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

1-1 The R/v Alpha Helix Symbios Expedition: A Retrospective Analysis Of A Milestone in Coral Reef Research Christopher F. D'ELIA* 1 , Abbie Rae HARRIS*2 1 Environmental Science and Policy, University of South Florida St. Petersburg, Saint Petersburg, FL, 2 College of Marine Science, University of South Florida, Saint Petersburg, FL In the spring of 1971, a team of more than 20 marine scientists arrived at Enewetak Atoll in the Marshall Islands to conduct the most comprehensive study of a coral reef yet undertaken: the Symbios Expedition, using the R/V Alpha Helix for logistical support. While many coral reef researchers are aware that this team-oriented research program made significant contributions to the understanding of coral reef metabolism and function, neither a history of the Expedition has been done nor a formal assessment has been made on its impact on the field. This is not surprising, because scientists rarely concern themselves with documenting the history of the science they conduct or assessing the results of their research programs vis a vis the funding provided. Thus, we are typically left with only vague notions as to the scientific impact that a given project had and the factors that contributed. Clearly, science builds upon prior knowledge, and researchers recognize contributions to this knowledge by literature citations in their publications. Recently, citation analysis tools have become available to assess publication impact quantitatively. Using one such tool, Citespace II, together with quantitative and qualitative information gathered from historical reference materials and extensive interviews, we provide here a retrospective assessment of the Symbios Expedition that demonstrates its scientific impact and suggests some of the reasons for its success. 1-2 Caribbean Coral Reef Communities in the 1970's: An Ecosystem Baseline Data Set for Assessing Current Regional Reef Health Randolph BURKE* 1 , Walter ADEY 2 1 Botany, Smithsonian Institution, Mandan, ND, 2 Botany, Smithsonian Institution NHB, Washington D.C., DC Currently a great debate ensues among scientists about how well developed Caribbean reef communities were before the “crash” and exactly what changes occurred. Since the late 1980’s, Caribbean coral reefs have been repeatedly struck by hurricanes, diseases, high temperatures, over fishing, and locally, recreational and pollution disturbance. For these reasons most scientists consider these reefs to be currently in a state of collapse, but none have a Caribbean wide, historical data base on which to base their beliefs. A regional database, circum-Caribbean and Bahamas, consisting of still photographs (3350 frames, 60 mm and 35 mm; underwater and low altitude aerial) were taken over a two-week period in 1976. SCUBA diver measured transects of coral reef community data were taken concurrently during rest and refueling stops. Additionally, approximately 12 km of 16 mm motion picture film and 1650 still photographs (60 mm and 35mm; underwater and aerial) were taken between 1972 and 1987. This material was collected to support work on regional coral reef structure and ecosystem dynamics that resulted in numerous publications, but much of this supporting data has not been published. Current concerns about Caribbean coral reef health provided an opportunity to revisit this data. The capability of accurately relocating individual reefs was demonstrated by digitally overlaying 1976 digitized photos on exactly the same reef location captured in USGS Orthoimages and Landsat 7 images using Google Earth. More than 80% of the aerial photographs can be accurately relocated within a meter or less using Landsat imagery. The large format (60 mm) allows for size resolution of objects 0.5m and less. This provides historical data on the regional distribution of Acropora palmata, currently on the endangered species list. This data set is uniquely valuable for evaluating changes of shallow-water, Caribbean wide coral reef communities in the last three decades. Oral Mini-Symposium 1: Lessons From the Past 1-3 Estimating Live Coral Cover in Fossil Reefs: A Microboring Approach Halard LESCINSKY* 1 , Benjamin TITUS 1 , Avinash MINHAS 1 , Dennis HUBBARD 2 1 Department of Life and Earth Sciences, Otterbein College, Westerville, OH, 2 Department of Geology, Oberlin College, Oberlin, OH The recent widespread decrease in Caribbean live coral cover points out the need for a valid ecological baseline for understanding modern reefs. Here we show that live coral cover, comparable to that measured in modern reefs, can be estimated in fossil reefs using microboring abundance and taphograde analysis. Subaerially exposed reefs may contain wellpreserved corals that are topped by beds indicative of rapid burial. Since microborers infest coral skeleton within weeks of exposure, microboring analysis provides an objective way to identify corals with little post-mortem exposure and thus buried horizons of these corals can be censused to determine live coral cover in fossil reefs. We applied this technique to the Holocene (5-9,000 ybp) Enriquillo Valley reef in western Dominican Republic. A mud-rich event bed, characterized by Madracis auretenra, is found draping over corals for 125m within the massive coral zone at Cañada Honda. Field-estimated taphogrades correlated with microboring intensity. The best preserved corals (grade 1) had little or no microboring suggesting immediate burial, grade 2 corals had surficial boring (

1-5 The Effects Of Geology, Oceanography And Anthropogenic Activities On The Coral Reef Ecosystems Of The Pacific Remote Island Areas Joyce MILLER* 1,2 , Jamison GOVE 1,2 1 NOAA PIFSC Coral Reef Ecosystem Division, Honolulu, HI, 2 Joint Institute for Marine and Atmospheric Research -- Research Corp. Univ. of Hawaii, Honolulu A wealth of geologic, oceanographic, and biological data collected since 2000 provides a unique opportunity to understand the coral reef ecosystems of the Pacific Remote Island Areas (PRIA). These data were collected by the National Oceanic and Atmospheric Administration and the U.S. Fish and Wildlife Service (FWS) during biennial cruises to seven PRIA: Howland, Baker, and Jarvis Islands, Kingman Reef, and Palmyra, Johnston and Wake Atolls. Detailed bathymetric maps show seven tiny, isolated peaks on anomalously shallow seafloor ranging in age from 120 to 83 Ma, but the four islands that have been dated were all formed about 70 Ma. Small submerged terraces from previous sea level stands can also be detected, providing insight into how sea level change may affect the PRIA in the future. From an oceanographic perspective, these islands and atolls are located in three distinct current regimes, providing an understanding of how current patterns affect the distribution and types of organisms found at each location. Oceanographic data also provide baseline information for understanding the effects of climate change, storms, and bleaching events. Although most of the islands are FWS National Wildlife Refuges and are currently uninhabited, anthropogenic effects from previous guano mining, military and construction activities, fishing, and shipwrecks also have recognizable impacts. Combining this information with biological data on the corals, algae, fish, and macroinvertebrates of the PRIA shows complex interactions that all influence the health of what are thought to be some of the least disturbed coral reef ecosystems in the world. 1-6 Long-Term Records Of Reef Growth Under Terrigenoclastic Sediment Influence: Paluma Shoals, Central Great Barrier Reef, Australia Suzanne E PALMER* 1 , Chris T PERRY 2 , Scott G SMITHERS 3 1 Environmental & Geographical Sciences, Manchester Metorpolitan University, Manchester, United Kingdom, 2 Environmental & Geographical Sciences, Manchester Metropolitan University, Manchester, United Kingdom, 3 Earth and Environmental Sciences, James Cook University, Townsville, Australia Nearshore, turbid-zone reefs on the Great Barrier Reef (GBR) grow on the terrigenoclastic inner shelf and represent important analogues for understanding earlymid Holocene reef initiation on the GBR. They are recognised as ecologically and geologically significant, but knowledge of their development remains limited. The growth history of Paluma Shoals (Halifax Bay, north of Townsville) has been studied in detail to improve our understanding of inshore reef development. Paluma Shoals comprises two areas of active reef development. The reef structure displays distinct phases of reef initiation, reef accretion and reef ‘turn-off’, and the depositional sequence suggests 1) evidence for long-term reef accretion in association with terrigenoclastic sediment accumulation, and 2) phases of reef initiation, growth and burial influenced by nearshore sediment dynamics. Reef growth began ~1200 cal years BP over coarse-grained, terrigenoclastic-dominated subtidal sands and/or Pleistocene clays. The reef sequence is up to 2.0-2.5m thick, comprising an unconsolidated framework of coral rubble within a terrigenoclasticcarbonate matrix. In situ massive corals (Goniopora stokesi, Favites halicora) within basal units are interpreted as shallow pioneer coral communities (the ‘reef initiation’ phase), now enveloped in mainly terrigenoclastic silts. Later reef growth was dominated by framework builders Acropora pulchra, Turbinaria frondens and Montipora mollis, infilled with fine- to medium-grained sands. Reef growth has been characterised by vertical accretion and then seaward progradation, followed by accumulation landward. Since ~250 years BP reef growth of the South Shoal exhibits little variation in framework builders and is characterised by well-established intertidal coral communities and carbonate-rich sands. In contrast, the Northern Shoal exhibits an increase of terrigenous sands, interpreted as a ‘turn-off’ phase in reef development driven by natural shoreline dynamics. Oral Mini-Symposium 1: Lessons From the Past 1-7 Persistent Organic Pollutants And Trace Metals Associated With African Dust – Is There A Threat To Coral Reefs? Virginia GARRISON* 1 , Susan GENUALDI 2 , William FOREMAN 3 , Michael MAJEWSKI 4 , Azad MOHAMMED 5 , Staci SIMONICH 2 1 US Geological Survey, St. Petersburg, FL, 2 Oregon State University, Corvallis, OR, 3 US Geological Survey, Denver, CO, 4 US Geological Survey, Sacramento, CA, 5 University of the West Indies, St. Augustine, Trinidad and Tobago Increasing quantities of African dust transit the Atlantic and impact the Caribbean and Americas. As part of an investigation into the effects of African dust on coral reef organisms and human health, we analyzed African dust for contaminants and compared levels of persistent organic pollutants (POPs) and metals between the source and downwind regions. Air samples from Africa (Mali) were found to contain a greater variety and a higher concentration of pesticides, polychlorinated biphenyls (PCBs), and polycyclic aromatic hydrocarbons (PAHs) than downwind sites in the Caribbean (Trinidad and the U.S. Virgin Islands). To date, nine pesticides, 17 PAHs, and nine PCB congeners have been identified in air samples from the African Sahara/Sahel (Mali) and the Caribbean. One pesticide and four PAHs were detected only in samples from Africa. Of the more than 100 priority pollutant and common-use pesticides screened for in the samples, five pesticides (chlorpyrifos, dacthal, endosulfan I, hexachlorobenzene, and components of chlordane) were detected in samples from all sites. DDE (a breakdown product of DDT) was identified in Mali, USVI, and Trinidad samples. To date, DDT and chlorinated dioxins and furans have been detected only in samples from Mali. Eight and five PCB congeners were detected in Mali and Caribbean samples, respectively; of those, four congeners were detected in samples from both regions. Similarly, greater numbers of PAHs were detected in Mali than at downwind sites. Trace-metal concentrations in both regions were similar to crustal composition with slight enrichment of lead in Mali. Many of the identified POPs and metals are toxic to corals and other marine organisms and can interfere with reproduction, fertilization, and/or immune function. POP and metal contaminants commonly occur as mixtures that are likely to exhibit synergistic effects. Contaminant concentrations are sufficiently high to be of concern – for both marine organisms and humans. 1-8 Bioturbation, Taphonomic Bias And Time-Averaging in Tropical Molluscan Death Assemblages: Differential Shell Half-Lives in Great Barrier Reef Sediment Matthew A. KOSNIK* 1 , Quan HUA 2,3 , Darrell S. KAUFMAN 4 , Raphael A. WÜST 5 1 Department of Paleobiology, Smithsonian Institution, Washington, DC, 2 Australian Nuclear Science and Technology Organization, Menai, NSW, Australia, 3 Australian Nuclear Science and Technology Organization, Menai, Australia, 4 Department of Geology, Northern Arizona University, Flagstaff, AZ, 5 School of Earth and Environmental Sciences, James Cook University, Townsville, Australia Radiocarbon-calibrated amino acid racemization ages of 481 individually dated shells representing four molluscan taxa are used to quantify time-averaging and shell half-lives with increasing burial depth in the shallow-water carbonate lagoon of Rib reef, central Great Barrier Reef, Australia. The top 20 cm of sediment contain a distinct, essentially modern assemblage. Shells recovered at depths form 25 to 125 cm range in age from modern to 4,000 yrs old. They are age-homogeneous and significantly older than the surface layer. Taxon age distributions within layers indicate that the top 125 cm of lagoonal sediment is thoroughly mixed on a subcentury scale. The age distributions and shell half-lives of four taxa: Ethalia, Natica, Tellina and Turbo are found to be largely distinct. Shell half-lives do not coincide with any single morphological characteristic thought to infer greater durability, but they are related to a combined taphonomic score. These results illustrate the importance of bioturbation in tropical sedimentary environments, indicate that age estimates in this depositional setting are sensitive to specimen choice, and quantify a taxon-dependent bias in shell longevity and death assemblage formation. 2

1-1<br />

The R/v Alpha Helix Symbios Expedition: A Retrospective Analysis Of A Milestone<br />

in Coral Reef Research<br />

Christopher F. D'ELIA* 1 , Abbie Rae HARRIS*2<br />

1 Environmental Science and Policy, <strong>University</strong> of South Florida St. Petersburg, Saint<br />

Petersburg, FL, 2 College of Marine Science, <strong>University</strong> of South Florida, Saint<br />

Petersburg, FL<br />

In the spring of 1971, a team of more than 20 marine scientists arrived at Enewetak Atoll<br />

in the Marshall Islands to conduct the most comprehensive study of a coral reef yet<br />

undertaken: the Symbios Expedition, using the R/V Alpha Helix for logistical support.<br />

While many coral reef researchers are aware that this team-oriented research program<br />

made significant contributions to the understanding of coral reef metabolism and<br />

function, neither a history of the Expedition has been done nor a formal assessment has<br />

been made on its impact on the field. This is not surprising, because scientists rarely<br />

concern themselves with documenting the history of the science they conduct or<br />

assessing the results of their research programs vis a vis the funding provided. Thus, we<br />

are typically left with only vague notions as to the scientific impact that a given project<br />

had and the factors that contributed. Clearly, science builds upon prior knowledge, and<br />

researchers recognize contributions to this knowledge by literature citations in their<br />

publications. Recently, citation analysis tools have become available to assess<br />

publication impact quantitatively. Using one such tool, Citespace II, together with<br />

quantitative and qualitative information gathered from historical reference materials and<br />

extensive interviews, we provide here a retrospective assessment of the Symbios<br />

Expedition that demonstrates its scientific impact and suggests some of the reasons for its<br />

success.<br />

1-2<br />

Caribbean Coral Reef Communities in the 1970's: An Ecosystem Baseline Data Set<br />

for Assessing Current Regional Reef Health<br />

Randolph BURKE* 1 , Walter ADEY 2<br />

1 Botany, Smithsonian Institution, Mandan, ND, 2 Botany, Smithsonian Institution NHB,<br />

Washington D.C., DC<br />

Currently a great debate ensues among scientists about how well developed Caribbean<br />

reef communities were before the “crash” and exactly what changes occurred. Since the<br />

late 1980’s, Caribbean coral reefs have been repeatedly struck by hurricanes, diseases,<br />

high temperatures, over fishing, and locally, recreational and pollution disturbance. For<br />

these reasons most scientists consider these reefs to be currently in a state of collapse, but<br />

none have a Caribbean wide, historical data base on which to base their beliefs.<br />

A regional database, circum-Caribbean and Bahamas, consisting of still photographs<br />

(3350 frames, 60 mm and 35 mm; underwater and low altitude aerial) were taken over a<br />

two-week period in 1976. SCUBA diver measured transects of coral reef community data<br />

were taken concurrently during rest and refueling stops. Additionally, approximately 12<br />

km of 16 mm motion picture film and 1650 still photographs (60 mm and 35mm;<br />

underwater and aerial) were taken between 1972 and 1987. This material was collected to<br />

support work on regional coral reef structure and ecosystem dynamics that resulted in<br />

numerous publications, but much of this supporting data has not been published. Current<br />

concerns about Caribbean coral reef health provided an opportunity to revisit this data.<br />

The capability of accurately relocating individual reefs was demonstrated by digitally<br />

overlaying 1976 digitized photos on exactly the same reef location captured in USGS<br />

Orthoimages and Landsat 7 images using Google Earth. More than 80% of the aerial<br />

photographs can be accurately relocated within a meter or less using Landsat imagery.<br />

The large format (60 mm) allows for size resolution of objects 0.5m and less. This<br />

provides historical data on the regional distribution of Acropora palmata, currently on the<br />

endangered species list. This data set is uniquely valuable for evaluating changes of<br />

shallow-water, Caribbean wide coral reef communities in the last three decades.<br />

Oral Mini-Symposium 1: Lessons From the Past<br />

1-3<br />

Estimating Live Coral Cover in Fossil Reefs: A Microboring Approach<br />

Halard LESCINSKY* 1 , Benjamin TITUS 1 , Avinash MINHAS 1 , Dennis HUBBARD 2<br />

1 Department of Life and Earth Sciences, Otterbein College, Westerville, OH, 2 Department of<br />

Geology, Oberlin College, Oberlin, OH<br />

The recent widespread decrease in Caribbean live coral cover points out the need for a valid<br />

ecological baseline for understanding modern reefs. Here we show that live coral cover,<br />

comparable to that measured in modern reefs, can be estimated in fossil reefs using<br />

microboring abundance and taphograde analysis. Subaerially exposed reefs may contain wellpreserved<br />

corals that are topped by beds indicative of rapid burial. Since microborers infest<br />

coral skeleton within weeks of exposure, microboring analysis provides an objective way to<br />

identify corals with little post-mortem exposure and thus buried horizons of these corals can be<br />

censused to determine live coral cover in fossil reefs. We applied this technique to the<br />

Holocene (5-9,000 ybp) Enriquillo Valley reef in western Dominican Republic. A mud-rich<br />

event bed, characterized by Madracis auretenra, is found draping over corals for 125m<br />

within the massive coral zone at Cañada Honda. Field-estimated taphogrades correlated with<br />

microboring intensity. The best preserved corals (grade 1) had little or no microboring<br />

suggesting immediate burial, grade 2 corals had surficial boring (

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