Department of Botany, Washington State University, Pullman, Wash.
Planta. 1967 Dec;74(4):350-67. doi: 10.1007/BF00389093.
Microautoradiographic techniques were used to determine the distribution of Ca(45) and S(35) in regions of the bean root where anatomical features may influence the processes of ion uptake and translocation. Root tissue from intact plants was prepared by methods that preserve both soluble and insoluble Ca and S. Ca(45) distribution was determined after 1 hour and 15 min, of uptake, after 2 efflux periods, and after replacement by non-tracer Ca.S(35) distribution was determined after 1 hour and 15 min of uptake.The quantity of Ca(45) that entered the root was greater than the quantity of S(35). Ca(45) concentration within the root increased with linear distance from the 8-mm level behind the tip. The pathways of Ca and S across the cortex appeared to be different since Ca(45) was particularly associated with cell walls and S(35) was distributed more evenly through the cells. There was no evidence that the endodermis was a diffusion barrier for Ca; the small parenchyma cells associated with conducting elements acquired a high concentration of Ca(45) and thus appear to be implicated in absorption and perhaps in transfer to the xylem. The evidence suggests that the endodermis may have been a barrier for S, but if so, certain parenchyma cells inside the stele, especially at xylem poles, were equally involved. The region from 30 to 80 mm from the tip appeared to participate in Ca uptake and transfer to the xylem; because of tissue immaturity the 8-mm region, which contained the least Ca(45), was thought not to translocate to the shoot. Deposition of Ca(45) in oxalate crystals represented almost complete immobilization. Calcium oxalate metabolism was most active in the 30-mm region of secondary roots and in their small branches. S(35)-labelled nuclei occurred in the cortex 2.5 to 3 mm behind the root tip.
采用显微放射自显影技术来确定 Ca(45)和 S(35)在菜豆根中分布的位置,这些位置的解剖学特征可能影响离子吸收和转运过程。通过既能保存可溶性钙和硫又能保存不溶性钙和硫的方法来制备完整植株的根组织。在吸收 1 小时 15 分钟后、2 次外排期后以及用非示踪 Ca 取代后,测定 Ca(45)的分布。在吸收 1 小时 15 分钟后,测定 S(35)的分布。进入根中的 Ca(45)数量大于 S(35)的数量。根内 Ca(45)浓度随距离根尖 8mm 后沿皮层线性增加。Ca 和 S 穿越皮层的途径似乎不同,因为 Ca(45)与细胞壁特别相关,而 S(35)在细胞中分布更为均匀。没有证据表明内皮层是 Ca 的扩散屏障;与导性组织有关的小薄壁细胞获得了 Ca(45)的高浓度,因此似乎与吸收有关,或许与向木质部转移有关。有证据表明,内皮层可能是 S 的屏障,但如果是这样,木质部内的某些中柱薄壁细胞,特别是在木质部极点,同样参与其中。从根尖到 30-80mm 的区域似乎参与 Ca 的吸收和向木质部的转移;由于组织不成熟,认为包含最少 Ca(45)的 8mm 区域不会转运到地上部分。Ca(45)在草酸晶体中的沉积几乎代表了完全的固定化。在次生根的 30mm 区域及其小分枝中,Ca 草酸代谢最为活跃。S(35)标记的核出现在根尖后 2.5-3mm 的皮层中。