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…

Effect of partial net shading on the temperature and radiation in the grapevine canopy, consequences on the grape quality of cv. Gros Manseng in PDO Pacherenc-du-vic-Bilh

As elsewhere, southwestern France vineyards face more recurrent summer heat waves these last years. Among the possibilities of adaptation to this climate changing parameter, the use of net shading is a technique that allow for limiting canopy exposure to radiations. In this trial, we tested net shading installed on one face of the canopy, on a north-south row-oriented plot of cv. Gros Manseng trained on VSP system in the PDO Pacherenc-du-Vic-Bilh. The purpose was to characterize the effects on the ambient canopy temperatures and radiations during the season and to observe the consequences on the composition of grapes and wines. Two sorts of net were used with two levels of obstruction (50% and 75%) of the photosynthesis active radiation (PAR). They have been installed on the west side of the canopy and compared to a netless control. Temperature and PAR sensors registered hourly data during the season. On specific summer day (hot and sunny) manual measurements took also place on bunches (temperature) and in different spots of the canopy (PAR). The results showed that, on clear days, the radiation is lowered by the shade nets respecting the supplier criteria. The effects on the ambient canopy temperature were inconstant on this plot when we observed the data from the global period of shading between fruit set and harvest. However, during hot days (>30°C), the temperature in the canopy was reduced during afternoon and the temperature of the bunch surface was reduced as well comparing to the control. A decrease of the maturity parameters of the berries, sugar and acidity, was also observed. Concerning the wine aromatic potential, no differences clearly appeared.

Spatiotemporal patterns of chemical attributes in Vitis vinifera L. cv. Cabernet Sauvignon vineyards in Central California

Spatial variability of vine productivity in winegrapes is important to characterise as both yield and quality are relevant for the production of different wine styles and products. The objectives were to understand how patterns of variability of Cabernet Sauvignon fruit composition changed over time and space, how these patterns could be characterised with indirect measurements, and how spatial patterns of the variation in fruit compositional attributes can aid in improving management. Prior to the 2017 vintage, 125 data vines were distributed across each of four vineyards in the Lodi American Viticultural Area (AVA) of California. Each data vine was sampled at commercial harvest in 2017, 2018, and 2019. Yield components and fruit composition were measured at harvest for each data vine, and maps of yield and fruit composition were produced for eight ‘objective measures of fruit quality’: total anthocyanins, polymeric tannins, quercetin glycosides, malic acid, yeast assimilable nitrogen, β-damascenone, C6 alcohols and aldehydes, and 3-isobutyl-2-methoxypyrazine. Patterns of variation in anthocyanins and phenolic compounds were found to be most stable over time. Given this relative stability, management decisions focused on fruit quality could be based on zonal descriptions of anthocyanins or phenolics to increase profitability in some vineyards. In each vineyard, dormant season pruning weights and soil cores were collected at each location, elevation and soil apparent electrical conductivity surveys were completed, and remotely sensed imagery was captured by fixed wing aircraft and two satellite platforms at major phenological stages. The data collected were used to develop relationships among biophysical data, soil, imagery, and fruit composition. The standardised and aggregated samples from four vineyards over three seasons were included in the estimation of ‘common variograms’ to assess how this technique could aid growers in producing geostatistically rigorous maps of fruit composition variability without cumbersome, single season sampling efforts.

Local adaptation tools to ensure the viticultural sustainability in a changing climate

[lwp_divi_breadcrumbs home_text="IVES" use_before_icon="on" before_icon="||divi||400" module_id="publication-ariane" _builder_version="4.19.4" _module_preset="default" module_text_align="center" module_font_size="16px" text_orientation="center"...

Sustaining wine identity through intra-varietal diversification

With contemporary climate change, cultivated Vitis vinifera L. is at risk as climate is a critical component in defining ecologically fitted plant materiel. While winegrowers can draw on the rich diversity among grapevine varieties to limit expected impacts (Morales-Castilla et al., 2020), replacing a signature variety that has created a sense of local distinctiveness may lead to several challenges. In order to sustain wine identity in uncertain climate outcomes, the study of intra-varietal diversity is important to reflect the adaptive and evolutionary potential of current cultivated varieties. The aim of this ongoing study is to understand to what extent can intra-varietal diversity be a climate change adaptation solution. With a focus on early (Sauvignon blanc, Riesling, Grolleau, Pinot noir) to moderate late (Chenin, Petit Verdot, Cabernet franc) ripening varieties, data was collected for flowering and veraison for the various studied accessions (from conservatory plots) and clones. For these phenological growing stages, heat requirements were established using nearby weather stations (adapted from the GFV model, Parker et al., 2013) and model performances were verified. Climate change projections were then integrated to predict the future behaviour of the intra-varietal diversity. Study findings highlight the strong phenotypic diversity of studied varieties and the importance of diversification to enhance climate change resilience. While model performances may require improvements, this study is the first step towards quantifying heat requirements of different clones and how they can provide adaptation solutions for winegrowers to sustain local wine identity in a global changing climate. As genetic diversity is an ongoing process through point mutations and epigenetic adaptations, perspective work is to explore clonal data from a wide variety of geographic locations.

Terroir traceability in grapes, musts and wine: results of research on Gewürztraminer and Sauvignon Blanc grape varieties in northern Italy

In the study of terroir, a separate analysis of its many component factors can be of great help in accurately identifying a vineyard’s natural elements that impact wine quality and typicity. This research used a dedicated pluri-disciplinary approach to investigate the ecological characteristics, including geology and geographical features, of 14 vineyards that produce Gewürztraminer and Sauvignon Blanc cultivars in the alpine Alto Adige DOC wine region. Both the geopedological method using Vineyards Geological Identity (VGI) and the new Solar Radiaton Identity (SRI) topoclimatic classification method were used to provide analytical measurements and qualitative/quantitative characterisations. In addition, wide-ranging targeted and untargeted oenological and chemical analyses were carried out on grapes, musts and wines to correlate the soils’ geomineral and physical conditions with the biochemical properties of their fruits and wines. The research identified strong correlations between vineyard geo-identity and wine biofingerprint, confirming a mineral traceability of strontium rubidium ratio and some minerals distinctive to the local geology, such as K, Ca, Ag, Ba and Mn.  The study also discovered that particular geomineral and physical soil conditions of the studied vineyards are related to the different amount of amino acids, primary varietal aromas and polyphenols found in grapes, musts and wines. The research confirmed that winemaking technologies support oenological quality, although in some cases, human practices can overpower certain characteristic elements in wine, erasing the typical imprint left by the vineyards’ natural terroir, which becomes less traceable. Terroir abiotic ecological factors and vineyard identity can be classified in detail using the new VGI and SRI analysis methods to discover interrelationships between geo-pedological and topoclimatic conditions that impact wine quality. These methods are also helpful in identifying which ecological elements are exclusive to a particular vineyard or wine sub-region.