HIGH VAPOR-PRESSURE DEFICIT AND LOW SOIL-WATER AVAILABILITY ENHANCE SHOOT GROWTH-RESPONSES OF A C-4 GRASS (PANICUM-COLORATUM CV BAMBATSI) TO CO2 ENRICHMENT
Sp. Seneweera et al., HIGH VAPOR-PRESSURE DEFICIT AND LOW SOIL-WATER AVAILABILITY ENHANCE SHOOT GROWTH-RESPONSES OF A C-4 GRASS (PANICUM-COLORATUM CV BAMBATSI) TO CO2 ENRICHMENT, Australian journal of plant physiology, 25(3), 1998, pp. 287-292
The hypothesis that shoot growth responses of C-4 grasses to elevated
CO2 are dependent on shoot water relations was tested using a C-4 gras
s, Panicum coloratum (NAD-ME subtype). Plants were grown for 35 days a
t CO2 concentrations of 350 or 1000 mu L CO2 L-1. Shoot water relation
s were altered by growing plants in soil which was brought daily to 65
, 80 or 100% field capacity (FC) and by maintaining the vapour pressur
e deficit (VPD) at 0.9 or 2.1 kPa. At 350 mu L CO2 L-1, high VPD and l
ower soil water content depressed shoot dry mass, which declined in pa
rallel at each VPD with decreasing soil water content. The growth depr
ession at high VPD was associated with increased shoot transpiration,
whereas at low soil water, leaf water potential was reduced. Elevated
CO2 ameliorated the impact of both stresses by decreasing transpiratio
n rates and raising leaf water potential. Consequently, high CO2 appro
ximately doubled shoot mass and leaf length at a VPD of 2.1 kPa and so
il water contents of 65 and 80% FC but had no effect on unstressed pla
nts. Water use efficiency was enhanced by elevated CO2 under condition
s of stress but this was primarily due to increases in shoot mass. Hig
h CO2 had a greater effect on leaf growth parameters than on stem mass
. Elevated CO2 increased specific leaf area and leaf area ratio, the l
atter at high VPD only. We conclude that high CO2 increases shoot grow
th of C-4 grasses by ameliorating the effects of stress induced by eit
her high VPD or low soil moisture. Since these factors limit growth of
field-grown C-4 grasses, it is likely that their biomass will be enha
nced by rising atmospheric CO2 concentrations.