Griffiths Howard, Cousins Asaph B, Badger Murray R, von Caemmerer Susanne
Physiological Ecology Group, Department of Plant Sciences, University of Cambridge, Cambridge CB2 3EA, United Kingdom.
Plant Physiol. 2007 Feb;143(2):1055-67. doi: 10.1104/pp.106.088302. Epub 2006 Dec 1.
A model defining carbon isotope discrimination (delta13C) for crassulacean acid metabolism (CAM) plants was experimentally validated using Kalanchoe daigremontiana. Simultaneous measurements of gas exchange and instantaneous CO2 discrimination (for 13C and 18O) were made from late photoperiod (phase IV of CAM), throughout the dark period (phase I), and into the light (phase II). Measurements of CO2 response curves throughout the dark period revealed changing phosphoenolpyruvate carboxylase (PEPC) capacity. These systematic changes in PEPC capacity were tracked by net CO2 uptake, stomatal conductance, and online delta13C signal; all declined at the start of the dark period, then increased to a maximum 2 h before dawn. Measurements of delta13C were higher than predicted from the ratio of intercellular to external CO2 (p(i)/p(a)) and fractionation associated with CO2 hydration and PEPC carboxylations alone, such that the dark period mesophyll conductance, g(i), was 0.044 mol m(-2) s(-1) bar(-1). A higher estimate of g(i) (0.085 mol m(-2) s(-1) bar(-1)) was needed to account for the modeled and measured delta18O discrimination throughout the dark period. The differences in estimates of g(i) from the two isotope measurements, and an offset of -5.5 per thousand between the 18O content of source and transpired water, suggest spatial variations in either CO2 diffusion path length and/or carbonic anhydrase activity, either within individual cells or across a succulent leaf. Our measurements support the model predictions to show that internal CO2 diffusion limitations within CAM leaves increase delta13C discrimination during nighttime CO2 fixation while reducing delta13C during phase IV. When evaluating the phylogenetic distribution of CAM, carbon isotope composition will reflect these diffusive limitations as well as relative contributions from C3 and C4 biochemistry.
利用落地生根对一个定义景天酸代谢(CAM)植物碳同位素分馏(δ¹³C)的模型进行了实验验证。在光周期后期(CAM的IV期)、整个黑暗期(I期)以及进入光照期(II期)期间,同步测量了气体交换和瞬时CO₂分馏(针对¹³C和¹⁸O)。在整个黑暗期对CO₂响应曲线的测量揭示了磷酸烯醇式丙酮酸羧化酶(PEPC)能力的变化。PEPC能力的这些系统性变化通过净CO₂吸收、气孔导度和在线δ¹³C信号进行跟踪;所有这些在黑暗期开始时下降,然后在黎明前2小时增加到最大值。δ¹³C的测量值高于仅根据细胞间与外界CO₂的比率(p(i)/p(a))以及与CO₂水合和PEPC羧化相关的分馏所预测的值,使得黑暗期叶肉导度g(i)为0.044 mol m⁻² s⁻¹ bar⁻¹。需要更高的g(i)估计值(0.085 mol m⁻² s⁻¹ bar⁻¹)来解释整个黑暗期模拟和测量的δ¹⁸O分馏。来自两种同位素测量的g(i)估计值的差异,以及源水和蒸腾水的¹⁸O含量之间 -5.5‰ 的偏移,表明在单个细胞内或肉质叶片中,CO₂扩散路径长度和/或碳酸酐酶活性存在空间变化。我们的测量结果支持模型预测,表明CAM叶片内的内部CO₂扩散限制在夜间CO₂固定期间增加了δ¹³C分馏,而在IV期降低了δ¹³C。在评估CAM的系统发育分布时,碳同位素组成将反映这些扩散限制以及C3和C4生物化学的相对贡献。