Changes in reef community structure after fifteen years of natural disturbances in the eastern Pacific (Costa Rica)
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- Reef recovery 20 years after the 1982–1983 El Niño massive mortality (2007, background): “Klapfer, personal communication 2003; Garrison 2005), suggesting that the thermal sensitivity of Cocos Island corals was similar to that of corals at other areas of Costa Rica (Guzman and Cortes 2001; Jimenez and Cortes 2003).”
- Climate change and coral reef bleaching: An ecological assessment of long-term impacts, recovery trends and future outlook (2008, background): “Such delayed predation has been reported in the eastern Pacific (Glynn, 1985b; Guzmán and Cortés, 2001), the central and western Pacific (van Woesik et al., 2004; Wilkinson, 2004) and Indian Ocean (McClanahan et al., 2000).”
- The Adaptive Hypothesis of Bleaching (2004, background): “Field data indicate that El Niño-related bleaching on eastern Pacific reefs was much worse during the 1982–1983 event than the 1997–1998 event, even though temperature excursions during the two events were similar (Glynn et al. 2001; Guzmán and Cortés 2001; Podestá and Glynn 2001).”
- Recovery of coral populations after the 1998 bleaching on Shiraho Reef, in the southern Ryukyus, NW Pacific (2002, background): “Previous studies have focused on the role of recruitment in the recovery of coral populations (Brown & Suharsono 1990, McClanahan 2000, Guzmán & Cortés 2001).”
- Palau’s coral reefs show differential habitat recovery following the 1998-bleaching event (2007, background): “However, both Guzman and Cortes (2001) and Glynn et al. (2001) both assume that both bleaching events, for 1982–1983 and 1997–1998 events, had similar light fields.”
- Immediate and delayed effects of a mass mortality event on gorgonian population dynamics and benthic community structure in the NW Mediterranean Sea (2005, background): “Because recruitment success is generally low, the recovery of these populations depends mainly on the capacity of colonies to recover from damage, the effects of which may persist for a long time after an event (Hoegh-Guldberg 1999, Wilkinson et al. 1999, Guzmán & Cortés 2001).”