Stoichiometry of potassium is largely determined by water availability and growth in Catalonian forests

Jordi Sardans, Josep Peñuelas, Marta Coll, Jordi Vayreda, Albert Rivas-Ubach

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    Abstract

    The study of the relationships between organisms and environmental elemental stoichiometry and ecosystem structure and function has recently received increasing attention. Some elements, however, have been less studied or have even been neglected. One of these elements is K, despite its critical importance in the water economy of plants. We hypothesized that K concentrations and especially K contents (concentrations × biomass), their stoichiometries with respect to C, N, and P contents, and their relative allocations to foliar and woody compartments would be linked to climatic gradients in the availability of water, forest type and growth. We tested this hypothesis by analysing the data set of the Catalan Forest Inventory. Evergreens, the type of tree with the slowest growth, showed the highest K contents, especially in wood, and the lowest plasticity to change the stoichiometry of K within and between foliar and woody biomasses along climatic gradients. The allocation of K to leaves in relation to the allocation of C, N and P increased with mean annual precipitation (MAP) and was concomitant with decreases in the allocation of K to wood in relation to the allocation of C, N and P (higher K:C L/W, K:N L/W and K:P L/W). In summer, the driest period, higher K:C, K:N and K:P content ratios in leaves were accompanied by lower K:C, K:N and K:P content ratios in wood, mainly in the species at the driest sites. Higher K:C and K:N content ratios in leaves and above-ground biomass in all forest types, and higher K:C L/W and K:N L/W in conifers and deciduous trees were related to higher growth. K contents of leaves were better correlated with tree growth than were K concentrations of leaves in all forest types. These results show that the stoichiometry of K is strongly related to the availability of water and that the uptake of K is more related to the uptake of water than the uptake of N and P. Stoichiometric differences involving K are related to both the response of plants to drought and to plant growth. K thus plays a key role, together with N and P, in the response of plants to climatic gradients for improving the capacities for growth and adaptation to water stress along environmental gradients and through time (seasons). Moreover, these results show that the differences in stoichiometric composition and plasticity involving K contents can underlie the long-term adaptation of trees to different ecological styles of life. K should thus be considered in ecological stoichiometric studies of terrestrial plants. © 2012 The Authors. Functional Ecology © 2012 British Ecological Society.
    Original languageEnglish
    Pages (from-to)1077-1089
    JournalFunctional Ecology
    Volume26
    Issue number5
    DOIs
    Publication statusPublished - 1 Oct 2012

    Keywords

    • C:K
    • Growth rate hypothesis
    • Mean annual precipitation (MAP)
    • Mean annual temperature (MAT)
    • Mediterranean ecosystem
    • N:K
    • P:K
    • Plant growth
    • Water stress

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