11th ICRS Abstract book - Nova Southeastern University

11th ICRS Abstract book - Nova Southeastern University 11th ICRS Abstract book - Nova Southeastern University

24.12.2012 Views

18.702 Evidence Of An Outbreak Of Crown-Of-Thorns Starfish (Cots) in French Polynesia: Observations Between 2005 And 2007 Bernard SALVAT* 1 , Yannick CHANCERELLE 2 , Thierry LISON DE LOMA 2 , Lucie PENIN 1 , Céline STIEVENART 1 , Franck LEROUVREUR 2 , Annie AUBANEL 3 , Christian MONIER 4 , Elodie LAGOUY 5 , Mehdi ADJEROUD 1 1 Biologie et Ecologie Tropicale et Méditerranéenne, Université de Perpignan, Ecole Pratique des Hautes Etudes, UMR 5244 CNRS-EPHE-UPVD, Perpignan, France, 2 Centre de Recherches Insulaires et Observatoire de l'Environnement, Moorea, French Polynesia, 3 Serive de l'Urbanisme IFRECOR, Tahiti, French Polynesia, 4 Service de la Pêche, Tahiti, French Polynesia, 5 Reef Check Polynésie, Moorea, French Polynesia Outbreaks of Acanthaster planci (COTS) in French Polynesia were observed in 1969 and between 1980-1984 where concentrations as high as 110 ind/hectare were observed at Tahiti and Moorea in 1984. Subsequently, outer reef slopes have recovered their preoutbreak percentage coral cover. According to a general survey carried out at the end of 2006, COTS have increased in abundance on islands of both the Society (Tahiti, Moorea, Bora Bora, Raiatea, Huahine) and the Austral archipelagos (Rurutu), but not for the Tuamotu atolls (Manihi, Rangiroa, Tikehau, Fakarava). In order to evaluate the distribution and abundance of COTS at an island scale, a « manta tow » was developed to survey the outer reef slope along the 95 km perimeter of Moorea. This method consists of evaluating feeding marks and after establishing the correlation between feeding marks and COTS abundance, the density of COTS is calculated. Results from 2006-2007 show a mosaic distribution of COTS around Moorea. The outer slope of Moorea, between 10 and 30 m in depth was divided into sectors 250 m long, parallel with the reef crest. Only a few sectors (10 out of 395), mainly on the North and East coasts, show COTS concentrations above 17 ind, which is lower than in 1984. Other sectors show lower concentrations, of which 117 sectors had less than 2 COTS. A comparison of COTS densities between November 2006 and April 2007 does not indicate that the COTS outbreak is progressing. Nevertheless on some sectors with COTS, coral cover, mainly Acropora and Pocillopora, has been reduced by up to 50 %. Future surveys are planned to monitor this event and its consequences. 18.703 Status Of Shallow Water Coral Communities in Little Cayman in 2006-2007 Lindsay HUEBNER* 1 , Carey BATHA 1 , Max MULLEN 1 , Roy DUCOTE 1 , Vania COELHO 1,2 1 Central Caribbean Marine Institute, North Coast Road, Cayman Islands, 2 Natural Sciences and Math, Dominican University of California, San Rafael This study focuses on a comparative analysis of the coral populations in shallow water reefs (1-2 m deep) of Little Cayman, Cayman Islands, in 2006 and 2007. The purpose of this comparison is to understand the temporal dynamics of shallow reef coral communities and analyze the possible influence of the proximity to no-take reserves located in deeper reefs. We conducted surveys of 4 fringing reefs on the north and south sides of Little Cayman, near and far from marine no-take zones located in deeper water (9-15m). Live coral cover, coral diversity, disease, bleaching, mortality, diameter and height were measured of colonies found under 10 m line transects randomly placed on the reefs. We also recorded fish bites and sponge and tunicate overgrowth on corals. A total of 36 and 75 transects, and 458 and 553 corals were analyzed in 2006 and 2007 respectively. We found a statistically significant decline in live coral cover, from 14.8 to 9.5%, a small but significant decrease in mortality from 33.1 to 28.3%, and an increase in sponge overgrowth from 0 to 1.5%. Mean diameter and height were similar over time (~ 36 cm and 18 cm, respectively). No significant differences were observed for bleaching (~3%), disease (~0.5%), fish bites (~0.3%) or tunicate overgrowth (none), however partial bleaching was more common in 2007. No main change in relative abundance of coral genera composition was observed, with Porites being the most abundant genus (~ 40% of the corals). Distance from marine no-take reserves had no distinguishable effect on the parameters analyzed in this study. Poster Mini-Symposium 18: Reef Status and Trends 18.704 Algal Cover And Coral Recruitment in Shallow Reefs in Little Cayman in 2006-2007 Lindsay HUEBNER* 1 , Carey BATHA 1 , Max MULLEN 1 , Roy DUCOTE 1 , Vania COELHO 1,2 1 Central Caribbean Marine Institute, North Coast Road, Cayman Islands, 2 Natural Sciences and Math, Dominican University of California, San Rafael In this study we analyzed algal cover and coral recruitment in shallow water reefs around Little Cayman, Cayman Islands, in 2006 and 2007. We also examined if marine no-take zones had an influence on adjacent shallow water sites (1-2 m deep) regarding upright (fleshy and calcareous) and encrusting calcareous algal cover, as well as coral recruitment. We conducted surveys of 4 fringing reefs (1-2 m) on the north and south sides of Little Cayman, near and far from marine no-take zones located in deeper water (9-15 m). Ten meter long line transects were randomly placed on the reef, and algal cover and number of coral recruits were recorded in quadrats 25 x 25 cm placed every other meter along the transects. In addition, the number of damselfish and Diadema found 0.5 meter from the transect line was also noted. A total of 36 and 75 transects, and 180 and 375 quadrats were analyzed in 2006 and 2007 respectively. From 2006 to 2007, there was a significant decrease in fleshy upright macroalgal cover from 17.2 to 12.1% and an increase in upright calcareous macroalgal cover from 5.0 to 7.0%. No other statistically significant changes were observed. From one year to the next mean encrusting calcareous algal cover varied from 9.1 to 5.6%, total upright macroalgal cover from 22.2 to 20.4%, number of recruits from 0.04 to 0.09 per quadrat, Diadema from 2.3 to 1.8 per transect, and damselfish from 2.6 to 3.2 per transect. Proximity to no-take zones had no clear effect on the parameters analyzed during the study period. 18.705 Spatial And Temporal Recovery Patterns Of Coral Reefs Within The Gulf Of Oman (Uae) Following The 2007 Cyclone Disturbance Kristi FOSTER* 1 1 National Coral Reef Institute, Nova Southeastern University, Dania Beach, FL In June 2007 Cyclone Gonu, the most powerful storm in the region in 60 years, impacted reefs in the United Arab Emirates along the Gulf of Oman coastline. The extent of destruction of the reef corals varied considerably depending on site, taxa and colony morphology. The most severely damaged sites were completely razed. These included areas that had been dominated by tabular Acropora clathrata, some larger than 2m in diameter. Moderately damaged sites included areas of dense monospecific stands of Pocillopora damicornis from which individual colonies were dislodged or broken. The least damaged sites included areas with massive colonies of Platygyra and Favia spp. that survived relatively unscathed, showing little or no signs of scouring or partial mortality. This study describes quantitatively the first stage of recovery of these reefs, two months and twelve months following the cyclone disturbance. Monitoring stations have been installed near Dibba and Fujairah along the northern and southern sections of the UAE coastline, respectively. Each station consists of two primary components; (i) transect markers that create a “Mercedes star” pattern for repetitive photographic surveys along three 10m2 rays, and (ii) a settlement plate rack with horizontal and vertical limestone tiles. Analyses of the transect photographs provide spatial and temporal comparisons such as coral area cover, colony size frequency distributions and colony growth rates. Examination of the settlement plates indicates coral larvae recruitment into the area, which may also indicate future shifts in community structure. Site data such as hourly seawater temperatures measured approximately 0.5m above the reef, sea urchin densities, and rugosity (topographic complexity) are evaluated in relation to the spatial and temporal patterns. While this study focuses on the short-term recovery of these reefs, future studies may continue to track their long-term progression at the permanent monitoring stations. 439

18.706 Coral Reef Monitoring in the OECS and Tobago Marcia CREARY* 1 , Joseph MCGANN 2 1 Centre for Marine Sciences, University of the West Indies, Kingston 7, Jamaica, 2 MACC Project, Belmopan City, Belize The objectives of this project was to expand the coral reef monitoring programme started under the CPACC (Caribbean Planning for Global Climate Change) Project to the countries of the Eastern Caribbean. The Centre for Marine Sciences (CMS) of the University of the West Indies (UWI) Jamaica was contracted by the MACC (Mainstreaming Adaptation to Climate Change) Project to oversee this process. Sixteen participants from seven Eastern Caribbean countries (Antigua, Dominica, Grenada, St Kitts and Nevis, St Lucia, St Vincent and Tobago) were trained in coral reef monitoring, using the video monitoring protocol developed under CPACC, in St Lucia during September 2007. Following the training, each country selected a monitoring site and monitoring was conducted (during the period September to November 2007) at these sites under the supervision of resources persons from the CMS. The videotapes were processed and the data are being analysed at the CMS. This paper will discuss the results of the monitoring exercise for each of the seven countries with reference to the recommendations coming out of the CPACC pilot phase. The paper will go further to highlight the challenges encountered in establishing a regional monitoring programme that meets the needs of the participating countries and will make recommendations on how to use the lesson learnt to ensure country buy-in and continuity. 18.707 Recovery And Current Status Of Coral Reefs Of The Gulf Of Mannar, Southeastern India Edward JK PATTERSON* 1 , G. MATHEWS 1 , Jamila PATTERSON 1 , Jerker TAMELANDER 2 , Dan WILHELMSSON 3 , Olof LINDEN 4 1 Suganthi Devadason Marine Research Institute, Tuticorin, India, 2 IUCN Global Marine Programme, Dar es salaam, Tanzania, 3 Stockholm University, Stockholm, Sweden, 4 International Maritime Organization, World Maritime University, Malmo, Sweden The Gulf of Mannar (GoM) is one of the four major reef areas in India, located on the mainland Southeastern coast and encompassing coral reefs around 21 uninhabited islands. Surveys in 2003-2005, and during March and November 2007 were carried out to assess reef status and trends and population structure. An increase in mean live coral cover from 36.98±13.12% to 41.11±11.62% was observed possibly due to a reduction in human disturbance in the area, in particular a complete halt to coral mining, in combination with high recruitment rates. Montipora sp. dominated the assemblages of recruits, with a mean recruit density of 1.98±0.43 per m2 followed by Acropora sp. (1.77±0.25 per m2). Other common genera among the recruits included Pocillopora sp., Echinopora sp., Porites sp., Favia sp., Favites sp., Pavona sp., Merulina sp., and Hydnopora sp. The new recruits represented 6 families and 10 genera. The recruit size class data was derived from very short time series, but fast growth in species such as Pocillopora sp., Montipora sp. and Acropora sp. was evidenced by a shift of cohorts from smaller to larger size classes, e.g. the percentage of recruits in the 0-5 cm size class went from 64.11 in March to 37.23 in November, while share of recruits in the 6-10 cm size class increased from 32.55% to 51.02%; 11-20 cm from 3.37% to 10.71%; and 21-40 cm from 0% to 1.04%. Although a significant increase in live coral cover on the reefs was indicated, efforts have to be taken to manage the reefs in GoM from compounded threats of direct local stress and climate change. Poster Mini-Symposium 18: Reef Status and Trends 18.708 The Effects Of 2004 Tsunami On Seaweed And Seagrass Community in The Inter-Tidal Rocky Shore And Shallow Sub-Tidal Coral Reefs Anchana PRATHEP* 1 , Piyalap TUNTIPRAPAS 1 , Anuchit DARAKRAI 1 , Pimonrat THONGROY 1 , Jaruwan MAYAKUN 1 , Bongkot WICHACHUCHERD 1 , Sutinee SINUTOK 1 1 Department of Biology, Prince of Songkla Unviersity, HatYai, Thailand, HatYai, Thailand The 26th December, 2004 tsunami hit 6 Andaman provinces in southern Thailand, caused great damage to life, property and coastal resources. Here we examined the effect of tsunami on seaweed and seagrass biodiversity at 2 sites: 1) Talibong island, Trang province and 2) Sirinart Marine National Park, Phuket province. These two study sites are monitored by seaweeds and seagrass research unit, Prince of Songkla University for over 3 years, thus the baseline data before the tsunami are provided. At Talibong island , fifteen of 50 cm x 50 cm quadrats were mapped and monitored in the shallow sub-tidal coral community, seaweed diversity and abundance in each plot were investigated. While, Ten of line transects were used to investigate diversity and distribution of seaweeds and seagrasses at Sirinart Marine National Park, an intertidal habitat. These dataset would allow us to assess the effects of tsunami on diversity, percentage cover of seaweed and seagrass before and after the tsunami; and the effects of the tsunami on the different sites. The results showed that diversity and percentage cover of seaweeds and seagrasses dropped by 50% after the tsunami at both sites. There were differences in the effect of tsunami on seaweed and seagrass species, depending on morphology and structure. Seagrass could recover after a few months after the tsunami, while seaweeds have not recovered yet after two years of tsunami catastrophe. We also reported the status of nearby coral reefs community, which hit by the tsunami, some of which were badly effected and showed no recovery yet. 18.709 Change And Resilience At Stetson Bank, A High Latitude Coral Community in The Gulf Of Mexico George SCHMAHL* 1 , Jennifer DEBOSE 1 , Emma HICKERSON 1 1 NOAA, Flower Garden Banks National Marine Sanctuary, Galveston, TX Stetson Bank, located near 28.2° N, 94.3° W in the northwestern Gulf of Mexico, 70 miles offshore of Galveston, Texas, is an uplifted claystone feature associated with an underlying salt dome. Rising from surrounding water depths of over 180 feet, Stetson Bank crests within 50 to 80 feet of the surface. Due to the influence of the warm, clear waters of the Gulf Stream loop current, Stetson Bank supports a well-developed benthic community comprised of tropical marine sponges, coral and other invertebrates. Living coral cover can comprise up to 30% of the reef surface. The predominant species is the hydrozoan Millepora alcicornis (fire coral), although eleven other species of hermatypic corals have been documented. Sponges, primarily Chondrilla nucula, Ircinia strobilina, and Agelas clathrodes, comprise up to another 30% of the substrate. A long-term monitoring program was initiated in 1993 consisting of over 60 permanently marked stations on the reef surface that are photographed annually and analyzed for changes in community structure and benthic cover. Until 2005, the benthic community of Stetson Bank showed remarkable stability. However, in the summer of 2005, significant mortality of coral was documented in association with a major bleaching event in the Gulf of Mexico. In addition, the area was subject to significant coastal runoff resulting from two major hurricanes (Katrina and Rita). The living cover of fire coral at Stetson Bank was significantly reduced as a result of these impacts. Sponges were not significantly affected. Surprisingly, by 2007, coral cover had substantially recovered. The resiliency demonstrated at Stetson Bank is hypothesized to be due to its offshore location, relative stability of most environmental factors, and depth. Although subjected to similar water temperature regimes in previous years, the synergistic effect of both coastal runoff and elevated temperature may have contributed to mortality in 2005. 440

18.702<br />

Evidence Of An Outbreak Of Crown-Of-Thorns Starfish (Cots) in French<br />

Polynesia: Observations Between 2005 And 2007<br />

Bernard SALVAT* 1 , Yannick CHANCERELLE 2 , Thierry LISON DE LOMA 2 , Lucie<br />

PENIN 1 , Céline STIEVENART 1 , Franck LEROUVREUR 2 , Annie AUBANEL 3 ,<br />

Christian MONIER 4 , Elodie LAGOUY 5 , Mehdi ADJEROUD 1<br />

1 Biologie et Ecologie Tropicale et Méditerranéenne, Université de Perpignan, Ecole<br />

Pratique des Hautes Etudes, UMR 5244 CNRS-EPHE-UPVD, Perpignan, France, 2 Centre<br />

de Recherches Insulaires et Observatoire de l'Environnement, Moorea, French Polynesia,<br />

3 Serive de l'Urbanisme IFRECOR, Tahiti, French Polynesia, 4 Service de la Pêche, Tahiti,<br />

French Polynesia, 5 Reef Check Polynésie, Moorea, French Polynesia<br />

Outbreaks of Acanthaster planci (COTS) in French Polynesia were observed in 1969 and<br />

between 1980-1984 where concentrations as high as 110 ind/hectare were observed at<br />

Tahiti and Moorea in 1984. Subsequently, outer reef slopes have recovered their preoutbreak<br />

percentage coral cover. According to a general survey carried out at the end of<br />

2006, COTS have increased in abundance on islands of both the Society (Tahiti, Moorea,<br />

Bora Bora, Raiatea, Huahine) and the Austral archipelagos (Rurutu), but not for the<br />

Tuamotu atolls (Manihi, Rangiroa, Tikehau, Fakarava). In order to evaluate the<br />

distribution and abundance of COTS at an island scale, a « manta tow » was developed to<br />

survey the outer reef slope along the 95 km perimeter of Moorea. This method consists of<br />

evaluating feeding marks and after establishing the correlation between feeding marks<br />

and COTS abundance, the density of COTS is calculated. Results from 2006-2007 show<br />

a mosaic distribution of COTS around Moorea. The outer slope of Moorea, between 10<br />

and 30 m in depth was divided into sectors 250 m long, parallel with the reef crest. Only<br />

a few sectors (10 out of 395), mainly on the North and East coasts, show COTS<br />

concentrations above 17 ind, which is lower than in 1984. Other sectors show lower<br />

concentrations, of which 117 sectors had less than 2 COTS. A comparison of COTS<br />

densities between November 2006 and April 2007 does not indicate that the COTS<br />

outbreak is progressing. Nevertheless on some sectors with COTS, coral cover, mainly<br />

Acropora and Pocillopora, has been reduced by up to 50 %. Future surveys are planned<br />

to monitor this event and its consequences.<br />

18.703<br />

Status Of Shallow Water Coral Communities in Little Cayman in 2006-2007<br />

Lindsay HUEBNER* 1 , Carey BATHA 1 , Max MULLEN 1 , Roy DUCOTE 1 , Vania<br />

COELHO 1,2<br />

1 Central Caribbean Marine Institute, North Coast Road, Cayman Islands, 2 Natural<br />

Sciences and Math, Dominican <strong>University</strong> of California, San Rafael<br />

This study focuses on a comparative analysis of the coral populations in shallow water<br />

reefs (1-2 m deep) of Little Cayman, Cayman Islands, in 2006 and 2007. The purpose of<br />

this comparison is to understand the temporal dynamics of shallow reef coral<br />

communities and analyze the possible influence of the proximity to no-take reserves<br />

located in deeper reefs. We conducted surveys of 4 fringing reefs on the north and south<br />

sides of Little Cayman, near and far from marine no-take zones located in deeper water<br />

(9-15m). Live coral cover, coral diversity, disease, bleaching, mortality, diameter and<br />

height were measured of colonies found under 10 m line transects randomly placed on the<br />

reefs. We also recorded fish bites and sponge and tunicate overgrowth on corals. A total<br />

of 36 and 75 transects, and 458 and 553 corals were analyzed in 2006 and 2007<br />

respectively. We found a statistically significant decline in live coral cover, from 14.8 to<br />

9.5%, a small but significant decrease in mortality from 33.1 to 28.3%, and an increase in<br />

sponge overgrowth from 0 to 1.5%. Mean diameter and height were similar over time (~<br />

36 cm and 18 cm, respectively). No significant differences were observed for bleaching<br />

(~3%), disease (~0.5%), fish bites (~0.3%) or tunicate overgrowth (none), however<br />

partial bleaching was more common in 2007. No main change in relative abundance of<br />

coral genera composition was observed, with Porites being the most abundant genus (~<br />

40% of the corals). Distance from marine no-take reserves had no distinguishable effect<br />

on the parameters analyzed in this study.<br />

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

18.704<br />

Algal Cover And Coral Recruitment in Shallow Reefs in Little Cayman in 2006-2007<br />

Lindsay HUEBNER* 1 , Carey BATHA 1 , Max MULLEN 1 , Roy DUCOTE 1 , Vania COELHO 1,2<br />

1 Central Caribbean Marine Institute, North Coast Road, Cayman Islands, 2 Natural Sciences and<br />

Math, Dominican <strong>University</strong> of California, San Rafael<br />

In this study we analyzed algal cover and coral recruitment in shallow water reefs around Little<br />

Cayman, Cayman Islands, in 2006 and 2007. We also examined if marine no-take zones had an<br />

influence on adjacent shallow water sites (1-2 m deep) regarding upright (fleshy and calcareous)<br />

and encrusting calcareous algal cover, as well as coral recruitment. We conducted surveys of 4<br />

fringing reefs (1-2 m) on the north and south sides of Little Cayman, near and far from marine<br />

no-take zones located in deeper water (9-15 m). Ten meter long line transects were randomly<br />

placed on the reef, and algal cover and number of coral recruits were recorded in quadrats 25 x<br />

25 cm placed every other meter along the transects. In addition, the number of damselfish and<br />

Diadema found 0.5 meter from the transect line was also noted. A total of 36 and 75 transects,<br />

and 180 and 375 quadrats were analyzed in 2006 and 2007 respectively. From 2006 to 2007,<br />

there was a significant decrease in fleshy upright macroalgal cover from 17.2 to 12.1% and an<br />

increase in upright calcareous macroalgal cover from 5.0 to 7.0%. No other statistically<br />

significant changes were observed. From one year to the next mean encrusting calcareous algal<br />

cover varied from 9.1 to 5.6%, total upright macroalgal cover from 22.2 to 20.4%, number of<br />

recruits from 0.04 to 0.09 per quadrat, Diadema from 2.3 to 1.8 per transect, and damselfish<br />

from 2.6 to 3.2 per transect. Proximity to no-take zones had no clear effect on the parameters<br />

analyzed during the study period.<br />

18.705<br />

Spatial And Temporal Recovery Patterns Of Coral Reefs Within The Gulf Of Oman (Uae)<br />

Following The 2007 Cyclone Disturbance<br />

Kristi FOSTER* 1<br />

1 National Coral Reef Institute, <strong>Nova</strong> <strong>Southeastern</strong> <strong>University</strong>, Dania Beach, FL<br />

In June 2007 Cyclone Gonu, the most powerful storm in the region in 60 years, impacted reefs<br />

in the United Arab Emirates along the Gulf of Oman coastline. The extent of destruction of the<br />

reef corals varied considerably depending on site, taxa and colony morphology. The most<br />

severely damaged sites were completely razed. These included areas that had been dominated<br />

by tabular Acropora clathrata, some larger than 2m in diameter. Moderately damaged sites<br />

included areas of dense monospecific stands of Pocillopora damicornis from which individual<br />

colonies were dislodged or broken. The least damaged sites included areas with massive<br />

colonies of Platygyra and Favia spp. that survived relatively unscathed, showing little or no<br />

signs of scouring or partial mortality. This study describes quantitatively the first stage of<br />

recovery of these reefs, two months and twelve months following the cyclone disturbance.<br />

Monitoring stations have been installed near Dibba and Fujairah along the northern and<br />

southern sections of the UAE coastline, respectively. Each station consists of two primary<br />

components; (i) transect markers that create a “Mercedes star” pattern for repetitive<br />

photographic surveys along three 10m2 rays, and (ii) a settlement plate rack with horizontal and<br />

vertical limestone tiles. Analyses of the transect photographs provide spatial and temporal<br />

comparisons such as coral area cover, colony size frequency distributions and colony growth<br />

rates. Examination of the settlement plates indicates coral larvae recruitment into the area,<br />

which may also indicate future shifts in community structure. Site data such as hourly seawater<br />

temperatures measured approximately 0.5m above the reef, sea urchin densities, and rugosity<br />

(topographic complexity) are evaluated in relation to the spatial and temporal patterns. While<br />

this study focuses on the short-term recovery of these reefs, future studies may continue to track<br />

their long-term progression at the permanent monitoring stations.<br />

439

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