West Jason B, Ehleringer James R, Cerling Thure E
Department of Biology, University of Utah, 257 South 1400 East, Salt Lake City, Utah 84112, USA.
J Agric Food Chem. 2007 Aug 22;55(17):7075-83. doi: 10.1021/jf071211r. Epub 2007 Jul 21.
Wine hydrogen and oxygen stable isotopes record the climatic conditions experienced by the grape vine and the isotopic composition of the vine's source water during berry development. As such, stable isotopes have been explored extensively for use in detecting wine adulteration or for independently verifying claims of origin. We present the results of a study designed to evaluate the relationships between wine water delta18O and spatial climate and precipitation delta18O patterns across the winegrape-growing regions of Washington, Oregon, and California. Retail wines produced from typically small vineyards across these regions were obtained from the 2002 vintage, and the delta18O of wine water was analyzed using a CO2 equilibration method. Significant correlations were observed between the measured wine water delta18O from 2002 and the long-term average precipitation delta18O and late season 2002 climate, based on a spatial join with continuous geographic information system (GIS) maps of these drivers. We then developed a regression model that was implemented spatially in a GIS. The GIS model is the first of its kind and allows spatially explicit predictions of wine delta18O across the region. Because high spatial resolution monthly climate layers are now available for many years, wine delta18O could be modeled for previous years. We therefore tested the model by executing it for specific years and comparing the model predictions with previously published results for wine delta18O from seven vintages from Napa and Livermore Valleys, California. With the exception of one year, an anomaly potentially related to the effects of El Niño on precipitation isotopic composition, the model predicted well the wine delta18O for both locations for all vintages and generally reflected the consistent enrichment of wine from Napa relative to Livermore. Our results suggest that wine water delta18O records both source water delta18O and climate during the late stages of winegrape ripening and that GIS models of wine water delta18O are useful tools for independently verifying claims of regional origin and vintage.
葡萄酒中的氢和氧稳定同位素记录了葡萄藤在浆果发育过程中所经历的气候条件以及葡萄藤源水的同位素组成。因此,稳定同位素已被广泛研究用于检测葡萄酒掺假或独立验证产地声明。我们展示了一项研究的结果,该研究旨在评估华盛顿州、俄勒冈州和加利福尼亚州葡萄酒产区葡萄酒水的δ18O与空间气候以及降水δ18O模式之间的关系。从这些地区典型的小葡萄园生产的2002年份零售葡萄酒被采集,葡萄酒水的δ18O使用二氧化碳平衡法进行分析。基于与这些驱动因素的连续地理信息系统(GIS)地图的空间连接,观察到2002年测量的葡萄酒水δ18O与长期平均降水δ18O以及2002年后期气候之间存在显著相关性。然后我们开发了一个在GIS中进行空间实施的回归模型。该GIS模型是同类中的首个模型,能够对整个地区的葡萄酒δ18O进行空间明确的预测。由于现在有多年的高空间分辨率月度气候层数据,因此可以对往年的葡萄酒δ18O进行建模。我们通过针对特定年份运行该模型并将模型预测结果与之前发表的加利福尼亚州纳帕谷和利弗莫尔谷七个年份葡萄酒δ18O的结果进行比较来测试该模型。除了一年可能与厄尔尼诺对降水同位素组成的影响有关的异常情况外,该模型对所有年份两个地点的葡萄酒δ18O都预测良好,并且总体上反映了纳帕葡萄酒相对于利弗莫尔葡萄酒的持续富集情况。我们的结果表明,葡萄酒水δ18O记录了葡萄成熟后期的源水δ18O和气候,并且葡萄酒水δ18O的GIS模型是独立验证地区产地和年份声明的有用工具。