Norisada Mariko, Hara Masashi, Yagi Hisayoshi, Tange Takeshi
Asian Natural Environmental Science Center, The University of Tokyo, Japan.
Tree Physiol. 2005 Nov;25(11):1447-55. doi: 10.1093/treephys/25.11.1447.
In many temperate evergreen plant species, reductions in turgor loss point of leaves (Psi(tlp)) and leaf osmotic potential at full turgor (pi(sat)) occur from late summer to winter. To test the hypothesis that this seasonal change in leaf water relations is driven by root temperature, we manipulated the temperature of the roots and shoots of Cryptomeria japonica D. Don seedlings separately. Whole-plant warming diminished the seasonal changes in shoot water relations observed in the control plants, whereas shoot warming did not. Compared with the controls, root warming diminished the change in Psi(tlp) but not in pi(sat), whereas cooling accelerated the seasonal changes in shoot water relations. These results indicate that: (1) temperature responses of roots are involved in the seasonal changes in Psi(tlp) from late summer to winter; and (2) root temperature is partly responsible for the simultaneous changes in pi(sat). Whole-plant cooling caused increased root hydraulic resistance, suggesting that seasonal changes in shoot water relations represent adaptive responses to increased root hydraulic resistance at low root temperatures.
在许多温带常绿植物物种中,叶片膨压丧失点(Ψ(tlp))和完全膨压下的叶片渗透势(π(sat))从夏末到冬季都会降低。为了验证叶片水分关系的这种季节性变化是由根温度驱动的这一假设,我们分别对日本柳杉幼苗的根和地上部分的温度进行了调控。整株升温减少了对照植株中观察到的地上部分水分关系的季节性变化,而地上部分升温则没有。与对照相比,根升温减少了Ψ(tlp)的变化,但没有减少π(sat)的变化,而降温则加速了地上部分水分关系的季节性变化。这些结果表明:(1)根的温度响应参与了从夏末到冬季Ψ(tlp)的季节性变化;(2)根温度部分导致了π(sat)的同步变化。整株降温导致根水力阻力增加,这表明地上部分水分关系的季节性变化代表了对低根温度下根水力阻力增加的适应性反应。