, Volume 158, Issue 2, pp 371–371

Foliar δ15N values characterize soil N cycling and reflect nitrate or ammonium preference of plants along a temperate grassland gradient

Open Access

DOI: 10.1007/s00442-008-1133-8

Cite this article as:
Kahmen, A., Wanek, W. & Buchmann, N. Oecologia (2008) 158: 371. doi:10.1007/s00442-008-1133-8

Erratum to: Oecologia (2008) 156:861–870 DOI 10.1007/s00442-008-1028-8

Unfortunately, the publisher printed Fig. 2 with errors. The correct Fig. 2 is given here.
Fig. 2

Simple linear regression analyses between δ15N of bulk soil and leaf δ15N for different forb and grass species as well as the relationship between daily net mineralization (Nmin) and foliar Δδ15N (δ15N plant − δ15N soil) for different forb and grass species in 18 temperate grasslands. d−1 Day−1

Copyright information

© Springer-Verlag 2008

Authors and Affiliations

  • Ansgar Kahmen
    • 1
    • 3
  • Wolfgang Wanek
    • 2
  • Nina Buchmann
    • 1
    • 4
  1. 1.Max Planck Institute for BiogeochemistryJenaGermany
  2. 2.Department of Chemical Ecology and Ecosystem ResearchUniversity of ViennaViennaAustria
  3. 3.Center for Stable Isotope Biogeochemistry, Department of Integrative BiologyUniversity of CaliforniaBerkeleyUSA
  4. 4.Institute of Plant SciencesETH ZurichZurichSwitzerland

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