Responses of the carbon and oxygen isotope compositions of desert plants to spatial variation in soil salinity in Central Asia
Annotatsiya
Abstract We examined the isotopic parameters in two C 3 species ( Artemisia diffusa H. Krasch and Tamarix hispida Willd.) and a C 4 species [ Haloxylon aphyllum (Minkw.) Iljin.] growing or planted in soils with different levels of salinity in a Central Asian desert. The oxygen isotope ratios of stem water (δ 18 O stem ) in T. hispida and H. aphyllum distributed in high‐salinity zones were similar to the δ 18 O of artesian water (δ 18 O artesian ) and different from that in A. diffusa distributed in lower‐salinity zones. This indicates that T. hispida and H. aphyllum depend on water with low salinity in the deeper soil layer, whereas A. diffusa depends on water in the shallower soil layer that would be affected by salt accumulation. The carbon isotope composition of leaf organic matter (δ 13 C om ) and oxygen isotope enrichment in leaf organic matter above stem water (Δ 18 O om ) were lower in A. diffusa than in the other species. The responses of δ 13 C om and Δ 18 O om to soil salinity observed for T. hispida suggest that the species decreased its transpiration rate and increased its intrinsic water‐use efficiency in response to increasing soil salinity. The δ 13 C om and Δ 18 O om of H. aphyllum were higher than those of the C 3 species, and were not correlated with soil salinity, suggesting that H. aphyllum reduced its salt uptake by decreasing transpiration—even though it was able to access less saline water in the deeper soil layer. These results indicate that the water‐use strategy of desert plants in high‐salinity environments can be assessed based on their carbon and oxygen isotope ratios.