Abstract

To quantify the resistance of different co-occurring species to drought and osmotic stress (salinity stress), plant water (Ψ) and osmotic (Ψp) potentials were measured during the dry season. We applied a pressure chamber and cryoscopy to measure Ψ and Ψp, respectively. The species revealed a wide range of responses to water stress (-0.83 to -5.8 MPa) and osmotic stress (-1.3 to -3.2 MPa) and not all plants fit closely into one or the other category. Evergreen species tended to have lower Ψ than deciduous species. Notably, Dobera glabra, well known as drought indicator tree in the region, showed the lowest Ψ (up to -5.8 MPa) and Ψp (-3.2 MPa). This indicates its outstanding drought and osmotic stress tolerance and explains its ability to thrive in drought prone areas and years. The recent expansion of A. oerfota and A. mellifera in the study area could be related to their tolerance of osmotic stress, which may imply a trend of soil salinization. The division of plant responses into categories or strategies can be valuable aid to understanding long-term plant survival and distribution, monitor site condition and predict the direction of future changes.

Highlights

  • Conditions for plant establishment, growth and yield in arid and semi-arid areas are harsh, because these areas are subjected to natural and anthropogenic stresses

  • This study examined the plant water relations of D. glabra and co-occurring species with the aim of examining their drought and osmotic stress tolerance and comparative advantages

  • The differences among the species suggest that the species respond differently to water and osmotic stress, and that they employ different strategies to offset the deleterious effects of drought and osmotic stress

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Summary

Introduction

Conditions for plant establishment, growth and yield in arid and semi-arid areas are harsh, because these areas are subjected to natural and anthropogenic stresses. Drought and soil salinity are the main plant growth limiting factors (Shannon, 1998; Mitlöhner, 1998; Serrano et al, 1998). Environments under primary salinity, i.e. climate and soil induced salinity, are covered with adapted vegetation that evolved to cope with the limiting factors of drought and excess salt (Mitlöhner & Koepp, 2007). Climate change is expected to cause temperature rise and shortage of water in most parts of Africa, which will exacerbate high solute concentration. Under such conditions, the physiological regulation of water use in response to water depletion and high solute concentration (salinization) is essential for species survival, productivity, distribution and competitive relationships

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