New VME Indicator Species (Excluding Corals and Sponges) and Some Potential VME Elements of the NAFO Regulatory Area
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Vmes on the Corner Seamounts] NAFO
Vulnerable Marine Ecosystems Database Newfoundland Seamounts Geographical reference Northwest Atlantic Management Body/Authority Northwest Atlantic Fisheries Organization (NAFO) Area Type Seamount closure (NAFO) Closed since 2007-01-01 until 2021-12-31 Habitat and Biology General Biology Seamounts are uniquely complex habitats that rise into bathyal and epi-pelagic depths. In general seamounts, owing to their isolation tend to support endemic populations and unique faunal assemblages. Physical description of the environment: Seamounts Newfoundland Seamounts consist of 6 peaks with summits all deeper than 2400 m, with most of the area being deeper than 3500m. The Newfoundland seamounts were volcanically active in the late Cretaceous period. Named seamounts include Shredder and Scruntion. Map FAO Fisheries and Aquaculture Department Disclaimer The boundaries and names shown and the designations used on this map do not imply the expression of any opinion whatsoever on the part of FAO concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers and boundaries. Dashed lines on maps represent approximate border lines for which there may not yet be full agreement. Management Measures specific to this area Area closed to bottom fishing from 1 Jan 2007 to 31 Dec 2010. Provisions for exploratory fishery, encounters and temporary closures. (Art 15.5-10) Period in force: 2007-01-01 to 2010-12-31 Source of information NAFO Conservation and Enforcement Measures 2010 (NAFO FC Doc. 10/1 Serial No. N5740) http://archive.nafo.int/open/fc/2010/fcdoc10-01.pdf 2010 NAFO. 2010. Scientific Council Meeting, 20-24 Sep 2010. -
Grebmeier, Jacqueline M., Lee W.Cooper, and Michael J
Limnol. Oceanogr., 35(S), 1990, 1 182-1195 0 1990, by the American Society of Limnology and Oceanography, Inc. Oxygen isotopic composition of bottom seawater and tunicate cellulose used as indicators of water masses in the northern Bering and Chukchi Seas Abstract -Oxygen isotopic composition of rivers, evaporated surface ocean waters, bottom seawater and tunicate cellulose were used melting glaciers, and melting sea ice can be as short-term and long-term indicators, respec- tively, of water-mass characteristics in the north- separated and water types characterized (e.g. ern Bering and Chukchi Seas. Oxygen isotopic Epstein and Mayeda 1953; Tan and Strain composition of northeastern Bering Sea waters is 1980; Bedard et al. 198 1). In contrast to the influenced by Yukon River inflows of IsO-de- variability in the surface ocean, average 180 : pleted continental water mixing with relatively 180-enriched waters contributed by the Anadyr 160 ratios for the deep (> 500 m) sea vary Current. Tunicate cellulose sampled under Alas- by < 1%~ when expressed in the conven- ka coastal water is more depleted in IsO than that tional 6 notation: collected under Bering shelf and Anadyr waters, which reflects the oxygen isotopic composition 6180 = (Rstd/R,mple- 1) X 1030/oo (1) of these waters. Tunicate cellulose collected un- der the mixed Bering shelf water displays inter- where R = 180 : l 6O and std is Standard Mean mediate 6180 values. Oxygen isotopic analyses of Ocean Water (SMOW). The low variability bottom seawater were used to determine the spa- in V80 values of waters in the deep sea has tial location and influence of continental and led to widespread use of oxygen isotopes as coastal-derived precipitation and of sea-ice for- mation on water-mass structure on the continen- a paleothermometric indicator. -
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. -
Atlantic Universities Geological Conference 2000
Atlantic Geology 179 Atlantic Universities Geological Conference 2000 October 12-14,2000 ABSTRACTS Conference hosted by: G.M. Dawson Geology Club Dalhousie University Halifax, Nova Scotia Again this year, abstracts from the annual Atlantic Universities Geological Conference (AUGC) are published in Atlantic Geology. This provides a permanent record o f the abstracts, and also focuses attention on the excellent quality o f these presentations and the interesting and varied geoscience that they cover. The Editors Abstracts published with financial assistance from the Earth Science Committee of APICS Atlantic Geology 36, 179-183 (2000) 0843-5561 /00/020179-5$ 1.75/0 180 AUGC-A bstracts The geology of the Fogo seamounts Ashely de Jonge Department of Geology, Saint Mary's University, Halifax, NS B3H 3C3 The Fogo seamounts are located approximately 500 km volcanism is seen across the transform margin. Flat tops of offshore Newfoundland and southwest of the Grand Banks. seamounts indicate marine erosion once volcanic activity They are early Cretaceous basalts partially buried under slope stopped, followed by subsidence as the oceanic lithosphere deposits that mantle a transform fault zone. It is believed that cooled. The flat tops show a complex pattern but are generally the seamounts formed one of two ways. They may have deeper to the NW, suggesting greater time for subsidence in formed either from the relative movement of the lithosphere that direction. This is supported by biostratigraphic and over a mantle hot spot or by magma rising along a linear fault radiometric data from wells and a dredge sample taken from zone. The distribution and age of the Fogo seamounts was the area as the seamounts appear to go decrease in age from studied to decide which of these processes was likely NW to SE. -
1 Phylogeny of the Families Pyuridae and Styelidae (Stolidobranchiata
* Manuscript 1 Phylogeny of the families Pyuridae and Styelidae (Stolidobranchiata, Ascidiacea) 2 inferred from mitochondrial and nuclear DNA sequences 3 4 Pérez-Portela Ra, b, Bishop JDDb, Davis ARc, Turon Xd 5 6 a Eco-Ethology Research Unit, Instituto Superior de Psicologia Aplicada (ISPA), Rua 7 Jardim do Tabaco, 34, 1149-041 Lisboa, Portugal 8 9 b Marine Biological Association of United Kingdom, The Laboratory Citadel Hill, PL1 10 2PB, Plymouth, UK, and School of Biological Sciences, University of Plymouth PL4 11 8AA, Plymouth, UK 12 13 c School of Biological Sciences, University of Wollongong, Wollongong NSW 2522 14 Australia 15 16 d Centre d’Estudis Avançats de Blanes (CSIC), Accés a la Cala St. Francesc 14, Blanes, 17 Girona, E-17300, Spain 18 19 Email addresses: 20 Bishop JDD: [email protected] 21 Davis AR: [email protected] 22 Turon X: [email protected] 23 24 Corresponding author: 25 Rocío Pérez-Portela 26 Eco-Ethology Research Unit, Instituto Superior de Psicologia Aplicada (ISPA), Rua 27 Jardim do Tabaco, 34, 1149-041 Lisboa, Portugal 28 Phone: + 351 21 8811226 29 Fax: + 351 21 8860954 30 [email protected] 31 1 32 Abstract 33 34 The Order Stolidobranchiata comprises the families Pyuridae, Styelidae and Molgulidae. 35 Early molecular data was consistent with monophyly of the Stolidobranchiata and also 36 the Molgulidae. Internal phylogeny and relationships between Styelidae and Pyuridae 37 were inconclusive however. In order to clarify these points we used mitochondrial and 38 nuclear sequences from 31 species of Styelidae and 25 of Pyuridae. Phylogenetic trees 39 recovered the Pyuridae as a monophyletic clade, and their genera appeared as 40 monophyletic with the exception of Pyura. -
Redalyc.Keys for the Identification of Families and Genera of Atlantic
Biota Neotropica ISSN: 1676-0611 [email protected] Instituto Virtual da Biodiversidade Brasil Moreira da Rocha, Rosana; Bastos Zanata, Thais; Moreno, Tatiane Regina Keys for the identification of families and genera of Atlantic shallow water ascidians Biota Neotropica, vol. 12, núm. 1, enero-marzo, 2012, pp. 1-35 Instituto Virtual da Biodiversidade Campinas, Brasil Available in: http://www.redalyc.org/articulo.oa?id=199123750022 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Keys for the identification of families and genera of Atlantic shallow water ascidians Rocha, R.M. et al. Biota Neotrop. 2012, 12(1): 000-000. On line version of this paper is available from: http://www.biotaneotropica.org.br/v12n1/en/abstract?identification-key+bn01712012012 A versão on-line completa deste artigo está disponível em: http://www.biotaneotropica.org.br/v12n1/pt/abstract?identification-key+bn01712012012 Received/ Recebido em 16/07/2011 - Revised/ Versão reformulada recebida em 13/03/2012 - Accepted/ Publicado em 14/03/2012 ISSN 1676-0603 (on-line) Biota Neotropica is an electronic, peer-reviewed journal edited by the Program BIOTA/FAPESP: The Virtual Institute of Biodiversity. This journal’s aim is to disseminate the results of original research work, associated or not to the program, concerned with characterization, conservation and sustainable use of biodiversity within the Neotropical region. Biota Neotropica é uma revista do Programa BIOTA/FAPESP - O Instituto Virtual da Biodiversidade, que publica resultados de pesquisa original, vinculada ou não ao programa, que abordem a temática caracterização, conservação e uso sustentável da biodiversidade na região Neotropical. -
Review of the Impact Assessment Agency's Draft Regional
Canadian Science Advisory Secretariat Newfoundland and Labrador Region Science Response 2020/033 REVIEW OF THE IMPACT ASSESSMENT AGENCY’S DRAFT REGIONAL ASSESSMENT OF OFFSHORE OIL AND GAS EXPLORATORY DRILLING EAST OF NEWFOUNDLAND AND LABRADOR Context The Impact Assessment Agency (IAA), in collaboration with Natural Resources Canada and the Newfoundland and Labrador (NL) Department of Natural Resources, and guided by a Committee appointed by the Minister of Environment and Climate Change Canada (ECCC), is developing a Regional Assessment (RA) pertaining to offshore oil and gas exploratory drilling east of Newfoundland and Labrador. The final Agreement to Conduct a Regional Assessment of Offshore Oil and Gas Exploratory Drilling East of Newfoundland and Labrador (hereafter referred to as “the Agreement”) was signed on April 15, 2019 between Her Majesty the Queen in Right of Canada as represented by the federal Ministers of the Environment and Natural Resources and Her Majesty the Queen in Right of Newfoundland and Labrador, as represented by the provincial Ministers of Natural Resources and Intergovernmental and Indigenous Affairs. On the same date, a joint committee was established between the Governments of Canada and Newfoundland and Labrador. The roles of the Committee, as well as the Task Team and the Technical Advisory Group are described in the Agreement. The RA is intended as a Regional Study pursuant to the Canadian Environmental Assessment Act (CEAA 2012) and will assess the potential effects of existing or future physical activities carried out in the Study Area (see Figure 1) which contains multiple current and proposed oil and gas exploration and production activities. The focus of the RA is to bring together existing and available data on the environmental setting of the Study Area, in order to provide a general, regional-scale description of key environmental components at a level of detail that is considered useful and appropriate for the purposes of the RA. -
Rio Grande Rise Hot Spot System' Implicationsfor African and South American Plate Motions Over Plumes
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 95, NO. BI1, PAGES 17,475-17,502,OCTOBER 10, 1990 Evolution of the Walvis Ridge-Rio Grande Rise Hot Spot System' Implicationsfor African and South American Plate Motions Over Plumes JOHN M. O'CONNOR AND ROBERT A. DUNCAN College of Oceanography,Oregon State University,Corvallis Crystallizationages of volcanicrocks, dredged or drilled from the Walvis Ridge (ten sites)and the Rio GrandeRise (one site), have been determined by the 40Ar/39Ar incremental heating technique. The fundamentallyage-progressive distribution of thesebasement ages suggests a commonhot spot sourcefor volcanismon the island of Tristan da Cunha, along the Walvis Ridge and Rio Grande Rise, and for the formation of the continental flood basalts located in Namibia (Africa) and Brazil (South America). The WalvisRidge-Rio Grande Rise volcanic system evolved along a sectionof the SouthAtlantic spreading-axis, as the African and South American plates migratedapart, astride,or in closeproximity to, an upwelling plume. Reconstructionsof the spatialrelationship between the spreading-axis,the Tristan hot spot, and the evolvingWalvis Ridge-Rio Grande Rise volcanic feature show that, at about70 Ma, thespreading-axis began to migratewestward, away from the hot spot. The resultingtransition to intraplatehot spotvolcanism along the Walvis Ridge (and associatedtermination of Rio GrandeRise formation)also involveda northward migrationof previouslyformed African seafloor over the hot spot. Rotationparameters for Africanmotion overfixed hot spots(i.e., absolutemotion) have been recalculated such that the predictedtrail of the Tristan hotspot agrees with the distribution of radiometricand fossil basement ages along the Walvis Ridge. African absolutemotion has been extended to the Southand North American plates, by the additionof relativemotion reconstructionpoles. -
Comdoc17-16 Revisionneseamountsclosure
Northwest Atlantic Fisheries Organization Serial No. N6741 NAFO/COM Doc. 17-16 [Adopted] 39th ANNUAL MEETING OF NAFO - SEPTEMBER 2017 Revision of New England Seamounts Closure Explanatory memorandum Under the revised NAFO convention, NAFO members have recommitted themselves to applying an ecosystem approach to fisheries management, including conserving the marine biodiversity within NAFO waters. This responsibility to ensure sustainable fisheries and safeguarding the marine environment has been reflected in NAFO’s efforts to protect vulnerable marine ecosystem elements, such as seamounts and their associated fisheries. In 2014, the Scientific Council recommended expansion of the seamount protection zones surrounding the New England and Corner Rise Seamount chains located within the NAFO Regulatory Area (SCS 14/17 REV). With regards to the New England and Corner Rise seamount chains, the SC recommended that the polygons be expanded to include all relevant seamounts. Subsequently, and as directed by the Commission at its 2016 annual meeting, the Joint Commission-Scientific Council Working Group on Ecosystem Approach Framework to Fisheries Management (WG-EAFFM) gave consideration to the boundary of the New England Seamounts at its July 2017 meeting. While no proposal for amendment of the current polygon was developed, there was a general agreement that the peaks shallower than 2000m must be protected. The WG also recognized that the current seamount closures included very large areas that do not contain seamounts. Therefore, and on this basis, the United States and Canada propose refining the boundary of the New England Seamounts closure reducing the overall footprint to 178 535 km2, compared to the original closure area of 275 225 km2. -
Decade of North American Geology Geologic Map of North America—Perspectives and Explanation
Decade of North American Geology Geologic Map of North America—Perspectives and explanation John C. Reed Jr. U.S. Geological Survey MS 980, Denver Federal Center Denver, Colorado 80225 USA John O. Wheeler Geological Survey of Canada 605 Robson Street Vancouver, British Columbia V6B 5J3 Canada Brian E. Tucholke Woods Hole Oceanographic Institution Department of Geology and Geophysics MS 22, Woods Hole, Massachusetts 02543-1541 USA with contributions from Will R. Stettner and David R. Soller 3300 Penrose Place, P.O. Box 9140 Boulder, Colorado 80301-9140 USA 2005 Copyright © 2005, The Geological Society of America, Inc. (GSA). All rights reserved. GSA grants permission to individual scientists to make unlimited photocopies of one or more items from this volume for noncommercial purposes advancing science or education, including classroom use. For permission to make photocopies of any item in this volume for other noncommercial, nonprofit purposes, contact the Geological Society of America. Written permission is required from GSA for all other forms of capture or reproduction of any item in the volume including, but not limited to, all types of electronic or digital scanning or other digital or manual transformation of articles or any portion thereof, such as abstracts, into computer-readable and/or transmittable form for personal or corporate use, either noncommercial or commercial, for-profit or otherwise. Send permission requests to GSA Copyright Permissions, 3300 Penrose Place, P.O. Box 9140, Boulder, Colorado 80301-9140, USA. Copyright is not claimed on any material prepared wholly by government employees within the scope of their employment. Published by The Geological Society of America, Inc. -
Phd in Marine Sciences
Title/Name of the area: Madeira – Tore Presented by Maria Ana Dionísio (PhD in marine sciences), with a grant funded by Instituto da Conservação da Natureza e das Florestas and ISPA - Instituto Universitário de Ciências Psicológicas, Sociais e da Vida, [email protected] Pedro Ivo Arriegas, Instituto da Conservação da Natureza e das Florestas, [email protected] Abstract (in less than 150 words) Madeira-Tore EBSA includes a total of 17 seamounts. Seamounts are hotspots of marine life and in general they represent areas of an enhanced productivity, especially when compared with nearby abyssal areas. This EBSA has a total area of 197431 km2 with depths ranging from 25m (top of Gettysburg seamount) to 4930m (bottom of Tore seamount). The area includes a proposed Site of Community Importance - Gorringe Bank and an OSPAR High Seas Marine Protected Area – Josephine seamount. All structures included in the Madeira-Tore EBSA fulfill four or more out of the seven EBSA scientific criteria. A total of 965 species are present in this EBSA of which 7% are protected under international or regional law. Introduction (To include: feature type(s) presented, geographic description, depth range, oceanography, general information data reported, availability of models) The Madeira-Tore EBSA includes a total of 17 seamounts (Ampere, Ashton, Coral Patch (northern part of), Dragon, Erik, Gago Coutinho, Godzilla, Gorringe Bank (Ormond and Gettysburg seamounts), Hirondelle II, Josephine, Lion, Pico Pia, Tore, Seine, Sponge Bob, and Unicorn). These seamounts present particular features which make this area eligible as an EBSA when assessed against the EBSA scientific criteria. Benthic biological communities on seamounts are highly vulnerable to human activities. -
Scs18-23 WG-ESA Report 2018
Northwest Atlantic Fisheries Organization Serial No N6900 NAFO SCS Doc. 18/23 SC WORKING GROUP ON ECOSYSTEM SCIENCE AND ASSESSMENT – NOVEMBER 2018 Report of the 11th Meeting of the NAFO Scientific Council Working Group on Ecosystem Science and Assessment (WG-ESA) NAFO Headquarters, Dartmouth, Canada 13 - 22 November 2018 Contents Introduction ........................................................................................................................................................................................................3 Theme 1: spatial considerations................................................................................................................................................................4 1.1. Update on VME indicator species data and distribution .............................................................................4 1.2 Progress on implementation of workplan for reassessment of VME fishery closures. .................9 1.3. Discussion on updating Kernel Density Analysis and SDM’s .....................................................................9 1.4. Update on the Research Activities related to EU-funded Horizon 2020 ATLAS Project ...............9 1.5. Non-sponge and non-coral VMEs (e.g. bryozoan and sea squirts). ..................................................... 14 1.6 Ecological diversity mapping and interactions with fishing on the Flemish Cap .......................... 14 1.7 Sponge removal by bottom trawling in the Flemish Cap area: implications for ecosystem functioning ...................................................................................................................................................................