ATMOSPHERIC oxygen is not in equilibrium with sea water with respect to the isotope exchange illustration but has an ¹⁸O excess of about 22‰ compared to sea water¹. This could be due to isotope fractionation during respiration². Another large contribution to the effect has been overlooked up to now. Photosynthesis on land takes place in transpiring leaves, where the difference in the vapour pressure of ¹⁶OH₂ and ¹⁸OH₂ concentrates the heavy molecules in their stationary water content. Since the free oxygen stems from the water in which photosynthesis takes place^3–8 (with only a very small shift in isotopic composition⁹), photosynthesis on land is an ¹⁸O source for atmospheric O₂. We have begun to study this effect quantitatively.

Open image in new window