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…

Assessing the climate change vulnerability of European winegrowing regions by combining exposure, sensitivity and adaptive capacity indicators

Winegrowing regions recognized as protected designations of origin (PDOs) are closely tied to well defined geographic locations with a specific set of pedoclimatic attributes and strictly regulated by legal specifications. However, climate change is increasingly threatening these regions by changing local conditions and altering winegrowing processes. The vulnerability to these changes is largely heterogenous across different winegrowing regions because it is determined by individual characteristics of each region, including the capacity to adapt to new climatic conditions and the sensitivity to climate change, which depend not only on natural, but also socioeconomic and legal factors. Accurate vulnerability assessments therefore need to combine information about adaptive capacity and climate change sensitivity with projected exposure to new climatic conditions. However, most existing studies focus on specific impacts neglecting important interactions between the different factors that determine climate change vulnerability. Here, we present the first comprehensive vulnerability assessment of European wine PDOs that spatially combines multiple indicators of adaptive capacity and climate change sensitivity with high-resolution climate projections. We found that the climate change vulnerability of PDO areas largely depends on the complex interactions between physical and socioeconomic factors. Homogenous topographic conditions and a narrow varietal spectrum increase climate change vulnerability, while the skills and education of farmers, together with a good economic situation, decrease their vulnerability. Assessments of climate change consequences therefore need to consider multiple variables as well as their interrelations to provide a comprehensive understanding of the expected impacts of climate change on European PDOs. Our results provide the first vulnerability assessment for European winegrowing regions at high spatiotemporal resolution that includes multiple factors related to climate exposure, sensitivity, and adaptive capacity on the level of single winegrowing regions. They will therefore help to identify hot spots of climate change vulnerability among European PDOs and efficiently direct adaptation strategies.

Water deficit differentially impacts the performances and the accumulation of grape metabolites of new varieties tolerant to fungi

The use of resistant varieties is a long-term but promising solution to reduce chemical input in viticulture. Several important breeding programs in Europe and abroad are now releasing a range of new hybrids performing well regarding fungi susceptibility and producing good quality wines. Unfortunately, insufficient attention is paid by the breeders to the adaptation of these varieties to climatic changes, notably to the increased climatic demand and water deficit (WD). Thus, prior to the adoption of such varieties by the wine industry in Mediterranean regions, there is a need to consider their suitability to WD. This study aimed to characterize the different drought-strategies adopted by 6 new resistant varieties selected by INRAE in comparison to Syrah. To allow the assessment of long-term impacts of WD, field-grown vines were exposed to contrasted WD from 2018 to 2021 under a semi-arid Mediterranean climate. A gradient of WD was applied in the field and controlled through plant measurements at the single plant level. Grape development was non-destructively monitored to determine the arrest of berry phloem unloading. The impacts of WD on berry composition, including water, primary metabolites (sugars, organic acids), secondary metabolites (anthocyanins, thiols precursors) and main cations contents, were assessed at this specific stage. Results showed different varietal responses during the year and inter-annual acclimation in terms of plant water use efficiency, biomass accumulation, as well as yield components and berry composition. WD differentially reduced the accumulation of primary metabolites at plant and berry levels, but it little changed their concentrations in the fruits at the ripe stage. Moreover, WD differentially impacted the accumulation of secondary metabolites and major cations between the varieties. In the talk, we’ll present the main results regarding the WD impacts on fruit metabolites and enlarge the reflection about the practical assessment of the grapevine acclimation to WD.

Late frost protection in Champagne

Probably one of the most counterintuitive impacts of climate change on vine is the increased frequency of late frost. Champagne, due to its septentrional position is historically and regularly affected by this meteorological hazard. Champagne has therefore developed a strong experience in frost protection with first experiments dating from the end of 19th century. Frost protection can be divided in two parts: passive and active. Passive protection includes all the methods that do not seek to modify the vine’s environment or resistance at the time of frost. The most iconic passive protection in Champagne is the establishment of the individual reserve. This reserve allows to stock a certain quantity of clear wine during a surplus year to compensate a meteorological hazard like frost during the following years. Other common passive methods are the control of planting area (walls, bushes, topography), the choice of grape variety, late pruning, or the impact of grass cover and tillage. Active frost protection is also divided in two parts. Most of the existing techniques tend to modify vine’s environment. Most of the time they provide warmth (candles, heaters, windmills, heating cables…), or stabilise bud’s temperature above a lethal threshold (water sprinkling). The other way to actively fight is to enhance the resistance of buds to frost (elicitors). The Comité Champagne evaluates frost protection methods following three main axes: the efficiency, the profitability, and the environmental impact through a lifecycle assessment. This study will present the results on both passive and active protection following these three axes.

Local adaptation tools to ensure the viticultural sustainability in a changing climate

[lwp_divi_breadcrumbs home_text="IVES" use_before_icon="on" before_icon="||divi||400" module_id="publication-ariane" _builder_version="4.19.4" _module_preset="default" module_text_align="center" module_font_size="16px" text_orientation="center"...

Influence of agronomic practices in soil water content in mid-mountain vineyards

In the context of LIFE project MIDMACC (LIFE18 CCA/ES/001099), several pilots have been installed in vineyards in mid mountain areas of Catalonia (NE Spain) to test well stablished agronomic practices to increase the adaptation of Mediterranean mid mountain to climate change. Soil water content (SWC) at three different depths (15, 30 and 45cm) was measured in continuum from August 2020. One pilot (WC) included a well-established green cover (GC), a new GC (NC) and a conventional soil management (CM, tilling+herbicides). NC presented an intermediate state between WC and CM, responding similarly to CM in autumn but quickly reaching similar SWC to WC, then following the same evolution till next spring, with CM presenting lower values along autumn and winter. Then vegetation activation decreased SWC in all plots, (much slower in CM, lacking GC). Sensibility to spring rains is again intermediate for NC, which joins SWC evolution of CM by the end of spring till next autumn. It is expected that NC will resemble WC more and more as its GC develops. In the pilot combining vine training (VSP vs Gobelet) and hillside management (slope vs terrace), no clear pattern could be related with these conditions. However, both terraces seem to be more sensitive to spring rains. A third pilot included new vineyards (7 and 1 year old). In the new vineyard (N), higher canopy development, a spontaneous green cover and row straw resulted in a slower SWC dynamic, not so sensitive to rains but conserving more soil water in spring and most of summer, even with presumably a higher water extraction by vines. In the newest vineyard (VN) the deepest sensor is still sensitive to rain events all over the year and SWC is always highest at this depth, revealing small water capture by vines.