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8 - Molybdenum Availability in Alkaline Soils

Published online by Cambridge University Press:  10 December 2009

Umesh C. Gupta
Affiliation:
Agriculture and Agri-Food Canada Research Centre
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Summary

Introduction

Molybdenum (Mo) is essential for higher plants (Arnon and Stout, 1939). As a constituent of nitrate reductase, sulfite reductase, and, in nodulated legumes, nitrogenase and xanthine oxidase, it is involved in electron-transfer reactions. Nitrate reductase, which catalyzes the conversion of nitrate to nitrite by transfer of electrons from Mo to nitrate, is an inducible enzyme that depends on Mo for its synthesis. There is a close relationship involving Mo supply, nitrate reductase activity, and plant growth. In the nitrogenase of legumes and other plants that fix atmospheric nitrogen, Mo is directly involved in the reduction of N2 (Witt and Jungk, 1977). As a constituent of xanthine oxidase it catalyzes the oxidation of xanthine to uric acid, which is a precursor of allantoin and allantoic acid in most tropical and subtropical legumes. Besides playing a catalytic role, Mo is required for plant reproductive development (Agarwala et al., 1979) and nodulation of leguminous and nonleguminous N-fixing plants (Becking, 1961).

Compared with those for other micronutrients, the physiological requirements for Mo are very low (Stout and Meagher, 1948; Hewitt, 1963). The adequate concentrations of Mo in most crops range between 0.1 and 1. Omgkg–1 (Bergmann, 1988), but the threshold for Mo toxicity in plants is much higher than that for any other micronutrient. Some plants can accumulate 1,000 times their adequate concentrations of Mo without exhibiting any visible signs of toxicity: cotton (Gossypium spp.), tomato (Lycopersicon esculentum Mill.), and Phaseolus beans (Joham, 1953; Johnson, 1966; Widdowson, 1966).

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Publisher: Cambridge University Press
Print publication year: 1997

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