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Rice Quality Deterioration due to Chalky-ring Formation Caused by Simultaneous Starch Biosynthesis Reduction with Osmotic Adjustment under Foehn-induced Dry Wind

机译:在Foehn引起的干风作用下,通过渗透调节同时减少淀粉的生物合成,导致稻米环形成而导致稻米品质下降

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摘要

Foehn-like extreme hot and dry wind conditions (34°C, >2.5 kPa vapor pressure deficit, and 7 m s−1) strongly affect grain quality in rice (Oryza sativa L.). This is a current concern because of the increasing frequency and intensity of combined heat and water-deficit stress under climate change. Foehn-induced dry wind conditions during the grain-filling stage increase ring-shaped chalkiness as a result of spatiotemporal reduction in starch accumulation in the endosperm, but kernel growth is sometimes maintained by osmotic adjustment. Here, we assess the effects of dry wind on chalky ring formation in environmentally controlled growth chambers. Our results showed that hot and dry wind conditions that lasted for >24 h dramatically increased chalky ring formation. Hot and dry wind conditions temporarily reduced panicle water potential to –0.65 MPa; however, kernel growth was maintained by osmotic adjustment at control levels with increased transport of assimilate to the growing kernels. Dynamic tracer analysis with a nano-electrospray-ionization Orbitrap mass spectrometer and quantitative polymerase chain reaction analysis revealed that starch degradation was negligible in the short-term treatment. Overall expression of starch synthesis-related genes was found to be down-regulated at moderately low water potential. Because the events observed at low water potential preceded the packing of starch granules in cells, we concluded that reduced rates of starch biosynthesis play a central role in the events of cellular metabolism that are altered at osmotic adjustment, which leads to chalky ring formation under short-term hot and dry wind conditions.
机译:类似于Foehn的极端热风和干风条件(34°C,> 2.5 kPa蒸气压亏空,和7 m s-1)强烈影响水稻(Oryza sativa L.)的谷粒品质。由于在气候变化下热与缺水的综合压力越来越大,强度和强度也越来越高,这引起了当前的关注。籽粒充实阶段,Foehn引起的干燥风条件增加了环状白垩度,这是胚乳中淀粉积累时空减少的结果,但有时通过渗透调节可以保持籽粒的生长。在这里,我们评估了干燥风对受环境控制的生长室中白垩环形成的影响。我们的结果表明,持续超过24小时的热风和干风条件显着增加了白垩环的形成。炎热和干燥的风力条件将穗水势暂时降低至–0.65 MPa;但是,通过在控制水平上进行渗透调节来保持籽粒的生长,同化物向生长中的籽粒的转运增加。使用纳米电喷雾电离Orbitrap质谱仪进行的动态示踪分析和定量聚合酶链反应分析表明,在短期处​​理中淀粉降解可忽略不计。发现淀粉合成相关基因的总体表达在中等低水势下被下调。因为在低水势下观察到的事件先于淀粉颗粒在细胞中堆积,所以我们得出结论,降低淀粉生物合成的速率在渗透调节下改变的细胞代谢事件中起着核心作用,这导致短时间内形成白垩环炎热和干燥风的条件。

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