Calcium and oxalate content of the leaves of Phaseolus vulgaris at different calcium supply in relation to calcium oxalate crystal formation

Soluble and insoluble oxalate and insoluble calcium were measured in the leaves of Phaseolus vulgaris. The plants were grown in nutrient solutions with two different concentrations of calcium. Two developmental stages of the leaves were studied. Although the content of insoluble calcium differs widely according to leaf age and growth conditions, the percentage bound in crystals is nearly the same in all cases. In the growing leaves, concentrations of total oxalate are independent of calcium supply, thus, showing that the known rise in numbers of crystals, and of cells containing them, is not induced via oxalate biosynthesis. Fully expanded leaves contain more oxalate when grown in a nutrient solution with higher calcium concentration. Amounts of oxalate in percent of dry weight are similar to those given in the literature for other legume leaves.     

Quantitative determination of calcium oxalate and oxalate in developing seeds of soybean (Leguminosae)

Developing soybean seeds accumulate very large amounts of both soluble oxalate and insoluble crystalline calcium (Ca) oxalate. Use of two methods of detection for the determination of total, soluble, and insoluble oxalate revealed that at +16 d postfertilization, the seeds were 24% dry mass of oxalate, and three-fourths of this oxalate (18%) was bound Ca oxalate. During later seed development, the dry mass of oxalate decreased. Crystals were isolated from the seeds, and X-ray diffraction and polarizing microscopy identified them as Ca oxalate monohydrate. These crystals were a mixture of kinked and straight prismatics. Even though certain plant tissues are known to contain significant amounts of oxalate and Ca oxalate during certain periods of growth, the accumulation of oxalate during soybean seed development was surprising and raises interesting questions regarding its function.     

天津盐渍化生境54种植物钙晶体与钙组分特征

植物钙包括游离态的Ca²⁺和结合态易溶、微溶和难溶于水的钙盐,而难溶于水的钙盐常会形成钙晶体.为了解盐渍化生境中不同生长型植物体内的钙状况,本文对天津市54种植物进行了钙晶体的镜检和钙组分的测定.结果表明： 在盐渍化生境中的54种植物体内,有38种植物体内镜检到较多的钙晶体,其中37种植物体内为以簇晶和方晶为主的草酸钙晶体,只在桑科的无花果叶片中观察到内含碳酸钙晶体的钟乳体.按生长型统计,落叶乔、灌木体内的草酸钙晶体较多,藤本植物体内的草酸钙晶体较少,而草本植物和常绿乔木体内未镜检到草酸钙晶体.同时,从乔木、灌木、藤本到草本,植物体内盐酸溶性钙含量逐渐减少而水溶性钙含量逐渐增多,且草本植物体内的水溶性钙含量显著高于乔木和灌木.在盐渍化生境中,植物体内的钙晶体和钙组分因生长型不同而有所差异,草酸钙在落叶乔、灌木抵御盐分胁迫中发挥着重要作用.     

堇菜叶片草酸钙晶体与水分维持的关系

随着全球气候变化加重,干旱强度和持续时间逐渐增加,严重影响植物生长和作物产量。喀斯特为典型的干旱和高钙生境,植物叶片富集大量的草酸钙晶体,而该晶体与植物耐旱性之间的关系并不清楚。该研究以喀斯特适生植物堇菜(Viola verecumda)为材料,土壤进行自然干旱,分析堇菜叶片的草酸钙晶体变化特征与水分之间的关系。结果表明:在土壤自然干旱条件下,堇菜主要通过细胞内束缚水的释放,维持细胞内水分平衡;而在干旱后期,叶片通过关闭气孔,将部分自由水转变为束缚水,防止水分流失。此外,草酸钙晶体的密度与束缚水含量具有极其显著的强正相关线性回归关系(r=0.825 3,P0.000 1),表明草酸钙晶体作为主要的束缚水物质。因此,堇菜植物在耐旱过程中可能协调草酸钙晶体和气孔的生理行为忍耐干旱胁迫。     

Accumulation of Oxalate in Tissues of Sugar-beet, and the Effect of Nitrogen Supply

In field-grown sugar-beet concentration of insoluble oxalatewas low in roots and high (about 12 per cent of ethanol insolublematerial) in leaves, and for a particular leaf the concentrationincreased continuously during its life. Of the insoluble oxalate,15–30 per cent was present as the magnesium salt and theremainder as the calcium salt. Oxalate contents of plants grownin culture solutions with nitrate as nitrogen source were similarto those of plants grown in soil, but when nitrogen was suppliedas ammonium sulphate or ammonium nitrate both soluble and insolubleoxalate were low. Plants grown in soil with regular additionsof ammonium sulphate or ammonium nitrate also had very low concentrationsof soluble oxalate although insoluble oxalate was only slightlylower than with nitrate nitrogen. Disks of root or leaf tissuewashed for several days in distilled water lost insoluble oxalatebut when washed in tap water insoluble oxalate increased morethan twofold. Addition of calcium and nitrate to the distilledwater caused an increase of insoluble oxalate, while additionof potassium caused a decrease. Use of ¹⁴C labelled oxalateand washing experiments showed that oxalate can be metabolizedby tissue disks and so is not necessarily a final product ofmetabolism. The accumulation of oxalate appears to be connectedwith the assimilation of nitrate and the preservation of thecation-anion balance of the plant.     

Medicago truncatula mutants demonstrate the role of plant calcium oxalate crystals as an effective defense against chewing insects

Calcium oxalate is the most abundant insoluble mineral found in plants and its crystals have been reported in more than 200 plant families. In the barrel medic Medicago truncatula Gaertn., these crystals accumulate predominantly in a sheath surrounding secondary veins of leaves. Mutants of M. truncatula with decreased levels of calcium oxalate crystals were used to assess the defensive role of this mineral against insects. Caterpillar larvae of the beet armyworm Spodoptera exigua Hübner show a clear feeding preference for tissue from calcium oxalate-defective (cod) mutant lines cod5 and cod6 in choice test comparisons with wild-type M. truncatula. Compared to their performance on mutant lines, larvae feeding on wild-type plants with abundant calcium oxalate crystals suffer significantly reduced growth and increased mortality. Induction of wound-responsive genes appears to be normal in cod5 and cod6, indicating that these lines are not deficient in induced insect defenses. Electron micrographs of insect mouthparts indicate that the prismatic crystals in M. truncatula leaves act as physical abrasives during feeding. Food utilization measurements show that, after consumption, calcium oxalate also interferes with the conversion of plant material into insect biomass during digestion. In contrast to their detrimental effects on a chewing insect, calcium oxalate crystals do not negatively affect the performance of the pea aphid Acyrthosiphon pisum Harris, a sap-feeding insect with piercing-sucking mouthparts. The results confirm a long-held hypothesis for the defensive function of these crystals and point to the potential value of genes controlling crystal formation and localization in crop plants.     

不同生态区域沙地建群种油蒿的钙组分特征

为探索同一物种在不同生态区域钙组分特征的差异,选择我国北方沙地重要建群种油蒿(Artemisia ordosica)为研究对象,采集了内蒙古杭锦旗、乌审旗、阿拉善左旗以及宁夏盐池县和陕西榆林市榆阳区不同沙地类型、不同生长阶段的油蒿样品,利用连续组分法测定分析了油蒿的钙组分特征.结果表明,在油蒿的不同器官中,叶水溶性钙和醋酸溶性钙均显著高于枝和根,叶与根盐酸溶性钙均显著高于枝.在不同生态区域,降水量较多的地区油蒿体内水溶性钙含量较多,降水量较少的地区油蒿体内盐酸溶性钙含量较高.分析得知,降水条件较好的地区较高的水溶性钙主要体现在油蒿的叶中,而降水条件较差的地区较高的盐酸溶性钙主要体现在油蒿的叶和根中.油蒿在不同生长阶段钙组分没有显著差异,但不同类型沙地上油蒿的钙组分却有显著差异.可见,不同生态区域的油蒿,生境条件越好体内水溶性钙含量越高,生境条件越差体内盐酸溶性钙含量越高.     

Medicago truncatula-derived calcium oxalate crystals have a negative impact on chewing insect performance via their physical properties

Plant structural traits often act as defenses against herbivorous insects, causing them to avoid feeding on a given plant or tissue. Mineral crystals of calcium oxalate in Medicago truncatula Gaertn. (Fabaceae) leaves have previously been shown to be effective deterrents of lepidopteran insect feeding. They are also inhibitors of conversion of plant material into insect body mass during or after consumption. Growth of beet armyworm, Spodoptera exigua Hübner (Lepidoptera: Noctuidae), larvae was correspondingly greater on calcium oxalate‐defective (cod) mutants of M. truncatula with lower levels of crystal accumulation. Data presented here show that insects feeding on M. truncatula leaves with calcium oxalate crystals experience greater negative effects on growth and mandible wear than those feeding on artificial diet amended with smaller amorphous crystals from commercial preparations. Commercial calcium oxalate can be added to insect artificial diet at levels up to 7.5‐fold higher than levels found in wild‐type M. truncatula leaves with minimal effect on insect growth or lepidopteran mandibles. These data suggest that negative impacts of calcium oxalate in the diet of larvae are due to physical factors, and not toxicity of the compound, as high levels of the commercial crystals are readily tolerated. In contrast to the dramatic physical effects that M. truncatula‐derived crystals have on insect mandibles, we could detect no damage to insect peritrophic gut membranes due to consumption of these crystals. Taken together, the data indicate that the size and shape of prismatic M. truncatula oxalate crystals are important factors in determining effects on insect growth. If manipulation of calcium oxalate is to be used in developing improved insect resistance in plants, then our findings suggest that controlling not only the overall amount, but also the size and shape of crystals, could be valuable traits in selecting desirable plant lines.     

Accumulation and interaction of calcium and manganese in Phytolacca americana

To further understand the hyperaccumulation of Mn, the present study investigated the accumulation of Ca and Mn and their interaction in Mn hyperaccumulator pokeweed (Phytolacca americana Linn.). Exogenous Ca was observed to have a distinctive impact on the Mn phytotoxicity and accumulation in pokeweed, but exogenous Mn had little influence on the accumulation of Ca. Both Ca and Mn accumulated in pokeweed were detected to be mainly in the form of oxalate. Investigation with SEM and TEM found there were two kinds of crystals in the leaves, Ca oxalate crystals and Mn-containing crystals. Further detection showed that there was no inclusion of Mn inside the Ca oxalate crystals, and that other elements, such as C, O and P, were present in the Mn-containing crystals. These results suggest that Ca oxalate crystals in pokeweed have no direct effect on the detoxification of Mn. In addition, the finding of element P and O in the Mn-containing crystals indicates that excess Mn could be deposited by phosphate, which could contribute to Mn accumulation and detoxification in pokeweed.     

Insolubilization of potassium chloride crystals in Tradescantia pallida

Summary. Calcium oxalate crystals are by far the most prevalent and widely distributed mineral deposits in higher plants. In Tradescantia pallida, an evergreen perennial plant widely used as an ornamental plant, calcium oxalate crystals occur in the parenchymal tissues of stem, leaf, and root, as well as in flower organs, in the form of either raphides or tetragonal prismatic crystals or both. Energy-dispersive X-ray analysis revealed that C, O, and Ca were the main elements; and K, Cl, and Si, the minor elements. Infrared and X-ray analyses of crystals collected from these tissues detected the coexistence of two calcium oxalate chemical forms, i.e., whewellite and weddellite, as well as calcite, opal, and sylvite. Here, we show for the first time the occurrence of epitaxy in mineral crystals of plants. Epitaxy, which involves the oriented overgrowth of one crystal onto a second crystalline substrate, might explain how potassium chloride (sylvite) – one of the most water-soluble salts – stays insoluble in crystal form when coated with a calcium oxalate epilayer. The results indicate the potential role of crystals in regulating the ionic equilibrium of both calcium and potassium ions. Correspondence and reprints: Departamento de Biodiversidad y Biología Experimental, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Pabellón 2, Ciudad Universitaria, C1428EGA, Ciudad de Buenos Aires, Argentina.     

Calcium oxalate crystals of some <Emphasis Type="Italic">Crataegus</Emphasis> (Rosaceae) species growing in Aegean region

In this study, Ca oxalate crystals were isolated from the leaves and X-ray diffraction identified them as weddelite in Crataegus pontica C. Koch, C. stevenii Polar., C. monogyna ssp. monogyna Jacq. in C. orientalis var. orientalis Pallas ex Bieb. both whewellite and weddelite crystals were found. Although there were some differences among the soluble and insoluble oxalate contents, they were not notable in the species of C. stevenii (10%; 18%), C. orientalis (12.4%; 15%), C. monogyna (12.9%; 13%), whereas in C. pontica the difference was so great with the lowest soluble (4%), and highest (28%) insoluble oxalate content. Crystals have tetragonal or prismatic shape in general but tetrahedral kinked and straight shapes were seen in C. orientalis, tetragonal aggregates in C. stevenii, and also pseudo-tetrahedral cordate (heart) shape were found in C. monogyna ssp. monogyna and C. pontica. As the crystal biomineralization is under genetic control, this characteristic hydration state of crystals of Crataegus orientalis var. orientalis must be important for systematic phylogenetics.     

Isolation of a crystal matrix protein associated with calcium oxalate precipitation in vacuoles of specialized cells

The formation of calcium (Ca) oxalate crystals is considered to be a high-capacity mechanism for regulating Ca in many plants. Ca oxalate precipitation is not a stochastic process, suggesting the involvement of specific biochemical and cellular mechanisms. Microautoradiography of water lettuce (Pistia stratiotes) tissue exposed to 3H-glutamate showed incorporation into developing crystals, indicating potential acidic proteins associated with the crystals. Dissolution of crystals leaves behind a crystal-shaped matrix "ghost" that is capable of precipitation of Ca oxalate in the original crystal morphology. To assess whether this matrix has a protein component, purified crystals were isolated and analyzed for internal protein. Polyacrylamide gel electrophoresis revealed the presence of one major polypeptide of about 55 kD and two minor species of 60 and 63 kD. Amino acid analysis indicates the matrix protein is relatively high in acidic amino acids, a feature consistent with its solubility in formic acid but not at neutral pH. 45Ca-binding assays demonstrated the matrix protein has a strong affinity for Ca. Immunocytochemical localization using antibody raised to the isolated protein showed that the matrix protein is specific to crystal-forming cells. Within the vacuole, the surface and internal structures of two morphologically distinct Ca oxalate crystals, raphide and druse, were labeled by the antimatrix protein serum, as were the surfaces of isolated crystals. These results demonstrate that a specific Ca-binding protein exists as an integral component of Ca oxalate crystals, which holds important implications with respect to regulation of crystal formation.     

The solubility of calcium oxalate in tissue culture media

The equilibrium parameters for calcium oxalate solubility in tissue culture media were investigated because of the current interest in oxalate toxicity. The calcium selective ion electrode methodology was evaluated and calcium concentrations from potentiometric calculations were verified by d-c argon plasma emission spectroscopy. The experimental K(sp)'s at 25 degrees C for Dulbecco's modified Eagle media and McCoys 5A media are equivalent to the literature K(sp) of 2.3 x 10(-9) for low ionic strength. The equilibrium concentration products, [Ca2+] [C2O2-(4)], are ten times higher than the K(sp)'s due to the high ionic strengths of tissue culture media. At 37 degrees C, addition of soluble oxalate at the 10(-3) to 10(-4) M level causes >50% precipitation of the oxalate resulting in equilibrium oxalate concentrations of less than 6 x 10(-5) M. This relatively inexpensive selective ion technique allows the determination of oxalate concentrations in equilibrium-saturated media which are substantially less than those calculated by the amount of soluble oxalate added to the media.     

Calcium fertilization increases the concentration of calcium in sapwood and calcium oxalate in foliage of red spruce

Calcium cycling plays a key role in the health and productivity of red spruce forests in the northeastern US. A portion of the flowpath of calcium within forests includes translocation as Ca²⁺ in sapwood and accumulation as crystals of calcium oxalate in foliage. Concentrations of Ca in these tree tissues have been used as markers of environmental change due to acidic deposition or forest management practices. We compared the effects of Ca fertilization treatment on Ca concentration in wood and Ca and oxalate (Ox) concentration in foliage at two locations with different initial concentrations of Ca in the soil. We found greater amounts of Ca in wood from the high-Ca location than from the low-Ca location. Ca concentration was greater in wood formed in the 1970s than for wood formed in the 1980s, the outermost decadal band in these samples. The Ca-treatment was detected as an increased concentration of Ca in the 1970s and 1980s decadal bands. We also found that variation in Ca and Ox in foliage was essentially stoichiometric. The appearance and response to chemical tests of crystals in foliage were consistent with identification as calcium oxalate. The increased Ca in wood after Ca-treatment of the soil supports the use of dendrochemistry of base cations to investigate environmental change. However, differences in Ca concentration between the two outermost decadal bands of wood illustrate that internal processes of translocation and storage also affect Ca concentration. Calcium oxalate production in foliage diverts carbon from ordinary biosynthesis and energy-yielding processes. This sequestration, shedding, and decomposition of foliage may represent a significant and under-recognized contribution to carbon and Ca cycling.     

Some effects of varied calcium nutrition on the growth and composition of tomato plants

Summary Tomato plants were grown in nutrient solutions containing 0.05, 0.2, 1.0, 5.0, 15.0 and 30.0 meq Ca/l. Plants grown at the lowest level of calcium suffered from calcium deficiency and produced the least amount of dry matter. Dry matter yield was optimal from plants grown in the solution containing only 0.2 meq Ca/l and decreased at higher levels of substrate calcium. Despite large differences in the concentrations of the individual ions in the dried material, highly significant (P < 0.001) relationships were found between total cations and total anions and between insoluble calcium and oxalate.An explanation for the observed response to calcium is suggested based on the stimulation of the synthesis of oxalate by tissue calcium at the expense of carbohydrates. re]19760812     

Oxalate balance in fat sand rats feeding on high and low calcium diets

Oxalate reduces calcium availability of food because it chelates calcium, forming the sparingly soluble salt calcium-oxalate. Nevertheless, fat sand rats (Psammomys obesus; Gerbillinae) feed exclusively on plants containing much oxalate. We measured the effects of calcium intake on oxalate balance by comparing oxalate intake and excretion in wild fat sand rats feeding on their natural, oxalate-rich, calcium-poor diet with commercially-bred fat sand rats feeding on an artificial, calcium-rich, oxalate-poor diet of rodent pellets. We also tested for the presence of the oxalate degrading bacterium Oxalobacter sp. in the faeces of both groups. Fat sand rats feeding on saltbush ingested significantly more oxalate than fat sand rats feeding on pellets (P < 0.001) and excreted significantly more oxalate in urine and faeces (P < 0.01 for both). However the fraction of oxalate recovered in excreta [(oxalate excreted in urine + oxalate excreted in faeces)/oxalate ingested] was significantly higher in pellet-fed fat sand rats (61%) than saltbush-fed fat sand rats (27%). We found O. sp. in the faeces of both groups indicating that fat sand rats harbor oxalate degrading bacteria, and these are able, to some extent, to degrade oxalate in its insoluble form.     

Heavy metal stress reduces the deposition of calcium oxalate crystals in leaves of Phaseolus vulgaris

Calcium oxalate (CaOx) crystals in plants may serve as a sink for the absorption of excess calcium, and they could play an important role in heavy metal detoxification. In this study, the effect of heavy metals and different calcium concentrations on the growth of calcium oxalate crystals in leaves of Phaseolus vulgaris was investigated. Different analytical techniques were used to determine the influence of exogenous lead and zinc on CaOx deposition and to detect a presence of these metals in CaOx crystals. We found a positive correlation between the calcium concentration in the nutrient medium and the production of calcium oxalate crystals in leaves of hydroponically grown plants. On the other hand, addition of the heavy metals to the nutrient medium decreased the number of crystals. Energy dispersive X-ray spectrometry did not detect the inclusion of heavy metals inside the CaOx crystals. Our investigation suggests that CaOx crystals do not play a major role in heavy metal detoxification in P. vulgaris but do play an important role in bulk calcium regulation.     

Partitioning of Soluble Calcium in the Water Hyacinth (Eichhornia crassipes (Martius) Solms) in Lake Victoria,Uganda

Abstract: An investigation of soluble calcium partitioning in organs of the water hyacinth growing along the shores of L. Victoria, bordering Jinja town was carried out. The levels of Na⁺, K⁺, Mg²⁺ and Ca²⁺ in the lake water were also estimated. The pH and electrical conductivity of lake water were determined. There was a differential accumulation of Ca and oxalate between component organs of the water hyacinth. The concentration of oxalate in the various organs was more than twice that of Ca. Soluble Ca decreased with age in all organs except the leaf, while oxalate increased with age in all organs except the rhizome. There were site variations in the partitioning of both Ca and oxalate in the water hyacinth.     

两个柑橘品种花期前后子房(幼果)和春梢叶中不同形态钙和果胶含量变化

对单性结实的龟井温州蜜柑和自花结实的鄂柑1号花期前后子房(幼果)和春梢叶的果胶酸钙、草酸钙、水溶性果胶和原果胶含量变化进行研究。结果表明:(1)两品种子房(幼果)和春梢叶中果胶酸钙含量变化均相类似且变幅小,但鄂柑1号的含量相对较高;两品种草酸钙的含量变化则因器官不同而有所区别,在春梢叶中,两者呈类似的上升趋势,而于子房(幼果)中两者却相反,龟井蜜柑花后趋下降,鄂柑1号却明显上升;鄂柑1号子房(幼果)的草酸钙含量较龟井蜜柑高。(2)两品种子房(幼果)和春梢叶原果胶含量动态相似,均于花后出现明显上升;而水溶性果胶动态差异明显,龟井蜜柑子房(幼果)和春梢叶在花后6d均出现上升峰值;鄂柑1号的水溶性果胶和原果胶含量均相对较高。     

Incorporation of strontium into plant calcium oxalate crystals

Summary Lemna minor, which produces many calcium oxalate raphide crystals, was grown on media containing in addition to Ca, 200 M of one of the following divalent cations: Ba, Cd, Co, Mn or Sr. Energy dispersive X-ray analysis showed that only Sr was incorporated into the raphides at levels detectable by the analysis technique. Incorporation of Sr into other insoluble compounds, such as cell wall material, could not be detected. Plant species which form different crystal types in their leaves (Beta vulgaris, crystal sand;Arthrostema ciliatum, druse;Glycine canescens, prismatic) also incorporated Sr into their crystals when grown hydroponically on nutrient medium containing 200 M Sr.Axenic cultures ofL. minor were used to examine further the process of Sr incorporation into plant crystals. When grown on nutrient solution with 5 M Ca, increasing the Sr concentration resulted in increases of the amount of Sr incorporated into the raphide crystals. The ratio of Sr to Ca became greater as the Sr concentration was increased. This ratio change was due to both an increase in the amount of Sr incorporated and a decrease in the Ca incorporated. Analysis of the number of crystal idioblasts formed as a function of Sr concentration shows fewer idioblasts are produced as Sr became high. Competition with Ca and interference of Ca utilization by Sr is indicated.