Abstract

SUMMARYCrops of winter wheat (Triticum aestivumL. cv. Hereward) were grown within temperature gradient tunnels at a range of temperatures at eitherc.350 or 700 μmol mol−1CO2in 1991/92 and 1992/93 at Reading, UK. At terminal spikelet stage, leaf area was 45% greater at elevated CO2in the first year due to more tillers, and was 30% greater in the second year due to larger leaf areas on the primary tillers. At harvest maturity, total crop biomass was negatively related to mean seasonal temperature within each year and CO2treatment, due principally to shorter crop durations at the warmer temperatures. Biomass was 6–31% greater at elevated compared with normal CO2and was also affected by a positive interaction between temperature and CO2in the first year only. Seed yield per unit area was greater at cooler temperatures and at elevated CO2concentrations. A 7–44% greater seed dry weight at elevated CO2in the first year was due to more ears per unit area and heavier grains. In the following year, mean seed dry weight was increased by > 72% at elevated CO2, because grain numbers per ear did not decline with an increase in temperature at elevated CO2. Grain numbers were reduced by temperatures > 31 °C immediately before anthesis at normal atmospheric CO2in 1992/93, and at both CO2concentrations in 1991/92. To quantify the impact of future climates of elevated CO2concentrations and warmer temperatures on wheat yields, consideration of both interactions between CO2and mean seasonal temperature, and possible effects of instantaneous temperatures on yield components at different CO2concentrations are required. Nevertheless, the results obtained suggest that the benefits to winter wheat grain yield from CO2doubling are offset by an increase in mean seasonal temperature of only 1·0 °C to 1·8 °C in the UK.

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