A tale of two ENSO events : Carbonate budgets and the influence of two warming disturbances and intervening variability, Uva Island, Panama

By C. M. Eakin. 2001

110 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/3869ebf0c539a867fbf83ccba56545bea5132b3a

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Citations in the corpus

Caribbean Corals in Crisis: Record Thermal Stress, Bleaching, and Mortality in 2005 (2010, background): “biodiversity that lasted a decade or more [8,9].”
Alternative states on coral reefs: beyond coral–macroalgal phase shifts (2009, background): “However, the carbon budget of Uva Island reef has remained negative and erosive (–3000 to –18 000 kg CaCO3 yr–1), from a net production of >8600 kg CaC03 yr–1 before 1982–1983 (Eakin 2001).”
Changing geo‐ecological functions of coral reefs in the Anthropocene (2018, background): “…often remain high, at least initially (Perry & Morgan, 2017a), meaning that the budgets of reefs rapidly transition to strongly net‐negative states (Eakin, 2001) and surficial structural complexity declines through progressive reef framework collapse (Lasagna, Albertelli, Colantoni, Morri, &…”
Climate change and coral reef bleaching: An ecological assessment of long-term impacts, recovery trends and future outlook (2008, background): “Reanalysis after the 1997–98 El Niño bleaching event again demonstrated that the reef continued in an erosional state, with net erosion ¼ 0.36 kg m 2 y 1 (Eakin, 2001).”
Bioerosion: the other ocean acidification problem: Towards a Broader Perspective on Ocean Acidification Research Part 2 A special issue of the ICES Journal of Marine Science (2017, background): “after coral demise due to thermal bleaching, is thought to be a strong driver that can significantly enhance bioeroder abundances and thus bioerosion rates (e.g. Reaka-Kudla et al., 1996; Scoffin and Bradshaw, 2000; Eakin, 2001; Rützler, 2002; Sheppard et al., 2002; Schönberg and Ortiz, 2009; Carrei”
Reef recovery 20 years after the 1982–1983 El Niño massive mortality (2007, background): “1991, 2000) and high erosion caused by the sea urchin Diadema mexicanum (Agassiz) (Colgan 1990; Eakin 2001).”
Phase shifts and stable states on coral reefs (2010, background): “Eakin (2001) had already noted, however, that although coral cover remained low ( 10”
Bioerosion and Coral Reef Growth: A Dynamic Balance (2015, background): “Continuing studies in the Galápagos Islands and Panamá, to the year 2000, demonstrate virtually total reef frame loss in the former region (Glynn, 1994; ReakaKudla et al., 1996; Glynn et al., 2001) and substantial calcium carbonate declines in the latter (Eakin, 2001).”