El Niño–Southern Oscillation (ENSO) events are increasing globally in both frequency and strength, and they can elicit coral bleaching events. The 1997–1998 ENSO caused mass coral mortality with a 96% decline in live coral cover along the Central Mexican Pacific. However, in recent years, these sites have shown signs of recovery. We used data collected in 1997 and 2015–2017 to evaluate the coral recovery in this region and coral cover levels have now reached 50% of their pre-1997–1998 El Niño values. Furthermore, a strong 2015–2016 ENSO event did not significantly affect the live coral cover, potentially demonstrating that the local corals have acclimatized or even adapted to higher temperatures. Even though branching species remain the most abundant morphotype, a PERMANOVA revealed significant changes in the coral assemblage. Collectively, this dataset is testament to the fact that corals within this region are capable of resisting or at least partially recovering from thermal anomalies caused by ENSO events.

The coral Porites sverdrupi is the only scleractinian endemic to the Gulf of California. Over the last 2 decades its populations have been restricted to 3 areas, La Paz Bay, Loreto Bay, and Concepción Bay. As this species faces a high risk of extinction, there is an urgent need for biological, ecological, and genetic information for the guidance of conservation efforts. This is the first study on genetic diversity and connectivity in the species. For this, we analyzed coral colonies from Loreto Bay and Concepción Bay. Our results show that there is high genetic diversity in P. sverdrupi at both sites, with significant genetic structure between them. This condition is caused by a combination of short pelagic larval duration, low dispersal potential between the populations, and local adaptation. Our results emphasize the need for more research in order to establish adequate conservation strategies.

Introduction: The 1997-98 El Niño event caused massive coral bleaching and mortality in the Central Mexican Pacific (CMP). Punta de Mita alone used to harbor more than 30 % of the coral coverage in this region, with a mono-specific Pocillopora coverage. The 1997-1998 ENSO event caused massive coral mortality reducing live coral coverage to < 5 %. Despite being considered a coral region unlikely to recover, recent restoration efforts have been implemented to rehabilitate the coral community. Objective: To assess coral recovery by analyzing the coral growth and survival rates of branching Pocillopora species at Punta de Mita. Methods: Healthy coral fragments of opportunity were re-attached to the natural substrata using zip ties and measured considering their growth in terms of maximum length and width (cm) to determine their annual extension rates. Results: After 50 weeks, corals duplicated their size, with a mean growth of ~ 4 cm year-1. After 100 weeks (2 years), corals triplicated their size, increasing on average 8–9 cm in each diameter. Conclusions: Successful coral reef restoration activities in the Central Mexican Pacific are the result of Pocillopora’s physiological processes, such as fast growth rates, and recent life-history traits, like the ability to cope with thermal anomalies, which enable them to thrive in a dynamic region severely affected by natural and anthropogenic perturbations. Indeed, a region considered unlikely to recover has regained its live coral cover from < 5 % in 1998 up to 15 % in 20 years. This demonstrates the importance of assisting natural coral recovery with restoration efforts, especially in coral locations that, despite environmental perturbations, have proven to be resilient and may become coral refugia areas under the current climate change scenario. Introducción: El evento El Niño de 1997-98 causó un blanqueamiento y mortalidad masiva de corales en el Pacífico Central Mexicano (CMP). Solo Punta de Mita albergaba más del 30 % de la cobertura coralina de esta región, con una cobertura monoespecífica de Pocillopora. El evento ENSO de 1997-1998 causó una mortalidad masiva de corales que redujo la cobertura de corales vivos a < 5 %. A pesar de ser considerada una región de coral con pocas probabilidades de recuperarse, se han implementado esfuerzos de restauración recientes para rehabilitar la comunidad coralina. Objetivo: Evaluar la recuperación de coral analizando el crecimiento coralino y las tasas de supervivencia de especies ramificadas de Pocillopora en Punta de Mita. Métodos: Fragmentos de oportunidad de coral sanos se volvieron a unir a los sustratos naturales usando bridas y se midieron considerando su crecimiento en términos de longitud y ancho máximos (cm) para determinar sus tasas de extensión anual. Resultados: Después de 50 semanas, los corales duplicaron su tamaño, con un crecimiento promedio de ~ 4 cm año-1. Después de 100 semanas (2 años), los corales triplicaron su tamaño, aumentando en promedio 8–9 cm en cada diámetro. Conclusiones: Las actividades exitosas de restauración de arrecifes de coral en el Pacífico Central Mexicano son el resultado de los procesos fisiológicos de Pocillopora, tales como tasas de crecimiento rápido, y rasgos de historia de vida reciente, como la capacidad de hacer frente a anomalías térmicas, que les permiten prosperar en una región dinámica severamente afectada por perturbaciones naturales y antropogénicas. De hecho, esta región que se consideraba poco probable que se recuperara, ha recuperado su cobertura de coral vivo de < 5 % en 1998 hasta 15 % en 20 años. Esto demuestra la importancia de ayudar a la recuperación natural de los corales con los esfuerzos de restauración, especialmente en las ubicaciones de corales que, a pesar de las perturbaciones ambientales, han demostrado ser resistentes y pueden convertirse en áreas de refugio de corales ante el escenario actual de cambio climático.

Intervention techniques to restore coral communities have become an important management tool to help recover and rehabilitate damaged reefs. The direct transplantation of healthy coral fragments is the most common method; however, there is controversy in the long-term success, as using coral clones may diminish the genetic diversity of the coral population. Genetic recombination can be achieved when the coral colony produces gametes and eventually reproduces; therefore, it is important to provide evidence that restored colonies produce gametes as their naturally recruited counterparts with similar colony size (age). Natural and restored Pocillopora coral colonies of the same size range (between 40 and 50 cm in diameter) were tagged and sampled during the rainy season to determine gamete maturation. Our results show no differences in the reproductive activity among colonies: natural and restored coral colonies matured gametes from June to October, with a peak in sexually active coral colonies in July. Also, gamete malformation was not observed. During the gamete production period, the area’s temperature ranged from 27.9 to 30.02 °C. The results’ evidence that coral colonies formed through active restoration contribute not only to the increase in live coral cover as seen in previous studies but potentially contribute in the medium term (>5 years after out-planting) to the production of larvae and local and subsidiary recruitment, since they exhibit the same reproductive patterns as their naturally formed counterparts and no differences in the reproductive activity among coral colonies. Therefore, long-term coral restoration projects contribute to maintaining the live coral cover and the genetic diversity in the region, eventually rehabilitating the coral community.