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On the Controls of Leaf-Water Oxygen Isotope Ratios in the Atmospheric Crassulacean Acid Metabolism Epiphyte Tillandsia usneoides(1)([W])([OA])
Previous theoretical work showed that leaf-water isotope ratio (δ(18)O(L)) of Crassulacean acid metabolism epiphytes was controlled by the δ(18)O of atmospheric water vapor (δ(18)O(a)), and observed δ(18)O(L) could be explained by both a non-steady-state model and a “maximum enrichment” steady-state...
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| Autor principal: | |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
American Society of Plant Biologists
2011
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| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3091089/ https://ncbi.nlm.nih.gov/pubmed/21300917 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1104/pp.111.172494 |
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