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11th ICRS Abstract book - Nova Southeastern University

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18.603<br />

Sea Urchin Abundance, Distribution And Erosion Along Kuwait’s Coral Island<br />

Reef<br />

Shaker ALHAZEEM 1 , Adel ALSAFFAR 2 , Shaker ALHAZEEM* 2<br />

1 Mariculture and Fisheries Dept. (MFD), Kuwait Institute for Scientific Research (KISR),<br />

Kuwait City, Kuwait, 2 MFD, KISR, Kuwait City, Kuwait<br />

Changes in sea urchin abundance and distribution around three of Kuwait’s coral islands,<br />

Kubbar, Qaru and Umm AlMaradim, in the northern Arabian Gulf, were studied between<br />

2003 and 2004 with particular emphasis on the role and impact of sea urchins in<br />

structuring the coral reef communities. Diver surveys of sea urchin Echinometra mathaei<br />

and Diadema setosum, densities along transects taken at different depths around the reefs<br />

demonstrated no significant differences in density (19.35-33.44 m-2) between 2003 and<br />

2004 or between transect depth, coral reef island, or reef exposure. The highest densities<br />

of E. mathaei (35 mβ) were observed at Umm AlMaradim Island. The distribution and<br />

abundance of E. mathaei and D. setosum around the coral islands suggests they are a<br />

bioindicator of reef health and of environmental stress. The contribution of sea urchins to<br />

bioerosion of the reefs was investigated using cage exclusion and gut evacuation<br />

experiments. Using a gut evacuation experiment grazing rates of E. mathaei were<br />

calculated at 3.84g of coral.sea urchin-1.day-1. The cage exclusion experiment<br />

highlighted the extent of the damage caused by boat anchor and fishing practices around<br />

the 3 reefs.<br />

18.604<br />

Disturbance And Rehabilitation Of Tsunami Impact On Mangrove Forests And<br />

Macrobenthic Communities in Andaman Sea, Thailand<br />

Yoshimi FUJIOKA* 1 , Ryuichi TABUCHI 2 , Yasumasa HIRATA 2 , Reiji YONEDA 2 ,<br />

Pipat PATANAPONPAIBOON 3 , Takuro SHIBUNO* 4 , Hideo OHBA 5<br />

1 National Research Institute of Aquaculture, Minami-ise, Japan, 2 Forestry and Forest<br />

Products Research Institute, Tsukuba, Japan, 3 Chulalongkorn <strong>University</strong>, Bangkok,<br />

Thailand, 4 Seikai National Fisheries Research Institute, Okinawa, Japan, 5 Tokyo<br />

<strong>University</strong> of Marine Science and Technology, Tokyo, Japan<br />

On December 26th, 2004, the impact of tsunami waves caused by an undersea earthquake<br />

off Sumatra Island generated severe damage to artificial constructions and natural<br />

ecosystems especially coral reefs and mangroves on the coastal area of Andaman Sea.<br />

One year before the tsunami disaster, we established permanent survey plots for some<br />

characteristic mangrove forests on the coast of Ranong, Thailand. Since that time, we<br />

have continued to survey mangrove stands and macrobenthic assemblages. Therefore,<br />

this survey became not only to monitor the usual dynamics of mangrove ecosystems but<br />

also to demonstrate the tsunami impact and rehabilitation process after the tsunami.<br />

Damage of mangrove stands were occurred by (1) direct physical destruction by wave<br />

impact and (2) sand settlement on the substratum of mangrove swamp. Three dominant<br />

macrobenthic communities, polychaetes, mollusks and arthropods, on the mangrove<br />

swamps were changed by tsunami; endobenthic organisms such as polychaetes and<br />

bivalves decreased due to be buried in sand, while epibenthic organisms such as<br />

gastropods and crustaceans decreased at once but recovered immediately, and terrestrial<br />

organisms such as insecta increased on dried sandy substratum. On damaged areas,<br />

biomass and diversity of macrobenthos decreased significantly after tsunami.<br />

Poster Mini-Symposium 18: Reef Status and Trends<br />

18.605<br />

Coral Reef Conservation Status In The East Coast Of Peninsular Malaysia<br />

Asami NAKAYAMA* 1 , Ryota NAKAJIMA 1 , LaiPeng FOONG 2 , Rajuddin KUSHARI 3 ,<br />

Victor KUWAHARA 1 , Hideo MIYAGUCHI 1 , Ross OTHMAN 2 , Tatuki TODA 1<br />

1 Soka university, Tokyo, Japan, 2 Universiti Kebangssan Malaysia, Selangor, Malaysia,<br />

3 Universiti Industri Selangor, Selangor, Malaysia<br />

The conservation status of coral reefs was investigated along the east coast of Peninsular<br />

Malaysia in years 2001 and 2007. In 2001, a total of 7 sites from 3 islands were selected for this<br />

investigation; Dalam Bay and Ruang Bay at Perhentian Island; Tulai Reef, Manggo Reef and<br />

Renggis Reef at Tioman Island; Pasir Bay and Rimba Reef at Sibu Island. In 2007, the same<br />

sampling sites were revisited and investigated with additional sites in Batu Tengara and Coral<br />

Garden of Kapas Island, totaling to 9 sites. Estimated coverage of coral communities was<br />

examined by applying quantitative digital image analysis to the line transect method. In 2001,<br />

three coral community types were characterized by dominant genera and lifeforms: Montipora-<br />

Acropora community, Acropora branching community and Heliopora community. Among<br />

them, the most dominant coral community in the east coast was Montipora-Acropora<br />

community. Dalam Bay in Perhentian Island showed the highest community diversity at 19<br />

coral genera, while Renggis Reef in Tioman Island had the lowest at 9 genera. Live coral<br />

coverage in study sites ranged from 21% to 69%. Most reefs were in ″good″ or ″fair″ condition<br />

while some reefs were shown to be in ″poor″ condition following the criterion of Gomez et al.<br />

(1994). The coral conservation status of year 2001 and 2007 in the east coast of Peninsular<br />

Malaysia is compared, and changes in the reef community and effect of human activity on the<br />

coral community between 2001 and 2007 are discussed.<br />

18.606<br />

The Distribution Of Coral, Reefs And Coastal Habitats in North Central Cuba<br />

Aisling BRADY* 1 , Sharon COWLING 1<br />

1 Geography, <strong>University</strong> of Toronto, Toronto, ON, Canada<br />

A coastal causeway connecting Cayo Coco to Cayo Guillermo in Ciego d’Avila, Cuba, has not<br />

only transformed the tourism industry in this region, but has also produced new reef habitats.<br />

Scleractinian coral communities have begun to form under small inlet-style bridges along the<br />

causeway, surrounded by seagrass beds, mangroves and natural reefs. To identify the role of<br />

these bridge reefs in the ecological functioning of the Cayo Coco-Guillermo reef tract, we need<br />

to understand how these bridge reefs formed and characterize their attributes relative to<br />

surrounding communities. A combination of ecological observations and δ13 carbon isotopes<br />

were collected from the bridges and surrounding reef communities, mangrove channels and<br />

Thalassia patches. Detrended Correspondence Analysis and Canonical Correspondence<br />

Analysis were carried out to group which physical attributes contributed to the coral<br />

communities in the bridge reefs and also which habitats the bridge reefs were most similar to,<br />

with respect to coral and benthos composition. δ 13 C was used as a tracer in the bridges,<br />

marking where organic sediment originated from, and how their origins changed in surrounding<br />

habitats. Coral assemblages at bridge reefs resembled communities in surrounding patch reefs<br />

and mangrove channels, while benthic coverage at bridge sites was most similar to mangrove<br />

channels, suggesting the inflow of water through mangroves during high tides played a role in<br />

shaping the substrate of the bridge reefs. Of the physical attributes measured, depth, current<br />

speed and turbidity gradients were considered the most important environmental factors<br />

influencing coral communities. By understanding how these bridge reefs formed,<br />

recommendations can be made for recreating ecologically similar conditions during future<br />

development of surrounding cays, while results also contribute to growing inventories of<br />

benthic communities in North Central Cuba.<br />

415

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