Glera vineyards from the Prosecco wine district in northern Italy have been characterized in terms of the 87Sr/86 Sr isotope-ratio of musts from the 2010, 2011 and 2012 vintages, coupled with the isotopic analysis of Sr in the labile fraction of the soils of provenance. For a single vineyard, detailed Sr isotopic analyses were carried out in sequentially extracted soil fractions at three different depths, and in the grape components (skin, seeds, must and stem), in order to verify the lack of Sr isotopic fractionation within the plant. The 87Sr/86Sr in must, seeds and stem overlaps within experimental uncertainties; skins are shifted towards a lower Sr isotopic composition. A large range of Sr isotopic compositions (87Sr/86 21 Sr between 0.70706 and 0.71215) characterizes musts from the different vineyards, notwithstanding the relatively limited extension of the investigated geographic area. A statistically significant correspondence between the soil labile fraction and must is observed.
The 87Sr/86Sr strontium isotopic systematics applied to Glera vineyards: a tracer for the geographical origin of the Prosecco / Petrini R.; Sansone L.; Slejko F.F.; Buccianti A.; Marcuzzo P.; Tomasi D.. - In: FOOD CHEMISTRY. - ISSN 0308-8146. - STAMPA. - 170:(2015), pp. 138-144. [10.1016/j.foodchem.2014.08.051]
The 87Sr/86Sr strontium isotopic systematics applied to Glera vineyards: a tracer for the geographical origin of the Prosecco
BUCCIANTI, ANTONELLA;
2015
Abstract
Glera vineyards from the Prosecco wine district in northern Italy have been characterized in terms of the 87Sr/86 Sr isotope-ratio of musts from the 2010, 2011 and 2012 vintages, coupled with the isotopic analysis of Sr in the labile fraction of the soils of provenance. For a single vineyard, detailed Sr isotopic analyses were carried out in sequentially extracted soil fractions at three different depths, and in the grape components (skin, seeds, must and stem), in order to verify the lack of Sr isotopic fractionation within the plant. The 87Sr/86Sr in must, seeds and stem overlaps within experimental uncertainties; skins are shifted towards a lower Sr isotopic composition. A large range of Sr isotopic compositions (87Sr/86 21 Sr between 0.70706 and 0.71215) characterizes musts from the different vineyards, notwithstanding the relatively limited extension of the investigated geographic area. A statistically significant correspondence between the soil labile fraction and must is observed.File | Dimensione | Formato | |
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