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…

Estimating bulk stomatal conductance of grapevine canopies

In response to changes in their environment, grapevines regulate transpiration using various physiological mechanisms that alter conductance of water through the soil-plant-atmosphere continuum. Expressed as bulk stomatal conductance at the canopy scale, it varies diurnally in response to changes in vapor pressure deficit and net radiation, and over the season to changes in soil water deficits and hydraulic conductivity of both soil and plant. It is necessary to characterize the response of conductance to these variables to better model how vine transpiration also responds to these variables. Furthermore, to be relevant for vineyard-scale modeling, conductance is best characterized using data collected in a vineyard setting. Applying a crop canopy energy flux model developed by Shuttleworth and Wallace, bulk stomatal conductance was estimated using measurements of individual vine sap flow, temperature and humidity within the vine canopy, and estimates of net radiation absorbed by the vine canopy. These measurements were taken on several vines in a non-irrigated vineyard in Bordeaux France, using equipment that did not interfere with ongoing vineyard operations. An inverted Penman-Monteith equation was then used to calculate bulk stomatal conductance on 15-minute intervals from July to mid-September 2020. Time-series plots show significant diurnal variation and seasonal decreases in conductance, with overall values similar to those in the literature. Global sensitivity analysis using non-parametric regression found transpiration flux and vapor pressure deficit to be the most important input variables to the calculation of bulk stomatal conductance, with absorbed net radiation and bulk boundary layer conductance being much less important. Conversely, bulk stomatal conductance was one of the most important inputs when calculating vine transpiration, further emphasizing the need for characterizing its response to environmental changes for use in vineyard water use modeling.

Terroir analysis and its complexity

Terroir is not only a geographical site, but it is a more complex concept able to express the “collective knowledge of the interactions” between the environment and the vines mediated through human action and “providing distinctive characteristics” to the final product (OIV 2010). It is often treated and accepted as a “black box”, in which the relationships between wine and its origin have not been clearly explained. Nevertheless, it is well known that terroir expression is strongly dependent on the physical environment, and in particular on the interaction between soil-plant and atmosphere system, which influences the grapevine responses, grapes composition and wine quality. The Terroir studying and mapping are based on viticultural zoning procedures, obtained with different levels of know-how, at different spatial and temporal scales, empiricism and complexity in the description of involved bio-physical processes, and integrating or not the multidisciplinary nature of the terroir. The scientific understanding of the mechanisms ruling both the vineyard variability and the quality of grapes is one of the most important scientific focuses of terroir research. In fact, this know-how is crucial for supporting the analysis of climate change impacts on terroir resilience, identifying new promised lands for viticulture, and driving vineyard management toward a target oenological goal. In this contribution, an overview of the last findings in terroir studies and approaches will be shown with special attention to the terroir resilience analysis to climate change, facing the use and abuse of terroir concept and new technology able to support it and identifying the terroir zones.

Influence of climatic conditions on grape composition of Tempranillo in La Mancha DO (Spain)

The aim of this work was to analyze the variability in grape composition of the Tempranillo cultivar related to climatic conditions, in La Mancha Designation of Origin. Grape composition (sugar content, total acidity, pH, malic acid, and total and extractable anthocyanins) recorded during ripening, were analysed for the period 2000-2019. The weather conditions at daily time scale, recorded during the same period, were also evaluated. The relationships between grape parameters with climatic variables related to temperature and to water deficits, referring different periods between phenological events along the growing cycle, were evaluated using regression analysis. High variability in grape composition was observed in the period analysed. Total acidity varied between 3.7 and 7.3 gL-1 while malic acid varied between 1.2 and 4 gL-1. The extractable anthocyanins ranged between 526 and 972 mgL-1, and total anthocyanins ranged between 922 and 1388 mgL-1, being the lowest values recorded in the hottest year (2017). Total acidity decreased 0.77 gL-1 for an increase of 100 GDD, while malic acid decrease in 0.42 gL-1 for the same GDD increase, being the period between veraison and harvest the one that seemed to have higher influence on acidity. In addition, it was confirmed that increasing water deficits decreased acidity. Total and extractable anthocyanins increased in about 210 and 105 mgL-1, respectively, with an increase of 100 GDD from veraison to harvest, and the increase in water deficits favour the increase of anthocyanins, both total and extractable anthocyanins. Total and extractable anthocyanins concentration increased in 35 and 22 mgL-1 per an increase of 10 mm in the water deficit. These results can be of interest to understand the potential changes that grapes composition may suffer under future warmer climates.

Elucidating vineyard site contributions to key sensory molecules: Identification of correlations between elemental composition and volatile aroma profile of site-specific Pinot noir wines

The reproducibility of elemental profile in wines produced across multiple vintages has been previously reported using grapes from a single scion clone of Vitis vinifera L. cv. Pinot noir. The grapevines were grown on fourteen different vineyard sites, from Oregon to southern California in the U.S.A., which span distances from approximately hundreds of meters to 1450 km, while elevations range from near sea level to nearly 500 m. In addition, sensorial (i.e. aroma, taste, and mouthfeel) and chemical (i.e. polyphenolic and volatile) differences across the different vineyard sites have also been observed among these wines at two aging time points. While strong evidence exists to support that grapes grown in different regions can produce wines with unique chemical and sensorial profiles, even when a single clone is used, the understanding of growing site characteristics that result in this reproducible differentiation continues to emerge. One hypothesis is that the elemental profile that a vineyard site imparts to the grape berries and the resulting wine is an important contributor to this differentiation in chemistry and sensory of wines. For example, various classes of enzymes that catalyze the formation of key aroma compounds or their precursors require specific metals. In this work, we begin to report correlations between elemental and volatile aroma profiles of site-specific Pinot noir wines, made under standardized winemaking conditions, that have been previously shown to be distinguished separately by these chemical analyses.

The use of rootstock as a lever in the face of climate change and dieback of vineyard

As viticulture faces challenges such as climate change or vineyard dieback, the choice of the variety and rootstock becomes more and more crucial. To study rootstock levers in the Bordeaux region, a parcel of Cabernet Sauvignon (CS) was planted with four rootstocks in 2014. Twenty repetitions of each of the following four rootstocks were set up: 101-14 MGt, Nemadex AB, 420A MGt and Gravesac. The number of bunches, yields and pruning weights of the vine shoots were measured individually on 240 vines from 2017 to 2021. Since 2020, nitrogen status assessed by assimilable nitrogen level, hydric status assessed by δ13C and berry maturity were measured on 80 samples taken from 20 repetitions of the four rootstocks. A lower yield was measured for CS grafted onto Nemadex AB due to the lower number of bunches and the lower weight of berries. The differences between the other three rootstocks are small, but CS grafted onto 420A MGt was the most productive. The CS grafted onto Nemadex AB had the lowest pruning weight while 101-14 MGt had the highest. In 2020, δ13C showed a more moderate water stress with 101-14 MGt and 420A MGt than with Nemadex AB. Surprisingly, the Gravesac was under more stress than the 101-14 MGt. The nitrogen status in the berries was better for Nemadex AB but this was perhaps due to the significantly lower weight of the berries.Rootstock 101-14 MGt attained the highest accumulation of sugars in the berries while 420A MGt allows to preserve higher acidity. The parcel is still young which may explain some of the results. These measures must therefore be continued over the next several years to fully assess the effects of these rootstocks on the development of the vines and the quality of the production under new climatic conditions.