Terroir 1996 banner
IVES 9 IVES Conference Series 9 Influence de l’ensoleillement sur la composante aromatique des baies de raisin

Influence de l’ensoleillement sur la composante aromatique des baies de raisin

Abstract

La Syrah est un raisin à expression aromatique faible. Ce cépage atypique en tant que fruit permet l’élaboration de vins de grande réputation pour lesquels la particularité aromatique joue un rôle important. L’arôme variétal est constitué de substances volatiles directement perceptibles par la muqueuse olfactive et de précurseurs d’arôme, dont les glycosides constituent une classe importante. Ces derniers, des molécules inodores, sont en effet susceptibles, lors de la vinification, de donner naissance à des composés volatils et odorants participant à l’arôme du vin. Dans les baies de raisin de nombreux cépages et en l’occurrence dans la Syrah, les teneurs en glycosides sont nettement supérieures à celles des constituants volatils libres (Gunata et al., 1985 et Parle et al., 1991), ce qui montre l’importance des glycosides en terme de potentiel aromatique. Les glycosides peuvent être classés, en fonction de leur aglycone, par familles distinguant ainsi les composés en C6, les alcools, les phénols, les terpénols, les C13-norisoprénoïdes…Ces derniers, d’un grand intérêt olfactif, ont été identifiés dans le raisin et le vin (Strauss et al., 1987; Abbott, 1989). Dans les vins de Syrah, souvent caractérisés par une note de violette, les C13-norisoprénoïdes doivent contribuer fortement à l’arôme. En effet, parmi les composés les plus connus de la famille des Ci3-norisoprénoïdes, la β-ionone présente cette odeur de violette. L’importance des C13-norisoprénoïdes du point de vue de leur diversité olfactive et de leur teneur dans la fraction glycosylée de Syrah, nous a conduit à nous intéresser à leurs précurseurs, les caroténoïdes (Enzeil, 1985 ; Williams et al, 1992 ; Winterhalter, 1993). La teneur en caroténoïdes, relativement importante dans les baies vertes, diminue au cours de la maturation des baies (Razungles et al., 1988), ce qui laisse supposer que les C13-norisoprénoïdes trouvés dans les vins sont issus de ce catabolisme (Marais et al., 1991 ; Razungles et al., 1993). Les C13-norisoprénoïdes ont en effet le comportement inverse puisqu’ils augmentent avec la maturation des baies. L’importance du climat et du millésime sur la teneur en caroténoïdes et en arômes dans les baies a été montrée (Razungles et al., 1987 ; Marais et al., 1991 ; 1992). Nous nous sommes plus particulièrement intéressés dans ce travail à l’influence de l’éclairement des baies.

DOI:

Publication date: March 25, 2022

Issue: Terroir 1996

Type : Poster

Authors

S. BUREAU (1), A. RAZUNGLES (1), R. BAUMES (2), C. BAYONOVE (2)

(1) Institut Supérieur de la Vigne et du Vin, ENSAM- UFR de Technologie Oenologie
(2) Institut Supérieur de la Vigne et du Vin, INRA- Unité de Recherches sur les Arômes et Substances Naturelles – 2, Place Viala 34060 Montpellier cedex 1 France

Tags

IVES Conference Series | Terroir 1996

Citation

Related articles…

Genotypic variability in root architectural traits and putative implications for water uptake in grafted grapevine

Root system architecture (RSA) is important for soil exploration and edaphic resources acquisition by the plant, and thus contributes largely to its productivity and adaptation to environmental stresses, particularly soil water deficit. In grafted grapevine, while the degree of drought tolerance induced by the rootstock has been well documented in the vineyard, information about the underlying physiological processes, particularly at the root level, is scarce, due to the inherent difficulties in observing large root systems in situ. The objectives of this study were to determine genetic differences in the root architectural traits and their relationships to water uptake in two Vitis rootstocks genotypes (RGM, 140Ru) differing in their adaptation to drought. Young rootstocks grafted upon the Riesling variety were transplanted into cylindrical tubes and in 2D rhizotrons under two conditions, well watered and moderate water stress. Root traits were analyzed by digital imaging and the amount of transpired water was measured gravimetrically twice a week. Root phenotyping after 30 days reveal substantial variation in RSA traits between genotypes despite similar total root mass; the drought-tolerant 140Ru showed higher root length density in the deep layer, while the drought-sensitive RGM was characterised by shallow-angled root system development with more basal roots and a larger proportion of fine roots in the upper half of the tube. Water deficit affected canopy size and shoot mass to a greater extent than root development and architectural-related traits for both 140Ru and RGM, suggesting vertical distribution of roots was controlled by genotype rather than plasticity to soil water regime. The deeper root system of 140Ru as compared to RGM correlated with greater daily water uptake and sustained stomata opening under water-limited conditions but had little effect on above-ground growth. Our results highlight that grapevine rootstocks have constitutively distinct RSA phenotypes and that, in the context of climate change, those that develop an extensive root network at depth may provide a desirable advantage to the plant in coping with reduced water resources.

Delaying irrigation initiation linearly reduces yield with little impact on maturity in Pinot noir

When to initiate irrigation is a critical annual management decision that has cascading effects on grapevine productivity and wine quality in the context of climate change. A multi-site trial was begun in 2021 to optimize irrigation initiation timing using midday stem water potential (ψstem) thresholds characterized as departures from non-stressed baseline ψstemvalues (Δψstem). Plant material, vine and row spacing, and trellising systems were concomitant among sites, while vine age, soil type, and pruning systems varied. Five target Δψstem thresholds were arranged in an RCBD and replicated eight times at each site: 0.2, 0.4, 0.6, 0.8, and 1.0 MPa (T1, T2, T3, T4, and T5, respectively). When thresholds were reached, plots were irrigated weekly at 70% ETc. Yield components and berry composition were quantified at harvest. To better generalize inferences across sites, data were analyzed by ANOVA using a mixed model including site as a random factor. Across sites, irrigation was initiated at Δψstem = 0.24, 0.50, 0.65, 0.93, and 0.98 MPa for T1, T2, T3, T4, and T5, respectively. Consistent significant negative linear trends were found for several key yield and berry composition variables. Yield decreased by 12.9, 15.9, 19.5, and 27.4% for T2, T3, T4, and T5, respectively, compared to T1 (p < 0.0001) across sites that were driven by similarly linear reductions in berry weight (p < 0.0001). Comparatively, berry composition varied little among treatments. Juice total soluble solids decreased linearly from T1 to T5 – though only ranged 0.9 Brix (p = 0.012). Because producers are paid by the ton, and contracts simply stipulate a target maturity level, first-year results suggest that there is no economic incentive to induce moderate water deficits before irrigation initiation, regardless of vineyard site. Subsequent years will further elucidate the carryover effects of delaying irrigation initiation on productivity over the long term.

Climate modeling at local scale in the Waipara winegrowing region in the climate change context

In viticulture, a warming climate can have a very significant impact on grapevine development and therefore on the quality and characteristics of wines across different spatial scales, ranging from global to local. In order to adapt wine-growing to climate change, global climate models can be used to define future scenarios, but only at the scale of major wine regions. Despite the huge progress made over the last ten years in terms of the spatial resolution of climate models (now downscaled to a few square kilometres), they are not yet sufficiently precise to account for the local climate variability associated with such parameters as local topography, in spite of these parameters being decisive for vine and wine characteristics. This study describes a method to downscale future climate scenarios to vineyard scale. Networks of data loggers have been used to collect air temperature at canopy level in the Waipara winegrowing region (New Zealand) over five growing seasons. These measurements allow the creation of fine-scale geostatistical models and maps of temperature (at 100 m resolution) for the growing season. In order to model climate change at pilot site scale, these geostatistical models have been combined with regional climate change predictions for the periods 2031-2050 and 2081-2100 based on the RCP8.5 climate change scenario. The integration of local climate variability with regionalized climate change simulations allows assessment of the impacts of climate change at the vineyard scale. The improved knowledge gained using this methodology results from the increased horizontal resolution that better addresses the concerns of winegrowers. The results provide the local winegrowers with information necessary to understand current processes, as well as historical and future viticulture trends at the scale of their site, thereby facilitating decisions about future response strategies.

Under-vine management effects on grapevine production, soil properties and plant communities in South Australia

Under-vine (UV) management has traditionally consisted of synthetic herbicide use to limit competition between weeds and grapevines. With growing global interest towards non-synthetic chemical use, this study aimed to capture the effects of alternative UV management at two commercial Shiraz vineyards in South Australia, where the sole management variables were UV management since 2016. In adjacent treatment blocks, cultivation (CU) was compared to spontaneous vegetation (SV) in McLaren Vale (MV), and herbicide was compared to SV in Eden Valley (EV). Soil water infiltration rates were slower and grapevine stem water potential was lower in CU compared to SV in MV, with the latter having a plant community dominated by soursob (Oxalis pes-caprae) during winter; while in EV, there was little separation between the treatments. Yields were affected at both sites, with SV being higher in MV and HE being higher in EV. In MV, the only effect on grape must was a lower 13C:12C isotope ratio in CU, indicating greater grapevine water stress. In the grape must at EV, SV had higher total soluble solids, total phenolics, anthocyanins, and yeast available nitrogen; and lower pH and titratable acidity. Pruning weights were not affected by the treatments in MV, while they were higher in HE at EV. Assessments revealed that the differing soil types at the two sites were likely the main determinants of the opposing production outcomes associated with UV management. In the silty loam soil of MV, the higher yields in SV were likely due to more plant-available water, as a potential result of the continuous soil bio-pores formed by winter UV vegetation. Conversely, in the loamy sand soils of EV with a lower cation exchange capacity, the lower yields and pruning weights in SV suggest the UV vegetation competed significantly with the grapevines for available water and nutrients.

Analysis of Cabernet Sauvignon and Aglianico winegrape (V. vinifera L.) responses to different pedo-climatic environments in southern Italy

Water deficit is one of the most important effects of climate change able to affect agricultural sectors. In general, it determines a reduction in biomass production, and for some plants, as in the case of grapevine, it can endorse fruit quality. The monitoring and management of plant water stress in the vineyard