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Sinks for nitrogen inputs in terrestrial ecosystems: a meta-analysis of 15N tracer field studies
Authors:Templer P H  Mack M C  Chapin F S  Christenson L M  Compton J E  Crook H D  Currie W S  Curtis C J  Dail D B  D'Antonio C M  Emmett B A  Epstein H E  Goodale C L  Gundersen P  Hobbie S E  Holland K  Hooper D U  Hungate B A  Lamontagne S  Nadelhoffer K J  Osenberg C W  Perakis S S  Schleppi P  Schimel J  Schmidt I K  Sommerkorn M  Spoelstra J  Tietema A  Wessel W W  Zak D R
Affiliation:Department of Biology, Boston University, 5 Cummington Street, Boston, Massachusetts 02215, USA. ptempler@bu.edu
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 x ha(-1) x yr(-1) above which most ecosystems showed net losses of applied 15N tracer in response to N fertilizer addition.
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