Terroir 2004 banner
IVES 9 IVES Conference Series 9 Phenology and bioclimate of grapevine varieties in the tropical region of the São Francisco Valley, Brazil

Phenology and bioclimate of grapevine varieties in the tropical region of the São Francisco Valley, Brazil

Abstract

[English version below]

La région de la Vallée du São Francisco, situe à 9º S, est en train d’augmenter la production des vins fins les dernières années. La région présente climat du type tropical semi-aride (climat viticole à variabilité intra-annuelle selon le Système CCM Géoviticole : “très chaud, à nuits chaudes et à sécheresse forte à sub-humide” en fonction de la période de l’année dans laquelle le raisin est produit). La recherche objective la caractérisation de la phénologie et de la bioclimatologie des raisins de cuve dans la région. Ont été évalues 4 cépages avec différents niveaux de précocité – Syrah, Cabernet Sauvignon, Muscat Canelli et Schönburger, greffés sur IAC 572, vigne en premier cycle productif conduite en système pergola. Ont été évalués les stades phénologiques suivants selon le système d’Eichhorn & Lorenz : débourrement (B) – stade 05, floraison (F) – stade 23 et véraison (V) – stade 35. La date de récolte (H) corresponde à la récolte commerciale des raisins. La durée des sous-périodes phénologiques B-F, F-V, V-H et B-H a été calculée. Sur chacun des sous-périodes, ont été calculés 16 indices climatiques thermiques et hydriques. Les résultats de la Vallée du São Francisco ont été comparés avec les mêmes cépages d’une région de climat tempérée – la Serra Gaúcha (climat “tempéré chaud, à nuits tempérées, humide” selon le Système CCM Géoviticole), située à 29º S. Les résultats ont montré que la durée de la période B-H a été de 124, 123, 116 et 104 jours pour la Syrah, Cabernet Sauvignon, Muscat Canelli et Schönburger, tandis que dans la Serra Gaúcha, la durée a été de 158, 160, 160 et 138 jours, respectivement. Pour les caractéristiques bioclimatiques, dans la Vallée du São Francisco les températures moyennes de l’air de la période B-H ont varié entre 25,4 à 28,1 ºC, tandis que dans la Serra Gaúcha les températures ont varié entre 15,8 et 21,8 ºC. L’évapotranspiration potentielle, même si elle a présenté des moyennes journalières plus élevées dans la Vallée, ont été similaires pour le total dans la période B-H entre les 2 régions. Le rayonnement solaire global de la période B-H dans la Vallée du São Francisco a été inférieur si comparé avec la Serra Gaúcha. Ce résultat est lié surtout à la latitude (photopériode) et à la durée plus courte de la période B-H en condition tropicale. Le travail présente les indices bioclimatiques par cépage et sous-période, en comparant la région de baisse avec la région de moyenne latitude. On a conclu que le cycle végétatif de la vigne (B-H) est significativement plus court dans la Vallée du São Francisco (durée moyenne, pour les 4 cépages évalués, 37 jours inférieure que dans la Serra Gaúcha). Tel comportement est dû essentiellement à un raccourcissement de la période B-F (29 jours plus court en moyenne). On observe que le comportement phénologique de la vigne dans la Vallée du São Francisco, distinct par rapport à une région de climat tempérée, peut être expliqué surtout par le bioclimat particulier trouvé en zone tropicale.

The region of the São Francisco Valley, located at 9° S, has been increasing the production of fine wines during the last years. The region has a tropical semi-arid climate (viticultural climate with intra-annual variability according to the Geoviticultural CCM System : “very warm, with warm nights, very dry to sub-humid” depending on the period of the year in which the grapes are produced). The research aims at characterizing the phenology and bioclimatology of the region’s wine grapes. Four cultivars with different levels of precocity were evaluated – Syrah, Cabernet Sauvignon, Muscat Canelli and Schönburger, grafted on IAC 572, a vineyard in its first productive cycle, using the pergola as training system. The phenological stages bud burst (B) – stage 05, flowering (F) – stage 23 and veraison (V) – stage 35 were evaluated according to the system of Eichhorn & Lorenz. The date of the harvest (H) corresponds to the commercial grape harvest. The duration of the phenological subperiods B-F, F-V V-H and B-H has been calculated. For each subperiod 16 thermal and hydric climatic indices have been calculated. The results of the São Francisco Valley have been compared with the same cultivars from a temperate climate region – the Serra Gaúcha (“temperate warm, with temperate nights, humid viticulture climate” according to the Geoviticultural CCM System), located 29°S. The results have shown that the duration of the period B-H has been 124, 123, 116 and 104 days for Syrah, Cabernet Sauvignon, Muscat Canelli and Schönburger, while in the Serra Gaúcha the duration has been 158, 160, 160 and 138 days, respectively. As for the bioclimatic characteristics, the mean air temperature in the São Francisco Valley in the period B-H have varied from 25,4 to 28,1ºC, whereas in the Serra Gaúcha the temperatures have oscillated between 15,8 and 21,8ºC. The potential evapotranspiration, even when showing higher mean day values in the Valley, was similar in both regions during the whole period B-H. The global solar radiation for the period B-H in the São Francisco Valley was lower when compared with the Serra Gaúcha. This result is related especially to the latitude (photoperiod) and the shorter duration of the B-H period under tropical conditions. The study presents the bioclimatic indices by cultivar and subperiod, comparing the region of low with that one of mean latitude. It has been concluded that the vegetative cycle of the grapevine (B-H) is significantly shorter in the the São Francisco Valley (mean duration, for the 4 evaluated cultivars, 37 days less than in the Serra Gaúcha). Such behavior is a consequence, essentially, of a shortening of the period B-F (29 days shorter in the average). It can be stated that the phenological behavior of the grapevine in the São Francisco Valley, although distinct from a temperate climate region, can be understood above all by the particular bioclimate found in the tropical zone.

 

DOI:

Publication date: January 12, 2022

Issue: Terroir 2004

Type: Article

Authors

U. A. Camargo (1), J.Tonietto (1), F. Mandelli (1) and F.M. de Amorim (2)

U. A. Camargo (1)(1) Embrapa – National Center for Grape and Wine Research – Cnpuv, Rua Livramento, 515; 9570000-000 – Bento Gonçalves, Brazil
(2) Grant from CNPq/FINEP

Contact the author

Keywords

Wine grapes, tropical viticulture

Tags

IVES Conference Series | Terroir 2004

Citation

Related articles…

Analysis of Cabernet Sauvignon and Aglianico winegrape (V. vinifera L.) responses to different pedo-climatic environments in southern Italy

Water deficit is one of the most important effects of climate change able to affect agricultural sectors. In general, it determines a reduction in biomass production, and for some plants, as in the case of grapevine, it can endorse fruit quality. The monitoring and management of plant water stress in the vineyard

Genotypic variability in root architectural traits and putative implications for water uptake in grafted grapevine

Root system architecture (RSA) is important for soil exploration and edaphic resources acquisition by the plant, and thus contributes largely to its productivity and adaptation to environmental stresses, particularly soil water deficit. In grafted grapevine, while the degree of drought tolerance induced by the rootstock has been well documented in the vineyard, information about the underlying physiological processes, particularly at the root level, is scarce, due to the inherent difficulties in observing large root systems in situ. The objectives of this study were to determine genetic differences in the root architectural traits and their relationships to water uptake in two Vitis rootstocks genotypes (RGM, 140Ru) differing in their adaptation to drought. Young rootstocks grafted upon the Riesling variety were transplanted into cylindrical tubes and in 2D rhizotrons under two conditions, well watered and moderate water stress. Root traits were analyzed by digital imaging and the amount of transpired water was measured gravimetrically twice a week. Root phenotyping after 30 days reveal substantial variation in RSA traits between genotypes despite similar total root mass; the drought-tolerant 140Ru showed higher root length density in the deep layer, while the drought-sensitive RGM was characterised by shallow-angled root system development with more basal roots and a larger proportion of fine roots in the upper half of the tube. Water deficit affected canopy size and shoot mass to a greater extent than root development and architectural-related traits for both 140Ru and RGM, suggesting vertical distribution of roots was controlled by genotype rather than plasticity to soil water regime. The deeper root system of 140Ru as compared to RGM correlated with greater daily water uptake and sustained stomata opening under water-limited conditions but had little effect on above-ground growth. Our results highlight that grapevine rootstocks have constitutively distinct RSA phenotypes and that, in the context of climate change, those that develop an extensive root network at depth may provide a desirable advantage to the plant in coping with reduced water resources.

A spatial explicit inventory of EU wine protected designation of origin to support decision making in a changing climate

Winemaking areas recognized as protected designations of origin (PDOs) shape important economic, environmental and cultural values that are tied to closely defined geographic locations. To preserve wine products and wine-growing practices adopted in different PDOs these areas are strictly regulated by legal specifications. However, quality viticulture is increasingly under pressure from climate change, which is altering the local conditions of many winegrowing areas. Therefore, maintaining traditional wine products will require the adoption of tailored adaptation strategies, including possible changes in the legal regulation of protected wines. To this end, it is necessary to have a comprehensive knowledge on PDOs including their extension, products and allowed practices. While there have been efforts to build databases that summarize the characteristics for individual wine PDO areas and to quantify the related effects of climate change, much information is still included only in the official documentation of the EU geographical indication register and has never been collected in a comprehensive manner. With this study we aim at filling this gap by building a spatial inventory of European wine PDOs that supports decision making in viticulture in the context of climate change. To map and characterize European wine PDOs, we analysed their legal documents and extracted relevant information useful for climate change adaptation. The output consists of a comprehensive geographical dataset that identifies the boundaries of all 1200 European wine PDOs at unprecedented spatial resolution and includes a set of legally binding regulations, such as authorized vine varieties, maximum yields and planting density. The inventory will allow researchers to analyse the impacts of climate change on European wine PDOs and support decision makers in developing tailored adaptation strategies. This includes, among others, the evaluation of new vineyard site selection, the expansion of cultivated varieties or the authorization of irrigation in vineyards.

Evolution of the amino acids content through grape ripening: Effect of foliar application of methyl jasmonate with or without urea

The parameters that determine the grape quality, and therefore the optimal harvest time, suffer variations during berry ripening, related to climate change, with the widely known problem of the gap between technological and phenolic maturities. However, there are few studies about its incidence on grape nitrogen composition. For this reason, the use of an elicitor, methyl jasmonate (MeJ), alone or with urea, is proposed as a tool to reduce climatic decoupling, allowing to establish the harvest time in order to achieve the optimum grape quality. The aim was to study the effect of MeJ and MeJ+Urea foliar applications on the evolution of Tempranillo amino acids content throughout the grape maturation. Three treatments were foliarly applied, at veraison and 7 days later: control (water), MeJ (10 mM) and MeJ+Urea (10 mM+6 kg N/ha). Grape samples were taken at five stages of maturation: day before the first and second applications, 15 days after the second application (pre-harvest), harvest day, and 15 days after harvest (post-harvest). The amino acids analysis of the samples was carried out by HPLC. Results showed that the evolution of amino acids was similar regardless of the treatment; however, foliar applications influenced the nitrogen compounds content, i.e., there was no qualitative effect but quantitative one. Most of the amino acids reached their maximum concentration in pre-harvest, being higher in grapes from the treatments than in the control. In general, no differences in grape amino acids content were observed between MeJ and MeJ+Urea treatments. Foliar applications with MeJ and MeJ+Urea enhanced the grape amino acids content, without affecting their profile, helping to optimize their quality and allowing to establish a more complete grape ripening standard. Therefore, MeJ and MeJ+Urea foliar applications can be a simple agronomic practice, which has shown promising results in order to enhance the grape quality.

Effects of organic mulches on the soil environment and yield of grapevine

Farming management practices aiming at conserving soil moisture have been developed in arid and semiarid-areas facing water scarcity problems. Organic mulching is an effective method to manipulate the crop-growing microclimate increasing crop yield by controlling soil temperature, and retaining soil moisture by reducing soil evaporation. In this sense, the effectiveness of different organic mulching materials (straw mulch and grapevine pruning debris) applied within the row of a vineyard was evaluated on the soil and on the vine in a Tempranillo vineyard located in La Rioja (Spain). Organic mulches were compared with a traditional bare soil management technique (based on the use of herbicides to avoid weed incidence). Mulching coverages favourably influenced the soil water retention throughout all the grapevine vegetative cycle. However, the soil-moisture variation was not the same under different mulching materials, being the straw mulch (SM) the one that retained more water in comparison with grapevine pruning debris (GPD) based-cover. The changes of soil moisture in the upper surface layer (0–10 cm) were highly dynamic, probably due to water vapour fluxes across the soil-atmospheric interface. However, both, SM and GPD reduced these fluctuations as compared with bare soils. A similar trend occurred with soil temperature. Both organic mulches altered soil temperature in comparison with bare soil by reducing soil temperature in summer and raising it in winter. Moreover, the same buffering effect for the temperature on the covered soil also remains in the deeper layers. To conclude, we could see that organic mulching had a positive impact on soil-moisture storage and soil temperature and the extent of this effect depends on the type of mulching materials. These changes led to higher rates of photosynthesis and stomatal conductivity compared to bare soils, also favouring crop growth and grape yields.