| Abstract: | Waterlogging stress limits the productivity of winter wheat(Triticum aestivum L. emend. Thell.) in many parts of the world.When wheat is grown under waterlogged conditions, a reddish-brownmineral coating can form on the epidermal surface of the roots.In wetland plants such as rice, the amount of mineral coatingformed on root surfaces is positively related to yield. Thisstudy was conducted to determine whether mineral coating onthe roots of wheat is related to yield potential under waterloggedconditions. Root mineral coatings formed under waterlogged conditionswere studied in 12 cultivars and two breeding lines over threeyears of greenhouse pot studies. Soil redox potential in thewaterlogged treatment ranged between - 46 and 171 mV, and grainyield was suppressed by 28–49% compared to well-drainedcontrols. Mineral coating formed on the roots from the waterloggedtreatment was determined to be composed primarily of iron, basedon ICP elemental analysis, iron-specific staining, and ion-mappingby scanning electron microscopy using an X-ray detector. Of11 elements quantified by ICP spectroscopy, six were significantlyaffected by waterlogging treatment, and three of these, Fe,Mn and P, were well-correlated negatively to yield. Aerenchymaformation in the heavily coated waterlogged roots appeared todisrupt the internal root structure, and exceeded 40% of cross-sectionalarea in one cultivar. Unlike rice, which shows a positive relationshipbetween oxygen release from roots, grain yield and mineral coating,in winter wheat, the amount of mineral coating is negativelyrelated to grain yield under waterlogged conditions. Key words: Wheat, mineral coating, waterlogging, aerenchyma, hypoxia |
