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11th ICRS Abstract book - Nova Southeastern University

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Poster Mini-Symposium 10: Ecological Processes on Today's Reef Ecosystems<br />

10.359<br />

Population Projections And Management Recommendations For The Threatened<br />

acropora Palmata: What Life History Stage Should We Protect?<br />

Tali VARDI* 1 , Dana E. WILLIAMS 2,3<br />

1 Scripps Institution of Oceanography, La Jolla, CA, 2 Cooperative Institute for Marine and<br />

Atmospheric Studies, <strong>University</strong> of Miami RSMAS, Miami, FL, 3 Southeast Fisheries<br />

Science Center, NOAA Fisheries, Miami<br />

Acropora palmata was once the dominant hermatypic coral throughout the Caribbean,<br />

Florida, and Bahamas. Since the 1980s it has suffered a 97% decline in abundance<br />

throughout its range and was included on the US Endangered Species List in 2006.<br />

Despite the dramatic nature of this decline, and the implications a potential extinction<br />

would have for loss of habitat to other species, neither abundance nor rates of decline<br />

have been documented systematically throughout the Caribbean. In Autumn 2007,<br />

abundance of A. palmata was estimated in Florida, Puerto Rico, Jamaica, Virgin Gorda,<br />

and Curaçao. Abundance in Florida was dramatically lower than in other sites. Causes of<br />

the rarity of A. palmata in Florida have not been clearly identified. To explore<br />

population changes in more detail, a size-based population model was developed to help<br />

identify life history stages most affected. Based on A. palmata’s population trajectory<br />

since 2004, as measured by a standardized, size-based demographic monitoring protocol<br />

in the Florida Keys, the local population will reach a stable distribution in 20 years. At<br />

that time, the current population structure, in which 35% are pre-reproductive and 45%<br />

are reproductive, will have become dominated by pre-reproductive individuals with only<br />

20% of colonies capable of sexual reproduction. This loss of large individuals would also<br />

reduce the number of asexually derived fragments, leading to an overall reduction in<br />

abundance of colonies in Florida. Parallel research on the island of Curacao shows both a<br />

greater abundance of A. palmata overall and no significant change in the relative<br />

abundance of larger individuals. These results suggest that protecting the largest adults<br />

may reverse the current trend toward a left-skewed A. palmata population structure in<br />

Florida.<br />

10.360<br />

Top-Down Factors Explain Benthic Community Structure On A Near-Pristine<br />

Coral Reef Ecosystem<br />

Kimberly PAGE-ALBINS* 1 , Peter VROOM 2 , Celia SMITH 3 , Edward DEMARTINI 4 ,<br />

Scott GODWIN 5<br />

1 Zoology, Oregon State <strong>University</strong>, Corvallis, OR, 2 Joint Institute for Marine and<br />

Atmospheric Research, Honolulu, HI, 3 Department of Botany, <strong>University</strong> of Hawaii at<br />

Manoa, Honolulu, HI, 4 Coral Reef Ecosystem Division, NOAA Fisheries, Honolulu, HI,<br />

5 Hawaii Institute of Marine Biology, Kaneohe, HI<br />

The debate continues over the relative contributions of top-down mechanisms such as<br />

removal of herbivores, and bottom-up mechanisms such as eutrophication, to coral reef<br />

decline and phase shifts from coral to algal dominated reefs. While it is likely that both<br />

of these mechanisms influence coral reef community composition, the dominant<br />

mechanism regulating a particular community is likely determined, in part, by the level of<br />

anthropogenic impact present. In order to effectively manage remaining intact reef<br />

systems, it has become increasingly important to pinpoint which factors regulate the<br />

composition of coral reef communities. Here, we examine models of top-down and<br />

bottom-up community regulation in a near-pristine coral reef system, Pearl and Hermes<br />

Atoll (PHA), Northwestern Hawaiian Islands. PHA represents one end of a continuum in<br />

coral reef health. Percent cover of benthic organisms along with herbivorous fish density<br />

and biomass, urchin density, and nutrient availability were measured. Multi-linear<br />

regressions revealed that for each of the benthic functional groups examined (coral,<br />

frondose macroalgae, crustose coralline red algae, and turf algae) herbivorous fish<br />

density was a significant explanatory factor. Herbivorous fish biomass and urchin<br />

density were also significant explanatory factors in models explaining benthic community<br />

composition. When all benthic functional groups were combined in a multivariate<br />

analysis, herbivorous fish density combined with wave exposure was identified as having<br />

the highest significant correlation with benthic community composition at PHA.<br />

Conversely, nutrient availability, based on algal tissue nutrient content, did not correlate<br />

with percent cover of benthic organisms. These results suggest that at PHA, a site which<br />

represents one end of a global continuum ranging from near-pristine to highly degraded,<br />

top-down mechanisms have primacy over bottom-up mechanisms.<br />

10.361<br />

The Effect Of Increased Seawater Temperature On The Skeletal Development Of favia<br />

Fragum And porites Astreoides New Recruits<br />

Lara GATES 1,2 , Samantha DE PUTRON* 2<br />

1 2<br />

The College of William and Mary, Williamsburg, VA, Bermuda Institute of Ocean Sciences,<br />

St Georges, Bermuda<br />

Recent studies show that rising seawater temperatures affect the vitality of both adult corals and<br />

planulae. Data is lacking, however, concerning the intermittent life-history stage - new settled<br />

coral recruits (spat). The proper development of spat is critical to the success of the coral, as<br />

well as the success of the reef in terms of population sustainability. To address this, an analysis<br />

of spat skeletal development with respect to temperature was performed. Adult corals of two<br />

common brooding species, Favia fragum and Porites astreoides were collected from Bermuda’s<br />

inshore platform just prior to their known planulation period during the summer of 2007, and<br />

planulae were collected in aquaria upon release. Planulae were settled and grown in varying<br />

temperatures. Upon termination of growth, skeletons were evaluated quantitatively in terms of<br />

height and volume as well as qualitatively concerning maturity of development. F. fragum spat<br />

grown in the highest temperature (33°C) were significantly smaller than those grown in ambient<br />

temperature (28.5°C) over the course of one and two weeks of growth. Similar results were<br />

found within the first week of growth for P. astreoides spat. Qualitatively, the evaluation of<br />

maturity of F. fragum skeletons indicated reduced developmental stage with higher<br />

temperatures. In addition, visual observations of the live spat revealed that those in higher<br />

temperatures appeared white and transparent while those in lower temperatures maintained a<br />

green translucence, indicating possible bleaching (zooxanthellae loss) in the higher temperature<br />

treatments. These results suggest a biological basis for decreased growth in higher temperatures<br />

via the expulsion of zooxanthellae resulting in a lack of energy or shortage of skeletal ‘building<br />

blocks’. In this age of predicted global warming, our results suggest a possible disruption of<br />

foundational skeletal development, which may lead to decreased survivorship of coral recruits<br />

of some species and subsequent depletion of coral reefs.<br />

10.362<br />

Recruitment Dynamics Of Scleractinian Corals in A Network Of National Parks And<br />

Marine Protected Areas: West Coast Hawai’i Island<br />

Lawrence BASCH* 1,2 , Angela LEEMHUIS 3 , James WHITE 3 , William WALSH 4<br />

1 National Parks Service, Honolulu, HI, 2 <strong>University</strong> of Hawaii, Cooperative Ecosystems Study<br />

Unit, Honolulu, 3 <strong>University</strong> of Hawaii, Cooperative Ecosystems Study Unit, Honolulu, HI,<br />

4 Hawaii State Department of Land and Natural Resources, Division of Aquatic Resources,<br />

Kailua-Kona, HI<br />

Maintenance of adequate levels of coral settlement and recruitment is vital to sustain coral reefs.<br />

Because early life stages are often more susceptible than adults to environmental stressors, data<br />

on settlement and recruitment can help predict potential effects of disturbance from, and<br />

resilience to environmental change. This study is a large scale, multi-year effort to assess<br />

recruitment of Scleractinians along the west coast of Hawai’i Island in support of long term<br />

benthic monitoring and marine protected area management. Terra cotta tiles have been used at<br />

nine sites over three years as settlement substrate to help determine spatial and temporal<br />

variation in coral settlement and recruitment. Tiles are replaced biannually before and after<br />

known seasonal peaks in coral reproduction and recruitment.<br />

Several spatial and temporal trends were discovered in this ongoing study. Peak settlement of<br />

coral larvae consistently occurred across years in summer (approximately April-September) in<br />

species with and without planktonic larvae. Most species showed spatial patterns in settlement<br />

patterns at the 1-10 km scale (between sites). The northernmost site, Waikalio, had significantly<br />

higher densities of juvenile corals with settlement among sites decreasing immediately toward<br />

the south. Porites spp. had the highest recruitment overall, followed by Montipora spp., then<br />

Pocillopora spp. for most sites. Most Montipora spp. juveniles observed were single polyps<br />

with little or no extension of skeleton beyond the corallite wall; none had multiple polyps.<br />

The north to south pattern in settlement density suggests large scale oceanography is not driving<br />

settlement-recruitment dynamics. Possible alternative influences include smaller, sub regional<br />

differences in ocean currents, habitat structure, disturbance regimes, and anthropogenic<br />

influences.<br />

Combined with emerging oceanographic data, this work provides an initial basis for long term<br />

benthic monitoring of ecological change in, and conservation of, park’s marine resources.<br />

352

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