Affiliation:
1. Institute of Forest Ecology, Department of Forest and Soil Sciences, University of Natural Resources and Life Sciences (BOKU), Peter-Jordan-Straße 82, 1190 Vienna, Austria
Abstract
The growth of forest trees in the relatively young soils of Europe has historically been limited by nitrogen (N). The high anthropogenic N deposition and intense forest management during the last century, however, have caused forest trees in large areas to show signs of being limited by phosphorus (P) or base cations. This indicates that the current situation is not sustainable. The net addition of N to forests here stems from deposition and N fixation, both processes that add N to the topsoil. Phosphorus and cations are released by weathering in the mineral soil. Do European trees have what it takes to efficiently take up P and cation nutrients when they become scarce? Important factors influencing their capacity to take up P and cations are their roots’ distribution and function, mycorrhizal distribution and type, and the response of their root and mycorrhizal growth and function to N depositions and nutrient deficiencies. The literature shows that the ability to be limited by something other than nitrogen will be hardest for shallow-rooted conifer trees, followed by ectomycorrhizal deciduous trees; arbuscular mycorrhizal trees will handle the shift best. This knowledge should be incorporated into forest growth models to promote sustainable management decisions.
Funder
University of Natural Resources and Life Sciences Vienna
Reference97 articles.
1. Sverdrup, H., and Stjernquist, I. (2002). Nutrient sustainability for Swedish forests. Developing Principles and Models for Sustainable Forestry in Sweden, Kluwer Academic Publishers.
2. Krüger, I.S.T., Potočić, N., and Ukonmaanaho, L.P.R. (2020). Increased Evidence of Nutrient Imbalances in Forest Trees across Europe, ICP Forests Brief 4, Thünen Institute of Forest Ecosystems.
3. Ice age legacies in the geographical distribution of tree species richness in Europe;Svenning;Global Ecol. Biogeogr.,2007
4. Chemical and biological gradients along the Damma Glacier soil chronosequence (Switzerland);Bernasconi;Vadose Zone J.,2011
5. Tamm Review: Revisiting the influence of nitrogen deposition on Swedish forests;Binkley;For. Ecol. Manage.,2016