5.2 Celtic Seas Ecoregion – Fisheries Overview, Including Mixed-Fisheries Considerations
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THE DEVELOPMENT of MESOZOIC SEDIMENTARY IBASINS AROUND the MARGINS of the NORTH ATLANTIC and THEIR HYDROCARBON POTENTIAL D.G. Masson and P.R
INTERNAL DOCUMENT IIL THE DEVELOPMENT OF MESOZOIC SEDIMENTARY IBASINS AROUND THE MARGINS OF THE NORTH ATLANTIC AND THEIR HYDROCARBON POTENTIAL D.G. Masson and P.R. Miles Internal Document No. 195 December 1983 [This document should not be cited in a published bibliography, and is supplied for the use of the recipient only]. iimsTit\jte of \ OCEANOGRAPHIC SCIENCES % INSTITUTE OF OCEANOGRAPHIC SCIENCES Wormley, Godalming, Surrey GU8 5UB (042-879-4141) (Director: Dr. A. S. Laughton, FRS) Bidston Observatory, Crossway, Birkenhead, Taunton, Mersey side L43 7RA Somerset TA1 2DW (051-653-8633) (0823-86211) (Assistant Director: Dr. D. E. Cartwright) (Assistant Director: M.J. Tucker) THE DEVELOPMENT OF MESOZOIC SEDIMENTARY BASINS AROUND THE MARGINS OF THE NORTH ATLANTIC AND THEIR HYDROCARBON POTENTIAL D.G. Masson and P.R. Miles Internal Document No. 195 December 1983 Work carried out under contract to the Department of Energy This document should not be cited in a published bibliography except as 'personal communication', and is supplied for the use of the recipient only. Institute of Oceanographic Sciences, Brook Road, Wormley, Surrey GU8 SUB ABSTRACT The distribution of Mesozoic basins around the margins of the North Atlantic has been summarised, and is discussed in terms of a new earliest Cretaceous palaeogeographic reconstruction for the North Atlantic area. The Late Triassic-Early Jurassic rift basins of Iberia, offshore eastern Canada and the continental shelf of western Europe are seen to be the fragments of a formerly coherent NE trending rift system which probably formed as a result of tensional stress between Europe, Africa and North America. The separation of Europe, North America and Iberia was preceded by a Late Jurassic-Early Cretaceous rifting phase which is clearly distinct from the earlier Mesozoic rifting episode and was little influenced by it. -
European Collection 2015
European Collection 2015 WESTERN MEDITERRANEAN & THE RIVIERAS EASTERN MEDITERRANEAN & GREEK ISLES NORTHERN EUROPE & BRITISH ISLES CONTINENTAL EUROPE CONTENTS 2 EXPERIENCE 96 TRANSOCEANIC VOYAGES The OlifeTM 104 gRAND VOYAGES 16 TASTE The Finest Cuisine at Sea 114 EXPLORE ASHORE Shore Excursion Collections & Land Tour Series 28 VALUE Best Value in Upscale Cruising 123 HOTEL PROGRAMS Pre- & Post-Cruise Hotel Programs 32 OcEANIA CLUB 126 SUITES & STATEROOMS 34 DESTINATION SPECIALISTS Culinary Discovery ToursTM & New Ports of Call 136 DECK PLANS 42 WESTERN MEDITERRANEAN 140 PROGRAMS & INFORMATION & THE RIVIERAS Travel Protection & Air Program Details 62 EASTERN MEDITERRANEAN 142 CRUISE CALENDAR & GREEK ISLES 144 EXPERIENCE OcEANIACRUISES.COM 74 NORTHERN EUROPE & BRITISH ISLES 145 GENERAL INFORMATION Oceania Club Terms & Conditions 90 CONTINENTAL EUROPE ON THE COVER Scottish kilts originate back to the 16th century and were traditionally worn as full length garments by Gaelic-speaking male Highlanders of northern Scotland POINTS OF DISTINCTION n FREE AIRFARE* on every voyage n Mid-size, elegant ships catering to just 684 or 1,250 guests n Finest cuisine at sea, served in a variety of distinctive open-seating Europe Collection restaurants, at no additional charge n Gourmet culinary program crafted 2015 by world-renowned Master Chef Jacques Pépin THE MAGIC OF THE OLD WORLD | When millenniums of history and great works n of art meet captivating cultures and generous smiles, you know you’ve arrived in Europe. Spectacular port-intensive itineraries featuring overnight visits and extended From Michelangelo’s David in Florence to Rembrandt’s masterpieces in Amsterdam, you evening port stays will be awed and inspired. Stand on the Acropolis in Athens or explore the gilded czar palaces in St. -
Is Map Is Just As Accurate As the One We're All Used To
ROSS SEA WEDDELL SEA AMUNDSEN SEA ANTARCTICA BELLINGSHAUSEN SEA AMERY ICE SHELF SOUTHERN OCEAN SOUTHERN OCEAN SOUTHERN OCEAN SCOTIA SEA DRAKE PASSAGE FALKLAND ISLANDS Stanley (U.K.) THE RATIO OF LAND TO WATER IN THE SOUTHERN HEMISPHERE BY THE TIME EUROPEANS ADOPTED IS 1 TO 5 THE NORTH-POINTING COMPASS, PTOLEMY WAS A HELLENIC Wellington THEY WERE ALREADY EXPERIENCED NEW TASMAN SEA ZEALAND CARTOGRAPHER WHOSE WORK CHILE IN NAVIGATING WITH REFERENCE TO IN THE SECOND CENTURY A.D. ARGENTINA THE NORTH STAR Canberra Buenos Santiago GREAT AUSTRALIAN BIGHT POPULARIZED NORTH-UP Montevideo Aires SOUTH PACIFIC OCEAN SOUTH ATLANTIC OCEAN URUGUAY ORIENTATION SOUTH AFRICA Maseru LESOTHO SWAZILAND Mbabane Maputo Asunción AUSTRALIA Pretoria Gaborone NEW Windhoek PARAGUAY TONGA Nouméa CALEDONIA BOTSWANA Saint Denis NAMIBIA Nuku’Alofa (FRANCE) MAURITIUS Port Louis Antananarivo MOZAMBIQUE CHANNEL ZIMBABWE Suva Port Vila MADAGASCAR VANUATU MOZAMBIQUE Harare La Paz INDIAN OCEAN Brasília LAKE SOUTH PACIFIC OCEAN FIJI Lusaka TITICACA CORAL SEA GREAT GULF OF BARRIER CARPENTARIA Lilongwe ZAMBIA BOLIVIA FRENCH POLYNESIA Apia REEF LAKE (FRANCE) SAMOA TIMOR SEA COMOROS NYASA ANGOLA Lima Moroni MALAWI Honiara ARAFURA SEA BRAZIL TIMOR LESTE PERU Funafuti SOLOMON Port Dili Luanda ISLANDS Moresby LAKE Dodoma TANGANYIKA TUVALU PAPUA Jakarta SEYCHELLES TANZANIA NEW GUINEA Kinshasa Victoria BURUNDI Bujumbura DEMOCRATIC KIRIBATI Brazzaville Kigali REPUBLIC LAKE OF THE CONGO SÃO TOMÉ Nairobi RWANDA GABON ECUADOR EQUATOR INDONESIA VICTORIA REP. OF AND PRINCIPE KIRIBATI EQUATOR -
Chapter 24. the BAY of BISCAY: the ENCOUNTERING of the OCEAN and the SHELF (18B,E)
Chapter 24. THE BAY OF BISCAY: THE ENCOUNTERING OF THE OCEAN AND THE SHELF (18b,E) ALICIA LAVIN, LUIS VALDES, FRANCISCO SANCHEZ, PABLO ABAUNZA Instituto Español de Oceanografía (IEO) ANDRE FOREST, JEAN BOUCHER, PASCAL LAZURE, ANNE-MARIE JEGOU Institut Français de Recherche pour l’Exploitation de la MER (IFREMER) Contents 1. Introduction 2. Geography of the Bay of Biscay 3. Hydrography 4. Biology of the Pelagic Ecosystem 5. Biology of Fishes and Main Fisheries 6. Changes and risks to the Bay of Biscay Marine Ecosystem 7. Concluding remarks Bibliography 1. Introduction The Bay of Biscay is an arm of the Atlantic Ocean, indenting the coast of W Europe from NW France (Offshore of Brittany) to NW Spain (Galicia). Tradition- ally the southern limit is considered to be Cape Ortegal in NW Spain, but in this contribution we follow the criterion of other authors (i.e. Sánchez and Olaso, 2004) that extends the southern limit up to Cape Finisterre, at 43∞ N latitude, in order to get a more consistent analysis of oceanographic, geomorphological and biological characteristics observed in the bay. The Bay of Biscay forms a fairly regular curve, broken on the French coast by the estuaries of the rivers (i.e. Loire and Gironde). The southeastern shore is straight and sandy whereas the Spanish coast is rugged and its northwest part is characterized by many large V-shaped coastal inlets (rias) (Evans and Prego, 2003). The area has been identified as a unit since Roman times, when it was called Sinus Aquitanicus, Sinus Cantabricus or Cantaber Oceanus. The coast has been inhabited since prehistoric times and nowadays the region supports an important population (Valdés and Lavín, 2002) with various noteworthy commercial and fishing ports (i.e. -
Names of Sub-Areas and Divisions of FAO Fishing Areas 27 and 37 NORTH-EAST ATLANTIC
Names of Sub-areas and Divisions of FAO fishing areas 27 and 37 NORTH-EAST ATLANTIC Subarea I Barents Sea Subarea II Norwegian Sea, Spitzbergen, and Bear Island Division II a Norwegian Sea Division II b Spitzbergen and Bear Island Subarea III Skagerrak, Kattegat, Sound, Belt Sea, and Baltic Sea; the Sound and Belt together known also as the Transition Area Division III a Skagerrak and Kattegat Division III b,c Sound and Belt Sea or Transition Area Division III b (23) Sound Division III c (22) Belt Sea Division III d (24-32) Baltic Sea Subarea IV North Sea Division IV a Northern North Sea Division IV b Central North Sea Division IV c Southern North Sea Subarea V Iceland and Faroes Grounds Division V a Iceland Grounds Division V b Faroes Grounds Subarea VI Rockall, Northwest Coast of Scotland and North Ireland, the Northwest Coast of Scotland and North Ireland also known as the West of Scotland Division VI a Northwest Coast of Scotland and North Ireland or West of Scotland Division VI b Rockall Subarea VII Irish Sea, West of Ireland, Porcupine Bank, Eastern and Western English Channel, Bristol Channel, Celtic Sea North and South, and Southwest of Ireland - East and West Division VII a Irish Sea Division VII b West of Ireland Division VII c Porcupine Bank Division VII d Eastern English Channel Division VII e Western English Channel Division VII f Bristol Channel Division VII g Celtic Sea North Division VII h Celtic Sea South Division VII j South-West of Ireland - East Division VII k South-West of Ireland - West Subarea VIII Bay of Biscay -
Bianca Elliott Lesson Title WHAT to THINK ABOUT the BALKAN
Bianca Elliott Lesson Title WHAT TO THINK ABOUT THE BALKAN SITUATION IN THE 1800S AND 1900S Class and Grade level(s) High School World History Classes or Western Civilization Classes Goals and Objectives The student will be able to: • Read and view materials that provide multiple views of the Balkan situation in the 1800 and 1900 AD. • After reading the selections, students will determine the geographic relevance of the activi- ties that occurred in the Balkans and the political entities involved. • Students will then decide if geography played a critical part in the decision they made and the decisions made in the past. They will verify their answers. • Students will analyze the different forces pulling at and within the Balkans and determine if there were any other ways the end could have changed and how. Curriculum standards addressed: Geography: The student uses a working knowledge and understanding of the spatial organiza- tion of Earth’s surface and relationships between peoples and places and physical and human environments in order to explain the interactions that occur in Kansas, the United States, and in our world. Benchmark 1: Geographic Tools and Location: The student uses maps, graphic representations, tools, and technologies to locate, use, and present information about people, places, and environ- ments. The student: 1. (K) locates major political and physical features of Earth from memory and compares the rela- tive locations of those features. Locations will be included in indicator at each grade level (e.g., Beijing, English Channel, India, Iraq, Moscow, Sahara Desert, South Africa, Venezuela, Balkan Peninsula, Berlin, Black Sea, Bosporus Strait, Euphrates River, Geneva, Hong Kong, Israel, Libya, North Korea, Pakistan, Saudi Arabia, Singapore, South Korea, Suez Canal, Tigris River, Tokyo, Yangtze River). -
Temporal Patterns in Habitat Use by Small Cetaceans at an Oceanographically Dynamic Marine Renewable Energy Test Site in the Celtic Sea
Deep-Sea Research II ∎ (∎∎∎∎) ∎∎∎–∎∎∎ Contents lists available at ScienceDirect Deep-Sea Research II journal homepage: www.elsevier.com/locate/dsr2 SI: European Marine Megafauna Temporal patterns in habitat use by small cetaceans at an oceanographically dynamic marine renewable energy test site in the Celtic Sea S.L. Cox a,b,n, M.J. Witt c, C.B. Embling a,d, B.J. Godley d, P.J. Hosegood b, P.I. Miller e, S.C. Votier c, S.N. Ingram a a Marine Biology and Ecology Research Centre, Plymouth University, Plymouth PL4 8AA, UK b Marine Physics Research Group, Plymouth University, Plymouth PL4 8AA, UK c Environment and Sustainability Institute, University of Exeter, Penryn TR10 9FE, UK d Centre for Ecology and Conservation, College of Life Sciences, University of Exeter, Penryn TR10 9FE, UK e Plymouth Marine Laboratory, Prospect Place, Plymouth PL1 3DH, UK article info abstract Shelf-seas are highly dynamic and oceanographically complex environments, which likely influences the Keywords: spatio-temporal distributions of marine megafauna such as marine mammals. As such, understanding Marine predator natural patterns in habitat use by these animals is essential when attempting to ascertain and assess the Habitat use impacts of anthropogenically induced disturbances, such as those associated with marine renewable Fronts energy installations (MREIs). This study uses a five year (2009–2013) passive acoustics (C-POD) dataset to Passive acoustics examine the use of an oceanographically dynamic marine renewable energy test site by small cetaceans, Marine -
Annual Variation in Diets, Feeding Locations and Foraging Behaviour of Gannets in the North Sea: Flexibility, Consistency and Constraint
MARINE ECOLOGY PROGRESS SERIES Vol. 338: 295–305, 2007 Published May 24 Mar Ecol Prog Ser Annual variation in diets, feeding locations and foraging behaviour of gannets in the North Sea: flexibility, consistency and constraint K. C. Hamer1,*, E. M. Humphreys1, 2, S. Garthe3, J. Hennicke4, G. Peters5, D. Grémillet6, R. A. Phillips7, M. P. Harris8, S. Wanless8 1Earth Biosphere Institute and Faculty of Biological Sciences, University of Leeds, Leeds LS2 9JT, UK 2British Trust for Ornithology Scotland, School of Biological and Environmental Sciences, Stirling University, Stirling FK9 4LA, UK 3Centre for Research and Technology Westkuste, University of Kiel, 25761 Büsum, Germany 4Institute of Zoology, University of Hamburg, 20146 Hamburg, Germany 5Earth & Ocean Technologies, Krummbogen 32, 24113 Kiel, Germany 6Percy FitzPatrick Institute, University of Cape Town, Rondebosch 7701, South Africa 7NERC British Antarctic Survey, Madingley Road, Cambridge CB3 0ET, UK 8NERC Centre for Ecology and Hydrology, Banchory Research Station, Hill of Brathens, Aberdeenshire AB31 4BY, UK ABSTRACT: Many seabirds nesting in areas bordering the North Sea have recently experienced large annual variation in breeding success, including reproductive failures in some cases. In contrast, the breeding success of northern gannets Morus bassanus has remained remarkably stable. The pre- sent study examines data from the large gannet colony at the Bass Rock (southeast Scotland) across 3 years, to assess the extent to which such stability may reflect both flexibility and consistency in diets and foraging behaviour. Adults exhibited great flexibility both in the species and sizes of prey con- sumed and in foraging trip durations, ranges and total distances travelled. They also showed a high degree of consistency in bearings of foraging trips and in behaviour at sea; the sinuosity of foraging tracks and average speed of travel was very similar each year and birds in all years spent about half their time at sea in flight. -
Emodnet Phase 2 – Final Report Reporting Period: 01/09/2013 – 01/09/2016
EMODnet Thematic Lot n° 5 Biology EMODnet Phase 2 – Final report Reporting Period: 01/09/2013 – 01/09/2016 Simon Claus1, Dan Lear2, Daphnis De Pooter1, Leen Vandepitte1, Nicolas Bailly3, Olivier Beauchard4, Peter Herman4, Lennert Tyberghein1, Klaas Deneudt1, Francisco Souza Dias1, Francisco Hernandez1, and project partners5 1: Flanders Marine Institute (VLIZ, Belgium) 2: Marine Biological Association (MBA, United Kingdom) 3: Hellenic Centre for Marine Research (HCMR, Greece) 4: Royal Netherlands Institute for Sea Research (NIOZ, The Netherlands) 5: The International Council for Exploration of the Sea (ICES), the Sir Alister Hardy Foundation for Ocean Science (SAHFOS, United Kingdom), the Université de Liège, GeoHydrodynamics and Environment Research (GHER, Belgium), the Global Biodiversity Information Facility (GBIF), the University of Bremen, Centre for Marine Environmental Sciences (MARUM, Germany), the Marine Information Service (MARIS, The Netherlands), the Swedish Meteorological and Hydrological Institute (SMHI, Sweden), the Instituto Español de Oceanografía (IEO, Spain), the Havforskningsinstituttet Institute of Marine Research (IMR, Norway), the Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER, France), the Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Section of Oceanography (OGS, Italy), the Aarhus University, DCE-Danish Centre for Environment and Energy (Denmark), the Institute for Agricultural and Fisheries Research (ILVO, Belgium), the Stichting Deltares (The Netherlands) and IMARES (The -
English Channel (East) / Dover Strait
Seascape Assessment for the South Marine Plan Areas MCA 12: English Channel (East) / Dover Strait Snapshot Key Characteristics Description Visual Resource Mapping © Crown copyright and database right 2013. All rights reserved. Permission Number Defra 012012.003. Contains Ordnance Survey Licence No. 100049981 and UK Hydrographic Office data. © Marine Management Organisation. Licence No EK001-201188. Esri, GEBCO, NOAA, CHS, CSUMB, National Geographic, DeLorme, and NAVTEQ. MCA 12: English Channel (East) / Dover Strait Overall cShnaarpaschteort Key Characteristics Description Visual Resource Mapping Location and boundaries The Marine Character Area (MCA) covers the Dover Strait, as depicted on the international Vessel Traffic Services (VTS) guide. The inshore boundaries largely follow the Traffic Separation Zone of the shipping channel (approximately 20 kilometres or 11 nautical miles offshore), whilst the outer boundaries are formed by the edge of the offshore marine plan area and territorial limits, approximately 55 kilometres (30 nautical miles) from the coast. The functional extent of the Dover Strait stretches beyond English territorial waters into France, where the second shipping lane is located. The shipping lane in English waters contains south moving traffic, and the two one-way lanes are separated by a Traffic Separation Zone. The functional extent of the Channel extends eastwards into adjoining MCAs 13 and 14. Please note that the MCA boundaries represent broad zones of transition (not immediate breaks in character). Natural, visual, cultural and socio- economic relationships between adjacent MCAs play a key role in shaping overall character. Therefore individual MCAs should not be considered in isolation. Overall character This MCA has a rich physical and cultural heritage that is reflected in its character today. -
Atlantic Herring (Clupea Harengus) in the Irish and Celtic Seas; Tracing Populations of the Past and Present
Atlantic herring (Clupea harengus) in the Irish and Celtic Seas; tracing populations of the past and present Nóirín D. Burke A thesis submitted to the School of Science, Galway Mayo Institute of Technology in fulfilment for the degree of Doctor of Philosophy Department of Life and Physical Sciences June 2008 Head of Department: Dr Seamus Lennon Supervisors: Dr Deirdre Brophy Dr Pauline A. King Galway-Mayo Institute of Technology, Dublin Rd., Galway, Ireland TABLE OF CONTENTS Chapter 1: General Introduction……………………………………………........... 10 1.1 Herring biology and population structure………………………. 10 1.2 Herring fisheries around Ireland………………………………... 12 1.3 Stock structure of Celtic and Irish Sea herring………………….. 14 1.4 Herring assessments in the Irish and Celtic Seas……………….. 15 1.5 Otolith applications in fisheries science………………………… 16 1.6 Otolith microstructure……………...……………………………. 17 1.7 Otolith morphometrics and shape analysis……………………… 18 1.8 Summary of objectives………………………………………….. 19 Chapter 2: Shape analysis of otolith annuli in Atlantic herring (Clupea harengus); a new method for tracking fish populations………………………….. 23 2.1 Abstract………………………………………………………….. 23 2.2 Introduction……………………………………………………… 23 2.3 Methods………………………………………………………….. 26 2.4 Results…………………………………………………………… 32 2.5 Discussion……………………………………………………….. 33 2.6 Conclusion……………………………………………………….. 40 Chapter 3: Otolith shape analysis, its applications to distinguishing between Irish and Celtic Sea herring (Clupea harengus) stocks in the Irish Sea……………….. 49 3.1 Abstract………………………………………………………….. 49 3.2 Introduction……………………………………………………… 49 3.3 Methods…………………………………………………………. 51 3.4 Results…………………………………………………………… 54 3.5 Discussion……………………………………………………….. 55 3.6 Conclusion……………………………………………………….. 57 Chapter 4: Otolith shape analysis provides evidence of natal homing in Atlantic herring (Clupea harengus)………………………………………………………… 62 4.1 Abstract………………………………………………………….. 62 4.2 Introduction……………………………………………………… 62 4.3 Methods…………………………………………………………. -
Celtic Seas Ecoregion – Ecosystem Overview
ICES Ecosystem Overviews Celtic Seas Ecoregion Published 14 December 2018 https://doi.org/ 10.17895/ices.pub.4667 7.1 Celtic Seas Ecoregion – Ecosystem overview Ecoregion description The Celtic Seas ecoregion covers the northwestern shelf seas of the EU. It includes areas of the deeper eastern Atlantic Ocean and coastal seas that are heavily influenced by oceanic inputs. The ecoregion ranges from north of Shetland to Brittany in the south. Three key areas constitute this ecoregion: • the Malin shelf; • the Celtic Sea and west of Ireland; • the Irish Sea. The Celtic Seas ecoregion includes all or parts of the Exclusive Economic Zones (EEZs) of three EU Member States. Fisheries in the Celtic Seas are managed through the EU Common Fisheries Policy (CFP), with fisheries of some stocks managed by the North East Atlantic Fisheries Commission (NEAFC) and by coastal state agreements. Responsibility for salmon fisheries is taken by the North Atlantic Salmon Conservation Organization (NASCO) and for large pelagic fish by the International Commission for the Conservation of Atlantic Tunas (ICCAT). Collective fisheries advice is provided by the International Council for the Exploration of the Sea (ICES), the European Commission’s Scientific Technical and Economic Committee for Fisheries (STECF), and the North Western Waters and Pelagic ACs. Environmental policy is managed by national governments and agencies and by OSPAR; advice is provided by national agencies, OSPAR, the European Environment Agency (EEA), and ICES. International shipping is managed under the International Maritime Organization (IMO). Figure 1 The Celtic Seas ecoregion, showing EEZs, larger offshore Natura 2000 sites, and operational and authorized wind farms.