Martre Pierre, Durand Jean-Louis, Cochard Herve
1 Unité d'Ecophysiologie des Plantes Fourragères, Institut National de la Recherche Agronomique, F-86 600 Lusignan, France.
New Phytol. 2000 May;146(2):235-247. doi: 10.1046/j.1469-8137.2000.00641.x.
Xylem maturation in elongating leaf blades of tall fescue (Festuca arundinacea) was studied using staining and microcasting. Three distinctive regions were identified in the blade: (1) a basal region, in which elongation was occurring and protoxylem (PX) vessels were functioning throughout; (2) a maturation region, in which elongation had stopped and narrow (NMX) and large (LMX) metaxylem vessels were beginning to function; (3) a distal, mature region in which most of the longitudinal water movements occurred in the LMX. The axial hydraulic conductivity (K ) was measured in leaf sections from all these regions and compared with the theoretical axial hydraulic conductivity (K ) computed from the diameter of individual inner vessels. K was proportional to K throughout the leaf, but K was about three times K . The changes in K and K along the leaf reflected the different stages of xylem maturation. In the basal 60 mm region, K was about 0.30±0.07 mmol s mm MPa . Beyond that region, K rapidly increased with metaxylem element maturation to a maximum value of 5.0±0.3 mmol s mm MPa , 105 mm from the leaf base. It then decreased to 3.5±0.2 mmol s mm MPa near the leaf tip. The basal expanding region was observed to restrict longitudinal water movement. There was a close relationship between the water deposition rate in the elongation zone and the sum of the perimeters of PX vessels. The implications of this longitudinal vasculature on the partitioning of water between growth and transpiration is discussed.
利用染色和微铸技术研究了高羊茅(Festuca arundinacea)伸长叶片中木质部的成熟过程。在叶片中确定了三个不同的区域:(1)基部区域,在此区域叶片正在伸长,原生木质部(PX)导管始终在发挥功能;(2)成熟区域,在此区域伸长停止,窄(NMX)和大(LMX)后生木质部导管开始发挥功能;(3)远端成熟区域,在此区域大部分纵向水分运动发生在LMX中。测量了所有这些区域叶片切片的轴向水力传导率(K),并与根据单个内部导管直径计算出的理论轴向水力传导率(K)进行比较。在整个叶片中,K与K成正比,但K约为K的三倍。K和K沿叶片的变化反映了木质部成熟的不同阶段。在基部60毫米区域,K约为0.30±0.07 mmol s mm MPa。在该区域之外,随着后生木质部元素的成熟,K迅速增加,在距叶基部105毫米处达到最大值5.0±0.3 mmol s mm MPa。然后在叶尖附近降至3.5±0.2 mmol s mm MPa。观察到基部扩展区域限制纵向水分运动。伸长区的水分沉积速率与PX导管周长总和之间存在密切关系。讨论了这种纵向维管系统对生长和蒸腾之间水分分配的影响。