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Interactive effects of warming and increased nitrogen deposition on 15 N tracer retention in a temperate old field: seasonal trends
Author(s) -
TURNER MICHELLE M.,
HENRY HUGH A. L.
Publication year - 2009
Publication title -
global change biology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 4.146
H-Index - 255
eISSN - 1365-2486
pISSN - 1354-1013
DOI - 10.1111/j.1365-2486.2009.01881.x
Subject(s) - environmental science , global warming , growing season , nitrogen , temperate climate , ecosystem , shoot , agronomy , climate change , chemistry , ecology , biology , organic chemistry
The extent to which increased atmospheric nitrogen (N) deposition will drive changes in plant productivity and species composition over the next century will depend on how other influential global change factors, such as climate warming, affect the N retention of ecosystems. We examined the interactive effects of simulated climate warming and N deposition on the recoveries of 15 N‐labeled ammonium and 15 N‐labeled nitrate tracers added as a pulse to grass‐dominated, temperate old‐field plots at spring thaw. In addition to the year‐round warming treatment, a winter‐only warming treatment was applied to a set of plots to explore the contribution of this component of climate warming to the overall warming effect. By the end of the plant growing season, there was approximately twice as much 15 N enrichment in the plant roots and bulk soil from 15 NH 4 + ‐addition plots than from 15 NO 3 − ‐addition plots, but there were no effects of warming or N fertilization on 15 N recovery. Over winter, approximately half of the excess 15 N present in plant shoots was lost, which corresponded with large 15 N losses from bulk soil in N fertilized plots and large 15 N increases in bulk soil in nonfertilized plots. By the next spring, there was decreased 15 N recovery in plants in response to N fertilization, which was largely offset by increases in plant 15 N recovery in response to year‐round warming. However, 15 N retention in bulk soil, where the major part of the 15 N label was recovered, was approximately 40% higher in nonfertilized plots than in N fertilized plots. Overall, our results indicate that climate warming increases plant N sequestration in this system but this effect is overwhelmed by the overall effect of nitrogen deposition on ecosystem N losses.