Biodiversity of Biogenic Habitats
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Order BERYCIFORMES ANOPLOGASTRIDAE Fangtooths (Ogrefish) by J.A
click for previous page 1178 Bony Fishes Order BERYCIFORMES ANOPLOGASTRIDAE Fangtooths (ogrefish) by J.A. Moore, Florida Atlantic University, USA iagnostic characters: Small (to about 160 mm standard length) beryciform fishes.Body short, deep, and Dcompressed, tapering to narrow peduncle. Head large (1/3 standard length). Eye smaller than snout length in adults, but larger than snout length in juveniles. Mouth very large and oblique, jaws extend be- hind eye in adults; 1 supramaxilla. Bands of villiform teeth in juveniles are replaced with large fangs on dentary and premaxilla in adults; vomer and palatines toothless. Deep sensory canals separated by ser- rated ridges; very large parietal and preopercular spines in juveniles of one species, all disappearing with age. Gill rakers as clusters of teeth on gill arch in adults (lath-like in juveniles). No true fin spines; single, long-based dorsal fin with 16 to 20 rays; anal fin very short-based with 7 to 9 soft rays; caudal fin emarginate; pectoral fins with 13 to 16 soft rays; pelvic fins with 7 soft rays. Scales small, non-overlapping, spinose, goblet-shaped in adults; lateral line an open groove partially bridged by scales; no enlarged ventral keel scutes. Colour: entirely dark brown or black in adults. Habitat, biology, and fisheries: Meso- to bathypelagic, at depths of 75 to 5 000 m. Carnivores, with juveniles feeding on mainly crustaceans and adults mainly on fishes. May sometimes swim in small groups. Uncommon deep-sea fishes of no commercial importance. Remarks: The family was revised recently by Kotlyar (1986) and contains 1 genus with 2 species throughout the tropical and temperate latitudes. -
Jolanta KEMPTER*, Maciej KIEŁPIŃSKI, Remigiusz PANICZ, and Sławomir KESZKA
ACTA ICHTHYOLOGICA ET PISCATORIA (2016) 46 (4): 287–291 DOI: 10.3750/AIP2016.46.4.02 MICROSATELLITE DNA-BASED GENETIC TRACEABILITY OF TWO POPULATIONS OF SPLENDID ALFONSINO, BERYX SPLENDENS (ACTINOPTERYGII: BERYCIFORMES: BERYCIDAE)—PROJECT CELFISH—PART 2 Jolanta KEMPTER*, Maciej KIEŁPIŃSKI, Remigiusz PANICZ, and Sławomir KESZKA Division of Aquaculture, West Pomeranian University of Technology, Szczecin, Kazimierza Krolewicza 4, 71-550 Szczecin, Poland Kempter J., Kiełpinski M., Panicz R., Keszka S. 2016. Microsatellite DNA-based genetic traceability of two populations of splendid alfonsino, Beryx splendens (Actinopterygii: Beryciformes: Berycidae)— Project CELFISH—Part 2. Acta Ichthyol. Piscat. 46 (4): 287–291. Background. The study is a contribution to Project CELFISH which involves genetic identifi cation of populations of fi sh species presenting a particular economic importance or having a potential to be used in the so-called commercial substitutions. The EU fi sh trade has been showing a distinct trend of more and more fi sh species previously unknown to consumers being placed on the market. Molecular assays have become the only way with which to verify the reliability of exporters. This paper is aimed at pinpointing genetic markers with which to label and differentiate between two populations of splendid alfonsino, Beryx splendens Lowe, 1834, a species highly attractive to consumers in Asia and Oceania due to the meat taste and low fat content. Material and methods. DNA was isolated from fragments of fi ns collected at local markets in Japan (MJ) (n = 10) and New Zealand (MNZ) (n = 18). The rhodopsin gene (RH1) fragment and 16 microsatellite DNA fragments (SSR) were analysed in all the individuals. -
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. -
Taxonomic Checklist of CITES Listed Coral Species Part II
CoP16 Doc. 43.1 (Rev. 1) Annex 5.2 (English only / Únicamente en inglés / Seulement en anglais) Taxonomic Checklist of CITES listed Coral Species Part II CORAL SPECIES AND SYNONYMS CURRENTLY RECOGNIZED IN THE UNEP‐WCMC DATABASE 1. Scleractinia families Family Name Accepted Name Species Author Nomenclature Reference Synonyms ACROPORIDAE Acropora abrolhosensis Veron, 1985 Veron (2000) Madrepora crassa Milne Edwards & Haime, 1860; ACROPORIDAE Acropora abrotanoides (Lamarck, 1816) Veron (2000) Madrepora abrotanoides Lamarck, 1816; Acropora mangarevensis Vaughan, 1906 ACROPORIDAE Acropora aculeus (Dana, 1846) Veron (2000) Madrepora aculeus Dana, 1846 Madrepora acuminata Verrill, 1864; Madrepora diffusa ACROPORIDAE Acropora acuminata (Verrill, 1864) Veron (2000) Verrill, 1864; Acropora diffusa (Verrill, 1864); Madrepora nigra Brook, 1892 ACROPORIDAE Acropora akajimensis Veron, 1990 Veron (2000) Madrepora coronata Brook, 1892; Madrepora ACROPORIDAE Acropora anthocercis (Brook, 1893) Veron (2000) anthocercis Brook, 1893 ACROPORIDAE Acropora arabensis Hodgson & Carpenter, 1995 Veron (2000) Madrepora aspera Dana, 1846; Acropora cribripora (Dana, 1846); Madrepora cribripora Dana, 1846; Acropora manni (Quelch, 1886); Madrepora manni ACROPORIDAE Acropora aspera (Dana, 1846) Veron (2000) Quelch, 1886; Acropora hebes (Dana, 1846); Madrepora hebes Dana, 1846; Acropora yaeyamaensis Eguchi & Shirai, 1977 ACROPORIDAE Acropora austera (Dana, 1846) Veron (2000) Madrepora austera Dana, 1846 ACROPORIDAE Acropora awi Wallace & Wolstenholme, 1998 Veron (2000) ACROPORIDAE Acropora azurea Veron & Wallace, 1984 Veron (2000) ACROPORIDAE Acropora batunai Wallace, 1997 Veron (2000) ACROPORIDAE Acropora bifurcata Nemenzo, 1971 Veron (2000) ACROPORIDAE Acropora branchi Riegl, 1995 Veron (2000) Madrepora brueggemanni Brook, 1891; Isopora ACROPORIDAE Acropora brueggemanni (Brook, 1891) Veron (2000) brueggemanni (Brook, 1891) ACROPORIDAE Acropora bushyensis Veron & Wallace, 1984 Veron (2000) Acropora fasciculare Latypov, 1992 ACROPORIDAE Acropora cardenae Wells, 1985 Veron (2000) CoP16 Doc. -
Order BERYCIFORMES ANOPLOGASTRIDAE Anoplogaster
click for previous page 2210 Bony Fishes Order BERYCIFORMES ANOPLOGASTRIDAE Fangtooths by J.R. Paxton iagnostic characters: Small (to 16 cm) Dberyciform fishes, body short, deep, and compressed. Head large, steep; deep mu- cous cavities on top of head separated by serrated crests; very large temporal and pre- opercular spines and smaller orbital (frontal) spine in juveniles of one species, all disap- pearing with age. Eyes smaller than snout length in adults (but larger than snout length in juveniles). Mouth very large, jaws extending far behind eye in adults; one supramaxilla. Teeth as large fangs in pre- maxilla and dentary; vomer and palatine toothless. Gill rakers as gill teeth in adults (elongate, lath-like in juveniles). No fin spines; dorsal fin long based, roughly in middle of body, with 16 to 20 rays; anal fin short-based, far posterior, with 7 to 9 rays; pelvic fin abdominal in juveniles, becoming subthoracic with age, with 7 rays; pectoral fin with 13 to 16 rays. Scales small, non-overlap- ping, spinose, cup-shaped in adults; lateral line an open groove partly covered by scales. No light organs. Total vertebrae 25 to 28. Colour: brown-black in adults. Habitat, biology, and fisheries: Meso- and bathypelagic. Distinctive caulolepis juvenile stage, with greatly enlarged head spines in one species. Feeding mode as carnivores on crustaceans as juveniles and on fishes as adults. Rare deepsea fishes of no commercial importance. Remarks: One genus with 2 species throughout the world ocean in tropical and temperate latitudes. The family was revised by Kotlyar (1986). Similar families occurring in the area Diretmidae: No fangs, jaw teeth small, in bands; anal fin with 18 to 24 rays. -
How Much Longer Will It Take?
How much longer will it take? A ten-year review of the implementation of United Nations General Assembly resolutions 61/105, 64/72 and 66/68 on the management of bottom fisheries in areas beyond national jurisdiction FULL REPORT – AUGUST 2016 DAVID SHALE/NATURE PICTURE LIBRARAY SHALE/NATURE DAVID Leiopathes sp., a deepwater black coral, has lifespans in excess of 4,200 years (Roark et al., 2009*), making it one of the oldest living organism on Earth. Specimen was located off the coast of Oahu, Hawaii, in ~400 m water depth. * Roark, E.B., Guilderson, T.P., Dunbar, R.B., Fallon, S.J., and Mucciarone, D.A., 2009. Extreme longevity in proteinaceous deep-sea corals. Proceedings of the National Academy of Sciences, 106: 520– 5208, doi: 10.1073/pnas.0810875106. © HAWAII UNDERSEA RESEARCH LABORATORY, TERRY KERBY AND MAXIMILIAN CREMER Contents Executive summary 03 1.0 Introduction 09 2.0 North Atlantic 10 2.1 Northeast Atlantic 10 2..2 Northwest Atlantic 21 3.0 South Atlantic 33 3.1 Southeast Atlantic 33 3.2 Southwest Atlantic and other non-RFMO areas 39 4.0 North Pacific 42 Citation: 5.0 South Pacific 49 Gianni, M., Fuller, S.D., Currie, D.E.J., Schleit, 6.0 Indian Ocean 60 K., Goldsworthy, L., Pike, B., Weeber, B., 7.0 Southern Ocean 66 Owen, S., Friedman, A. How much longer will it take? A ten-year 8.0. Mediterranean Sea 71 review of the implementation of United Annex 1. Acronyms 73 Nations General Assembly resolutions Annex 2. History of the UNGA negotiations 73 61/105, 64/72 and 66/68 on the management Annex 3. -
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MARINE ECOLOGY PROGRESS SERIES Vol. 152: 227-239, 1997 Published June 26 Mar Ecol Prog Ser 1 Habitat specialisation and the distribution and abundance of coral-dwelling gobies Philip L. Munday*, Geoffrey P. Jones, M. Julian Caley Department of Marine Biology, James Cook University of North Queensland. Townsville, Queensland 4811, Australia ABSTRACT Many fishes on coral reefs are known to associate with particula~microhabitats If these associations help determine population dynamics then we would expect (1) a close assoclation between the abundances of these fishes and the abundances of the most frequently used mlcrohabitats and (2) changes in the abundance of microhabitats would result in a corresponding change In fish population sizes We examined habitat associations among obligate coral-dwelling gob~es(genus Goblodon) and then investigated relationships between the spatial and temporal ava~labilltyof habitats and the abundances of Goblodon species among locations and anlong zoncs on the leef at Lizard Island (Great Barrler Reef) Out of a total of 11 Acropora species found to be used by Gobiodon, each specic3s of Goblodon occupied 1 01 2 species of Acropora significantly more often than expected from the avail- ability of these corals on the reef Across reef zones, the abundance of most species of Gobiodon was closely correlated with the abundance of coral species most frequently inhabited However, the abun- dance of 1 species G ax~llar~s.iiras not conelated with the availability of most frequently used corals aci oss reef zones or among -
Composition and Ecology of Deep-Water Coral Associations D
HELGOLK---~DER MEERESUNTERSUCHUNGEN Helgoltinder Meeresunters. 36, 183-204 (1983) Composition and ecology of deep-water coral associations D. H. H. Kfihlmann Museum ffir Naturkunde, Humboldt-Universit~t Berlin; Invalidenstr. 43, DDR- 1040 Berlin, German Democratic Republic ABSTRACT: Between 1966 and 1978 SCUBA investigations were carried out in French Polynesia, the Red Sea, and the Caribbean, at depths down to 70 m. Although there are fewer coral species in the Caribbean, the abundance of Scleractinia in deep-water associations below 20 m almost equals that in the Indian and Pacific Oceans. The assemblages of corals living there are described and defined as deep-water coral associations. They are characterized by large, flattened growth forms. Only 6 to 7 % of the species occur exclusively below 20 m. More than 90 % of the corals recorded in deep waters also live in shallow regions. Depth-related illumination is not responsible for depth differentiations of coral associations, but very likely, a complex of mechanical factors, such as hydrodynamic conditions, substrate conditions, sedimentation etc. However, light intensity deter- mines the general distribution of hermatypic Scleractinia in their bathymetric range as well as the platelike shape of coral colonies characteristic for deep water associations. Depending on mechani- cal factors, Leptoseris, Montipora, Porites and Pachyseris dominate as characteristic genera in the Central Pacific Ocean, Podabacia, Leptoseris, Pachyseris and Coscinarea in the Red Sea, Agaricia and Leptoseris in the tropical western Atlantic Ocean. INTRODUCTION Considerable attention has been paid to shallow-water coral associations since the first half of this century (Duerden, 1902; Mayer, 1918; Umbgrove, 1939). Detailed investigations at depths down to 20 m became possible only through the use of autono- mous diving apparatus. -
Scleractinian Reef Corals: Identification Notes
SCLERACTINIAN REEF CORALS: IDENTIFICATION NOTES By JACKIE WOLSTENHOLME James Cook University AUGUST 2004 DOI: 10.13140/RG.2.2.24656.51205 http://dx.doi.org/10.13140/RG.2.2.24656.51205 Scleractinian Reef Corals: Identification Notes by Jackie Wolstenholme is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 3.0 Unported License. TABLE OF CONTENTS TABLE OF CONTENTS ........................................................................................................................................ i INTRODUCTION .................................................................................................................................................. 1 ABBREVIATIONS AND DEFINITIONS ............................................................................................................. 2 FAMILY ACROPORIDAE.................................................................................................................................... 3 Montipora ........................................................................................................................................................... 3 Massive/thick plates/encrusting & tuberculae/papillae ................................................................................... 3 Montipora monasteriata .............................................................................................................................. 3 Massive/thick plates/encrusting & papillae ................................................................................................... -
Pleistocene Reefs of the Egyptian Red Sea: Environmental Change and Community Persistence
Pleistocene reefs of the Egyptian Red Sea: environmental change and community persistence Lorraine R. Casazza School of Science and Engineering, Al Akhawayn University, Ifrane, Morocco ABSTRACT The fossil record of Red Sea fringing reefs provides an opportunity to study the history of coral-reef survival and recovery in the context of extreme environmental change. The Middle Pleistocene, the Late Pleistocene, and modern reefs represent three periods of reef growth separated by glacial low stands during which conditions became difficult for symbiotic reef fauna. Coral diversity and paleoenvironments of eight Middle and Late Pleistocene fossil terraces are described and characterized here. Pleistocene reef zones closely resemble reef zones of the modern Red Sea. All but one species identified from Middle and Late Pleistocene outcrops are also found on modern Red Sea reefs despite the possible extinction of most coral over two-thirds of the Red Sea basin during glacial low stands. Refugia in the Gulf of Aqaba and southern Red Sea may have allowed for the persistence of coral communities across glaciation events. Stability of coral communities across these extreme climate events indicates that even small populations of survivors can repopulate large areas given appropriate water conditions and time. Subjects Biodiversity, Biogeography, Ecology, Marine Biology, Paleontology Keywords Coral reefs, Egypt, Climate change, Fossil reefs, Scleractinia, Cenozoic, Western Indian Ocean Submitted 23 September 2016 INTRODUCTION Accepted 2 June 2017 Coral reefs worldwide are threatened by habitat degradation due to coastal development, 28 June 2017 Published pollution run-off from land, destructive fishing practices, and rising ocean temperature Corresponding author and acidification resulting from anthropogenic climate change (Wilkinson, 2008; Lorraine R. -
Volume 2. Animals
AC20 Doc. 8.5 Annex (English only/Seulement en anglais/Únicamente en inglés) REVIEW OF SIGNIFICANT TRADE ANALYSIS OF TRADE TRENDS WITH NOTES ON THE CONSERVATION STATUS OF SELECTED SPECIES Volume 2. Animals Prepared for the CITES Animals Committee, CITES Secretariat by the United Nations Environment Programme World Conservation Monitoring Centre JANUARY 2004 AC20 Doc. 8.5 – p. 3 Prepared and produced by: UNEP World Conservation Monitoring Centre, Cambridge, UK UNEP WORLD CONSERVATION MONITORING CENTRE (UNEP-WCMC) www.unep-wcmc.org The UNEP World Conservation Monitoring Centre is the biodiversity assessment and policy implementation arm of the United Nations Environment Programme, the world’s foremost intergovernmental environmental organisation. UNEP-WCMC aims to help decision-makers recognise the value of biodiversity to people everywhere, and to apply this knowledge to all that they do. The Centre’s challenge is to transform complex data into policy-relevant information, to build tools and systems for analysis and integration, and to support the needs of nations and the international community as they engage in joint programmes of action. UNEP-WCMC provides objective, scientifically rigorous products and services that include ecosystem assessments, support for implementation of environmental agreements, regional and global biodiversity information, research on threats and impacts, and development of future scenarios for the living world. Prepared for: The CITES Secretariat, Geneva A contribution to UNEP - The United Nations Environment Programme Printed by: UNEP World Conservation Monitoring Centre 219 Huntingdon Road, Cambridge CB3 0DL, UK © Copyright: UNEP World Conservation Monitoring Centre/CITES Secretariat The contents of this report do not necessarily reflect the views or policies of UNEP or contributory organisations. -
Holobiont Transcriptome of Colonial Scleractinian Coral Alveopora
Marine Genomics 43 (2019) 68–71 Contents lists available at ScienceDirect Marine Genomics journal homepage: www.elsevier.com/locate/margen Holobiont transcriptome of colonial scleractinian coral Alveopora japonica T ⁎ Taewoo Ryua, Wonil Choa, Seungshic Yumb,c, Seonock Wooc,d, a APEC Climate Center, Busan 48058, South Korea b South Sea Environment Research Center, Korea Institute of Ocean Science and Technology, Geoje 53201, South Korea c Faculty of Marine Environmental Science, University of Science and Technology (UST), Geoje 53201, South Korea d Marine Biotechnology Research Center, Korea Institute of Ocean Science and Technology, Busan 49111, South Korea ARTICLE INFO ABSTRACT Keywords: Climate change rapidly warms the ocean and marine species often move northwards for suitable habitats. Stony Alveopora japonica coral, Alveopora japonica, is observed more frequently for the last few years in temperate sea like Jeju Island, Coral South Korea. To understand the ecological consequences such as habitat formation and fate of this species in Holobiont changing environment, unraveling the genetic makeup of the species is essential. We sequenced the tran- Transcriptome scriptome of the A. japonica holobionts using Illumina HiSeq2000 platform. De novo assembly and analysis of Climate change coding regions predicted 108,636 coding sequences consisted of the coral host and residing Symbiodinium. Homology analysis showed the gene contents from our assembly are comparable to other sequenced corals and Symbiodiniums. The reference assembly of A. japonica will be a valuable resource to study the ecological characteristics of this species in the marine benthic ecosystem. 1. Introduction temperate region of Japan. The KC is experiencing a rapid increase in seawater temperature in response to global climate change and warmed The colonial stony coral Alveopora japonica is a zooxanthellate most rapidly from 1981 to 1998, when the surface temperatures rose by scleractinian coral in the family Acroporidae (WoRMS, n.d.).