Ab. Samarakoon et Rm. Gifford, ELEVATED CO2 EFFECTS ON WATER-USE AND GROWTH OF MAIZE IN WET AND DRYING SOIL, Australian journal of plant physiology, 23(1), 1996, pp. 53-62
It is unclear from the literature as to whether growth of C-4 species
is responsive to elevated atmospheric CO2 concentration. Reports vary
between no response to strong response. To explore the origin of this
discrepancy, spaced plants of maize (Zea mays) were grown at atmospher
ic CO2 concentrations of 362 or 717 mu L L(-1) under continuously wet
or drying soil regimes. The aims were to evaluate the comparative grow
th promotion from elevated CO2 in a C-4 plant under the two contrastin
g water regimes and the causes of any such promotion, and also how wat
er-use efficiency (WUE) is influenced by high CO2 under the two water
regimes. In wet soil, transpiration rate was reduced on average by 29%
at high CO2 but neither total dry matter nor plant height was signifi
cantly affected by CO2 level. Leaf area was not influenced significant
ly, so daily water use per plant was 25% lower and WUE was increased e
ntirely due to reduced water use at high CO2. In soil that was drying
from field capacity, plants in high CO2 used about 30% less water than
those in ambient CO2 while the soil was still wet. This resulted in h
igher soil water content at high CO2. Plant growth showed a marked res
ponse, accumulating 35% more leaf area and 50% more dry matter. Young
internodes elongated up to 170% more, giving taller plants. The growth
enhancement was largely due to higher average net assimilation rate i
ndicating that C-4 photosynthesis responded to elevated CO2 during dro
ught. In drying soil the increase in WUE was due to both increased dry
matter and reduced water use, the contribution from each depending on
the stage of soil drying. We hypothesise therefore that literature ex
amples where maize growth responded to elevated CO2 may have involved
(possibly unrecognised) minor water deficits.