The objectives of this paper were to review the literature on the responses
of root systems to elevated CO2 in intact, native grassland ecosystems, an
d to present the results from a 2-yr study of root production and mortality
in an intact calcareous grassland in Switzerland. Previous work in intact
native grassland systems has revealed that significant stimulation of the s
ize of root systems (biomass, length density or root number) is not a unive
rsal response to elevated CO2. Of the 12 studies reviewed, seven showed lit
tle or no change in root-system size under elevated CO2, while five showed
marked increases (average increase 38%). Insufficient data are available on
the effects of elevated CO2 on root production, mortality and life span to
allow generalization about effects. The diversity of experimental techniqu
es employed in these native grassland studies also makes generalization dif
ficult. In the present study, root production and mortality were monitored
rn situ in a species-rich calcareous grassland community using minirhizotro
ns in order to test the hypothesis that an increase in these two measures w
ould help explain the increase in net ecosystem CO2 uptake (net ecosystem e
xchange) previously observed under elevated CO2 at this site (600 vs 350 mu
l CO2 l(-1); eight 1.2-m(2) experimental plots per CO2 level using the scr
een-aided CO2 control method). However, results from the first 2 yr showed
no difference in overall root production or mortality in the top 18 cm of s
oil, where 80-90% of the roots occur. Elevated CO2 was associated with an u
pward shift in root length density: under elevated CO2 a greater proportion
of roots were found in the upper 0-6-cm soil layer, and a lower proportion
of roots in the lower 12-18 cm, than under ambient CO2. Elevated CO2 was a
lso associated with an increase in root survival probability (RSP; e.g. for
roots still alive 280 d after they were produced under ambient CO2, RSP =
0.30; elevated CO2, RSP = 0.56) and an increase (48% ) in median root life
span in the deepest (12-18 cm) soil layer. The factors driving changes in r
oot distribution and longevity with depth under elevated CO2 were not clear
, but might have been related to increases in soil moisture under elevated
CO2 interacting with vertical patterns in soil temperatures. Thus extra CO2
taken up in this grassland ecosystem during the growing season under eleva
ted CO2 could not be explained by changes in root production and mortality.
However, C and nutrient cycling might be shifted closer to the soil surfac
e, which could potentially have a substantial effect on the activities of s
oil heterotrophic organisms as CO2 levels rise.