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首页> 外文期刊>Plant Science: An International Journal of Experimental Plant Biology >Oxygen isotope enrichment in rice (Oryza sativa L.) grain organic matter captures signature of relative humidity
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Oxygen isotope enrichment in rice (Oryza sativa L.) grain organic matter captures signature of relative humidity

机译:氧气同位素富集水稻(Oryza sativa L.)谷物有机物捕获相对湿度的特征

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摘要

The oxygen isotopic composition (delta O-18) of plant organic matter (OM) is primarily governed by the delta O-18 of source water (delta O-18(SW)) and climatic factor of relative humidity (RH). Among the cereals, the growth of rice plants is critically dependent on the water availability in the growth-environment. In the present study, we investigated the sensitivity of delta O-18 in the bulk organic matter of rice grains to RH of their growth-environment. Our experimental setup consisted of both glasshouse and field experiments, where eight genotypes were grown at RH levels ranging from 67% to 87%. The delta O-18 measured in bulk grain OM and source water was used to calculate the net oxygen isotopic enrichment (Delta O-18(oM)). Regression analysis of Delta O-18(oM) with RH demonstrated a significant relationship (r(2) = 0.96; p & 0.0001), thereby implying that the isotopic signature of evaporative conditions gets recorded in the rice grain OM. In addition, our study involved a separate experiment that monitored the degree of oxygen isotope enrichment in water samples extracted from different parts of the rice plant. For this purpose, we sampled four of the above eight genotypes along with three other rice genotypes that were grown in both open cultivation fields and glasshouse. Water present in the culms, leaves, and grains were extracted quantitatively. Isotopic analyses revealed progressive O-18 enrichment of the water in the culms and leaves and intermediate enrichment values of that in the grains. Based on the isotope data, we validated mechanistic models for prediction of delta O-18 of the leaf water and that of the plant carbohydrates. The model predictions were in close agreement with the experimental observations. The study provides insights into the rice plant's oxygen isotope systematics that build the foundation for future applications of the stable isotope technique to study the interactions between rice and environment.
机译:植物有机物(OM)的氧同位素组合物(Delta O-18)主要由源水(Delta O-18(SW))和相对湿度(RH)的气候因子来控制。在谷物中,水稻植物的生长尺寸依赖于生长环境中的水可用性。在本研究中,我们研究了Delta O-18在其生长环境中籽粒的块状有机物中的ΔO-18的敏感性。我们的实验设置包括玻璃室和田间实验,其中8种基因型在Rh水平范围为67%至87%。在散装谷物OM和源水中测量的δO-18用于计算净氧同位素富集(Delta O-18(OM))。随着RH的ΔO-18(OM)的回归分析证明了显着的关系(R(2)= 0.96; p& 0.0001),从而暗示蒸发条件的同位素特征在水稻颗粒OM中记录。此外,我们的研究涉及一种独立的实验,该实验是监测从水稻不同部位提取的水样中的氧同位素富集程度。为此目的,我们将四种上述八种基因型中的四种基因型进行了抽样,其中三种其他水稻基因型在开放的栽培领域和玻璃盆中种植。定量提取秆,叶子和晶粒中存在的水。同位素分析揭示了在秆中的水和叶片中的水和颗粒中的中间富集值的逐步o-18富集。基于同位素数据,我们验证了用于预测叶片水的δO-18的机制模型及植物碳水化合物的机械模型。模型预测与实验观察密切一致。该研究为水稻植物的氧同位素系统提供了深入,为稳定同位素技术的未来应用构建了基础,以研究水稻和环境之间的相互作用。

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