Kermeur Nolenn, Pédrot Mathieu, Cabello-Hurtado Francisco
University of Rennes, CNRS, Ecobio, UMR 6553, Rennes, France.
University of Rennes, CNRS, Géosciences Rennes, UMR 6118, Rennes, France.
Methods Mol Biol. 2023;2642:49-81. doi: 10.1007/978-1-0716-3044-0_3.
Iron is an essential element for all living organisms, playing a major role in plant biochemistry as a redox catalyst based on iron redox properties. Iron is the fourth most abundant element of the Earth's crust, but its uptake by plants is complex because it is often in insoluble forms that are not easily accessible for plants to use. The physical and chemical speciation of iron, as well as rhizosphere activity, are key factors controlling the bioavailability of Fe. Iron can be under reduced (Fe) or oxidized (Fe) ionic forms, adsorbed onto mineral surfaces, forming complexes with organic molecules, precipitated to form poorly crystalline hydroxides to highly crystalline iron oxides, or included in crystalline Fe-rich mineral phases. Plants must thus adapt to a complex and changing iron environment, and their response is finely regulated by multiple signaling pathways initiated by a diversity of stimulus perceptions. Higher plants possess two separate strategies to uptake iron from rhizosphere soil: the chelation strategy and the reduction strategy in grass and non-grass plants, respectively. Molecular actors involved in iron uptake and mobilization through the plant have been characterized for both strategies. All these processes that contribute to iron homeostasis in plants are highly regulated in response to iron availability by downstream signaling responses, some of which are characteristic signaling signatures of iron dynamics, while others are shared with other environmental stimuli. Recent research has thus revealed key transcription factors, cis-acting elements, post-translational regulators, and other molecular mechanisms controlling these genes or their encoded proteins in response to iron availability. In addition, the most recent research is increasingly highlighting the crosstalk between iron homeostasis and nutrient response regulation. These regulatory processes help to avoid plant iron concentrations building up to potential cell functioning disruptions that could adversely affect plant fitness. Indeed, when iron is in excess in the plant, it can lead to the production and accumulation of dangerous reactive oxygen species and free radicals (HO, HO, O, HO) that can cause considerable damages to most cellular components. To cope with iron oxidative stress, plants have developed defense systems involving the complementary action of antioxidant enzymes and molecular antioxidants, safe iron-storage mechanisms, and appropriate morphological adaptations.
铁是所有生物必需的元素,基于铁的氧化还原特性作为氧化还原催化剂在植物生物化学中发挥着重要作用。铁是地壳中含量第四丰富的元素,但植物对其吸收过程复杂,因为它常以不溶性形式存在,植物难以利用。铁的物理和化学形态以及根际活性是控制铁生物有效性的关键因素。铁可以处于还原态(Fe)或氧化态(Fe)离子形式,吸附在矿物表面,与有机分子形成络合物,沉淀形成结晶度低的氢氧化物至高结晶度的铁氧化物,或包含在富含铁的结晶矿物相中。因此,植物必须适应复杂多变的铁环境,其反应受到多种由不同刺激感知引发的信号通路的精细调节。高等植物有两种从根际土壤吸收铁的不同策略:禾本科植物的螯合策略和非禾本科植物的还原策略。参与这两种策略中铁吸收和在植物体内转运的分子作用因子已得到表征。所有这些有助于植物铁稳态的过程都通过下游信号反应对铁的可用性进行高度调节,其中一些是铁动态的特征信号特征,而其他一些则与其他环境刺激共享。因此,最近的研究揭示了关键转录因子、顺式作用元件、翻译后调节因子以及其他响应铁可用性控制这些基因或其编码蛋白质的分子机制。此外,最新研究越来越强调铁稳态与营养反应调节之间的相互作用。这些调节过程有助于避免植物铁浓度升高到可能对细胞功能产生潜在干扰并对植物适应性产生不利影响的水平。实际上,当植物中铁过量时,会导致危险的活性氧和自由基(HO、HO、O、HO)的产生和积累,这些物质会对大多数细胞成分造成相当大的损害。为了应对铁氧化应激,植物已经发展出防御系统,包括抗氧化酶和分子抗氧化剂的协同作用、安全的铁储存机制以及适当的形态适应。