Due to the CO 2 greenhouse effect, elevated atmospheric concentration leads to higher temperatures, accompanied by episodes of less water availability in semiarid and arid areas or drought periods. Studies investigating these three factors (CO 2 , temperature and water availability) simultaneously in grapevine are scarce. The present work aims to analyze the combined effects of high CO 2 (700 ppm), high temperature (ambient +4 C) and drought on the photosynthetic activity, biomass allocation, leaf non-structural carbon composition, and carbon/nitrogen (C/N) ratio in grapevine. Two grapevine cultivars, red berry Tempranillo and white berry Tempranillo, were used, the latter being a natural, spontaneous mutant of the red cultivar. The experiment was performed on fruit-bearing cuttings during a 3-month period, from June (fruit set) to August (maturity). The plants were grown in research-oriented facilities, temperature-gradient greenhouses, where temperature, CO 2 , and water supply can be modified in a combined way.Drought had the strongest effect on biomass accumulation compared to the other environmental variables, and root biomass allocation was increased under water deficit. CO 2 and temperature effects were smaller and depended on cultivar, and on interactions with the other factors. Acclimation effects were observed on both cultivars as photosynthetic rates under high atmospheric CO 2 were reduced by long-term exposition to elevated CO 2 . Exposure to such high CO 2 resulted in increased starch concentration and reduced C/N ratio in leaves.A correlation between the intensity of the reduction in photosynthetic rates and the accumulation of starch in the leaves was found after prolonged exposure to elevated CO 2 .
| INTRODUCTIONIn many agricultural areas, precipitation patterns are expected to change in the future, with more frequent drought events in semiarid and arid regions and others where precipitation will likely increase (IPCC, 2013). A Representative Concentration Pathway (RCP) is an atmospheric greenhouse gas concentration trajectory considered possible in the future by the Intergovernmental Panel on Climate Change (IPCC). With respect to CO 2 , the concentration may increase to somewhere between 670 and 936 ppm by the year 2100 (RCP 6.0 and RCP 8.5 respectively, depending on the volume of CO 2 emitted in the years to come) (Moss et al., 2008(Moss et al., , 2010. According to the concentration-driven Coupled Model Intercomparison Project 5 (CMIP5) model simulations, the CO 2 increases are expected to raise the global mean temperature by 2.2 ± 0.5 and 3.7 ± 0.7 C, respectively (IPCC, 2013;Taylor et al., 2012).