Shifts in carbon isotope ratios of two C3 halophytes under natural and artificial conditions

Summary The total carbon ¹³C values of two C₃ halophytes,Salicornia europaea L. ssp.rubra (Nels.) Breitung andPuccinellia muttalliana (Schultes) Hitch., native to inland saline areas of Alberta, Canada, were determined for plants grown under controlled conditions of supplied NaCl in the nutrient solution, and for plants found growing in the field. Field specimens were collected along line transects which ran from areas of high salinity to areas of low salinity across the pattern of species zonation. The ¹³C value of the two species seemed to reflect the water potential of the soil ( _w ^soil ) as measured arbitrarily at a depth of 10 cm, becoming less negative as the _w ^soil decreased. Over a linear distance of 5.55 m,S. europaea spp.rubra showed a shift of +5.3 as the _w ^soil went from-25x10² kPa to a minimum of-73x10² kPa. ForP. nuttalliana, the ¹³C values differed by 3.4 over a distance of 7.45 m where the maximum difference in _w ^soil was 12.7x10² kPa. However, ¹³C values ofP. nuttalliana only roughly reflected the spatial trends in _w ^soil at the time of collection. In the growth chamber, the ¹³C value ofS. europaea ssp.rubra changed by a maximum of +8.0 when the solute potential of the nutrient solution ( _w ^soil ) was dropped from-0.25x10² kPa to-64.25x10² kPa; while the ¹³C value ofP. nuttalliana changed by a maximum of +10.8 when the _w ^soil was dropped from-0.25x10² kPa to-40.25x10² kPa. Linear regression analyses indicated that the ¹³C values of both species were strongly correlated (P<0.2%) with _w ^soil . The observed shifts in ¹²C may represent changes in the mode of photosynthetic CO₂ fixation. However, a number of other explanations, some of which are discussed in the text, are also possible. A proper ecophysiological interpretation of such shifts in ¹³C values of C₃ plants awaits a better understanding of the isotope fractionation mechanisms involved.