Responses to internal potassium ion concentrations of two Taraxacum microspecies of contrasting mineral ecology: The role of inorganic ions in growth

The two microspecies were Taraxacum sellandii Dahlst., which usually occurs in heavily fertilized grasslands, and Taraxacum nordstedtii Dahlst., which on the whole is restricted to undisturbed and mineral‐poor habitats. Growth response curves were established, depicting the relative yield of (whole) plant tissue water and the internal K+ concentration (on a whole plant basis). The critical K+ concentration, i.e. the lowest [K+]i associated with maximal growth, was derived from the response curve. T. nordstedtii , the microspecies with the low maximal growth, showed a distinctly lower critical K+ concentration than T. sellandii. A relationship between growth potential and critical K+ concentration is proposed. Responses to a declining [K+]i differed between the two microspecies. The roots of T. nordstedtii stopped functioning as a sink for inulin, and mobilized additional carbohydrates for maintaining osmotic potential and growth. The productive strategy of the fast‐growing T. sellantlii is lacking such a mechanism to buffer effects of a declining [K+]i.
Various changes were noted as regards the internal concentrations of other inorganic ions, measured as a function of [K+]i, With declining [K+]i, internal NO‐3 decreased considerably in shoot and roots, especially in T. nordstedtii , while Mg2+ accumulated, especially in the roots of T. sellandii. The interactions between growth potential and the accumulation of inorganic ions are discussed