Role of bacterial communities in coral’s defence against a causative agent of coral bleaching: Vibrio coralliilyticus

Aims: Different studies have shown that members of the Vibrio such as Vibrio coralliilyticus and Vibrio shiloi are opportunistic pathogens which can cause coral lysis. The aims of this study were to assess whether this results of the virulence of V. coralliilyticus are transmittable to Acropora hyacinthus and Porites lobata, and what role the microbiome of the corals plays during exposure to V. coralliilyticus. Methodology and results: In laboratory-based experiments, we examined the impact of V. coralliilyticus (ATCC BAA- 450) to the microbiome of Acropora hyacinthus and Porites lobata. A. hyacinthus and P. lobata were exposed to ampicillin, V. coralliilyticus, and a combination of both. Results indicate a resistance of A. hyacinthus to V. coralliilyticus through the microbiome and underpin the importance of the microbiome for the coral’s health. Conclusion, significance and impact study: Further studies are needed to identify the bacteria responsible for the coral resistance and could in future lead to the development of a probiotic treatment or prevention of bleaching for sensitive corals.

Massive hard coral loss after a severe bleaching event in 2010 at Los Roques, Venezuela / Pérdida masiva de coral duro después de un evento de blanqueamiento severo en 2010 en Los Roques, Venezuela

Thermal anomalies have become more severe, frequent and well-documented across the Caribbean for the past 30 years. This increase in temperature has caused coral bleaching resulting in reef decline. At Los Roques National Park, Venezuela, temperature has been monitored at four reef sites. In mid-September 2010, seawater temperature reached 30.85°C at 5 m depth in Los Roques, an archipelago only slightly affected by previous bleaching events. For example, bleaching in Los Roques in 2005 was mild compared to the rest of the Caribbean and to the results in this study. In 2010, seawater temperatures remained above 29.0°C from mid-August until the first week of November, resulting in +16 Degree Heating Weeks by that time. Our annual survey of four reef sites indicated that 72% of 563 scleractinian colonies were partial or totally bleached (white) or pale (discolored) in October 2010. In February 2011, there were still 46% of coral colonies affected; but most of them were pale and only 2% were bleached. By February, coral cover had declined 4 to 30% per transect, with a mean of 14.3%. Thus, mean coral cover dropped significantly from 45 to 31% cover (a 34% reduction). In addition to bleaching, corals showed a high prevalence (up to 16%) of black band disease in October 2010 and of white plague (11%) in February 2011. As a consequence, coral mortality is expected to be larger than reported here. Reef surveys since 2002 and personal observations for more than 20 years indicated that this bleaching event and its consequences in Los Roques have no precedent. Our results suggest that reef sites with no previous record of significant deterioration are more likely to become affected by thermal anomalies. However, this archipelago is relatively unaffected by local anthropogenic disturbance and has a high coral recruitment, which may contribute to its recovery.

Durante las últimas décadas las anomalías térmicas han sido más frecuentes y severas en el Caribe, quedando pocos arrecifes exentos de eventos masivos de blanqueamiento (EMB). En el Parque Nacional Los Roques, Venezuela, un archipiélago poco afectado previamente por EMB, la temperatura del agua a 5m de profundidad alcanzó 30,85°C en septiembre 2010, y fue >29,0°C entre mediados de agosto y la primera semana de noviembre en cuatro arrecifes. El 72% de 563 colonias de escleractinios estaban blanqueadas o pálidas para octubre de 2010, mientras que para febrero 2011, el 46% de las colonias aún estaban afectadas. Para febrero 2011, la cobertura béntica coralina promedio disminuyó de 45 a 31%. Además, los arrecifes mostraron una alta prevalencia (de hasta 16%) de enfermedad de banda negra en Octubre 2010, y de plaga blanca (11%) en Febrero 2011. Como consecuencia, es probable que la mortalidad coralina resulte mayor a la reportada acá. Sin embargo, Los Roques es poco afectado por perturbaciones antropogénicas y cuenta con un alto reclutamiento de corales, lo cual podría contribuir a su recuperación.

Agents of coral mortality on reef formations of the Colombian Pacific

The National Monitoring System for Coral Reefs of Colombia (SIMAC) monitors the impact of some of the most important agents of coral tissue loss (bleaching and/or disease) in the Colombian Pacific coral formations since 1998. Physiological bleaching is among the main results of stress in the area. Signs of coral diseases resembling bacterial bleaching such as White Plague and White Band, were observed in Malpelo and Gorgona islands. Damage to the Pacific gorgonian Pacifigorgia spp., similar to those produced by Aspergillosis in Caribbean corals, was detected in Utría Bay. The presence of tumors in colonies of massive corals was also recorded. Even though coral diseases are globally widespread, their occurrence in American Pacific reefs has been poorly documented to date. Rev. Biol. Trop. 58 (Suppl. 1): 133-138. Epub 2010 May 01.

A través del Sistema Nacional de Monitoreo de Arrecifes Coralinos en Colombia-SIMAC se han evaluado algunos agentes de mortalidad coralina en el Pacifico Colombiano desde 1998. Uno de los principales factores que han contribuido a la pérdida de cobertura coralina han sido los eventos de blanqueamiento. No obstante, también se han observado signos que sugieren la presencia de enfermedades coralinas como el blanqueamiento bacteriano, la Plaga Blanca, la Banda Blanca, los tumores coralinos y la Aspergilosis en Pacifigorgia spp.. Aunque las enfermedades coralinas están globalmente distribuidas, su ocurrencia en el Pacifico tropical americano ha sido pobremente documentada. Esta nota incluye la ocurrencia de potenciales enfermedades coralinas en el Pacífico Colombiano.

Branqueamento de corais nos recifes da Bahia e sua relação com eventos de anomalias térmicas nas águas superficiais do oceano / Coral bleaching in Bahia reefs and its relation with sea surface temperature anomalies

A partir de 1993 foram registrados vários eventos de branqueamento de coral na Bahia, com recuperação total dos corais afetados. O primeiro registro ocorreu em Abrolhos no verão de 1993/1994, quando o percentual de colônias branqueadas variou entre 50 e 90 por cento. No verão de 1997/1998, ocorreu no Litoral Norte da Bahia uma anomalia térmica de 1 ºC, com temperaturas medidas no campo de 29 a 30,5 ºC, o que causou branqueamento em 60 por cento dos corais. De 1998 a 2005, foi observado que nos recifes costeiros, localizados muito próximos (<5km) ou adjacentes à costa, a permanência de anomalias térmicas de 0,25 ºC por mais de duas semanas causou branqueamento em mais de 10 por cento dos corais. Porém para os recifes de Abrolhos, localizados a mais de 10 km da costa, apenas anomalias acima de 0,50 ºC com duração de mais de duas semanas causaram branqueamento em mais de 10 por cento dos corais. Mussismilia hispida, Siderastrea spp., Montastraea cavernosa, Agaricia agaricites e Porites astreoides foram as espécies de coral mais afetadas pelo branqueamento e são as espécies mais freqüentes nos recifes costeiros. Todas as espécies apresentaram graus diferentes de branqueamento, "fraco" ou "forte". Nos recifes da Bahia há uma forte relação entre o branqueamento de corais e os eventos de anomalias da temperatura da superfície do mar (TSM), e os recifes mais afetados pelo branqueamento foram os recifes costeiros. Estes recifes localizados muito próximos da costa estão mais expostos aos efeitos dos impactos provenientes de processos que ocorrem na região costeira, sugerindo que, muito provavelmente, os corais mais expostos a níveis elevados de nutriente e sedimento, e variações sazonais mais altas da TSM, podem já estarem mais resistentes aos efeitos pós branqueamento como, por exemplo, doenças infecciosas e mortalidade em massa.

Since 1993 several coral bleaching events were registered in Bahia. There were no mass coral death associated to these events and the affected corals fully recovered after the impact. The first occurrence was registered during the southern hemisphere summer of 1993/1994, in Abrolhos, when 50 to 90 percent of the coral colonies were bleached. In the North Coast of Bahia, during the summer of 1997/1998, a sea surface temperature (SST) anomaly of 1 ºC matched with SST registered in the field (29 to 30.5 ºC). As a result, up to 60 percent corals bleached. From 1998 to 2005 anomalies of 0.25 ºC, for two weeks, caused bleaching in more than 10 percent corals from the coastal reefs, which are located adjacent or less than 5 km from the coastline. However in the Abrolhos region, where reefs are located more than 10 km from the continent, only SST anomalies higher than 0.50 ºC,persisting for more than two weeks, caused bleaching up to 10 percent of the investigated corals. Mussismilia hispida, Siderastreaspp., Montastraea cavernosa, Agaricia agaricites and Porites astreoides were the coral species most severely impacted by bleaching, and they are also the most common species in the coastal reefs. All species presented different levels of bleaching, 'light' or 'heavy'. In Bahia, there is a strong linkage between coral bleaching and periods of elevated sea surface temperature, and the most affected corals were the ones from the coastal reefs. These coastal reefs are exposed to the impacts from processes occurring in the continent, suggesting that corals exposed to high levels of nutrient and sediment loads, and large SST fluctuations, may be more resistant to the post bleaching effects, such as infectious diseases and mass mortality.

Fragmentation of the gastrodermis and detachment of zooxanthellae in symbiotic cnidarians: a role for hydrogen peroxide and Ca2+ in coral bleaching and algal density control / Fragmentación de la gastrodermis y desprendimiento de zooxantelas en cnidarios simbióticos: papel del peróxido de hidrógeno y el Ca2+ en el blanqueamiento de corales y el control de la densidad de algas

Coral bleaching involves the detachment of zooxanthellae and the simultaneous fragmentation of the gastrodermis. Results obtained with a cell permeant fluorescent probe for calcium ions (Ca2+) indicates that "thermal" bleaching is the result of a temperature related breakdown of the Ca2+ exclusion system. "Solar" bleaching, which takes place at lower temperatures and is driven by light, is the result of a build-up of photo-synthetically produced hydrogen peroxide in the tissues. Gastrodermal tissue with its symbionts, scraped from between septa of corals, was observed under controlled conditions of high light and temperature. Pieces of gastrodermis round off, zooxanthellae move to the surface, protrude from the surface and after a delay, detach, surrounded by a thin layer of host cytoplasm, inclusions and plasma membrane. The higher the temperature and light level the shorter the delay and higher the rate of algal detachment. Fragmentation by the ballooning-out and detachment of small spheres of cytoplasm (bleb formation) takes place simultaneously. This is likely to be due to oxidation, by hydrogen peroxide (H2O2), of -SH groups on the cytoskeleton and its attachment to the plasma membrane. Ground, polished and stained thin acrylic resin sections reveal similar processes taking place in artificially bleached corals. Isolated zooxanthellae and whole corals are shown to release H2O2 in the light. This process of algal detachment and fragmentation that takes place at normal sea temperatures may underlie the mechanism limiting algal populations in the gastrodermis and may be localized to areas with a concentration of algae near the membrane. At above-normal temperatures under the synergistic effect of light and temperature, the rate of production of H2O2 exceeds the rate at which can it be lost by diffusion or destroyed and H2O2 accumulates. This results in damage to the calcium exclusion system, detachment of zooxanthellae into the coelenteron and fragmentation of the gastrodermis. Rev. Biol. Trop. 54 (Suppl. 3): 79-96. Epub 2007 Jan. 15.

El blanqueamiento de los corales implica el desprendimiento de zooxantelas y la simultánea fragmentación de la gastrodermis. Resultados obtenidos con una sonda florescente de iones Calcio (Ca2+) para células permeables, indican que el blanqueamiento "térmico" es el resultado de una interrupción del sistema de exclusión de Ca2+, provocada por la temperatura. El blanqueamiento "solar", que tiene lugar a temperaturas más bajas y está determinado por la luz, es el resultado de una acumulación de peróxido de hidrógeno producido fotosintéticamente en los tejidos. Para ver el proceso, se raspó tejido gastrodermal, junto con sus simbiontes, de entre los septos de los corales y se observó en condiciones controladas de luz y temperatura. Primero, los trozos de gastrodermis se dan vuelta, luego las zooxantelas se mueven hacia la superficie, sobresalen desde ella y tras un tiempo, se desprenden, rodeadas de una delgada capa de citoplasma del hospedero, inclusiones y membrana plasmática. Mientras mayor sea la temperatura y el nivel de luz, menor es el tiempo que tardan las zooxantelas en desprenderse y mayor es la tasa de desprendimiento algal. La fragmentación producida por el inflamación y el desprendimiento de pequeñas esferas de citoplasma (formación de ampollas), tiene lugar simultáneamente. Probablemente, esto es causado por oxidación en el citoesqueleto de grupos -SSH por el peróxido de hidrógeno (H2O2), y por su acoplamiento a la membrana plasmática. Secciones de resina acrílica delgada molida, pulida y teñida revelan que en corales blanqueados artificialmente se llevan a cabo procesos similares. Se ha demostrado que tanto las zooxantelas aisladas como los corales enteros, liberan H2O2 en la luz. Debajo este proceso de desprendimiento algal y fragmentación que tiene lugar a temperaturas normales en el mar, puede encontrarse el mecanismo que limita las poblaciones algales en la gastrodermis, el cual podría estar localizado en áreas con concentraciones de alga cerca de la membrana. A temperaturas más altas de lo normal, bajo el efecto sinérgico de la luz y la temperatura, la tasa de producción de H2O2 excede la tasa a la cual éste puede destruirse o perderse por difusión y, por ende,se acumula. Esto resulta en daño al sistema de exclusión de calcio, desprendimiento de zooxantelas hacia el celenterón y fragmentación de la gastrodermis.