TY - JOUR
T1 - Soil [N] modulates soil C cycling in CO2-fumigated tree stands : a meta-analysis
AU - Dieleman, W. I. J.
AU - Luyssaert, S.
AU - Rey, A.
AU - De Angelis, P.
AU - Barton, C. V. M.
AU - Broadmeadow, M. S. J.
AU - Broadmeadow, S. B.
AU - Chigwerewe, K. S.
AU - Medlyn, B.
AU - [and fifteen others], null
PY - 2010
Y1 - 2010
N2 - Under elevated atmospheric CO2 concentrations, soil carbon (C) inputs are typically enhanced, suggesting larger soil C sequestration potential. However, soil C losses also increase and progressive nitrogen (N) limitation to plant growth may reduce the CO2 effect on soil C inputs with time. We compiled a data set from 131 manipulation experiments, and used meta-analysis to test the hypotheses that: (1) elevated atmospheric CO2 stimulates soil C inputs more than C losses, resulting in increasing soil C stocks; and (2) that these responses are modulated by N. Our results confirm that elevated CO2 induces a C allocation shift towards below-ground biomass compartments. However, the increased soil C inputs were offset by increased heterotrophic respiration (Rh), such that soil C content was not affected by elevated CO2. Soil N concentration strongly interacted with CO2 fumigation: the effect of elevated CO2 on fine root biomass and -production and on microbial activity increased with increasing soil N concentration, while the effect on soil C content decreased with increasing soil N concentration. These results suggest that both plant growth and microbial activity responses to elevated CO2 are modulated by N availability, and that it is essential to account for soil N concentration in C cycling analyses.
AB - Under elevated atmospheric CO2 concentrations, soil carbon (C) inputs are typically enhanced, suggesting larger soil C sequestration potential. However, soil C losses also increase and progressive nitrogen (N) limitation to plant growth may reduce the CO2 effect on soil C inputs with time. We compiled a data set from 131 manipulation experiments, and used meta-analysis to test the hypotheses that: (1) elevated atmospheric CO2 stimulates soil C inputs more than C losses, resulting in increasing soil C stocks; and (2) that these responses are modulated by N. Our results confirm that elevated CO2 induces a C allocation shift towards below-ground biomass compartments. However, the increased soil C inputs were offset by increased heterotrophic respiration (Rh), such that soil C content was not affected by elevated CO2. Soil N concentration strongly interacted with CO2 fumigation: the effect of elevated CO2 on fine root biomass and -production and on microbial activity increased with increasing soil N concentration, while the effect on soil C content decreased with increasing soil N concentration. These results suggest that both plant growth and microbial activity responses to elevated CO2 are modulated by N availability, and that it is essential to account for soil N concentration in C cycling analyses.
KW - biomass
KW - carbon sequestration
KW - microbial respiration
KW - nitrogen fertilizers
KW - roots (botany)
UR - http://handle.uws.edu.au:8081/1959.7/uws:33442
U2 - 10.1111/j.1365-3040.2010.02201.x
DO - 10.1111/j.1365-3040.2010.02201.x
M3 - Article
SN - 0140-7791
VL - 33
SP - 2001
EP - 2011
JO - Plant, Cell and Environment
JF - Plant, Cell and Environment
IS - 12
ER -