Marine Debris in Reef Habitats
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Socan Monitoring Workshop
SOCAN MONITORING WORKSHOP Image credit: Lauren Valentino, NOAA/AOML 2/28/17 WorksHop Report SOCAN MONITORING WORKSHOP SOCAN MONITORING WORKSHOP IDENTIFYING PRIORITY LOCATIONS FOR OCEAN ACIDIFICATION MONITORING IN THE U.S. SOUTHEAST SUMMARY The Southeast Ocean and Coastal Acidification Network (SOCAN) held a worksHop in CHarleston, SoutH Carolina to facilitate discussion on priority locations for ocean acidification monitoring in tHe SoutHeast. The discussion included identification of key gradients in physical, chemical and biological parameters along tHe SoutHeast coast, a review of current monitoring efforts, and an assessment of stakeHolder needs. Sixteen monitoring locations were identified as potential acidification monitoring locations (see page 12). The following three monitoring locations were HigHligHted as priority sites tHat would furtHer our understanding of the chemistry and regional drivers of ocean acidification and address stakeholder needs: (1) Sapelo Island, GA (2) Gulf Stream, offsHore of Gray’s Reef, GA (3) Biscayne National Park, FL The workshop concluded witH a discussion of logistics and opportunities to pursue monitoring at tHe recommended locations. A copy of tHe agenda is included in Appendix 1. PROCEEDINGS Approximately 16 experts gatHered for tHe SOCAN Monitoring Workshop to outline recommendations for priority ocean acidification monitoring locations in tHe SoutHeast (Attendee List, Appendix 2). The worksHop began witH introductory remarks regarding tHe structure and responsibilities of SOCAN and SECOORA. Following the introductory remarks, participants reviewed the proposed agenda; no modifications were made. The first half-day was spent reviewing tHe state of ocean acidification science and regional response. Kim Yates sHared a syntHesis of tHe 2016 SOCAN State of the Science meeting, wHicH included a review of webinars and key findings related to OA chemistry, modeling and organismal response. -
Mangroves and Coral Reefs: David Stoddart and the Cambridge Physiographic Tradition Colin D
University of Wollongong Research Online Faculty of Science, Medicine and Health - Papers: Faculty of Science, Medicine and Health Part B 2018 Mangroves and coral reefs: David Stoddart and the Cambridge physiographic tradition Colin D. Woodroffe University of Wollongong, [email protected] Publication Details Woodroffe, C. D. (2018). Mangroves and coral reefs: David Stoddart and the Cambridge physiographic tradition. Atoll Research Bulletin, 619 121-145. Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Mangroves and coral reefs: David Stoddart and the Cambridge physiographic tradition Abstract Mangroves are particularly extensive on sheltered, macrotidal, muddy tropical coastlines, but also occur in association with coral reefs. Reefs attenuate wave energy, in some locations enabling the accretion of fine calcareous sediments which in turn favour establishment of seagrasses and mangroves. Knowledge of the distribution and ecology of both reefs and mangroves increased in the first half of the 20th century. J Alfred Steers participated in the Great Barrier Reef Expedition in 1928, and developed an interest in the geomorphological processes by which islands had formed in this setting. It became clear that many mangrove forests showed a zonation of species and some researchers inferred successional changes, even implying that reefs might transition through a mangrove stage, ultimately forming land. Valentine Chapman studied the ecology of mangroves, and Steers and Chapman described West Indian mangrove islands in the 1940s during the University of Cambridge expedition to Jamaica. These studies provided the background for David Stoddart's participation in the Cambridge Expedition to British Honduras and his PhD examination of three Caribbean atolls. -
III. Species Richness and Benthic Cover
2009 Quick Look Report: Miller et al. III. Species Richness and Benthic Cover Background The most species-rich marine communities probably occur on coral reefs and this pattern is at least partly due to the diversity of available habitats and the degree to which species are ecologically restricted to particular niches. Coral reefs in the Indo-Pacific and Caribbean in particular are usually thought to hold the greatest diversity of marine life at several levels of biological diversity. Diversity on coral reefs is strongly influenced by environmental conditions and geographic location, and variations in diversity can be correlated with differences in reef structure. For example, shallow and mid-depth fore-reef habitats in the Caribbean were historically dominated by largely mono-specific zones of just two Acropora species, while the Indo-Pacific has a much greater number of coral species and growth forms. Coral reefs are in a state of decline worldwide from multiple stressors, including physical impacts to habitat, changes in water quality, overfishing, disease outbreaks, and climate change. Coral reefs in a degraded state are often characterized by one or more signs, including low abundances of top-level predators, herbivores, and reef-building corals, but higher abundances of non-hermatypic organisms such as seaweeds. For the Florida Keys, there is little doubt that areas historically dominated by Acropora corals, particularly the shallow (< 6 m) and deeper (8-15 m) fore reef, have changed substantially, largely due to Caribbean-wide disease events and bleaching. However, debate continues regarding other causes of coral reef decline, thus often making it difficult for resource managers to determine which courses of action to take to minimize localized threats in lieu of larger-scale factors such as climate change. -
Cryptic Herbivorous Invertebrates Restructure the Composition of Degraded Coral Reef Communities in the Florida Keys, Florida, USA
Old Dominion University ODU Digital Commons Biological Sciences Theses & Dissertations Biological Sciences Spring 2019 Cryptic Herbivorous Invertebrates Restructure the Composition of Degraded Coral Reef Communities in the Florida Keys, Florida, USA Angelo Jason Spadaro Old Dominion University, [email protected] Follow this and additional works at: https://digitalcommons.odu.edu/biology_etds Part of the Biology Commons, Ecology and Evolutionary Biology Commons, and the Natural Resources and Conservation Commons Recommended Citation Spadaro, Angelo J.. "Cryptic Herbivorous Invertebrates Restructure the Composition of Degraded Coral Reef Communities in the Florida Keys, Florida, USA" (2019). Doctor of Philosophy (PhD), Dissertation, Biological Sciences, Old Dominion University, DOI: 10.25777/fg35-1j72 https://digitalcommons.odu.edu/biology_etds/86 This Dissertation is brought to you for free and open access by the Biological Sciences at ODU Digital Commons. It has been accepted for inclusion in Biological Sciences Theses & Dissertations by an authorized administrator of ODU Digital Commons. For more information, please contact [email protected]. CRYPTIC HERBIVOROUS INVERTEBRATES RESTRUCTURE THE COMPOSITION OF DEGRADED CORAL REEF COMMUNITIES IN THE FLORIDA KEYS, FLORIDA, USA by Angelo Jason Spadaro B.S. May 2010, Old Dominion University A Dissertation Submitted to the Faculty of Old Dominion University in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY ECOLOGICAL SCIENCES OLD DOMINION UNIVERSITY May 2019 Approved by: Mark J Butler, IV (Director) Eric Walters (Member) Dan Barshis (Member) Seabird McKeon (Member) ABSTRACT CRYPTC HERBIVOROUS INVERTEBRATES RESTRUCTURE THE COMPOSITION OF DEGRADED CORAL REEF COMMUNITIES IN THE FLORIDA KEYS, FLORIDA, USA Angelo Jason Spadaro Old Dominion University, 2019 Director: Dr. -
Decade-Scale Trend in Sea Water Salinity Revealed Through ฮด<Sup>
BULLETIN OF MARINE SCIENCE, 54(3): 670-678, 1994 DECADE-SCALE TREND IN SEA WATER SALINITY REVEALED THROUGH 8180 ANALYSIS OF MONTASTRAEA ANNULARIS ANNUAL GROWTH BANDS Robert B. Halley, Peter K. Swart, Richard E. Dodge, and J. Harold Hudson ABSTRACT Stable oxygen isotope ratios (1)180) of coral skeletons are influenced by ambient water temperature and by the oxygen isotope ratio in the surrounding sea water, which, in turn, is linked to evaporation (salinity) and precipitation. To investigate this relationship more thor- oughly, we collected hourly temperature data from the Hen and Chickens Reef in the Florida Keys between 1975 and 1988 and compared them to'the 1)180 of Montastraea annularis skeleton that grew during the same interval. To ensure that we obtained the correct oxygen isotopic range in the skeleton we typically sampled the coral at a resolution of 20-30 samples in 1 year; in 1 year we sampled the coral at a resolution of 70 samples·year-'. Despite our high-resolution sampling, we were unable to obtain the full temperature-induced 1)180 range in the skeleton. Our data suggest that, during the summer, evaporation causes isotopic en- richment in the water, partially masking the temperature-induced signal. Our data also show that oxygen isotopic composition of seawater at the reef has increased since 1981. This increase indicates that salinity has increased slightly during the past decade, perhaps as a result of increased evaporation in waters of Florida Bay and the Keys. This phenomenon is probably not caused by a decrease in the outflow of freshwater into Florida Bay from the Everglades but may be related to the measured deficit in precipitation that has occurred over the past decade. -
Natural Resources Management Needs for Coastal and Littoral Marine Ecosystems of the U.S
Technical Report HCSU-002 NATURAL RESOURCES MANAGEMENT NEEDS FOR COASTAL AND LITTORAL MARINE ECOSYSTEMS OF THE U.S. AFFILIATED PACIFIC ISLANDS: American Samoa, Guam, COMMONWealth OF THE Northern MARIANAS Maria Haws, Editor Hawai`i Cooperative Studies Unit, University of Hawai`i at Hilo, Pacific Aquaculture and Coastal Resources Center (PACRC), P.O. Box 44, Hawai`i National Park, HI 96718 Hawai`i Cooperative Studies Unit University of Hawai`i at Hilo 200 W. Kawili St. Hilo, HI 96720 (808) 933-0706 Technical Report HCSU-002 NATURAL RESOURCES MANAGEMENT NEEDS FOR COASTAL AND LITTORAL MARINE ECOSYSTEMS OF THE U.S. AFFILIATED PACIFIC ISLANDS: American Samoa, Guam, Commonwealth of the Northern Marianas Islands, Republic of the Marshall Islands, Federated States of Micronesia and the Republic of Palau Maria Haws, Ph.D., Editor Pacific Aquaculture and Coastal Resources Center/University of Hawai’i Hilo University of Hawaii Sea Grant College Program 200 W. Kawili St. Hilo, HI 96720 Hawai’i Cooperative Studies Unit University of Hawai’i at Hilo Pacific Aquaculture and Coastal Resources Center (PACRC) 200 W. Kawili St. Hilo, Hawai‘i 96720 (808)933-0706 November 2006 This product was prepared under Cooperative Agreement CA03WRAG0036 for the Pacific Island Ecosystems Research Center of the U.S. Geological Survey The opinions expressed in this product are those of the authors and do not necessarily represent the opinions of the U.S. Government. Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Technical Report HCSU-002 NATURAL RESOURCES MANAGEMENT NEEDS FOR COASTAL AND LITTORAL MARINE ECOSYSTEMS OF THE U.S. -
Corals Sustain Growth but Not Skeletal Density Across the Florida Keys Reef Tract Despite Ongoing Warming
bioRxiv preprint doi: https://doi.org/10.1101/310037; this version posted April 28, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Title: Corals sustain growth but not skeletal density across the Florida Keys Reef Tract despite 2 ongoing warming 3 Running head: Coral growth on the Florida Keys Reef Tract 4 5 John P. Rippe1*, Justin H. Baumann1, Daphne N. De Leener1, Hannah E. Aichelman1,y, Eric B. 6 Friedlander2, Sarah W. Davies1,g and Karl D. Castillo1,3 7 8 1Department of Marine Sciences, University of North Carolina at Chapel Hill, 3202 Murray Hall, 9 Chapel Hill, NC, USA. 10 2Department of Statistics and Operations Research, University of North Carolina at Chapel Hill, 11 318 Hanes Hall, Chapel Hill, NC, USA. 12 3Curriculum for Environment and Ecology, University of North Carolina at Chapel Hill, 3202 13 Murray Hall, Chapel Hill, NC, USA. 14 yCurrent address: Department of Biological Sciences, Old Dominion University, 110 Mills 15 Godwin Life Sciences Building, Norfolk, VA, USA. 16 gCurrent address: Department of Biology, Boston University, 5 Cummington Mall, Boston, MA, 17 USA. 18 *Corresponding author (Email: [email protected]) 19 20 Keywords: Coral reef, calcification, Caribbean, Florida Keys, sclerochronology, climate change, 21 global warming, ocean acidification 22 Paper type: Primary research article 1 bioRxiv preprint doi: https://doi.org/10.1101/310037; this version posted April 28, 2018. -
ATOLL RESEARCH BULLETIN No. 256 CAYS of the BELIZE
ATOLL RESEARCH BULLETIN No. 256 CAYS OF THE BELIZE BARRIER REEF AND LAGOON by D . R. Stoddart, F. R. Fosberg and D. L. Spellman Issued by THE SMlTHSONlAN INSTITUTION Washington, D. C., U.S.A. April 1982 CONTENTS List of Figures List of Plates i i Abstract 1 1. Introduction 2 2. Structure and environment 5 3. Sand cays of the northern barrier reef 9 St George's East Cay Paunch Cay Sergeant' s Cay Curlew Cay Go£ f ' s Cay Seal Cay English Cay Sandbore south of English Cay Samphire Spot Rendezvous Cay Jack's Cays Skiff Sand Cay Glory Tobacco Cay South Water Cay Carrie Bow Cay Curlew Cay 5. Sand cays of the southern barrier reef 23 Silk or Queen Cays North Silk Cay Middle Silk Cay Sauth Silk Cay Samphire Cay Round Cay Pompion Cay Ranguana Cay North Spot Tom Owen's Cay Tom Owen's East Cay Tom Owen's West Cay Cays between Tom Owen's Cays and Northeast Sapodilla Cay The Sapodilla Cays Northeast Sapodilla Cay Frank 's Cays Nicolas Cay Hunting Cay Lime Cay Ragged Cay Seal Cays 5. Cays of the barrier reef lagoon A. The northern lagoon Ambergris Cay Cay Caulker Cay Chapel St George ' s Cay Cays between Cay Chapel and Belize ~ohocay Stake Bank Spanish Lookout Cay Water Cay B. The Southern Triangles Robinson Point Cay Robinson Island Spanish Cay C. Cays of the central lagoon Tobacco Range Coco Plum Cay Man-o '-War Cay Water Range Weewee Cay Cat Cay Lagoon cays between Stewart Cay and Baker's Rendezvous Jack's Cay Buttonwood Cay Trapp 's Cay Cary Cay Bugle Cay Owen Cay Scipio Cay Colson Cay Hatchet Cay Little Water Cay Laughing Bird Cay Placentia Cay Harvest Cay iii D. -
Mission to Recover the Coral Reefs of the Florida Keys
MISSION: ICONIC REEFS Photo: Coral Restoration Foundation Mission to Recover the Coral Reefs of the Florida Keys he iconic coral reefs of the Florida Keys are the foundation of the vibrant regional economy that hosts 5 million visitors per year. North America’s only barrier reef protects the island communities from catastrophic storm surge, while also supporting a world-renowned destination for diving, snorkeling, Tand fishing. However, decades of compounding stress from coral bleaching, coral disease, hurricanes, and high impact human use have significantly degraded the coral reefs. The United States is on the verge of losing a national treasure. Emergency action is required to keep Florida Keys coral reefs from collapsing beyond a point at which they can be restored and protect the economy that depends on them. Restoration Strategy NOAA and partners have developed a bold mission to restore seven ecologically and culturally significant coral reefs within Florida Keys National Marine Sanctuary. The selected restoration sites represent a diversi- ty of habitats, support a range of human uses, span the full geographic range of the Florida Keys, and show a high probability of restoration success. The mission represents one of the largest investments ever under- taken in coral restoration. Informed by years of research, successful trials, and expertise from scientists and restoration practitioners, this effort complements other regional management efforts and will result in resilient and regenerative coral reefs in the Florida Keys. Carysfort Reef Horseshoe Reef Cheeca Rocks Sombrero Reef Newfound Harbor Photo: Ken Nedimyer Looe Key Reef Eastern Dry Rocks www.fisheries.noaa.gov/iconic-reefs Coral reefs are dynamic ecosystems comprised of stony corals, soft corals, sponges, and algae. -
JANUARY 28, 2021 ADDENDUM to NOVEMBER 19, 2019 ICRI MEMBERSHIP LETTER Coral Reef Research and Restoration: an Update on Activities and Accomplishments During 2020
JANUARY 28, 2021 ADDENDUM TO NOVEMBER 19, 2019 ICRI MEMBERSHIP LETTER Coral Reef Research and Restoration: An Update on Activities and Accomplishments during 2020 Summary Mote Marine Laboratory’s Coral Reef Research and Restoration initiatives supports numerous scientists working across multiple disciplines to reverse decades of ecosystem decline, bringing new life and new hope to Coral Reefs around the world. Over the last decade, Specifically, Mote is: • Identifying disease-resistant and climate-resilient corals and using this knowledge to ensure the success of long-term reef restoration efforts • Creating new genetic diversity within coral species through sexual propagation of branching corals and micro-fragmenting of massive corals • Restoring Florida’s Coral Reef through outplanting disease-resistant and climate-resilient corals, bringing degraded reefs back to life with living coral coverage • Preserving genetic diversity for future research, propagation, and restoration by establishing a storm-safe, inland coral gene bank • Expanding capacity to increase coral spawning from once-yearly to year-round through new spawning methods and technology Current coral health and disease research initiatives include: • Identifying resilient corals for restoration by quantifying phenotypic variability to three major stressors: high water temperature, ocean acidification, and disease • Developing methods for the treatment of coral diseases at Virgin Islands National Park, St. John and Buck Island Reef National Monument, St. Croix USVI • Collaborating -
CIMAS 2013 Annual Report
Third Annual Report NOAA Cooperative Agreement NA10OAR4320143 July 1, 2012 – June 30, 2013 Peter B. Ortner, Director David Die, Associate Director UNIVERSITY OF MIAMI ROSENSTIEL SCHOOL OF MARINE AND ATMOSPHERIC SCIENCE TABLE OF CONTENTS I. Executive Summary………………………………………………………………………. 2 II. CIMAS Mission and Organization…………………………………………………….…. 6 III. Personnel………………………………………………………………………………..... 9 IV. Funding………………………………………………………………………………….. 12 V. Research Themes Overview…………………………………………………………….. 17 VI. Research Reports Theme 1: Climate Research Impacts………………………………………………… 20 Theme 2: Tropical Weather…………………………………………………………. 51 Theme 3: Sustained Ocean and Coastal Observations……………………………… 100 Theme 4: Ocean Modeling…………………………………………….……………. 153 Theme 5: Ecosystem Modeling and Forecasting…………………………………… 168 Theme 6: Ecosystem Management…….…………………………………………… 182 Theme 7: Protection and Restoration of Resources………………………………… 200 VII. Education and Outreach………………………………………………………………… 238 VIII. CIMAS Fellows and Executive Advisory Board………………………………………. 250 IX. Awards and Honors……………………………………………………………………... 254 X. Postdoctoral Fellows and Graduate Students…………………………………………… 256 XI. Research Staff…………………………………………………………………………… 257 XII. Visiting Scientist Program……………………………………………………………… 260 XIII Publications ……………………………………………………………………………. 261 1 I. EXECUTIVE SUMMARY The Cooperative Institute for Marine and Atmospheric Studies (CIMAS) is a research institute hosted at the University of Miami (UM) in the Rosenstiel School of Marine and Atmospheric Science -
ATOLL RE3EARCH BULLETIN 9. the Coral Reefs of Urno Atoll., Marshall
ATOLL RE3EARCH BULLETIN ---.. 9. The Coral Reefs of Urno Atoll., Marshall Islands Issued by THE PncIiw SCIENCE EO~D National Academy of Sciences - National Research Council Rashington, D. 2. December 15, 1951 SCIINTIE'IC I>JVF;STIGATI(!NS IN i.iIC1JUPESIA - P:?cii'ic Science bard An atoll. has 8. top tha%'s S1n.t And fe,s.tureless extremely. Corals and. algae make a mat Where mountains are not seemly. John 1. l'ells Cornell University December 1951 The aufJno? of this report participated in the 1950 SIM (Sc-entific Investigations in Micronesj.a) Project of the Pacific Science Board of the National Research Council. This project ties support,ed bf funds granted to the Nstionai 4ca3emy of Sciences the Office of N~valResearch, and the fie16 work was carried 0u.t with the active assistance of the Navy Lie?artment, the Military Air Transport Service, and the officials of the Civil lidminjstrative Staff of the Trust Territory (Navy). To all of the above who helped to make possibie the research described in this report I wish to express sy gratitude and sppreciction. Special thanks are due to Mr. 3onald F'. Squires (Cornell '50) without whose able assistance in the field much less would have been accomplished. Page I F:.elcj, -----.------.---.-------------- 1 A. Reefs ?. B. Lagoon 3A. C. Collections i 11. Stri-ct~reand F'nysical Processes ------ 2 A. (;eneral. Sta terne?.t -- 2 B. Structure of Che Atoll Islands ---- 3 C. Surface Processes 2nd Chacgee ----- 5 D. Reef Types " E. Lanoon Reefs ...................... 0 i P. Corc1 Knolls ---- -.-- 9 ZII.