Abstract

In tropical montane areas, water limitation is a common occurrence, and both pioneer and forests species experience water stress during the dry season. Adjustments of leaf area during periods of drought allow for the maintenance of the water supply and physiological functions of the remaining leaves. Here, we compared leaf blade water relations between pioneer and forest tree species. Leaf pressure-volume (P-V) curves were determined from samples taken prior to the dry season, to assess how leaves of the different species were adapted to prepare for and endure water deficits. The following parameters were calculated: osmotic potential at full (Ψπ(100)) and zero (Ψπ(0)) turgor, relative water content at zero turgor (RWC0), volumetric elastic modulus (&#949) as well as apoplasm (A) and symplasm (S) water content and their ratio (A/S). Although the pioneer and forest species occupied contrasting habitats, and both groups were clearly differentiated with respect to their water transport capability and water use efficiency, their leaf tissue water relations showed clear differences across species but not between the groups. Some species underwent leaf shedding and accumulated xylem embolisms during the dry season, and their leaves had high cell elasticity. Consequently, these species presented large cell volume changes with turgor loss. Conversely, species with rigid leaves were able to undergo lower leaf turgor with only small changes in cell volume during drought, which might aid to preserve leaf cell function, maintain water uptake, and consequently avoid accelerated leaf senescence and shedding during the dry season.

Highlights

  • The changes in an ecosystem that follow a disturbance are collectively called succession, which is a dynamic and continuous process, often occurring gradually over time [1]

  • Dry mass per unit leaf area (Sw), water content (Wc), wet season (WS) and dry season(DS) water potential (Ψ), as well as terminal branch specific conductivity (Ks) and reduction of both Ks and leaf area during DS as percentage of values found during WS, in two pioneer species (A-B: C. lanata and O. verbesinoides) and two forest species (C-D: C xantochloros and F. mathewsii) from tropical montane habitats as we reported previously in the same habitats and species [9] [12]

  • These results demonstrate a high solute concentration in leaf cells of F. mathewsii (FS) and C. lanata (PS) compared to the other two species (Figure 1)

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Summary

Introduction

The changes in an ecosystem that follow a disturbance are collectively called succession, which is a dynamic and continuous process, often occurring gradually over time [1]. Compared to forest species, pioneer species are prolific seeders, fast-growing, short-lived, generally shade intolerant and with high rates of mortality under resource deprivation. After stand-scale disturbance of natural forests, the landscape changes into patchy vegetation with defined areas including pioneer species and different degree of successional forests. In open habitats occupied by pioneer species forming sparse communities, competition for water and nutrients is lower in comparison to forest habitats [6]. Open habitats created by deforestation experience relatively high variation in light intensity, temperature and water availability as compared to forest habitats [7] [8]. In forest areas, solar radiation is received by the canopy and heat is dissipated efficiently by transpiration. In open areas light is received by the soils and heat is dissipated by convection which is a less efficient process

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