生态系统
陆地生态系统
环境科学
示踪剂
丰度(生态学)
灌木丛
δ15N
环境化学
生态学
农学
δ13C
化学
稳定同位素比值
生物
量子力学
物理
核物理学
作者
Pamela H. Templer,Michelle C. Mack,F. Stuart Chapin,Lynn M. Christenson,Jana E. Compton,H. D. Crook,William S. Currie,C. J. Curtis,D. B. Dail,Carla M. D’Antonio,Bridget A. Emmett,Howard E. Epstein,Christine L. Goodale,Per Gundersen,Sarah E. Hobbie,Keri Holland,David U. Hooper,Bruce A. Hungate,Sébastien Lamontagne,Knute J. Nadelhoffer
出处
期刊:Ecology
[Wiley]
日期:2012-08-01
卷期号:93 (8): 1816-1829
被引量:234
摘要
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 15 N isotope tracers in order to synthesize information about total ecosystem N retention (i.e., total ecosystem 15 N recovery in plant and soil pools) across natural systems and N partitioning among ecosystem pools. The greatest recoveries of ecosystem 15 N 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 15 N tracer application), total ecosystem 15 N recovery was negatively correlated with fine‐root and soil 15 N 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 15 N tracer application), total ecosystem 15 N retention was negatively correlated with foliar natural‐abundance 15 N but was positively correlated with mineral soil C and N concentration and C : N, showing that plant and soil natural‐abundance 15 N and soil C:N are good indicators of total ecosystem N retention. Foliar N concentration was not significantly related to ecosystem 15 N tracer recovery, suggesting that plant N status is not a good predictor of total ecosystem N retention. Because the largest ecosystem sinks for 15 N 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 15 N 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 15 N tracer in response to N fertilizer addition.
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