Coral bleaching: the role of the host

2009 ◽  
Vol 24 (1) ◽  
pp. 16-20 ◽  
Author(s):  
Andrew H. Baird ◽  
Ranjeet Bhagooli ◽  
Peter J. Ralph ◽  
Shunichi Takahashi
Keyword(s):  
2017 ◽  
Vol 23 (9) ◽  
pp. 3838-3848 ◽  
Author(s):  
Claudia Pogoreutz ◽  
Nils Rädecker ◽  
Anny Cárdenas ◽  
Astrid Gärdes ◽  
Christian R. Voolstra ◽  
...  

2021 ◽  
Author(s):  
Wenhui ZHAO ◽  
Yi HUANG ◽  
Steven T Siems ◽  
Michael J Manton

2018 ◽  
Author(s):  
Guillermo Yudowski ◽  
Loretta Roberson ◽  
Michael Marty-Rivera

Coral bleaching, loss of symbiotic dinoflagellate algae from the coral holobiont, is a complex phenomenon that can result in coral death and reef degradation. Reactive oxygen species (ROS) have been suggested as a possible mechanism underlying this event. To determine if antioxidants can be used to reduce ROS production and coral bleaching, we tested the effects of thermal stress in Aiptasia pallida a model system for coral bleaching studies, and the scleractinian coral, Porites astreoides. We analyzed host ROS levels, symbiont dark-adapted quantum yield of photosystem II, and symbiont loss in the presence or absence of antioxidants. We found that a single dose of the antioxidant catechin, significantly reduced ROS levels in the hosts, mitigated the degradation of the symbionts quantum yield and reduced the loss of symbionts from thermally stressed P. astreoides but not from A. pallida. Taken together, these results support a key role of ROS and that antioxidants can prevent symbiont degradation and loss during thermally-induced bleaching in P. astreoides.


2021 ◽  
Vol 8 (11) ◽  
Author(s):  
Gonzalo Pérez-Rosales ◽  
Héloïse Rouzé ◽  
Gergely Torda ◽  
Pim Bongaerts ◽  
Michel Pichon ◽  
...  

Climate change and consequent coral bleaching are causing the disappearance of reef-building corals worldwide. While bleaching episodes significantly impact shallow waters, little is known about their impact on mesophotic coral communities. We studied the prevalence of coral bleaching two to three months after a heat stress event, along an extreme depth range from 6 to 90 m in French Polynesia. Bayesian modelling showed a decreasing probability of bleaching of all coral genera over depth, with little to no bleaching observed at lower mesophotic depths (greater than or equal to 60 m). We found that depth-generalist corals benefit more from increasing depth than depth-specialists (corals with a narrow depth range). Our data suggest that the reduced prevalence of bleaching with depth, especially from shallow to upper mesophotic depths (40 m), had a stronger relation with the light-irradiance attenuation than temperature. While acknowledging the geographical and temporal variability of the role of mesophotic reefs as spatial refuges during thermal stress, we ought to understand why coral bleaching reduces with depth. Future studies should consider repeated monitoring and detailed ecophysiological and environmental data. Our study demonstrated how increasing depth may offer a level of protection and that lower mesophotic communities could escape the impacts of a thermal bleaching event.


Author(s):  
Wenhui ZHAO ◽  
Yi Huang ◽  
Steven Siems ◽  
Michael Manton

2020 ◽  
Vol 96 (3) ◽  
pp. 431-448
Author(s):  
Severino G Salmo ◽  
John Charles A Altomonte

We investigated shifts in nekton assemblages in coral reef, seagrass, and mangrove habitats that coincided with a coral bleaching event in June 2016. The study was conducted in May 2016 (prebleaching), July 2016 (bleaching), October 2016 (4-mo postbleaching), and February 2017 (7-mo postbleaching) in relatively undisturbed coastal areas in Busuanga, Palawan, western Philippines. We used triangular trap nets to capture nekton samples from each habitat. In coral reef and mangrove habitats, there were increases in nekton abundance and biomass from the prebleaching to the bleaching period. After the bleaching event, however, there were reductions in nekton abundance and biomass at the coral reefs until 7-mo postbleaching. Species composition changed at all sites where shifts in dominant species, habitat affinity, and trophic category were observed. The postbleaching increase in nekton abundance in mangroves coincided with the decreased nekton abundance in the coral reef, suggesting a cross-habitat movement, likely due to the reduced suitability and/or food in the bleached coral reef. The changes in the nekton assemblage may also have been due to seasonal fluctuations in environmental parameters, especially salinity. Our study presents evidence of the possible role of coral bleaching or seasonal changes on cross-habitat movements of nekton assemblages, which can be inferred as an indicator of disturbance. The presence of adjacent vegetated habitats may provide refuge for the affected nekton assemblage of the coral reef.


Coral Reefs ◽  
2011 ◽  
Vol 31 (1) ◽  
pp. 1-12 ◽  
Author(s):  
Lida Teneva ◽  
Mandy Karnauskas ◽  
Cheryl A. Logan ◽  
Laura Bianucci ◽  
Jock C. Currie ◽  
...  

Author(s):  
Kamonphon Patthanasiri ◽  
◽  
Thaithaworn Lirdwitayaprasit ◽  
Thamasak Yeemin ◽  
Ing-on Thongcamdee ◽  
...  

Coral bleaching occurs when cell density or the concentration of photosynthetic pigments of the endosymbionts, zooxanthellae are decreased. This incident may possibly be caused by some environmental stresses, especially under conditions of elevated temperature, decrease in water salinity, or a combination of these factors. To determine the role of temperature and salinity on zooxanthellae and coral bleaching this study was conducted in aquariums under laboratory conditions on cauliflower coral Pocillopora damicornis. The samples were collected from three sites around Samaesan Island, Chonburi, Thailand. Three sets of experiments were conducted at three levels of temperature: room temperature 27 (control), 30, and 33 oC respectively. At each temperature level, three levels of salinities; 10, 20 and 30 (control) psu were tested as well. Coral bleaching percentage and zooxanthellae density in the water column were observed every 6 hours during the period of 72 hours. The results showed that when coral exposed to the highest temperature (33 oC) under the lowest salinity (10 psu), 50-90% bleaching was found and higher symbiont densities in the water column were detected. These results suggested that the combination of the high temperature and low salinity had synergistic effects on coral bleaching and zooxanthellae.


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