11th ICRS Abstract book - Nova Southeastern University

More documents

Recommendations

Info

Oral Mini-Symposium 25: Predicting Reef Futures in the Context of Climate Change 25-13 Combined Effects Of Elevated Temperature And Pco2 On The Photo-Physiology Of symbiodinium Spp. in Two Scleractinian Coral Species Andrew BAKER 1 , Paul JONES* 1 , Ranjeet BHAGOOLI 2 , Herman WIRSHING 1 , Tom CAPO 1 , Christopher LANGDON 1 1 Marine Biology and Fisheries, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL, 2 Department of Biosciences, University of Mauritius, Reduit, Mauritius Few studies have investigated how reef corals respond to the combined effects of thermal stress and elevated pCO2, yet these conditions are likely to be an environmental reality of the 21st century. To better understand how these factors interact, we undertook a 14week pilot experiment using two Caribbean coral species, Porites furcata and Montastraea faveolata. We exposed replicate nubbins of each species to three pCO2 levels (360, 550 and 800ppm) and three temperatures (28, 30 and 32oC); conditions were maintained using CO2 bubblers and a computer-controlled heater-chiller system. Additionally, we used an outdoor system and neutral density screens to expose corals to ambient or 50% solar irradiance. Prior to the start of the experiment, coral nubbins were acclimated to different pCO2 levels at ambient temperature (28oC) for four weeks, before being heated at a rate of 0.3oC per day to the experimental temperatures (30 and 32oC). Temperatures were maintained (+/- 0.2oC) for nine weeks before being returned to ambient levels at the same rate. Corals were then monitored for five weeks during a recovery phase. Elevated pCO2 levels were maintained throughout the acclimation, exposure and recovery phases. Every 2-4 weeks chlorophyll fluorescence was analyzed using an Imaging-PAM (Walz, GmbH), and coral tissue samples were taken to determine algal symbiont densities, pigment concentrations, and Symbiodinium identity. Colorscaled photographs documented temporal changes in tissue pigmentation and health. Corals in the highest temperature and light treatments exhibited the most severe bleaching, regardless of CO2 levels. However, at control temperatures (28oC), elevated CO2 resulted in healthier corals, as evidenced by symbiont counts, photographs and fluorescence properties. P. furcata bleached more readily than M. faveolata, although these species also hosted different Symbiodinium. Together, these results suggest temperature and CO2 interact in unexpected ways to influence coral health. 25-14 Ocean Acidification Changes The Early Life History Of Scleractinian Corals. Selina WARD* 1 , Sophie DOVE 2 , david KLINE 2 , kenneth ANTHONY 2 , Ove HOEGH- GULDBERG 1 1 Centre for Marine Studies, The University of Queensland, Brisbane, Australia, 2 Centre for Marine Studies, The University of Queensland, brisbane, Australia Predictions of doubling preindustrial carbon dioxide levels by the middle of this century create serious concerns for the future state of coral reefs. Reproduction and the early life history stages of corals have been shown to be particularly sensitive to adverse conditions. In experiments with four species of acroporid corals, settlement of larvae and early calcification of the newly settled corals were detrimentally affected by seawater with reduced pH. Gametes from these species were collected, fertilised and larvae reared at One Tree Island on the Great Barrier Reef, Australia in spring 2007. Eight thousand Acropora millepora larvae were placed in ambient seawater or sea water of pH 7.8 or 7.6 with preconditioned terracotta tiles for the settlement period. pH was maintained by bubbling carbon dioxide in to the seawater. Settlement success was significantly reduced at pH 7.6 and 7.8 compared to that in ambient seawater. In a separate experiment, larvae of four species were settled on terracotta tiles in ambient seawater. As soon as most of the larvae had metamorphosed, the tiles were scored for the number of larvae that had settled, calcified or were attached but not metamorphosed. Over 16 000 settled corals were used in the experiment. The tiles were then transferred to 250L chambers of either ambient seawater, pH of 7.8 or 7.6 for five days. Tiles were then rescored in a similar manner but stage of calcification was also recorded. Most coral spat in the pH 7.8 and 7.6 treatments did not calcify past the very early stages of calcification in all four species. These results represent crucial information for the future of recruitment on coral reefs. 25-15 Effects Of Climate Change On Coral Reef Algae: Will Algae Be The Winners? Guillermo DIAZ-PULIDO* 1 , Kenneth R.N. ANTHONY 2 , David I. KLINE 2 , Laurence MCCOOK 3 , Selina WARD 2 , Ove HOEGH-GULDBERG 2 , Sophie DOVE 2 1 Centre for Marine Studies and ARC Centre of Excellence for Coral Reef Studies, University of Queensland, Brisbane, St Lucia, Australia, 2 Centre for Marine Studies and ARC Centre of Excellence for Coral Reef Studies, University of Queensland, St Lucia, Brisbane, Australia, 3 Great Barrier Reef Marine Park Authority, Townsville, Australia Climate change predictions imply that intensified levels of thermal bleaching and ocean acidification will lead to increasing rates of coral mortality. A general perception is that such coral reef degradation will result in a phase shift from coral to macroalgal dominance. However, the effects of ocean acidification and warming on tropical coral reef algae have rarely been studied and the vulnerabilities of this key group of organisms to climate change are poorly known. Here we explore the impacts of warming and ocean acidification due to rising atmospheric carbon dioxide emissions on a range of coral reef macroalgae, including crustose coralline algae (CCA) and fleshy macroalgae. We used controlled experimental conditions to simulate acidification and warming scenarios for the Great Barrier Reef, Australia (GBR) in the years 2050 and 2100. Preliminary results from the southern GBR indicate that both groups of benthic algae (calcareous and fleshy) are highly sensitive to climate change. Rates of calcification, photosynthesis, survivorship and recruitment of the CCA Porolithon onkodes were severely reduced with increasing CO2 levels and temperature. Similarly, the fleshy macroalga Lobophora variegata showed a 50% growth reduction under high levels of CO2 and temperature representative of levels predicted for 2100. Further experiments performed on Lizard Island (northern GBR), confirmed that other species of coral reef macroalgae have relatively low temperature thresholds for physiological stress. Our results suggest that the coral reef macroalgae studied are at least as vulnerable to ocean acidification and global warming as are corals. The high vulnerability of CCA is likely to lower the reef’s recovery and cementation capacity, while a reduction in fleshy macroalgae may affect primary productivity with consequences for trophic relations and ecosystem function. 25-16 Climate Change Thresholds And Coral Reef Degradation Kenneth ANTHONY* 1 , Guillermo DIAZ-PULIDO 1 1 Centre for Marine Studies, University of Queensland, St Lucia, Australia The healthy functioning of coral reefs is underpinned by processes operating at organism, population, community and ecosystem levels. Current reef-resilience models provide excellent insight into the role of coral-algae-herbivore interactions. However, predictions of how coral reefs will behave under unprecedented climate conditions require information about stress responses across all organizational levels. Here, we explore coral community responses along gradients of ocean acidification and thermal stress using a new dynamic coral community model parameterized by organism and population responses to climate-change variables from experimental studies. Model runs for years 2050 and 2100 indicate that key framework builders such as crustose coralline algae and Acroporid corals will gradually diminish in reef communities on the Great Barrier Reef. Contrary to general assumptions, transitions from healthy to degraded reefs are not triggered by the exceedence of distinct threshold values, but show a gradual decline to depauperate states. Whether corals will be replaced by macroalgae depends on the physiological responses of the algal species, and model runs based on recent data suggest that shifts to barren rather than algal-dominated reefs are likely outcomes. 231
Oral Mini-Symposium 25: Predicting Reef Futures in the Context of Climate Change 25-17 Climate Change And Reef Development in The Tropical Eastern Pacific Richard ARONSON* 1 , Ian MACINTYRE 2 , Steven VOLLMER 3 , Jennifer HOBBS 4 , Anke MOESINGER 1 1 Dauphin Island Sea Lab, Dauphin Island, AL, 2 Department of Paleobiology, Smithsonian Institution, Washington, DC, 3 Marine Sciences Center, Northeastern University, Nahant, MA, 4 School of Marine and Atmospheric Science, Stony Brook University, Stony Brook, NY Understanding how biotic turnover controls the development of coral reefs will be critical to projecting their future in a rapidly changing world. How well reefs keep up with rising sea level will determine the extent to which they protect adjacent land masses from coastal erosion. In the tropical eastern Pacific, populations of Pocillopora damicornis, the dominant constructor of reef framework, were bleached on a regional scale by the 1982– 83 El Niño event. Subsequent coral mortality and bioerosion suggested that centennialscale recurrences of extreme thermal anomalies associated with the El Niño–Southern Oscillation have slowed accretion rates of eastern Pacific reefs by killing Pocillopora episodically. Off the Pacific coast of Panamá, Pocillopora recovered rapidly after 1983 in some places but not in others. Where it did not recover, the Pocillopora rubble was colonized by another coral species, Psammocora stellata, which is not a frameworkbuilder. Coring studies in the Gulf of Panamá showed that Pocillopora kills and shifts to Psammocora occurred episodically over the past 6000–7000 years; however, Pocillopora growth was suppressed for centuries to millennia, depressing vertical reef accretion for intervals far longer than the return time of strong El Niño events. These protracted intervals of suppressed coral growth can be used to parameterize models of reef accretion under scenarios of biannual to annual coral bleaching, predicted to commence in the next several decades. Oceanic acidification will further inhibit reef accretion, especially in the tropical eastern Pacific where upwelled waters already expose Pocillopora populations to elevated concentrations of dissolved carbon dioxide. 25-18 Fragile Reefs Of The Eastern Pacific: A Model For Reefs in A High Co2 World Derek MANZELLO* 1 , Joanie KLEYPAS 2,3 , David BUDD 4 , Mark EAKIN 5 1 Cooperative Institute for Marine and Atmospheric Studies, Rosenstiel School, University of Miami, Miami, FL, 2 Institute for the Study of Society and Environment, National Center for Atmospheric Research, Boulder, CO, 3 Institute for the Study of Society and Environment, National Center for Atmospheric Research, Boulder, 4 Dept. of Geological Sciences, Univ. of Colorado, Boulder, CO, 5 Coral Reef Watch, NOAA NESDIS, Silver Spring, MD Ocean acidification describes the progressive, global reduction in seawater pH that is currently underway due to the oceanic uptake of increasing atmospheric CO2. Acidification is expected to reduce coral reef calcification and increase reef dissolution, and the relative rates of change will likely be a function of pCO2 (the partial pressure of CO2) in seawater, which is directly proportional to pCO2 in the atmosphere. Little is known about the effects of acidification on syndepositional processes that affect the persistence and preservation of carbonates (i.e., early marine diagenesis). Newly analyzed samples agree with previous studies showing that only trace amounts of inorganic cements occur in modern day coral reefs that exist naturally under low ambient pH in the eastern Tropical Pacific (ETP). The variation in cement abundance and rates of bioerosion between sites in Panamá and Galápagos appears to be related to differences in the saturation state of CaCO3 (Ω); suggesting a link between Ω, inorganic cementation and coral reef development in the ETP. ETP reefs may thus provide a real-world model of coral reef growth in low Ω waters and provide insights into the role of decreasing Ω on reefs beyond the prediction of reduced CaCO3 production. 25-19 Phase Shifts in Coral Reefs – Comparative Investigation Of Corals And Benthic Algae As Ecosystem Engineers Christian WILD* 1 , Andreas HAAS 1 , Malik NAUMANN 1 , Christoph MAYR 2 1 Coral Reef Ecology (CORE) Work Group,GeoBio-Center, Ludwig-Maximilians-Universität München, München, Germany, 2 GeoBio-Center, Ludwig-Maximilians-Universität München, München, Germany Global climate change and direct anthropogenic stress factors do strongly affect the benthic community structure in coral reefs. It is reported from the literature that hermatypic corals are gradually replaced by benthic micro- and macro-algae at many reef locations around the world, a process which is commonly referred to as phase shift. Recent research showed that hermatypic corals via the release of organic matter and concomitant effects on cycles of matter can act as engineers of reef ecosystems. There are strong indications that reef associated benthic algae do also affect reef ecosystem functioning via organic matter release, but all relevant information is lacking. To gain a better understanding of the biogeochemical consequences such phase shifts from corals to algae entail, a series of comparative studies with hermatypic corals and benthic algae were conducted in reefs of the Northern Red Sea during four seasonal expeditions in 2006-2008. These investigations primarily focused on the quantity and quality of the organic matter released by both groups of organisms involving dissolved organic carbon (DOC), particulate organic carbon (POC) and particulate nitrogen (PN). Supplementary mass spectrometric analyses were conducted in order to analyse stable isotope signatures of coral- or algae-derived organic matter. Finally, planktonic and benthic degradation of the respective organic matter were investigated in the field using bottle incubation experiments and stirred benthic chambers, respectively. Our data show clear differences between organic matter release by benthic reef algae or corals for most of the measured parameters, thus, suggest a massive influence of the described phase shifts onto biogeochemical cycles and processes in warm water coral reefs. 25-20 Long-Term, Regional-Scale Patterns in Caribbean Coral Bleaching Responses Allison L. PERRY* 1,2 , Isabelle M. CÔTÉ 3 , John D. REYNOLDS 3 , Andrew R. WATKINSON 4,5 1 WorldFish Center, Bayan Lepas, Penang, Malaysia, 2 School of Biological Sciences, University of East Anglia, Norwich, United Kingdom, 3 Department of Biological Sciences, Simon Fraser University, Burnaby, BC, Canada, 4 School of Environmental Sciences, University of East Anglia, Norwich, United Kingdom, 5 Tyndall Centre for Climate Change Research, Norwich, United Kingdom Coral bleaching is one of the most serious and immediate ecological impacts of climate change, with bleaching events increasing in frequency, severity and extent with rising sea surface temperatures (SSTs). Given the geographically widespread nature of this phenomenon, there is a need to understand patterns and drivers of bleaching over multiple spatial and temporal scales. We take a regional-scale approach, and examine long-term trends in the occurrence of coral bleaching in the Caribbean region, and in the SST anomalies associated with bleaching. Using data over a 24-year period, we assess whether corals may be adjusting to rising temperatures, and examine the regional-scale relationship between the geographic extent of bleaching and rising SST anomalies. At both local and regional scales, there is little evidence to support the possibility that Caribbean reefs are keeping pace with rising sea temperatures, while the geographic extent of bleaching in the region is accelerating with rising sea temperatures even more rapidly than previously known. In combination, our results emphasise the particular vulnerability of reefs to climatic warming. 232
Page 2 and 3:
Contents Sponsors..................
Page 4 and 5:
Sponsors 11th ICRS Co-Sponsors Barr
Page 6 and 7:
Mini-Symposium Co-Chairs Mini-Sympo
Page 8:
Mini-Symposium 23: Reef Management
Page 12 and 13:
Plenary Lessons from the Past Malco
Page 14:
Plenary Drivers of Coral Infectious
Page 18 and 19:
1-1 The R/v Alpha Helix Symbios Exp
Page 20 and 21:
1-9 Coral Community Change Over A C
Page 22 and 23:
1-17 Holocene Reef Development At T
Page 24 and 25:
1-25 Paleoecology Of Mio-Pliocene F
Page 26 and 27:
Oral Mini-Symposium 2: Biotic Respo
Page 28 and 29:
Oral Mini-Symposium 2: Biotic Respo
Page 30 and 31:
Oral Mini-Symposium 3: Calcificatio
Page 32 and 33:
Oral Mini-Symposium 3: Calcificatio
Page 34 and 35:
3-17 The Effect Of Depressed Aragon
Page 36 and 37:
Oral Mini-Symposium 4: Coral Reef O
Page 38 and 39:
Page 40 and 41:
Page 42 and 43:
Page 44 and 45:
Oral Mini-Symposium 5: Functional B
Page 46 and 47:
Page 48 and 49:
Page 50 and 51:
Page 52 and 53:
Page 54 and 55:
Page 56 and 57:
Oral Mini-Symposium 6: Ecological a
Page 58 and 59:
Page 60 and 61:
Page 62 and 63:
Page 64 and 65:
7-5 Coral Yellow Band Disease; Curr
Page 66 and 67:
7-13 Black Band Disease (BBD): A Po
Page 68 and 69:
7-21 Coral Host Processes Associate
Page 70 and 71:
7-29 Can the Presence of Disease Si
Page 72 and 73:
7-37 Developing An Expert System Fo
Page 74 and 75:
7-45 The Effect Of Sediment And Hea
Page 76 and 77:
8-1 From Bacterial Bleaching To The
Page 78 and 79:
8-9 Milkfish Feces Share Common Bac
Page 80 and 81:
8-17 Bacteria Associated With Symbi
Page 82 and 83:
8-26 Photosynthetic Microorganisms
Page 84 and 85:
8-35 Tissue Loss And Tropical Storm
Page 86 and 87:
9-5 Evaluation Of Biotic And Abioti
Page 88 and 89:
9-13 Is Allelopathy Involved in Cor
Page 90 and 91:
Oral Mini-Symposium 10: Ecological
Page 92 and 93:
Page 94 and 95:
Page 96 and 97:
Page 98 and 99:
Page 100 and 101:
10-41 Substrate Effects On Reef Fis
Page 102 and 103:
Page 104 and 105:
Page 106 and 107:
Page 108 and 109:
Oral Mini-Symposium 11: From Molecu
Page 110 and 111:
Page 112 and 113:
Page 114 and 115:
Page 116 and 117:
Page 118 and 119:
12-5 The Contribution Of Heterotrop
Page 120 and 121:
12-14 Ocean Dynamics Drive Coral Re
Page 122 and 123:
12-23 Coral Reef Resilience To Chro
Page 124 and 125:
13-1 Prioritizing Conservation Hots
Page 126 and 127:
Oral Mini-Symposium 13: Evolution a
Page 128 and 129:
14-6 Modelling Coral Larval Dispers
Page 130 and 131:
14-14 Environmentally-Mediated Vari
Page 132 and 133:
14-21 Same, Same, But Different: Co
Page 134 and 135:
14-29 Complex Patterns of Genetic C
Page 136 and 137:
14-37 Genetic Connectivity in Phili
Page 138 and 139:
14-45 Range-Wide Population Genetic
Page 140 and 141:
14-55 The Importance Of Behavior On
Page 142 and 143:
Oral Mini-Symposium 15: Progress in
Page 144 and 145:
Oral Mini-Symposium 15: Progress in
Page 146 and 147:
Oral Mini-Symposium 16: Ecosystem A
Page 148 and 149:
Page 150 and 151:
Page 152 and 153:
Page 154 and 155:
Page 156 and 157:
Page 158 and 159:
Oral Mini-Symposium 17: Emerging Te
Page 160 and 161:
Page 162 and 163:
Page 164 and 165:
Page 166 and 167:
Page 168 and 169:
18-5 Coral Reef Habitat Around New
Page 170 and 171:
18-13 Response Of High Latitude Her
Page 172 and 173:
18-21 Socio-Economic Monitoring (So
Page 174 and 175:
18-29 Extent And Timing Of Disturba
Page 176 and 177:
18-37 It Depends On Where You Look:
Page 178 and 179:
18-45 New Insights Into The Exposur
Page 180 and 181:
Oral Mini-Symposium 19: Biogeochemi
Page 182 and 183:
Page 184 and 185:
Page 186 and 187:
Page 188 and 189:
Oral Mini-Symposium 20: Modeling Co
Page 190 and 191:
Oral Mini-Symposium 20: Modeling Co
Page 192 and 193:
21-9 Integrated Economic Valuation
Page 194 and 195:
21-19 Towards Local Fishers Partici
Page 196 and 197:
21-27 The Political Aspects Of Resi
Page 198 and 199: 21-37 Exploitation And Trade Of Cor
Page 200 and 201: 22-1 Complex Ecological Effects Of
Page 202 and 203: 22-9 Comparative Evaluation Of Reef
Page 204 and 205: 22-17 Managing Fishing Gear To Enco
Page 206 and 207: 22-25 Estimating Harvest Pressure O
Page 208 and 209: 22-33 Are The Coral Reef Finfish Fi
Page 210 and 211: 22-41 Using Length-Frequency Data T
Page 212 and 213: 22-50 Changes in Ecosystem Structur
Page 214 and 215: 23-5 Measuring Success in Managing
Page 216 and 217: 23-13 Some Hints About The Impacts
Page 218 and 219: 23-21 Fishery Management For Artisa
Page 220 and 221: 23-29 “To Live With The Sea”; D
Page 222 and 223: 23-37 Challenges Facing An Mpa Mana
Page 224 and 225: 23-45 Assessing Global Coral Reef M
Page 226 and 227: 23-53 Developing A Model For Ecosys
Page 228 and 229: 23-61 Mitigating The Effects Of Cor
Page 230 and 231: 23-69 Restore Or Not To Restore? Vl
Page 232 and 233: 24-1 Fates Of Restored Acropora Pal
Page 234 and 235: 24-9 Sponge-Mediated Coral Reef Res
Page 236 and 237: 24-17 Coral Community Restorations
Page 238 and 239: 24-25 Development Of A Coral Nurser
Page 240 and 241: 24-33 Transplantation of Porites lu
Page 242 and 243: 24-41 Scleractinian Coral Relocatio
Page 244 and 245: 24-50 Gametogenesis in Cultured Ver
Page 246 and 247: Oral Mini-Symposium 25: Predicting
Page 260 and 261: Oral Mini-Symposium 26: Biodiversit
Page 272 and 273: 26-54 Gene Genealogies Reveal Phylo
Page 276: Poster Session
Page 279 and 280: 1.13 Depth-Related Patterns of Infa
Page 281 and 282: 1.20 Grain Size And Sedimentary Con
Page 283 and 284: 1.3 Environmental Effects On Back-R
Page 285 and 286: Poster Mini-Symposium 2: Biotic Res
Page 287 and 288: Poster Mini-Symposium 3: Calcificat
Page 293 and 294: Poster Mini-Symposium 4: Coral Reef
Page 299 and 300:
Poster Mini-Symposium 4: Coral Reef
Page 301 and 302:
Poster Mini-Symposium 5: Functional
Page 303 and 304:
Page 305 and 306:
Page 307 and 308:
Page 309 and 310:
Page 311 and 312:
Page 313 and 314:
Page 315 and 316:
Page 317 and 318:
Page 319 and 320:
Poster Mini-Symposium 6: Ecological
Page 321 and 322:
7.162 Disease Ecology And Local Pat
Page 323 and 324:
7.170 Coralline Algal Disease in Th
Page 325 and 326:
7.179 Physiological Effects Of Aspe
Page 327 and 328:
7.187 Characterizing Surface Microo
Page 329 and 330:
7.195 How Quickly Does gorgonia Ven
Page 331 and 332:
7.203 Spatial and temporal variabil
Page 333 and 334:
8.210 Quorum Sensing Inhibitory Act
Page 335 and 336:
8.218 Bacterial Communities Associa
Page 337 and 338:
8.226 Bacterial Growth On Coral Muc
Page 339 and 340:
8.234 Functional Diversity of Micro
Page 341 and 342:
8.242 Microbial Community Profile O
Page 343 and 344:
9.248 Chemistry And Ecology Of A Co
Page 345 and 346:
Poster Mini-Symposium 10: Ecologica
Page 347 and 348:
Page 349 and 350:
Page 351 and 352:
Page 353 and 354:
Page 355 and 356:
Page 357 and 358:
Page 359 and 360:
Page 361 and 362:
Page 363 and 364:
Page 365 and 366:
Page 367 and 368:
Page 369 and 370:
Page 371 and 372:
Page 373 and 374:
Page 375 and 376:
Page 377 and 378:
Poster Mini-Symposium 11: From Mole
Page 379 and 380:
Page 381 and 382:
Page 383 and 384:
12.413 Spatial Patterns Of Stony Co
Page 385 and 386:
Poster Mini-Symposium 13: Evolution
Page 387 and 388:
Poster Mini-Symposium 13: Evolution
Page 389 and 390:
14.432 Gene flow of Symbiodinium on
Page 391 and 392:
14.441 Population Genetics Of Spott
Page 393 and 394:
14.449 Mitochondrial Phylogeography
Page 395 and 396:
14.457 Undirect Evidences On The Co
Page 397 and 398:
14.466 South East African, High-Lat
Page 399 and 400:
14.474 Population Genetic Structure
Page 401 and 402:
14.483 Influences Of Wind-Wave Expo
Page 403 and 404:
14.491 Distributions And Diversity
Page 405 and 406:
14.499 Do Mangroves And Seagrass Be
Page 407 and 408:
14.507 Genetic variation of the hyd
Page 409 and 410:
Poster Mini-Symposium 15: Progress
Page 411 and 412:
Poster Mini-Symposium 15: Progress
Page 413 and 414:
Poster Mini-Symposium 16: Ecosystem
Page 415 and 416:
Page 417 and 418:
Page 419 and 420:
Poster Mini-Symposium 17: Emerging
Page 421 and 422:
Page 423 and 424:
Page 425 and 426:
Page 427 and 428:
Page 429 and 430:
Page 431 and 432:
18.599 A Palaeoecological Perspecti
Page 433 and 434:
18.607 Susceptibility Of Corals To
Page 435 and 436:
18.616 Coral Reefs in Costa Rican C
Page 437 and 438:
18.624 Environmental Endocrine Disr
Page 439 and 440:
18.633 Northern Acehnese Coral Reef
Page 441 and 442:
18.641 The Status Of Coral Reefs in
Page 443 and 444:
18.649 The Effects of Increased Sea
Page 445 and 446:
18.658 “Changing Times, Changing
Page 447 and 448:
18.666 Assessing Land Based Inputs
Page 449 and 450:
18.674 Monitoring Of Coral Recovery
Page 451 and 452:
18.682 Seasonal Investigation On St
Page 453 and 454:
18.690 Assessment Of The Coral Reef
Page 455 and 456:
18.698 Distribution Of Seagrasses i
Page 457 and 458:
18.706 Coral Reef Monitoring in the
Page 459 and 460:
18.714 Pacific-Wide Status Of The R
Page 461 and 462:
18.722 Quantitative Underwater Ecol
Page 463 and 464:
18.730 Community Structure Of Reef
Page 465 and 466:
18.738 Morphological Variation In T
Page 467 and 468:
18.746 Decade-Long (1998-2007) Tren
Page 469 and 470:
18.755 Coral Community Composition
Page 471 and 472:
18.763 Changes in Coral Reef Ecosys
Page 473 and 474:
18.771 Bathymetric Distribution Of
Page 475 and 476:
Poster Mini-Symposium 19: Biogeoche
Page 477 and 478:
Page 479 and 480:
Page 481 and 482:
Poster Mini-Symposium 20: Modeling
Page 483 and 484:
21.807 The Recreational Value Of Co
Page 485 and 486:
21.815 Dilemma in Coral Conservatio
Page 487 and 488:
22.821 Estimating Populations Of Tw
Page 489 and 490:
22.829 Commercial Topshell, trochus
Page 491 and 492:
22.837 Trajectories Of Ecosystem Ch
Page 493 and 494:
22.845 Ornamental Fish Trade in The
Page 495 and 496:
22.854 Short-Term Recovery Of Explo
Page 497 and 498:
22.863 Marine Protected Areas: Boon
Page 499 and 500:
22.871 Rotary Time-Lapse Photograph
Page 501 and 502:
22.879 Assessing And Mapping The Di
Page 503 and 504:
22.887 Spatial Variations in Elemen
Page 505 and 506:
23.1004 Coral Reef Conservation Cam
Page 507 and 508:
23.1014 Second And Third Order Mana
Page 509 and 510:
23.1023 Why do Divers Dive Where Th
Page 511 and 512:
23.1031 The Colonial Tunicate tridi
Page 513 and 514:
23.1039 Effectiveness Of A Small Mp
Page 515 and 516:
23.893 Man Made Stress Reliever? An
Page 517 and 518:
23.901 Reef Monitoring Project For
Page 519 and 520:
23.909 Patterns Of Spatial Variabil
Page 521 and 522:
23.917 Culture And Updated Traditio
Page 523 and 524:
23.925 Scientific Monitoring And Cu
Page 525 and 526:
23.934 Characterizing Local Stakeho
Page 527 and 528:
23.942 Challenges in Coral Reef Man
Page 529 and 530:
23.951 Coral Reef-Based Tourism And
Page 531 and 532:
23.959 Marine Protected Area Report
Page 533 and 534:
23.967 Reef Watch Monitoring And Ho
Page 535 and 536:
23.975 A Comparison Of The Permanen
Page 537 and 538:
23.984 Damselfish Embryo Assay: Fie
Page 539 and 540:
23.992 The Decline Of Coral Reef Co
Page 541 and 542:
24.1043 Characteristics Of Seagrass
Page 543 and 544:
24.1051 Mass Culture Of acropora Co
Page 545 and 546:
24.1059 Identifying Sediment-Tolera
Page 547 and 548:
24.1067 Growth Of Newly Settled Ree
Page 549 and 550:
24.1076 Herbivore Effects On Coral
Page 551 and 552:
24.1084 Coral Reefs Conservation Pr
Page 553 and 554:
24.1092 Lessons Learned On Demonstr
Page 555 and 556:
24.1100 Proceedings in Shipgroundin
Page 557 and 558:
24.1108 Restoring An Artificial "En
Page 559 and 560:
24.1116 A Newly Established Coral R
Page 561 and 562:
24.1124 Is The Scale Of Your Coral
Page 563 and 564:
Poster Mini-Symposium 25: Predictin
Page 565 and 566:
Page 567 and 568:
Page 569 and 570:
Page 571 and 572:
Page 573 and 574:
Poster Mini-Symposium 26: Biodivers
Page 575 and 576:
Page 577 and 578:
Page 579 and 580:
Page 581 and 582:
Page 583 and 584:
Page 585 and 586:
Page 587 and 588:
Page 589 and 590:
Page 591 and 592:
Memo ..............................
Page 593 and 594:
Authors INDEX Author Session Page A
Page 595 and 596:
Page 597 and 598:
Page 599 and 600:
Page 601 and 602:
Page 603 and 604:
Page 605 and 606:
Page 607 and 608:
Page 609 and 610:
Page 611 and 612:
Page 613 and 614:
Page 615 and 616:
Page 617 and 618:
Page 619 and 620:
Page 621 and 622:
Page 623 and 624:
Page 625 and 626:
Page 627 and 628:
Page 629 and 630:
Page 631 and 632:
Page 633 and 634:
Page 635 and 636:
Page 637 and 638:
Page 639 and 640:
Page 641 and 642:
Page 643 and 644:
Page 645 and 646:
Page 647 and 648:
show all

11th ICRS Abstract book - Nova Southeastern University

Create successful ePaper yourself

Delete template?

Save as template?