Soil‐plant element relationships in a tundra ecosystem Article

Marion, GM, Hastings, SJ, Oberbauer, SF et al. (1989). Soil‐plant element relationships in a tundra ecosystem . ECOGRAPHY, 12(3), 296-303. 10.1111/j.1600-0587.1989.tb00849.x

cited authors

  • Marion, GM; Hastings, SJ; Oberbauer, SF; Oechel, WC

authors

abstract

  • The objectives of this study were to (1) provide a baseline estimate of soil and plant element concentrations for an intensive research site at Imnavait Creek in northern Alaska, and (2) examine the relationships between soil and plant elements in an arctic ecosystem. Soil and plant element concentrations were highly variable along biotic, spatial, and temporal axes. Deciduous shrubs had higher leaf concentration of N, P. K and Mg, whereas an evergreen shrub had higher leaf concentrations of Ca, Mn, Al and Si. Based on high required solution phase turnover rates, the most likely elemental deficiencies are N > P > K > Ca = Mg. Based on low required solution phase turnover rates and high soil concentrations. Fe, Mn, Zn and Cu deficiencies are unlikely. Manganese could be present in toxic concentrations. The nutrient bottleneck in tundra ecosystems appears to be the rate of nutrient movement to the solution phase. Copyright © 1989, Wiley Blackwell. All rights reserved

publication date

  • January 1, 1989

published in

Digital Object Identifier (DOI)

start page

  • 296

end page

  • 303

volume

  • 12

issue

  • 3