向日葵根系水通道蛋白活性与苗龄关系的研究

利用压力室结合水通道蛋白抑制剂氯化汞(HgCl2)检测了不同苗龄(15d、25d和35d)向日葵根系水通道的活性,结果显示此生长期间根系导水率保持相对恒定,但0．1mmol／L氯化汞使所有苗龄根系的水流速率和根系导水率迅速降低,而降幅随根龄的增大而增大,表明向日葵根存在调节水分进入根系的水通道蛋白,其活性随根龄的增大而提高,质外体水流随根龄的增大而减小。结论是：在根系生长过程中,细胞到细胞途径水通道蛋白活性的提高可以补偿由于质外体途径导水度降低所致根系导水率的降低,从而维持根系导水率的相对稳定。     

植物质外体的研究方法

质外体是细胞之间的空间和细胞膜与细胞壁之间的微小空间通过细胞壁上的微孔连接而成的一个连续［１］。整株植物的质外体是连续的。它是养分运输的重要途径,并有贮存养分和活化养分的功能。因此,质外体在植物代谢中的作用倍受人们的重视。然而由于质外体在植物中所占的比例较小,它与膜内细胞质之间存在着水分与物质的平衡,从而给有关质外体的研究带来许多困难。近些年来,国际上在这方面的研究取得了一些进展。本文着重介绍目前在植物营养研究中几种常用的质外体研究方法。１植物地上部质外体的测定方法在质外体的研究中,根系质外体已…     

两种苹果砧木根系水力结构及其PV曲线水分参数对干旱胁迫的响应

研究干旱胁迫对平邑甜茶(Malus hupehensis)和楸子(Malus prunifolia)根系水力结构及其PV曲线水分参数的影响.设定正常与干旱2种水分处理,对2种苹果砧木进行氯化汞-巯基乙醇处理和压力室-容积(PV)曲线测定试验,并利用高压流速仪(HPFM),测定平邑甜茶和楸子根系水力结构.结果表明:随着水分胁迫的加重,平邑甜茶和楸子的根系导水率、根系叶比导水率、根系茎比导水率出现减少趋势.在适宜水分和重度干旱条件下,平邑甜茶根系叶比导水率分别为楸子根系叶比导水率的95％和92％,平邑甜茶根系茎比导水率分别为楸子根系茎比导水率的52％和62％,楸子与平邑甜茶相比在根系茎比导水率和根系叶比导水率上出现增加趋势.干旱胁迫可能会导致水通道蛋白的活性受到抑制,致使其根系导水率出现降低,继而导致了地上部分气体交换受到影响.严重干旱时,楸子与平邑甜茶相比可能具有更大的水孔蛋白表达量来抵御干旱胁迫.在2种水分条件下,楸子的初始质壁分离时的渗透势(ψstlp)、饱和含水时的渗透势(Ψssal)、初始质壁分离时的相对水含量(RWCtlp)、初始质壁分离时的相对渗透水含量(ROWCtlp)、组织细胞总体弹性模量(ε')值与平邑甜茶相比较均处于较低水平,束缚水含量(Va)值处在较高水平.对PV曲线水分参数进行隶属函数综合评价得出的△值为楸子大于平邑甜茶,平邑甜茶和楸子之间b值差异不明显.在适宜水分和重度干旱条件下楸子所体现出的输水策略优于平邑甜茶.PV曲线水分参数同苹果砧木根系的水力结构一样能够随着植物所处的环境做出相应的调整.对于PV曲线水分参数研究发现,楸子在膨压保持方面与平邑甜茶相比,其抗旱性优于平邑甜茶.     

干旱低磷胁迫对不同品种小麦根系导水率的影响

控制磷素水平,采用控制灌水量(正常供水、中度及重度干旱胁迫)的盆栽试验法,选择抗旱性小麦品种陕合6号(W1)和水分敏感型品种郑引1号(W2)为供试材料。用压力室法测定了三叶期的两品种小麦根系导水率(LPr)的变化规律。结果表明：陕合6号,在有磷正常供水处理( PH)下具有较高的导水率,干旱胁迫时LPr降低较少,且复水后有较强的恢复能力。郑引1号, PH的LPr值相对较小,干旱导致的根系导水率下降非常突出,复水后的恢复能力也较弱。另外,干旱胁迫对小麦苗期根系导水率的影响大于磷胁迫对其导水率的影响,且两品种小麦无磷止常供水处理(-PH)的LPr分别为 PH的31．9%和53．6％,即磷对前者LPr的影响大于后者。     

糖-质子的共运输和韧皮部的装入T.E.汉弗莱斯(Humphreys)

仅仅是在最近些年,植物生理学家才能够清楚地说明,叶子的绿色组织中合成的蔗糖是如何进入小叶脉的韧皮部并在那里浓缩的。蔗糖由绿色组织进入韧皮部的过程中,必须穿过两层膜和一个细胞间隙。首先,蔗糖在绿色组织细胞的细胞质中合成,并从那里穿过质膜进入质外体。质外体是植物无生命的细胞壁空间,它含有处于细胞壁的表面上和其间隙中的水溶液。蔗糖穿过绿色组织细胞的质膜时,就进入这个溶液。第二,蔗糖在质外体溶液中向韧皮部细胞扩散(不超过五个细胞直径的距离),并通过质膜被吸收进入这些细胞。在质外体内的蔗糖     

PV技术在研究细胞壁弹性调节上的应用

应用压力室测定PV曲线,然后用PV曲线推导、计算水分参数,称为PV技术。这一技术是植物水分生理研究中的重要手段之一,应用也相当广泛「’,”。它可以用于确定植物的相对含水量（RWC）、饱和渗透势（w”）、质外体水（I”。）、共质体水（1”。）、总体容积弹性模量（Ev）等”‘,并可用以阐明植物的渗透调节和植物对干旱的适应性卜”。近年来,植物水分生理研究领域内的学者们越来越意识到细胞壁弹性在维持细胞膨压中具有重要作用,在植物抗旱生理研究中也具有重要意义k－。‘。为此,根据有关资料和我们多年实验,总结出了弹性调节…     

干燥密罗木复水过程中光诱导蒸腾拉力变化与复水时间的关系

该文探讨了干燥脱水后的复苏植物密罗木(Myrothamnus flabellifolia)的复水速度和复水后不同时间下的木质部压力与植物对光-暗反应的关系。研究结果表明, 密罗木整株植物和离体枝条复水时水分在茎内的上升速度都很快, 10小时左右水分即可接近枝条的顶端。在植物复水初期, 木质部压力反应随着复水时间的延长不断增加, 3周后达到正常值。这种木质部压力的调节能力可能与气孔功能的恢复程度有关。同时, 密罗木在整个复水恢复过程中受到光照时木质部压力下降的弛豫时间都明显大于植物在光源关闭时木质部压力上升的弛豫时间。表明密罗木对蒸腾速率上升过程的调节速度明显低于对蒸腾速率下降过程的调节速度。     

植物钙素吸收和运转

近年来,钙素在植物体内的吸收和运输研究主要集中在细胞和分子水平,但整株水平上的研究也同样重要.整株水平上的钙吸收和运输包括根细胞的钙吸收、钙离子横向穿过根系并进入木质部、在木质部运输、从木质部移出并进入叶片或果实及在叶片或果实中运转分配等环节,既经过质外体也穿越共质体.钙离子通道、Ca2 -ATP酶和Ca2 /H 反向转运器等参与根细胞的钙吸收.在钙离子横向穿根进入木质部的过程中,需要穿越内皮层和木质部薄壁细胞组织.根系内皮层凯氏带阻挡了Ca2 沿质外体途径由内皮层外侧向内侧的移动,部分Ca2 由此通过离子通道流进内皮层细胞而转入共质体并到达木质部薄壁细胞组织,而由木质部薄壁细胞组织进入中柱质外体可能需要Ca2 -ATP酶驱动;还有一些Ca2 由内皮层细胞运出,沿内皮层内侧的质外体途径进入木质部导管,并通过导管运向枝干.钙离子以螯合态的形式在枝干导管运输;水流速率是影响钙离子沿导管运输的关键因子.钙离子在果实和叶片中的运输和分配不仅通过质外体途径也通过共质体途径.     

1株裂殖壶菌(Schizochytrium sp.的分离鉴定*

采用松树花粉诱集法从乐清湾红树林分离到一株纯培养物,其特点为:营养菌体为椭圆球形,单核;营养菌体的细胞壁由许多紧压在一起的致密鳞片层构成,在细胞壁不连续处可分辨鳞片;营养菌体形成外质网,它产生于外质网形成体;营养菌体以产生游动孢子行无性繁殖,游动孢子为双鞭毛;无性繁殖过程中形成四分体结构。据此鉴定为裂殖壶菌(Schizochytrium sp·)。     

1株裂殖壶菌(Schizochytrium sp.)的分离鉴定

采用松树花粉诱集法从乐清湾红树林分离到一株纯培养物,其特点为：营养菌体为椭圆球形,单核;营养菌体的细胞壁由许多紧压在一起的致密鳞片层构成,在细胞壁不连续处可分辨鳞片;营养菌体形成外质网,它产生于外质网形成体;营养菌体以产生游动孢子行无性繁殖,游动孢子为双鞭毛;无性繁殖过程中形成四分体结构。据此鉴定为裂殖壶菌（Schizochytrium sp．）。     

Water uptake by roots: effects of water deficit

The variable hydraulic conductivity of roots (Lp(r)) is explained in terms of a composite transport model. It is shown how the complex, composite anatomical structure of roots results in a composite transport of both water and solutes. In the model, the parallel apoplastic and cell-to-cell (symplastic and transcellular) pathways play an important role as well as the different tissues and structures arranged in series within the root cylinder (epidermis, exodermis, cortex, endodermis, stelar parenchyma). The roles of Casparian bands and suberin lamellae in the root's endo- and exodermis are discussed. Depending on the developmental state of these apoplastic barriers, the overall hydraulic resistance of roots is either more evenly distributed across the root cylinder (young unstressed roots) or is concentrated in certain layers (exo- and endodermis in older stressed roots). The reason for the variability of root Lp(r), is that hydraulic forces cause a dominating apoplastic flow of water around protoplasts, even in the endodermis and exodermis. In the absence of transpiration, water flow is osmotic in nature which causes a high resistance as water passes across many membranes on its passage across the root cylinder. The model allows for a high capability of roots to take up water in the presence of high rates of transpiration (high demands for water from the shoot). By contrast, the hydraulic conductance is low, when transpiration is switched off. Overall, this results in a non-linear relationship between water flow and forces (gradients of hydrostatic and osmotic pressure) which is otherwise hard to explain. The model allows for special root characteristics such as a high hydraulic conductivity (water permeability) in the presence of a low permeability of nutrient ions once taken up into the stele by active processes. Low root reflection coefficients are in line with the idea of some apoplastic bypasses for water within the root cylinder. According to the composite transport model, the switch from the hydraulic to the osmotic mode is purely physical. In the presence of heavily suberized roots, the apoplastic component of water flow may be too small. Under these conditions, a regulation of radial water flow by water channels dominates. Since water channels are under metabolic control, this component represents an 'active' element of regulation. Composite transport allows for an optimization of the water balance of the shoot in addition to the well-known phenomena involved in the regulation of water flow (gas exchange) across stomata. The model is employed to explain the responses of plants to water deficit and other stresses. During water deficit, the cohesion-tension mechanism of the ascent of sap in the xylem plays an important role. Results are summarized which prove the validity of the coehesion/tension theory. Effects of the stress hormone abscisic acid (ABA) are presented. They show that there is an apoplastic component of the flow of ABA in the root which contributes to the ABA signal in the xylem. On the other hand, (+)-cis-trans-ABA specifically affects both the cell level (water channel activity) and water flow driven by gradients in osmotic pressure at the root level which is in agreement with the composite transport model. Hydraulic water flow in the presence of gradients in hydrostatic pressure remains unchanged. The results agree with the composite transport model and resemble earlier findings of high salinity obtained for the cell (Lp) and root (Lp(r)) level. They are in line with known effects of nutrient deprivation on root Lp(r )and the diurnal rhythm of root Lp(r )recently found in roots of LOTUS.     

Review article. How does water get through roots?

On the basis of recent results with young primary maize roots, a model is proposed for the movement of water across roots. It is shown how the complex, 'composite anatomical structure' of roots results in a 'composite transport' of both water and solutes. Parallel apoplastic, symplastic and transcellular pathways play an important role during the passage of water across the different tissues. These are arranged in series within the root cylinder (epidermis, exodermis, central cortex, endodermis, pericycle stelar parenchyma, and tracheary elements). The contribution of these structures to the root's overall radial hydraulic resistance is examined. It is shown that as soon as early metaxylem vessels mature, the axial (longitudinal) hydraulic resistance within the xylem is usually not rate-limiting. According to the model, there is a rapid exchange of water between parallel radial pathways because, in contrast to solutes such as nutrient ions, water permeates cell membranes readily. The roles of apoplastic barriers (Casparian bands and suberin lamellae) in the root's endo- and exodermis are discussed. The model allows for special characteristics of roots such as a high hydraulic conductivity (water permeability) in the presence of a low permeability of nutrient ions once taken up into the stele by active processes. Low root reflection coefficients indicate some apoplastic by-passes for water within the root cylinder. For a given root, the model explains the large variability in the hydraulic resistance in terms of a dependence of hydraulic conductivity on the nature and intensity of the driving forces involved to move water. By switching the apoplastic path on or off, the model allows for a regulation of water uptake according to the demands from the shoot. At high rates of transpiration, the apoplastic path will be partially used and the hydraulic resistance of the root will be low, allowing for a rapid uptake of water. On the contrary, at low rates of transpiration such as during the night or during stress conditions (drought, high salinity, nutrient deprivation), the apoplastic path will be less used and the hydraulic resistance will be high. The role of water channels (aquaporins) in the transcellular path is in the fine adjustment of water flow or in the regulation of uptake in older, suberized parts of plant roots lacking a substantial apoplastic component. The composite transport model explains how plants are designed to optimize water uptake according to demands from the shoot and how external factors may influence water passage across roots.     

Control of water uptake by rice (<Emphasis Type="Italic">Oryza sativa</Emphasis> L.): role of the outer part of the root

A new pressure-perfusion technique was used to measure hydraulic and osmotic properties of the outer part of roots (OPR) of 30-day-old rice plants (lowland cultivar: IR64, and upland cultivar: Azucena). The OPR comprised rhizodermis, exodermis, sclerenchyma and one cortical cell layer. The technique involved perfusion of aerenchyma of segments from two different root zones (20-50 mm and 50-100 mm from the tip) at precise rates using aerated nutrient solution. The hydraulic conductivity of the OPR (Lp(OPR)=1.2x10(-6) m s(-1) MPa(-1)) was larger by a factor of 30 than the overall hydraulic conductivity (Lp(r)=4x10(-8) m s(-1) MPa(-1)) as measured by pressure chamber and root pressure probe. Low reflection coefficients were obtained for mannitol and NaCl for the OPR (sigma(sOPR)=0.14 and 0.09, respectively). The diffusional water permeability ( P(dOPR)) estimated from isobaric flow of heavy water was smaller by three orders of magnitude than the hydraulic conductivity (Lp(OPR)/ P(fOPR)). Although detailed root anatomy showed well-defined Casparian bands and suberin lamellae in the exodermis, the findings strongly indicate a predominantly apoplastic water flow in the OPR. The Lp(OPR) of heat-killed root segments increased by a factor of only 2, which is in line with the conclusion of a dominating apoplastic water flow. The hydraulic resistance of the OPR was not limiting the passage of water across the root cylinder. Estimations of the hydraulic properties of aerenchyma suggested that the endodermis was rate-limiting the water flow, although the aerenchyma may contribute to the overall resistance. The resistance of the aerenchyma was relatively low, because mono-layered cortical septa crossing the aerenchyma ('spokes') short-circuited the air space between the stele and the OPR. Spokes form hydraulic bridges that act like wicks. Low diffusional water permeabilities of the OPR suggest that radial oxygen losses from aerenchyma to medium are also low. It is concluded that in rice roots, water uptake and oxygen retention are optimized in such a way that hydraulic water flow can be kept high in the presence of a low efflux of oxygen which is diffusional in nature.     

Water uptake by plant roots: an integration of views

A COMPOSITE TRANSPORT MODEL is presented which explains the variability in the ability of roots to take up water and responses of water uptake to different factors. The model is based on detailed measurements of 'root hydraulics' both at the level of excised roots (root hydraulic conductivity, Lp_r) and root cells (membrane level; cell Lp) using pressure probes and other techniques. The composite transport model integrates apoplastic and cellular components of radial water flow across the root cylinder. It explains why the hydraulic conductivity of roots changes in response to the nature (osmotic vs. hydraulic) and intensity of water flow. The model provides an explanation of the adaptation of plants to conditions of drought and other stresses by allowing for a `coarse regulation of water uptake' according to the demands from the shoot which is favorable to the plant. Coarse regulation is physical in nature, but strongly depends on root anatomy, e.g. on the existence of apoplastic barriers in the exo- and endodermis. Composite transport is based on the composite structure of roots. A `fine regulation' results from the activity of water channels (aquaporins) in root cell membranes which is assumed to be under metabolic and other control.     

Aerenchyma Formed Under Phosphorus Deficiency Contributes to the Reduced Root Hydraulic Conductivity in Maize Roots

Root hydraulic conductivity has been shown to decrease under phosphorus （P） deficiency. This study Investigated how the formation of aerenchyma is related to this change. Root anatomy, as well as root hydraulic conductivity was studied In maize （Zea mays L.） roots under different phosphorus nutrition conditions. Plant roots under P stress showed enhanced degradation of cortical cells and the aerenchyma formation was associated with their reduced root hydraulic conductivity, supporting our hypothesis that air spaces that form in the cortex of phosphorusstressed roots Impede the radial transport of water in a root cylinder. Further evidence came from the variation In aerenchyma formation due to genotypic differences. Five maize inbred lines with different porosity in their root cortex showed a significant negative correlation with their root hydraulic conductivity. Shoot relative water content was also found lower In P-deficient maize plants than that in P-sufficient ones when such treatment was prolonged enough, suggesting a limitation of water transport due to lowered root hydraulic conductivity of P-deficient plants.     

Arbuscular mycorrhizal symbiosis increases relative apoplastic water flow in roots of the host plant under both well-watered and drought stress conditions

Background and Aims

The movement of water through mycorrhizal fungal tissues and between the fungus and roots is little understood. It has been demonstrated that arbuscular mycorrhizal (AM) symbiosis regulates root hydraulic properties, including root hydraulic conductivity. However, it is not clear whether this effect is due to a regulation of root aquaporins (cell-to-cell pathway) or to enhanced apoplastic water flow. Here we measured the relative contributions of the apoplastic versus the cell-to-cell pathway for water movement in roots of AM and non-AM plants.

Methods

We used a combination of two experiments using the apoplastic tracer dye light green SF yellowish and sodium azide as an inhibitor of aquaporin activity. Plant water and physiological status, root hydraulic conductivity and apoplastic water flow were measured.

Key Results

Roots of AM plants enhanced significantly relative apoplastic water flow as compared with non-AM plants and this increase was evident under both well-watered and drought stress conditions. The presence of the AM fungus in the roots of the host plants was able to modulate the switching between apoplastic and cell-to-cell water transport pathways.

Conclusions

The ability of AM plants to switch between water transport pathways could allow a higher flexibility in the response of these plants to water shortage according to the demand from the shoot.     

Transpiration difference under high evaporative demand in chickpea (Cicer arietinum L.) may be explained by differences in the water transport pathway in the root cylinder

• Terminal drought substantially reduces chickpea yield. Reducing water use at vegetative stage by reducing transpiration under high vapor pressure deficit (VPD), i.e. under dry/hot conditions, contributes to drought adaptation. We hypothesized that this trait could relate to differences in a genotype's dependence on root water transport pathways and hydraulics.
• Transpiration rate responses in conservative and profligate chickpea genotypes were evaluated under increasing VPD in the presence/absence of apoplastic and cell‐to‐cell transport inhibitors.
• Conservative genotypes ICC 4958 and ICC 8058 restricted transpiration under high VPD compared to the profligate genotypes ICC 14799 and ICC 867. Profligate genotypes were more affected by aquaporin inhibition of the cell‐to‐cell pathway than conservative genotypes, as measured by the root hydraulic conductance and transpiration under high VPD. Aquaporin inhibitor treatment also led to a larger reduction in root hydraulic conductivity in profligate than in conservative genotypes. In contrast, blockage of the apoplastic pathway in roots decreased transpiration more in conservative than in profligate genotypes. Interestingly, conservative genotypes had high early vigour, whereas profligate genotypes had low early vigour.
• In conclusion, profligate genotypes depend more on the cell‐to‐cell pathway, which might explain their higher root hydraulic conductivity, whereas water‐saving by restricting transpiration led to higher dependence on the apoplastic pathway. This opens the possibility to screen for conservative or profligate chickpea phenotypes using inhibitors, itself opening to the search of the genetic basis of these differences.

     

Chemical composition of apoplastic transport barriers in relation to radial hydraulic conductivity of corn roots (Zea mays L.)

The hydraulic conductivity of roots (Lp_r) of 6- to 8-d-old maize seedlings has been related to the chemical composition of apoplastic transport barriers in the endodermis and hypodermis (exodermis), and to the hydraulic conductivity of root cortical cells. Roots were cultivated in two different ways. When grown in aeroponic culture, they developed an exodermis (Casparian band in the hypodermal layer), which was missing in roots from hydroponics. The development of Casparian bands and suberin lamellae was observed by staining with berberin-aniline-blue and Sudan-III. The compositions of suberin and lignin were analyzed quantitatively and qualitatively after depolymerization (BF₃/methanol-transesterification, thioacidolysis) using gas chromatography/mass spectrometry. Root Lp_r was measured using the root pressure probe, and the hydraulic conductivity of cortical cells (Lp) using the cell pressure probe. Roots from the two cultivation methods differed significantly in (i) the Lp_r evaluated from hydrostatic relaxations (factor of 1.5), and (ii) the amounts of lignin and aliphatic suberin in the hypodermal layer of the apical root zone. Aliphatic suberin is thought to be the major reason for the hydrophobic properties of apoplastic barriers and for their relatively low permeability to water. No differences were found in the amounts of suberin in the hypodermal layers of basal root zones and in the endodermal layer. In order to verify that changes in root Lp_r were not caused by changes in hydraulic conductivity at the membrane level, cell Lp was measured as well. No differences were found in the Lp values of cells from roots cultivated by the two different methods. It was concluded that changes in the hydraulic conductivity of the apoplastic rather than of the cell-to-cell path were causing the observed changes in root Lp_r. Received: 17 March 1999 / Accepted: 22 June 1999     

Comparison between gradient-dependent hydraulic conductivities of roots using the root pressure probe: the role of pressure propagations and implications for the relative roles of parallel radial pathways

Hydrostatic pressure relaxations with the root pressure probe are commonly used for measuring the hydraulic conductivity (Lp(r)) of roots. We compared the Lp(r) of roots from species with different root hydraulic properties (Lupinus angustifolius L. 'Merrit', Lupinus luteus L. 'Wodjil', Triticum aestivum L. 'Kulin' and Zea mays L. 'Pacific DK 477') using pressure relaxations, a pressure clamp and osmotic gradients to induce water flow across the root. Only the pressure clamp measures water flow under steady-state conditions. Lp(r) determined by pressure relaxations was two- to threefold greater than Lp(r) from pressure clamps and was independent of the direction of water flow. Lp(r) (pressure clamp) was two- to fourfold higher than for Lp(r) (osmotic) for all species except Triticum aestivum where Lp(r) (pressure clamp) and Lp(r) (osmotic) were not significantly different. A novel technique was developed to measure the propagation of pressure through roots to investigate the cause of the differences in Lp(r). Root segments were connected between two pressure probes so that when root pressure (P(r)) was manipulated by one probe, the other probe recorded changes in P(r). Pressure relaxations did not induce the expected kinetics in pressure in the probe at the other end of the root when axial hydraulic conductance, and probe and root capacitances were accounted for. An electric circuit model of the root was constructed that included an additional capacitance in the root loaded by a series of resistances. This accounted for the double exponential kinetics for intact roots in pressure relaxation experiments as well as the reduced response observed with the double probe experiments. Although there were potential errors with all the techniques, we considered that the measurement of Lp(r) using the pressure clamp was the most unambiguous for small pressure changes, and provided that sufficient time was allowed for pressure propagation through the root. The differences in Lp(r) from different methods of measurement have implications for the models describing water transport through roots and the potential role of aquaporins.