Sinks for nitrogen inputs in terrestrial ecosystems: a meta-analysis of 15N tracer field studies

Authors
  • P.H. Templer
  • M.C. Mack
  • F.S. Chapin III
  • L.M. Christenson
  • J.E. Compton
  • H.D. Crook
  • W.S. Currie
  • C.J. Curtis
  • D.B. Dail
  • C.D.M. D'Antonio
  • B.A. Emmett
  • H.E. Epstein
  • C.L. Goodale
  • P. Gundersen
  • S.E. Hobbie
  • K. Holland
  • D.U. Hooper
  • B.A. Hungate
  • S. Lamontagne
  • K.J. Nadelhoffer
  • C.W. Osenberg
  • S.S. Perakis
  • P. Schleppi
  • J. Schimel
  • I.K. Schmidt
  • M. Sommerkorn
  • J. Spoelstra
  • A. Tietema
  • W.W. Wessel
  • D.R. Zak
Publication date 2012
Journal Ecology
Volume | Issue number 93 | 8
Pages (from-to) 1816-1829
Organisations
  • Faculty of Science (FNWI) - Institute for Biodiversity and Ecosystem Dynamics (IBED)
Abstract
Effects of anthropogenic nitrogen (N) deposition and the ability of terrestrial ecosystems to store carbon (C) depend in part on the amount of N retained in the system and its partitioning among plant and soil pools. We conducted a meta-analysis of studies at 48 sites across four continents that used enriched 15N isotope tracers in order to synthesize information about total ecosystem N retention (i.e. total ecosystem 15N recovery in plant and soil pools) across natural systems and N partitioning among ecosystem pools. The greatest ecosystem tracer 15N recoveries occurred in shrublands (mean = 89.5%) and wetlands (84.8%) followed by forests (74.9%) and grasslands (51.8%). In the short-term (<1 week after 15N tracer application), total ecosystem 15N recovery was negatively correlated with fine root and soil 15N natural abundance, and organic soil C and N concentration, but was positively correlated with mean annual temperature and mineral soil C:N. In the longer-term (3 to 18 months after 15N tracer application), total ecosystem 15N retention was negatively correlated with foliar natural abundance 15N, but was positively correlated with mineral soil C and N concentration and C:N, showing that plant and soil natural abundance 15N and soil C:N are good indicators of total ecosystem N retention. Foliar N concentration was not significantly related to ecosystem 15N tracer recovery, suggesting that plant N status is not a good predictor of total ecosystem N retention. Because the largest ecosystem sinks for tracer 15N were belowground in forests, shrublands, and grasslands, we conclude that growth enhancement and potential for increased C storage in aboveground biomass from atmospheric N deposition is likely to be modest in these ecosystems. Total ecosystem 15N recovery decreased with N fertilization, with an apparent threshold fertilization rate of 46 kg N ha-1 yr-1 above which most ecosystems showed net losses of applied tracer 15N in response to N fertilizer addition.
Document type Article
Language English
Related dataset Appendix A. Site characteristics and experimental design for 15N tracer studies included in the meta-analysis.
Published at https://doi.org/10.1890/11-1146.1
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