On-line version ISSN 0253-939X
S. Afr. J. Enol. Vitic. vol.36 n.2 Stellenbosch 2015
F. Jara-RojasI; S. Ortega-FariasI, II, *; H. Valdés-GómezI, II; C. Acevedo-OpazoI, II
IFacultad de Ciencias Agrarias, Universidad de Talca, P.O. Box 747, Talca 346-0000, Chile
IICITRA, Universidad de Talca, P.O. Box 747, Talca 346-0000, Chile
A study was carried out to evaluate the leaf gas exchange relations and water-use efficiency (WUE) of ungrafted Carménère (Vitis vinifera L.) grapevines growing under field conditions and different levels of water stress. Stomatal conductance (gs), transpiration (E), net CO2 assimilation (AN) and stem water potential (i*s) were measured at midday in a drip-irrigated commercial vineyard located in the Maule Valley (Chile) during three growing seasons (2005 to 2009). In addition, the instantaneous (AN/E) and intrinsic (AN/gs) water-use efficiencies and stomatal sensitivity factor (k) were estimated for the own-rooted grapevines. In this study a significant non-linear relationship was observed between AN and gs (r2 = 0.82), with values of AN decreasing from 14.9 to 3.5 pmol/m2/sec as gs diminished from 0.5 to 0.05 mol/m2/sec. This resulted in a progressive increase in WUEi (intrinsic water use efficiency). A significant linear relationship was observed between i*s and gs (r2 = 0.39) for measurements taken before and after véraison, with an increasing scattering from -1.6 to -0.4 MPa. Finally, k decreased as water stress increased, with values of 234 and 120 for no and severe water stress respectively, while k ranged from 264 to 480 and 255 to 297 for the measurements taken before and after véraison respectively. Based on the results obtained in the present study, the cultivar Carménère could be classified as drought tolerant at low water potentials, with a large range of physiological parameters changing in response to water stress.
Key words: Water stress, irrigation, stomatal sensitivity, Carménère grapevines
'Carménère' is an emblematic grapevine cultivar in Chile, and has recently been reintroduced to commercial production after its disappearance from Europe during the 19th century. Because the Carménère grapevines are not spread worldwide, few studies on its leaf gas exchange relations and water-use efficiencies have been published. Furthermore, studies of cv. Carménère growing under field conditions and natural variability become an important topic, especially when taking into account the exceptional sanitary conditions in Chile (i.e. absence of Phylloxera), which allow grapevines to grow without grafting and to express their genotypic characteristics. Any knowledge about leaf gas exchange relations generated under field conditions could lead to the development of irrigation tools oriented to optimise water productivity and improve berry composition (Basile et al., 2012; Fernandes de Oliveira et al., 2013; Shellie, 2014).
Under semi-arid conditions, with no or a reduced water supply (i.e. regulated deficit irrigation), vine water stress gradually increases as both soil water depletion and atmospheric water demand are augmented during the growing season. In this case, photosynthetic activity decreases due to stomatal and non-stomatal limitations (Moutinho-Pereira et al., 2004). This situation occurs very slowly until a certain level of water deficit, after which the photosynthetic activity decreases rapidly (Pellegrino et al., 2006). Stomatal closure in response to chemical signals synthesised in the dehydrating roots (including abscisic acid) is generally accepted to be the main factor for the depletion of photosynthesis (AN) and gas exchange under mild to moderate water stress (Chaves et al., 2010). When the drought period is lengthened, dehydration is more severe, or other environmental stresses are superimposed and a decline in mesophyll photosynthesis may occur because of a down-regulation process (Medrano et al., 2002). If this condition persists, irreversible reductions in dry matter accumulation and failure of grape maturation may occur. Flexas et al. (2002) have suggested that the stomatal conductance (gs) could be an integrative indicator of water stress intensity in relation to photosynthesis (via a coupled AN-gs relationship), as well as serving to unify data from different experiments and allowing the examination of a continuous gradient of water stress. Also, the AN-gs relationship could be an informative tool to demonstrate how other types of stress may influence photosynthesis and water-use efficiency (Naor & Wample, 1995). Cifre et al. (2005) suggest that three phases of photosynthesis response can be identified along a water stress gradient using stomatal conductance as a physiological indicator. In this regard, gs values are from 0.7 to 0.15, 0.15 to 0.05 and < 0.05 mol H2O/ m2/sec for the mild, moderate and severe water stress phases, respectively.
Since the water scarcity in viticultural areas is increasing progressively, the need for better water-use efficiency in grapevines is increasingly urgent. Moreover, additional knowledge of the mechanisms involved in grapevine tolerance to water stress and a better understanding of its genetic variability will be relevant to future breeding improvement (Chaves et al., 2010; Flexas et al., 2010). In this sense, water-use efficiency to leaf level has been studied in several grapevine cultivars around the world under very different growing conditi=ns. UnUer different soil water and atmospheric conditions, stomatal regulation allows plants to reduce fluctuations in the water status of tissues and hold xylem integrity (Prieto et al., 2010). According to their stomatal control, vines can be classified physiologically into two categories (Tardieu & Simonneau, 1998; Schultz, 2003; Prieto et al., 2010): (i) isohydric or near-isohydric vines that maintain tight stomatal regulation of the transpiration rate, resulting in nearly constant leaf water potential in drought-exposed and well-irrigated conditions. In contrast, (ii) anisohydric vines display lower stomatal control of transpiration, resulting in large fluctuations in leaf wate potential under soil water deficit and high evaporative demand. These conditions allow the vines higher rates of gas exchange and assimilation.
Also, stomatal sensitivity and the degree of coupling of stomatal conductance and photosynthesis generally have been considered in relation to single variables, mostly because interactions between factors have been difficult to quantify in a simple way. In this regard, Ball et al. (1987) demonstrated that gs as a function of the 'Ball factor' (see Equation 4) would yield a linear relationship between gs and AN measured under different levels of CO2 concentration, light intensities, vapour pressure deficit and temperature. The slope of this relationship is named the sensitivity factor (k), and it has been used successfully to evaluate stomatal responsiveness to water stress in several Vitis species and cultivars (Schultz et al., 1999; Schultz, 2000).
Unpublished field data suggest the Carménère cultivar presents an anisohydric-like behaviour, since stomatal conductance remains relatively high with moderate to strong water stress and saturating light conditions. As working hypothesis, the cv. Carménère has the ability to maintain a significant assimilation rate and stomatal conductance under increasing water stress. Thus, the objective of this study was to assess leaf gas exchange relations and water-use efficiency of ungrafted Carménère grapevines (Vitis vinifera L.) growing in a drip-irrigated commercial vineyard.
MATERIALS AND METHODS
Field data were collected from a drip-irrigated Carménère commercial vineyard in the 2005/2006, 2007/2008 and 2008/2009 growing seasons. The vineyard, with 11-year-old plants at the beginning of the experiment, was located in the Talca Valley, Maule Region, Chile (35°25.170' S, 71°33.228' W, WGS 84; 137 m.a.s.l.). The own-rooted vines were trained on a Geneva double curtain (GDC) (spacing 3.3 m between rows and 1.5 m within the row) and pruned into two bilateral spur cordons (12 buds per cordon), with the fruiting zone at 1.8 m above ground and vine rows oriented 330° NW. The canopy geometry of this training system was conserved after bloom (about mid-November) by hedging two or three times during the summer. The soil texture was clay loam with a rooting depth of 150 cm. It is classified as Talca series (fine family, mixed, thermic Ultic Haploxeralf). From 0 to 150 cm, the bulk density, field capacity, wilting point and available water were 1.36 g/cm3, 0.31 m3/m3, 0.13 m3/m3 and 0.18 m3/m3, respectively. Standard agronomical practices were performed during each season for sanitary care and productivity.
Water requirements and irrigation
Vineyard evapotranspiration was calculated as:
where ETv is the actual evapotranspiration of the vineyard (mm/day), ET0 is the reference evapotranspiration (mm/day) computed using the Penman-Monteith model (Allen et al., 1998), and Kc is the crop coefficient assigned according to phenologicalstage (dimensionier). Kc values were 0.11, 0.24, 0.61 and 0.49 for budburst, setting, véraison and near to harvest respectively. These Kc values were obtained using measurements of midday stem water potential (Ψs and soil water content during a three-year experiment (unpublished data), and were similar to those indicated by Acevedo-Opazo et al. (2010) and Ortega-Farias et al. (2005).
Waterwas supplied to the vineyard making use of two 2.0 L/h drippers per plant at a frequency of two times per week. Also, the irrigation timing varied according to atmospheric demand and the application of regulated deficit irrigation with fho aim ofimproving berry quality. Due to the high soil water-holding capacity of the rooting zone (270 mm), the first irrigations were applied in late December or early January, which corresponded to the phenological stages between post-setting and before véraison. In this case, the farmer applied about 2 990, 2 570 and 3 140 m3/ha/season, while the yield was 9.0, 9.2 and 11.0 t/ha for the 2005/2006, 2007/2008 and 2008/2009 growing seasons respectively. The increase in water application was associated with a higher atmospheric demand observed during the last season
Standard weather variables used to calculate ET0 from a reference grass were collected at 30-min intervals using an automatic meteorological station (Adcon Telemetry, model A730, Klosterneuburg, Austria), located about 8 km NW from the experimental site. Air temperature (T), relative humidity (RH), solar radiation (Rs), precipitation (P), wind velocity (Wv) and direction (Wd) were measured from 1 May to 30 April of each year.
Growing degree-days and seasonal dryness characterisation
To characterise the climatic conditions at the experimental site, growing degree-day s ( GDD, °Cd) and dryness index (DI, mm) were estimated for each growing season. The GDD were calculated as:
where Tmax and Tmin are daily maximum and minimum temperatures (° C) respectively, and Tb is the base temperature (10 °C).The phenological stages of the vines were observed in 18 representative vines across the experimental field using the modified Eichhorn and Lorenz system (Coombe, 1995). Two fruit-bearing shoots per plant were selected and labelled ft)r the successivereadings.
For the three seasons, the dryness index (DI, mm) was calcmated followingthe methodology proposed by Tonietto and Carbonneau (2004):
where W0 is the initial useful soil water reserve available at the rooting depth (200 mm), P is the monthly precipitation (mm), Tvis the monthly potential transpiration in the vineyard (mm) and Esis the monthly direct evaporation from the soil (mm). Using DI, climates are considered to be humid (DI > 150 mm), sub-humid (150 > DI > 50 mm), moderately dry (50 > DI > -100 mm) or very dry (DI < -100 mm).
Leaf gas exchange measurement
An infrared gas analyser (ADC BioScientific Ltd., model LCi, Hoddesdon, UK) was used to estimate midday values of photosynthetically active radiation (PAR), stomatal conductance (gs), transpiration (E), net CO2 assimilation (AN) and CO2 concentrations both internal (Ci) and external (Ca) to the atmosphere. CO2 mesophyll conductance (gm, AN/ Ci), intrinsic (WUEi, AN/gs) and instantaneous (WUE, AN/E) water-use efficiencies also were calculated. Mesophyll conductance to CO2 was calculated as the ratio of AN/(Ci-Cc), assuming that the CO2 partial pressure at the site of carboxylation (Cc) is zero (Candolfi-Vanconcelos & Koblet, 1991; Moutinho-Pereira et al., 2004).
A total of 362 fully expanded, mature, sun-exposed, healthy leaves were chosen from the mid-zone of the canopy (6th leaf from the tip on fruit-bearing shoots). The measurements of leaf gas exchange were made between 12:00 and 14:00 local time (solar zenith) on fully sunny days without changing the original position of the selected leaves in the canopy and maintaining the same light regime, ensuring a saturating sunlight exposure of the leaves (PAR > 800 μmol/m2/sec).
Plant water status
To evaluate vine water status, midday stem water potential (¾¾ was measured using a pressure chamber (PMS Instrument Co., model 600, Corvallis, Oregon, USA). Fully expanded, healthy leaves were wrapped with plastic transparent film and aluminium foil at least 2 h before taking the measurements, allowing an equilibrium between leaf and plant xylem water status to be achieved (Scholander et al., 1965; Begg & Turner, 1970; Choné et al., 2001). Care was taken to minimise water loss during the transfer of the leaf to the chamber, so less than 30 sec were allowed to pass between the excision of the petiole and the measurement. The measurements of ΨFs and leaf gas exchange were taken every 20 days from December (one month before véraison) to March (near harvest) in each growing season.
Several thresholds of plant water status to define water stress levels have been developed for different grapevine cultivars (Carbonneau & Costanza, 2004; Sibille et al., 2007; Van Leeuwen et al., 2009). To define the level of water stress in this study, data were divided into ranges according to the thresholds proposed by Van Leeuwen et al. (2009): i) no water deficit (Ψs > -0.6 MPa), ii) weak water deficit (-0.9 MPa < ΨFs < -0.6 MPa), iii) moderate to weak water deficit (-1.1 MPa < ΨFs < -0.9 MPa), iv) moderate to severe water deficit (-1.4 MPa < ΨFs < -1.1 MPa) and v) severe water deficit(-l .CMPa> Ψs).
Stomatal sensitivity factor
Cultivar-specific stomatal sensitivity was analysed using the model approach of Ball et al. (1987) that allows the evaluation of the stomatal conductance response to the combined effects of climatic variables through a stomatal sensitivity factor (k) calculated by a linear regression analysis (Prieto et al., 2010):
where g0 is a residual stomatal conductance (mmol/m2/ sec); AN is the net CO2 assimilation ^mol/m2/sec); RH is the relative humidity (%); and Ca is CO2 concentration at the leaf surface μmol/mol). Also, the factor 'AN (RH/Ca)' is termed the 'Ball factor'. Schultz et al. (1999) indicated that a higher value of k means less stomatal responsiveness to water stress (inverse relationship between k and stomatal closure control), consequently leading to lower WUE and WUEi.
Data filtering and analysis
The whole database of gas exchange was submitted to an exploratory data analysis to determine the existence of measurement errors. Data were removed from the dataset when (i) the temperature within the infrared gas analyser chamber was over 42 °C (Jacobs et al., 1996; Jara-Rojas et al., 2009), and (ii) when gs and/or Ci where close or equal to zero under saturating sunlight conditions (PAR > 800 μmol/ m2/sec; Prieto et al., 2010).
Non-linear regressions between AN and gs, Ci and gs, gm and gs, AN/gs and gs and AN/E and gs were developed for different levels of vine water status. For these levels, linear regressions between gs and the 'Ball factor' also were done to calculate the values of k before and after véraison. It is important to indicate that the stomatal sensitivity factor corresponds to the slope of the linear regression. The coefficient of determination (r2) was used to evaluate how well the regression line represents the data (percentage of the data that is the closest to the line of best fit.
Furthermore, a statistical analysis of climatic data was performed using the Kruskal-Wallis range test, while that for vine water status was done using a two-way ANOVA. The mean separation was done using Tukey's test at a 95% confidence level (P-value < 0.05).
Local growing conditions
In general, the seasonal mean values of Tmax, VPD and GDD were statistically higher during the 2008/2009 season than during the other seasons (Table 1). Also, the seasonal Tmin was lower during the 2007/2008 season in comparison with the other seasons, but there was not a significant difference in Rs values among the seasons. The highest atmospheric demand was observed between setting and véraison, with the mean values of Tmax and Tmin. ranging between 29.3 and 30.3°C and 12.5 and 13.1 °C, respectively. The mean seasonal values of VPD ranged between 0.6 and 0.9 kPa, while those of R were between 21.4 and 22.6 MJ/m2/d. The seasonal values of GDD were between 1 632 and 1 793°C, which, according to Tonietto and Carbonneau (2004), indicates that there were good climatic conditions to reach appropriate berry maturation. Table 2 indicates that the cumulative values of ETv and ET0 ranged between 315 and 349 mm and between 893 and 983 mm respectively. Moreover, the DI was between -115 and -151 mm, indicating that the area was very dry. Under these atmospheric conditions, the mean values of were maintained between -0.69 and -1.05 MPa from setting to véraison, indicating that the farmer maintained the Carménère commercial vineyard under a water status from moderate to weak water deficit (Fig. 1) (Van Leeuwen et al., 2009). It was only in the 2005/2006 growing season that the vineyard showed values of Ψs < -1.4 (severe water stress) during post-véraison and pre-harvest; during the other seasons, the vineyard was always maintained under > -1.1 MPa. It is important to indicate that there were no significant differences in mean ΨFs between seasons and phenological stages.
Gas exchange performance
For the field-grown grapevines, a significant non-linear regression was observed between AN and gs (r2 = 0.82), in spite of the large scattering observed in this study (Fig. 2). Also, the results show that the net CO2 assimilation was between 5.8 and 14.9 and 3.5 and 11.3 μmol CO2/m2/sec for Carménère vines under mild (gs values from 0.5 to 0.15 mol/ m2/sec) and moderate (gs values from 0.15 to 0.05 mol/m2/sec) water stress respectively. In Fig. 3A, a significant non-linear relationship between Ci and gs (r2 = 0.54) can be observed, with an important scattering of the gs value ranging from 0.05 to 0.15 mol/ m2/sec. The mean values of Ci were 233.4 (± 16.9) and 211.2 (± 25) μmol CO2/mol air for the mild and moderate water stress phases respectively. In Fig. 3B, a significant non-linear regression can be observed between the mesophyll conductance of the leaf (gm = AN/Ci) and gs (r2 = 0.49), with a very large scattering of gs ranging between 0.15 and 0.5 mol/m2/sec.
Figs 4A and 4B show the intrinsic (WUEi = AN/gs) and instantaneous (WUE = AN/E) water-use efficiencies of the cv. Carménère for the different values of stomatal conductance. The values of WUEi and WUE increased from mild to moderate water stress, but the pattern of WUEi was better than that of WUE. The mean values of WUEi and WUE for mild water stress (gs values from 0.5 to 0.15 mol/ m2/sec) ranged between 28.7 and -73.4 μmol/mol and 0.8 to 2.9 mmol/mol, respectively, while those for moderate water stress (gs values from 0.15 to 0.05 mol/m2/sec) ranged between 41.5 and 110.3 μmol/mol and 0.9 and 4.6 mmol/mol, respectively.
Vine water status and stomatal sensitivity factor
A significant linear relationship was observed between Ψs and gs (r2 = 0.39) for measurements taken before and after véraison, with an increasing scattering from -1.6 to -0.4 MPa (Fig. 5). In addition, a very large scattering of gs was observed for ranging between -0.4 and -0.9 MPa. For this range, the cv. Carménère maintained values of stomatal conductance > 0.1 mol/m2/sec. Also, Fig. 5 shows that stressed and non-stressed leaves were observed both before (black circles) and after (white circles) véraison. Finally, leaves under severe water stress (ΨFs < -1.4 MPa) were only observed in the véraison-pre-harvest period in the 2005/2006 season (Fig. 1).
The stomatal sensitivity (k) calculated for the water deficit ranges suggested by Van Leeuwen et al. (2009) is indicated in Fig. 6. This figure shows that k decreased as water stress increased, with values of 234 and 120 for no and severe water stress respectively. Moreover, Fig. 7 indicates that the values of k ranged between 264 and 480 and 255 and 297 for the measurements taken before and after véraison respectively. In this case, values of r2 for the linear regressions between gs and the 'Ball factor' ranged between 0.23 and 0.78.
Gas exchange behaviour under open field conditions
The response of plants to drought is generally categorised as being typical for desiccation or drought tolerance mechanisms instead of drought avoidance, since drought is a form of stress that all plants can tolerate but none can avoid. In this regard, we can distinguish between desiccation postponement (the ability to maintain tissue hydration) and desiccation tolerance (the ability to function while dehydrated), which sometimes are referred to as drought tolerance at high and low water potentials respectively. For grapevines, the range of observed responses exhibited by the different cultivars is very large (Chaves et al., 2010) and several classifications seem possible. Based on all the parameters measured in the present study, the cultivar Carménère could be classified as drought tolerant at low water potentials, with a large range of physiological parameters changing in response to water stress. The stomatal aperture reflects the differential turgor between guard cells and neighbouring cells. The epidermal turgor can be affected by humidity and drought, so that appropriate stomatal responses could occur passively (i.e. hydraulically) without any active (i.e. metabolic) involvement (Schultz, 2000). In the case of the cultivar Carménère, the results show that its stomatal closure cannot be purely hydraulic, since the stomata remained partially open even at *Fs between -1.6 and -1.4 MPa (severe water stress) (Fig. 5). This result suggests that, for complete stomatal closure to occur, an extra signal from the roots may be needed (i.e. ABA). In this regard, Sauter et al. (2001) suggested that the stomatal sensitivity to the root signal could vary in different cultivars.
In this study of field-grown grapevines, a good hyperbolic relationship was observed between AN and gs, with a large scattering of the data. The AN-gs relationship was observed for different cultivars under non-irrigated and irrigated conditions (both field- and pot-grown vines), which suggests that this association can be used as an integrative tool to evaluate the response of different photosynthetic processes to drought (Flexas et al., 2002; Medrano et al., 2002; Cifre et al., 2005). In this regard, it should be mentioned that the maximum value of AN observed in this study was close to 15 μmol/m2/sec, which is lower than that (19 μmol/m2/sec) reported by Medrano et al. (2002). The large scattering of gas exchange measurements reported in this study have also been observed in field-grown and potted grapevines under different growing conditions (Flexas & Medrano, 2002; Flexas et al., 2002; Medrano et al., 2002). The factors that can explain this scattering are related to the constantly changing light, temperature and vapour pressure conditions present across the canopy (Flexas & Medrano, 2002; Flexas et al., 2002; Medrano et al., 2002). The values of AN and gs observed in this study are within the ranges indicated in the literature for isohydric (Mourvèdre, Manto Negro, Tempranillo, Grenache and Ekigaïna) and anisohydric (Syrah and Marselan) cultivars growing under different levels of water stress. For instance, Romero et al. (2010) indicated that AN and gs ranged between 4 and 16 μmol/m2/sec and 0.03 and 0.3 mol/m2/sec, respectively for cv. Mourvèdre. Flexas and Medrano (2002) observed that AN was between 0 and 18 μmol/m2/sec and gs was between 0 and 0.5 mol/m2/sec for Manto Negro and Tempranillo, while Prieto et al. (2010) indicated that AN was between 0 and 21 μmol/m2/sec and that gs ranged between 0 and 0.4 mol/m2/sec for the cvs Syrah, Marselan, Grenache, Mourvèdre and Ekigaïna. Finally, Chaves et al. (2007) observed that AN and gs ranged between 4 and 15 μmol/m2/sec and 0.05 and 0.3 mol/m2/sec for the cvs Moscatel and Castelào, respectively.
With regard to water-use efficiencies, Cifre et al. (2005) and Flexas et al. (2010) indicated that a decreasing range of gs, from 0.5 to 0.05 mol/m2/sec produces a decline in AN, which results in the progressive increase of WUEi. This pattern was also found in the ungrafted Carménère grapevines growing under field conditions. According to Romero et al. (2010) and Prieto et al. (2010), WUEi ranged between 10 and 230 μmol/mol in isohydric and anisohydric cultivars. These values of WUEi are similar to those reported in this study for the cv. Carménère under midday stem water potentials, ranging from -0.3 to -1.7 MPa. From a plant physiological point of view, WUEi should be understood as a cultivar-specific way to express water-use efficiency, since it avoids the large fluctuations observed in the values of WUE (AN/E) that are caused by differences in evaporative demand without changes in stomatal conductance (Schultz, 2000).
Stomatal conductance response under changing plant water status
Similar distributions of ΨFs for the gs values ranging from 0.45 to about 0.05 mol/m2/sec were observed regardless of whether the data was collected before or after véraison (Fig. 5). The lowest values of Ψs and gs observed after véraison can be explained through the water restriction observed in the 2005/2006 season. These results are similar to the ones reported by Prieto et al. (2010) in their work with anisohydric grapevine cultivars (Syrah and Marselan). The stomatal sensitivity values reported in this study (Figs 6 and 7) are similar to those found by Schultz et al. (1999), who reported that the k values changed over the growing season, going from high (poorly sensitive) in the early season to lower values as véraison and harvest approached. In addition, these authors indicated that high values of k (inverse relationship with stomatal closure control) are associated with cultivars with low stomatal sensitivity to stressful environmental conditions. Furthermore, these authors also indicated that k ranged between 73 and 159 in anisohydric cultivars (Riesling, Chardonnay, Cabernet Sauvignon, Syrah, Touriga Nacional and Semillon) and had a value of 83 in an isohydric cultivar (Grenache). Prieto et al. (2010) observed k values of 150 and 120 in anisohydric (cv. Syrah) and isohydric (cv. Ekigaïna) grapevines respectively. The decrease in k may reflect the effect of shoot lignification late in the season, which alters the hydraulic capabilities of plant organs such as shoots and leaves. In the present study, véraison and shoot lignification usually started in the second half of January, a period that coincides with the shift in stomatal sensitivity (Schultz et al., 1999; Schultz, 2000). Fig. 7 indicates that the values of k were higher before than after véraison for the Carménère grapevines. In this regard, Speirs et al. (2013) indicated that the stomatal sensitivity increased (lower values) as the level of water stress increased, possibly due to an earlier or accelerated shoot lignification induced as a response of stress-hormone feedback. Similarly, Schultz (2000) observed that the stomatal sensitivity increased as the pre-dawn water potential decreased.
In Carménère, the transpiration could be sustained, despite presenting a large leaf area (GDC training system supports large canopies) through less sensitive stomata. In this case, the system needs a high water transport capacity in the soil-plant-atmosphere continuum and might be less sensitive to xylem embolisms. In this regard, Zufferey et al. (2011) described diurnal cycles of embolism formation and repair in petioles of stressed grapevines (cv. Chasselas). Nevertheless, the results showed that once véraison was reached, the stomatal sensitivity factor shifted to a more responsive state (Fig. 7), possibly because of the natural lignification of shoots, which resulted in a more conservative water behaviour after this period (Domec & Johnson, 2012; Rogiers et al., 2012; Zhang et al., 2012).
In this study, significant non-linear relationships were observed between AN and gs (r2 = 0.82) Ci and gs (r2 = 0.54) and AN/Ci and gs (r2 = 0.49) for ungrafted Carménère grapevines growing in a drip-irrigated commercial vineyard. The values of AN diminished from 14.9 to 3.5 μmol/m2/sec as g decreased from 0.5 to 0.05 mol/m2/sec, which resulted in a progressive increase in WUEi. In this cases, the mean values of WUEi for mild water stress (gs values from 0.5 to 0.15 mol/m2/sec) ranged between 28.7 and 73.4 μmol/mol, while those for moderate water stress (gs values from 0.15 to 0.05 mol/m2/sec) ranged between 41.5 and 110.3 μmol/mol. Also, a significant linear relationship was observed between Ys and gs (r2 = 0.39) for measurements taken before and after véraison, with an increasing scattering from -1.6 to -0.4 MPa. Finally, k decreased as water stress increased, with values of 234 and 120 for no and severe water stress respectively, while k ranged between 264 and 480 and 255 and 297 for the measurements taken before and after véraison respectively. Based on all the parameters measured in the present study, the cultivar Carménère could be classified as drought tolerant at low water potentials, with a large range of physiological parameters changing in response to water stress.
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Submitted for publication: July 2014
Accepted for publication: December 2014
* Corresponding author: E-mail address: firstname.lastname@example.org [Tel.: +56 71 2200426]
Acknowledgements: This study was supported by the Chilean government through the projects FONDECYT (N° 1030314) and FONDEF (N°D10I1157), by the Universidad de Talca through the research programme, "Adaptation of Agriculture to Climate Change (A2C2)", and through doctoral scholarship support for Francisco Jara-Rojas