Atoll Research Bulletin No. 307
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Reef Coralgal Assemblages As Recorders of Paleobathymetry and Sea Level Changes in the Indo-Pacific Province
PERGAMON Quaternary Science Reviews 18 (1999) 1681-1695 QSR Reef coralgal assemblages as recorders of paleobathymetry and sea level changes in the Indo-Pacific province I' G. Cabioch">*,L.F. Montaggionib, G. Faurec, A. Ribaud-Lamentib "ORSTOM (L'Institut franqais de Recherche scientifique pour le Développement en Coopérationj, UMR 6526 'Géosciences Azur', B.P. A5, Noum& Cedex, New Caledonia '.:I bUPRESA CNRS 6019, Centre de Sédinientologie et Palhontologie, Université de Provence, 13331 Marseille Cedex 3, France 'UPRESA CNRS 6019, Laboratoire $Hydrobiologie A.larine et Continentale, Université des Sciences et Techniques du Languedoc, Place Eugène Bataillon, 34095 Montpellier Cedex 5, France æiP Abstract Science Ltd. All Eights reserved. - __ D l I Fonds Documentaire I R 1 I I 1 I O Il lull~Illi~~lÎ~~~~i~iipillill1002 1466 1. Introduction building coral communities, are regarded as- one of the most reliable sea-level markers (Liglity et al., 1978; During thellast few decades, our knowledge of psst- 1 Davies and Montaggioni, 1985; Hopley, 1986; Montag- glacial sea-level changes has been greatly enhanced gioni and Faure, 1997). through studies of reef sites (Fairbanks, 1989; Bard et al., Corals older than 6 ka BP are not generally directly 1990,1996; Chappell and Polach, 1991; Edwards et al., accessible from rapidly subsiding (e.g. intraplate volcanic 1993).The tropical zone offers the opportunity to exami- islands) or slowly uplifting coasts (e.g. hydro-isostasy- ne sea-level changes and the melting history of continen- experiencing areas). As a result, the only way to recover tal ice sheets far from the polar zones (Bard et al., 1996). -
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. -
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). -
Full Text in Pdf Format
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 -
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. -
The Importance of Live Coral Habitat for Reef Fishes and Its Role in Key Ecological Processes
ResearchOnline@JCU This file is part of the following reference: Coker, Darren J. (2012) The importance of live coral habitat for reef fishes and its role in key ecological processes. PhD thesis, James Cook University. Access to this file is available from: http://eprints.jcu.edu.au/23714/ The author has certified to JCU that they have made a reasonable effort to gain permission and acknowledge the owner of any third party copyright material included in this document. If you believe that this is not the case, please contact [email protected] and quote http://eprints.jcu.edu.au/23714/ THE IMPORTANCE OF LIVE CORAL HABITAT FOR REEF FISHES AND ITS ROLE IN KEY ECOLOGICAL PROCESSES Thesis submitted by Darren J. Coker (B.Sc, GDipResMeth) May 2012 For the degree of Doctor of Philosophy In the ARC Centre of Excellence for Coral Reef Studies and AIMS@JCU James Cook University Townsville, Queensland, Australia Statement of access I, the undersigned, the author of this thesis, understand that James Cook University will make it available for use within the University Library and via the Australian Digital Thesis Network for use elsewhere. I understand that as an unpublished work this thesis has significant protection under the Copyright Act and I do not wish to put any further restrictions upon access to this thesis. Signature Date ii Statement of sources Declaration I declare that this thesis is my own work and has not been submitted in any form for another degree or diploma at my university or other institution of tertiary education. Information derived from the published or unpublished work of others has been acknowledged in the text and a list of references is given. -
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. -
Unique Quantitative Symbiodiniaceae Signature of Coral Colonies Revealed
www.nature.com/scientificreports OPEN Unique quantitative Symbiodiniaceae signature of coral colonies revealed through spatio- Received: 14 November 2018 Accepted: 25 April 2019 temporal survey in Moorea Published: xx xx xxxx Héloïse Rouzé1, Gaël Lecellier 2,3, Xavier Pochon4,5, Gergely Torda6 & Véronique Berteaux-Lecellier 1,2 One of the mechanisms of rapid adaptation or acclimatization to environmental changes in corals is through the dynamics of the composition of their associated endosymbiotic Symbiodiniaceae community. The various species of these dinofagellates are characterized by diferent biological properties, some of which can confer stress tolerance to the coral host. Compelling evidence indicates that the corals’ Symbiodiniaceae community can change via shufing and/or switching but the ecological relevance and the governance of these processes remain elusive. Using a qPCR approach to follow the dynamics of Symbiodiniaceae genera in tagged colonies of three coral species over a 10–18 month period, we detected putative genus-level switching of algal symbionts, with coral species-specifc rates of occurrence. However, the dynamics of the corals’ Symbiodiniaceae community composition was not driven by environmental parameters. On the contrary, putative shufing event were observed in two coral species during anomalous seawater temperatures and nutrient concentrations. Most notably, our results reveal that a suit of permanent Symbiodiniaceae genera is maintained in each colony in a specifc range of quantities, giving a unique ‘Symbiodiniaceae signature’ to the host. This individual signature, together with sporadic symbiont switching may account for the intra-specifc diferences in resistance and resilience observed during environmental anomalies. Dinofagellate algae from the family Symbiodiniaceae are one of the keystone taxa for coral reef ecosystems.