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Volume 10, issue 2
Biogeosciences, 10, 999–1011, 2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Nitrogen and global change

Biogeosciences, 10, 999–1011, 2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 13 Feb 2013

Research article | 13 Feb 2013

Interactions between leaf nitrogen status and longevity in relation to N cycling in three contrasting European forest canopies

L. Wang1, A. Ibrom2, J. F. J. Korhonen3, K. F. Arnoud Frumau4, J. Wu2, M. Pihlatie3, and J. K. Schjoerring1 L. Wang et al.
  • 1Plant and Soil Science Section, Department of Plant and Environmental Sciences, Faculty of Science, University of Copenhagen Thorvaldsensvej 40, 1871 Frederiksberg C, Denmark
  • 2Technical University Denmark, Department of Chemical and Biochemical Engineering, Centre for Ecosystem & Environmental Sustainability, Frederiksborgvej 399, Risø-Campus, 4000 Roskilde, Denmark
  • 3Department of Physics, P.O. Box 48, 00014 University of Helsinki, Finland
  • 4ECN, Environmental Assessment group, P.O. Box 1, 1755 ZG, Petten, The Netherlands

Abstract. Seasonal and spatial variations in foliar nitrogen (N) parameters were investigated in three European forests with different tree species, viz. beech (Fagus sylvatica L.), Douglas fir (Pseudotsuga menziesii (Mirb.) Franco) and Scots pine (Pinus sylvestris L.) growing in Denmark, the Netherlands and Finland, respectively. The objectives were to investigate the distribution of N pools within the canopies of the different forests and to relate this distribution to factors and plant strategies controlling leaf development throughout the seasonal course of a vegetation period. Leaf N pools generally showed much higher seasonal and vertical variability in beech than in the coniferous canopies. However, also the two coniferous tree species behaved very differently with respect to peak summer canopy N content and N re-translocation efficiency, showing that generalisations on tree internal vs. ecosystem internal N cycling cannot be made on the basis of the leaf duration alone. During phases of intensive N turnover in spring and autumn, the NH4+ concentration in beech leaves rose considerably, while fully developed green beech leaves had relatively low tissue NH4+, similar to the steadily low levels in Douglas fir and, particularly, in Scots pine. The ratio between bulk foliar concentrations of NH4+ and H+, which is an indicator of the NH3 emission potential, reflected differences in foliage N concentration, with beech having the highest values followed by Douglas fir and Scots pine. Irrespectively of the leaf habit, i.e. deciduous versus evergreen, the majority of the canopy foliage N was retained within the trees. This was accomplished through an effective N re-translocation (beech), higher foliage longevity (fir) or both (boreal pine forest). In combination with data from a literature review, a general relationship of decreasing N re-translocation efficiency with the time needed for canopy renewal was deduced, showing that leaves which live longer re-translocate relatively less N during senescence. The Douglas fir stand, exposed to relatively high atmospheric N deposition, had by far the largest peak summer canopy N content and also returned the largest amount of N in foliage litter, suggesting that higher N fertility leads to increased turnover in the ecosystem N cycle with higher risks of losses such as leaching and gas emissions.

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