Intact leaves of Kalanchoi daigremonntana were exposed to CO2 partial pressures of 100, 300, and 1000 microbars. Malic acid was extracted, purified, and degraded in order to obtain isotopic composition of carbon-I and carbon-4. From these data, it is possible to calculate the carbon isotope composition of newly fixed carbon in malate. In aUl three treatments, the isotopic composition of newly introduced carbon is the same as that of the CO2 source and is independent of CO2 partial pressures over the range tested. Comparison with numerical models described previously (O'Leary 1981 Phytochemistry 20: 553-567) indicates that we would expect carbon 4 of malate to be 4%o more negative than source CO2 if diffusion is totally limiting or 7%o more positive than source CO2 if carboxylation is totally limiting. Our results demonstrate that stomatal aperture adjusts to changing CO2 partial pressures and maintains the ratio of diffusion resistance to carboxylation resistance approximately constant. In this study, carboxylation and diffusion resistances balance so that essentially no fractionation occurs during malate synthesis. Gas exchange studies of the same leaves from which malate was extracted show that the extent of malate synthesis over the whole night is nearly independent ofCO2 partial pressure, although there are small variations in CO2 uptake rate. Both the gas exchange and the isotope studies indicate that the ratio of external to internal CO2 partial pressure is the same in all three treatments. Inasmuch as a constant ratio will result in constant isotope fractionation, this observation may explain why plants in general have fairly invariable ' C contents, despite growing under a variety of environmental conditions. The carbon isotope fractionations which accompany fixation of atmospheric CO2 during photosynthesis can be used to distinguish between C3 and C4 plants (14,21,23 Such compositions reflect carbon fixation pathways (C3 versus C4, dark versus light CO2 fixation), but they are unlikely to provide detailed pictures of either short-term or localized phenomena within plant metabolism. Studies of isotopic compositions of undifferentiated metabolites of a given class (lipids, amino acids, etc.) provide only a modest improvement (4, 5). To circumvent the difficulties associated with whole plant or metabolite pool studies, we have developed an approach to plant isotope fractionations based on measurements of the particular carbon atom within a particular metabolite which was introduced by the carbon fixation process (15). To date, we have studied the isotopic composition of carbon-4 of malate formed during dark CO2 fixation in CAM plants. This experimental system is useful because malate is accumulated and stored in the vacuole and is not subject to further metabolism until the following light period. After appropriate corrections, this isotopic composition provides the correct basis for evaluating contributions from CO2 diffusion, dissolution, hydration, and carboxylation.In the first application of t...