Terroir 2014 banner
IVES 9 IVES Conference Series 9 Berry carbon (δ13C) and nitrogen (δ15N) isotopic ratio reflects within farm terroir diffferences

Berry carbon (δ13C) and nitrogen (δ15N) isotopic ratio reflects within farm terroir diffferences

Abstract

ÂThe natural abundance of carbon stable isotopes has been reported to be related to water availability in grapevines quite widely. In the case of nitrogen, the natural abundance of its stable isotopes is mainly affected by the nature of the source of nitrogen (organic vs. inorganic) used by the plant, though the bibliography available for grapevine is very scarce. The aim of this work was to evaluate the effect of terroir on carbon and nitrogen stable isotope natural abundance within a single grape growing farm. Three vineyards representative of three terroirs within a grape growing farm were selected. The mesoclimatic differences between them can be considered negligible, and crop management was in general terms the same. Therefore, the differences in plant behaviour should be majorly a consequence of soil characteristics (deep gravely vs. shallower loamy soil, cover crop vs. bare soil). During five consecutive seasons, plant vegetative growth and stem water potential (Ψs) were monitored throughout the growing season and, at harvest, yield and grape composition were determined including carbon (δ13C) and nitrogen (δ15N) isotopic ratios. Consistent differences for both δ13C and δ15N were found when the three terroirs were compared. On the one hand, δ13C reflected well the differences in water availability arising from either soil characteristics (deep gravelly vs. shallower loamy soil) and from the presence of a cover crop. On the other hand, δ15N was clearly higher in the gravelly soil area, possibly indicating nitrate leakage, since soil organic matter is known to have higher δ15N than inorganic fertilizers. The competition the cover crop exerted for N was reflected in berry nitrogen content but, on the contrary, did not affect δ15N.

DOI:

Publication date: July 31, 2020

Issue: Terroir 2014

Type: Article

Authors

Luis G. SANTESTEBAN, Carlos MIRANDA, Izaskun BARBARIN, José B. ROYO

Dpto. Prod. Agraria, Univ. P. Navarra, 31006 Pamplona, NA, Spain. 

Contact the author

Keywords

natural isotope abundance, water use efficiency, water status, nutrition, nitrogen sources, Vitis vinifera L.

Tags

IVES Conference Series | Terroir 2014

Citation

Related articles…

Crossed approaches to experimental economics and sensory analysis regarding noble rot sweet wines perception

Noble rot sweet wines are reputed wines, traditionally elaborated according to a singular vinification process involving the harvesting of overripe grapes under the action of the ascomycete fungus Botrytis cinerea.

Chemical and biochemical formation of polysulfides in synthetic and real wines using UHPLC-HRMS

ulfur compounds in wine have been studied for several years due to their impact on wine flavour, but the role of polysulfides is a recent topic. Polysulfides in wine are formed when two sulfhydryl groups oxidize, especially in presence of elemental sulfur or metal catalysts from field treatment residues (Ugliano et al. 2011). These compounds are odourless, but can degrade during storage and affect the wine quality. The mechanism of their formation is still largely unknown but different chemical and biochemical pathways have been suggested. Disulfides from cysteine (Cys) and glutathione (GSH) have been revealed in model wines (Kreitman et al. 2016) and more recently also higher polymerized forms in real wines (Van Leeuwen et al. 2020). Volatile varietal thiols like 3-mercaptohexanol (3MH) and 4-mercaptopentanone (4MMP) – flavour compounds with tropical or fruity notes – could undergo similar reactions, also with Cys and GSH, subsequently losing their flavour property (fate). Even more concerning is the possible release of H2S from polysulfides during storage, leading to undesired off-flavours (Sarrazin et al. 2010).

Do high temperature extremes impact berry tannin composition?

Flavonoids, including flavonols, anthocyanins, and tannins, are important contributors to grape and wine quality, and their biosynthesis is strongly influenced by bunch microclimate.

Rare earth elements distribution in grape berries

Rare Earth Elements (REEs) include 15 lanthanides, yttrium and scandium. Their occurrence in soil and plants seems to be closely tied to the geological composition of the underlying mother rock, to the physical and chemical properties of the soil and to the specific ability of the plant to take up and accumulate these microelements.

La zonazione della valle d’Illasi (Verona)

In the bottom of Val d’Illasi (Verona province), one of the major valleys which passes through the Lessini mountains, viticulture is widely extended. In the territory belonging to Illasi and Tregnago villages, which includes ca. 1100 ha of vineyards, devoted to produce Soave and Valpolicella DOC wines, an experimental survey was conducted on a network of twenty five reference vineyards.