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…

Metabolomic discrimination of grapevine water status for Chardonnay and Pinot noir

Water status impact in viticulture has been widely explored, as it strongly affects grapevine physiology and grape chemical composition. It is considered as a key component of vitivinicultural terroir. Most of the studies concerning grapevine water status have focused on either physiological traits, or berry compounds, or traits involved in wine quality. Here, the response of grapevine to water availability during the ripening period is assessed through non-targeted metabolomics analysis of grape berries by ultra-high resolution mass spectrometry. The grapevine water status has been assessed during 2 consecutive years (2019 & 2020), through carbon isotope discrimination on juices from berries collected at maturity (21.5 brix approx.) for 2 Vitis vinifera cv. Pinot noir (PN) and Chardonnay (CH). A total of 220 grape juices were collected from 5 countries worldwide (Italy; Argentina; France; Germany; Portugal). Measured δ13C (‰) varied from -28.73 to -22.6 for PN, and from -28.79 to -21.67 for CH. These results also clearly revealed higher water stress for the 2020 vintage. The same grape juices have been analysed by Fourier Transform Ion Cyclotron Resonance Mass Spectrometry (FT-ICR-MS) and Liquid Chromatography coupled to Mass Spectrometry (LC-qTOF-MS), leading to the detection of up to 4500 CHONS containing elemental compositions, and thus likely tens of thousands of individual compounds, which include fatty acids, organic acids, peptides, phenolics, also with high levels of glycosylation. Multivariate statistical analysis revealed that up to 160 elemental compositions, covering the whole range of detected masses (100 –1000 m/z), were significantly correlated to the observed gradients of water status. Examples of chemical markers, which are representative of these complex fingerprints, include various derivatives of the known abscisic acid (ABA), such as phaesic acid or abscisic acid glucose ester, which are significantly correlated with higher water stress, regardless of the variety. Cultivar-specific behaviours could also be identified from these fingerprints. Our results provide an unprecedented representation of the metabolic diversity, which is involved in the water status regulation at the grape level, and which could contribute to a better knowledge of the grapevine mitigation strategy in a climate change context.

The interplay between grape ripening and weather anomalies – A modeling exercise

Current climate change is increasing inter- and intra-annual variability in atmospheric conditions leading to grapevine phenological shifts as well altered grape ripening and composition at ripeness. This study aims to (i) detect weather anomalies within a long-term time series, (ii) model grape ripening revealing altered traits in time to target specific ripeness thresholds for four Vitis vinifera cultivars, and (iii) establish empirical relationships between ripening and weather anomalies with forecasting purposes. The Day of the Year (DOY) to reach specific grape ripeness targets was determined from time series of sugar concentrations, total acidity and pH collected from a private company in the period 2009-2021 in North-Eastern Italy. Non-linear models for the DOY to reach the specified ripeness thresholds were assessed for model efficiency (EF) and error of prediction (RMSE) in four grapevine cultivars (Merlot, Cabernet Sauvignon, Glera and Garganega). For each vintage and cultivar, advances or delays in DOY to target specified ripeness thresholds were assessed with respect to the average ripening dynamics. Long-term meteorological series monitored at ground weather station by means of hourly air temperature and rainfall data were analyzed. Climate statistics were obtained and for each time period (month, bimester, quarter and year) weather anomalies were identified. A linear regression analysis was performed to assess a possible correlation that may exist between ripening and weather anomalies. For each cultivar, ripeness advances or delays expressed in number of days to target the specific ripening threshold were assessed in relation to registered weather anomalies and the specific reference time period in the vintage. Precipitation of the warmest month and spring quarter are key to understanding the effect of climate change on sugar ripeness. Minimum temperatures of May-June bimester and maximum temperatures of spring quarter best correlate with altered total acidity evolution and pH increment during the ripening process, respectively.

Assessment of climate change impacts on water needs and growing cycle on grapevine in three DOs of NE Spain

This study assessed the suitability of grapevine growing in three DOs (Empordà, Pla de Bages and Penedès) of Catalonia (NE Spain) over the 21st century. For this purpose, an estimation of water needs and agroclimatic and phenological indicators was made. Climate change impacts were estimated at 1 km pixel resolution using temperature and precipitation projections from several general circulation models (GCM) and two climate change scenarios: RCP 4.5 (stabilization scenario) and RCP 8.5 (worst-case scenario). Potential crop evapotranspiration (following FAO procedure) and a daily water balance considering soil water holding capacity were used to estimate actual evapotranspiration of vines and, finally, water needs. Dynamics would be similar in the three DOs studied although the magnitude of impact differs. Water needs would be 2 and 3 times greater (ranging from 0 to more than 1500 m3/ha) than current water needs at both climate change scenarios. Moreover, blooming date would advance from 3 to 6 weeks, harvest date from 1 to 2.5 months, resulting in growing cycles from 10 to 80 days shorter. It should also be noted that frost risk would decrease from 6 to 76%, the number of days with temperatures above 30ºC during ripening would rise from 48 to 500% and tropical nights (minimum temperature >20ºC) at ripening would increase from 28 to 150%, depending on the scenario and the DOs. The impacts of climate change in the three DOs could result in significant limitations for grapevine cultivation and wine production if adaptive strategies are not applied. This result could serve as a basis for the design of specific and particular adaptation strategies to improve and maintain vineyards in the DOs studied and could be extrapolated to similar DOs and regions.

VineyardFACE: Investigation of a moderate (+20%) increase of ambient CO2 level on berry ripening dynamics and fruit composition

Climate change and rising atmospheric carbon dioxide concentration is a concern for agriculture, including viticulture. Studies on elevated carbon dioxide have already been on grapevines, mainly taking place in greenhouses using potted plants or using field grown vines under higher CO2 enrichment, i.e. >650 ppm. The VineyardFACE, located at Hochschule Geisenheim University, is an open field Free Air CO2 Enrichment (FACE) experimental set-up designed to study the effects of elevated carbon dioxide using field grown vines (Vitis vinifera L. cvs. Riesling and Cabernet Sauvignon). As the carbon dioxide fumigation started in 2014, the long term effects of elevated carbon dioxide treatment can be investigated on berry ripening parameters and fruit metabolic composition.
The present study aims to investigate the effect on fruit composition under a moderate increase (+20%; eCO2) of carbon dioxide concentration, as predicted for 2050 on both Riesling and Cabernet Sauvignon. Berry composition was determined for primary (sugars, organic acids, amino acids) and secondary metabolites (anthocyanins). Special focus was given on monitoring of berry diameter and ripening rates throughout three growing seasons. Compared to previous results of the early adaptative phase of the vines [1], our results show little effect of eCO2 treatment on primary metabolites composition in berries. However, total anthocyanins concentration in berry skin was lower for eCO2 treatment in 2020, although the ratio between anthocyanins derivatives did not differ.
[1] Wohlfahrt Y., Tittmann S., Schmidt D., Rauhut D., Honermeier B., Stoll M. (2020) The effect of elevated CO2 on berry development and bunch structure of Vitis vinifera L. cvs. Riesling and Cabernet Sauvignon. Applied Science Basel 10: 2486

Making sense of available information for climate change adaptation and building resilience into wine production systems across the world

Effects of climate change on viticulture systems and winemaking processes are being felt across the world. The IPCC 6thAssessment Report concluded widespread and rapid changes have occurred, the scale of recent changes being unprecedented over many centuries to many thousands of years. These changes will continue under all emission scenarios considered, including increases in frequency and intensity of hot extremes, heatwaves, heavy precipitation and droughts. Wine companies need tools and models allowing to peer into the future and identify the moment for intervention and measures for mitigation and/or avoidance. Previously, we presented conceptual guidelines for a 5-stage framework for defining adaptation strategies for wine businesses. That framework allows for direct comparison of different solutions to mitigate perceived climate change risks. Recent global climatic evolution and multiple reports of severe events since then (smoke taint, heatwave and droughts, frost, hail and floods, rising sea levels) imply urgency in providing effective tools to tackle the multiple perceived risks. A coordinated drive towards a higher level of resilience is therefore required. Recent publications such as the Australian Wine Future Climate Atlas and results from projects such as H2020 MED-GOLD inform on expected climate change impacts to the wine sector, foreseeing the climate to expect at regional and vineyard scale in coming decades. We present examples of practical application of the Climate Change Adaptation Framework (CCAF) to impacts affecting wine production in two wine regions: Barossa (Australia) and Douro (Portugal). We demonstrate feasibility of the framework for climate adaptation from available data and tools to estimate historical climate-induced profitability loss, to project it in the future and to identify critical moments when disruptions may occur if timely measures are not implemented. Finally, we discuss adaptation measures and respective timeframes for successful mitigation of disruptive risk while enhancing resilience of wine systems.