Coral Health and Disease in the Pacific: Vision for Action
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
High Clonality in Acropora Palmata and Acropora Cervicornis Populations of Guadeloupe, French Lesser Antilles
CSIRO PUBLISHING Marine and Freshwater Research Short Communication http://dx.doi.org/10.1071/MF14181 High clonality in Acropora palmata and Acropora cervicornis populations of Guadeloupe, French Lesser Antilles A. JapaudA, C. BouchonA, J.-L. ManceauA and C. FauvelotB,C AUMR 7208 BOREA, LabEx CORAIL, Universite´ des Antilles et de la Guyane, BP 592, 97159 Pointe-a`-Pitre, Guadeloupe. BUMR 9220 ENTROPIE, LabEx CORAIL, Centre IRD de Noume´a, 101 Promenade Roger Laroque, BPA5, 98848 Noume´a, New Caledonia. CCorresponding author. Email: [email protected] Abstract. Since the 1980s, population densities of Acroporidae have dramatically declined in the Caribbean Sea. Quantitative censuses of Acroporidae provide information on the number of colonies (i.e. ramets), but not on the number of genetically distinct individuals (i.e. genets). In this context, the aim of our study was to provide an overview of the genetic status of Acropora populations in Guadeloupe by examining the genotypic richness of Acropora palmata and Acropora cervicornis. Using 14 microsatellite loci, we found extremely low genotypic richness for both species from Caye-a`-Dupont reef (i.e. 0.125 for A. palmata and nearly zero for A. cervicornis). Because genetic diversity contributes to the ability of organisms to evolve and adapt to new environmental conditions, our results are alarming in the context of ongoing global warming as long periods of clonal growth without sexual recruitment may lead to the extinction of these populations. Additional keywords: genotypic richness, Acroporidae, microsatellites, Caribbean Sea. Received 27 June 2014, accepted 5 November 2014, published online 19 March 2015 Introduction censuses of acroporid densities report on the number of ramets Stony corals of the Acroporidae (Class Anthozoa, Order Scler- (i.e. -
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 Reefs & Global Climate Change
environment+ + Coral reefs & Global climate change Potential Contributions of Climate Change to Stresses on Coral Reef Ecosystems + Robert W. Buddemeier KANSAS G EOLOGICAL S URVEY Joan A. Kleypas NATIONAL C ENTER FOR ATMOSPHERIC R ESEARCH Richard B. Aronson DAUPHIN I SLAND S EA L AB + Coral reefs & Global climate change Potential Contributions of Climate Change to Stresses on Coral Reef Ecosystems Prepared for the Pew Center on Global Climate Change by Robert W. Buddemeier KANSAS G EOLOGICAL S URVEY Joan A. Kleypas NATIONAL C ENTER FOR ATMOSPHERIC R ESEARCH Richard B. Aronson DAUPHIN I SLAND S EA L AB February 2004 Contents Foreword ii Executive Summary iii I. Introduction 1 A. Coral Reefs and Reef Organisms 1 B. The “Coral Reef Crisis” 4 C. Climate and Environmental Change 5 II. Nonclimatic Stresses to Coral Reefs 7 A. Types and Categories of Stresses and Effects 7 B. Terrestrial Inputs 9 C. Overfishing and Resource Extraction 11 D. Coastal Zone Modification and Mining 13 E. Introduced and Invasive Species 13 III. Climatic Change Stresses to Coral Reefs 14 A. Coral Bleaching 15 B. Global Warming and Reef Distribution 17 C. Reduced Calcification Potential 19 D. Sea Level 21 E. El Niño-Southern Oscillation 21 F. Ocean Circulation Changes 22 + G. Precipitation and Storm Patterns 22 IV. Synthesis and Discussion 24 A. Infectious Diseases 24 B. Predation 25 C. Connections with Global Climate Change and Human Activity 26 D. Regional Comparison 27 E. Adaptation 28 V. Resources at Risk 30 + A. Socioeconomic Impacts 30 B. Biological and Ecological Impacts 31 C. Protection and Conservation 31 VI. -
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. -
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). -
What Evidence Exists on the Impacts of Chemicals Arising from Human Activity on Tropical Reef-Building Corals?
Ouédraogo et al. Environ Evid (2020) 9:18 https://doi.org/10.1186/s13750-020-00203-x Environmental Evidence SYSTEMATIC MAP PROTOCOL Open Access What evidence exists on the impacts of chemicals arising from human activity on tropical reef-building corals? A systematic map protocol Dakis‑Yaoba Ouédraogo1* , Romain Sordello2, Sophie Brugneaux3, Karen Burga4, Christophe Calvayrac5,6, Magalie Castelin7, Isabelle Domart‑Coulon8, Christine Ferrier‑Pagès9, Mireille M. M. Guillaume10,11, Laetitia Hédouin11,12, Pascale Joannot13, Olivier Perceval14 and Yorick Reyjol2 Abstract Background: Tropical coral reefs cover ca. 0.1% of the Earth’s surface but host an outstanding biodiversity and provide important ecosystem services to millions of people living nearby. However, they are currently threatened by both local (e.g. nutrient enrichment and chemical pollution of coastal reefs, arising from poor land management, agriculture and industry) and global stressors (mainly seawater warming and acidifcation, i.e. climate change). Global and local stressors interact together in diferent ways, but the presence of one stressor often reduces the tolerance to additional stress. While global stressors cannot be halted by local actions, local stressors can be reduced through ecosystem management, therefore minimizing the impact of climate change on reefs. To inform decision‑makers, we propose here to systematically map the evidence of impacts of chemicals arising from anthropogenic activities on tropical reef‑building corals, which are the main engineer species of reef ecosystems. We aim to identify the combina‑ tions of chemical and coral responses that have attracted the most attention and for which evidence can be further summarized in a systematic review that will give practical information to decision‑makers. -
1 Ecological Engineering Considerations for Coral
ECOLOGICAL ENGINEERING CONSIDERATIONS FOR CORAL REEFS IN THE DESIGN OF MULTIFUNCTIONAL COASTAL STRUCTURES Michael Foley1, Yuko Stender2, Amarjit Singh1, Paul Jokiel2, and Ku‘ulei Rodgers2 A multifunctional structure is being designed for the Kahului Harbor, Maui, Hawai‘i, to mitigate operational problems caused by wave energy while also providing coral reef habitat. There is limited information on how the design of a coastal structure can be manipulated to enhance the ecology of targeted coral communities. To inform the ecological engineering of an artificial coral reef, the relationship between substrate characteristics and coral colonization was investigated through coral recruitment experiments and study of field conditions. Three concrete compositions that differed by the use of basalt, limestone, or recycled aggregates were tested in field and laboratory experiments to determine the impact of each substrate on the recruitment of juvenile hermatypic corals. The concrete test plates were deployed in three environments for a period of about one year, after which the coral recruits on each plate were identified and counted. No significant difference was found in the average number of coral recruits on the concrete mixed with basalt, limestone and recycled aggregate (60 ± 9, 83 ± 17 and 77 ± 14, respectively). Significant differences in coral recruitment were found due to the laboratory tanks, deep water, and shallow water field tests environments (86 ± 11, 135 ± 15 and 4 ± 1, respectively). These results highlight the importance of environmental site conditions for the development of coral reef habitat. A field study was conducted in the vicinity of purposed artificial reef site to relate the topographic features of the surrounding environment to the levels of live coral coverage. -
A Scientific Forum on the Gulf of Mexico: the Islands in the Stream Concept
Proceedings: Gulf of Mexico Science Forum A Scientific Forum on the Gulf of Mexico: The Islands in the Stream Concept Proceedings of the Forum: 23 January 2008 Keating Education Center Mote Marine Laboratory Sarasota, Florida Proceedings: Gulf of Mexico Science Forum Table of Contents Forward (Ernest Estevez) .............................................................................................................4 Executive Summary.....................................................................................................................6 Acknowledgements ......................................................................................................................9 Organizing Committee ................................................................................................................9 Welcome and Introduction (Kumar Mahadevan and Daniel J. Basta) .....................................10 Introduction to the Forum (Billy D. Causey)...........................................................................12 Summary of Scientific Forum (John Ogden) ...........................................................................14 Panel 1: The Geological Setting...............................................................................................17 Geologic Underpinnings of the “Islands in the Stream”; West Florida Margin (Albert Hine and Stanley Locker)...............................................17 Shelf Edge of the Northwest Gulf of Mexico (Niall Slowey).............................................22 -
Coral Reefs, Unintentionally Delivering Bermuda’S E-Mail: [email protected] fi Rst Colonists
Introduction to Bermuda: Geology, Oceanography and Climate 1 0 Kathryn A. Coates , James W. Fourqurean , W. Judson Kenworthy , Alan Logan , Sarah A. Manuel , and Struan R. Smith Geographic Location and Setting Located at 32.4°N and 64.8°W, Bermuda lies in the northwest of the Sargasso Sea. It is isolated by distance, deep Bermuda is a subtropical island group in the western North water and major ocean currents from North America, sitting Atlantic (Fig. 10.1a ). A peripheral annular reef tract surrounds 1,060 km ESE from Cape Hatteras, and 1,330 km NE from the islands forming a mostly submerged 26 by 52 km ellipse the Bahamas. Bermuda is one of nine ecoregions in the at the seaward rim of the eroded platform (the Bermuda Tropical Northwestern Atlantic (TNA) province (Spalding Platform) of an extinct Meso-Cenozoic volcanic peak et al. 2007 ) . (Fig. 10.1b ). The reef tract and the Bermuda islands enclose Bermuda’s national waters include pelagic environments a relatively shallow central lagoon so that Bermuda is atoll- and deep seamounts, in addition to the Bermuda Platform. like. The islands lie to the southeast and are primarily derived The Bermuda Exclusive Economic Zone (EEZ) extends from sand dune formations. The extinct volcano is drowned approx. 370 km (200 nautical miles) from the coastline of the and covered by a thin (15–100 m), primarily carbonate, cap islands. Within the EEZ, the Territorial Sea extends ~22 km (Vogt and Jung 2007 ; Prognon et al. 2011 ) . This cap is very (12 nautical miles) and the Contiguous Zone ~44.5 km (24 complex, consisting of several sets of carbonate dunes (aeo- nautical miles) from the same baseline, both also extending lianites) and paleosols laid down in the last million years well beyond the Bermuda Platform. -
Biomineralisation in Reef-Building Corals: from Molecular Mechanisms to Environmental Control
C. R. Palevol 3 (2004) 453–467 General Palaeontology (Palaeobiochemistry) Biomineralisation in reef-building corals: from molecular mechanisms to environmental control Denis Allemand a,b,*, Christine Ferrier-Pagès a, Paola Furla a,1, Fanny Houlbrèque a, Sandrine Puverel a,b, Stéphanie Reynaud a, Éric Tambutté a, Sylvie Tambutté a, Didier Zoccola a a Centre scientifique de Monaco, avenue Saint-Martin, 98000 Monaco, principauté de Monaco b UMR 1112 INRA–UNSA, faculté des sciences, université Nice–Sophia-Antipolis, parc Valrose, BP 71, 06108 Nice cedex 2, France Received 7 October 2003; accepted after revision 12 July 2004 Available online 30 September 2004 Written on invitation of the Editorial Board Abstract Coral reefs constitute real oasis sheltering for about one third of the identified fishes, representing a major advantage for the economy and tourism of many tropical countries. However it is paradoxical to notice that their formation at the cellular level or even at the scale of the organism is still poorly known. Effectively, biomineralisation, the process that is at the basis of their edification, is always the subject of numerous researches. Two combined mechanisms lead to the formation of a biomineral, the synthesis/secretion of macromolecules referred to as ‘organic matrix’, and the transport of ions (calcium, bicarbonates and protons in the case of calcification) to the mineralising site. This review shows a view of the works carried out on biominerali- sation in scleractinian corals, including some aspects on the control of calcification by environmental parameters. It also gives insights into the biological basis of the use of coral skeletons as environmental archives in palaeo-oceanography. -
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. -
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.