Purification effects show seed and root mucilage's ability to respond to changing rhizosphere conditions

Mucilage, a polysaccharide-containing hydrogel, is hypothesized to play a key role in the rhizosphere as a self-organized system because it may vary its supramolecular structure with changes in the surrounding solution. However, there is currently limited research on how these changes are reflected in the physical properties of real mucilage. This study examines the role of solutes in maize root, wheat root, chia seed, and flax seed mucilage in relation to their physical properties. Two purification methods, dialysis and ethanol precipitation, were applied to determine the purification yield, cation content, pH, electrical conductivity, surface tension, viscosity, transverse ¹H relaxation time, and contact angle after drying of mucilage before and after purification. The two seed mucilage types contain more polar polymers that are connected to larger assemblies via multivalent cation crosslinks, resulting in a denser network. This is reflected in higher viscosity and water retention ability compared to root mucilage. Seed mucilage also contains fewer surfactants, making them better wettable after drying compared to the two root mucilage types. The root mucilage types, on the other hand, contain smaller polymers or polymer assemblies and become less wettable after drying. However, wettability not only depends on the amount of surfactants but also on their mobility, as well as the strength and mesh size of the network structure. The changes in physical properties and cation composition observed after ethanol precipitation and dialysis suggest that the polymer network of seed mucilage is more stable and specialized in protecting the seeds from unfavorable environmental conditions. In contrast, root mucilage is characterized by fewer cationic interactions and its network relies more on hydrophobic interactions. This allows root mucilage to be more flexible in responding to changing environmental conditions, facilitating nutrient and water exchange between root surfaces and the rhizosphere soil.     

High Molecular Weight Organic Compounds in the Xylem Sap of Mangroves: Implications for Long-Distance Water Transport

The rise of sap in mangroves has puzzled plant physiologists for many decades. The current consensus is that negative pressures in the xylem exist which are sufficiently high to exceed the osmotic pressure of seawater (2.5 MPa). This implies that the radial reflection coefficients of the mangrove roots are equal to unity. However, direct pressure probe measurements in xylem vessels of the roots and stems of mangrove (Rhizophora mangle) grown in the laboratory or in the field yielded below-atmospheric, positive (absolute) pressure values. Slightly negative pressure values were recorded only occasionally. Xylem pressure did not change significantly when the plants were transferred from tap water to solutions containing up to 1700 mOsmol kg^?1 NaCl. This indicates that the radial reflection coefficient of the roots for salt, and therefore the effective osmotic pressure of the external solution, was essentially zero as already reported for other halophytes. The low values of xylem tension measured with the xylem pressure probe were consistent with previously published data obtained using the vacuum/leafy twig technique. Values of xylem tension determined with these two methods were nearly two orders of magnitude smaller than those estimated for mangrove using the pressure chamber technique (?3 to ?6MPa). Xylem pressure probe measurements and staining experiments with alcian blue and other dyes gave strong evidence that the xylem vessels contained viscous, mucilage- and/or protein-related compounds. Production of these compounds resulting from wound or other artifactual reactions was excluded. The very low sap flow rates of about 20–50 cm h^?1 measured in these mangrove plants were consistent with the presence of high molecular weight polymeric substances in the xylem sap. The presence of viscous substances in the xylem sap of mangroves has the following implications for traditional xylem pressure measurement techniques, development of xylem tension, and longdistance water transport: (1) high external balancing pressures in the pressure chamber are needed to force xylem sap to the cut surface of the twig; (2) stable tensions much larger than 0.1 MPa can be developed only occasionally because viscous solutions provide nucleation sites for gas bubble formation; (3) the frequent presence of small gas bubbles in viscous solutions allows water transport by interfacial, gravity-independent streaming at gas/water interfaces and (4) the increased density of viscous solutions creates (gravity-dependent) convectional flows. Density-driven convectional flows and interfacial streaming, but also the very low radial reflection coefficient of the roots to NaCl are apparently the means by which R. mangle maintains water transport to its leaves despite the high salinity of the environment.     

Root Cap Mucilage and Extracellular Calcium as Modulators of Cellular Growth in Postmitotic Growth Zones of the Maize Root Apex*

Abstract: The control of maize root growth by root cap mucilage and extracellular calcium (Ca) was examined. Special attention was paid to the influence of these factors on cellular aspects of root growth, such as cell shape and organization of the microtubular (MT) cytoskeleton. Externally supplied Ca impaired the transition of early post-mitotic cells from a more-or-less apolar mode of expansion to a strictly anisotropic mode of elongation accompanied by their more rapid growth. However, this inhibitory effect of Ca was not associated with any re-arrangement of the cortical MTs, their transverse arrays, with respect to the root axis, being maintained under these conditions. Root mucilage, collected from donor root caps and placed around root tips, exerted a similar effect on cell shapes as did externally supplied Ca. In contrast, roots grown in a medium of low Ca content, or from which the root cap mucilage was continually removed, had more elongated cell shapes in their post-mitotic growth regions when compared to the control roots. These findings are consistent with a notion that Ca is present in the root cap mucilage in physiologically relevant amounts and can mediate growth responses in both the PIG region and the apical part of the elongation zone. Integrating several known effects of Ca ions on growth at the root apex, a hypothesis is proposed that a Ca-mediated and MT-independent control of cell growth in the PIG region might be involved in morphogenetic root movements (e.g. gravitropism), and that root growth responses could be initiated by an asymmetric distribution of extracellular calcium, or root cap slime, around the growing root tip.     

DEVELOPMENT OF MUCILAGINOUS SURFACES IN EUGLENOIDS. I. STALK MORPHOLOGY OF COLACIUM MUCRONATUM1

The envelope and stalk of Colacium mucronatum Bourr. & Chad, were examined in living cells with light microscopy and in fixed preparations with scanning electron microscopy using critically point dried (CPD) and freeze dried (FD) preparations. The envelope of palmelloid cells is formed over the entire cell surface by many individual strands attached at right angles to areas of articulation of the pellicular strips. Strands were observed to anastomose on the posterior tip of otherwise naked cells. Stalks of living cells in India ink preparations had an optically dark inner core with a lighter outer sheath. In FD stalks a definite inner core was not evident, whereas CPD stalks had an outer surface composed of thick strands which may be the collapsed and aggregated strands of the FD stalks. In both there was also an amorphous matrix. The stalk forms from the aggregation of many strands from the anterior cell tip back to a point encompassing the cell surface anterior to a cross section of the tip 9 μm diam. The outer surface of the stalk comes from the pellicular surface joining that area and the core from the cell tip in the area of the canal opening. Any possible participation of the inner canal surface in stalk formation could not be determined because of the great density of the mucilage at the cell-tip/stalk junction.     

Isolation and partial characterization of components of Prunus avium L. styles,including an antigenic glycoprotein associated with a self-incompatibility genotype

Several components of buffer extracts of Prunus avium L. styles (cv. Lambert, S ₃ S ₄) have been isolated and partially characterized: the major component is a glycoprotein (molecular weight approx. 90,000; 95% protein, 5.4% carbohydrate). A sticky uronic-acid-containing component and an arabinogalactan are also present. Two minor components are an antigenic glycoprotein associated with the self-incompatibility genotype (Antigen S) and a component found in styles of all Prunus species (Antigen P). The isolated glycoproteins have a substantial carbohydrate content (Antigen P 17.2%; Antigen S 16.3%), and have apparent molecular weights of 32,000 (Antigen P) and 37,000–39,000 (Antigen S). They are antigenically quite distinct. Material corresponding to Antigen S is secreted into the medium of suspension-cultured callus cells raised from both leaf and stem of P. avium.Abbreviations DEAE diethylaminoethyl - SDS-PAGE sodium dodecylsulphate-polyacrylamide gel electrophoresis     

Physiological characterization of the sex pheromone protoplast-release-inducing protein from the Closterium peracerosum-strigosum-littorale complex (Charophyta)

In the unicellular charophycean alga Closterium peracerosum‐strigosum‐littorale complex, the protoplast‐release‐inducing protein (PR‐IP), a sex pheromone responsible for gametic protoplast release from mating‐type minus (mt^–) cells, was found to stimulate secretion of mucilage from the cells. Induction of sexual cell division by PR‐IP was also confirmed. Bioassays were used to determine the minimum doses required to induce these functions, revealing that 5 · 10^?16 M of PR‐IP stimulated mucilage secretion, and that 5 · 10^?10 M of PR‐IP were required for protoplast release. Exposure of the cells to 5 · 10^?11 M of PR‐IP resulted in the induction of sexual cell division as well as mucilage secretion. These results strongly suggest that PR‐IP is a multifunctional pheromone that independently promotes multiple steps in conjugation at the appropriate times through different induction mechanisms.     

PURIFICATION AND PROPERTIES OF THE MUCUS OF EUGLENA GRACILIS (EUGLENOPHYCEAE)1

Anionic groups were demonstrated in the mucus of Euglena gracilis Klebs var. bacillaris Cori by histochemical staining with alcian blue or diaminobenzidine tetrahydrochloride and were quantified during the growth cycle with an alcian blue dye-binding assay. Mucus in the culture increased during growth and became high when the culture entered the stationary phase. Cultures were grown under conditions which uniformly labeled all sulfur containing compounds with ³⁵S. A purification scheme was devised using 0.15 M NaCl and 0.10 M EDTA at pH 8 (Marmur's solution) to separate the mucus from the cells without cell breakage. The isolated purified mucus was fractionated with sodium dodecyl sulfate (SDS) at 100° C into soluble and insoluble components. The soluble fraction was separated by SDS polyacrylamide gel electrophoresis into 18 polypeptide bands ranging from 22 to 320 kdaltons that stained with Coomassie blue; 16 of these bands also stained for carbohydrates using periodic acid-Schiffs reagent, indicating their glycoprotein nature. On hydrolysis, the SDS soluble fraction yielded xylose, fucose, rhamnose, and hexose. The SDS insoluble fraction contained no ³⁵S label, and, therefore, presumably no protein or bound sulfate; this gelatinous material does not contain the same sugar residues as the glycoproteins in the SDS soluble fraction. Its staining properties with alcian blue and its resistance to hydrolysis suggested the presence of uronic acids. Comparison with other Euglena fractions showed that bands comigrating with the mucus glycoproteins were not detectable in the fractions containing the whole cells or the culture medium. Although the mucus of Euglena yielded appreciable sulfate during mild acid treatment, most if not all of this sulfate appears to have come from the oxidation of reduced sulfur rather than from the hydrolysis of covalently bound sulfate. An infrared spectrum of the mucus showed only minor peaks in the correct regions for the S-O linkage. Thus, the mucus of Euglena is composed of glycoproteins and polysaccharides which contain little or no ester sulfate.     

Physical properties of axenic maize root mucilage

Root mucilage was collected from 3–4 day-old axenically-grown maize seedlings (Zea mays L. cv. Freya). The water potential of the hydrated mucilage was measured by thermocouple psychrometry and the rheology at low deformation rates was studied using an oscillating cone and plate rheometer which provides information on both the elastic and viscous components of its behaviour. Water potential decreased as mucilage solute concentration increased, reaching a value of −60kPa at 1.2 mg mL⁻¹. At the lowest oscillation rate, the mucilage had a dynamic viscosity of 145 mPa s and behaved as a weak viscoelastic gel. After filtration to remove suspended root cap cells and other solid plant material, mucilage viscosity was reduced to 5–10 mPa s at low oscillation rates and the behaviour was that of a viscous liquid. The decrease in viscosity which occurs on filtration indicates that the root cap cells form an integral part of the gel system, either by interacting directly with each other or via the polysaccharide. Our observations provide further support for the idea that mucilage plays a major role in maintaining root-soil contact in the rhizosphere. This revised version was published online in June 2006 with corrections to the Cover Date.     

New approaches to studying chemical and physical changes in the rhizosphere: an overview

The past decade has seen the rapid development of new techniques that have revealed substantial changes in soil physical and chemical properties in the rhizosphere compared to the bulk soil. This brief overview focuses on some examples of recently developed, innovative techniques now available and indicates the technical developments required for the future. The development of non-invasive imaging allied with computed tomography has begun to allow the study of root systems in situ and the measurement of localized uptake of water. Further development is still required to disaggregate the simultaneous changes in bulk density and water content that may occur as roots occupy new soil volumes, but resolution of 0.1 mm is now feasible in scanning times of less than 1 h thereby allowing dynamic processes to be measured. Changes in surface tension and composition of solutions close to roots, and of pH, can now be measured with a variety of techniques. Temporal and spatial changes of pH can be measured with micro-electrodes and dye indicator/agar gel techniques have allowed quantitative estimates of H⁺ fluxes albeit in artificial systems. Novel micro-sampling techniques are under development to quantify rhizosphere changes. So far these techniques have rarely been applied in soils but innovative sampling and analytical techniques should soon allow such studies. This revised version was published online in June 2006 with corrections to the Cover Date.     

Ecophysiology of the hypotonic response in the salt-tolerant charophyte alga Lamprothamnium papulosum

The ecophysiology of the hypotonic response was studied in the charophyte alga, Lamprothamnium papulosum, which was grown in a marine (SW; 1072 mosmol kg^–1) and a brackish (1/2 SW; 536 mosmol kg^–1) environment. The cells produced an extracellular mucilage identified by histochemical staining as a mixture of sulphated and carboxylated polysaccharides. The thickness and chemical composition of the mucilage layer was a function of environmental salinity and cell age. Mucilage progressively increased in thickness from the apex (9 SW cells: 12·6 ± 1·8 μm; 15 1/2 SW cells: 4·8 ± 0·7 μm) to the base of the plants (15 SW cells: 44·8 ± 3·3 μm; nine 1/2 SW cells: 23·8 ± 2·5 μm); with a corresponding increase in the sulphated proportion. The mucilage was significantly thicker in SW plants. Hydraulic conductivity (Lp) at the apex of SW plants, measured by transcellular osmosis, was 8·3 × 10^–13 m s^–1 Pa^–1. This was close to Lp of freshwater Chara (8·5 × 10^–13 m s^–1 Pa^–1) which lacked mucilage. Basal SW cells with thicker mucilage had a smaller apparent Lp of 3·5 × 10^–13 m s^–1 Pa^–1. The electrophysiology of the resting state and hypotonic response was compared in cells from the two environments based on current/voltage (I/V) analysis. The resting potential difference (PD) and conductance differed (11 SW cells: – 102·4 ± 10·1 mV, eight SW cells: 18·6 ± 2·4 S m^–2; 19 1/2 SW cells: –125·7 ± 5·9 mV, 8·3 ± 0·8 S m^–2). The type of cellular response to a hypotonic shock (decrease of 268 mosmol kg^–1) also differed. In 1/2 SW plants, only the apical cells with thin mucilage responded classically with depolarization, conductance increase, Ca²⁺ influx, cessation of cytoplasmic streaming, and K⁺ and Cl^– effluxes. Older cells making up the bulk of the plants responded with depolarization, but continued cytoplasmic streaming, and had only a small increase in conductance; or depolarized transiently without altering the I/V profile, conductance or streaming speed. Most cells remained depolarized and in the K⁺ state 1 h post-shock. Cells treated with the K⁺ channel blocker tetraethylammonium chloride also depolarized and remained depolarized. The SW cells depolarized but otherwise responded minimally to a 268 mosmol kg^–1 drop in osmolarity and required a further 268 mosmol kg^–1 down-step to elicit a change in the conductance. A spectrum of responses was measured in successively older and more mucilaginous cells from the same marine plant. We discuss the ecophysiological significance of the mucilage layer which modulates the cellular response to osmotic shock and which can be secreted to different degrees by plants inhabiting environments of different salinity.