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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. -
World Cruise - 2022 Use the Down Arrow from a Form Field
This document contains both information and form fields. To read information, World Cruise - 2022 use the Down Arrow from a form field. 20 world JAN 5, 2022 JAN 19, 2022 JAN 19, 2022 JAN 5, 2022 111 days 111 days 97 days 88 days 22 cruise roundtrip from roundtrip from Los Angeles to Ft. Lauderdale Ft. Lauderdale Los Angeles Ft. Lauderdale to Rome Florence/Pisa (Livorno) Genoa Rome (Civitavecchia) Catania Monte Carlo (Sicily) MONACO ITALY Naples Marseille Mykonos FRANCE GREECE Kusadasi PORTUGAL Atlantic Barcelona Heraklion Ocean SPAIN (Crete) Los Angeles Lisbon TURKEY UNITED Bermuda Ceuta Jerusalem/Bethlehem STATES (West End) (Spanish Morocco) Seville (Ashdod) ine (Cadiz) ISRAEL Athens e JORDAN Dubai Agadir (Piraeus) Aqaba Pacific MEXICO Madeira UNITED ARAB Ocean MOROCCO l Dat L (Funchal) Malta EMIRATES Ft. Lauderdale CANARY (Valletta) Suez Abu ISLANDS Canal Honolulu Huatulco Dhabi ne inn Puerto Santa Cruz Lanzarote OMAN a a Hawaii r o Hilo Vallarta NICARAGUA (Arrecife) de Tenerife Salãlah t t Kuala Lumpur I San Juan del Sur Cartagena (Port Kelang) Costa Rica COLOMBIA Sri Lanka PANAMA (Puntarenas) Equator (Colombo) Singapore Equator Panama Canal MALAYSIA INDONESIA Bali SAMOA (Benoa) AMERICAN Apia SAMOA Pago Pago AUSTRALIA South Pacific South Indian Ocean Atlantic Ocean Ocean Perth Auckland (Fremantle) Adelaide Sydney New Plymouth Burnie Picton Departure Ports Tasmania Christchurch More Ashore (Lyttelton) Overnight Fiordland NEW National Park ZEALAND up to continentscontinents (North America, South America, 111 51 Australia, Europe, Africa -
The Crotone Megalandslide, Southern Italy: Architecture, Timing And
www.nature.com/scientificreports OPEN The Crotone Megalandslide, southern Italy: Architecture, timing and tectonic control Received: 2 March 2018 Massimo Zecchin1, Flavio Accaino1, Silvia Ceramicola1, Dario Civile1, Salvatore Critelli2, Accepted: 1 May 2018 Cristina Da Lio3, Giacomo Mangano1, Giacomo Prosser4, Pietro Teatini3,5 & Luigi Tosi3 Published: xx xx xxxx Large-scale submarine gravitational land movements involving even more than 1,000 m thick sedimentary successions are known as megalandslides. We prove the existence of large-scale gravitational phenomena of the Crotone Basin, a forearc basin located on the Ionian side of Calabria (southern Italy), by seismic, morpho-bathymetric and well data. Our study reveals that the Crotone Megalandslide started moving between Late Zanclean and Early Piacenzian and was triggered by a contractional tectonic event leading to the basin inversion. Seaward gliding of the megalandslide continued until roughly Late Gelasian, and then resumed since Middle Pleistocene with a modest rate. Interestingly, the onshore part of the basin does not show a gravity-driven deformation comparable to that observed in the marine area, and this peculiar evidence allows some speculations on the origin of the megalandslide. Kilometer- to tens of km-scale submarine gravitational collapses, here referred to as megalandslides, consist of land movements involving up to 1 km (or even more) thick sedimentary successions sliding on a basal surface that may classify as ‘basal overpressured shale detachment’ or ‘salt detachment’1. Gravity gliding may be instanta- neous, associated with mass wasting and shallow detachment, or slow, in connection with a deep detachment and long-term geological processes such as high sedimentation rates or uplif in adjacent areas1. -
Ecosystems Mario V
Ecosystems Mario V. Balzan, Abed El Rahman Hassoun, Najet Aroua, Virginie Baldy, Magda Bou Dagher, Cristina Branquinho, Jean-Claude Dutay, Monia El Bour, Frédéric Médail, Meryem Mojtahid, et al. To cite this version: Mario V. Balzan, Abed El Rahman Hassoun, Najet Aroua, Virginie Baldy, Magda Bou Dagher, et al.. Ecosystems. Cramer W, Guiot J, Marini K. Climate and Environmental Change in the Mediterranean Basin -Current Situation and Risks for the Future, Union for the Mediterranean, Plan Bleu, UNEP/MAP, Marseille, France, pp.323-468, 2021, ISBN: 978-2-9577416-0-1. hal-03210122 HAL Id: hal-03210122 https://hal-amu.archives-ouvertes.fr/hal-03210122 Submitted on 28 Apr 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Climate and Environmental Change in the Mediterranean Basin – Current Situation and Risks for the Future First Mediterranean Assessment Report (MAR1) Chapter 4 Ecosystems Coordinating Lead Authors: Mario V. Balzan (Malta), Abed El Rahman Hassoun (Lebanon) Lead Authors: Najet Aroua (Algeria), Virginie Baldy (France), Magda Bou Dagher (Lebanon), Cristina Branquinho (Portugal), Jean-Claude Dutay (France), Monia El Bour (Tunisia), Frédéric Médail (France), Meryem Mojtahid (Morocco/France), Alejandra Morán-Ordóñez (Spain), Pier Paolo Roggero (Italy), Sergio Rossi Heras (Italy), Bertrand Schatz (France), Ioannis N. -
Is the Gulf of Taranto an Historic Bay?*
Ronzitti: Gulf of Taranto IS THE GULF OF TARANTO AN HISTORIC BAY?* Natalino Ronzitti** I. INTRODUCTION Italy's shores bordering the Ionian Sea, particularly the seg ment joining Cape Spartivento to Cape Santa Maria di Leuca, form a coastline which is deeply indented and cut into. The Gulf of Taranto is the major indentation along the Ionian coast. The line joining the two points of the entrance of the Gulf (Alice Point Cape Santa Maria di Leuca) is approximately sixty nautical miles in length. At its mid-point, the line joining Alice Point to Cape Santa Maria di Leuca is approximately sixty-three nautical miles from the innermost low-water line of the Gulf of Taranto coast. The Gulf of Taranto is a juridical bay because it meets the semi circular test set up by Article 7(2) of the 1958 Geneva Convention on the Territorial Sea and the Contiguous Zone. 1 Indeed, the waters embodied by the Gulf cover an area larger than that of the semi circle whose diameter is the line Alice Point-Cape Santa Maria di Leuca (the line joining the mouth of the Gulf). On April 26, 1977, Italy enacted a Decree causing straight baselines to be drawn along the coastline of the Italian Peninsula.2 A straight baseline, about sixty nautical miles long, was drawn along the entrance of the Gulf of Taranto between Cape Santa Maria di Leuca and Alice Point. The 1977 Decree justified the drawing of such a line by proclaiming the Gulf of Taranto an historic bay.3 The Decree, however, did not specify the grounds upon which the Gulf of Taranto was declared an historic bay. -
Wave Energy in the Balearic Sea. Evolution from a 29 Year Spectral Wave Hindcast
1 Wave energy in the Balearic Sea. Evolution from a 29 2 year spectral wave hindcast a b,∗ c 3 S. Ponce de Le´on , A. Orfila , G. Simarro a 4 UCD School of Mathematical Sciences. Dublin 4, Ireland b 5 IMEDEA (CSIC-UIB). 07190 Esporles, Spain. c 6 Institut de Ci´enciesdel Mar (CSIC). 08003 Barcelona, Spain. 7 Abstract 8 This work studies the wave energy availability in the Western Mediterranean 9 Sea using wave simulation from January 1983 to December 2011. The model 10 implemented is the WAM, forced by the ECMWF ERA-Interim wind fields. 11 The Advanced Scatterometer (ASCAT) data from MetOp satellite and the 12 TOPEX-Poseidon altimetry data are used to assess the quality of the wind 13 fields and WAM results respectively. Results from the hindcast are the 14 starting point to analyse the potentiality of obtaining wave energy around 15 the Balearic Islands Archipelago. The comparison of the 29 year hindcast 16 against wave buoys located in Western, Central and Eastern basins shows a 17 high correlation between the hindcasted and the measured significant wave 18 height (Hs), indicating a proper representation of spatial and temporal vari- 19 ability of Hs. It is found that the energy flux at the Balearic coasts range 20 from 9:1 kW=m, in the north of Menorca Island, to 2:5 kW=m in the vicinity 21 of the Bay of Palma. The energy flux is around 5 and 6 times lower in 22 summer as compared to winter. 23 Keywords: Mediterranean Sea, WAM model, wave energy, wave climate 24 variability, ASCAT, TOPEX-Poseidon ∗Corresponding author PreprintEmail submitted address: [email protected] Elsevier(A. -
THE MARINE PROTECTED AREAS of the BALEARIC SEA Marilles Foundation
THE MARINE PROTECTED AREAS OF THE BALEARIC SEA Marilles Foundation THE MARINE PROTECTED AREAS OF THE BALEARIC SEA A brief introduction What are marine protected areas? Marine Protected Areas (MPAs) are portions of the marine The level of protection of the Balearic Islands’ MPAs varies environment, sometimes connected to the coast, under depending on the legal status and the corresponding some form of legal protection. MPAs are used globally as administrations. In the Balearic Islands we find MPAs in tools for the regeneration of marine ecosystems, with the inland waters that are the responsibility of the Balearic dual objective of increasing the productivity of fisheries Islands government and island governments (Consells), and resources and conserving marine habitats and species. in external waters that depend on the Spanish government. Inland waters are those that remain within the polygon We define MPAs as those where industrial or semi-indus- marked by the drawing of straight lines between the capes trial fisheries (trawling, purse seining and surface longlining) of each island. External waters are those outside. are prohibited or severely regulated, and where artisanal and recreational fisheries are subject to regulation. Figure 1. Map of the Balearic Islands showing the location of the marine protection designations. In this study we consider all of them as marine protected areas except for the Natura 2000 Network and Biosphere Reserve areas. Note: the geographical areas of some protection designations overlap. THE MARINE PROTECTED AREAS OF THE BALEARIC SEA Marilles Foundation Table 1. Description of the different marine protected areas of the Balearic Islands and their fishing restrictions. -
SESSION I : Geographical Names and Sea Names
The 14th International Seminar on Sea Names Geography, Sea Names, and Undersea Feature Names Types of the International Standardization of Sea Names: Some Clues for the Name East Sea* Sungjae Choo (Associate Professor, Department of Geography, Kyung-Hee University Seoul 130-701, KOREA E-mail: [email protected]) Abstract : This study aims to categorize and analyze internationally standardized sea names based on their origins. Especially noting the cases of sea names using country names and dual naming of seas, it draws some implications for complementing logics for the name East Sea. Of the 110 names for 98 bodies of water listed in the book titled Limits of Oceans and Seas, the most prevalent cases are named after adjacent geographical features; followed by commemorative names after persons, directions, and characteristics of seas. These international practices of naming seas are contrary to Japan's argument for the principle of using the name of archipelago or peninsula. There are several cases of using a single name of country in naming a sea bordering more than two countries, with no serious disputes. This implies that a specific focus should be given to peculiar situation that the name East Sea contains, rather than the negative side of using single country name. In order to strengthen the logic for justifying dual naming, it is suggested, an appropriate reference should be made to the three newly adopted cases of dual names, in the respects of the history of the surrounding region and the names, people's perception, power structure of the relevant countries, and the process of the standardization of dual names. -
Zooplankton Communities Fluctuations from 1995 to 2005 in the Bay of Villefranche-Sur-Mer (Northern Ligurian Sea, France)
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Biogeosciences Discuss., 7, 9175–9207, 2010 Biogeosciences www.biogeosciences-discuss.net/7/9175/2010/ Discussions doi:10.5194/bgd-7-9175-2010 © Author(s) 2010. CC Attribution 3.0 License. This discussion paper is/has been under review for the journal Biogeosciences (BG). Please refer to the corresponding final paper in BG if available. Zooplankton communities fluctuations from 1995 to 2005 in the Bay of Villefranche-sur-Mer (Northern Ligurian Sea, France) P. Vandromme1,2, L. Stemmann1,2, L. Berline1,2, S. Gasparini1,2, L. Mousseau1,2, F. Prejger1,2, O. Passafiume1,2, J.-M. Guarini3,4, and G. Gorsky1,2 1UPMC Univ. Paris 06, UMR 7093, LOV, Observatoire oceanologique,´ 06234, Villefranche/mer, France 2CNRS, UMR 7093, LOV, Observatoire oceanologique,´ 06234, Villefranche/mer, France 3UPMC Univ. Paris 06, Oceanographie,´ Environnements Marins, 4 Place Jussieu, 75005 Paris 4CNRS, INstitute Environment Ecology, INEE, 3 Rue Michel-Ange, 75016 Paris 9175 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Received: 8 November 2010 – Accepted: 18 November 2010 – Published: 15 December 2010 Correspondence to: L. Stemmann ([email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. 9176 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract An integrated analysis of the pelagic ecosystems of the Ligurian Sea is performed com- bining time series of different zooplankton groups (small and large copepods, chaetog- naths, appendicularians, pteropods, thaliaceans, decapods larvae, other crustaceans, 5 other gelatinous and other zooplankton), chlorophyll-a and nutrients, seawater salinity, temperature and density and local weather at the Point B coastal station (Northern Lig- urian Sea). -
Stock Assessment Form Demersal Species Reference Year: 2012 Reporting Year: 2013
Stock Assessment Form Demersal species Reference year: 2012 Reporting year: 2013 P. longirostris represents one of the most important resources of the demersal assemblage in the Ionian sea where it is distributed between 100 and 500 m depth and targeted mainly by trawlers. A first stock assessment of this species in the area has been performed in 2013, during the EWG 13- 09, using different sources of data (fishery dependent and fishery independent). Given the results from this analysis, the stock is in overfishing and it is necessary to consider a reduction of the fishing mortality. Here the evaluation is expanded to an exercise using the ALADYM simulation model to explore effects of possible different management scenarios. Stock Assessment Form version 1.0 (January 2014) Uploader: Isabella Bitetto Stock assessment form 1 Basic Identification Data .............................................................................................................. 3 2 Stock identification and biological information ........................................................................... 5 2.1 Growth and maturity ............................................................................................................. 5 3 Fisheries information ................................................................................................................... 9 3.1 Description of the fleet .......................................................................................................... 9 3.2 Historical trends ................................................................................................................. -
SEISMIC REFRACTION MEASUREMENTS in the WESTERN MEDITERRANEAN SEA by DAVIS ARMSTRONG FAHLQUIST BS, Brown University
0 ~I~i7 SEISMIC REFRACTION MEASUREMENTS IN THE WESTERN MEDITERRANEAN SEA by DAVIS ARMSTRONG FAHLQUIST B. S., Brown University (1950) SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY June, 1963 Signature of Author Department of Geoogy and Geophysics Certified by 2%Kes~i Supervisor Accepted by Chairman, Departmental Committee on Graduate Students 2 38 ABSTRACT SEISMIC REFRACTION MEASUREMENTS IN THE WESTERN MEDITERRANEAN SEA by Davis Armstrong Fahlquist Submitted to the Department of Geology and Geophysics on 4 February, 1963, in partial fulfillment of requirements for the degree of Doctor of Philosophy. Results of seismic refraction studies conducted from the research vessels ATLANTIS and CHAIN (Woods Hole Oceanographic Institution), WINNARETTA SINGER (Musee Oceanographique de Monaco), and VEMA (Lamont Geological Observatory) are presented. Depths to the Mohorovicic discontinuity vary from 11 to 14 km. at four refraction stations located in the deep water area bounded by the Balearic Islands, Corsica, and southern France; the mantle veloci- ties measured at these stations vary from 7. 7 to 8. 0 km/sec. Over- lying the high velocity material at three of these stations is a layer of material having a velocity of 6. 5 to 6. 8 km/sec and varying in thickness from 2 to 3 km. A significantly lower velocity, 6. 0 km/ sec, was measured for the layer directly overlying the mantle on the profile extending from near Cape Antibes to Corsica. All profiles in the northern part of the western Mediterranean Basin show the pres- ence of a 4 to 6 km. -
17Th World Championships
_______________________________________________________________________________________ 26th Shore Angling Clubs World Championship from 19th to 26th May in Catanzaro (Italy) 26th Shore Angling Clubs World Championship 19 – 26 May 2018 - Catanzaro (Italy) Welcome, dear angler friends I am delighted to express on my name and on behalf of the Italian Sport Fishing and Underwater Activities Federation (FIPSAS),the best greetings to all participants at this World Championship that this year is going to take place from May the 19th until 26th 2018, in a charming area of Calabria Region, along the Catanzaro coast. I am sure that all attending athletes, who will join Catanzaro as well as all managers, judges and stewards will find a way to explore and appreciate our beauties and taste Calabria people’s hospitality and of all those who have made all efforts for the organization of this sport fishing important event. I am particularly delighted to express my warmest welcoming to all in the aim to live together some happy days in the name of sport. A special “good luck” to all Judges convened to manage this race, in the certainty of their professional and fair commitment they have also expressed in precedent occasions. Finally, I wish to thank the hosting Organizers, the local authorities and all journalists for their support and contribution for this event’s good success. The FIPSAS President 2 Welcome, dear angling friends. Both personally and on behalf of FIPSAS Surface Fishing Division — which I am honoured to chair — I am pleased to extend my warmest and heartfelt welcome to all the participants in the 26th World Club Long Casting Championship scheduled to take place along the magnificent coast of the Ionian sea in the province of Catanzaro from 19 to 26 May 2018.