Fujikawa S, Kuroda K
Institute of Low Temperature Science, Hokkaido University, 060-0819, Sapporo, Japan.
Micron. 2000 Dec;31(6):669-86. doi: 10.1016/s0968-4328(99)00103-1.
Differential thermal analysis (DTA) has indicated that xylem ray parenchyma cells (XRPCs) of hardwood species adapt to freezing of apoplastic water either by deep supercooling or by extracellular freezing, depending upon the species. DTA studies indicated that moderately cold hardy hardwood species exhibiting deep supercooling in the XRPCs were limited in latitudinal distribution within the -40 degrees C isotherm, while very hardy hardwood species exhibiting extracellular freezing could distribute in colder areas beyond the -40 degrees C isotherm. Predictions based on the results of DTA, however, indicate that XRPCs exhibiting extracellular freezing may appear not only in very hardy woody species native to cold areas beyond the -40 degrees C isotherm but also in less hardy hardwood species native to tropical and subtropical zones as well as in a small number of moderately hardy hardwood species native to warm temperate zones. Cryo-scanning electron microscopic (cryo-SEM) studies on the freezing behavior of XRPCs have revealed some errors in DTA. These errors are originated mainly due to the overlap between exotherms produced by freezing of water in apoplastic spaces (high temperature exotherms, HTEs) and exotherms produced by freezing of intracellular water of XRPCs by breakdown of deep supercooling (low temperature exotherms, LTEs), as well as to the shortage of LTEs produced by intracellular freezing of XRPCs. In addition, DTA results are significantly affected by cooling rates employed. Further, cryo-SEM observations, which revealed the true freezing behavior of XRPCs, changed the previous knowledge of freezing behavior of XRPCs that had been obtained by freeze-substitution and transmission electron microscopic studies. Cryo-SEM results, in association with results obtained from DTA that were reconfirmed or changed by observation using a cryo-SEM, revealed a clear tendency of the freezing behavior of XRPCs in hardwood species to change with changes in the temperature in the growing conditions, including both latitudinal and seasonal temperature changes. In latitudinal temperature changes, XRPCs in less hardy hardwood species native to tropical and subtropical zones exhibited deep supercooling to -10 degrees C, XRPCs in moderately hardy hardwood species native to temperate zones exhibited a gradual increase in the supercooling ability to -40 degrees C from warm toward cool temperate zones, and XRPCs in very hardy hardwood species native to boreal forests exhibited extracellular freezing via an intermediate form of freezing behavior between deep supercooling and extracellular freezing. In seasonal temperature changes, XRPCs in hardwood species native to temperate zones changed their supercooling ability from a relatively low degree in summer to a high degree in winter. XRPCs in hardwood species native to boreal forests changed their freezing behavior from deep supercooling to -10 degrees C in summer to extracellular freezing in winter. These results indicate that the freezing behavior of XRPCs in hardwood species tends to shift gradually from supercooling of -10 degrees C, to a gradual increase in the deep supercooling ability to -40 degrees C or less, and finally to extracellular freezing as a result of cold acclimation in response to both latitudinal and seasonal temperature changes. It is thought that these temperature-dependent changes in the freezing behavior of XRPCs in hardwood species are mainly controlled by changes in cell wall properties, although no distinct changes were detected by electron microscopic observations in cell wall organization between hardwood species or between seasons. Evidence of temperature-dependent changes in the freezing behavior of XRPCs in hardwood species provided by the results of studies using a cryo-SEM has indicated the need for further investigation to clarify cold acclimation-induced cell wall changes at the sub-electron microscopic level in order to understand the mechanisms of freezing adaptation.
差示热分析(DTA)表明,阔叶树种的木质部射线薄壁细胞(XRPCs)通过深度过冷或胞外结冰来适应质外体水的冻结,这取决于树种。DTA研究表明,在XRPCs中表现出深度过冷的中度抗寒阔叶树种在-40℃等温线内的纬度分布有限,而表现出胞外结冰的极抗寒阔叶树种可以分布在-40℃等温线以外的更寒冷地区。然而,基于DTA结果的预测表明,表现出胞外结冰的XRPCs不仅可能出现在-40℃等温线以外寒冷地区的极抗寒木本物种中,也可能出现在热带和亚热带地区的抗寒能力较弱的阔叶树种中,以及少数暖温带地区的中度抗寒阔叶树种中。对XRPCs冷冻行为的低温扫描电子显微镜(cryo-SEM)研究揭示了DTA中的一些误差。这些误差主要源于质外体空间中水结冰产生的放热峰(高温放热峰,HTEs)与深度过冷破坏导致的XRPCs细胞内水结冰产生的放热峰(低温放热峰,LTEs)之间的重叠,以及XRPCs细胞内结冰产生的LTEs不足。此外,DTA结果受所采用的冷却速率的显著影响。此外,cryo-SEM观察揭示了XRPCs的真实冷冻行为,改变了之前通过冷冻置换和透射电子显微镜研究获得的关于XRPCs冷冻行为的认识。cryo-SEM结果与通过cryo-SEM观察重新确认或改变的DTA结果相结合,揭示了阔叶树种中XRPCs的冷冻行为随着生长条件下温度的变化而变化的明显趋势,包括纬度和季节温度变化。在纬度温度变化中,热带和亚热带地区抗寒能力较弱的阔叶树种中的XRPCs表现出深度过冷至-10℃,温带地区中度抗寒阔叶树种中的XRPCs表现出随着从暖温带向寒温带的过渡,过冷能力逐渐增加至-40℃,而北方森林中极抗寒阔叶树种中的XRPCs通过深度过冷和胞外结冰之间的中间冷冻行为形式表现出胞外结冰。在季节温度变化中,温带地区阔叶树种中的XRPCs将其过冷能力从夏季的相对较低程度改变为冬季的较高程度。北方森林中阔叶树种中的XRPCs将其冷冻行为从夏季的深度过冷至-10℃改变为冬季的胞外结冰。这些结果表明,阔叶树种中XRPCs的冷冻行为倾向于逐渐从-10℃的过冷转变为深度过冷能力逐渐增加至-40℃或更低,最终由于对纬度和季节温度变化的冷驯化而转变为胞外结冰。据认为,阔叶树种中XRPCs冷冻行为的这些温度依赖性变化主要受细胞壁性质变化的控制,尽管在阔叶树种之间或季节之间的细胞壁组织中通过电子显微镜观察未检测到明显变化。cryo-SEM研究结果提供的阔叶树种中XRPCs冷冻行为的温度依赖性变化的证据表明,需要进一步研究以阐明冷驯化诱导的亚电子显微镜水平的细胞壁变化,以便理解冷冻适应机制。