Terroir 2010 banner
IVES 9 IVES Conference Series 9 Paysages viticoles et terroir dans l’OAC Ribeira Sacra (Galice, NO de l’Espagne)

Paysages viticoles et terroir dans l’OAC Ribeira Sacra (Galice, NO de l’Espagne)

Abstract

[English version below]

La notion d’Appellation d’Origine Contrôlée (AOC), repose sur l’existence d’un lien entre les caractéristiques du terroir et la qualité et la typicité de la production (DELAS, 2000). Si pendant longtemps, ce lien n’est apparu que comme le fruit de l’empirisme, les recherches entreprises dernièrement ont permis de fonder scientifiquement les relations complexes entre fonctionnement des milieux naturels et aptitude à une production de qualité.
L’aire d’AOC Ribeira Sacra s’étend sur presque 195 km au large des versants escarpés du Miño et du Sil, dans la Galice (Espagne). Cette AOC couvre presque 1100 hectares, soit 5,2% de la surface viticole galicien, produisant en moyenne 22000 hl du vin. Enfoncées de plusieurs centaines de mètres dans les vieilles surfaces d’aplanissement du massif ancien, les vallées du Miño et du Sil et les parties inférieures de certains de leurs affluents (Bibei, Cabe, Bubal et Mao), ont été découpées en un extraordinaire escalier de terrasses viticoles. Réservées à la viticulture –la vigne est souvent l’unique culture et lorsqu’elle n’existe pas, le versant est abandonné aux broussailles-, la construction de ces terrassettes (appelées “socalcos” par les paysans) a exigé un travail gigantesque de remodelage des versants et leur entretien demandait des soins constants.
Dans ces vallées en gorge, les terrasses viticoles occupent souvent tout le versant et encerclent les rares chicots rocheux qui n’ont pu être conquis. Ces terrasses, le plus souvent entaillées dans des roches granitiques, sont en effet de remarquables constructions: chaque “socalco”, qui suit les courbes de niveau sur des pentes qui atteignent parfois 45 degrés, est soutenu par un mur de pierre sèche et sa largeur est souvent si faible qu’il ne peut accueillir qu’une seule rangée de ceps (les gradins n’ont souvent plus d’un mètre de large). Ces terrasses constituent un exemple remarquable de formations anthropiques très effectives du point de vue de minimiser l’érosion du sol et de la formation de microclimats particulièrement adaptés aux besoins de la vigne.
Par leurs caractéristiques constructives on peut parler de véritables anthrosols. Du point de vue pédologique la région est bien homogène, même s’il y a quelques variations en raison des conditions particulières d’orographie, de la nature de la roche-mère (granites, gneiss, ardoises). Par contre, l’influence de l’altitude (200 à 450 m) et l’exposition (de l’ouest a sud-est) est évidente.
L’étude vise à caractériser les conditions climatiques, géologiques et pédologiques des différentes situations des vignobles d’OAC Ribeira Sacra, pour faire une première approximation à l’influence de l’altitude et l’exposition au zonage vitivinicole de l’AOC Ribeira Sacra.

The concept of Appellation d’Origine (AOC) is based on the existence of a link between the characteristics of the soil and quality and specificity of production grape and quality wine. This AOC include 1100 hectares (5.2% of the Galicia vineyard), planted on the valleys of the rivers Miño and Sil. The vine is planted in terraces, with different altitude (200-450 m) and exposition (west to southeast), example of anthropogenic formations very effective in terms of minimizing soil erosion and formation of microclimates particularly suited to the needs of vine. The area is divided into five sub-zones, with different edaphoclimate characteristics, Chantada, Amandi, Ribeiras do Miño, Ribeiras do Sil-Ourense, Quiroga-Bibei. The diversity of local climates allows to produce different type of cultivars, white (Albariño and Godello), as red (including Mencía, Brancellao and Merenzao).
This study aims to characterize the climatic conditions, geological and soil of vineyards of different situations from OAC Ribeira Sacra, to know the influence of altitude and exposure on wine characteristics.

DOI:

Publication date: December 3, 2021

Issue: Terroir 2010

Type: Article

Authors

Queijeiro J. (1), Vilanova M. (2), Rodriguez I. (1), de la Montaña J. (1)

(1) Sciences Faculty of Ourense, Edificio Politécnico, As Lagos s/n 32004. Ourense, Spain
(2) Misión Biológica de Galicia, Spain

Contact the author

Keywords

Ribeira Sacra, sols, pente, altitude, exposition
Mesoclimate, slope, bench terraces, altitude, exposition

Tags

IVES Conference Series | Terroir 2010

Citation

Related articles…

Soil functional characteristics for qualitative Sangiovese wine production in Tuscany (Italy)

Le but de ce travail est de faire une synthèse des résultats de plusieurs années de recherche en Italie centrale, sur les caractéristiques fonctionnelles du sol pour la production de vin de qualité. Le cépage de référence est le Sangiovese

Varietal differences between Shiraz and Cabernet sauvignon wines revealed by yeast metabolism

This study investigated if compositional differences between Shiraz and Cabernet Sauvignon grape varieties could influence the production of yeast-derived compounds. This work was based on the analysis of 40 experimental red wines made in triplicate fermentations from grapes harvested from two consecutive vintages in New South Wales (Australia). Grapes were picked at three maturity stages using berry sugar accumulation as physiological indicator, from nine commercial vineyards located in three different climatic regions (temperate, temperate-warm and warm-hot). A range of 30 yeast-derived wine volatiles including esters and alcohols were quantified by HS/SPME-GC/MS. Ammonia, amino-acids and lipids were analysed in the corresponding grapes. The juice total soluble solids (°Brix) in addition to the wine alcohol and residual sugar levels were also measured. The influence of grape maturity on wine ester composition was also variety dependent, particularly for higher alcohol acetate and ethyl ester of branched acids. This study highlights that varietal differences observed in Shiraz and Cabernet Sauvignon wines involve fermentation-derived compounds irrespective of the site (soil, climate, viticultural practices).

Intravarietal diversity: an opportunity for climate change adaptation

Merlot grapevine is the second wine cultivar most planted in the world and especially in the Bordeaux wine region. This cultivar has many advantages in producing high quality wine; however, in the last decade, climate change has increased the sugar concentration in berries at harvest and shortened the maturation cycle. If this has been up to now a great opportunity to improve wine quality profile, we are touching the tipping point. High sugar concentration at harvest induces high alcool content in wine which can negatively impact wine quality. There are many viticultural and oenological practices possible to limit this effect. In this study we focus on plant material through intra-varietal diversity of Merlot cultivar.

How much does the soil, climate and viticultural practices contribute to the variability of the terroir expression?

When considering the application of a systemic approach to assess the intrinsic complexity of agricultural production, the following question immediately arises

PINKING PHENOMENA ON WHITE WINES: RELATION BETWEEN PINKING SUSCEPTIBILITY INDEX (PSI) AND WINE ANTHOCYANINS CONTENT

Pinking is the emergence of pink tones in white wines exclusively produced from white grape varieties, known as pinking phenomena for many years. Pinking is essentially appeared when white wines are produced under reducing conditions [1,2,3]. Pinking usually occurs after bottling and storage of white wines, but its appearance has also been described after alcoholic fermentation or even as soon as the grape must is extracted [4]. Therefore, the purpose of this work was to investigate the existence of an-thocyanins in white wines made from different white grape varieties and grown locations and critically evaluate the most common method used for predicting pinking appearance in white wines: the Pinking Susceptibility Index (PSI).