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…

Soil, vine, climate change – what is observed – what is expected

To evaluate the current and future impact of climate change on Viticulture requires an integrated view on a complex interacting system within the soil-plant-atmospheric continuum under continuous change. Aside of the globally observed increase in temperature in basically all viticulture regions for at least four decades, we observe several clear trends at the regional level in the ratio of precipitation to potential evapotranspiration. Additionally the recently published 6th assessment report of the IPCC (The physical science basis) shows case-dependent further expected shifts in climate patterns which will have substantial impacts on the way we will conduct viticulture in the decades to come.
Looking beyond climate developments, we observe rising temperatures in the upper soil layers which will have an impact on the distribution of microbial populations, the decay rate of organic matter or the storage capacity for carbon, thus affecting the emission of greenhouse gases (GHGs) and the viscosity of water in the soil-plant pathway, altering the transport of water. If the upper soil layers dry out faster due to less rainfall and/or increased evapotranspiration driven by higher temperatures, the spectral reflection properties of bare soil change and the transport of latent heat into the fruiting zone is increased putting a higher temperature load on the fruit. Interactions between micro-organisms in the rhizosphere and the grapevine root system are poorly understood but respond to environmental factors (such as increased soil temperatures) and the plant material (rootstock for instance), respectively the cultivation system (for example bio-organic versus conventional). This adds to an extremely complex system to manage in terms of increased resilience, adaptation to and even mitigation of climate change. Nevertheless, taken as a whole, effects on the individual expressions of wines with a given origin, seem highly likely to become more apparent.

VINIoT – Precision viticulture service

The project VINIoT pursues the creation of a new technological vineyard monitoring service, which will allow companies in the wine sector in the SUDOE space to monitor plantations in real time and remotely at various levels of precision. The system is based on spectral images and an IoT architecture that allows assessing parameters of interest viticulture and the collection of data at a precise scale (level of grape, plant, plot or vineyard) will be designed. In France, three subjects were specifically developed: evaluation of maturity, of water stress, and detection of flavescence dorée. For the evaluation of maturity, it has been decided first to work at the berry scale in the laboratory, then at the bunch scale and finally in the vineyard. The acquisition of the spectral hyperstal image as well as the reference analyzes to measure the maturity, were carried out in the laboratory after harvesting the berries in a maturity monitoring context. This work focuses on a case study to predict sugar content of three different grape varieties: Syrah, Fer Servadou and Mauzac. A robust method called Roboost-PLSR, developed in the framework of this work (Courand et al., 2022), to improve prediction model performance was applied on spectra after the acquirement of hyperspectral images. Regarding the evaluation of water stress, to work with a significant variability in terms of water status, it has been worked first with potted plants under 2 different water regimes. The facilities have allowed the supervision of irrigation and micro-climatic conditions. The regression models on agronomic variables (stomatal conductance, water potential, …) are studied. To detect flavescence dorée, the experimental plan has consisted of work at leaf scale in the laboratory first, and then in the field. To detect the disease from hyper-spectral imaging, a combination of multivariate curve resolution-alternating least squares (MCR-ALS) and factorial discriminant analysis (FDA) was proposed. This strategy proved the potential towards the discrimination of healthy and infected leaves by flavescence dorée based on the use of hyperspectral images (Mas Garcia et al., 2021).

Combining effect of leaf removal and natural shading on grape ripening under two irrigation strategies in Manto negro (Vitis vinifera L.)

The increasingly frequent heat waves during grape ripening pose challenges for high quality wine grape production. Defoliation is a common practice that can improve the control of diseases in bunches, but also it increases the exposure to sunlight. Grapes exposed to solar radiation reach temperatures over the optimum for berry development and maturation. This makes the development of irrigation and canopy management techniques of great importance to maximize yield and grape quality. A field experiment was carried out during 2021 using Manto negro wine grapes to study the effect of applied irrigation and different light exposure levels on grape quality. Two irrigation treatments were imposed based on the frequency and amount of water doses in a four-block experimental vineyard at Bodega Ribas (Mallorca). Three light exposure treatments were randomly applied in each irrigation plot. The light treatments included exposed clusters from pea size, non-exposed clusters, and shaded clusters after softening. Leaf area index and canopy porosity was estimated every 2 weeks. Midday leaf water potential was measured weekly. Additionally, apparent electrical conductivity was measured between rows to estimate the soil water content variability. Light and temperature sensors were installed at the bunch level to quantify the differences in bunch temperature and light intensity among treatments. The effect of irrigation and cluster light exposure on berry weight, TSS, TA, malic acid, tartaric acid, K+, and pH were analysed at 5 moments along grape ripening. During different heat waves, the natural shading technique decreased the maximum bunch temperature around 10 °C respect to the exposed bunches in both irrigation strategies. The combination of defoliation and shading techniques after softening decreased TSS at harvest and affected most of the quality parameters during the last stages of ripening, showing an interesting technique to delay ripening in warm viticulture areas.

Influence of weather and climatic conditions on the viticultural production in Croatia

The research includes an analysis of the impact of weather conditions on phenological development of the vine and grape quality, through monitoring of four experimental cultivars (Chardonnay, Graševina, Merlot and Plavac mali) over two production years. In each experimental vineyard, which were evenly distributed throughout the regions of Slavonia and The Croatian Danube, Croatian Uplands,

Evolution of the amino acids content through grape ripening: Effect of foliar application of methyl jasmonate with or without urea

The parameters that determine the grape quality, and therefore the optimal harvest time, suffer variations during berry ripening, related to climate change, with the widely known problem of the gap between technological and phenolic maturities. However, there are few studies about its incidence on grape nitrogen composition. For this reason, the use of an elicitor, methyl jasmonate (MeJ), alone or with urea, is proposed as a tool to reduce climatic decoupling, allowing to establish the harvest time in order to achieve the optimum grape quality. The aim was to study the effect of MeJ and MeJ+Urea foliar applications on the evolution of Tempranillo amino acids content throughout the grape maturation. Three treatments were foliarly applied, at veraison and 7 days later: control (water), MeJ (10 mM) and MeJ+Urea (10 mM+6 kg N/ha). Grape samples were taken at five stages of maturation: day before the first and second applications, 15 days after the second application (pre-harvest), harvest day, and 15 days after harvest (post-harvest). The amino acids analysis of the samples was carried out by HPLC. Results showed that the evolution of amino acids was similar regardless of the treatment; however, foliar applications influenced the nitrogen compounds content, i.e., there was no qualitative effect but quantitative one. Most of the amino acids reached their maximum concentration in pre-harvest, being higher in grapes from the treatments than in the control. In general, no differences in grape amino acids content were observed between MeJ and MeJ+Urea treatments. Foliar applications with MeJ and MeJ+Urea enhanced the grape amino acids content, without affecting their profile, helping to optimize their quality and allowing to establish a more complete grape ripening standard. Therefore, MeJ and MeJ+Urea foliar applications can be a simple agronomic practice, which has shown promising results in order to enhance the grape quality.