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

Poster Mini-Symposium 19: Biogeochemical Cycles in Coral Reef Environments 19.782 Exposure To Nutrient-Enriched Sediments Mitigates The Negative Impacts Of Sedimentation On Coral Growth in The Caribbean Corals Porites Astreoides And Siderastrea Siderea Diego LIRMAN 1 , James HERLAN* 1 , Chis LANGDON 1 , Tom CAPO 1 1 Marine Biology and Fisheries, University of Miami, Miami, FL Sedimentation is one of the main sources of disturbance to coral reefs worldwide. However, the recent documentation of healthy coral communities in areas with high sediment and nutrient inputs suggests that an enhanced heterotrophic environment may allow corals to thrive under conditions often considered as marginal. In this study, we document the effects of sedimentation on the growth of Porites astreoides and Siderastrea siderea to evaluate whether the higher nutrient content of enriched sediments can be utilized by corals to offset the negative impacts of sedimentation. Both P. astreoides and S. siderea showed a high tolerance to chronic, high sedimentation levels that reduced light levels and covered corals daily for three weeks. Limited tissue losses were observed, but none of the coral fragments (2-3 cm in diameter) exhibited total mortality. The growth of P. astreoides and P. siderea was significantly influenced by the addition of sediments. For P. astreoides, control corals had the fastest growth rates, followed by corals from the enriched nutrient treatment, non-enriched sediment treatment, and finally, the shading treatment. No significant difference in growth rates were documented between control corals and corals exposed to enriched sediments, but these two groups grew significantly faster than shaded corals and corals exposed to nonenriched sediments. For S. siderea, growth rates were highest for control corals, followed by corals in the enriched sediments treatment, the shading treatment, and the nonenriched sediment treatment. Significant differences were only documented between controls and corals exposed to non-enriched sediments. The enhanced growth of Porites astreoides and Siderastrea siderea exposed to nutrient-enriched sediments shows that corals are able, at least in part, to offset the negative impacts of sedimentation by assimilating sediment nutrients. 19.783 Clipperton Lagoon: A Possible Future For An Atoll Lagoon Charpy LOIC* 1 , Rodier MARTINE 1 1 UR167, IRD, Marseille, France, Metropolitan Clipperton Island, which is sometimes referred as Ile de la Passion (10°17’ N 109°13’ W) is the unique coral atoll, in the eastern Pacific. During 2005, we participated to the Jean- Louis Etienne expedition to investigate the lagoon and the surrounding oceanic waters of Clipperton. Our results confirm the meromictic character of the deep basins due to the last closure of the lagoon around 1849. We found a system with three layers of water which did not intermix and the deepest layer did not contain any dissolved oxygen. The transition layer between brackish and salted waters is characterized by a temperature inversion of 1.6°C. The origin of this increase is probably due to the microbial activity. Taking into account the methodological problems of previous measurements, the physical characteristics of the lagoon do not seem to have changed significantly since the last expeditions. The low DIN and SRP concentrations observed in the upper layer reflects the important nutrient uptake by primary producers of the lagoon as attested by the elevated gross primary production (3.8 g C m-2 day-1) estimated by O2 method. Phytoplankton production integrated in the upper 3 m represents 21 % of the total primary production (benthos + plankton). This comparison confirms the dominant role of benthic plants (macrophytes or epiphytes) in lagoon global metabolism. 19.784 Variability Of Uvr Penetration And Its Biogeochemical Implications For Coral Reef Ecosystems in Malaysia Victor KUWAHARA* 1 , Taeko FURUKAWA 1 , Asami NAKAYAMA 2 , Ryota NAKAJIMA 2 , B. H. Ross OTHMAN 3 , Tatsuki TODA 2 1 Faculty of Education, Soka University, Tokyo, Japan, 2 Faculty of Engineering, Soka University, Tokyo, Japan, 3 School of Environmental & Natural Resources Science, Universiti Kebangsaan Malaysia, Bangi Selangor, Malaysia Biologically diverse coral reef ecosystems, which are symbiotically dependent on photosynthesizing zooxanthellae, are indirectly susceptible to small increases or changes to the spectral UVR distribution. Prior studies have described that the photobiological effects of UVR are largely determined by the underwater spectral UVR:PAR ratio that is directly controlled by the absorption and scattering of biogeochemical material within the water column, i.e. particulate organic matter (POM), dissolved organic matter (DOM), etc. The purpose of this survey was to, 1) establish the current variability of UVR and PAR penetration above coral reefs around the Malaysian peninsula, 2) measure the variability and distribution of UVR specific biogeochemical factors and 3) determine the impact of biogeochemical variability as it affects the UVR:PAR ratio. Downwelling UVR and PAR irradiance and bio-optically derived biogeochemical factors were collected at 14 different coral biodiversity survey stations around the entire Malaysian peninsula from August 10 – 29, 2007. The results show mean penetration of the 1% surface UV-B radiation (320 nm) is generally deeper above reefs on the East coast (16±7 m) relative to the West coast (5±3 m) around the Malaysian peninsula. The UVR:PAR ratio was also generally higher on the East coast relative to the West coast reefs suggesting variable concentrations of UVR-specific absorption. UVR attenuation at all biodiversity stations showed significant relationships (P

Poster Mini-Symposium 19: Biogeochemical Cycles in Coral Reef Environments 19.786 Using Fatty Acid Biomarkers And Nutrients in Sediments To Detect Seasonal Changes in Organic Matter And Nutrient Sources Within A Mixed Coral And Seagrass Community, Bise, Okinawa, Japan Preetika SINGH* 1 , Makoto TSUCHIYA 1 , Nakano YOSHIKATSU 1 , Ninomiya SAYUKO 2 1 University of the Ryukyus, Okinawa, Japan, 2 Tokyo Kyuei Co., Ltd, Kawaguchi, Japan Changes in fatty acid biomarkers and nutrients in sediments from various areas of a coral and seagrass moat were analyzed. Sediments near the wastewater pipes leading into the moat were compared with sediments from the subtidal region, which comprised of a seagrass bed, and a mixed coral and seagrass community. The high amount of nitrites (0.7 µMol/g ) from autumn 2006 until spring 2007, and ammonium (21.6 µMol/g) during the spring season in 2007 observed in sediments near the wastewater pipes indicates that there is a significant input of nutrients from the terrestrial sources. The fatty acid results show that the sediments near the wastewater pipes had a significantly high amount of essential fatty acids (ω3 and ω6 polyunsaturated fatty acids) in autumn of 2006 and macroalgal fatty acids in winter. In the subtidal regions, the seagrass bed sediments had the highest amounts of ammonium (24.4 µMol/g) during the summer season and this was followed by ammonium levels in the sediments from the mixed coral and seagrass community (17.7 µMol/g). The sediments also had the highest essential fatty acids and microalgal biomarkers concentrations during the summer season. The fatty acids results thus indicate that while the sediments near the wastewater pipe are contributing a significant amount of organic matter during autumn and winter, the diatoms and dinoflagellates may be contributing to organic matter within the subtidal sediments during the summer season. 19.787 Nutrient Enrichment Of A Marine Cage Culture And Its Impact On The Composition Of Coral Species in The Subtropical Coral Community Yuan Chao Angelo HUANG* 1 , Pei-Jie MENG 2 , Yung- Song CHEN 3 , Shou Chong HUANG 4 , Chaolun Allen CHEN 5 1 Institute of Oceanography, National Taiwan university, Taipei, Taiwan, 2 National Museum of Marine Biology and Aquarium, Pintung, Taiwan, 3 Department of Animal Science, National IlanUniversity, Ilan, Taiwan, 4 Researcg Center for Biodiversity, Academia Sinica, Taipei, Taiwan, 5 Research Centre for Biodiversity, Academia Sinica, Taipei, Taiwan Offshore cage culture has been demanded increasingly in the oligotrophic water around coral reefs, particularly in those reefs of developing countries. However, the nutrient enrichment and its impact on the adjacent coral community remain unexplored. In this study, the nutrient gradient and the coral species composition in a subtropical coral community were investigated from 2006 to 2007 in the Makong inner Bay (23¢X32.471'N; 119¢X35.320'E), Penghu Islands, Taiwan. Three zones, cage, middle, and none-cage, were divided according to the GPS of cages and coral community. The results indicated that nutrient enrichment in cage zone was significantly higher, especially the nitrogenous components (Ammonia) from the metabolized waste of the cultivated fishes. The other environmental factors presumably affected by cage cultures, including sedimentation rate, organic matter content, and total suspend solids, were not significantly different between cage zone and these other two zones. The highest coral species richness was observed in the middle zone (29 species). In the cage zone coral species richness was slightly decreased to 20 species, and in the non-cage zone it sharply decreased to between 4 and14 species. This tendency is also reflected by the variability of Shannon-Weaver species diversity index. In conclusion, there was a distinct within-reef zonation in coral distribution. Furthermore, nutrient enrichment caused by effluent from the cage did not reduce the coral diversity, but changed the species composition of reefbuilding corals. 19.788 Submarine Groundwater Discharge And Its Role in Structuring Coral Reef Communities Along The Arid Kona Coast Of Hawaii, Usa Eric GROSSMAN* 1 , Karen LISA-KNEE 2 , Adina PAYTAN 3 , Ann GIBBS 1 , Josh LOGAN 1 , Kathy PRESTO 1 , Curt STORLAZZI 1 , Sallie BEAVERS 4 , Lisa MARRACK 4 , Rebecca MOST 4 1 Coastal and Marine Geology Program, US Geological Survey, Santa Cruz, CA, 2 Stanford University, Palo Alto, CA, 3 Institute of Marine Sciences, University of California Santa Cruz, Santa Cruz, CA, 4 National Park Service, Kailua-Kona, HI Coral reef mapping and measurements of nearshore water temperature (T), salinity (S), Radium (Ra) isotope quartets, nutrients, waves, and tidal currents suggest that submarine groundwater discharge (SGD) may play an important role in shaping coral reef communities along the arid Kona coast of the island of Hawaii. Seasonal and tidal surveys across the reef complex of Kaloko-Honokohau National Historical Park (KAHO) between Dec 2003 and April 2006 show persistent discharge of cool, fresh surface water into the nearshore and patterns of transport and mixing with marine waters. In the absence of stream flow, these data reveal that the source of this fresh to brackish water is SGD. Fluxes to the park’s coastal waters ranged between 9.4 and 47.0 m3/d/m of coast and are adequate to maintain a buoyant fresh to brackish surface lens across extensive areas of the reef complex. Nutrient concentrations in groundwater were an order of magnitude higher than surrounding coastal waters of the park. Northerly, alongshore currents generally transported this nutrient-rich water through the park from a dominant source (Honokohau Small Boat Harbor), while large waves mixed the water column to ~10-15 m depths. Coral zonation largely reflects wave exposure along KAHO, however, the octocoral Sarcothelia edmonsoni and various green and brown algae were most dense in areas of high SGD. It is likely that recent increases in municipal groundwater withdrawals and nutrient (urban chemical) loadings translate to elevated SGD-derived nutrient and contaminant discharges. Such data provide important near-baseline information for assessing and predicting climate, land use, and SGD impacts to the area’s fragile ecosystems. 19.789 Detrital Resources in An Undisturbed Coral Reef Food Web: Preliminary Findings From Palmyra Atoll's Coral Reefs Lisa MAX* 1 1 Ecology Evolution and Marine Biology, University of California, Santa Barbara, Santa Barbara, CA Coral reef food web studies have traditionally focused on the competitive and predator-prey relationships between reef organisms. These studies often discount the driving roles that ecosystem processes, such as detritus-cycling, play in maintaining energetic and nutritional pathways on coral reefs. Detritus, the pool of non-living organic material that organisms contribute to via metabolic by-products and eventual death, is an important conduit of energy and nutrients to all trophic levels within ecological communities, yet it receives scant attention in coral reef food web literature. My preliminary studies on the role of detritus at Palmyra Atoll National Wildlife Refuge, demonstrate that detrital material is of high nutritional quality, and is a likely food source for a wide variety of reef organisms in this undisturbed coral reef system. Stable isotope analyses performed on detrital samples demonstrate that its isotopic signature varies among Palmyra’s backreef and forereef habitats. Detrital material used in this study was collected via suction sampling from reef substrates and via sediment traps fixed to the benthos. In order to characterize the biological community in each sampling area, still photo-quadrats and fish and invertebrate surveys were carried out. Overall, this study’s findings suggest that detritus may be an important link in Palmyra Atoll’s coral reef food webs, opening avenues for further research on Palmyra and other coral reefs systems. 460

Poster Mini-Symposium 19: Biogeochemical Cycles in Coral Reef Environments<br />

19.782<br />

Exposure To Nutrient-Enriched Sediments Mitigates The Negative Impacts Of<br />

Sedimentation On Coral Growth in The Caribbean Corals Porites Astreoides And<br />

Siderastrea Siderea<br />

Diego LIRMAN 1 , James HERLAN* 1 , Chis LANGDON 1 , Tom CAPO 1<br />

1 Marine Biology and Fisheries, <strong>University</strong> of Miami, Miami, FL<br />

Sedimentation is one of the main sources of disturbance to coral reefs worldwide.<br />

However, the recent documentation of healthy coral communities in areas with high<br />

sediment and nutrient inputs suggests that an enhanced heterotrophic environment may<br />

allow corals to thrive under conditions often considered as marginal. In this study, we<br />

document the effects of sedimentation on the growth of Porites astreoides and<br />

Siderastrea siderea to evaluate whether the higher nutrient content of enriched sediments<br />

can be utilized by corals to offset the negative impacts of sedimentation.<br />

Both P. astreoides and S. siderea showed a high tolerance to chronic, high sedimentation<br />

levels that reduced light levels and covered corals daily for three weeks. Limited tissue<br />

losses were observed, but none of the coral fragments (2-3 cm in diameter) exhibited total<br />

mortality. The growth of P. astreoides and P. siderea was significantly influenced by the<br />

addition of sediments. For P. astreoides, control corals had the fastest growth rates,<br />

followed by corals from the enriched nutrient treatment, non-enriched sediment<br />

treatment, and finally, the shading treatment. No significant difference in growth rates<br />

were documented between control corals and corals exposed to enriched sediments, but<br />

these two groups grew significantly faster than shaded corals and corals exposed to nonenriched<br />

sediments. For S. siderea, growth rates were highest for control corals, followed<br />

by corals in the enriched sediments treatment, the shading treatment, and the nonenriched<br />

sediment treatment. Significant differences were only documented between<br />

controls and corals exposed to non-enriched sediments. The enhanced growth of Porites<br />

astreoides and Siderastrea siderea exposed to nutrient-enriched sediments shows that<br />

corals are able, at least in part, to offset the negative impacts of sedimentation by<br />

assimilating sediment nutrients.<br />

19.783<br />

Clipperton Lagoon: A Possible Future For An Atoll Lagoon<br />

Charpy LOIC* 1 , Rodier MARTINE 1<br />

1 UR167, IRD, Marseille, France, Metropolitan<br />

Clipperton Island, which is sometimes referred as Ile de la Passion (10°17’ N 109°13’ W)<br />

is the unique coral atoll, in the eastern Pacific. During 2005, we participated to the Jean-<br />

Louis Etienne expedition to investigate the lagoon and the surrounding oceanic waters of<br />

Clipperton. Our results confirm the meromictic character of the deep basins due to the<br />

last closure of the lagoon around 1849. We found a system with three layers of water<br />

which did not intermix and the deepest layer did not contain any dissolved oxygen. The<br />

transition layer between brackish and salted waters is characterized by a temperature<br />

inversion of 1.6°C. The origin of this increase is probably due to the microbial activity.<br />

Taking into account the methodological problems of previous measurements, the physical<br />

characteristics of the lagoon do not seem to have changed significantly since the last<br />

expeditions. The low DIN and SRP concentrations observed in the upper layer reflects<br />

the important nutrient uptake by primary producers of the lagoon as attested by the<br />

elevated gross primary production (3.8 g C m-2 day-1) estimated by O2 method.<br />

Phytoplankton production integrated in the upper 3 m represents 21 % of the total<br />

primary production (benthos + plankton). This comparison confirms the dominant role of<br />

benthic plants (macrophytes or epiphytes) in lagoon global metabolism.<br />

19.784<br />

Variability Of Uvr Penetration And Its Biogeochemical Implications For Coral Reef<br />

Ecosystems in Malaysia<br />

Victor KUWAHARA* 1 , Taeko FURUKAWA 1 , Asami NAKAYAMA 2 , Ryota NAKAJIMA 2 ,<br />

B. H. Ross OTHMAN 3 , Tatsuki TODA 2<br />

1 Faculty of Education, Soka <strong>University</strong>, Tokyo, Japan, 2 Faculty of Engineering, Soka<br />

<strong>University</strong>, Tokyo, Japan, 3 School of Environmental & Natural Resources Science, Universiti<br />

Kebangsaan Malaysia, Bangi Selangor, Malaysia<br />

Biologically diverse coral reef ecosystems, which are symbiotically dependent on<br />

photosynthesizing zooxanthellae, are indirectly susceptible to small increases or changes to the<br />

spectral UVR distribution. Prior studies have described that the photobiological effects of UVR<br />

are largely determined by the underwater spectral UVR:PAR ratio that is directly controlled by<br />

the absorption and scattering of biogeochemical material within the water column, i.e.<br />

particulate organic matter (POM), dissolved organic matter (DOM), etc. The purpose of this<br />

survey was to, 1) establish the current variability of UVR and PAR penetration above coral<br />

reefs around the Malaysian peninsula, 2) measure the variability and distribution of UVR<br />

specific biogeochemical factors and 3) determine the impact of biogeochemical variability as it<br />

affects the UVR:PAR ratio. Downwelling UVR and PAR irradiance and bio-optically derived<br />

biogeochemical factors were collected at 14 different coral biodiversity survey stations around<br />

the entire Malaysian peninsula from August 10 – 29, 2007. The results show mean penetration<br />

of the 1% surface UV-B radiation (320 nm) is generally deeper above reefs on the East coast<br />

(16±7 m) relative to the West coast (5±3 m) around the Malaysian peninsula. The UVR:PAR<br />

ratio was also generally higher on the East coast relative to the West coast reefs suggesting<br />

variable concentrations of UVR-specific absorption. UVR attenuation at all biodiversity stations<br />

showed significant relationships (P

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