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首页> 外文期刊>Phytochemistry >Temperature effect on leaf water deuterium enrichment and isotopic fractionation during leaf lipid biosynthesis: Results from controlled growth of C-3 and C-4 land plants
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Temperature effect on leaf water deuterium enrichment and isotopic fractionation during leaf lipid biosynthesis: Results from controlled growth of C-3 and C-4 land plants

机译:温度对叶脂生物合成过程中叶水氘富集和同位素分馏的影响:C-3和C-4陆地植物受控生长的结果

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The hydrogen isotopic ratios (H-2/H-1) of land plant leaf water and the carbon-bound hydrogen of leaf wax lipids are valuable indicators for climatic, physiological, metabolic and geochemical studies. Temperature will exert a profound effect on the stable isotopic composition of leaf water and leaf lipids as it directly influences the isotopic equilibrium (IE) during leaf water evaporation and cellular water dissociation. It is also expected to affect the kinetics of enzymes involved in lipid biosynthesis, and therefore the balance of hydrogen inputs along different biochemical routes. We conducted a controlled growth experiment to examine the effect of temperature on the stable hydrogen isotopic composition of leaf water and the biological and biochemical isotopic fractionations during lipid biosynthesis. We find, that leaf water H-2 enrichment at 20 degrees C is lower than that at 30 degrees C. This is contrary to the expectation that at lower temperatures leaf water should be more enriched in H-2 due to a larger equilibrium isotope effect associated with evapotranspiration from the leaf if all other variables are held constant. A hypothesis is presented to explain the apparent discrepancy whereby lower temperature-induced down-regulation of available aquaporin water channels and/or partial closure of transmembrane water channel forces water flow to "detour" to a more convoluted apoplastic pathway, effectively increasing the length over which diffusion acts against advection as described by the Peclet effect (Farquhar and Lloyd, 1993) and decreasing the average leaf water enrichment. The impact of temperature on leaf water enrichment is not reflected in the biological isotopic fractionation or the biochemical isotopic fractionation during lipid biosynthesis. Neither the biological nor biochemical fractionations at 20 degrees C are significantly different from that at 30 degrees C, implying that temperature has a negligible effect on the isotopic fractionation during lipid biosynthesis
机译:陆地植物叶水的氢同位素比(H-2 / H-1)和叶蜡脂质的碳结合氢是气候,生理,代谢和地球化学研究的重要指标。温度将直接影响叶水蒸发和细胞水解离过程中的同位素平衡(IE),对叶水和叶脂的稳定同位素组成产生深远影响。还预期它会影响参与脂质生物合成的酶的动力学,从而影响沿不同生化途径的氢输入的平衡。我们进行了受控生长实验,以研究温度对脂质水合成过程中叶水的稳定氢同位素组成以及生物和生化同位素分馏的影响。我们发现,在20摄氏度时叶片水的H-2富集低于在30摄氏度时的叶片。这与以下预期相反:由于更大的平衡同位素效应,在较低温度下叶片水应更富于H-2。如果所有其他变量保持不变,则与叶的蒸散量相关。提出了一个假设来解释明显的差异,即较低的温度诱导的可用水通道蛋白水通道的下调和/或跨膜水通道的部分关闭迫使水流“绕道”至更复杂的外质体途径,从而有效地增加了长度如Peclet效应(Farquhar和Lloyd,1993)所述,这种扩散对平流起反作用,并降低了平均叶片水分富集。温度对叶水富集的影响没有反映在脂质生物合成过程中的生物同位素分馏或生化同位素分馏中。 20摄氏度时的生物学和生物化学分馏均与30摄氏度时的生物学和生化分数均无显着差异,这表明温度在脂质生物合成过程中对同位素分馏的影响可忽略不计

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