On the potential for ocean acidification to be a general cause of ancient reef crises
Version of Record online: 24 FEB 2010
© 2010 Blackwell Publishing Ltd
Global Change Biology
Volume 17, Issue 1, pages 56–67, January 2011
How to Cite
KIESSLING, W. and SIMPSON, C. (2011), On the potential for ocean acidification to be a general cause of ancient reef crises. Global Change Biology, 17: 56–67. doi: 10.1111/j.1365-2486.2010.02204.x
- Issue online: 24 FEB 2010
- Version of Record online: 24 FEB 2010
- Received 18 November 2009; revised version received 4 February 2010 and accepted 5 February 2010
Figure S1. Changes (log-return) of globally preserved reef volume in three categories (supplementing Fig. 2). Significant crises are highlighted by black dots and the boundary of the pre-crisis is indicated by a dashed line. The grey box delineates background fluctuations. Arrows indicate that the true value is below the plot margins, which is the case for most reef types after the Permian-Triassic boundary, because no non-microbial reefs are known in the first stage of the Triassic period (log return = minus infinity). O=Ordovician; S=Silurian; D=Devonian; C=Carboniferous; P=Permian; Tr=Triassic; J=Jurassic; K=Cretaceous; Pg=Paleogene; N=Neogene.
Figure S2. Preservation (sampling completeness) of stony corals and hypercalcifying sponges versus all other organisms through time. See Fig. 5 for additional information.
Table S1. Definition of time intervals for reef crises.
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Please note: Wiley Blackwell is not responsible for the content or functionality of any supporting information supplied by the authors. Any queries (other than missing content) should be directed to the corresponding author for the article.