shark populations. These spatial patterns remain poorly understood, particularly for oceanic species such as blue shark (Prionace glauca), despite its importance for the management and conservation of this highly migratory species. This study presents the results of a long- term electronic tagging experiment to investigate the migratory patterns of blue shark, to elucidate how these patterns change across its life history and to assess the existence of a nursery area in the central North Atlantic. Blue sharks belonging to different life stages (n = 34) were tracked for periods up to 952 days during which they moved extensively (up to an estimated 28.139 km), occupying large parts of the oceanic basin. Notwithstanding a large individual variability, there were pronounced differences in movements and space use across the species’ life history. The study provides strong evidence for the existence of a discrete central North Atlantic nursery, where juveniles can reside for up to at least 2 years. In contrast with previously described nurseries of coastal and semi-pelagic sharks, this oceanic nursery is comparatively vast and open suggesting that shelter from predators is not its main function. -
Vulnerable Marine Ecosystems – Processes and Practices in the High Seas Vulnerable Marine Ecosystems Processes and Practices in the High Seas
ISSN 2070-7010 FAO 595 FISHERIES AND AQUACULTURE TECHNICAL PAPER 595 Vulnerable marine ecosystems – Processes and practices in the high seas Vulnerable marine ecosystems Processes and practices in the high seas This publication, Vulnerable Marine Ecosystems: processes and practices in the high seas, provides regional fisheries management bodies, States, and other interested parties with a summary of existing regional measures to protect vulnerable marine ecosystems from significant adverse impacts caused by deep-sea fisheries using bottom contact gears in the high seas. This publication compiles and summarizes information on the processes and practices of the regional fishery management bodies, with mandates to manage deep-sea fisheries in the high seas, to protect vulnerable marine ecosystems. ISBN 978-92-5-109340-5 ISSN 2070-7010 FAO 9 789251 093405 I5952E/2/03.17 Cover photo credits: Photo descriptions clockwise from top-left: Acanthagorgia spp., Paragorgia arborea, Vase sponges (images courtesy of Fisheries and Oceans, Canada); and Callogorgia spp. (image courtesy of Kirsty Kemp, the Zoological Society of London). FAO FISHERIES AND Vulnerable marine ecosystems AQUACULTURE TECHNICAL Processes and practices in the high seas PAPER 595 Edited by Anthony Thompson FAO Consultant Rome, Italy Jessica Sanders Fisheries Officer FAO Fisheries and Aquaculture Department Rome, Italy Merete Tandstad Fisheries Resources Officer FAO Fisheries and Aquaculture Department Rome, Italy Fabio Carocci Fishery Information Assistant FAO Fisheries and Aquaculture Department Rome, Italy and Jessica Fuller FAO Consultant Rome, Italy FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2016 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. -
Review and Analysis of International Legal and Policy Instruments Related
REVIEW AND ANALYSIS OF INTERNATIONAL LEGAL AND POLICY INSTRUMENTS RELATED TO DEEP-SEA FISHERIES AND BIODIVERSITY CONSERVATION IN AREAS BEYOND NATIONAL JURISDICTION Cover photograph: Unknown fish (possibly Antimora spp.) photographed in waters 1 800–3 000 m, 300 km northeast of St John’s, Canada. Courtesy of Bedford Institute of Oceanography. REVIEW AND ANALYSIS OF INTERNATIONAL LEGAL AND POLICY INSTRUMENTS RELATED TO DEEP-SEA FISHERIES AND BIODIVERSITY CONSERVATION IN AREAS BEYOND NATIONAL JURISDICTION Dr James Harrison Director of the Scottish Centre for International Law University of Edinburgh Law School Mr Terje Lobach International Legal specialist Prof Elisa Morgera Director of the Strathclyde Centre for Environmental Law and Governance University of Strathclyde Law School with technical inputs by Mr Pio Manoa Development Law Service FAO Legal Office The ABNJ Deep Seas Project Sustainable Fisheries Management and Biodiversity Conservation of Deep-sea Living Marine Resources and Ecosystems in the Areas Beyond National Jurisdiction (ABNJ) )RRGDQG$JULFXOWXUH2UJDQL]DWLRQRIWKH8QLWHG1DWLRQV 5RPH The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO. -
Special Publication No. 6
SECTION C 435 C-l C-1 REMARKS ON EFFECT OF FOOD ANIMALS ON COD BEHAVIOUR By Sv. Aa. Horsted and Erik Smidt1 ABSTRACT In Greenland waters cod make long spawning and feeding migrations. The most important feeding ugrations take place in early summer, when cod follow the capelin into the fjords to the shore, lnd later in the summer, when cod follow the launce over the banks in the Davis Strait and in coastal iaters. Later on cod have been observed feeding quite near the shore in coastal areas, where the food consists of small capelin, Arctic squid and euphausiids. Cod may also be concentrated near lcebergs in summer and autumn. Finally. when cod have disappeared from the upper water layers be :ause of winter cooling, large numbers can be taken on the prawn grounds, where PandaZua borealis Ls the main food. COD PURSUING THE CAPELIN INTO THE FJORDS IN THE EARLY SUMMER In West Greenland large shoals of capelin (Mal lotus villosus) migrate into many 'of the fjords :or spawning, and in Southwest Greenland they are often pursued by cod. Both when the capelin ,efore spawning swim in shoals over the deeper parts of the fjords and coastal waters and when they ~ather near shore to spawn, one can follow the cod hunting them right up to the surface (Hansen, L949, p. 40), and investigations of cod stomachs show that they are full of capelin. During this Jeriod it is often difficult to catch cod with jig or long-line, as they pay no attention to the looks, even when baited with fresh capelin. -
A Review of the Effects of Seamounts on Biological Processes
A REVIEW OF THE EFFECTS OF SEAMOUNTS ON BIOLOGICAL PROCESSES George W. Boehlert Southwest Fisheries Center Honolulu Laboratory, National Marine Fisheries Service. NOAA. 2570 Dole St., Honolulu, HI 96822-2396 Amatzia Genin Scripps Institution of Oceanography, A-008, University of California, La Jolla, CA 92093 Abstract. Seamounts interacting with oceanic continental shelf or slope counterparts at similar currents create flow complexities which depend water depths [Hubbs, 19591. In the open ocean, upon current speed, stratification. latitude, and seamounts interact with ocean currents and create seamount morphology. Seamount effects. which variability in the physical flow field. Several include internal wave generation. eddy formation. studies have described these effects on the Gulf local upwelling. and closed circulation patterns Stream [Vastano and Warren, 19761 and the Kuroshio called Taylor columns. have important effects upon [Roden et al.. 1982; Roden. 19871. The physical pelagic and benthic ecosystems over seamounts. effects include local small- and mesosca7.e phe- The biological effects of these current-topography nomena including the shedding of mesoscale eddies interactions are poorly understood. Flow accel- which alter flow patterns for significant dis- eration on upper flanks of seamounts may lead to tances downstream of the seamounts [Royer. 19781. low sedimentation but areas of high standing Biological effects of these physical complexities stocks of benthic fauna, particularly filter feed- are not well understood [Genin and Boehlert 1985; ers. Other effects extend into the water column: Boehlert, 19861. Discovery of seamount fishery nutrient enrichment and enhanced primary produc- [Uchida and Tagami. 19841 and mineral resources tivity occur over some seamounts. Longer observa- [Manheim, 19861, however, has caused increased tional periods will be necessary to understand the interest in seamount oceanography and its effects time-varying nature of such enhanced productivity on biota [Darnitsky et al.