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…

First step in the preparation of a soil map of the Protected Designation of Origin Valdepeñas (Central, Spain)

This work is a first step to make a map of vineyard soils. The characterization of the soils of the Protected Designation of Origin (D.P.O.) Valdepeñas will allow to group the studied profiles according to their physico-chemical characteristics and the concentrations of most relevant chemical elements. 90 soil profiles were analysed throughout the territory and the soils were sampled and described according to FAO (2006) and classified according to and Soil Taxonomy (2014). All samples were air dried, sieved and some physico-chemical parameters were determined following standard protocols. Also, major and trace elements were analysed by X-ray fluorescence. The statistically study was made using the SPSS program. Trend maps were made using the ArcGIS program. The studied soils have the following average properties: pH, 8.3; electrical conductivity, 0,20 dS/m (low); clay, 18.8% (medium) and CaCO3, 17.1% (high). In the study for the major elements. The major elements of these soils are Si, followed by Ca and Al, with an average content of 203.7 g/kg, 105.5 g/kg and 74.0 g/kg respectively. On the other hand, 27 trace elements have been studied. Of all of them, it can be highlighted the average values of Ba (361.8 mg/kg), Sr (129.3 mg/kg), Rb (83.4 mg/kg), V (74.2 mg/kg) and Ce (70.6 mg/kg). Ba, V and Ce values are higher and the values of Sr and Rb are lower to those found in the literature. The discriminant analysis shows a percentage of grouping of 91%. The content of chemical elements together with the physico-chemical characteristics allows grouping the soils in 4 group according to their order in the classification to Soil Taxonomy; due to the importance of the Calcisols in Castilla-La Mancha, it has been decided to establish them as their own group even if they do not appear in Soil Taxonomy classification.

Adaptation to soil and climate through the choice of plant material

Choosing the rootstock, the scion variety and the training system best suited to the local soil and climate are the key elements for an economically sustainable production of wine. The choice of the rootstock/scion variety best adapted to the characteristics of the soil is essential but, by changing climatic conditions, ongoing climate change disrupts the fine-tuned local equilibrium. Higher temperatures induce shifts in developmental stages, with on the one hand increasing fears of spring frost damages and, on the other hand, ripening during the warmest periods in summer. Expected higher water demand and longer and more frequent drought events are also major concerns. The genetic control of the phenotypes, by genomic information but also by the epigenetic control of gene expression, offers a lot of opportunities for adapting the plant material to the future. For complex traits, genomic selection is also a promising method for predicting phenotypes. However, ecophysiological modelling is necessary to better anticipate the phenotypes in unexplored climatic conditions Genetic approaches applied on parameters of ecophysiological models rather than raw observed data are more than ever the basis for finding, or building, the ideal varieties of the future.

De novo Vitis champinii whole genome assembly allows rootstock-specific identification of potential candidate genes for drought and salt tolerance

Vitis champinii cultivars Ramsey and Dog-ridge are main choices for rootstocks to adapt viticulture in semi-arid and arid regions thanks to their distinctive tolerance to drought and salinity. However, genetic studies on non-vinifera rootstocks have heavily relied on the grapevine (Vitis vinifera) reference genome, which difficulted the assessment of the genetic variation between rootstock species and grapevines. In the present study, this limitation is addressed by introducing a novo phased genome assembly and annotation of Vitis champinii. This new Vitis champinii genome was employed as reference for mapping RNA-seq reads from the same species under drought and salt stresses, and for comparison the same reads were also mapped to the Vitis vinifera PN40024.V4 reference genome. A significant increase in alignment rate was gained when mapping Vitis champinii RNA-seq reads to its own genome, compared to the Vitis vinifera PN40024.V4 reference genome, thus revealing the expression levels of genes specific to Vitis champinii. Moreover, differences in coding sequences were observed in ortholog genes between Vitis champinii and Vitis vinifera, which therefore challenges previous differential expression analyses performed between contrasting Vitis genotypes on the same gene from the Vitis vinifera genome. Genes with possible implications in drought and salt tolerance have been identified across the genome of Vitis champinii, and the same genomic data can potentially guide the discovery of candidate genes specific from Vitis champinii for other traits of interest, therefore becoming a valuable resource for rootstock breeding designs, specially towards increased drought and salinity due to climate change.

Grapevine yield-gap: identification of environmental limitations by soil and climate zoning in Languedoc-Roussillon region (south of France)

Grapevine yield has been historically overlooked, assuming a strong trade-off between grape yield and wine quality. At present, menaced by climate change, many vineyards in Southern France are far from the quality label threshold, becoming grapevine yield-gaps a major subject of concern. Although yield-gaps are well studied in arable crops, we know very little about grapevine yield-gaps. In the present study, we analysed the environmental component of grapevine yield-gaps linked to climate and soil resources in the Languedoc Roussillon. We used SAFRAN data and IGP Pays d’Oc wine yields from 2010 to 2018. We selected climate and soil indicators proving to have a significant effect on average wine yield-gaps at the municipality scale. The most significant factors of grapevine yield were the Soil Available Water Capacity; followed by the Huglin Index and the Climatic Dryness Index. The Days of Frost; the Soil pH; and the Very Hot Days were also significant. Then, we clustered geographical zones presenting similar indicators, facilitating the identification of resources yield-gaps. We discussed the number of zones with the experts of IGP Pays d’Oc label, obtaining 7 zones with similar limitations for grapevine yield. Finally, we analysed the main resources causing yield-gaps and the grapevine varieties planted on each zone. Mapping grapevine resource yield-gaps are the first stage for understanding grapevine yield-gaps at the regional scale.

Influence of weather and climatic conditions on the viticultural production in Croatia

The research includes an analysis of the impact of weather conditions on phenological development of the vine and grape quality, through monitoring of four experimental cultivars (Chardonnay, Graševina, Merlot and Plavac mali) over two production years. In each experimental vineyard, which were evenly distributed throughout the regions of Slavonia and The Croatian Danube, Croatian Uplands,