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Primary Research Article
Temperature-driven coral decline: the role of marine protected areas
Article first published online: 2 MAR 2012
DOI: 10.1111/j.1365-2486.2012.02658.x
© 2012 Blackwell Publishing Ltd
Additional Information
How to Cite
Selig, E. R., Casey, K. S. and Bruno, J. F. (2012), Temperature-driven coral decline: the role of marine protected areas. Global Change Biology, 18: 1561–1570. doi: 10.1111/j.1365-2486.2012.02658.x
Publication History
- Issue published online: 9 APR 2012
- Article first published online: 2 MAR 2012
- Accepted manuscript online: 31 JAN 2012 11:48AM EST
- Manuscript Accepted: 10 JAN 2012
- Manuscript Received: 15 OCT 2011
Funded by
- NOAA
- EPA STAR
- Charlotte Johnson Family Fellowship
- University of North Carolina Ross
- Abstract
- Article
- References
- Supporting Information
- Cited By
| Filename | Format | Size | Description |
|---|---|---|---|
| gcb2658-sup-0001-TableS1.docx | Word document | 18K | Table S1. AIC values for different multi-level model forms. The number of temperature anomalies must be a level-1 variable because it varies at the reef level. In each group of models, we selected the model with the lowest AIC (bold). Models are listed in order of increasing complexity. In cases where the difference between two models was less than 2, which indicates that both models have support in an AIC context (Burnham & Anderson, 2002), we selected the most parsimonious model. Models that did not converge have no AIC value and are indicated with a dash. |
| gcb2658-sup-0002-TableS2.docx | Word document | 19K | Table S2. Multilevel model predictions of the mean annual effect of thermal stress anomalies (TSA) on the change in coral cover at (a) 10%, (b) 20%, (c) 50%, and (d) 80% coral cover and 95% credible intervals. |
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