Factors affecting ¹³C/¹²C ratios of inland halophytes. II. Ecophysiological interpretations of patterns in the field

Abstract

By measuring δ 13 C values, 9 of 42 species inhabiting saline sites in Alberta were found to be C 4 plants. None of these, however, are dominant species in wet saline situations. A salinity gradient was studied along a transect to provide improved field data on δ 13 C variations among C 3 halophytes. Soils were dominated by sulphates of sodium and, less so, magnesium. Soil water potential [Formula: see text] was highest at a depth of about 10 cm and, on a daily basis, changed little. The δ 13 C values of Puccinellia nuttalliana (Schultes) Hitch, were well correlated with [Formula: see text]. The same appeared true for Salicornia europaea L. ssp. rubra (Nels.) Brietung. In a scattergram representing five major species, a close correlation was also evident for Hordeum jubatum L. The relationship could not be extended to Triglochin maritima L. and Sonchus arvensis L., but values for these two species were not separable from those of P. nuttalliana and H. jubatum. Salicornia europaea ssp. rubra, however, differed by having δ 13 C values that were markedly more negative. Although partly associated with cover by other species, this tendency may reflect a lower water-use efficiency as afforded by a greater reliance on the uptake of readily available salt for osmotic adjustment.

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