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11th ICRS Abstract book - Nova Southeastern University

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Poster Mini-Symposium 25: Predicting Reef Futures in the Context of Climate Change<br />

25.1129<br />

High symbiodinium Diversity At High-Latitude Reef Sites – A Means Of Survival<br />

in The Face Of Climate Change?<br />

Laura WICKS 1 , Eugenia SAMPAYO 2 , Jonathan GARDNER 1 , Ove HOEGH-<br />

GULDBERG 3 , Simon DAVY* 1<br />

1 School of Biological Sciences, Victoria <strong>University</strong> of Wellington, Wellington, New<br />

Zealand, 2 Centre for Marine Studies, <strong>University</strong> of Queensland, Brisbane, Australia,<br />

3 Centre for Marine Studies, <strong>University</strong> of Queensland, Brisbane, New Zealand<br />

Little is known about Symbiodinium diversity of high latitude corals systems. These<br />

systems seasonally undergo significant variations in temperature and light, and gaining<br />

insights into symbiont diversity may help us understand how coral-algal associations can<br />

persist in marginal environments. To investigate this, the most common coral species<br />

were sampled from 5-15 m at two high-latitude sites in the South Pacific. In total 5 and<br />

12 host species were examined from the Kermadec Islands (29°S) and Lord Howe Island<br />

(31°S) respectively. Symbiont diversity was characterized using PCR and Denaturing<br />

Gradient Gel Electrophoresis (DGGE) of the ITS2 region. Most corals associated with<br />

clade-C Symbiodinium and symbiont diversity within specific hosts largely overlapped<br />

with that of tropical regions. However, previously unreported sub-cladal symbiont types<br />

were also identified, some of which were highly divergent from those occurring on<br />

nearby tropical locations. Multiple sub-cladal symbiont types were found between<br />

colonies of the same coral species (i.e. Acropora cuneata and Pocillopora damicornis)<br />

and varied both in relation to depth or location, suggesting the presence of<br />

environmentally-specialised symbionts. In conclusion, the common occurrence of<br />

multiple symbiont types within a single host species may represent an adaptive strategy<br />

to survive under the variable environmental conditions occurring at high latitude sites.<br />

Furthermore, the overlap between symbionts in this marginal environment and those<br />

previously studied in tropical reefs may provide an avenue for corals to extend their range<br />

margins, and limit the impacts of climate change.<br />

25.1130<br />

Gis Modeling And Mitigation Of Coral Reef Damage<br />

Richard SNOW* 1 , Mary SNOW 1<br />

1 Applied Aviation Sciences, Embry-Riddle Aeronautical <strong>University</strong>, Daytona Beach, FL<br />

In addition to supplying food and shelter for marine flora and fauna, coral reefs provide<br />

natural barriers as well as tourism and fishing income for coastal communities. However,<br />

a global inventory of Earth’s coral reefs estimates that nearly 60% are at risk, and 90% of<br />

all living reefs have been damaged by coral bleaching. Regionally, the occurrence of<br />

coral bleaching will be the highest in the Caribbean and could take place on an annual<br />

basis over the course of the next 30-50 years. The objective of this study is to<br />

demonstrate that an efficient instrument for conducting surveys and inventories of coral<br />

reefs to assess those ecosystems at higher risk and develop mitigation strategies is<br />

through the use of a Geographic Information System (GIS). Efficient monitoring requires<br />

the assessment of various coastal data baselines and the evaluation of subsequent<br />

alterations in spatial patterns. While monitoring involves real-time components, among<br />

the most powerful tools of a GIS are its modeling capabilities, which allow simulation of<br />

various climate change scenarios. Relevant aspects include changes in coastal land use,<br />

wetlands, and shoreline configuration. Using Caribbean coral reef examples, the results<br />

of this research reveal that GIS techniques and applications play an integral role in<br />

defending coral reefs from climate change and other threats. Planners and politicians<br />

require the ability to analyze risks, assess impacts, and consider alternatives based on<br />

input from researchers across diverse disciplines. GIS provides the collective tool that<br />

integrates multifaceted data and transforms it into a meaningful medium for informed<br />

decision-making.<br />

25.1131<br />

Climate Change Leads: Linking Environmental Analysis To Decision Support<br />

Alessandra SCORE 1 , Eric MIELBRECHT* 2 , Dan WAGNER 3<br />

1 South Florida Program, World Wildlife Fund, Key Largo, FL, 2 Emerald Coast Environmental<br />

Consulting, Washington, DC, 3 Florida Institute of Technology, Melbourne, FL<br />

Climate Change LEADS: Linking Environmental Analysis to Decision Support is an<br />

interdisciplinary initiative that is bringing together scientists, natural resource managers and<br />

decision-makers at the local, state and federal levels, with a full range of stakeholders to analyze<br />

coral resilience to climate change and transform these findings into effective management<br />

strategies. Florida’s stakeholders and decision-makers urgently need targeted research, clear<br />

communications, and powerful tools to better understand the likely impacts of climate change<br />

and coral bleaching so they may develop and implement successful management and mitigation<br />

initiatives. This project is synthesizing existing and emerging scientific data to identify resilient<br />

populations of coral and uncover the key environmental factors that confer this resilience. All<br />

relevant coral bleaching and water quality data for the Florida Keys is being obtained and<br />

transferred into a GIS framework to identify patterns in bleaching occurrence and recovery with<br />

respect to environmental variables such as water quality. These results are being used to create a<br />

tool that will help guide management decisions to better sustain the resilience of this ecosystem<br />

as climate change stresses increase. By involving the community and user groups directly in the<br />

design and implementation of the project and working closely with local partners such as the<br />

Florida Reef Resilience Program (FRRP), the Florida Keys National Marine Sanctuary, the<br />

Florida Department of Environmental Protection, the Nature Conservancy, and a various<br />

Universities , WWF has established a critically-important process for information to flow<br />

between scientists, stakeholders and managers in the region.<br />

25.1132<br />

The Heterogeneity Of Temperature Change And Coral Bleaching During Temperature<br />

Abnormally Warm In Summer 2007<br />

Tung-Yung FAN* 1 , Bing-Je WU 2 , Lee-Shing FANG 3<br />

1 Department of Biology, National Museum of Marine Biology and Aquarium, Pingtung,<br />

Taiwan, 2 National Museum of Marine Biology and Aquarium, Pingtung, Taiwan, 3 Cheng Shiu<br />

<strong>University</strong>, Pingtung, Taiwan<br />

The sea surface temperature in the tropical West-Pacific surrounding Taiwan was abnormally<br />

warm in summer 2007 and caused mass coral bleaching. To test the hypothesis that temperature<br />

and coral bleaching might be different at various sites, the seawater temperature change and<br />

coral bleaching were examined in shallow water (< 10m) of coral reefs at 9 sites around<br />

southern Taiwan and Dongsha island in South China Sea. Censuses completed over 4 months<br />

time frame identified three broad patterns of variation in seawater temperature and coral<br />

bleaching (defined as Type I - III). Type I bleaching occurring at 6 sites where the seawater<br />

temperature exceeded 30 o C and the percentage of coral bleached ranged from 29-60%. Type II<br />

bleaching occurred at 2 sites with the temperature higher than 30 o C, but the percentage of coral<br />

bleached was lower than 5%. Type III bleaching occurred at 1 site with the temperature lower<br />

than 30 o C and corals did not bleach. The three patterns of variation in seawater and coral<br />

bleaching was caused by different effects of geography, as well as upwelling- and typhooninduced<br />

temperature decreasing. The striking spatial variation in seawater temperature and the<br />

extent of mass coral bleaching acted together to create large patches of reef affected by<br />

bleaching that were interspersed with areas that appear relatively unaffected by bleaching. This<br />

pattern may have ecological importance as it suggests that the healthy patches might be capable<br />

of functioning as refugia for coral reefs affected by global warming.<br />

546

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