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O-31<br />

Mapping genetic loci for tolerance to iron induced chlorosis in grapevine (Vitis vinifera L.)<br />

S. Decroocq, L. Bordenave, M. Donnart, C. Hévin, J.-P. Dodane, N. Ollat, P-F. Bert*<br />

Institut des Sciences de la Vigne et du Vin, UMR 1287 Ecophysiologie et Génomique<br />

Fonctionnelle de la Vigne INRA, Université de Bordeaux 1, Université Victor Ségalen Bordeaux<br />

2, Centre INRA de Bordeaux, Villenave d’Ornon, France<br />

*Corresponding author: pfbert@bordeaux.inra.fr<br />

Iron is essential to plants for chlorophyll formation as well as for the functioning of various ironcontaining<br />

enzymes. Iron deficiency chlorosis is a wide-spread disorder of plants, in particular of<br />

those on calcareous soils. In the soil matrix, Fe exists in one of two forms, Fe2+or Fe3+.<br />

However, many environmental conditions, including the high pH of calcareous soils, can result<br />

in little Fe2+ availability ("lime-induced chlorosis"). To survive in iron limiting environments,<br />

plants have evolved two iron uptake strategies, Strategy I <strong>and</strong> II. Dicot species, including<br />

grapevine, utilize the Strategy I mechanism to take up the Fe2+ ion. Strategy I plants utilize an<br />

ATPase to secrete protons from the roots to acidify the rhizosphere which aids the release of Fe<br />

from chelating agents in the soil. A root membrane reductase reduces the prevalent Fe3+ion to<br />

the biologically usable Fe2+ ion, which can then be transported into the roots of the plant where<br />

it is available for use in various cellular processes. For Strategy I plants, the iron reduction by<br />

plant roots has been identified as the rate-limiting step in iron deficiency. Strategy II plants, such<br />

as monocot species, release phytosiderophores from the roots that chelate Fe3+ ions. The entire<br />

phytosiderophore iron complex is then transported into the root system of the plant. Complex<br />

genetic <strong>and</strong> environmental interactions have made iron induced chlorosis an extremely difficult<br />

trait to study in field trials <strong>and</strong> today, the mechanisms of tolerance remain poorly understood.<br />

The aim of the experiment was to characterize the genetic basis of grapevine chlorosis tolerance<br />

under lime stress conditions. A segregating population of 138 F1 genotypes issued from an interspecific<br />

cross between V. vinifera Cabernet Sauvignon (tolerant) × V. riparia Gloire de<br />

Montpellier (sensitive) was developed <strong>and</strong> grown both as cuttings <strong>and</strong> as rootstock grafted plants<br />

<strong>with</strong> Cabernet Sauvignon scions in pots of non-chlorosing <strong>and</strong> chlorosing soils. Tolerance was<br />

evaluated by chlorosis score, chlorophyll contents <strong>and</strong> growth parameters of shoots <strong>and</strong> roots.<br />

Experiments were done in 2001, 2003 <strong>and</strong> 2006 <strong>and</strong> the material from the 2006 assay was reused<br />

in 2007. The most significant findings of the trial were: (a) the soil properties strongly affected<br />

both shoot <strong>and</strong> root development; (b) there are differences in tolerance among segregating<br />

genotypes when grown as cuttings or as rootstocks on calcareous soil; (c) calcareous conditions<br />

induced chlorosis <strong>and</strong> revealed QTLs implicated in polygenic control of tolerance; (d) rootstock<br />

strongly contributes to lime-induced chlorosis tolerance <strong>and</strong>; (e) a QTL <strong>with</strong> strong effect (from<br />

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