Response of soybean to soil waterlogging associated with iron excess in the reproductive stage

Soil waterlogging is a common problem in some agricultural areas, including regions under soybean ( Glycine max ) cultivation. In waterlogged soils, soil O 2 depletion occurs due to aerobic microorganisms and plants, affecting the metabolic and physiological processes of plants after suffering anoxi...

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Published in:Physiology and molecular biology of plants Vol. 26; no. 8; pp. 1635 - 1648
Main Authors: Lapaz, Allan de Marcos, de Camargos, Liliane Santos, Yoshida, Camila Hatsu Pereira, Firmino, Ana Carolina, de Figueiredo, Paulo Alexandre Monteiro, Aguilar, Jailson Vieira, Nicolai, Artur Bernardeli, Silva de Paiva, Wesller da, Cruz, Victor Hugo, Tomaz, Rafael Simões
Format: Journal Article
Language:English
Published: New Delhi Springer India 01-08-2020
Springer Nature B.V
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Summary:Soil waterlogging is a common problem in some agricultural areas, including regions under soybean ( Glycine max ) cultivation. In waterlogged soils, soil O 2 depletion occurs due to aerobic microorganisms and plants, affecting the metabolic and physiological processes of plants after suffering anoxia in their root tissue. Another harmful factor in this situation is the exponential increase in the availability of iron (Fe) in the soil, which may result in absorption of excess Fe. The present study sought to evaluate the response mechanisms in soybean leaves ‘Agroeste 3680’ by physiological and biochemical analyses associating them with the development of pods in non-waterlogged and waterlogged soil, combined with one moderate and two toxic levels of Fe. Gas exchange was strongly affected by soil waterlogging. Excess Fe without soil waterlogging reduced photosynthetic pigments, and potentiated this reduction when associated with soil waterlogging. Starch and ureide accumulation in the first newly expanded trifoliate leaves proved to be response mechanisms induced by soil waterlogging and excess Fe, since plants cultivated under soil non-waterlogged soil at 25 mg dm −3 Fe showed lower contents when compared to stressed plants. Thus, starch and ureide accumulation could be considered efficient biomarkers of phytotoxicity caused by soil waterlogging and excess Fe in soybean plants. The reproductive development was abruptly interrupted by the imposition of stresses, leading to a loss of pod dry biomass, which was largely due to the substantial decrease in the net photosynthetic rate, as expressed by area ( A ), the blockage of carbohydrate transport to sink tissues and an increase of malondialdehyde (MDA). The negative effect on reproductive development was more pronounced under waterlogged soil.
ISSN:0971-5894
0974-0430
DOI:10.1007/s12298-020-00845-8