Terroir 2008 banner
IVES 9 IVES Conference Series 9 Geopedological and climatic zoning of northern Malaga vineyards region: Fuente de Piedra, Humilladero and Mollina (southern Spain)

Geopedological and climatic zoning of northern Malaga vineyards region: Fuente de Piedra, Humilladero and Mollina (southern Spain)

Abstract

The vineyards placed in the municipal areas of Fuente de Piedra, Humilladero and Mollina constitute a wine-growing important area of the “Zona Norte” of the province of Málaga. Its products are protected by the Regulatory Council of the Origin Denomination “Málaga”, ” Sierras de Málaga ” and ” Pasas de Málaga”. A study of viticultural zoning of the areas belonging to those municipalities, in which diverse varieties of recommended and/or authorized grapevines are cultivated, have been realized taking in consideration principally geological, pedological and climatic characteristics.
In the region, the formations of the Mid Subbetico -constituted by limy materials of different facies- dates of the Jurassic Period mainly, and they are the original constituents of the mountainous zones with altitudes superior to 500 m a.s.l.; from North to South they form La Camorra (686 m), Sierra Mollina (796 m) and Sierra de Humilladero (656 m). The lower zones have altitudes less than 450 m. They are constituted by karstic areas, that operate of sink of the Fuente de Piedra lagoon; by the Quaternary low areas associated with this one; by those areas of the edge of the fluvial valley that feeds it, and by the southeastern edge of the municipal area of Mollina, related to the hydrographic network of the Depression of Antequera and Guadalhorce River.
The zones of medium altitudes, those of major agricultural interest for their extension, phisiografy and geopedological characteristics, are constitued by Postorogenic Tertiary Formations of the Miocene (Tortoniense – Andaluciense), and by those ones dating of the Trias -marls, sandstones and gypsum– which are highly represented in the surface of the eastern Mollina. They can be divided in several basins; the two principal ones are those of the East (Mollina) and of the West (Humilladero and Fuente de Piedra); in addition, one at the south of Sierra de Humilladero, and another one at the north of Fuente de Piedra, Humilladero and Mollina.
The zones of medium altitudes includes tabular reliefs –concerning those three municipalities-; plains and hills of dissection, glacises of coverage that surround the mountainous formations; and conical hills of the trias from the northwestern and eastern sectors of the region.
The soils of agricultural interest (olive grove, vineyard and dry and irrigated cereals) are very degraded; they are principally on Tertiary and Quaternary limy materials and, in minor extension, on the eastern Trias of the region. On the Postorogenic Tertiary they are formed soils (Calcisols and Cambisols) on calcarenites with a limy crust (“blancales“), and others on marls (Regosols, Cambisols and Vertisols). On Quaternary sediments and/or on marls and limy sandstones of the Trias, Regosols, Cambisols and Luvisols are formed; and in very minor extension some Fluvisols (“vegas”, “cubrijales”).
Finally, four climatic zones have been delimited in the region according to the rainfall and temperature -differentiating four periods according to its viticultural interest (C1, C2, C3 and C4)- by using series of 20 years from five metereological stations. The climatic zone of the South is considered to be as Thermo-Humid; that of the North as Subthermo-Subhumid; the eastern area as Mesothermo-Humid and that at the West, Mesothermo-Subhumid.
Diverse maps of zoning have been made: Z-1, geology, altitude and fluvial network; Z-2, geomorphology, altitude and fluvial network; Z-3, Soil groups and geomorphology; Z-4 geology and geomorphology; and map Z-5, viticultural areas. A global appraisal of the areas has been been carried out, resulting four classes of suitability of the same ones on the basis of the studied characteristics and requirements for the grapevine growing.
Finally, several pictures and descriptive and analytical tables contain detailed information of the different representative “areas”, “pagos” or “terroirs” in this region.

DOI:

Publication date: December 8, 2021

Issue: Terroir 2008

Type : Article

Authors

Patricia PANEQUE, Consuelo Paloma OSTA, Celia ESPINO, Guillermo PANEQUE

Dpto de Cristalografía, Mineralogía y Química Agrícola, Universidad de Sevilla. c/ Profesor García González 1. 41012 Seville, Spain

Contact the author

Keywords

Málaga Norte, geology, soil, climate, zoning

Tags

IVES Conference Series | Terroir 2008

Citation

Related articles…

Exploring diversity of grapevine responses to Flavescence dorée infection

Flavescence dorée, a serious threat to grapevine cultivation in several European Countries, is caused by phytoplasmas in the 16Sr-V ribosomal group, classified as quarantine organisms in the EU and transmitted mainly by the insect vector Scaphoideus titanus. The disease is controlled only by indirect and preventive measures, with important economic and environmental concerns. Genetic resources from the great variety of Vitis vinifera germplasm together with application of new genomic techniques could be applied to produce resistant/tolerant plants, once the genetic bases of susceptibility are elucidated. In a current Italian project (BIORES*) we are evaluating different international and local grapevine cvs. as well as microvine plants for their response to FD transmission and multiplication in controlled conditions.

Growth in global table grape production and consumption is fueled by the introduction of new seedless varieties

Table grape consumption worldwide has experienced a remarkable growth in the first two decades of the 21st century, becoming the third most consumed fresh fruit in some countries, after bananas and apples. This increase has been attributed to several reasons, including the availability of seedless grapes, which has been a key factor in the increase in consumption.

Rootstock regulation of scion phenotypes: the relationship between rootstock parentage and petiole mineral concentration

Grapevine is grown as a graft since the end of the 19th century. Rootstocks not only provide tolerance to Phylloxera but also ensure the supply of water and mineral nutrients to the scion. Rootstocks are an important mean of adaptation to environmental conditions, because the scion controls the typical features of the grapes and wine. However, among the large diversity of rootstocks worldwide, few of them are commercially used in the vineyard. The aim of this study was to investigate the extent to which rootstocks modify the mineral composition of the petioles of the scion. Vitis vinifera cvs. Cabernet-Sauvignon, Pinot noir, Syrah and Ugni blanc were grafted onto 55 different rootstock genotypes and planted in a vineyard as three replicates of 5 vines. Petioles were collected in the cluster zone with 6 replicates per combination. Petiolar concentrations of 13 mineral elements (N, P, K, S, Mg, Ca, Na, B, Zn, Mn, Fe, Cu, Al) at veraison were determined. Scion, rootstock and the interaction explained the same proportion of the phenotypic variance for most mineral elements. Rootstock genotype showed a significant influence on the petiole mineral element composition. Rootstock effect explained from 7 % for Cu to 25 % for S of the variance. The difference of rootstock conferred mineral status is discussed in relation to vigor and fertility. Rootstocks were also genotyped with 23 microsatellite markers. Data were analysed according to genetic groups in order to determine whether the petiole mineral composition could be related to the genetic parentage of the rootstock. Thanks to a highly powerful design, it is the first time that such a large panel of rootstocks grafted with 4 scions has been studied. These results give the opportunity to better characterize the rootstocks and to enlarge the diversity used in the vineyard.

Study of Spanish wine sensory analysis data over a 3-year period

This study presents an investigation based on sensory analysis data of Spanish wines with geographical indications collected over a three-year period. Sensory analysis plays a crucial role in assessing the quality, characteristics, and perception of wines. The trained tasting panel at Dolmar Laboratory, accredited for objective sensory evaluation of wines since 2016, has been tasting over 5000 wines. However, it is since 2021, when a computer application for tastings was developed, that the digitalization of data allows for detailed statistical analysis of the results.

Spatial variability of grape berry maturation program at the molecular level 

The application of sensors in viticulture is a fast and efficient method to monitor grapevine vegetative, yield and quality parameters and determine their spatial intra-vineyard variability. Molecular analysis at the gene expression level can further contribute to the understanding of the observed variability by elucidating how pathways responsible for different grape quality traits behave in zones diverging for one or the other parameter. The intra-vineyard variability of a Cabernet Sauvignon vineyard was evaluated by a standard Normalized Difference Vegetation Index (NDVI) mapping approach, employing UAV platform, accompanied by detailed ground-truthing (e.g. vegetative, yield, and berry ripening compositional parameters) that was applied in 14 spots in the vineyard. Berries from different spots were additionally investigated by microarray gene expression analysis, performed at five time points from fruit set to full ripening.