Terroir 1996 banner
IVES 9 IVES Conference Series 9 The origin and the discovery of “terroir”

The origin and the discovery of “terroir”

Abstract

Le mot “terroir” dérive du latin “terra”, mais déjà les Romains l’indiquaient comme “locus” ou”loci”, c’est-à-dire un lieu ayant le “genius”destiné à la production d’un produit d’excellente qualité. Les Égyptiens, les Juifs, les Grecs et les Romains employèrent les premiers le nom du lieu d’origine pour indiquer le vin sur le “pittacium” en argile qui était apposé sur les amphores en terre cuite qui contenaient le vin. De cette façon naquit la dénomination d’origine. Les peuples anciens de la Méditerranée n’ont pas utilisé le nom des variétés de vigne pour distinguer les différentes typologies de vin, mais leur lieu d’origine.
Les Grecs anciens, déjà à l’époque de Homère, choisissaient pour les vignes les terroirs qui permettaient la vie aux plantes du maquis méditerranéen, puisqu’ils étaient surs que le climat de ces lieux permettraient aux baies de mûrir parfaitement et de fournir des vins très corsés, fort structurés, riches en sucre et en alcool, mais pauvres en acides et en arômes facilement oxydables. Ce furent les anciens Romains qui en partant de la ”Provincia” de la Gaule transalpine remontèrent le Rhône, le Rhin, la Moselle, le Danube, et d’autres fleuves, en rependant la vigne dans le nord de l’Europe et en créant ce que l’on peut appeler la “viticulture fluviale”, qui s’oppose à la viticulture méditerranéenne pour la production de vins plus légers de corps, moins alcooliques, plus aromatiques, plus acides etc … Les Romains démontrèrent que la vigne peut mûrir même dans des climats plus septentrionaux, où les Grecs n’osèrent pas s’engager, en atteignant la limite septentrionale de culture du vignoble dans l’hémisphère Nord, c’est à dire jusqu’à 50° de latitude Nord.
Le premier exemple de délimitation géographique et territoriale nous vient de Pline (N.H., livre 14, chapitre V) qui avait étudié de façon approfondie le plus ancien cru Romain, c’est-à­-dire le Falernum.
Dans le premier siècle après J.-C., Pline décrit ainsi la zone de production du Falernum : “toute cette zone de la Campania qui s’étend en rive gauche du pont Campanus à la colonie urbaine de Silla est pleine de collines à vignobles très renommés à cause du très généreux vin qui prend le nom du village Falerne.”
C’est encore Plinius qui précise “à la gauche du pont commence la campagne de Falerne”.
Le pont cité existe encore sur le fleuve Liri et il lie l’ancienne Sineussa à la mer.
Son nom comme le dit Pline dérive du pays Falernum.
Le “genius loci” a été encore confirmé pendant le moyen-âge et pendant les époques historiques suivantes, jusqu’au moment où des règlements et des lois ont établi les premières délimitations de ces lieux. Plus tard, après la découverte de l’Amérique, la viticulture du nouveau Monde se développa, comprenant les Etats Unis, le Canada, l’Australie, la Nouvelle Zélande, l’Afrique du Sud et toute l’Amérique Latine, des pays qui, récemment, ont découvert l’importance du terroir.
Dans l’hémisphère sud, la vigne trouve sa limite de culture à 45° environ de latitude sud.
En 1700 fut délimitée par un document officiel (décret) la zone de production du Tokay Hongrois, suivie par celle du Chianti (1716) et celle du Porto (1755).
L’essence du terroir fut toutefois amplifiée en 1855 à Bordeaux avec la publication de la liste des “crus”. En effet, le “cru” est produit par un terroir ayant le “genius loci ” pour un vin d’excellente qualité. On fait remonter l’origine du terme “cru” à deux mots différents. Normalement on le définit comme participe passé du verbe “croître”, c’est-à-dire crû sur un terroir spécifique, mais, selon l’interprétation de certains latinistes d’anciennes abbayes françaises, cela signifie également “cru”, c’est-à-dire considéré comme “célèbre”, ayant une renommée auprès des consommateurs. C’est justement à travers les “crus” que les Français ont inventé le terme terroir, désormais utilisé dans tout le monde de la viticulture.

DOI:

Publication date: February 16, 2022

Issue: Terroir 2002 

Type: Article

Authors

M.FREGONI

Université Catholique – Piacenza (Italie)
Via E. Parmense, 84
29100 PIACENZA – Italie

Keywords

Histoire, Terroir, Appellation d’origine contrôlé

Tags

IVES Conference Series | Terroir 2002

Citation

Related articles…

Impact of climate variability and change on grape yield in Italy

Viticulture is entangled with weather and climate. Therefore, areas currently suitable for grape production can be challenged by climate change. Winegrowers in Italy already experiences the effect of climate change, especially in the form of warmer growing season, more frequent drought periods, and increased frequency of weather extremes.
The aim of this study is to investigate the impact of climate variability and change on grape yield in Italy to provide winegrowers the information needed to make their business more sustainable and resilient to climate change. We computed a specific range of bioclimatic indices, selected by the International Organisation of Vine and Wine (OIV), and correlated them to grape yield data. We have worked in collaboration with some wine consortiums in northern and central Italy, which provided grape yield data for our analysis.
Using climate variables from the E-OBS dataset we investigate how the bioclimatic indices changed in the past, and the impact of this change on grape productivity in the study areas. The climate impact on productivity is also investigated by using high-resolution convection-permitting models (CPMs – 2.2 horizontal resolution), with the purpose of estimating productivity in future emission scenarios. The CPMs are likely the best available option for this kind of impact studies since they allow a better representation of small-scale processes and features, explicitly resolve deep convection, and show an improved representation of extremes. In our study, we also compare CPMs with regional climate models (RCMs – 12 km horizontal resolution) to assess the added value of high-resolution models for impact studies. Further development of our study will lead to assessing the future suitability for vine cultivation and could lead to the construction of a statistical model for future projection of grape yield.

Climate change projections to support the transition to climate-smart viticulture

The Earth’s system is undergoing major changes through a wide range of spatial and temporal scales as a response to growing anthropogenic radiative forcing, which is pushing the whole system far beyond its natural variability. Sources of greenhouse gases largely exceed their sinks, thus leading to a strengthened greenhouse effect. More energy is thereby being supplied to the system, with inevitable shifts in climatic patterns and weather regimes. Over the last decades, these modifications have been manifested in the full statistical distributions of the atmospheric variables, with dramatic changes in the frequency and intensity of extremes. Natural hazards, such as severe droughts, floods, forest fires, or heatwaves, are being triggered by extreme atmospheric events worldwide, thus threatening human activities. Viticultculture is not only exposed to changing climates but is also highly vulnerable, as grapevine phenology and physiological development are strongly controlled by atmospheric conditions. Therefore, the assessment of climate change projections for a given region is critical for climate change adaptation and risk reduction in viticulture. By adopting timely and suitable measures, the future sustainability and resiliency of the sector can be fostered. Climate-grapevine chain modelling is an essential tool for better planning and management. However, the accuracy of the resulting projections is limited by many uncertainties that must be duly taken into account when transferring knowledge to stakeholders and decision-makers. Climate-smart viticulture will comprise ensembles of locally tuned strategies, envisioning both adaptation and mitigation, assisted by emerging technologies and decision-support systems.

Evolution of the amino acids content through grape ripening: Effect of foliar application of methyl jasmonate with or without urea

The parameters that determine the grape quality, and therefore the optimal harvest time, suffer variations during berry ripening, related to climate change, with the widely known problem of the gap between technological and phenolic maturities. However, there are few studies about its incidence on grape nitrogen composition. For this reason, the use of an elicitor, methyl jasmonate (MeJ), alone or with urea, is proposed as a tool to reduce climatic decoupling, allowing to establish the harvest time in order to achieve the optimum grape quality. The aim was to study the effect of MeJ and MeJ+Urea foliar applications on the evolution of Tempranillo amino acids content throughout the grape maturation. Three treatments were foliarly applied, at veraison and 7 days later: control (water), MeJ (10 mM) and MeJ+Urea (10 mM+6 kg N/ha). Grape samples were taken at five stages of maturation: day before the first and second applications, 15 days after the second application (pre-harvest), harvest day, and 15 days after harvest (post-harvest). The amino acids analysis of the samples was carried out by HPLC. Results showed that the evolution of amino acids was similar regardless of the treatment; however, foliar applications influenced the nitrogen compounds content, i.e., there was no qualitative effect but quantitative one. Most of the amino acids reached their maximum concentration in pre-harvest, being higher in grapes from the treatments than in the control. In general, no differences in grape amino acids content were observed between MeJ and MeJ+Urea treatments. Foliar applications with MeJ and MeJ+Urea enhanced the grape amino acids content, without affecting their profile, helping to optimize their quality and allowing to establish a more complete grape ripening standard. Therefore, MeJ and MeJ+Urea foliar applications can be a simple agronomic practice, which has shown promising results in order to enhance the grape quality.

Protected Designation of Origin (D.P.O.) Valdepeñas: classification and map of soils

The objective of the work described here is the elaboration of a map of the different types of vineyard soils that to guide the famers in the choice of the most productive vine rootstocks and varieties. 90 vineyard soils profiles were analysed in the entire territory of the Origen Denominations of Valdepeñas. The sampling was carried out in 2018 (June to October) by making a sampling grid, followed by photointerpretation and control in the field. The studied soils can be grouped into 9 different soil types (according to FAO 2006 classification): Leptosols, Regosols, Fluvisols, Gleysols, Cambisols, Calcisols, Luvisols and Anthrosols. A map showing the soil distribution with different type of soils has been made with the ArcGIS program. Regarding to the choice of rootstock, Calcisoles are soils with a high active limestone content, so the rootstocks used in these soils must be resistant to this parameter; Luvisols are deep soils with high clay content, so they will support vigorous rootstocks. Because the cartographic units are composed of two or more subgroups, with are associated in variable proportions, 9 different soil associations have been established; Unit 1: Leptosols, Cambisols and Luvisols (80%, 15% and 5% respectively); Unit 2: Cambisols with Regosols and Luvisols (40%, 30% and 30% respectively); Unit 3: Cambisols and Gleysols with Regosols (40%, 40% and 20% respectively); Unit 4: Regosols with Cambisols, Leptosols and Calcisols (40%, 30%, 15% and 15% respectively); Unit 5: Cambisols, Leptosols, Calcisols and Regosols (25% each of them); Unit 6: Luvisols with Cambisol and Calcisols (80%, 10% and 10% respectively); Unit 7: Luvisols and Calcisols with Cambisols (40%, 40% and 20% respectively); Unit 8: Calcisols with, Cambisols and Luvisols (80%, 10% and 10% respectively); Unit 9: Anthrosols. These study allow to elaborate the first map of vineyard soils of this Protected Designation of Origin in Castilla-La Mancha.

A better understanding of the climate effect on anthocyanin accumulation in grapes using a machine learning approach

The current climate changes are directly threatening the balance of the vineyard at harvest time. The maturation period of the grapes is shifted to the middle of the summer, at a time when radiation and air temperature are at their maximum. In this context, the implementation of corrective practices becomes problematic. Unfortunately, our knowledge of the climate effect on the quality of different grape varieties remains very incomplete to guide these choices. During the Innovine project, original experiments were carried out on Syrah to study the combined effects of normal or high air temperature and varying degrees of exposure of the berries to the sun. Berries subjected to these different conditions were sampled and analyzed throughout the maturation period. Several quality characteristics were determined, including anthocyanin content. The objective of the experiments was to investigate which climatic determinants were most important for anthocyanin accumulation in the berries. Temperature and irradiance data, observed over time with a very thin discretization step, are called functional data in statistics. We developed the procedure SpiceFP (Sparse and Structured Procedure to Identify Combined Effects of Functional Predictors) to explain the variations of a scalar response variable (a grape berry quality variable for example) by two or three functional predictors (as temperature and irradiance) in a context of joint influence of these predictors. Particular attention was paid to the interpretability of the results. Analysis of the data using SpiceFP identified a negative impact of morning combinations of low irradiance (lower than about 100 μmol m−2 s−1 or 45 μmol m−2 s−1 depending on the advanced-delayed state of the berries) and high temperature (higher than 25oC). A slight difference associated with overnight temperature occurred between these effects identified in the morning.