A SHIFT IN THE LONG-TERM MODE OF FORAMINIFERAN SIZE EVOLUTION CAUSED BY THE END-PERMIAN MASS EXTINCTION
Article first published online: 18 OCT 2012
© 2012 The Author(s). Evolution© 2012 The Society for the Study of Evolution.
Volume 67, Issue 3, pages 816–827, March 2013
How to Cite
Payne, J. L., Jost, A. B., Wang, S. C. and Skotheim, J. M. (2013), A SHIFT IN THE LONG-TERM MODE OF FORAMINIFERAN SIZE EVOLUTION CAUSED BY THE END-PERMIAN MASS EXTINCTION. Evolution, 67: 816–827. doi: 10.1111/j.1558-5646.2012.01807.x
- Issue published online: 5 MAR 2013
- Article first published online: 18 OCT 2012
- Accepted manuscript online: 20 SEP 2012 01:00PM EST
- Received May 15, 2012 Accepted August 30, 2012 Data Archived: Dryad: doi:10.5061/dryad.5pr86
Table S1. AICc measures of model support across the primary models considered in the paper, geochemical covariates, and alternative reconstructions of environmental convariates.
Table S2. Model fit (adjusted R2) for simple linear regression of body size on a wide range of environmental covariates.
Table S3. Model results and AICc weights for all possible transitions in the two-phase model of foraminiferan size evolution, showing that the Scythian (Early Triassic: 247.7 million years ago) is strongly favored as the transition point, with atmospheric pO2 as the best Paleozoic model and stasis as the best post-Paleozoic model.
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