MODIFICATIONS OF THE CARBON AND NITROGEN ALLOCATIONS IN THE PLANT (TRITICUM-AESTIVUM L) SOIL SYSTEM IN RESPONSE TO INCREASED ATMOSPHERIC CO2 CONCENTRATION
G. Billes et al., MODIFICATIONS OF THE CARBON AND NITROGEN ALLOCATIONS IN THE PLANT (TRITICUM-AESTIVUM L) SOIL SYSTEM IN RESPONSE TO INCREASED ATMOSPHERIC CO2 CONCENTRATION, Plant and soil, 157(2), 1993, pp. 215-225
The aim of this work was to examine the response of wheat plants to a
doubling of the atmospheric CO2 concentration on: (1) carbon and nitro
gen partitioning in the plant, (2) carbon release by the roots; and (3
) the subsequent N uptake by the plants. The experiment was performed
in controlled laboratory conditions by exposing fast-growing spring wh
eat plants, during 28 days, to a (CO2)-C-14 concentration of 350 or 70
0 muL L-1 at two levels of soil nitrogen fertilization. Doubling CO2 a
vailability increased total plant production by 34% for both N treatme
nt. In the N-fertilized soil, the CO2 enrichment resulted in an increa
se in dry mass production of 41% in the shoots and 23% in the roots; w
ithout N fertilization this figure was 33% and 37%, respectively. In t
he N-fertilized soil, the CO2 increase enhanced the total N uptake by
14% and lowered the N concentration in the shoots by 23%. The N concen
tration in the roots was unchanged. In the N-fertilized soil, doubling
CO2 availability increased N uptake by 32% but did not change the N c
oncentrations, in either shoots or roots. The CO2 enrichment increased
total root-derived carbon by 12% with N fertilization, and by 24% wit
hout N fertilization. Between 85 and 90% of the total root derived-C-1
4 came from respiration, leaving only 10 to 15% in the soil as organic
C-14. However, when total root-derived C-14 was expressed as a functi
on of root dry weight, these differences were only slightly significan
t. Thus, it appears that the enhanced carbon release from the living r
oots in response to increased atmospheric CO2, is not due to a modific
ation of the activity of the roots, but is a result of the increased s
ize of the root system. The increase of root dry mass also resulted in
a stimulation of the soil N mineralization related to the doubling at
mospheric CO2 concentration. The discussion is focused on the interact
ions between the carbon and nitrogen allocation, especially to the roo
t system, and the implications for the acquisition of nutrients by pla
nts in response to CO2 increase.