Terroir 2010 banner
IVES 9 IVES Conference Series 9 Geology and landscape as determining factors in microfields and development of the different Spanish appellations of origin

Geology and landscape as determining factors in microfields and development of the different Spanish appellations of origin

Abstract

Dividing agrarian exploitations into microfields is a problem that influences the modern viticulture in a very important way. The aim of this work is the study of the influence of Geology and Geomorphology in agricultural structures, and more exactly applied to viticulture microfields, as determining factors in evolution and development of certain Appellation of Origin (AO). The field division of three AO in the Northwest of Spain (Toro, Bierzo, Arribes) is compared. These three regions were chosen because they have similar influence elements.
The Toro AO (total area 76.076,43 ha; vineyard area 4.887,12 ha) is located to the West of Duero river basin and it is formed with limestone and carbonated detritic materials from the tertiary series and with the materials from the glacis and the medium and low terraces of the own river. In this context the altitude difference is small (650-825 m) and the shapes are flat and smooth in the quaternary relieve and undulating in the link tertiary surfaces with slopes under 20%. There are neither rocky outcrops nor stoniness to block the crop technical development.
The Bierzo AO (total area 142.672,08 ha; vineyard area 3.785,33 ha) is located in a sinking intermontane depression basin that is filled up with terraces materials, plioquaternary piedmont which are locally linked through tertiary detritical series with quartzite and schist materials that end in the primary mountainous edges due to basin close. The difference among cotes is important (525-1100 m) and the slopes are very changeable; flat in the alluvials, medium and high in the tertiary relieves and very high in the mountainous ones. Only in the mountainous basin edges there are some zones with rocky outcrops that block the crop technical development.
The Arribes AO (total area 101.969,94 Ha, vineyard area 1.66679 Ha) is located in an erosive surface that includes a whole of deep incisions and canyons of the Duero and its associated systems. In this surface the granite materials and schist, gneiss and quartzite paleozoic materials are predominant. These materials are locally covered with rests of glacis and quaternary materials and these filled up some depressions. The relief is very varied, from soft undulating surfaces in the erosive zone to vertical walls related to the incisions. In the whole AO the rocky outcrops and the stoniness make up or have made up an obstacle to the crop technical development.
Even though in the three AO a selection of the medium size is appreciated, the vineyard medium size is more than two times smaller in Toro AO (2.84) and in Bierzo AO (2.84), but more than five times smaller (5.54) in Arribes AO. On the other hand, while in the Toro AO, the wine-grower can select the better quality zones and zones with a proper structure and a independent of the considered elements, in Bierzo AO and in Arribes AO the vine-growers election possibilities are much lower or there are problems with the slopes which are often in relationships to the soil small effective depth, or if these problems have been eliminated by the effort through centuries the microfields division impede the vineyard crop technical development; the vineyard medium size is more than ten times higher in Toro AO, than in Bierzo AO and Arribes AO.

DOI:

Publication date: December 3, 2021

Issue: Terroir 2010

Type: Article

Authors

Vicente GOMEZ-MIGUEL (1), Vicente SOTES (1)

(1) Universidad Politécnica de Madrid (UPM). Avda Complutense s/n. 28040-Madrid, Spain

Contact the author

Keywords

terroir, zoning, landscape, geology, microfield, Appellations of Origin, Spain

Tags

IVES Conference Series | Terroir 2010

Citation

Related articles…

Evaluation of climate change impacts at the Portuguese Dão terroir over the last decades: observed effects on bioclimatic indices and grapevine phenology

In the last decades the growers of the Portuguese Dão winegrowing region (center of Portugal) are experiencing changes in climate that are influencing either grape phenology berry health and ripening. Aiming to study the relationships between climate indices (CI), seasonal weather and grapevine phenology, in this work long-term climate and phenological data collected at the experimental vineyard of the Portuguese Dão research centre between 1958 and 2019 (61 years) for the red variety Touriga Nacional, was analyzed. The trends over time for the classical temperature-based indices (Growing Season Temperature – GST -, Growing Degree Days – GDD, Huglin Index – HI and Cool Night Index – CI) presented a significantly positive slope while the Dryness Index (DI) showed a negative trend over the last 61 years. Regarding grapevine phenology, an average advance of 4.5 days per decade in the harvest day was observed throughout the last 61 years. Consequently, the weather conditions during the ripening period have changed, showing an increasing trend over time in the average temperature (higher magnitude in the maximum than in the minimum temperature) and a decrease in the accumulated rainfall. A regression analysis showed that ~50% of harvest date variability over years was explained by the temperature-based indices variability. These observed effects of climate change on bioclimatic indices and corresponding anticipation of harvest date can still be considered advantageous for the Dão terroir as it allows to achieve an optimal berry ripening before the common equinox rains and, therefore, avoid the potential negative impacts of the rainfall on berry health and composition.

Amino nitrogen content in grapes: the impact of crop limitation

As an essential element for grapevine development and yield, nitrogen is also involved in the winemaking process and largely affects wine composition. Grape must amino nitrogen deficiency affects the alcoholic fermentation kinetics and alters the development of wine aroma precursors. It is therefore essential to control and optimize nitrogen use efficiency by the plant to guarantee suitable grape nitrogen composition at harvest. Understanding the impact of environmental conditions and cultural practices on the plant nitrogen metabolism would allow us to better orientate our technical choices with the objective of quality and sustainability (less inputs, higher efficiency). This trial focuses on the impact of crop limitation – that is a common practice in European viticulture – on nitrogen distribution in the plant and particularly on grape nitrogen composition. A wide gradient of crop load was set up in a homogeneous plot of Chasselas (Vitis vinifera) in the experimental vineyard of Agroscope, Switzerland. Dry weight and nitrogen dynamics were monitored in the roots, trunk, canopy and grapes, during two consecutive years, using a 15N-labeling method. Grape amino nitrogen content was assessed in both years, at veraison and at harvest. The close relationship between fruits and roots in the maintenance of plant nitrogen balance was highlighted. Interestingly, grape nitrogen concentration remained unchanged regardless of crop load to the detriment of the growth and nitrogen content of the roots. Meanwhile, the size and the nitrogen concentration of the canopy were not affected. Leaf gas exchange rates were reduced in response to lower yield conditions, reducing carbon and nitrogen assimilation and increasing intrinsic water use efficiency. The must amino nitrogen profiles could be discriminated as a function of crop load. These findings demonstrate the impact of plant balance on grape nitrogen composition and contribute to the improvement of predictive models and sustainable cultural practices in perennial crops.

Mesoclimate impact on Tannat in the Atlantic terroir of Uruguay

The study of climate is relevant as an element conditioning the typicity of a product, its quality and sustainability over the years. The grapevine development and growth and the final grape and wine composition are closely related to temperature, while climate components vary at mesoscale according to topography and/or proximity to large bodies of water. The objective of this work is to assess the mesoclimate of the Atlantic region of Uruguay and to determine the effect of topography and the ocean on temperature and consequently on Tannat grapevine behavior.

Climate, Viticulture, and Wine … my how things have changed!

The planet is warmer than at any time in our recorded past and increasing greenhouse emissions and persistence in the climate system means that continued warming is highly likely. Climate change has already altered the basic framework of growing grapes for wine production worldwide and will likely continue to do so for years to come. The wine sector can continue to play an important role in leading the agricultural sector in addressing climate change. From developing on…

δ13C : A still underused indicator in precision viticulture  

The first demonstration of the interest of carbon isotope composition of sugars in grapevine, as an integrated indicator of vineyard water status, dates back to 2000 (Gaudillère et al., 1999; Van Leeuwen et al., 2001). Thanks to the isotopic discrimination of Carbon that takes place during plant photosynthesis, under hydric stress conditions, it is possible to accurately estimate the photosynthetic activity. Ever since, δ13C has been widely applied with success to zonation, terroir studies and vine physiology research, but is still not widely used by viticulturists. This is quite astonishing by considering the impact of global warming on viticulture and the need to improve water management, that would justify a widespread use of δ13C.
The lack of private laboratories proposing the analysis, the cost of the technology, as well as the long analytical delays, have been detrimental to its development. Some laboratories tried to overcome the analytical difficulties of isotopic analysis by using fourier transformed infrared spectroscopy, as a fast and cheap alternative to the official OIV method (IRMS). These claimed FTIR models have never been published or peer reviewed and cannot be considered robust. In this work, thanks to the recent acquisition of IRMS technology, new modern and robust applications of δ13C for viticulture are proposed. This includes the use of the analysis to make parcel separations at harvesting, the possibility to increase the precision of hydric stress cartography and the potential cost reduction when compared with Scholander pressure bomb analysis.