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Checklist of Fish and Invertebrates Listed in the CITES Appendices
JOINTS NATURE \=^ CONSERVATION COMMITTEE Checklist of fish and mvertebrates Usted in the CITES appendices JNCC REPORT (SSN0963-«OStl JOINT NATURE CONSERVATION COMMITTEE Report distribution Report Number: No. 238 Contract Number/JNCC project number: F7 1-12-332 Date received: 9 June 1995 Report tide: Checklist of fish and invertebrates listed in the CITES appendices Contract tide: Revised Checklists of CITES species database Contractor: World Conservation Monitoring Centre 219 Huntingdon Road, Cambridge, CB3 ODL Comments: A further fish and invertebrate edition in the Checklist series begun by NCC in 1979, revised and brought up to date with current CITES listings Restrictions: Distribution: JNCC report collection 2 copies Nature Conservancy Council for England, HQ, Library 1 copy Scottish Natural Heritage, HQ, Library 1 copy Countryside Council for Wales, HQ, Library 1 copy A T Smail, Copyright Libraries Agent, 100 Euston Road, London, NWl 2HQ 5 copies British Library, Legal Deposit Office, Boston Spa, Wetherby, West Yorkshire, LS23 7BQ 1 copy Chadwick-Healey Ltd, Cambridge Place, Cambridge, CB2 INR 1 copy BIOSIS UK, Garforth House, 54 Michlegate, York, YOl ILF 1 copy CITES Management and Scientific Authorities of EC Member States total 30 copies CITES Authorities, UK Dependencies total 13 copies CITES Secretariat 5 copies CITES Animals Committee chairman 1 copy European Commission DG Xl/D/2 1 copy World Conservation Monitoring Centre 20 copies TRAFFIC International 5 copies Animal Quarantine Station, Heathrow 1 copy Department of the Environment (GWD) 5 copies Foreign & Commonwealth Office (ESED) 1 copy HM Customs & Excise 3 copies M Bradley Taylor (ACPO) 1 copy ^\(\\ Joint Nature Conservation Committee Report No. -
Updated Classification of Benthic Marine Habitat Types for The
Updated Classification of Benthic Marine Habitat Types for the Mediterranean Region TUNISIA - 2019 Legal notice: The designations employed and the presentation of the material in this document do not imply the expression of any opinion whatsoever on the part of the Specially Protected Areas Regional Activity Centre (SPA/RAC) and UN Environment/Mediterranean Action Plan (MAP) and those of the Lebanese Ministry of Environment concerning the legal status of any State, Territory, city or area, or of its authorities, or concerning the delimitation of their frontiers or boundaries. This publication was produced with the fi nancial support of the European Union in the framework of the MedMPA Network Project. Its contents are the sole responsibility of SPA/RAC and do not necessarily refl ect the views of the European Union. Copyright : All property rights of texts and content of different types of this publication belong to SPA/RAC. Reproduction of these texts and contents, in whole or in part, and in any form, is prohibited without prior written permission from SPA/RAC, except for educational and other non-commercial purposes, provided that the source is fully acknowledged. © 2019 - United Nations Environment Programme Mediterranean Action Plan Specially Protected Areas Regional Activity Centre (SPA/RAC) Boulevard du Leader Yasser Arafat B.P. 337 1080 Tunis Cedex - Tunisia. [email protected] For bibliographic purposes, this document may be cited as: SPA/RAC–UN Environment/MAP, 2019: Updated Classifi cation of Benthic Marine Habitat Types for the Mediterranean Region Layout : Atef OUERGHI Cover photos credit: © SPA/RAC, University of Seville, University of Alicante, Trainito E. -
Structure of Mediterranean 'Cnidarian Populations In
Homage to Ramon Marga/et,· or, Why there is such p/easure in studying nature 243 (J. D. Ros & N. Prat, eds.). 1991 . Oec% gia aquatica, 10: 243-254 STRUCTURE OF 'CNIDARIAN POPULATIONS IN MEDITERRANEAN SUBLITTORAL BENTHIC COMMUNITIES AS A RESUL T OF ADAPTATION TO DIFFERENT ENVIRONMENTAL CONDITIONS 2 JOSEP-MARIA GILIl & ENRIe BALLESTEROs .• 1 Insti t de Ciencies del Mar (CSIC). Passeig Nacional, s/n. 08039 Barcelona. Spain 2 � Centre d'Estudis Avanc;:atsde Blanes (CSIC). Camí de Santa Barbara, s/n. 17300 Blanes. Spain Received: March 1990 SUMMARY The presence and abundance of Cnidarians, extremely cornmon in Mediterranean sublittoral benthic communities, exerts a profound effect on the entire structure of such communities, although the roles of Anthozoans and Hydrozoans differ in accordance with their different biological characteristics. Structural differences in benthic cnidarian populations were observed in three sublittoral cornmunities located within 100 m of each other yet differing considerably in light intensity and water movement. Species-area and Shannon's diversity-area curves were computed for each community from reticulate samples constituted by 18 subsamples 2 of 289 cm . Species-area curves were fitted to semilogarithmic functions, while diversity-area curves were fitted to Michaelis-Menten functions by the method of least squares. Species richness, species distribution, alpha-diversity, and pattem diversity were estimated from the fitted curves. Patch size for Anthozoans was smaller than that for Hydrozoans in all three communities. Diversity was greatest in the cornmunities with the lowest and with the highest light intensity and water flow levels, but species richness was highest in the intermediate community. -
First Massive Mucilage Event Observed in Deep Waters of Çanakkale Strait (Dardanelles), Turkey
J. Black Sea/Mediterranean Environment Vol. 27, No. 1: 49-66 (2021) RESEARCH ARTICLE First massive mucilage event observed in deep waters of Çanakkale Strait (Dardanelles), Turkey H. Barış Özalp ORCID ID: 0000-0003-2640-8912 Vocational School of Ocean Engineering, Çanakkale Onsekiz Mart University, Çanakkale, TURKEY Faculty of Marine Sciences and Technology, Çanakkale Onsekiz Mart University, Çanakkale, TURKEY Corresponding author: [email protected] Abstract During the regular surveys on coral monitoring for setting their developmental level, health status and likely threats responsible for mortality, a massive mucilage phenomenon was identified in the largest coral habitats in the Çanakkale Strait (Dardanelles) in December 2020. This study was performed to determine the effect of mucilage event on corals mainly observed at the depth level of 39-51 m in two stations, one in the European and the other in the Anatolian side of the strait. A massive mucilage with expanding cloud and floc types of aggregates was detected only in the Eceabat region (European side). A false-benthos mucilage was also identified at depths 4-20 m in the following control surveys. The current report is of the first circalittoral observation of this damaging event in the northernmost region of the Mediterranean Sea. Previous records of massive mucilage were reviewed and the first deep infralittoral record of massive mucilage event in 2008 is also described. Keywords: Mucilage, zoobenthos, coral, ecology, Turkish Straits System Received: 05.03.2021, Accepted: 05.04.2021 Introduction Mucilage, also known as marine snow, aggregated mass, foam accumulation, formation of flocs, cloud or mucilaginous and mucous agglomeration (Suzuki and Kato 1953; Riley 1963; Lancelot 1995; Rinaldi et al. -
Corales De Las Islas Canarias
ETSI MINAS (UNIVERSIDAD POLITÉCNICA DE MADRID) CORALES DE LAS ISLAS CANARIAS FICHERO Ignacio Alonso Provencio Lorena Blanco Muñoz Marzo de 2013, Prácticas en los laboratorio del IGME 1 CONOCIMIENTOS PREVIOS SOBRE LOS CORALES: ANATOMÍA Los corales marinos son animales coloniales, salvo excepciones, pertenecientes al filo Cnidaria, clase Anthozoa. Las colonias están formadas por hasta miles de individuos zooides y pueden alcanzar grandes dimensiones. Las distintas especies de invertebrados con los que vamos a tratar perteneces al grupo de los antozoos, es decir, cnidarios que sólo tienen una fase pólipo (carecen de fase medusa) y poseen una cavidad gástrica dividida en compartimentos. El término "coral marino" suele usarse para designar a los antozoos; los corales se dividen en blandos y duros (en función del exoesqueleto que presenten), según tengan esqueleto o no: - DUROS: antozoos que generan un esqueleto calcáreo duro, especialmente si construyen colonias ramificadas. También son comunes las especies que forman colonias compactas incluso con un esqueleto córneo y flexible. - BLANDOS: son antozoos pertenecientes a las especies del orden Alcyonacea, que no generan esqueleto y utilizan el calcio en forma de espículas (unidades esqueléticas calcáreas o silíceas que forman parte del esqueleto de los poríferos) repartidas por su tejido carnoso, para proporcionarles mayor rigidez y consistencia. La perspectiva embriológica de los cnidarios es uno de los aspectos más importantes; normalmente el zigoto da lugar a una blástula con un espacio interior o bien, da lugar a una blástula maciza. Los antozoos, poseen tres capas de tejidos plenamente desarrollados: - ECTODERMO: capa celular primaria más externa del embrión. Da lugar al sistema nervioso, órganos especiales de los sentidos, la epidermis y derivados epidérmicos. -
Coralligenous Assemblages Along Their
Coralligenous assemblages along their geographical distribution: Testing of concepts and implications for management Melih Ertan Çinar, Jean-Pierre Féral, Christos Arvanitidis, Romain David, Ergün Taşkin, Maria Sini, Thanos Dailianis, Alper Doğan, Vasilis Gerovasileiou, Alper Evcen, et al. To cite this version: Melih Ertan Çinar, Jean-Pierre Féral, Christos Arvanitidis, Romain David, Ergün Taşkin, et al.. Coralligenous assemblages along their geographical distribution: Testing of concepts and implications for management. Aquatic Conservation: Marine and Freshwater Ecosystems, Wiley, 2020, 30, pp.1578 - 1594. 10.1002/aqc.3365. hal-02892573 HAL Id: hal-02892573 https://hal.archives-ouvertes.fr/hal-02892573 Submitted on 11 Jan 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. Aquatic Conservation, Marine and Freshwater Ecosystems (2020) 30: 1578-1594, DOI: 10.1002/aqc.3365 Coralligenous assemblages along their geographical distribution: Testing of concepts and implications for management Melih Ertan Çinar1 | Jean-Pierre Féral2 | Christos Arvanitidis3 -
(Adriatic Sea, Croatia). 1
NAT. CROAT. VOL. 11 No 3 265¿292 ZAGREB September 30, 2002 ISSN 1330-0520 original scientific paper / izvorni znanstveni rad UDK 591.9:593.6(497.5/(262.3)(1–13) MARINE FAUNA OF THE MLJET NATIONAL PARK (ADRIATIC SEA, CROATIA). 1. ANTHOZOA PETAR KRU@I] Faculty of Science, Department of Zoology, Rooseveltov trg 6, 10000 Zagreb, Croatia ([email protected]) Thais – Society for Exploration and Conservation of Nature, Primorska 23, 10000 Zagreb, Croatia Kru`i}, P.: Marine fauna of the Mljet National Park (Adriatic Sea, Croatia). 1. Anthozoa. Nat. Croat., Vol. 11, No. 3., 265–292, 2002, Zagreb. Fifty-two anthozoan species were recorded and collected in the area of Mljet National Park dur- ing surveys from 1995 to 1998. General and ecological data are presented for each species, as well as distribution and local abundance. Recorded species account for about 60% of anthozoans known in the Adriatic Sea, and for about 45% of anthozoans known in the Mediterranean Sea. Eight of these species were not recorded previously in the Adriatic Sea. Eleven species are considered to be Mediterranean endemics. The heterogeneity of substrates and benthic communities is considerable in the Mljet National Park, with anthozoans present on most different kinds of substrates and in a wide range of benthic communities. Remarkably, the colonial coral Cladocora caespitosa builds a large »reef-like« structure in the Veliko Jezero, in the area characterized by strong bottom hydro- dynamism. Key words: marine fauna, Anthozoa, Mljet, Adriatic Sea Kru`i}, P.: Morska fauna Nacionalnog parka Mljet (Jadransko more, Hrvatska). 1. -
Evolutionary Trends in the Epithecate Scleractinian Corals
Evolutionary trends in the epithecate scleractinian corals EWA RONIEWICZ and JAROSEAW STOLARSKI Roniewicz, E. & Stolarski, J. 1999. Evolutionary trends in the epithecate scleractinian corals. -Acta Palaeontologica Polonica 44,2, 131-166. Adult stages of wall ontogeny of fossil and Recent scleractinians show that epitheca was the prevailing type of wall in Triassic and Jurassic corals. Since the Late Cretaceous the fre- quency of epithecal walls during adult stages has decreased. In the ontogeny of Recent epithecate corals, epitheca either persists from the protocorallite to the adult stage, or is re- placed in post-initial stages by trabecular walls that are often accompanied by extra- -calicular skeletal elements. The former condition means that the polyp initially lacks the edge zone, the latter condition means that the edge zone develops later in coral ontogeny. Five principal patterns in wall ontogeny of fossil and Recent Scleractinia are distinguished and provide the framework for discrimination of the four main stages (grades) of evolu- tionary development of the edge-zone. The trend of increasing the edge-zone and reduction of the epitheca is particularly well represented in the history of caryophylliine corals. We suggest that development of the edge-zone is an evolutionary response to changing envi- ronment, mainly to increasing bioerosion in the Mesozoic shallow-water environments. A glossary is given of microstructural and skeletal terms used in this paper. Key words : Scleractinia, microstructure, thecal structures, epitheca, phylogeny. Ewa Roniewicz [[email protected]]and Jarostaw Stolarski [[email protected]], Instytut Paleobiologii PAN, ul. Twarda 51/55, PL-00-818 Warszawa, Poland. In Memory of Gabriel A. -
A Mediterranean Mesophotic Coral Reef Built by Non-Symbiotic
www.nature.com/scientificreports OPEN A Mediterranean mesophotic coral reef built by non-symbiotic scleractinians Received: 30 July 2018 Giuseppe Corriero1,2, Cataldo Pierri1,3, Maria Mercurio1,2, Carlotta Nonnis Marzano1,2, Accepted: 8 February 2019 Senem Onen Tarantini1, Maria Flavia Gravina4,2, Stefania Lisco5,2, Massimo Moretti5,2, Published: xx xx xxxx Francesco De Giosa6, Eliana Valenzano5, Adriana Giangrande2,7, Maria Mastrodonato1, Caterina Longo 1,2 & Frine Cardone 1,2 This is the frst description of a Mediterranean mesophotic coral reef. The bioconstruction extended for 2.5 km along the Italian Adriatic coast in the bathymetric range −30/−55 m. It appeared as a framework of coral blocks mostly built by two scleractinians, Phyllangia americana mouchezii (Lacaze- Duthiers, 1897) and Polycyathus muellerae (Abel, 1959), which were able to edify a secondary substrate with high structural complexity. Scleractinian corallites were cemented by calcifed polychaete tubes and organized into an interlocking meshwork that provided the reef stifness. Aggregates of several individuals of the bivalve Neopycnodonte cochlear (Poli, 1795) contributed to the compactness of the structure. The species composition of the benthic community showed a marked similarity with those described for Mediterranean coralligenous communities and it appeared to be dominated by invertebrates, while calcareous algae, which are usually considered the main coralligenous reef- builders, were poorly represented. Overall, the studied reef can be considered a unique environment, to be included in the wide and diversifed category of Mediterranean bioconstructions. The main reef- building scleractinians lacked algal symbionts, suggesting that heterotrophy had a major role in the metabolic processes that supported the production of calcium carbonate. -
Guidelines for Inventorying and Monitoring of Dark Habitats
UNITED NATIONS UNEP(DEPI)/MED WG. 431/Inf.12 UNITED NATIONS ENVIRONMENT PROGRAMME MEDITERRANEAN ACTION PLAN 31 March 2017 English Original: English Thirteenth Meeting of Focal Points for Specially Protected Areas Alexandria, Egypt, 9-12 May 2017 Agenda Item 4 : Progress report on activities carried out by SPA/RAC since the twelfth meeting of Focal Points for SPAs Draft Guidelines for Inventoring and Monitoring of Dark Habitats For environmental and economy reasons, this document is printed in a limited number and will not be distributed at the meeting. Delegates are kindly requested to bring their copies to meetings and not to request additional copies. UN Environment/MAP SPA/RAC - Tunis, 2017 Note: The designations employed and the presentation of the material in this document do not imply the expression of any opinion whatsoever on the part of Specially Protected Areas Regional Activity Centre (SPA/RAC) and UN Environment concerning the legal status of any State, Territory, city or area, or of its authorities, or concerning the delimitation of their frontiers or boundaries. © 2017 United Nations Environment Programme / Mediterranean Action Plan (UN Environment /MAP) Specially Protected Areas Regional Activity Centre (SPA/RAC) Boulevard du Leader Yasser Arafat B.P. 337 - 1080 Tunis Cedex - Tunisia E-mail: [email protected] The original version of this document was prepared for the Specially Protected Areas Regional Activity Centre (SPA/RAC) by Ricardo Aguilar & Pilar Marín, OCEANA and Vasilis Gerovasileiou, SPA/RAC Consultant with contribution from Tatjana Bakran- Petricioli, Enric Ballesteros, Hocein Bazairi, Carlo Nike Bianchi, Simona Bussotti, Simonepietro Canese, Pierre Chevaldonné, Douglas Evans, Maïa Fourt, Jordi Grinyó, Jean- Georges Harmelin, Alain Jeudy de Grissac, Vesna Mačić, Covadonga Orejas, Maria del Mar Otero, Gérard Pergent, Donat Petricioli, Alfonso A. -
Handbook for Interpreting Types of Marine Habitat for The
SUMMARY INTRODUCTION 09 Background 09 Some reminders about marine ecology 10 List of Mediterranean benthic biocenoses 10 Bibliographical references 11 I - SUPRALITTORAL STAGE I.2. SANDS I.2.1. Biocenosis of supralittoral sands 12 I.2.1.5. Facies with washed-up phanerogams (upper part) 14 II - MEDIOLITTORAL STAGE II.1. MUDS, SANDY MUDS AND SANDS OF LAGOONSAND ESTUARIES II.1.1. Biocenosis of muddy sands and muds 16 II.1.1.1. Association with halophytes 18 II.1.1.2. Facies of saltworks 20 II.3. STONES AND PEBBLES II.3.1. Biocenosis of mediolittoral detritic bottoms 22 II.3.1.1. Facies with banks of dead leaves of Posidonia oceanica and other phanerogams 24 II.4. HARD BEDS AND ROCKS II.4. 1. Biocenosis of the upper mediolittoral rock 26 II.4.1.3. Association with Nemalion helminthoides and Rissoella verruculosa 28 II.4.1.4. Association with Lithophyllum papillosum and Polysiphonia spp 30 II.4.2. Biocenosis of the lower mediolittoral rock 32 II.4.2.1. Association with Lithophyllum lichenoides (=L. tortuosum rim) 34 II.4.2.5. Facies with Pollicipes cornucopiae 36 II.4.2.7. The association with Fucus virsoides 38 II.4.2.8. Neogoniolithon brassica-forida concretion 40 II.4.2.10. Pools and lagoons sometimes associated with Vermetids (infralittoral enclave) See sheet III.6.1.3. Facies with Vermetids 90 I.4.3. Mediolittoral caves 42 II.4.3.1. Association with Phymatolithon lenormadii and Hildenbrandia rubra 44 III - INFRALITTORAL III.1. SANDY MUDS, SANDS, GRAVELS AND ROCKS IN EURYHALINE AND EURYTHERMAL ENVIRONMENT III.1.1. -
Chapter 4. Deep-Sea Coral Genetics Morrison Et Al. 4 - 1
Chapter 4. Deep-sea Coral Genetics Morrison et al. 4 - 1 MOLECULAR ASSESSMENT OF DEEP-SEA SCLERACTINIAN CORAL BIODIVERSITY AND POPULATION STRUCTURE OF LOPHELIA PERTUSA IN THE GULF OF MEXICO Cheryl L. Morrison, Robin L. Johnson, Tim L. King, Steve W. Ross, and Martha S. Nizinski Key Words: Deep-sea coral, scleractinian biodiversity, mitochondrial 16S, phylogeny, ‘robust’ corals, ‘complex’ corals, Lophelia, microsatellites, population structure, dispersal, gene flow ABSTRACT Geographic patterns of genetic diversity in Lophelia pertusa were examined by quantifying genetic diversity present in populations, and assessing levels of genetic differentiation within the Gulf of Mexico (GOM, 5 sampling locations, <1-290 km apart). Patterns of differentiation observed within GOM Lophelia were compared to Lophelia populations from the Atlantic Ocean continental slope off the Southeastern U.S. (SEUS, 6 sampling locations, 18-990 km apart) and with northeast Atlantic Ocean (NEAO) populations off the coast of Europe (5,400-7,900 km away from sampled U.S. populations). Multilocus genotypes for 190 Lophelia individuals were determined using a suite of nine microsatellite markers developed for GOM Lophelia. Eighteen individuals (9%) with identical multi-locus genotypes were identified as clones. Populations of Lophelia harbored substantial genetic diversity. The majority of populations had unique alleles indicative of little gene flow. Pairwise chord distances were high among all populations and regional groupings of populations resulted from a neighbor-joining clustering analysis. North versus south areas of Viosca Knoll (VK) 826, the most intensively sampled area, had fixation index estimates significantly greater than zero, suggesting little larval mixing. Comparisons of all GOM Lophelia populations with the shallowest site, VK862, produced significant fixation indices.