Relationships between boring sponge assemblages and the availability of dead coral substrate on Mexican Pacific coral reefs

Author(s):  
Héctor Nava ◽  
Carlos Alberto Emmanuel García-Madrigal ◽  
José Luis Carballo

AbstractBoring sponges are an important component of bioeroder assemblages in tropical coral reefs. They are considered as a potential threat for coral reef health, and the increase of dead corals is expected to promote their abundance. The relationship between the availability of dead coral substrata and the development of boring sponge assemblages was evaluated during El Niño 2015–16 at five reefs from Zihuatanejo, Guerrero, Mexico. Environment and substrate quality were assessed. Overall, environment conditions remained normal in relation to previous studies in the area. Only water temperature showed unusually high records at all sites and coincided with bleaching and mortality of corals, possibly caused by the effects of the El Niño event. Abundance of boring sponges in dead corals and coral rubble was lower than during previous studies. Although sponge abundance was not directly related to cover of both dead corals and coral rubble, cover of dead corals showed a high correlation with the variation in the structure of sponge assemblages across sites.Cliona vermiferadominated sponge assemblages at all sites, and its abundance was high under conditions of high cover of live corals and low cover of bleached corals. Since overall sponge abundance responded in a similar way, these results suggest that boring sponge assemblages dominated byC. vermiferaare enhanced by conditions favourable for corals. Our results imply that El Niño events in the Mexican Pacific are not likely to cause immediate population outbreaks of boring sponges.

2021 ◽  
Vol 42 (2) ◽  
Author(s):  
Héctor Nava ◽  
Norma López ◽  
Pedro Ramírez‐García ◽  
Elizabeth Garibay‐Valladolid

2017 ◽  
Vol 14 (4) ◽  
pp. 817-826 ◽  
Author(s):  
Eghbert Elvan Ampou ◽  
Ofri Johan ◽  
Christophe E. Menkes ◽  
Fernando Niño ◽  
Florence Birol ◽  
...  

Abstract. The 2015–2016 El-Niño and related ocean warming has generated significant coral bleaching and mortality worldwide. In Indonesia, the first signs of bleaching were reported in April 2016. However, this El Niño has impacted Indonesian coral reefs since 2015 through a different process than temperature-induced bleaching. In September 2015, altimetry data show that sea level was at its lowest in the past 12 years, affecting corals living in the bathymetric range exposed to unusual emersion. In March 2016, Bunaken Island (North Sulawesi) displayed up to 85 % mortality on reef flats dominated by Porites, Heliopora and Goniastrea corals with differential mortality rates by coral genus. Almost all reef flats showed evidence of mortality, representing 30 % of Bunaken reefs. For reef flat communities which were living at a depth close to the pre-El Niño mean low sea level, the fall induced substantial mortality likely by higher daily aerial exposure, at least during low tide periods. Altimetry data were used to map sea level fall throughout Indonesia, suggesting that similar mortality could be widespread for shallow reef flat communities, which accounts for a vast percent of the total extent of coral reefs in Indonesia. The altimetry historical records also suggest that such an event was not unique in the past two decades, therefore rapid sea level fall could be more important in the dynamics and resilience of Indonesian reef flat communities than previously thought. The clear link between mortality and sea level fall also calls for a refinement of the hierarchy of El Niño impacts and their consequences on coral reefs.


2005 ◽  
Vol 5 (5) ◽  
pp. 584-589 ◽  
Author(s):  
Macias-Zamora . ◽  
Rene . ◽  
Vidaurri-Sotelo . ◽  
Ana Luisa . ◽  
Olivos-Ortiz Aramis .

AMBIO ◽  
2002 ◽  
Vol 31 (1) ◽  
pp. 40-48 ◽  
Author(s):  
Charles R. C. Sheppard ◽  
Mark Spalding ◽  
Clare Bradshaw ◽  
Simon Wilson
Keyword(s):  
El Niño ◽  

2015 ◽  
Vol 60 (6) ◽  
pp. 121 ◽  
Author(s):  
Juan José Alvarado ◽  
Jorge Cortés ◽  
Héctor Reyes-Bonilla
Keyword(s):  
El Niño ◽  
El Nino ◽  

<span>El fenómeno de El Niño de 1982-83 produjo una alta mortalidad coralina (50-90%) en varias localidades del Pacífico Tropical Oriental, lo que en algunos arrecifes trajo como consecuencia una explosión en la poblaciones de erizos de mar, <em>Diadema mexicanum</em>, y por consiguiente un aumento en la bioerosión del basamento coralino. En Costa Rica, el impacto fue diferencial en tres localidades arrecifales, siendo mayor en la Isla del Coco, intermedio en la Isla del Caño, y menor en Bahía Culebra, con similares patrones en la presencia del erizo<em> D. mexicanum</em>. Con el fin de poder entender el papel histórico que desempeña este erizo de mar en el balance entre bioerosión y bioacreción, se reconstruyó el impacto bioerosivo basándose en patrones actuales de ingestión de carbonatos por parte del erizo, tasas de crecimiento y densidad del esqueleto coralino, y datos históricos de densidad poblacional del erizo y cobertura coralina. Los resultados de las reconstrucciones variaron dependiendo de la localidad. En la Isla del Coco, el efecto de los erizos de mar varío de un efecto negativo sobre el balance arrecifal de carbonatos a un efecto positivo, favoreciendo el reclutamiento coralino y la recuperación del arrecife. En la Isla del Caño, <em>Diadema</em> presentó un efecto neutro, al no tener una participación preponderante en el balance de carbonatos de esta isla. Mientras, que en Bahía Culebra, los efectos de los erizos de mar pasaron de tener un efecto positivo-neutro, a uno negativo, posiblemente asociado a un incremento en condiciones eutróficas de la bahía que están favoreciendo un incremento en la bioerosión del basamento coralino. El valor de este erizo en la dinámica arrecifal y su relación con la protección, sobrepesca, y manejo costero, posee una gran influencia en el balance de carbonatos en los arrecifes coralinos del Pacífico de Costa Rica.</span>


2016 ◽  
Author(s):  
Eghbert Elvan Ampou ◽  
Ofri Johan ◽  
Christophe E. Menkes ◽  
Fernando Nino ◽  
Florence Birol ◽  
...  

Abstract. The 2015–2016 El-Niño and related ocean warming has generated significant coral bleaching and mortality worldwide. In Indonesia, first signs of bleaching were reported in April 2016. However, this El Niño has impacted Indonesian coral reefs since 2015 through a different process than temperature-induced bleaching. In September 2015, altimetry data shows that sea level was at its lowest in the past 12 years, affecting corals living in the bathymetric range exposed to unusual emersion. In March 2016, Bunaken Island (North Sulawesi) displayed up to 85 % mortality on reef flats dominated by Porites, Heliopora and Goniastrea corals with differential mortality rates by coral genus. Almost all reef flats showed evidence of mortality, representing 30 % of Bunaken reefs. For reef flat communities which were living at a depth close to the pre-El Niño mean low sea level, the fall induced substantial mortality likely by higher daily aerial exposure a least during low tide periods. Altimetry data was used to map sea level fall throughout Indonesia, suggesting that similar mortality could be widespread for shallow reef flat communities, which accounts for a vast percent of the total extent of coral reefs in Indonesia. The altimetry historical records also suggest that such event was not unique in the past two decades, therefore rapid sea level fall could be more important in the dynamics and resilience of Indonesian reef flat communities than previously thought. The clear link between mortality and sea level fall also calls for a refinement of the hierarchy of El Niño impacts and their consequences on coral reefs.


PLoS ONE ◽  
2018 ◽  
Vol 13 (2) ◽  
pp. e0190957 ◽  
Author(s):  
Danielle C. Claar ◽  
Lisa Szostek ◽  
Jamie M. McDevitt-Irwin ◽  
Julian J. Schanze ◽  
Julia K. Baum

2016 ◽  
Vol 70 (2) ◽  
pp. 175-190 ◽  
Author(s):  
Andrés López-Pérez ◽  
Sergio Guendulain-García ◽  
Rebeca Granja-Fernández ◽  
Valeria Hernández-Urraca ◽  
Laura Galván-Rowland ◽  
...  

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