Erico Albuquerque Santos , Luana Moreira Florisbal , Ross Stevenson , David Widory , Denilson Dortzbach , Bruna Saar de Almeida , Arcângelo Loss
{"title":"从岩石到瓶子:锶同位素(87Sr/86Sr)作为巴西南部<s:1> o Joaquim高原火山酒的来源指示","authors":"Erico Albuquerque Santos , Luana Moreira Florisbal , Ross Stevenson , David Widory , Denilson Dortzbach , Bruna Saar de Almeida , Arcângelo Loss","doi":"10.1016/j.catena.2024.108624","DOIUrl":null,"url":null,"abstract":"<div><div>Studies worldwide, particularly in Canada, Italy and Brazil, have demonstrated that the <sup>87</sup>Sr/<sup>86</sup>Sr ratio is a reliable indicator of the geographic origin of wines. We present here the first <sup>87</sup>Sr/<sup>86</sup>Sr isotope study for the <em>Wines of Altitude of Santa Catarina</em> geographical indication that was recently created in the state of Santa Catarina, southern Brazil. The goal of this study is to evaluate the forensic application of strontium isotope ratios as an indicator of provenance for the wines of São Joaquim, the main wine-growing region in the state of Santa Catarina, which produces wines from European grape varieties (<em>Vitis vinifera L.</em>) grown in soils formed by the weathering of volcanic rocks of the Serra Geral Group (Paraná Magmatic Province). The <sup>87</sup>Sr/<sup>86</sup>Sr of rocks, soils (bulk and labile fractions), vines (leaves and grapes) and wines (Sauvignon Blanc and Cabernet Sauvignon) from three wineries from São Joaquim were determined. Bedrock <sup>87</sup>Sr/<sup>86</sup>Sr ratios ranged from 0.705362 for the basaltic-andesitic rocks to 0.724819 for dacites, consistent with reported values for these types of rocks. We identified a strong correlation between the <sup>87</sup>Sr/<sup>86</sup>Sr ratios of the grapes and leaves, but in contrast to most previous studies there was no correlation between those of the soil (both bulk and labile fractions) and wine samples. This indicates that although the Sr isotopes in grapes and leaves behaved conservatively, the Sr isotopes in the soils may have been modified by vineyard agricultural practices, such as fertilization and liming. We thus recommend that soil sampling be done at depths >60 cm to avoid external addition of strontium. As the <sup>87</sup>Sr/<sup>86</sup>Sr ratios of commercial wines represent the average isotope ratio of a given vineyard, the isotope correlation between wines and the other samples may be challenging. Despite that, it was possible to distinguish the <sup>87</sup>Sr/<sup>86</sup>Sr ratios of the wines from São Joaquim, state of Santa Catarina, from the wines from Bento Gonçalves, state of Rio Grande do Sul. Even though the wines from both regions are made from grapes cultivated in the same geological unit, i.e., volcanic rocks from Serra Geral Group (Paraná Magmatic Province), the wines yield different Sr signatures.</div></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":"249 ","pages":"Article 108624"},"PeriodicalIF":5.7000,"publicationDate":"2025-02-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"From rock to bottle: strontium isotopes (87Sr/86Sr) as indicator of provenance for the volcanic wines of altitude from São Joaquim, southern Brazil\",\"authors\":\"Erico Albuquerque Santos , Luana Moreira Florisbal , Ross Stevenson , David Widory , Denilson Dortzbach , Bruna Saar de Almeida , Arcângelo Loss\",\"doi\":\"10.1016/j.catena.2024.108624\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Studies worldwide, particularly in Canada, Italy and Brazil, have demonstrated that the <sup>87</sup>Sr/<sup>86</sup>Sr ratio is a reliable indicator of the geographic origin of wines. We present here the first <sup>87</sup>Sr/<sup>86</sup>Sr isotope study for the <em>Wines of Altitude of Santa Catarina</em> geographical indication that was recently created in the state of Santa Catarina, southern Brazil. The goal of this study is to evaluate the forensic application of strontium isotope ratios as an indicator of provenance for the wines of São Joaquim, the main wine-growing region in the state of Santa Catarina, which produces wines from European grape varieties (<em>Vitis vinifera L.</em>) grown in soils formed by the weathering of volcanic rocks of the Serra Geral Group (Paraná Magmatic Province). The <sup>87</sup>Sr/<sup>86</sup>Sr of rocks, soils (bulk and labile fractions), vines (leaves and grapes) and wines (Sauvignon Blanc and Cabernet Sauvignon) from three wineries from São Joaquim were determined. Bedrock <sup>87</sup>Sr/<sup>86</sup>Sr ratios ranged from 0.705362 for the basaltic-andesitic rocks to 0.724819 for dacites, consistent with reported values for these types of rocks. We identified a strong correlation between the <sup>87</sup>Sr/<sup>86</sup>Sr ratios of the grapes and leaves, but in contrast to most previous studies there was no correlation between those of the soil (both bulk and labile fractions) and wine samples. This indicates that although the Sr isotopes in grapes and leaves behaved conservatively, the Sr isotopes in the soils may have been modified by vineyard agricultural practices, such as fertilization and liming. We thus recommend that soil sampling be done at depths >60 cm to avoid external addition of strontium. As the <sup>87</sup>Sr/<sup>86</sup>Sr ratios of commercial wines represent the average isotope ratio of a given vineyard, the isotope correlation between wines and the other samples may be challenging. Despite that, it was possible to distinguish the <sup>87</sup>Sr/<sup>86</sup>Sr ratios of the wines from São Joaquim, state of Santa Catarina, from the wines from Bento Gonçalves, state of Rio Grande do Sul. 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引用次数: 0
摘要
世界范围内的研究,特别是在加拿大、意大利和巴西,已经证明87Sr/86Sr比例是葡萄酒地理来源的可靠指标。我们在这里介绍了最近在巴西南部圣卡塔琳娜州创建的圣卡塔琳娜州地理标志海拔葡萄酒的第一个87Sr/86Sr同位素研究。本研究的目的是评估锶同位素比率的法医应用,作为圣卡塔琳娜州主要葡萄酒产区 o Joaquim葡萄酒的来源指标,该地区生产的葡萄酒来自欧洲葡萄品种(Vitis vinifera L.),这些葡萄品种生长在Serra Geral Group (paran岩浆省)火山岩风化形成的土壤中。测定了来自若阿金省三个酒庄的岩石、土壤(散装和不稳定组分)、葡萄(叶子和葡萄)和葡萄酒(长相思和赤霞珠)的87Sr/86Sr。玄武安山岩基岩87Sr/86Sr比值为0.705362,英安岩基岩87Sr/86Sr比值为0.724819,与报道的这类岩石值一致。我们发现葡萄和叶子的87Sr/86Sr比例之间存在很强的相关性,但与大多数先前的研究相反,土壤(散装和不稳定组分)与葡萄酒样品之间没有相关性。这表明,尽管葡萄和叶片中的Sr同位素表现保守,但土壤中的Sr同位素可能受到葡萄园农业实践(如施肥和石灰化)的改变。因此,我们建议土壤取样深度为60厘米,以避免外部添加锶。由于商业葡萄酒的87Sr/86Sr比率代表了给定葡萄园的平均同位素比率,因此葡萄酒与其他样品之间的同位素相关性可能具有挑战性。尽管如此,还是有可能区分出圣卡塔琳娜州若阿金州和南巴西格兰德州本托贡帕拉尔维斯州葡萄酒的87Sr/86Sr比例。尽管这两个产区的葡萄酒都是由同一地质单元种植的葡萄酿造而成,即来自Serra Geral Group (paran岩浆省)的火山岩,但葡萄酒的Sr特征却不同。
From rock to bottle: strontium isotopes (87Sr/86Sr) as indicator of provenance for the volcanic wines of altitude from São Joaquim, southern Brazil
Studies worldwide, particularly in Canada, Italy and Brazil, have demonstrated that the 87Sr/86Sr ratio is a reliable indicator of the geographic origin of wines. We present here the first 87Sr/86Sr isotope study for the Wines of Altitude of Santa Catarina geographical indication that was recently created in the state of Santa Catarina, southern Brazil. The goal of this study is to evaluate the forensic application of strontium isotope ratios as an indicator of provenance for the wines of São Joaquim, the main wine-growing region in the state of Santa Catarina, which produces wines from European grape varieties (Vitis vinifera L.) grown in soils formed by the weathering of volcanic rocks of the Serra Geral Group (Paraná Magmatic Province). The 87Sr/86Sr of rocks, soils (bulk and labile fractions), vines (leaves and grapes) and wines (Sauvignon Blanc and Cabernet Sauvignon) from three wineries from São Joaquim were determined. Bedrock 87Sr/86Sr ratios ranged from 0.705362 for the basaltic-andesitic rocks to 0.724819 for dacites, consistent with reported values for these types of rocks. We identified a strong correlation between the 87Sr/86Sr ratios of the grapes and leaves, but in contrast to most previous studies there was no correlation between those of the soil (both bulk and labile fractions) and wine samples. This indicates that although the Sr isotopes in grapes and leaves behaved conservatively, the Sr isotopes in the soils may have been modified by vineyard agricultural practices, such as fertilization and liming. We thus recommend that soil sampling be done at depths >60 cm to avoid external addition of strontium. As the 87Sr/86Sr ratios of commercial wines represent the average isotope ratio of a given vineyard, the isotope correlation between wines and the other samples may be challenging. Despite that, it was possible to distinguish the 87Sr/86Sr ratios of the wines from São Joaquim, state of Santa Catarina, from the wines from Bento Gonçalves, state of Rio Grande do Sul. Even though the wines from both regions are made from grapes cultivated in the same geological unit, i.e., volcanic rocks from Serra Geral Group (Paraná Magmatic Province), the wines yield different Sr signatures.
期刊介绍:
Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment.
Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.