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Development of tools to verify origin and varietal nature of wines

To investigate the ability of stable isotope measurements to determine the provenance of Australian wines.

Final Report
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Overview

  • Demonstrates that boron, oxygen and strontium isotope ratios can distinguish Australian wines from overseas wines, correctly classifying 97.3% of Australian samples (92.5% overall)
  • Shows lead isotope ratios are compromised by bentonite fining, informing which analytical parameters can be relied upon
  • Establishes baseline data linking Australian Crustal Elements (subsoil geology) to regional isotope signatures, supporting future work on regional origin verification and Geographical Indication integrity

Verifying the origin of wines by analysis relies on the use of parameters that not only reflect the geology and water source of the location where grapes are grown, but which are also not altered during winemaking. The project set out to identify analytical parameters based on isotope ratios to verify the geographic origin – or provenance – of Australian wines within the framework of the international packaged and bulk wine trade. Multi-dimensional statistical tools were employed, in particular Orthogonal Projection of Latent Structure-Discriminant Analysis (OPLS-DA) to analyse isotope ratios of boron, lithium, strontium and oxygen, which were determined using appropriate Inductively Coupled Plasma Mass Spectrometry (ICP-MS) methodology and Isotope Ratio Mass Spectrometry (IRMS). A discriminant model was developed using data from 292 Australian wines (from 16 production zones) and 94 international wines (from Europe, South America, Canada, New Zealand, South Africa and USA). The model had a successful classification rate of 97.3% for Australian wines, with a successful classification rate of 92.5% on average for all wine analysed. The main drivers of the model were isotopic ratios of boron, oxygen and strontium; however, some concentration data from selected trace elements including nickel, lithium and chrome was required to achieve these levels of discrimination. Identification of the region of origin of Australian wines, mostly through the impact of subsoil strata on strontium isotopes, was also achieved with a classification success rate of approximately 60%. The lower levels of successful classification for regions is strongly linked to the underlying similarity of geology that contributes to the subsoil composition of many Australian grapegrowing regions. This information will provide important baseline data for any future studies of analytical methods to determine regional origin of Australian wines. Several potentially confounding factors on these isotopic ratios and their ability to differentiate Australian from overseas wines were investigated: Vintage variation was measured using vertical series of three single-vineyard wines from very different regions across Australia over a period of ten years. This temporal variance was tested against that measured for all study samples and found to be

smaller for all isotopic parameters with the except of two lead isotope ratios. This allowed the majority of isotope ratios to be used. Grape variety variation was tested in ten cultivars, both red and white, grown in several locations of South Australia subjected to controlled micro-vinification. Differences in the isotope ratios of Li, O, and Sr differed by below 10% due to grape cultivar and were therefore useable. Neither vintage nor variety showed a significant negative effect on the use of the models to classify if a wine was of an Australian origin. Bottle source and type were considered to have potential to influence the boron isotopic ratios found in packaged wine. However, analysis demonstrated that the bottle did not make a significant contribution in comparison to the differences introduced by wine origin. Bentonite clay fining is a common winemaking practice which can introduce significant amounts of lead into wine. This fact makes the use of lead isotopic ratios unsuitable for classification of white wines. Analysis demonstrated that the lead isotopes were more useful at indicating the regional source of the bentonite used, an internationally traded commodity, than the wines origin. The success of this project in using combined isotopic ratios and statistical analysis to categorise a wine’s origin will allow the provenance of a wine that claims to be Australian to be analytically determined. While by its nature this technique is not suitable for rapid in-market applications, it will provide an important addition to technologies such as smart labelling and methods that compare direct retention samples of known wines. Significantly, unlike many other technologies used in authentication of wine, the use of isotopic ratios can link a wine’s provenance to the underlying physical attributes of its place of origin. This is important in cases where rather than being a direct forgery of an existing Australian product, a wine is simply making claims of Australian provenance. Such cases can expose the consumer to, at best, a disappointing quality outcome and at worst possible health impacts from the use of unapproved additive or ingredients, with additional obvious negative outcomes for the reputation of all Australian wines. While this work identified the overall potential of using a combined groups of isotopic ratios to provide information on wine origin, further work is needed to clarify nature of the links between the final values of these components in wine and the underlying sources in the geology, soil, water and air. Such an understanding will allow the much larger data sets compiled in environmental and geological studies to be used in the determination of the provenance of wine as well as other agricultural products.

Abstract

This project was successful in developing tools to identify the provenance of Australian wines in an international context, based on statistical analysis of selected isotope ratios naturally found in wine. The models developed were able to identify Australian wines when applied across different vintages and varieties of wines, demonstrating their robustness. The project also made important strides in understanding why some methods that have been previously promoted as tools for identifying provenance (particularly those involving analysis of lead isotope ratios and trace metal concentrations) have not been successful.

Objectives

To investigate the ability of stable isotope measurements to determine the provenance of Australian wines.

Background

Origin verification of wines relies on the use of parameters that not only reflect the geology and water source of the location where grapes are grown, but also parameters that are not altered during vinification. Building on a recently completed feasibility study (AWR 2.2.2 Feasibility study for origin verification of Australian wine), several elemental isotope ratios such as boron, lithium and lead will be measured to provide information in addition to the strontium isotope ratio, on the vineyard location of the grapes from which the wine was made.

To supplement this dataset of trace elements and their isotopes and to achieve true independence of multiple data sources, oxygen-18 will also be analysed as an indication of the vineyard water source. These parameters will be measured in Australian wines, and wines from North and South America, Europe, and mainland Asia and Africa.

Approach

To verify that chosen parameters are not affected by variety (as has been highlighted in several recent papers in the literature), laboratory-scale wines will be made to assess numerous varieties grown in the same soil across several different locations. In addition, the temporal variation of these parameters will be assessed through the analysis of several vertical series of wines made from single vineyards over the last ten years. This information will be combined with the continued survey of the parameters determined to be most robust over a five-year period, to provide a series of reliable analytical protocols and metrics for the determination of wine origin.

In the later years of the project, a review of chemical and genetic techniques for the determination of varietal origin of wine will be undertaken, with the aim of targeting appropriate tools for this aspect of wine authentication.

Sector benefits

This project will result in methods to analytically determine with a high degree of confidence, the origin of a wine, both variety and place.

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