Abstract

We evaluated effects of atmospheric deposition of nitrogen on the composition of forest understorey vegetation both in space and time, using repeated data from the European wide monitoring program ICP‐Forests, which focuses on normally managed forest. Our aim was to assess whether both spatial and temporal effects of deposition can be detected by a multiple regression approach using data from managed forests over a relatively short time interval, in which changes in the tree layer are limited. To characterize the vegetation, we used indicators derived from cover percentages per species using multivariate statistics and indicators derived from the presence/absence, that is, species numbers and Ellenberg's indicator values. As explanatory variables, we used climate, altitude, tree species, stand age, and soil chemistry, besides deposition of nitrate, ammonia and sulfate. We analyzed the effects of abiotic conditions at a single point in time by canonical correspondence analysis and multiple regression. The relation between the change in vegetation and abiotic conditions was analyzed using redundancy analysis and multiple regression, for a subset of the plots that had both abiotic data and enough species to compute a mean Ellenberg N value per plot using a minimum of three species. Results showed that the spatial variation in the vegetation is mainly due to “traditional” factors such as soil type and climate, but a statistically significant part of the variation could be ascribed to atmospheric deposition of nitrate. The change in the vegetation over the past c. 10 years was also significantly correlated to nitrate deposition. Although the effect of deposition on the individual species could not be clearly defined, the effect on the vegetation as a whole was a shift toward nitrophytic species as witnessed by an increase in mean Ellenberg's indicator value.

Highlights

  • Ecological effects of atmospheric deposition were first noticed in the 1960s (Odén, 1967) and generated extensive public debate, especially after large-­scale forest dieback had been predicted in the

  • To arrive at a better understanding of the response of forest vegetation to its abiotic environment, we fist analyzed the relation between vegetation at a single point in time on the one hand and abiotic and biotic conditions on the other

  • There appeared to be no significant effect of deposition on the change in the number of species, nor on the Lennon dissimilarity; these variables were only significantly influenced by soil chemistry

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Summary

| INTRODUCTION

Ecological effects of atmospheric deposition were first noticed in the 1960s (Odén, 1967) and generated extensive public debate, especially after large-­scale forest dieback had been predicted in the. It cannot be expected that forest management is constant over such a long period, whereas in unmanaged reserves succession in the tree layer will alter the environmental conditions for the understorey vegetation In their detailed resampling study of understorey vegetation in forest reserves in Central Europe, Verheyen et al (2012) found a significant overall increase in Ellenberg’s (1991) nutrient availability indicator (N), a marginally significant decrease in Ellenberg’s light indicator (L) but no significant change in species number. It could be hypothesized that due to the long observation period of Verheyen et al.’s (2012) study (17–67 years) in combination with the exclusive use of data from forest reserves, the changes in the tree layer have been so large that they mask the effect of deposition on understorey vegetation. To arrive at a better understanding of the response of forest vegetation to its abiotic environment, we fist analyzed the relation between vegetation at a single point in time on the one hand and abiotic and biotic conditions (i.e., soil, climate, deposition, and dominant tree species) on the other

| MATERIALS AND METHODS
Findings
| DISCUSSION AND CONCLUSIONS
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