Temperature Dependence of Carbon Isotope Fractionation in CAM Plants
Author(s) -
E. Deléens,
Isabel Treichel,
Marion H. O’Leary
Publication year - 1985
Publication title -
plant physiology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.554
H-Index - 312
eISSN - 1532-2548
pISSN - 0032-0889
DOI - 10.1104/pp.79.1.202
Subject(s) - fractionation , malic acid , crassulacean acid metabolism , isotopes of carbon , carboxylation , equilibrium fractionation , chemistry , isotope , stable isotope ratio , isotope fractionation , kinetic isotope effect , analytical chemistry (journal) , botany , chromatography , environmental chemistry , photosynthesis , biochemistry , biology , citric acid , total organic carbon , deuterium , physics , quantum mechanics , catalysis
The carbon isotope fractionation associated with nocturnal malic acid synthesis in Kalanchoë daigremontiana and Bryophyllum tubiflorum was calculated from the isotopic composition of carbon-4 of malic acid, after appropriate corrections. In the lowest temperature treatment (17 degrees C nights, 23 degrees C days), the isotope fractionation for both plants is -4 per thousand (that is, malate is enriched in (13)C relative to the atmosphere). For K. daigremontiana, the isotope fractionation decreases with increasing temperature, becoming approximately 0 per thousand at 27 degrees C/33 degrees C. Detailed analysis of temperature effects on the isotope fractionation indicates that stomatal aperture decreases with increasing temperature and carboxylation capacity increases. For B. tubiflorum, the temperature dependence of the isotope fractionation is smaller and is principally attributed to the normal temperature dependences of the rates of diffusion and carboxylation steps. The small change in the isotopic composition of remaining malic acid in both species which is observed during deacidification indicates that malate release, rather than decarboxylation, is rate limiting in the deacidification process.
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