COS 160-10 - Angiosperms evolved a higher mesophyll surface area per volume to maximize gas exchange surface under a low CO2 world

Thursday, August 10, 2017: 4:40 PM
D131, Oregon Convention Center
Guillaume Théroux-Rancourt1, J. Mason Earles2, Matthew E. Gilbert1, Maciej A. Zwieniecki1, C. Kevin Boyce3, Andrew J. McElrone4,5 and Craig R. Brodersen2, (1)Department of Plant Sciences, UC Davis, Davis, CA, (2)School of Forestry & Environmental Studies, Yale University, New Haven, CT, (3)3Department of Geological Sciences, Stanford University, Stanford, CA, (4)4USDA-Agricultural Research Service, Davis, CA, (5)5Deparment of Viticulture and Enology, UC Davis, Davis, CA
Background/Question/Methods

Variation in leaf mesophyll structure strongly affects CO2 diffusion and photosynthetic rates. One key trait is the surface of mesophyll cells exposed to intercellular airspace (Sm) which increases mesophyll conductance. Consequently, Sm is a key control of CO2 diffusion among species and genotypes. Using Sm values from the literature (> 200 species with 500 data points) and from our high-resolution X-ray computed tomography (µCT) dataset (currently > 100 species), we studied if there was an evolutionary trend in Sm. In order to normalize for leaf thickness, we also investigated the ratio of exposed mesophyll surface area to total mesophyll area or volume.

Results/Conclusions

Sm shows little variation from pteridophytes to early angiosperms, while eudicots show the greatest structural diversity. However, Sm increases with total thickness of the mesophyll. By considering the exposed surface of the mesophyll to the intercellular air space (IAS) on a leaf or mesophyll volume (Ames/Vmes) rather than leaf area basis (Sm), we demonstrate that angiosperms, and most specifically commelinids and non-basal eudicots, have constructed leaves with more surface per volume, while gymnosperms keep a constant Ames/Vmes ratio. Thus, this strong phylogenetic signal suggests that angiosperms have developed IAS properties favoring leaves with higher surface to volume ratio, trait that allowed for the potential of high productivity even as atmospheric CO2 declined over the Cenozoic.