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Maximum CO(2) diffusion inside leaves is limited by the scaling of cell size and genome size

Maintaining high rates of photosynthesis in leaves requires efficient movement of CO(2) from the atmosphere to the mesophyll cells inside the leaf where CO(2) is converted into sugar. CO(2) diffusion inside the leaf depends directly on the structure of the mesophyll cells and their surrounding airsp...

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Detalles Bibliográficos
Autores principales: Théroux-Rancourt, Guillaume, Roddy, Adam B., Earles, J. Mason, Gilbert, Matthew E., Zwieniecki, Maciej A., Boyce, C. Kevin, Tholen, Danny, McElrone, Andrew J., Simonin, Kevin A., Brodersen, Craig R.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7934972/
https://www.ncbi.nlm.nih.gov/pubmed/33622134
http://dx.doi.org/10.1098/rspb.2020.3145
Descripción
Sumario:Maintaining high rates of photosynthesis in leaves requires efficient movement of CO(2) from the atmosphere to the mesophyll cells inside the leaf where CO(2) is converted into sugar. CO(2) diffusion inside the leaf depends directly on the structure of the mesophyll cells and their surrounding airspace, which have been difficult to characterize because of their inherently three-dimensional organization. Yet faster CO(2) diffusion inside the leaf was probably critical in elevating rates of photosynthesis that occurred among angiosperm lineages. Here we characterize the three-dimensional surface area of the leaf mesophyll across vascular plants. We show that genome size determines the sizes and packing densities of cells in all leaf tissues and that smaller cells enable more mesophyll surface area to be packed into the leaf volume, facilitating higher CO(2) diffusion. Measurements and modelling revealed that the spongy mesophyll layer better facilitates gaseous phase diffusion while the palisade mesophyll layer better facilitates liquid-phase diffusion. Our results demonstrate that genome downsizing among the angiosperms was critical to restructuring the entire pathway of CO(2) diffusion into and through the leaf, maintaining high rates of CO(2) supply to the leaf mesophyll despite declining atmospheric CO(2) levels during the Cretaceous.