Terroir 1996 banner
IVES 9 IVES Conference Series 9 First results obtained with a terrain model to characterize the viticultural «terroirs» in Anjou (France)

First results obtained with a terrain model to characterize the viticultural «terroirs» in Anjou (France)

Abstract

En Anjou, une méthode de caractérisation des terroirs viticoles a été développée. Elle utilise un modèle de terrain basé sur la profondeur de sol et son degré d’argilisation. Il génère trois types de milieu sol : roche, altération, altérite. Les hypothèses testées concernent l’effet des trois types de milieu sur l’àlimentation en eau, la précocité de cycle de la vigne, le potentiel de vigueur et de rendement ainsi que sur la composition des baies.
Pour cela, un réseau de parcelles expérimentales de Chenin et Cabernet franc, comportant 3 répétitions par unité de terroir, a été mis en place. Il permet d’étudier les deux principaux systèmes géologiques de l’Anjou (Briovérien et Ordovicien-Dévonien)
Les résultats de 2000 et 2001 (années pluvieuses) montrent pour le cépage Chenin que le débourrement est significativement plus précoce en milieu roche qu’en milieu altérite. Le milieu altération ne se différencie pas significativement des deux autres. En 2000, des différences significatives d’alimentation hydrique entre terroirs sont apparues à partir du mois de septembre pour le cépage Chenin, et à un degré moindre pour le Cabernet franc. Ainsi, le milieu roche entraîne un abaissement significatif du potentiel hydrique foliaire de base, malgré l’année pluvieuse. Le milieu altération ne se différencie pas du milieu roche. Sur spilite de l’Ordovicien-Dévonien, le milieu roche induit une contrainte hydrique plus forte que sur métagrauwacke du Briovérien. Les résultats d’analyses de δ13C des baies sont très significatifs et confrrment ceux du potentiel hydrique foliaire. Ces deux types de mesures montrent que la contrainte hydrique pour la vigne est significativement plus forte en milieu roche qu’en milieu altérite. Les baies du cépage Chenin, en milieux roche et altération, sont significativement plus riches en sucres qu’en milieu altérite. Les milieux roche sur schiste gréseux et métagrauwacke ont des teneurs inférieures à celles de la spilite. Avec le Cabernet franc, les baies semblent plus riches en sucres sur milieu roche que sur altérite. Le milieu roche induit des teneurs en anthocyanes et polyphénols significativement supérieures à celles de l’altérite; et cela aussi bien dans les baies que dans les vins. Ces premiers résultats, encore fragmentaires, semblent confirmer la plupart des hypothèses de travail avancées.

In Anjou vineyard, the viticultural “terroirs” are studied with a method based” on the concept of the “Basic Terroir Unit” (BTU). To identify and cartography the BTU, a terrain model based on the depth and the clay content of soil was elaborated. It generates three kinds of soil environments which are designated by the French terms of: “roche, alteration and altérite”. The hypothesis tested concern the effect of each type of environment on water supply regime, earliness and vigour of vine which are the main factors of the “terroir” effect, and also on berries composition.
A multisite network of 21 plots with Chenin and Cabernet franc varieties, was established in 2000. It samples the two main geologic systems of Anjou (Brioverian and Ordovician­ Devonian), with three replicates for each BTU.
The first results (2000 & 2001), show for the variety Chenin that bud break is earlier in the “roche” environment than in the “altérite” environment. The “alteration” is not different from were detected in September; for the Chenin variety and, at a less degree, for the Cabernet franc. So the “roche” environment involves a significant lowering of the predawn leaf water potential, despite a rainy season. There are no significant differences between the “alteration” and the “roche” environment. The “roche” environment on spilite from Ordovician-Devonian involves significantly more water constraint than on metagrauwacke from Brioverian. The results of δ13 C measurements in berries are highly significant and confirm the ones of the predawn leaf water potential. These two kinds of measures show that the water availability is greater in the “altérite” environment than in the “roche” environment. The must sugar content on “roche” and “alteration” environments was significantly higher than on “altérite”. The rock environment on sandstone schist and metagrauwacke have a lesser sugar content than on spilite. With the Cabernet franc variety, the “roche” environment involves significantly greater anthocyanins and polyphenolic amounts than the “altérite”; both in berries and in wines. These first results seem to confirm most of the hypotheses.

DOI:

Publication date: February 15, 2022

Issue: Terroir 2002

Type: Article

Authors

Fabrice BODIN and René MORLAT

Unité Vigne et Vin. Centre INRA d’Angers. 42 rue Georges Morel. BP57.
49071 Beaucpuzé Cedex. France

Contact the author

Keywords

modèle de terrain, précocité de cycle, alimentation hydrique, cépage, composition des baies
terrain model, precocity, water supply regime, grape variety, berry composition

Tags

IVES Conference Series | Terroir 2002

Citation

Related articles…

Rootstock regulation of scion phenotypes: the relationship between rootstock parentage and petiole mineral concentration

Grapevine is grown as a graft since the end of the 19th century. Rootstocks not only provide tolerance to Phylloxera but also ensure the supply of water and mineral nutrients to the scion. Rootstocks are an important mean of adaptation to environmental conditions, because the scion controls the typical features of the grapes and wine. However, among the large diversity of rootstocks worldwide, few of them are commercially used in the vineyard. The aim of this study was to investigate the extent to which rootstocks modify the mineral composition of the petioles of the scion. Vitis vinifera cvs. Cabernet-Sauvignon, Pinot noir, Syrah and Ugni blanc were grafted onto 55 different rootstock genotypes and planted in a vineyard as three replicates of 5 vines. Petioles were collected in the cluster zone with 6 replicates per combination. Petiolar concentrations of 13 mineral elements (N, P, K, S, Mg, Ca, Na, B, Zn, Mn, Fe, Cu, Al) at veraison were determined. Scion, rootstock and the interaction explained the same proportion of the phenotypic variance for most mineral elements. Rootstock genotype showed a significant influence on the petiole mineral element composition. Rootstock effect explained from 7 % for Cu to 25 % for S of the variance. The difference of rootstock conferred mineral status is discussed in relation to vigor and fertility. Rootstocks were also genotyped with 23 microsatellite markers. Data were analysed according to genetic groups in order to determine whether the petiole mineral composition could be related to the genetic parentage of the rootstock. Thanks to a highly powerful design, it is the first time that such a large panel of rootstocks grafted with 4 scions has been studied. These results give the opportunity to better characterize the rootstocks and to enlarge the diversity used in the vineyard.

From a local to an international scale: sensory benchmarking of PDO wines. Quincy and Reuilly PDO wines (Sauvignon blanc) as a case study (France)

In a collective marketing strategy, the Protected Designation of Origin (PDO) can be used as a quality indicator. To highlight terroir specificities, it is useful to know how the wines are positioned on the local, national or international market from a sensory point of view. This is especially true for a comparison of varietal wines (e.g. Sauvignon blanc). We focus on the case of two closed Loire Valley PDO (France): Quincy and Reuilly. Three distinct tastings were organized. Firstly, at the local level comparing the 2 PDO (11 and 9 wines, 17 professional assessors); secondly at a regional level adding 3 closed PDO: Menetou-Salon, Sancerre and Pouilly-Fumé (3 wines per PDO, 16 assessors) and thirdly at an international level comparing these 5 PDO with Sauvignon Blanc wines coming from South Africa, New Zealand and Chile (1 to 3 wines per PDO, 19 assessors). All the wines were from the 2019 vintage and were considered to have a traditional elaboration process without contact with oak. A sensory descriptive analysis was performed using an aroma wheel allowing to combine a Check-All-That-Apply methodology, often used in sensory benchmarking, with a hierarchical structuration of the attributes. The aim is to facilitate data acquisition in a professional context without common training, to consider the hierarchical relationships among the attributes during the data analysis and to be able to characterize wines with a large range of sensorial variability. We use univariate, multivariate and clustering analyses. Similarities and differences between Quincy and Reuilly PDO wines and other Sauvignon blanc wines were identified. Specific attributes can distinguish the two PDO and different proximities exist with other local PDO, while clear differences were observed compared to international wines. Our study contributes to propose and discuss a method to do a wine sensory benchmarking highlighting sensory specificities linked to origin.

Downscaling of remote sensing time series: thermal zone classification approach in Gironde region

In viticulture, the challenges of local climate modelling are multiple: taking into account the local environment, fine temporal and spatial scales, reliable time series of climate data, ease of implementation and reproducibility of the method. At the local scale, recent studies have demonstrated the contribution of spatialization methods for ground-based climate observation data considering topographic factors such as altitude, slope, aspect, and geographic coordinates (Le Roux et al, 2017; De Rességuier et al, 2020). However, these studies have shown questions in terms of the reproducibility and sustainability of this type of climate study. In this context, we evaluated the potential of MODIS thermal satellite images validated with ground-based climate data (Morin et al, 2020). Previous studies have been encouraging, but questions remain to be explored at the regional scale, particularly in the dynamics of the massive use of bioclimatic indices to classify the climate of wine regions. The results at the local scale were encouraging, but this approach was tested in the current study at the regional scale. Several objectives were set: 1) to evaluate the downscaling method for land surface temperature time series, 2) to identify regional thermal structure variations. We used weekly minimum and maximum surface temperature time series acquired by MODIS satellites at a spatial resolution of 1000 m and downscaled at 500 m using topographical variables. Two types of analyses were performed:

Effects of graft quality on growth and grapevine-water relations

Climate change is challenging viticulture worldwide compromising its sustainability due to warmer temperatures and the increased frequency of extreme events. Grafting Vitis vinifera L.

Permanent cover cropping with reduced tillage increased resiliency of wine grape vineyards to climate change

Majority of California’s vineyards rely on supplemental irrigation to overcome abiotic stressors. In the context of climate change, increases in growing season temperatures and crop evapotranspiration pose a risk to adaptation of viticulture to climate change. Vineyard cover crops may mitigate soil erosion and preserve water resources; but there is a lack of information on how they contribute to vineyard resiliency under tillage systems. The aim of this study was to identify the optimum combination of cover crop sand tillage without adversely affecting productivity while preserving plant water status. Two experiments in two contrasting climatic regions were conducted with two cover crops, including a permanent short stature grass (P. bulbosa hybrid), barley (Hordeum spp), and resident vegetation under till vs. no-till systems in a Ruby Cabernet (V. vinifera spp.) (Fresno) and a Cabernet Sauvingon (Napa) vineyard. Results indicated that permanent grass under no-till preserved plant available water until E-L stage 17. Consequently, net carbon assimilation of the permanent grass under no-till system was enhanced compared to those with barley and resident vegetation. On the other hand, the barley under no-till system reduced grapevine net carbon assimilation during berry ripening that led to lower content of nonstructural carbohydrates in shoots at dormancy. Components of yield and berry composition including flavonoid profile at either site were not adversely affected by factors studied. Switching to a permanent cover crop under a no-till system also provided a 9% and 3% benefit in cultural practices costs in Fresno and Napa, respectively. The results of this work provides fundamental information to growers in preserving resiliency of vineyard systems in hot and warm climate regions under context of climate change.