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…

Impact on leaf morphology of Vitis vinifera L. cvs Riesling and Cabernet Sauvignon under Free Air Carbon dioxide Enrichment (FACE)

Atmospheric carbon dioxide (CO2) concentration has continuously increased since pre-industrial times from 280 ppm in 1750, and is predicted to exceed 700 ppm by the end of 21st century. For most of C3 plant species elevated CO2 (eCO2) improve photosynthetic apparatus results in an increased plant biomass production. To investigate the effects of eCO2 on morphological leaf characteristics the two Vitis vinifera L. cultivars, Riesling and Cabernet Sauvignon, grown in the Geisenheim VineyardFACE (Free Air Carbon dioxide Enrichment) system were used. The FACE site is located at Geisenheim University (49° 59′ N, 7° 57′ E, 94 m above sea level), Germany and was implemented in 2014 comparing future atmospheric CO2-concentrations (eCO2, predicted for the mid-21st century) with current ambient CO2-conditions (aCO2). Experiments were conducted under rain-fed conditions for two consecutive years (2015 and 2016). Six leaves per repetition of the CO2 treatment were sampled in the field and immediately fixed in a FAA solution (ethanol, H2O, formaldehyde and glacial acetic acid). After 24 h leaf samples were transferred and stored in an ethanol solution. Subsequently, leaf tissue was dehydrated using ethanol series and embedded in paraffin. By using a rotary microtomesections of 5 µm were prepared and fixed on microscopic slides. Subsequent the samples were stained using consecutive staining and washing solutions. Afterwards pictures of the leaf cross-sections were taken using a light microscope and consecutive measurements were conducted with an open source image software. Differences found in leaf cross-sections of the two CO2 treatments were detected for the palisade parenchyma. Leaf thickness, upper and lower epidermis and spongy parenchyma remained less affected under eCO2 conditions. The observed results within grapevine leaf tissues can provide first insights to seasonal adaptation strategies of grapevines under future elevated CO2 concentrations.

Analysis of some environmental factors and cultural practices that affect the production and quality of the Manto Negro, Callet and Prensal Blanc varieties

45 non irrigated vineyards distributed in the DO (Denomination) Pla i Llevant de Mallorca and the DO Binissalem Mallorca were used to investigate the characteristics of production and quality and their relationships certain environmental factors and cultural practices. The grape varieties investigated are autochthonous to the island of Mallorca, Manto Negro and Callet as red and Prensal Blanc as white. All plants were measured for four consecutive years in the main production and quality parameters. Among the environmental factors, the type of soil has been studied, more specifically its water retention capacity, the planting density, the age of the vineyard and the level of viral infection. The presence or absence of virus seems to have no effect on any component studied in the varieties studied. For the white variety Prensal Blanc age is negatively correlated with production and the number of bunches, nevertheless it does not cause any effect on the required quality parameters. However, for the red varieties Callet and Manto Negro, the age of the plantation is the variable that best correlates with the quality parameters, therefore the old vines should be the object of preservation by the viticulturists and winemakers in order to guarantee its contribution to the quality of the wines made with these varieties.

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.

Anthocyanin profile is differentially affected by high temperature, elevated CO2 and water deficit in Tempranillo (Vitis vinifera L.) clones

Anthocyanin potential of grape berries is an important quality factor in wine production. Anthocyanin concentration and profile differ among varieties but it also depends on the environmental conditions, which are expected to be greatly modified by climate change in the future. These modifications may significantly modify the biochemical composition of berries at harvest, and thus wine typicity. Among the diverse approaches proposed to reduce the potential negative effects that climate change may have on grape quality, genetic diversity among clones can represent a source of potential candidates to select better adapted plant material for future climatic conditions. The effects of individual and combined factors associated to climate change (increase of temperature, rise of air CO2 concentration and water deficit) on the anthocyanin profile of different clones of Tempranillo that differ in the length of their reproductive cycle were studied. The aim was to highlight those clones more adapted to maintain specific Tempranillo typicity in the future. Fruit-bearing cuttings were grown in controlled conditions under two temperatures (ambient temperature versus ambient temperature + 4ºC), two CO2 levels (400 ppm versus 700 ppm) and two water regimes (well-watered versus water deficit), both in combination or independently, in order to simulate future climate change scenarios. Elevated temperature increased anthocyanin acylation, whereas elevated CO2 and water deficit favoured the accumulation of malvidin derivatives, as well as the acylation and tri-hydroxylation level of anthocyanins. Although the changes in anthocyanin profile observed followed a common pattern among clones, such impact of environmental conditions was especially noticeable in one of the most widely distributed Tempranillo clones, the accession RJ43.

Terroir analysis and its complexity

Terroir is not only a geographical site, but it is a more complex concept able to express the “collective knowledge of the interactions” between the environment and the vines mediated through human action and “providing distinctive characteristics” to the final product (OIV 2010). It is often treated and accepted as a “black box”, in which the relationships between wine and its origin have not been clearly explained. Nevertheless, it is well known that terroir expression is strongly dependent on the physical environment, and in particular on the interaction between soil-plant and atmosphere system, which influences the grapevine responses, grapes composition and wine quality. The Terroir studying and mapping are based on viticultural zoning procedures, obtained with different levels of know-how, at different spatial and temporal scales, empiricism and complexity in the description of involved bio-physical processes, and integrating or not the multidisciplinary nature of the terroir. The scientific understanding of the mechanisms ruling both the vineyard variability and the quality of grapes is one of the most important scientific focuses of terroir research. In fact, this know-how is crucial for supporting the analysis of climate change impacts on terroir resilience, identifying new promised lands for viticulture, and driving vineyard management toward a target oenological goal. In this contribution, an overview of the last findings in terroir studies and approaches will be shown with special attention to the terroir resilience analysis to climate change, facing the use and abuse of terroir concept and new technology able to support it and identifying the terroir zones.