Le fer du sol aux produits végétaux

Abstract

As an essential mineral, iron plays an important role in fundamental biological processes such as photosynthesis, respiration, nitrogen fixation and assimilation, and DNA synthesis. Iron is also a co-factor of many enzymes involved in the synthesis of plant hormones. The latter are involved in many pathways controling plant development or adaptative responses to environmental conditions. Iron reactivity with oxygen leads to its insolubility (responsible for deficiency) and potential toxicity, and complicates iron use by aerobic organisms. If plants lacked an active root system with which to acquire iron from the soil, most would experience iron deficiency and show physiological changes. In contrast, an excess of soluble iron, which can occur in flooded acidic soils, can lead to ferrous iron toxicity due to iron reactivity with reduced forms of oxygen and subsequent free radical production. An optimal iron concentration is thus required for a plant to grow and develop normally. This concentration depends on multiple regulatory mechanisms controlling iron uptake from soil by the roots, as well as iron transport and distribution to the various plant organs. Optimized seed iron content is a major biotechnological challenge identified by the World Health Organization, and it is therefore crucial to understand the underlying mechanisms. Iron delivery to seeds is tightly controlled, and depends on the nature of iron speciation in specific chelates, and their transport.