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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 />

25.1153<br />

Algal Symbiont Communities in Scleractinian Corals in The Galapagos During The<br />

1997-1998 El Niño-Southern Oscillation Bleaching Event<br />

Lauren VANDEPAS* 1 , Andrew BAKER 2 , Peter GLYNN 2 , Josh FEINGOLD 3<br />

1 Marine Biology and Fisheries, Rosenstiel School of Marine and Atmorpheric Science,<br />

<strong>University</strong> of Miami, Miami, FL, 2 Marine Biology and Fisheries, Rosenstiel School of<br />

Marine and Atmospheric Science, <strong>University</strong> of Miami, Miami, FL, 3 Division of Math,<br />

Science and Technology, <strong>Nova</strong> <strong>Southeastern</strong> <strong>University</strong>, Ft. Lauderdale, FL<br />

The El Niño-Southern Oscillation (ENSO) bleaching event of 1997-1998 was a severe<br />

disturbance to coral reefs in the Galapagos. Sustained sea surface temperature anomalies<br />

of 3.5–4.5oC resulted in bleaching in a reported 70–90% of all coral species by February<br />

1998, and eventual mortality was approximately 26%. In March 1998, we sampled the<br />

algal symbiont communities (Symbiodinium spp.) from 139 samples of bleached and<br />

healthy corals, and compared them with 20 samples taken from healthy corals in June<br />

1997, before the bleaching event. Algal symbionts were identified using restriction<br />

fragment length polymorphisms (RFLPs) in large subunit ribosomal DNA, and<br />

denaturing gradient gel electrophoresis (DGGE) of the ITS-2 ribosomal region. Samples<br />

taken before the bleaching event (1997) contained a variety of Symbiodinium in clade C,<br />

but no clade D was detected, even in the scleractinian coral Pocillopora, which<br />

commonly hosts D at other sites in the far eastern Pacific (Panama, Mexico). Clade D<br />

was also rare in samples taken during the bleaching event (1998), although they were<br />

found in a few Pocillopora that were unaffected by bleaching, as well as in two almostdead<br />

Pocillopora sampled with the intention of identifying symbionts still remaining in<br />

bleached tissues. These results suggest that the comparative scarcity of heat tolerant<br />

symbionts in the Galapagos may explain why bleaching-related mortality was relatively<br />

higher in the Galapagos in 1997-98 compared to elsewhere in the eastern Pacific. These<br />

findings also indicate that heat tolerant symbionts may have been present in some hosts,<br />

but at levels that were not sufficiently high to affecting survivorship following bleaching.<br />

We hypothesize that the normally cool waters of the Galapagos result in the virtual<br />

absence of heat tolerant symbionts in clade D, resulting in these coral communities being<br />

particularly susceptible to the effects of high temperature bleaching in 1997-98.<br />

25.1154<br />

Coral Reefs Of The Gulf Of Mannar, <strong>Southeastern</strong> India -Observations On The<br />

Effect Of Elevated Sst During 2005-2007<br />

Edward JK PATTERSON* 1 , G. MATHEWS 1 , K. DIRAVIYARAJ 1 , Jerker<br />

TAMELANDER 2<br />

1 Suganthi Devadason Marine Research Institute, Tuticorin, India, 2 IUCN Global Marine<br />

Programme, Dar es salaam, Tanzania<br />

The effect of elevated sea surface temperature (SST) on the coral reefs of the Gulf of<br />

Mannar, <strong>Southeastern</strong> India was monitored during 2005-2007 using quadrate and LIT<br />

methods. The pattern of effect was almost similar on the reefs every year except the<br />

modest fluctuations in the temperature levels. The temperature varied between 31.50C<br />

and 33.60C during summer (April–June). The major reef areas in the Gulf of Mannar are<br />

shallow, between 0.5-3.0m depth and in general, comparatively high temperature<br />

prevailed and the reefs seem to be acclimatized to such situation. The average percentage<br />

of bleached corals during 2005, 2006 and 2007 was 14.6, 15.6, and 12.9 respectively. The<br />

bleaching of corals was noticed from mid April and high temperature existed for about a<br />

month from the end of April. Massive corals especially Porites sp. were the first to be<br />

affected and the other dominant coral species partially / fully bleached were Acropora<br />

cytherea, A. formosa, A. intermedia, A. nobilis, Montipora foliosa, M. digitata and<br />

Pocillopora damicornis. The incidence of bleaching was not uniform every year, in terms<br />

of area and depth, but the pattern was same. Depends on rainfall and winds, recovery<br />

began during June-July and completed in 1-4 months. The branching corals recovered<br />

quickly after temperature reduction, but massive corals took longer time. The fastest<br />

recovered coral size groups were 40-80 cm and 80-160 cm. There was no coral mortality<br />

in 3 years due elevated SST, but 80% of the bleached recruits dead in 2007.<br />

25.1155<br />

What Is The Scope For Adaptation And Acclimatization Of Corals – Seeing The Wood<br />

For The Trees<br />

David OBURA* 1<br />

1 CORDIO East Africa, Mombasa, Kenya<br />

Understanding the role of bleaching in corals and therefore its role in corals adapting to change<br />

has been an elusive goal. A rationale is presented here for a primary role of bleaching in<br />

regulation of the coral-zooxanthellae symbiosis. Stress magnifies the differential metabolic<br />

potential between coral and zooxanthellae such that a control mechanism limiting this<br />

differential is necessary for homeostasis; bleaching is induced to minimize damage from stress.<br />

Two general pathways have been demonstrated for bleaching: reduction of the productivity of<br />

individual zooxanthellae by reducing chlorophyll concentrations and reduction in the population<br />

of zooxanthellae. These are mediated through a variety of physiological mechanisms in the<br />

coral and/or zooxanthellae, and these have explicit gene-environment interactions and therefore<br />

also evolutionary implications where a persistent directional selective pressure is applied. The<br />

extreme thermal stress events causing mass coral bleaching worldwide lie outside the reaction<br />

norms for most corals, revealing the limitations of bleaching as a control mechanism. Limits to<br />

the rates and capacity for change in bleaching mechanisms are not yet known in sufficient detail<br />

to predict the scope for adaptation and acclimatization of corals under present scenarios of<br />

climate change.<br />

25.1156<br />

Effects Of Uv Radiation On The Sexual Reproduction Of The Threatened acropora<br />

Cervicornis<br />

Juan TORRES* 1 , Roy ARMSTRONG 2 , Ernesto WEIL 2<br />

1 Biology Department, <strong>University</strong> of Puerto Rico, San Juan, Puerto Rico, 2 Department of Marine<br />

Sciences, <strong>University</strong> of Puerto Rico at Mayaguez, Lajas, Puerto Rico<br />

The effects of enhanced ultraviolet radiation (280-400nm: UVR) on the fecundity of Acropora<br />

cervicornis were measured in field-transplanted colonies from 20 m to 1 m depth and vice<br />

versa at La Parguera, Puerto Rico. Fecundity was estimated from histological sections made<br />

from tissue samples obtained at different time intervals during the experimental period (March –<br />

August 2003). All colonies transplanted from 20 m to 1 m showed a 100% reduction in gonads<br />

per mesentery per polyp one month after transplantation, while those transplanted from 1 m to<br />

20 m did not show any significant reduction in fecundity throughout the experimental period.<br />

The latter colonies did show however, a delay in the spawning times by releasing their gamete<br />

bundles approximately two-three weeks after the controls at 1 m and two months after the<br />

controls at 20 m suggesting an induced response as a consequence of changes in their daily light<br />

cycle due to less radiation (PAR and UVR) available at 20 m compared to 1 m. Control colonies<br />

at 20 m spawned after the full moon of June 2003, while the controls at 1 m spawned 5-6 days<br />

after the full moon of July 2003. While a possible reabsorption of the gametes occurred in A.<br />

cervicornis colonies transplanted from 20 m to 1 m, the expulsion of these gametes due to the<br />

sudden stress caused by the transplantation is not discarded. The results suggest that sudden<br />

increases in UVR can completely stop sexual reproduction in ramose broadcasting coral<br />

species, which in turn can affect the dominance of the species and the composition and structure<br />

of shallow reef environments.<br />

552

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