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Metabolomic Responses of Guard Cells and Mesophyll Cells to Bicarbonate

Anthropogenic CO(2) presently at 400 ppm is expected to reach 550 ppm in 2050, an increment expected to affect plant growth and productivity. Paired stomatal guard cells (GCs) are the gate-way for water, CO(2), and pathogen, while mesophyll cells (MCs) represent the bulk cell-type of green leaves ma...

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Detalles Bibliográficos
Autores principales: Misra, Biswapriya B., de Armas, Evaldo, Tong, Zhaohui, Chen, Sixue
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2015
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4671721/
https://www.ncbi.nlm.nih.gov/pubmed/26641455
http://dx.doi.org/10.1371/journal.pone.0144206
Descripción
Sumario:Anthropogenic CO(2) presently at 400 ppm is expected to reach 550 ppm in 2050, an increment expected to affect plant growth and productivity. Paired stomatal guard cells (GCs) are the gate-way for water, CO(2), and pathogen, while mesophyll cells (MCs) represent the bulk cell-type of green leaves mainly for photosynthesis. We used the two different cell types, i.e., GCs and MCs from canola (Brassica napus) to profile metabolomic changes upon increased CO(2) through supplementation with bicarbonate (HCO(3) (-)). Two metabolomics platforms enabled quantification of 268 metabolites in a time-course study to reveal short-term responses. The HCO(3) (-) responsive metabolomes of the cell types differed in their responsiveness. The MCs demonstrated increased amino acids, phenylpropanoids, redox metabolites, auxins and cytokinins, all of which were decreased in GCs in response to HCO(3) (-). In addition, the GCs showed differential increases of primary C-metabolites, N-metabolites (e.g., purines and amino acids), and defense-responsive pathways (e.g., alkaloids, phenolics, and flavonoids) as compared to the MCs, indicating differential C/N homeostasis in the cell-types. The metabolomics results provide insights into plant responses and crop productivity under future climatic changes where elevated CO(2) conditions are to take center-stage.