GiESCO 2019 banner
IVES 9 IVES Conference Series 9 GiESCO 9 GiESCO 2019 9 Consistency of the hydraulic traits and stomatal responses in grapevines with contrasting hydraulic vulnerability

Consistency of the hydraulic traits and stomatal responses in grapevines with contrasting hydraulic vulnerability

Abstract

Context and purpose of the study ‐ Different from wild species in arid and semiarid conditions, cultivated species are very sensitive to drought and, beyond some stress thresholds, food production is not possible. It is therefore important to gain further knowledge on the responses of plant species of agricultural importance to realistic water shortage extents, and their consistencies. A valuable model for water stress studies has been the grapevine (Vitis vinifera L.), a species with a high variability in their stomatal sensitivity to water stress. In contrast to usual agricultural practices, grapevines for oenological purposes are grown under controlled water stress conditions.

Material and methods ‐ In the abovementioned context, we aimed to study the physiological responses to a progressive, not severe (Ѱpd > ‐1MPa), water deficit in the grapevine varieties Syrah and Carménère, in two consecutive season using different sites each year, and with different row orientation. We assessed a) the relationship between the water status of plants and the stomatal responses to water availability; b) the hydraulic traits derived from Ѱ isotherms (pressure vs volume curves); c) the impact of the water stress on the hydraulic traits derived from the pressure vs volume curves and on photosynthetic responses; d) the stomatal sensitivity to ABA (only on one of the study sites) and e) their stem hydraulic vulnerability in relation to xylem characteristics.

Results – Acording to the Ѱleaf/Ѱpd relationship (), and contrary to various previous reports, we found Syrah to be an isohydric grapevine variety, while Carménère, an emblematic variety cultivated in Chile, behaved as anisohydric. Syrah resulted to be more variable in terms of , gs50 and gs12 (the pd upon which stomata is reduced down to a 50% and 12%), 0 and tlp (the at full turgor and the  at turgor loss point), likely associated to the higher genetic variability of Syrah compared to that of Carménère. Also, Carménère, the anisohydric variety was capable of osmotic adjustment and was more sensitive to ABA at the stomatal level, two traits typical of anisohydric species, contrary to that observed in Syrah. Even though the capacity to maintain stomata open, theoretically, would imply a lower energy load into the photosynthetic systems, both varieties reduced their photosynthetic capacity up to a similar extent upon drought. Finally, Syrah, despite having wider xylem vessels than Carménère, is less vulnerable to cavitation, and had a lower hydraulic safety margin, typical of isohydric species. We will discuss our results in terms of the genetic variability of the varieties regarding the consistency of their hydraulic responses, the importance of the environment, the degree of isohydry in relation to stomatal responses to critical thresholds as well as drought resistance, and the implications for photosynthesis in the long term. 

DOI:

Publication date: June 19, 2020

Issue: GiESCO 2019

Type: Article

Authors

Luis VILLALOBOS‐GONZÁLEZ (1), Constanza QUINTANA (1), Dayna DONAIRE (1), Mariana MUÑOZ‐ ARAYA (1), Nicolás FRANCK, Claudio PASTENES (1)

(1) Universidad de Chile, Facultad de Ciencias Agronómicas.

Contact the author

Keywords

ABA sensitivity, anisohydry, drought resistance, grapevine, stomatal conductance

Tags

GiESCO 2019 | IVES Conference Series

Citation

Related articles…

Rootstock differences in soil-water uptake during drying-wetting cycles imaged with 3d electrical resistivity tomography

Limited knowledge has been acquired on grapevine roots and rhizosphere processes because of harder access when compared to aerial parts. There is need for new methods to study root behavior in undisturbed field conditions, and relate these effects on canopy and yield. The aim of this multidisciplinary study was to image and quantify spatial-temporal differences in soil-water uptake by genetically different rootstocks and to assess the response of the canopy during drought and rewetting.

PHENOTYPIC DIVERSITY AND BIO-PROTECTION CAPABILITY OF METSCHNIKOWIA SP. IN OENOLOGY

Nowadays, the trend is to reduce the use of chemical inputs in the food sector, including in oenology. One of the inputs widely used in the wine making process are sulfites, for its several properties: antimicrobial and antioxidiant. This use isn’t without consequences on consumer’s health and environment, it can lead for example to allergic reactions and pollution. To limit the addition of chemical inputs, microbial alternatives are used. It consists to inoculate in grape must, a micro-organism able to inhibit the growth of the negative indigenous flora during the phase before the fermentation and to guarantee the sensory qualities of wines.

Modélisation du régime thermique des sols de vignoble du Val de Loire : relations avec des variables utilisables pour la caractérisation des terroirs

Temperature has a decisive influence on the growth and development of plants (Carbonneau et al., 1992). In particular, in the case of the vine, the temperature is an omnipresent variable in the climatic indices (Huglin, 1986). For reasons of convenience, these indices use the temperature of the air measured under shelter in a meteorological station, making the implicit hypothesis of a concordance between this temperature and that of the sites of perception of the thermal stimulus by the plant. However, development may be more dependent on soil temperature than air temperature (Kliewer, 1975). Morlat (1989) thus verified that the variability in the precocity of the vine, positively correlated with the quality of the harvest and of the wine in the Loire Valley, was mainly explained by differences in temperature of the root zones.

Développement de l’appareil végétatif et maturation du raisin sur quatre sols de Pomerol en 1995

The Pomerol vineyard, located 35 km east of Bordeaux, covers around 800 ha on the left bank of the Isle. There is a system of fluvial terraces with more or less coarse gravel and pebble spreading, resting on a Tertiary substratum ranging from the Middle to Upper Eocene to the Lower Oligocene (Dubreuilh, 1993). This interweaving of terraces of varying thickness results in a brutal superposition of differentiated materials which give rise to various types of soil. Several site studies in this sector of the Libounais show significant morphological and analytical differences from one point to another (Guilloux et al ., 1978; Duteau, 1982; Van Leeuwen et al.., 1989). The distribution of the soils of the Pomerol vineyard was studied and resulted in a cartography at 1/25000th (Merouge, 1995).