scholarly journals Upwelling buffers climate change impacts on coral reefs of the eastern tropical Pacific

Ecology ◽  
2020 ◽  
Vol 101 (2) ◽  
Author(s):  
Carly J. Randall ◽  
Lauren T. Toth ◽  
James J. Leichter ◽  
Juan L. Maté ◽  
Richard B. Aronson
Author(s):  
J. J. Adolfo Tortolero-Langarica ◽  
Alma P. Rodríguez-Troncoso ◽  
Amílcar L. Cupul-Magaña ◽  
Baruch Rinkevich

Coral reef ecosystems are continuously degraded by anthropogenic and climate change drivers, causing a widespread decline in reef biodiversity and associated goods and services. In response, active restoration methodologies and practices have been developed globally to compensate for losses due to reef degradation. Yet, most activities employ the gardening concept that uses coral nurseries, and are centered in easily-accessible reefs, with existing infrastructure, and impractical for coral reefs in remote locations. Here we evaluate the effectiveness of direct outplanting of coral micro-fragments (Pavona clavus and Pocillopora spp.) as a novel approach to restore remote reefs in the Islas Marías archipelago in the Eastern Tropical Pacific. Coral growth (height-width-tissue cover), survival percentage, extension rates (cm year−1), skeletal density (g cm−3) and calcification rates (g cm−2 year−1) were assessed over 13 months of restoration. In spite of detrimental effects of Hurricane Willa, transplants showed a greater-than-twofold increase in all growth metrics, with ~58–61% survival rate and fast self-attachment (within ~3.9 months) for studied species, with Pocilloporids exhibiting higher extension, skeletal density, and calcification rates than Pavona. While comprehensive long-term studies are required, direct transplantation methodologies of coral micro-fragments are emerging as time-effective and affordable restoration tools to mitigate anthropogenic and climate change impacts in remote and marginal reefs.


2020 ◽  
Vol 27 (1) ◽  
pp. 65-81
Author(s):  
Tayler M. Clarke ◽  
Gabriel Reygondeau ◽  
Colette Wabnitz ◽  
Ross Robertson ◽  
Manuel Ixquiac‐Cabrera ◽  
...  

Diversity ◽  
2021 ◽  
Vol 13 (6) ◽  
pp. 251
Author(s):  
Adi Zweifler (Zvifler) ◽  
Michael O’Leary ◽  
Kyle Morgan ◽  
Nicola K. Browne

Increasing evidence suggests that coral reefs exposed to elevated turbidity may be more resilient to climate change impacts and serve as an important conservation hotspot. However, logistical difficulties in studying turbid environments have led to poor representation of these reef types within the scientific literature, with studies using different methods and definitions to characterize turbid reefs. Here we review the geological origins and growth histories of turbid reefs from the Holocene (past), their current ecological and environmental states (present), and their potential responses and resilience to increasing local and global pressures (future). We classify turbid reefs using new descriptors based on their turbidity regime (persistent, fluctuating, transitional) and sources of sediment input (natural versus anthropogenic). Further, by comparing the composition, function and resilience of two of the most studied turbid reefs, Paluma Shoals Reef Complex, Australia (natural turbidity) and Singapore reefs (anthropogenic turbidity), we found them to be two distinct types of turbid reefs with different conservation status. As the geographic range of turbid reefs is expected to increase due to local and global stressors, improving our understanding of their responses to environmental change will be central to global coral reef conservation efforts.


2019 ◽  
Vol 9 (1) ◽  
Author(s):  
José Luis Carballo ◽  
José Antonio Cruz-Barraza ◽  
Cristina Vega ◽  
Héctor Nava ◽  
María del Carmen Chávez-Fuentes

2008 ◽  
Vol 105 (30) ◽  
pp. 10450-10455 ◽  
Author(s):  
D. P. Manzello ◽  
J. A. Kleypas ◽  
D. A. Budd ◽  
C. M. Eakin ◽  
P. W. Glynn ◽  
...  

Eos ◽  
2021 ◽  
Vol 102 ◽  
Author(s):  
Andrew Chapman

The eastern tropical Pacific Ocean hasn’t warmed as much as climate change models projected. A new study shows that aerosols in the atmosphere could be responsible.


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