Nonlinear grassland responses to past and future atmospheric CO(2).
Carbon sequestration in soil organic matter may moderate increases in atmospheric CO(2) concentrations (C(a)) as C(a) increases to more than 500 micromol mol(-1) this century from interglacial levels of less than 200 micromol mol(-1) (refs 1 6). However, such carbon storage depends on feedbacks between plant responses to C(a) and nutrient availability. Here we present evidence that soil carbon storage and nitrogen cycling in a grassland ecosystem are much more responsive to increases in past C(a) than to those forecast for the coming century. Along a continuous gradient of 200 to 550 micromol mol(-1) (refs 9, 10), increased C(a) promoted higher photosynthetic rates and altered plant tissue chemistry. Soil carbon was lost at subambient C(a), but was unchanged at elevated C(a) where losses of old soil carbon offset increases in new carbon. Along the experimental gradient in C(a) there was a nonlinear, threefold decrease in nitrogen availability. The differences in sensitivity of carbon storage to historical and future C(a) and increased nutrient limitation suggest that the passive sequestration of carbon in soils may have been important historically, but the ability of soils to continue as sinks is limited.
Gill
Richard A
RA
Department of Biology, Duke University, Durham, NC 27708-0340, USA. rgill@wsu.edu
Polley
H Wayne
HW
Johnson
Hyrum B
HB
Anderson
Laurel J
LJ
Maherali
Hafiz
H
Jackson
Robert B
RB
D001272:Atmosphere / Q000737:chemistry*; D018533:Biomass; D002244:Carbon / Q000378:metabolism; D002245:Carbon Dioxide / Q000378:metabolism*; D017753:Ecosystem; D009584:Nitrogen / Q000378:metabolism; D010100:Oxygen / Q000378:metabolism; D010788:Photosynthesis; D006109:Poaceae / Q000502:physiology*; D012987:Soil / Q000032:analysis*
D012987:Soil; D002245:Carbon Dioxide; D002244:Carbon; D009584:Nitrogen; D010100:Oxygen