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…

Upscaling the integrated terroir zoning through digital soil mapping: a case study in the Designation of Origin Campo de Borja

homogeneous zones by intersecting several partial zonings of major factors that influence vineyard growth. Each of them follows specific process from their corresponding disciplines. Soil zoning specifically refers to a Soil Resource Inventory map that has traditionally been generated by conventional soil mapping methods. These methods have shortcomings in reaching fine cartographic and categorical details and involve significant expenses, which undermines their applicability. A new framework named Digital Soil Mapping has introduced quantitative models by statistical techniques to establish soil-landscape relationships and is able to provide intensive scale cartography.

In the present study, a microzoning at 1:10.000 scale is generated from an initial zoning, where the conventional soil map with polytaxic map units is replaced by a new one from digital techniques that disaggregates them. The comparison between the zonings considers a quantitative evaluation of capability for each Homogeneous Terroir Unit by means of the Viticultural Quality Index and its categorization based on its distribution by map. The spatial intersection of both maps gives rise to a confusion matrix in which the flows of class variations after the substitution are assessed.

The results show a five-fold increase in the number of Homogeneous Terroir Units identified and a larger differentiation among them, evidenced by a wider range in the capability index distribution. Both elements are accompanied by an increase in the detection of areas of higher potential within previously undervalued uniform zones.These features are a direct effect of the improvements brought by Digital Soil Mapping techniques and would verify the advantages of their implementation in the Integrated Terroir zoning. Eventually, such new highly detailed terroir units would benefit precision viticulture and sustainable management practices.

The concept of terroir: what place for microbiota?

Microbes play key roles on crop nutrient availability via biogeochemical cycles, rhizosphere interactions with roots as well as on plant growth and health. Recent advances in technologies, such as High Throughput Sequencing Techniques, allowed to gain deeper insight on the structure of bacterial and fungal communities associated with soil, rhizosphere and plant phyllosphere. Over the past 10 years, numerous scientific studies have been carried out on the microbial component of the vineyard. Whether the soil or grape compartments have been taken into account, many studies agree on the evidence of regional delineations of microbial communities, that may contribute to regional wine characteristics and typicity. Some authors proposed the term “microbial terroir” including “yeast terroir” for grapes to describe the connection between microbial biogeography and regional wine characteristics. Many factors are involved in terroir including climate, soil, cultivar and human practices as well as their interactions. Studies considering “microbial terroir” greatly contributed to improve our knowledge on factors that shape the vineyard microbial structure and diversity. However, the potential impact of “microbial terroir” on wine composition has yet not received strong scientific evidence and many questions remain to be addressed, related to the functional characterization of the microbial community and its impact on plant physiology and grape composition, the origins and interannual stability of vineyard microbiota, as well as their impact on wine sensorial attributes. The presentation will give an overview on the role of microbiota as a terroir component and will highlight future perspectives and challenges on this key subject for the wine industry.

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"...

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.

The rootstock, the neglected player in the scion transpiration even during the night

Water is the main limiting factor for yield in viticulture. Improving drought adaptation in viticulture will be an increasingly important issue under climate change. Genetic variability of water deficit responses in grapevine partly results from the rootstocks, making them an attractive and relevant mean to achieve adaptation without changing the scion genotype. The objective of this work was to characterize the rootstock effect on the diurnal regulation of scion transpiration. A large panel of 55 commercial genotypes were grafted onto Cabernet Sauvignon. Three biological repetitions per genotype were analyzed. Potted plants were phenotyped on a greenhouse balance platform capable of assessing real-time water use and maintaining a targeted water deficit intensity. After a 10 days well-watered baseline period, an increasing water deficit was applied for 10 days, followed by a stable water deficit stress for 7 days. Pruning weight, root and aerial dry weight and transpiration were recorded and the experiment was repeated during two years. Transpiration efficiency (ratio between aerial biomass and transpiration) was calculated and δ13C was measured in leaves for the baseline and stable water deficit periods. A large genetic variability was observed within the panel. The rootstock had a significant impact on nocturnal transpiration which was also strongly and positively correlated with maximum daytime transpiration. The correlations with growth and water use efficiency related traits will be discussed. Transpiration data were also related with VPD and soil water content demonstrating the influence of environmental conditions on transpiration. These results highlighted the role of the rootstock in modulating water deficit responses and give insights for rootstock breeding programs aimed at identifying drought tolerant rootstocks. It was also helpful to better define the mechanisms on which the drought tolerance in grapevine rootstocks is based on.