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

  • P. H. Templer
  • , M. C. Mack
  • , F. S. Chapin
  • , L. M. Christenson
  • , J. E. Compton
  • , H. D. Crook
  • , W. S. Currie
  • , C. J. Curtis
  • , D. B. Dail
  • , C. 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

Research output: Contribution to journalArticlepeer-review

225 Scopus citations

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 recoveries of ecosystem 15N tracer 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 (3-18 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 15N tracer were below ground 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 15N tracer in response to N fertilizer addition.

Original languageEnglish (US)
Pages (from-to)1816-1829
Number of pages14
JournalEcology
Volume93
Issue number8
DOIs
StatePublished - Aug 2012

Keywords

  • Atmospheric nitrogen deposition
  • Carbon storage
  • Data synthesis
  • Meta-analysis
  • Nitrogen retention and loss
  • Stable isotopes

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