Paulay Et Al 1999
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Papahānaumokuākea Marine National Monument Permit Application Cover Sheet
Papahānaumokuākea Marine National Monument Permit Application Cover Sheet This Permit Application Cover Sheet is intended to provide summary information and status to the public on permit applications for activities proposed to be conducted in the Papahānaumokuākea Marine National Monument. While a permit application has been received, it has not been fully reviewed nor approved by the Monument Management Board to date. The Monument permit process also ensures that all environmental reviews are conducted prior to the issuance of a Monument permit. Summary Information Applicant Name: Ruth D Gates Affiliation: Hawaii Institute of Marine Biology Permit Category: Research Proposed Activity Dates: May - Spetember 2010 Proposed Method of Entry (Vessel/Plane): Hi'ialakai NOAA RV Proposed Locations: French Frigate Shoals, Pearl & Hermes Estimated number of individuals (including Applicant) to be covered under this permit: 4 Estimated number of days in the Monument: 30 Description of proposed activities: (complete these sentences): a.) The proposed activity would… identify and monitor biological indicators of coral disease, bleaching, and impact to the reef and assess the diversity of coral-endosymbionts in Papahānaumokuākea. b.) To accomplish this activity we would …. sample coral colonies to determine the molecular diversity of coral endosymbionts. These activities will be performed using SCUBA from small boat operations launched from the Hi'ialakai NOAA vessel. c.) This activity would help the Monument by … identifying biological indicators of disease; revealing the diversity of coral-endoymbionts in Papahānaumokuākea; and determining the affect of global climate change on the coral reef ecosystem. Other information or background: The scleractinian corals provide the structural and biological framework that supports the high diversity of marine organisms that inhabit coral reef ecosystems. -
Microbiomes of Gall-Inducing Copepod Crustaceans from the Corals Stylophora Pistillata (Scleractinia) and Gorgonia Ventalina
www.nature.com/scientificreports OPEN Microbiomes of gall-inducing copepod crustaceans from the corals Stylophora pistillata Received: 26 February 2018 Accepted: 18 July 2018 (Scleractinia) and Gorgonia Published: xx xx xxxx ventalina (Alcyonacea) Pavel V. Shelyakin1,2, Sofya K. Garushyants1,3, Mikhail A. Nikitin4, Sofya V. Mudrova5, Michael Berumen 5, Arjen G. C. L. Speksnijder6, Bert W. Hoeksema6, Diego Fontaneto7, Mikhail S. Gelfand1,3,4,8 & Viatcheslav N. Ivanenko 6,9 Corals harbor complex and diverse microbial communities that strongly impact host ftness and resistance to diseases, but these microbes themselves can be infuenced by stresses, like those caused by the presence of macroscopic symbionts. In addition to directly infuencing the host, symbionts may transmit pathogenic microbial communities. We analyzed two coral gall-forming copepod systems by using 16S rRNA gene metagenomic sequencing: (1) the sea fan Gorgonia ventalina with copepods of the genus Sphaerippe from the Caribbean and (2) the scleractinian coral Stylophora pistillata with copepods of the genus Spaniomolgus from the Saudi Arabian part of the Red Sea. We show that bacterial communities in these two systems were substantially diferent with Actinobacteria, Alphaproteobacteria, and Betaproteobacteria more prevalent in samples from Gorgonia ventalina, and Gammaproteobacteria in Stylophora pistillata. In Stylophora pistillata, normal coral microbiomes were enriched with the common coral symbiont Endozoicomonas and some unclassifed bacteria, while copepod and gall-tissue microbiomes were highly enriched with the family ME2 (Oceanospirillales) or Rhodobacteraceae. In Gorgonia ventalina, no bacterial group had signifcantly diferent prevalence in the normal coral tissues, copepods, and injured tissues. The total microbiome composition of polyps injured by copepods was diferent. -
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. -
Coral Feeding on Microalgae Assessed with Molecular Trophic Markers
Molecular Ecology (2013) doi: 10.1111/mec.12486 Coral feeding on microalgae assessed with molecular trophic markers MIGUEL C. LEAL,*† CHRISTINE FERRIER-PAGES,‡ RICARDO CALADO,* MEGAN E. THOMPSON,† MARC E. FRISCHER† and JENS C. NEJSTGAARD† *Departamento de Biologia & CESAM, Universidade de Aveiro, Campus Universitario de Santiago, 3810-193 Aveiro, Portugal, †Skidaway Institute of Oceanography, 10 Ocean Science Circle, 31411 Savannah, GA, USA, ‡Centre Scientifique de Monaco, Avenue St-Martin, 98000 Monaco, Monaco Abstract Herbivory in corals, especially for symbiotic species, remains controversial. To investi- gate the capacity of scleractinian and soft corals to capture microalgae, we conducted controlled laboratory experiments offering five algal species: the cryptophyte Rhodo- monas marina, the haptophytes Isochrysis galbana and Phaeocystis globosa, and the diatoms Conticribra weissflogii and Thalassiosira pseudonana. Coral species included the symbiotic soft corals Heteroxenia fuscescens and Sinularia flexibilis, the asymbiotic scleractinian coral Tubastrea coccinea, and the symbiotic scleractinian corals Stylophora pistillata, Pavona cactus and Oculina arbuscula. Herbivory was assessed by end-point PCR amplification of algae-specific 18S rRNA gene fragments purified from coral tissue genomic DNA extracts. The ability to capture microalgae varied with coral and algal species and could not be explained by prey size or taxonomy. Herbivory was not detected in S. flexibilis and S. pistillata. P. globosa was the only algal prey that was never captured by any coral. Although predation defence mechanisms have been shown for Phaeocystis spp. against many potential predators, this study is the first to suggest this for corals. This study provides new insights into herbivory in symbiotic corals and suggests that corals may be selective herbivorous feeders. -
Acclimation of Symbiotic Reef-Building Corals to Extremely Low Light
Symbiosis, 33 (2002) 125-143 125 Balaban, Philadelphia/Rehovot Acclimation of Symbiotic Reef-Building Corals to Extremely Low Light E.A. TITLYANOVl,2*, T.V. TITLYANOVA2, and K. YAMAZATOl 1Tropical Biosphere Research Center, University of the Ryukyus, Sesoko Island, Okinawa 905, Japan; 2Jnstitute of Marine Biology, Far East Branch of Russian Academy of Sciences, Vladivostok 690041, Russia, Tel. +7-423-2310931, Fax. +7-423-2310900, Email. [email protected] Received March 13, 2002; Accepted August 2, 2002 Abstract This study investigated the photo-acclimation capacity of seven species of hermatypic corals subjected to 2%, 0.8% and 0.1% of incident surface photosynthetic active radiation (PARo) . Stylophora pistillata, Porites attenuata and Echinopora lamellosa photoacclimated to 2%, 0.8% and 0.1% PARO, Pocillopora damicornis only to 2% and 0.8% PARo, Seriatopora caliendrum, S. hystrix only to 2% PARo and the colonial hydroid Millepora intricata could not adapt to light intensity of 2% and lower. Physiological changes associated with photo• acclimation to extremely low light (i.e., 2%, 0.8% and 0.1% PARo) were a decline in zooxanthellae population densities, in zooxanthellae sizes, in cell division and degradation. Shade-intolerant species rapidly lost their zooxanthellae in extremely low light treatments and died, whereas shade-tolerant species maintained low zooxanthellae population densities in their tissue during 4 months and more. If the corals E. lamellosa and P. attenuata, acclimated to extremely low light, were transferred to dim light (30% PARo) , they regained their initial population densities within 90 days. We assume that specific distinction of corals under acclimation to extremely low light depends mainly on the composition of morphophysiologically and genetically different types of zooxanthellae living in a given colony of certain species. -
Hawai'i Institute of Marine Biology Northwestern Hawaiian Islands
Hawai‘i Institute of Marine Biology Northwestern Hawaiian Islands Coral Reef Research Partnership Quarterly Progress Reports II-III August, 2005-March, 2006 Report submitted by Malia Rivera and Jo-Ann Leong April 21, 2006 Photo credits: Front cover and back cover-reef at French Frigate Shoals. Upper left, reef at Pearl and Hermes. Photos by James Watt. Hawai‘i Institute of Marine Biology Northwestern Hawaiian Islands Coral Reef Research Partnership Quarterly Progress Reports II-III August, 2005-March, 2006 Report submitted by Malia Rivera and Jo-Ann Leong April 21, 2006 Acknowledgments. Hawaii Institute of Marine Biology (HIMB) acknowledges the support of Senator Daniel K. Inouye’s Office, the National Marine Sanctuary Program (NMSP), the Northwestern Hawaiian Islands Coral Reef Ecosystem Reserve (NWHICRER), State of Hawaii Department of Land and Natural Resources (DLNR) Division of Aquatic Resources, US Fish and Wildlife Service, NOAA Fisheries, and the numerous University of Hawaii partners involved in this project. Funding provided by NMSP MOA 2005-008/66832. Photos provided by NOAA NWHICRER and HIMB. Aerial photo of Moku o Lo‘e (Coconut Island) by Brent Daniel. Background The Hawai‘i Institute of Marine Biology (School of Ocean and Earth Science and Technology, University of Hawai‘i at Mānoa) signed a memorandum of agreement with National Marine Sanctuary Program (NOS, NOAA) on March 28, 2005, to assist the Northwestern Hawaiian Islands Coral Reef Ecosystem Reserve (NWHICRER) with scientific research required for the development of a science-based ecosystem management plan. With this overriding objective, a scope of work was developed to: 1. Understand the population structures of bottomfish, lobsters, reef fish, endemic coral species, and adult predator species in the NWHI. -
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. -
SEDIMENTARY FRAMEWORK of Lmainland FRINGING REEF DEVELOPMENT, CAPE TRIBULATION AREA
GREAT BARRIER REEF MARINE PARK AUTHORITY TECHNICAL MEMORANDUM GBRMPA-TM-14 SEDIMENTARY FRAMEWORK OF lMAINLAND FRINGING REEF DEVELOPMENT, CAPE TRIBULATION AREA D.P. JOHNSON and RM.CARTER Department of Geology James Cook University of North Queensland Townsville, Q 4811, Australia DATE November, 1987 SUMMARY Mainland fringing reefs with a diverse coral fauna have developed in the Cape Tribulation area primarily upon coastal sedi- ment bodies such as beach shoals and creek mouth bars. Growth on steep rocky headlands is minor. The reefs have exten- sive sandy beaches to landward, and an irregular outer margin. Typically there is a raised platform of dead nef along the outer edge of the reef, and dead coral columns lie buried under the reef flat. Live coral growth is restricted to the outer reef slope. Seaward of the reefs is a narrow wedge of muddy, terrigenous sediment, which thins offshore. Beach, reef and inner shelf sediments all contain 50% terrigenous material, indicating the reefs have always grown under conditions of heavy terrigenous influx. The relatively shallow lower limit of coral growth (ca 6m below ADD) is typical of reef growth in turbid waters, where decreased light levels inhibit coral growth. Radiocarbon dating of material from surveyed sites confirms the age of the fossil coral columns as 33304110 ybp, indicating that they grew during the late postglacial sea-level high (ca 5500-6500 ybp). The former thriving reef-flat was killed by a post-5500 ybp sea-level fall of ca 1 m. Although this study has not assessed the community structure of the fringing reefs, nor whether changes are presently occur- ring, it is clear the corals present today on the fore-reef slope have always lived under heavy terrigenous influence, and that the fossil reef-flat can be explained as due to the mid-Holocene fall in sea-level. -
2.02 Rajasuriya 2008
ARJAN RAJASURIYA National Aquatic Resources Research and Development Agency, Crow Island, Colombo 15, Sri Lanka [email protected]; [email protected] fringing and patch reefs (Swan, 1983; Rajasuriya et al., 1995; Rajasuriya & White, 1995). Fringing coral reef Selected coral reefs were monitored in the northern, areas occur in a narrow band along the coast except in western and southern coastal waters of Sri Lanka to the southeast and northeast of the island where sand assess their current status and to understand the movement inhibits their formation. The shallow recovery processes after the 1998 coral bleaching event continental shelf of Gulf of Mannar contains extensive and the 2004 tsunami. The highest rate of recovery coral patch reefs from the Bar Reef to Mannar Island was observed at the Bar Reef Marine Sanctuary where (Rajasuriya, 1991; Rajasuriya, et al. 1998a; Rajasuriya rapid growth of Acropora cytherea and Pocillopora & Premaratne, 2000). In addition to these coral reefs, damicornis has contributed to reef recovery. which are limited to a depth of about 10m, there are Pocillopora damicornis has shown a high level of offshore coral patches in the west and east of the recruitment and growth on most reef habitats island at varying distances (15 -20 km) from the including reefs in the south. An increase in the growth coastline at an average depth of 20m (Rajasuriya, of the calcareous alga Halimeda and high levels of 2005). Sandstone and limestone reefs occur as sedimentation has negatively affected some fringing discontinuous bands parallel to the shore from inshore reefs especially in the south. Reef surveys carried out areas to the edge of the continental shelf (Swan, 1983; for the first time in the northern coastal waters around Rajasuriya et al., 1995). -
Guide to the Identification of Precious and Semi-Precious Corals in Commercial Trade
'l'llA FFIC YvALE ,.._,..---...- guide to the identification of precious and semi-precious corals in commercial trade Ernest W.T. Cooper, Susan J. Torntore, Angela S.M. Leung, Tanya Shadbolt and Carolyn Dawe September 2011 © 2011 World Wildlife Fund and TRAFFIC. All rights reserved. ISBN 978-0-9693730-3-2 Reproduction and distribution for resale by any means photographic or mechanical, including photocopying, recording, taping or information storage and retrieval systems of any parts of this book, illustrations or texts is prohibited without prior written consent from World Wildlife Fund (WWF). Reproduction for CITES enforcement or educational and other non-commercial purposes by CITES Authorities and the CITES Secretariat is authorized without prior written permission, provided the source is fully acknowledged. Any reproduction, in full or in part, of this publication must credit WWF and TRAFFIC North America. The views of the authors expressed in this publication do not necessarily reflect those of the TRAFFIC network, WWF, or the International Union for Conservation of Nature (IUCN). The designation of geographical entities in this publication and the presentation of the material do not imply the expression of any opinion whatsoever on the part of WWF, TRAFFIC, or 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 TRAFFIC symbol copyright and Registered Trademark ownership are held by WWF. TRAFFIC is a joint program of WWF and IUCN. Suggested citation: Cooper, E.W.T., Torntore, S.J., Leung, A.S.M, Shadbolt, T. and Dawe, C. -
The Reproduction of the Red Sea Coral Stylophora Pistillata
MARINE ECOLOGY PROGRESS SERIES Vol. 1, 133-144, 1979 - Published September 30 Mar. Ecol. Prog. Ser. The Reproduction of the Red Sea Coral Stylophora pistillata. I. Gonads and Planulae B. Rinkevich and Y.Loya Department of Zoology. The George S. Wise Center for Life Sciences, Tel Aviv University. Tel Aviv. Israel ABSTRACT: The reproduction of Stylophora pistillata, one of the most abundant coral species in the Gulf of Eilat, Red Sea, was studied over more than two years. Gonads were regularly examined using histological sections and the planula-larvae were collected in situ with plankton nets. S. pistillata is an hermaphroditic species. Ovaries and testes are situated in the same polyp, scattered between and beneath the septa and attached to them by stalks. Egg development starts in July preceding the spermaria, which start to develop only in October. A description is given on the male and female gonads, their structure and developmental processes. During oogenesis most of the oocytes are absorbed and usually only one oocyte remains in each gonad. S. pistillata broods its eggs to the planula stage. Planulae are shed after sunset and during the night. After spawning, the planula swims actively and changes its shape frequently. A mature planula larva of S. pistillata has 6 pairs of complete mesenteries (Halcampoides stage). However, a wide variability in developmental stages exists in newly shed planulae. The oral pole of the planula shows green fluorescence. Unique organs ('filaments' and 'nodules') are found on the surface of the planula; -
Coral Health and Disease in the Pacific: Vision for Action
IV. STATE OF KNOWLEDGE IN THE PACIFIC—WHAT DO WE KNOW AND WHAT HAVE WE LEARNED? OVERVIEW OF ISSUES UNIQUE TO THE PACIFIC: BIOLOGICAL & SOCIAL PERSPECTIVES Michael J. Gawel Guam EPA 120 Bengbing St. Y-Papao Dededo, GU 96929 [email protected] Pacific Islands The term “Pacific Islands” in the context of this paper arbitrarily refers to those tropical islands of the central and western Pacific Ocean which support shallow hermatypic coral reefs, but excluding the Hawaiian Archipelago, which is covered in other papers. The tropical Pacific Island nations and territories all support coral reefs and, no doubt, harbor coral diseases, although these have not been scientifically documented in many of the islands. In fact, as part of the U.S. National Action Plan to Conserve Coral Reefs, surveys in 2002 and 2004 of coral reef academic scientists, resource managers, government agencies and NGOs recorded that in the U.S. Pacific islands they perceived “no threat” from coral disease, although American Samoa registered an increase to perception of “moderate threat” in the 2004 survey (Waddell, 2005). This lack of concern partially reflects a lack of information on the status of diseases in many islands. Wilkinson (2004, p. 405) notes that in American Samoa and Micronesia “Coral bleaching and disease were either rare or undocumented in 1994, but are now clearly evident and considered a serious threat to many reefs in the region.” The Pacific island coral reefs range from veneers on newly emergent volcanic islands, to platform-like fringing reefs, to barrier reefs with lagoons, to atolls, and include non- emergent isolated banks.