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11th ICRS Abstract book - Nova Southeastern University

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Poster Mini-Symposium 25: Predicting Reef Futures in the Context of Climate Change<br />

25.1141<br />

Variation in Zooxanthella Production Of Dimethylsulfoniopropionate (Dmsp)<br />

Mary Alice COFFROTH* 1 , Maria Gabriella JACKSON 1 , Patricia MATRAI 2 , Carlton<br />

RAUSCHENBERG 2<br />

1 Geology, <strong>University</strong> at Buffalo, Buffalo, NY, 2 Bigelow Laboratory for Ocean Sciences,<br />

W. Boothbay Harbor, ME<br />

Dimethylsulfoniopropionate (DMSP) is produced by many marine phytoplankton,<br />

including dinoflagellates. DMSP's proposed functions include an antioxidant, an<br />

osmolyte and a defensive compound, among others. Dinoflagellates within the genus<br />

Symbiodinium (zooxanthellae) that form symbioses with cnidarians also produce DMSP.<br />

However, its role in these organisms is not fully understood. We examined the variation<br />

of dissolved and particulate DMSP cellular quota (DMSPp and DMSPd, respectively)<br />

among different strains of Symbiodinium and investigated how this cellular quota<br />

changed in the presence of environmental stresses. Symbiodinium isolates from Pacific<br />

and Caribbean cnidarian hosts, reared under identical environmental conditions (14h:10h,<br />

light:dark cycle at 26oC), exhibited variation in DMSPp content both between and within<br />

clades (A, C, D, and F). Symbiodinium clade A isolates had the highest DMSPp cellular<br />

quota, suggesting a potential antioxidant role for these symbionts common in shallow,<br />

high light environments. In the intact symbiosis, DMSPp concentrations did not vary<br />

within colonies of Porites divaricata (Pd). However, significant variation was detected<br />

among coral species (Montastrea cavernosa (Mc), M. faveolata (Mf), Porites astreoides<br />

(Pa), and Pd), with Mf having the highest concentrations. We also investigated changes<br />

in DMSPp and DMSPd concentrations occurring in the intact symbiosis under<br />

temperature stress. Mc, Mf, Pa, and Pd were exposed to water temperature 2 o C above<br />

ambient for 2 weeks. Elevated temperatures did not result in a measurable increase in<br />

DMSPp concentrations compared to non-stressed corals; instead, DMSPp concentrations<br />

were greater prior to stress. However, DMSP concentrations in Pd did not change after 2<br />

weeks of heat stress. When this coral was subjected to elevated temperature over a longer<br />

time period (3.5 wks), it bleached and showed very high DMSPp levels.<br />

25.1142<br />

Coral Ultrastructural Response To Elevated Pco2 And Nutrients During Tissue<br />

Repair And Regeneration<br />

D. Abigail RENEGAR* 1 , Patricia L. BLACKWELDER 1,2 , Alison L. MOULDING 1<br />

1 National Coral Reef Institute, <strong>Nova</strong> <strong>Southeastern</strong> <strong>University</strong> Oceanographic Center,<br />

Dania, FL, 2 RSMAS, <strong>University</strong> of Miami, Miami<br />

Corals and coral reefs have recently experienced widespread decline attributed to<br />

anthropogenic pressure on reef systems. Growing coastal population density is expected<br />

to result in a concomitant increase in coastal runoff and nutrification of the coastal zone.<br />

Rising atmospheric CO2 partial pressure (pCO2) is predicted to change ocean surface<br />

water carbonate saturation, resulting in reduced coral calcification and reef growth.<br />

While it has been shown that nutrient and pCO2 stress effect coral growth and<br />

calcification, study of the specific effects on coral tissue has not received significant<br />

attention in the literature despite considerable current interest. The objective of this<br />

research is to examine, at the ultrastructural and histological level, the process of tissue<br />

repair in corals and how it is affected by exposure to elevated nutrients and pCO2. The<br />

target species of this proposed research, Montastraea cavernosa and Porites astreoides,<br />

are important and widespread Caribbean reef-builders. Coral tissue recovery and repair<br />

processes will be assessed with transmission (TEM) and scanning (SEM) electron<br />

microscopy by examining fragments of M. cavernosa and P. astreoides exposed to<br />

elevated nitrate, phosphate, and pCO2 during wound healing. These analyses will result<br />

in a more complete understanding of the complex process of tissue repair and<br />

regeneration in corals under varying environmental conditions.<br />

25.1143<br />

Using The Concept Of Degree Heating Weeks And The Threshold Of Coral Bleaching<br />

Temperature To Assess The Risk Of Coral Bleaching in Taiwan<br />

Tai-Ying WU* 1 , Sharon HORNG 1 , Chang-Feng DAI 1<br />

1 Institute of Oceanography, National Taiwan <strong>University</strong>, Taipei, Taiwan<br />

Degree Heating Weeks (DHWs) represent the accumulation of thermal stress that coral reefs<br />

experienced over the past 12 weeks was applied to evaluate the risk of coral bleaching under the<br />

impacts of climate change. One DHW is equivalent to one week of sea surface temperatures<br />

(SSTs) one degree Celsius greater than the expected summertime maximum. We used the<br />

threshold of coral bleaching temperature instead of the expected summertime maximum to<br />

estimate the DHW values for assessing the risk of coral bleaching in Taiwan. By reviewing the<br />

existing articles, we found the thresholds of coral bleaching temperature are negatively<br />

correlated with latitudes. To verify the applicability of the threshold, we collected SSTs from<br />

1990 to 2006 around Taiwan together with the records of coral bleaching, and the results<br />

confirmed the temperature thresholds are adequate for indicating the occurrence of coral<br />

bleaching. The DHWs of Kenting Reefs in 2007 were used to verify its applicability as an<br />

indicator for the risk of coral bleaching. The DHW was 1.03 in mid-July when the spotted cases<br />

of coral bleaching were observed. During August and September, the DHWs were above 5,<br />

when severe and extensive coral bleaching was observed in Kenting Reefs. These results<br />

support the DHW is a good indicator for coral bleaching in Taiwan. We further used the<br />

simulated SSTs from CGCM2 SRES A2 and B2 scenarios to evaluate the risk of coral<br />

bleaching from present to 2100. The results show the risk of coral bleaching in Taiwan will<br />

increase significantly after 2050 under the A2 scenario; however, under the B2 scenario, coral<br />

bleaching will be occasional events even after 2070. Thus, lowering the greenhouse gas<br />

emission will reduce the threats of global warming on coral reefs and provide longer time for<br />

preventing coral reefs from degradation in Taiwan.<br />

25.1144<br />

Heat Tolerant Corals (porites Lutea and galaxea Fascicularis) From Near-Shore And<br />

Offshore Reefs in Northern Vietnam<br />

Suzanne FAXNELD* 1 , Tove Lund JÖRGENSEN 1 , Michael TEDENGREN 1 , Magnus<br />

NYSTRÖM 1 , Ngai Dang NGUYEN 2<br />

1 2<br />

Systems Ecology, Stockholm <strong>University</strong>, Stockholm, Sweden, Institute of Marine<br />

Environment and Resources, Hai Phong, Vietnam<br />

The objective of this study was to investigate how two coral species, Porites lutea and Galaxea<br />

fasicularis responded to increased water temperature and if the responses differed between<br />

species and between corals from near-shore / offshore reefs.<br />

Corals were collected from near-shore, i.e. disturbed reefs, and offshore, i.e. reefs considered<br />

pristine. The corals were exposed to gradually increased temperatures for 96 h. (day 1: 27.5°C,<br />

day 2: 30.5°C, day 3: 33.5°C, day 4: 25.5°C). The corals in the control group were exposed to<br />

25.5°C.<br />

The results show that both species, with no regard of area, experienced a decrease in GP/R ratio<br />

day 1, after a moderate temperature increase. However, on the other exposure days there were<br />

no differences between heat treated and control corals, even though the temperature increase<br />

was 8°C above ambient on the third day of exposure.<br />

For Porties there were no differences in gross production or respiration between the two areas,<br />

while the pattern was different for Galaxea, where gross production and respiration increased<br />

only for corals from the pristine area.<br />

These results illustrate that even a small temperature increase affects the corals, but the corals<br />

then seem to adapt to the temperature changes. One explanation could be that these species are<br />

tolerant to bleaching and temperature increases, since they come from a high latitude reef and<br />

experience large temperature fluctuation over the year.<br />

The different results between disturbed and pristine area samples for Galaxea might be due to<br />

Galaxea being a sediment tolerant species which might therefore tolerate another stressor (i.e.<br />

elevated temperatures), due to useful clade types, genetic or physiological adaption to different<br />

environmental changes, or their ability to induce heat shock proteins.<br />

549

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