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Effects of low atmospheric CO2 and elevated temperature during growth on the gas exchange responses of C3, C3–C4 intermediate, and C4 species from three evolutionary lineages of C4 photosynthesis

机译:低大气CO2 和生长过程中高温对来自三个进化谱系的C3 ,C3 –C4 中间体和C4 物种气体交换反应的影响C4 的光合作用

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This study evaluates acclimation of photosynthesis and stomatal conductance in three evolutionary lineages of C3, C3–C4 intermediate, and C4 species grown in the low CO2 and hot conditions proposed to favo r the evolution of C4 photosynthesis. Closely related C3, C3–C4, and C4 species in the genera Flaveria, Heliotropium, and Alternanthera were grown near 380 and 180 μmol CO2 mol−1 air and dayight temperatures of 37/29°C. Growth CO2 had no effect on photosynthetic capacity or nitrogen allocation to Rubisco and electron transport in any of the species. There was also no effect of growth CO2 on photosynthetic and stomatal responses to intercellular CO2 concentration. These results demonstrate little ability to acclimate to low CO2 growth conditions in closely related C3 and C3–C4 species, indicating that, during past episodes of low CO2, individual C3 plants had little ability to adjust their photosynthetic physiology to compensate for carbon starvation. This deficiency could have favored selection for more efficient modes of carbon assimilation, such as C3–C4 intermediacy. The C3–C4 species had approximately 50% greater rates of net CO2 assimilation than the C3 species when measured at the growth conditions of 180 μmol mol−1 and 37°C, demonstrating the superiority of the C3–C4 pathway in low atmospheric CO2 and hot climates of recent geological time.
机译:本研究评估了在低CO2和Sub中生长的C3 ,C3 –C4 中间和C4 物种的三个进化世系中光合作用和气孔导度的适应性。提出了有利于C4 光合作用进化的高温条件。 Flaveria,Heliotropium和Alternanthera属中紧密相关的C3 ,C3 –C4 和C4 物种生长在380和180μmolCO2 mol−附近。 1 空气和白天/晚上的温度为37/29°C。生长的二氧化碳对任何物种的光合作用能力或氮对Rubisco的分配和电子传递均没有影响。生长CO2 对细胞间CO2 浓度的光合和气孔响应也没有影响。这些结果表明,在紧密相关的C3 和C3 –C4 物种中,几乎没有能力适应低CO2 的生长条件,表明在过去的低CO2 ,单个C3 植物几乎没有能力调节其光合生理来补偿碳饥饿。这种缺陷可能有利于选择更有效的碳同化模式,例如C3 –C4 中介。在180μmolmol-1 –C4 物种的净CO2 同化率比C3 高约50%。 >和37°C时,证明了C3 –C4 途径在低大气CO2 和近地质时代的炎热气候中的优越性。

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