Plant Osmoregulation as an Emergent Water‐Saving Adaptation

Soil salinity affects plant transpiration and growth through two main pathways: the osmotic effect of salt in the soil (osmotic stress; analogous to water stress) and the toxic effect of salt within the plant (ionic stress; salt specific). However, the drastic and sudden reduction of transpiration exhibited by most species in response to an increase of salinity in the root zone is mainly associated with the osmotic phase, while ionic stress appears at a later time, causing the premature senescence of leaves and the reduction of the plant photosynthetic area. To better investigate the effects of salinity on plant‐water relations, we introduce a parsimonious soil‐plant‐atmosphere continuum (SPAC) model accounting for both salt exclusion at the root level and osmoregulation—i.e., the adjustment of internal water potential in response to salt stress. The model is used to interpret a paradox observed in salt‐tolerant species where transpiration is maximum at an intermediate value of salinity ( C T r ,   max ⁡), and is lower in more fresh ( C < C T r ,   max ⁡) and more saline ( C > C T r ,   max ⁡) conditions. Such nonmonotonic transpiration‐salt concentration ( T r − C ) patterns can be largely explained by plant osmoregulation, while the peak of transpiration atC T r ,   max ⁡tends to disappear over longer time scales, when ionic stress appears and morphological adaptations become predominant. Osmoregulation emerges here as a water‐saving behavior similar to the strategies that xerophytes use to cope with aridity. The maximum of transpiration atC T r ,   max ⁡is thus the result of a trade‐off between the enhancement of salt‐tolerance and optimal carbon assimilation.