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.

An analytical framework to site-specifically study climate influence on grapevine involving the functional and Bayesian exploration of farm data time series synchronized using an eGDD thermal index

Climate influence on grapevine physiology is prevalent and this influence is only expected to increase with climate change. Although governed by a general determinism, climate influence on grapevine physiology may present variations according to the terroir. In addition, these site-specific differences are likely to be enhanced when climate influence is studied using farm data. Indeed, farm data integrate additional sources of variation such as a varying representativity of the conditions actually experienced in the field. Nevertheless, there is a real challenge in valuing farm data to enable grape growers to understand their own terroir and consequently adapt their practices to the local conditions. In such a context, this article proposes a framework to site-specifically study climate influence on grapevine physiology using farm data. It focuses on improving the analysis of time series of weather data. The analytical framework includes the synchronization of time series using site-specific thermal indices computed with an original method called Extended Growing Degree Days (eGDD). Synchronized time series are then analyzed using a Bayesian functional Linear regression with Sparse Steps functions (BLiSS) in order to detect site-specific periods of strong climate influence on yield development. The article focuses on temperature and rain influence on grape yield development as a case study. It uses data from three commercial vineyards respectively situated in the Bordeaux region (France), California (USA) and Israel. For all vineyards, common periods of climate influence on yield development were found. They corresponded to already known periods, for example around veraison of the year before harvest. However, the periods differed in their precise timing (e.g. before, around or after veraison), duration and correlation direction with yield. Other periods were found for only one or two vineyards and/or were not referred to in literature, for example during the winter before harvest.

Late season canopy management practices to reduce sugar loading and improve color profile of Cabernet-Sauvignon grapes and wines in the high irradiance and hot conditions of California Central Valley

Global warming is accelerating grape ripening, leading to unbalanced wines from fruit with high sugar content but poor aroma and colour development. Reducing the size of the photosynthetic apparatus after veraison has been shown to delay technological ripeness in cool climates, but methods have not been tested in areas with high irradiance and temperature where fruit exposure could have disastrous effects on berry composition. In this Cabernet-Sauvignon trial, we compared the application of an antitranspirant (pinolene), to severe canopy topping and above bunch zone leaf removal, all performed at mid-ripening, with an untouched control. We monitored the vines weekly by measuring stem water potential, gas exchange, fruit zone light exposure. We sampled berries to measure berry weight, total soluble solids, pH, titratable acidity, and the anthocyanin profile. At harvest, we assessed yield components, measured carbon isotope discrimination, rated sunburn on clusters, and produced experimental wines. We submitted harvest samples to metabolomic profiling through PFP-Q Exactive MS/MS and wines to sensory analysis. Application of the antitranspirant significantly reduced stomatal conductance and assimilation rate but did not affect the stem water potential. Inversely, leaf removal and topping increased water potential but did not affect leaf gas exchange. The late topping was the only treatment able to decrease sugar content (up to 2Bx), increase titratable acidity and pH, and improve anthocyanin content because of lower degradation of di-hydroxylated forms. Late leaf removal above the bunch zone increased lightning conditions in the canopy and produced the most significant damage on fruits. Yield components were not affected. This work suggests that late-season canopy management can effectively control ripening speeds and improve grapes and wines. Still, the effect on grape exposure in a critical time must be well balanced to avoid problems with the appropriate technique.

Low-cost sensors as a support tool to monitor soil-plant heat exchanges in a Mediterranean vineyard

Mediterranean viticulture is increasingly exposed to more frequent extreme conditions such as heat waves. These extreme events co-occur with low soil water content, high air vapor pressure deficit and high solar radiant energy fluxes and result in leaf and berry sunburn, lower yield, and berry quality, which is a major constraint for the sustainability of the sector. Grape growers must find ways to proper and effectively manage heat waves and extreme canopy and berry temperatures. Irrigation to keep soil moisture levels and enable adequate plant turgor, and convective and evaporative cooling emerged as a key tool to overcome this major challenge. The effects of irrigation on soil and plant water status are easily quantifiable but the impact of irrigation on soil and canopy temperature and on heat convection from soil to cluster zone remain less characterized. Therefore, a more detailed quantification of vineyard heat fluxes is highly relevant to better understand and implement strategies to limit the effects of extreme weather events on grapevine leaf and berry physiology and vineyards performance. Low-cost sensor technologies emerge as an opportunity to improve monitoring and support decision making in viticulture. However, validation of low-cost sensors is mandatory for practical applicability. A two-year study was carried in a vineyard in Alentejo, south of Portugal, using low-cost thermal cameras (FLIR One, 80×60 pixels and FLIR C5, 160×120 pixels, 8-14 µm, FLIR systems, USA) and pocket thermohygrometers (Extech RHT30, EXTECH instruments, USA) to monitor grapevine and soil temperatures. Preliminary results show that low-cost cameras can detect severe water stress and support the evaluation of vertical canopy temperature variability, providing information on soil surface temperature. All these thermal parameters can be relevant for soil and crop management and be used in decision support systems.

Vineyards and clay minerals: multi-technique analytical approach and correlations with soil properties

Purpose of this research is to quantitatively assess the mineral component of vineyard soils, with particular attention to the mineralogical analysis of clays, which represent an element of high importance in the vineyard culture as well as in general agriculture. An X-ray diffraction (XRD) / thermogravimetric (TG) multi-technique analytical approach was developed, tested on soil samples taken from vineyards around the world. This codified analytical procedure was necessary to obtain precise qualitative and quantitative mineralogical data, globally comparable to distinguish the geopedological identity of the vineyards. Soil samples from vineyards of various locations were analysed, in very different geological conditions. The bulk-rock quantitative phase analysis (QPA) was obtained by the Rietveld method while the detailed composition of the clay-sized fraction was determined by modelling of the oriented X-ray diffraction patterns. The research provided a precise classification of the mineral component of soils, distinguishing the mineral phases of the clays and the so-called mixed-layer clay minerals. We found that the content in mixed layers can be directly correlated with the water retention and the cation exchange capacity ​​of the soil, while the presence of other clayey minerals and phyllosilicates in this research did not affect this CEC parameter, which codes the fertility level of the soils. The study demonstrates that terroir, in particular soils formed in complex or very different geological conditions, can only be effectively interpreted by properly analysing its mineral phases, in particular the mixed-layer clay component. These are characteristic abiotic ecological indicators, which may have specific eco-physiological influences on the plant.