Terroir 2012 banner
IVES 9 IVES Conference Series 9 Typology of Terroirs around the world

Typology of Terroirs around the world

Abstract

It seems implausible that the geographical development of the vineyards could have been affected by a shift in the positions of the Earth’continents that started 250 million years ago. At one end of the geological timescale there are landscapes shaped by men, at the other, there are monumental upheavals so slow that they defy the imagination. In fact, the succession of landslides, collisions, eruptions, and subductions that marked the Paleozoic and Mesozoic eras and the Tertiary period was indeed the original source of the rocks and great masses that were then chiseled into shape 2 million years ago, at the start of the Quaternary period, to form the wine-growing landscapes that we see today. The study of these different phenomena allows to offer a classification, a typography of vitivinicultural terroirs across the world according to the history of geology and geomorphology of the different vitivinicultural areas.

DOI:

Publication date: August 26, 2020

Issue: Terroir 2012

Type: Article

Authors

Jacques FANET

Mas d’Arlenques 3 chemin des Combes d’Arlenques 34800 ASPIRAN – FRANCE

Contact the author

Keywords

Continental drift, geology, geomorphology, terroir

Tags

IVES Conference Series | Terroir 2012

Citation

Related articles…

Does treatment of grape juice with aspergillopepsin-i influence wine aroma?

Acid aspergillopepsins-i (ap-i) have been suggested for use in winemaking due to their ability to degrade proteins, which reduces haze formation and the necessity for bentonite to achieve protein stability. These endopeptidases cleave non-terminal amino acid bonds of proteins, resulting in their degradation.

IMPACT OF ACIDIFICATION AT BOTTLING BY FUMARIC ACID ON RED WINE AFTER 2 YEARS

Global warming is responsible for a lack of organic acid in grape berries, leading to wines with higher pH and lower titrable acidity. The chemical, microbiological and organoleptic equilibriums are impacted by this change of organic acid concentration. It is common practice to acidify the wine in order to prevent these imbalances that can lead to wine defects and early spoilage. Tartaric acid (TA) is most commonly used by winemaker for wine acidification purposes. Fumaric acid (FA), which is authorized by the OIV in its member states for the inhibition of malolactic fermentation, could also be used as a potential acidification candidate since it has a better acidifying power than tartaric acid.

Impact of reduction alcohol techiniques in the aromatic chemical profile of rosé Tempranillo wines

Studying the impact of reducing alcohol techniques in the chemical composition of the aromatic profile of rosé Tempranillo wines from the spanish region of Castilla-La Mancha INTRODUCTION: In the last decades there has been an increseasing demand of wines with low or non-existing alcohol concentration due to the negative effects that alcohol has in health. In spite of that, there are not laws that protect these products, and there is also a great difficulty in the elaboration of these type of wines due to the increasing temperatures because of climate change. This is why the oenological industry has made great advances in the development of different techniques that could satisfy consumers’ demands without modifying wine quality. The most used techniques have been post-fermentative ones.

Descriptive analysis of Sangiovese and Cabernet-Sauvignon wines from different terroirs in D.O.C. Bolgheri (Tuscany)

Different terroirs have been identified in Bolgheri area (a viticultural appellation in the Tirrenian coast of Tuscany) by the aid of pedological, landscape and agronomic observations in 1993. Numerous preliminary observations suggested that wines obtained from these different terroirs were unique.

The albarizas and the viticultural zoning of Jerez­-Xérès-Sherry and Manzanilla-Sanlúcar de Barrameda registered apellations of origin (Cadiz, Spain)

Le terme ”Albariza” (du latin “albus“, blanc) déterminait à l’origine un type particulier du terrain calcaire, mais à présent il sert aussi à définir les sols et la bibliographie géologique actuelle le cite également pour de roches sédimentaires originaires du Neogene Betic.