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. 2004 Oct;136(2):3350–3363. doi: 10.1104/pp.104.040758

Figure 3.

Figure 3.

The δ18O of chloroplast CO2 plotted against the δ18O of water at evaporative sites in R. communis leaves during photosynthesis. In this experiment, air entering the leaf chamber had an average CO2 partial pressure of 833 μbar, and air exiting the chamber had an average CO2 partial pressure of 363 μbar. Irradiance varied from 300 to 800 μmol PAR m−2 s−1, and chamber air temperature varied between 25 and 30°C. The δ18O of chloroplast CO2 was calculated as described in the theory section of the main text. The broken line on the graph represents the relationship expected if chloroplast CO2 were in full oxygen isotope equilibrium with water at the evaporative sites. The δ18O values are presented relative to VSMOW. The δ18O of irrigation water fed to the plants was −7.2‰. The arrow on the graph indicates an outlying datum that strongly influenced the slope of the regression between δc and δe. Excluding this datum resulted in a slope between δc and δe of 1.10.