Terroir 1996 banner
IVES 9 IVES Conference Series 9 Efecto de distintos ambientes sobre las características físico – químicas y sensoriales del Montepulciano d’Abruzzo DOC

Efecto de distintos ambientes sobre las características físico – químicas y sensoriales del Montepulciano d’Abruzzo DOC

Abstract

La región de Abruzzo está situada entre los Apeninos y el mar Adriático, limitando al norte con el río Tronto y al sur con el Trigno. Desde un punto de vista físico se divide en dos franjas: una montañosa al oeste constituida por rocas calcáreas con frecuentes fenómenos de erosión debido a las corrientes de agua y a la naturaleza calcárea del terreno (“carsismo”) y otra al este, más cercana al mar, representada por una amplia zona de colinas constituida por terrenos arcilloso ​calcáreos y arenosos. Obviamente el clima está influido por la presencia de las grandes montañas del Gran Sasso y Maiella y también por la proximidad al mar Adriático. Así, en las cercanías de la zona montañosa, en la parte occidental, la temperatura difícilmente alcanza la media anual de 12°C, mientras que en la región mas cercana al mar la media anual oscila entre los 12° y los 16°C. Exponemos, a este respecto, las conclusiones de Matassa et al. (1992): “El clima de Abruzzo está influenciado fuertemente por la orografía montañosa y muestra una fuerte variabilidad, pasando de regiones templadas en la costa, a moderadamente templadas en los valles internos y las altas colinas litorales, a moderadamente frías y frías en las montañas”. Así que en general el clima se puede considerar apacible y a excepción de algunas zonas particularmente secas del sur de la región, se da un buen nivel de pluviosidad y es altamente soleado (Matassa et al., 1992). En el área observada por nosotros, en el territorio de Vasto, la pluviosidad, definida por los valores registrados en las estaciones del “Genio Civile” (ente estatal, perteneciente al ministerio italiano de obras públicas) durante el período 1965-93, muestra un aumento desde la costa hacia el interior, pasando de los 630 mm deVasto a los 850 mm de Montazzoli. La actividad vinícola juega un papel de primordial importancia en la economía agrícola del territorio de Vasto ya sea en términos de superficie cultivada como en términos de producción bruta a la venta. En dicha área, 6000 hectáreas están dedicadas al cultivo de la vid, de las cuales aproximadamente 480 (1.8 %) pertenecen a la colina del interior y la alta colina próxima a los montes, mientras que las restantes 5500 ha (92% del total) están localizadas en la colina litoral. La forma de cultivo mas difundida es el clásico emparrado con distancias de plantación de 2,5m x 2,5 m a pesar de que en los últimos años se han adoptado otros sistemas como el GDC.
La región de Abruzzo, a través del ARSSA (Agenzia Regionale per i Servizi di Sviluppo Agricolo), ha participado en el proyecto “Caracterización de vinos típicos” y ha seleccionado el territorio de Vasto para el programa de caracterización del vino Montepulciano d’Abruzzo a Denominación de Origen. El criterio que se ha adoptado para la división del territorio y para el muestreo, ha tenido en consideración esencialmente la disponibilidad térmica, definida a través de los índices bioclimáticos de Winkler e Huglin con referencia a un trabajo precedente que consideraba dichos parámetros a nivel regional (Matassa et al., 1992). Debemos considerar, además, que las características pedológicas cambian poco dentro de cada area examinada, y la forma de cultivo, el emparrado, es la única en todo el territorio. Se considera que la compleja orografía del territorio puede influir de forma notable sobre la distribución de la disponibilidad térmica, determinando una amplia posibilidad de condiciones ambientales dentro de cada zona DOC del vino.
Sobre la base de las consideraciones expuestas se han definido tres áreas a distinta distancia de la costa (fig.1) caracterizadas por disponibilidades térmicas en disminución. Dentro de cada una de ellas se han elegido 5 viñedos muestra (tab.1).
Area A: representativa de la colina litoral donde el cultivo vitícola es mayor. En esta zona el viñedo del ayuntamiento de Pollutri se diferencia de los otros (Casalbordino e Scerni) por la altitud de solamente 40 m sobre el nivel del mar.
Area B: representativa de la colina adyacente a la litoral. Los viñedos pertenecen a dos ayuntamientos , de los cuales uno (Furci) tiene una altitud 3 veces superior a los restantes.
Area C: representativa de la colina próxima a los montes. Los viñedos pertenecen a un solo ayuntamiento y la altitud de los viñedos va desde los 470 a los 555 m sobre el nivel del mar.

DOI:

Publication date: February 25, 2022

Issue: Terroir 2000

Type: Article

Authors

B.Di Lena (1), M. Ubigli (2), M.C. Cravero (2), D. Voerzio (2), M.C. Pazo-Alvarez (2)

(1) A.R.S.S.A. Centro Agrometeorologico Regionale ​Via Colle Comune 11, 66020 Scerni (CH)- Italia
(2) Istituto Sperimentale per l’Enologia, Via P. Micca 35, 14100 Asti (AT) – Italia

Tags

IVES Conference Series | Terroir 2000

Citation

Related articles…

Rootstock regulation of scion phenotypes: the relationship between rootstock parentage and petiole mineral concentration

Grapevine is grown as a graft since the end of the 19th century. Rootstocks not only provide tolerance to Phylloxera but also ensure the supply of water and mineral nutrients to the scion. Rootstocks are an important mean of adaptation to environmental conditions, because the scion controls the typical features of the grapes and wine. However, among the large diversity of rootstocks worldwide, few of them are commercially used in the vineyard. The aim of this study was to investigate the extent to which rootstocks modify the mineral composition of the petioles of the scion. Vitis vinifera cvs. Cabernet-Sauvignon, Pinot noir, Syrah and Ugni blanc were grafted onto 55 different rootstock genotypes and planted in a vineyard as three replicates of 5 vines. Petioles were collected in the cluster zone with 6 replicates per combination. Petiolar concentrations of 13 mineral elements (N, P, K, S, Mg, Ca, Na, B, Zn, Mn, Fe, Cu, Al) at veraison were determined. Scion, rootstock and the interaction explained the same proportion of the phenotypic variance for most mineral elements. Rootstock genotype showed a significant influence on the petiole mineral element composition. Rootstock effect explained from 7 % for Cu to 25 % for S of the variance. The difference of rootstock conferred mineral status is discussed in relation to vigor and fertility. Rootstocks were also genotyped with 23 microsatellite markers. Data were analysed according to genetic groups in order to determine whether the petiole mineral composition could be related to the genetic parentage of the rootstock. Thanks to a highly powerful design, it is the first time that such a large panel of rootstocks grafted with 4 scions has been studied. These results give the opportunity to better characterize the rootstocks and to enlarge the diversity used in the vineyard.

Terroir traceability in grapes, musts and wine: results of research on Gewürztraminer and Sauvignon Blanc grape varieties in northern Italy

In the study of terroir, a separate analysis of its many component factors can be of great help in accurately identifying a vineyard’s natural elements that impact wine quality and typicity. This research used a dedicated pluri-disciplinary approach to investigate the ecological characteristics, including geology and geographical features, of 14 vineyards that produce Gewürztraminer and Sauvignon Blanc cultivars in the alpine Alto Adige DOC wine region. Both the geopedological method using Vineyards Geological Identity (VGI) and the new Solar Radiaton Identity (SRI) topoclimatic classification method were used to provide analytical measurements and qualitative/quantitative characterisations. In addition, wide-ranging targeted and untargeted oenological and chemical analyses were carried out on grapes, musts and wines to correlate the soils’ geomineral and physical conditions with the biochemical properties of their fruits and wines. The research identified strong correlations between vineyard geo-identity and wine biofingerprint, confirming a mineral traceability of strontium rubidium ratio and some minerals distinctive to the local geology, such as K, Ca, Ag, Ba and Mn.  The study also discovered that particular geomineral and physical soil conditions of the studied vineyards are related to the different amount of amino acids, primary varietal aromas and polyphenols found in grapes, musts and wines. The research confirmed that winemaking technologies support oenological quality, although in some cases, human practices can overpower certain characteristic elements in wine, erasing the typical imprint left by the vineyards’ natural terroir, which becomes less traceable. Terroir abiotic ecological factors and vineyard identity can be classified in detail using the new VGI and SRI analysis methods to discover interrelationships between geo-pedological and topoclimatic conditions that impact wine quality. These methods are also helpful in identifying which ecological elements are exclusive to a particular vineyard or wine sub-region.

Soil quality in Beaujolais vineyard. Importance of pedology and cultural practices

A pedological study was carried out from 2009 to 2017 in Beaujolais vineyard, to improve physical and chemical knowledge of soils. It was completed in 2016 and 2017 by the current study, dealing with microbial aspects, in order to build a reference frame for improved advice in soil management. Microbial biomass was measured on representative plots of the six most common soil types identified in Beaujolais and, for each soil type, on plots with different levels of the main impacting parameters: total organic carbon, pH, cation exchange capacity, extractable copper. A total of 59 soil samples were collected. Confirming the results of various trials carried out in Beaujolais over the past 20 years, the results of the present study showed that the soils were still alive, but exhibited a large variability of biological parameters, which appeared dependant on both pedological and anthropic factors. Therefore, a good interpretation of biological parameters and advice for vine growers must rely on a pedologically-based referential with differentiated main driving factors. For example, the control of pH is of primary importance in granitic soils and in no way organic matter addition can improve soil quality if pH is too low. Conversely, in calcareous soils, biological parameters are more directly affected by direct or indirect (cover crops for example) inputs of organic matter. The use of biological parameters, such as microbial biomass, is of great potential value to improve advice on agro-viticultural practices (soil management, fertilization, liming, etc.), basis of a sustainable wine production on fragile soils.

Influence of grapevine rootstock/scion combination on rhizosphere and root endophytic microbiomes

Soil is a reservoir of microorganisms playing important roles in biogeochemical cycles and interacting with plants whether in the rhizosphere or in the root endosphere. The composition of the microbial communities thus impacts the plant health. Rhizodeposits (such as sugar, organic and amino acids, secondary metabolites, dead root cells …) are released by the roots and influence the communities of rhizospheric microorganisms, acting as signaling compounds or carbon sources for microbes. The composition of root exudates varies depending on several factors including genotypes. As most of the cultivated grapevines worldwide are grafted plants, the aim of this study was to explore the influence of rootstock and scion genotypes on the microbial communities of the rhizosphere and the root endosphere. The work was conducted in the GreffAdapt plot (55 rootstocks x 5 scions), in which the 275 combinations have been planted into 3 blocks designed according to the soil resistivity. Samples of roots and rhizosphere of 10 scion x rootstock combinations were first collected in May among the blocks 2 and 3. The quantities of bacteria, fungi and archaea have been assessed in the rhizosphere by quantitative PCR, and by cultivable methods for bacteria and fungi. The communities of bacteria, fungi and arbuscular mycorrhizal fungi (AMF) was analyzed by Illumina sequencing of 16S rRNA gene, ITS and 28S rRNA gene, respectively. The level of mycorrhization was also evaluated using black ink coloration of newly formed roots harvested in October. The level of bacteria, fungi and archaea was dependent on rootstock and scion genotypes. A block effect was observed, suggesting that the soil characteristics strongly influenced the microorganisms from the rhizosphere and root endosphere. High-throughput sequencing of the different target genes showed different communities of bacteria, fungi and AMF associated with the scion x rootstock combinations. Finally, all the combinations were naturally mycorrhized. The root mycorrhization intensity was influenced by the rootstock genotype, but not by the scion one. Altogether, these results suggest that both rootstock and scion genotypes influence the rhizosphere and root endophytic microbiomes. It would be interesting to analyze the biochemical composition of the rhizodeposition of these genotypes for a better understanding of the processes involved in the modulation of these microbiomes. Moreover, crossing our data with the plant agronomic characteristics could provide insights into their roles on plant fitness.

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.