Research Article Coral Diversity and the Severity of Disease
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A Research Review of Interventions to Increase the Persistence and Resilience of Coral Reefs (2019)
THE NATIONAL ACADEMIES PRESS This PDF is available at http://nap.edu/25279 SHARE A Research Review of Interventions to Increase the Persistence and Resilience of Coral Reefs (2019) DETAILS 258 pages | 6 x 9 | PAPERBACK ISBN 978-0-309-48535-7 | DOI 10.17226/25279 CONTRIBUTORS GET THIS BOOK Committee on Interventions to Increase the Resilience of Coral Reefs; Ocean Studies Board; Board on Life Sciences; Division on Earth and Life Studies; National Academies of Sciences, Engineering, and Medicine FIND RELATED TITLES SUGGESTED CITATION National Academies of Sciences, Engineering, and Medicine 2019. A Research Review of Interventions to Increase the Persistence and Resilience of Coral Reefs. Washington, DC: The National Academies Press. https://doi.org/10.17226/25279. Visit the National Academies Press at NAP.edu and login or register to get: – Access to free PDF downloads of thousands of scientific reports – 10% off the price of print titles – Email or social media notifications of new titles related to your interests – Special offers and discounts Distribution, posting, or copying of this PDF is strictly prohibited without written permission of the National Academies Press. (Request Permission) Unless otherwise indicated, all materials in this PDF are copyrighted by the National Academy of Sciences. Copyright © National Academy of Sciences. All rights reserved. A Research Review of Interventions to Increase the Persistence and Resilience of Coral Reefs A RESEARCH REVIEW OF INTERVENTIONS TO INCREASE THE PERSISTENCE AND RESILIENCE OF CORAL REEFS Committee on Interventions to Increase the Resilience of Coral Reefs Ocean Studies Board Board on Life Sciences Division on Earth and Life Studies A Consensus Study Report of Copyright National Academy of Sciences. -
St. Kitts Final Report
ReefFix: An Integrated Coastal Zone Management (ICZM) Ecosystem Services Valuation and Capacity Building Project for the Caribbean ST. KITTS AND NEVIS FIRST DRAFT REPORT JUNE 2013 PREPARED BY PATRICK I. WILLIAMS CONSULTANT CLEVERLY HILL SANDY POINT ST. KITTS PHONE: 1 (869) 765-3988 E-MAIL: [email protected] 1 2 TABLE OF CONTENTS Page No. Table of Contents 3 List of Figures 6 List of Tables 6 Glossary of Terms 7 Acronyms 10 Executive Summary 12 Part 1: Situational analysis 15 1.1 Introduction 15 1.2 Physical attributes 16 1.2.1 Location 16 1.2.2 Area 16 1.2.3 Physical landscape 16 1.2.4 Coastal zone management 17 1.2.5 Vulnerability of coastal transportation system 19 1.2.6 Climate 19 1.3 Socio-economic context 20 1.3.1 Population 20 1.3.2 General economy 20 1.3.3 Poverty 22 1.4 Policy frameworks of relevance to marine resource protection and management in St. Kitts and Nevis 23 1.4.1 National Environmental Action Plan (NEAP) 23 1.4.2 National Physical Development Plan (2006) 23 1.4.3 National Environmental Management Strategy (NEMS) 23 1.4.4 National Biodiversity Strategy and Action Plan (NABSAP) 26 1.4.5 Medium Term Economic Strategy Paper (MTESP) 26 1.5 Legislative instruments of relevance to marine protection and management in St. Kitts and Nevis 27 1.5.1 Development Control and Planning Act (DCPA), 2000 27 1.5.2 National Conservation and Environmental Protection Act (NCEPA), 1987 27 1.5.3 Public Health Act (1969) 28 1.5.4 Solid Waste Management Corporation Act (1996) 29 1.5.5 Water Courses and Water Works Ordinance (Cap. -
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. -
Community Structure of Pleistocene Coral Reefs of Curacë Ao, Netherlands Antilles
Ecological Monographs, 71(1), 2001, pp. 49±67 q 2001 by the Ecological Society of America COMMUNITY STRUCTURE OF PLEISTOCENE CORAL REEFS OF CURACË AO, NETHERLANDS ANTILLES JOHN M. PANDOLFI1 AND JEREMY B. C. JACKSON2 Center for Tropical Paleoecology and Archeology, Smithsonian Tropical Research Institute, Apartado 2072, Balboa, Republic of Panama Abstract. The Quaternary fossil record of living coral reefs is fundamental for un- derstanding modern ecological patterns. Living reefs generally accumulate in place, so fossil reefs record a history of their former biological inhabitants and physical environments. Reef corals record their ecological history especially well because they form large, resistant skeletons, which can be identi®ed to species. Thus, presence±absence and relative abun- dance data can be obtained with a high degree of con®dence. Moreover, potential effects of humans on reef ecology were absent or insigni®cant on most reefs until the last few hundred years, so that it is possible to analyze ``natural'' distribution patterns before intense human disturbance began. We characterized Pleistocene reef coral assemblages from CuracËao, Netherlands Antil- les, Caribbean Sea, focusing on predictability in species abundance patterns from different reef environments over broad spatial scales. Our data set is composed of .2 km of surveyed Quaternary reef. Taxonomic composition showed consistent differences between environ- ments and along secondary environmental gradients within environments. Within environ- ments, taxonomic composition of communities was markedly similar, indicating nonrandom species associations and communities composed of species occurring in characteristic abun- dances. This community similarity was maintained with little change over a 40-km distance. The nonrandom patterns in species abundances were similar to those found in the Caribbean before the effects of extensive anthropogenic degradation of reefs in the late 1970s and early 1980s. -
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 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. -
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.