Report of the ICES\NAFO Joint Working Group on Deep-Water Ecology (WGDEC)
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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. -
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. -
Title a DISTRIBUTION STUDY of the OCTOCORALLIA OF
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Kyoto University Research Information Repository A DISTRIBUTION STUDY OF THE OCTOCORALLIA OF Title OREGON Author(s) Belcik, Francis P. PUBLICATIONS OF THE SETO MARINE BIOLOGICAL Citation LABORATORY (1977), 24(1-3): 49-52 Issue Date 1977-11-30 URL http://hdl.handle.net/2433/175960 Right Type Departmental Bulletin Paper Textversion publisher Kyoto University A DISTRIBUTION STUDY OF THE OCTOCORALLIA OF OREGON FRANCIS P. BELCIK Department of Biology, East Carolina University, Greenville, North Carolina 27834, U.S.A. With Text-figure 1 and Tables 1-2 Introduction: The purpose of this report was to identify the species of octocorals, note their occurrence or distribution and also their numbers. The Octocorals of this report were collected :rhainly from the Oregonian Region. The majority of specimens were collected by the Oceanography Department of Oregon State University at depths below 86 meters. A few inshore species were collected at various sites along the Oregon Coast (see Fig. 1). Only two species were found in the Intertidal Zone; the bulk of the Octocoral fauna occur offshore in deeper water. Most of the deep water specimens are now deposited in the Oceanography Department of Oregon State University in Corvallis, Oregon. The inshore speci mens have remained in my personal collection. Identification Methods: No references have been published for the soft corals of Oregon; although col lections have possibly been made in the past. Helpful sources for identification, after the standard methods of corrosion, and spicule measurements have been made are: Bayer, 1961; Hickson, 1915; Kiikenthal, 1907, and 1913; Nutting, 1909 and 1912; Utinomi, 1960, 1961, and 1966 and Verrill, 1922. -
Deep-Sea Coral Taxa in the Alaska Region: Depth and Geographical Distribution (V
Deep-Sea Coral Taxa in the Alaska Region: Depth and Geographical Distribution (v. 2020) Robert P. Stone1 and Stephen D. Cairns2 1. NOAA Auke Bay Laboratories, Alaska Fisheries Science Center, Juneau, AK 2. National Museum of Natural History, Smithsonian Institution, Washington, DC This annex to the Alaska regional chapter in “The State of Deep-Sea Coral Ecosystems of the United States” lists deep-sea coral species in the Phylum Cnidaria, Classes Anthozoa and Hydrozoa, known to occur in the U.S. Alaska region (Figure 1). Deep-sea corals are defined as azooxanthellate, heterotrophic coral species occurring in waters 50 meters deep or more. Details are provided on the vertical and geographic extent of each species (Table 1). This list is an update of the peer-reviewed 2017 list (Stone and Cairns 2017) and includes taxa recognized through 2020. Records are drawn from the published literature (including species descriptions) and from specimen collections that have been definitively identified by experts through examination of microscopic characters. Video records collected by the senior author have also been used if considered highly reliable; that is, in situ identifications were made based on an expertly identified voucher specimen collected nearby. Taxonomic names are generally those currently accepted in the World Register of Marine Species (WoRMS), and are arranged by order, and alphabetically within order by suborder (if applicable), family, genus, and species. Data sources (references) listed are those principally used to establish geographic and depth distribution, and are numbered accordingly. In summary, we have confirmed the presence of 142 unique coral taxa in Alaskan waters, including three species of alcyonaceans described since our 2017 list. -
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. -
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. -
VME Database Meeting [IX.5
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 2020-12-31 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. Closure rolled over until 31 Dec 2014. Provisions for exploratory fishery, encounters and temporary closures. (Art 15.5-10) Period in force: 2007-01-01 to 2014-12-31 Source of information NAFO Conservation and Enforcement Measures 2011 (NAFO FC Doc. 11/1 Serial No. N5867) http://archive.nafo.int/open/fc/2011/fcdoc11-01.pdf 2011 NAFO. -
Novel Secondary Metabolites from Selected Cold Water
NOVEL SECONDARY METABOLITES FROM SELECTED COLD WATER MARINE INVERTEBRATES By DAVID ELLIS WILLIAMS B.Sc.Hons, King's College, University of London, 1983 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in THE FACULTY OF GRADUATE STUDIES (Department of Chemistry) We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA October 1987 ® David Ellis Williams, 1987 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the head of my department or by his or her representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department The University of British Columbia 1956 Main Mall Vancouver, Canada DE-6(3/81) ABSTRACT. A study of the secondary metabolism of two nudibranchs and one soft coral has led to the isolation of eighteen new and two known secondary metabolites. The structures of all compounds were determined by a combination of the interpretation of spectral data, chemical degradations and interconversions, and single crystal x-ray diffraction analysis. The British Columbian dorid nudibranch Diaulula sandiegensis yielded two new steroidal metabolites, diaulusterols A (41) and B (42). The 25-(3-hydroxybutanoate) residue of diaulusterol A (41) and the 2a,3a-diol array of both 41 and 42 are not commonly encountered in naturally occurring steroids. -
An Examination of the Distribution, Abundance, and Habitat Preferences of Soft Corals (Octocorallia: Alcyonacea) in Offshore Nova Scotian Waters
An examination of the distribution, abundance, and habitat preferences of soft corals (Octocorallia: Alcyonacea) in offshore Nova Scotian waters ENVS 4902 Environmental Science Undergraduate Honours Thesis Lauren Ballantyne BSc. Honours Co-op Environmental Science minor in Biology Dalhousie University, Halifax, NS Supervisor: Dr. Susan Gass Senior Instructor and Academic Advisor Environmental Science Dalhousie University, Halifax, NS Supervisor: Dr. Francisco Javier Murillo Perez Research Scientist Ocean and Ecosystem Science Division of DFO Bedford Institute of Oceanography, Dartmouth, NS Course Instructor: Dr. Tarah Wright Professor Environmental Science Dalhousie University, Halifax, NS April 20, 2018 TABLE OF CONTENTS LIST OF FIGURES..................................................................................................................... IV LIST OF TABLES......................................................................................................................... V GLOSSARY ................................................................................................................................. VI ABSTRACT .............................................................................................................................. VIII 1.0 INTRODUCTION .................................................................................................................... 1 2.0 LITERATURE REVIEW ........................................................................................................ 8 2.1 CORAL -
New Taxa and Revisionary Systematics of Alcyonacean Octocorals from the Pacific Coast of North America (Cnidaria, Anthozoa)
A peer-reviewed open-access journal ZooKeys 283:New 15–42 taxa (2013) and revisionary systematics of alcyonacean octocorals from the Pacific coast... 15 doi: 10.3897/zookeys.283.4803 RESEARCH ARTICLE www.zookeys.org Launched to accelerate biodiversity research New taxa and revisionary systematics of alcyonacean octocorals from the Pacific coast of North America (Cnidaria, Anthozoa) Gary C. Williams1,† 1 Department of Invertebrate Zoology and Geology, California Academy of Sciences, 55 Music Concourse Dri- ve, San Francisco, California, 94118, USA † urn:lsid:zoobank.org:pub:B988C1E1-7D0A-44E1-9E7D-766D2CEC9079 Corresponding author: Gary C. Williams ([email protected]) Academic editor: B.W. Hoeksema | Received 4 February 2013 | Accepted 8 March 2013 | Published 3 April 2013 urn:lsid:zoobank.org:author:4BD094B7-F9C6-4FB5-89F4-3BAAFF46DD96 Citation: Williams GC (2013) New taxa and revisionary systematics of alcyonacean octocorals from the Pacific coast of North America (Cnidaria, Anthozoa). ZooKeys 283: 15–42. doi: 10.3897/zookeys.283.4803 Abstract A taxonomic assessment of four species of octocorals from the northeastern Pacific Ocean (British Colum- bia to California) is provided. Included here are a new species of clavulariid stolonifieran Cryptophyton, a new species of the nephtheid soft coral Gersemia, an undetermined species of soft coral in the genus Alcyonium that has been referred in the literature by several other names, and a new genus is named for a plexaurid sea fan originally described in the Indo-Pacific genusEuplexaura . Discussions are included that compare the species to related taxa, or provide revisionary assessments. Keywords Alcyonium, Cryptophyton, Gersemia, Octocorallia, northeastern Pacific, plexaurid gorgonian, soft corals, taxonomy Introduction Bayer (1981a: 7–9) reviewed the present status of knowledge of octocorals in the major geographical regions of the world and established four categories representing broad levels of taxonomic knowledge – essentially complete, moderately well-known, poorly Copyright Gary C.