| Literature DB >> 22928411 |
P H Templer1, 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.
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.Entities:
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Year: 2012 PMID: 22928411 DOI: 10.1890/11-1146.1
Source DB: PubMed Journal: Ecology ISSN: 0012-9658 Impact factor: 5.499