“…Furthermore, large differences between the oxygen isotope composition of soil and leaf water pools exist and can be used to track rapidly the relative contributions of soil and leaf CO 2 exchange (Ciais et al, 1997;Farquhar et al, 1993;Francey and Tans, 1987;Welp et al, 2011;Wingate et al, 2010). This large-scale and rapid hydration of CO 2 by the biosphere is accelerated by the family of carbonic anhydrase enzymes (CAs), which are ubiquitous in bacteria, algae, fungi and plants (Badger, 2003;Elleuche and Poggeler, 2010;Moroney et al, 2001;Smith and Ferry, 2000). In leaves the activity and concentration of CAs are high enough to expect that CO 2 diffusing out of the leaf is in nearly full isotopic equilibrium with leaf water (Farquhar and Cernusak, 2012;Gillon and Yakir, 2001).…”