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