Cytoplasmic streaming of calcium oxalate crystals in Callipsygma wilsonis (Bryopsidales, Chlorophyta)

Light microscopic study of the giant‐celled, marine green alga Callipsygma wilsonis J. Agardh (Udoteaceae, Bryopsidales) revealed numerous birefringent crystalline inclusions in the terminal segments of the assimilatory axes. The inclusions were thin plates with a triangular shape in face view, a base up to 75 μm in length, and a height that was one‐seventh the length of the base. Crystals of various sizes commonly were stacked face‐to‐face with one or more edges coinciding, but removal of organic material by treatment in sodium hypochlorite resulted in disaggregation. The crystals were soluble in dilute hydrochloric acid without effervescence but were insoluble in acetic acid. These diagnostic chemical solubility tests and a positive reaction to the Yasue staining reaction indicated that the crystals were composed of calcium oxalate. Scanning electron microscopy showed that most crystals had smoothly curving edges, but some had truncate or beveled margins. Calcium oxalate crystals have been reported to occur in the large central vacuoles of several bryopsidalean species, but the crystals in C. wilsonis were present in the parietal cytoplasm, which was evident from the presence of crystals in streaming cytoplasm. Calcium oxalate crystals, amyloplasts, chloroplasts, and other cytoplasmic constituents moved along cytoskeletal cables at rates of approximately 2.8 μm s⁻¹. These findings add to a growing body of evidence that calcium oxalate crystals in diverse algae may be present in cellular compartments other than the central vacuole.     

Calcium oxalate crystals in plants

Calcium (Ca) oxalate crystals occur in many plant species and in most organs and tissues. They generally form within cells although extracellular crystals have been reported. The crystal cells or idioblasts display ultrastructural modifications which are related to crystal precipitation. Crystal formation is usually associated with membranes, chambers, or inclusions found within the cell vacuole(s). Tubules, modified plastids and enlarged nuclei also have been reported in crystal idioblasts. The Ca oxalate crystals consist of either the monohydrate whewellite form, or the dihydrate weddellite form. A number of techniques exist for the identification of calcium oxalate. X-ray diffraction, Raman microprobe analysis and infrared spectroscopy are the most accurate. Many plant crystals assumed to be Ca oxalate have never been positively identified as such. In some instances, crystals have been classified as whewellite or weddellite solely on the basis of their shape. Certain evidence indicates that crystal shape may be independent of hydration form of Ca oxalate and that the vacuole crystal chamber membranes may act to mold crystal shape; however, the actual mechanism controlling shape is unknown. Oxalic acid is formed via several major pathways. In plants, glycolate can be converted to oxalic acid. The oxidation occurs in two steps with glyoxylic acid as an intermediate and glycolic acid oxidase as the enzyme. Glyoxylic acid may be derived from enzymatic cleavage of isocitric acid. Oxaloacetate also can be split to form oxalate and acetate. Another significant precursor of oxalate in plants is L-ascorbic acid. The intermediate steps in the conversion of L-ascorbic acid to oxalate are not well defined. Oxalic acid formation in animals occurs by similar pathways and Ca oxalate crystals may be produced under certain conditions. Various functions have been attributed to plant crystal idioblasts and crystals. There is evidence that oxalate synthesis is related to ionic balance. Plant crystals thus may be a manifestation of an effort to maintain an ionic equilibrium. In many plants oxalate is metabolized very slowly or not at all and is considered to be an end product of metabolism. Plant crystal idioblasts may function as a means of removing the oxalate which may otherwise accumulate in toxic quantities. Idioblast formation is dependent on the availability of both Ca and oxalate. Under Ca stress conditions, however, crystals may be reabsorbed indicating a storage function for the idioblasts for Ca. In addition, it has been suggested that the crystals serve purely as structural supports or as a protective device against foraging animals. The purpose of this review is to present an overview of plant crystal idioblasts and Ca oxalate crystals and to include the most recent literature.     

香樟叶肉含晶细胞季节变化研究

为探讨香樟(Cinnamomum camphora)叶肉含晶细胞超微结构的季节变化,阐明香樟叶肉中草酸钙晶体在春夏秋冬的变化规律。该研究以多年生香樟(C. camphora)叶片为材料,分别于春夏秋冬四个季节露地取样,制作超薄切片,用透射电子显微镜(TEM)观察叶肉含晶细胞超微结构的变化。结果表明:春季时香樟叶肉中只有少数细胞有草酸钙晶体,数量较少,晶体结构多为柱状晶、方晶; 夏季时香樟叶肉细胞中随机分布于液泡的草酸钙晶体明显比春季的数量多、体积大、形态丰富,晶体多为柱状晶、方晶、针晶、簇晶; 秋季时香樟叶肉细胞草酸钙晶体和夏季的类似,数量较多,形态多样,以方晶和柱状晶针晶为主,伴有晶簇; 冬季时香樟叶肉含晶细胞晶体形态为柱状晶、方晶、针晶,数量比夏季和秋季的数量略有减少。该研究结果表明在一年四季中香樟叶肉细胞液泡中均有草酸钙晶体结构存在。     

FINE STRUCTURE OF CAPITULAR FILAMENTS IN THE COENOCYTIC GREEN ALGA PENICILLUS1,2,3

Capitular filaments of Penicillus capitatus contain a large central vacuole. The parietal cytoplasm is densely packed, devoid of chloroplasts in the growing tip, and becomes convoluted and sponge-like as extensions of the vacuole penetrate the cytoplasm in mature portions of the filament. Structure of organelles and their distribution in the filament are described. The vacuole contains a variety of inclusions, such as membranous configurations, spherical bodies, electron dense bodies, and calcium oxalate monohydrate crystals, each of the latter surrounded by a chamber associated with microtubules. Endophytic bacteria are present throughout the vacuole and occasionally in the tip cytoplasm. Some vacuolar components of P. pyriformis are described for comparison.     

Cine-photomicrography of low temperature effects on cytoplasmic streaming, nucleoar activity and mitosis in single tobacco cells in microculture

Living, unstained, single tobacco (Nicoliana tabacum × N. glutinosa) cells (clone H-196) were grown in microcultures in liquid medium containing sucrose, mineral salts, coconut milk and 2,4-dichlorophenoxyaeetic acid. Time-lapse motion pictures were taken through interference and phase microscopes. The movement of cytoplasm and cell organelles gradually slowed and ultimately completely ceased as the cell was cooled by dry ice. The cessation of the movement of cell organelles took place between 5 and –7C. The typical cytoplasmic morphology was lost as the movement slowed. The cytoplasmic strands thinned out and numerous small vacuoles formed. During rewarming of the cell to room temperature, the vacuoles were replaced by numerous small globular masses of cytoplasm which reorganized into cytoplasmic strands. The normal movement of cytoplasmic strands and cell organelles was resumed. A number of small nucleolar vacuoles at room temperature gradually expanded and coaleseed to form a large central vacuole which underwent further expansion and then contracted rapidly. Four different concentric zones were visible across the nucleolar region. A white, highly reflecting, glossy substance appeared on the surface of the expanding vacuole. The position of the nucleus during contraction and expansion was never stationary. Some nucleolar vacuoles remained open for an indefinite period of time when the cell was cooled to 5C. No change was noticed during cooling, but during rewarming to room temperature, the nucleolar vacuole was partially closed. The pumping action of the nucleolar vacuole suggested important exchanges of metabolites between the nucleolus and the cytoplasm. A single cell of tobacco did not divide at –10C, but mitosis proceeded upon cooling the cell to – 12–15C for a brief period. Different phases of mitosis, specifically formation of the cell plate, cell wall, and separation of nuclei, were delayed by low temperature treatment.     

Structure of Crystal Cells and Influences of Leaf Development on Crystal Cell Development and Vice Versa in Phaseolus vulgaris (Leguminosae)

The structure of cells with calcium oxalate crystals and their nelghbouring cells has been studied by light and transmission electron microscopy at different stages of bean leaf development. Plants were grown with varying calcium supply to identify a possible influence of calcium nutrition on cell structure. Crystals are formed inside the vacuole of already highly vacuolated cells of bundle sheath extensions. The membrane around the crystal vacuole is continuous with the plasmalemma. The crystal vacuole contains membraneous structures. In the fully expanded leaf the crystal becomes ensheathed by wall material. Chloroplasts of bundle sheath extension cells, with or without crystals, are smaller, with fewer membranes, and with much narrower stroma regions than those of the palisade parenchyma. There is a stage in the young leaf when only the bundle sheath extension cells without crystals have starch grains in their chloroplasts. As their number is lower in plants grown with high calcium supply this means that, in this case, less cells are competent for photosynthesis.     

Developmental features of calcium oxalate crystal sand deposition inBeta vulgaris L. Leaves

Summary Sugar beet (Beta vulgaris L.) leaf has a layer of cells extended laterally between the palisade parenchyma and spongy mesophyll that develop numerous small crystals (crystal sand) within their vacuoles. Solubility studies and histochemical staining indicate the crystals are calcium oxalate. The crystals are deposited within the vacuoles early during leaf development, and at maturity the cells are roughly spherical in shape and 2 to 3 times larger than other mesophyll cells. Crystal deposition is preceeded by formation of membrane vesicles within the vacuole. The membranes are synthesizedde novo in the vacuole and have a typical trilaminate structure as viewed with the TEM. The membranes are formed within paracrystalline aggregates of tubular particles (6–8nm outer diameter) as membrane sheets, but are later organized into chambers or vesicles. Calcium oxalate is then precipitated within the membrane chambers. The tubular particles involved in membrane synthesis are usually present in the vacuoles of mature crystal cells, but in very small amounts.     

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.     

植物晶体的形态结构、生物功能及形成机制研究进展

晶体是植物体内产生的一种具有特殊形态结构与生理功能的代谢物,其分布广泛,已在500多种植物中发现有晶体的存在。晶体形态多样,有针晶、柱晶、棱晶、砂晶、簇晶等;类型丰富,有草酸钙晶体、钟乳体、硅质体、硫酸钙晶体及其它类型的晶体;功能特殊,具有钙调节、植物保护和防御、重金属解毒、离子平衡、缓解逆境胁迫及其它多种生物功能。晶体的形成涉及钙离子的体外吸收和体内转运,草酸的生物合成,以及钙离子和草酸的耦合过程;晶体的生长发育涉及液泡、晶异细胞的调控及与其它细胞结构的相互协作。对晶体的研究进行综述,以期为晶体的进一步研究提供基础资料。     

Calcium oxalate crystals in the red algaAntithamnion kylinii (Ceramiales): cytoplasmic and limited to indeterminate axes

Summary The red alga,Antithamnion kylinii Gardner, was found to have needle-shaped inclusions about 10 m long and less than 0.4 m thick. They ranged in abundance from one or a few in young cells to hundreds in fully enlarged cells. Under polarized light, the inclusions were birefringent, indicating crystallinity. Solubility tests suggested that the inclusions were composed of calcium oxalate: they dissolved in 1 N hydrochloric acid and in a saturated solution of aqueous cupric acetate, but they were not soluble in 10 N acetic acid or 5.25% sodium hypochlorite. X-ray microanalysis confirmed the presence of calcium. Calcium oxalate crystals were present in cells of indeterminate axes, but cells of determinate lateral filaments lacked them. Light and electron microscopic study demonstrated that the crystals were associated with the parietal cytoplasm. Calcium oxalate crystals were also present inA. defectum Kylin, but they were not found in ten more distantly related taxa.     

Isolated Medicago truncatula mutants with increased calcium oxalate crystal accumulation have decreased ascorbic acid levels.

The mechanisms controlling oxalate biosynthesis and calcium oxalate formation in plants remain largely unknown. As an initial step toward gaining insight into these regulatory mechanisms we initiated a mutant screen to identify plants that over-accumulate crystals of calcium oxalate. Four new mutants were identified, from an ethyl methanesulfonate (EMS)-mutagenized Medicago truncatula (cv. Jemalong genotype A17) population, that over-accumulated calcium oxalate crystals. The increased calcium oxalate content of these new mutants, as with the previously isolated mutant cod4, resulted from an increase in druse crystals accumulated within the mesophyll cells of leaves. Complementation and segregation analysis revealed that each mutant was affected at a different locus. This was confirmed through the genetic mapping of each mutation to different linkage groups. Together, these findings emphasize the complexity of factors that can contribute to oxalate biosynthesis and crystal formation in these plants. In addition, each mutant showed a common decrease in ascorbic acid content providing genetic support for ascorbic acid as a precursor in the oxalate biosynthetic pathway for druse crystal formation. Further support was obtained by the ability of an exogenous supply of ascorbate to induce druse crystal formation while other tested organic acids did not induce crystal production.     

Engineering calcium oxalate crystal formation in Arabidopsis

Many plants accumulate crystals of calcium oxalate. Just how these crystals form remains unknown. To gain insight into the mechanisms regulating calcium oxalate crystal formation, a crystal engineering approach was initiated utilizing the non-crystal-accumulating plant, Arabidopsis. The success of this approach hinged on the ability to transform Arabidopsis genetically into a calcium oxalate crystal-accumulating plant. To accomplish this transformation, two oxalic acid biosynthetic genes, obcA and obcB, from the oxalate-secreting phytopathogen, Burkholderia glumae were inserted into the Arabidopsis genome. The co-expression of these two bacterial genes in Arabidopsis conferred the ability not only to produce a measurable amount of oxalate but also to form crystals of calcium oxalate. Biochemical and cellular studies of crystal accumulation in Arabidopsis revealed features that are similar to those observed in the cells of crystal-forming plants. Thus, it appears that at least some of the basic components that comprise the calcium oxalate crystal formation machinery are conserved even in non-crystal-accumulating plants.     

The Isolation and Properties of Oxalate Crystals from Plants

A method of isolation of crystalline inclusions of plant cellsis described. The crystals consist mainly of calcium oxalatein plants grown under normal conditions, but when calcium isreplaced by magnesium, barium, or strontium in the culture solutionthese elements substitute for calcium in the crystals; evenunder normal conditions magnesium occurs in the crystals tothe extent of about 2 per cent. The crystal morphology vanesin the species examined from raphides to complex conglomeratesand X-ray diffraction demonstrates an association of raphideswith calcium oxalate monohydrate whilst other solitary formsand conglomerates are associated with calcium oxalate 2.25H₂O.On this basis the species examined can be divided mto threegroups.     

Calcium oxalate crystal morphology mutants from Medicago truncatula

Plants accumulate crystals of calcium oxalate in a variety of shapes and sizes. The mechanism(s) through which a plant defines the morphology of its crystals remains unknown. To gain insight into the mechanisms regulating crystal shapes, we conducted a mutant screen to identify the genetic determinants. This is the first reported mutant screen dedicated to the identification of crystal morphology mutants. A single leaf was harvested from individual Medicago truncatula L. plants that had been chemically mutagenized. Each leaf was visually inspected, using crossed-polarized light microscopy, for alterations in crystal shape and size. Seven different crystal morphology defective ( cmd) mutants were identified. Six cmd mutants were recessive and one dominant. Genetic analysis of the six recessive mutants suggested that each mutant was affected at a different locus. Each cmd mutant represents a new locus different than any previously identified. The plant phenotype of the cmd mutants appeared similar to that of the wild type in overall growth and development. This observation, coupled with the finding that several of the mutants had drastically altered the amount of calcium they partition into the oxalate crystal, questions current hypotheses regarding crystal function. Comparisons between the mutant crystals and those present in other legumes indicated the likelihood that simple point mutations contributed to the evolution of the variations in prismatic crystal shapes commonly observed in these plants today. The availability of cmd mutants provides the opportunity to investigate aspects of crystal shape and size that have been recalcitrant to previous approaches.     

An Assessment of Engineered Calcium Oxalate Crystal Formation on Plant Growth and Development as a Step toward Evaluating Its Use to Enhance Plant Defense

The establishment of new approaches to control chewing insects has been sought not only for direct use in reducing crop loss but also in managing resistance to the pesticides already in use. Engineered formation of calcium oxalate crystals is a potential strategy that could be developed to fulfill both these needs. As a step toward this development, this study investigates the effects of transforming a non-calcium oxalate crystal accumulating plant, Arabidopsis thaliana, into a crystal accumulating plant. Calcium oxalate crystal accumulating A. thaliana lines were generated by ectopic expression of a single bacterial gene encoding an oxalic acid biosynthetic enzyme. Biochemical and cellular studies suggested that the engineered A. thaliana lines formed crystals of calcium oxalate in a manner similar to naturally occurring crystal accumulating plants. The amount of calcium oxalate accumulated in leaves also reached levels similar to those measured in the leaves of Medicago truncatula in which the crystals are known to play a defensive role. Visual inspection of the different engineered lines, however, suggested a phenotypic consequence on plant growth and development with higher calcium oxalate concentrations. The restoration of a near wild-type plant phenotype through an enzymatic reduction of tissue oxalate supported this observation. Overall, this study is a first to provide initial insight into the potential consequences of engineering calcium oxalate crystal formation in non-crystal accumulating plants.     

Isolation of Medicago truncatula mutants defective in calcium oxalate crystal formation

Plants accumulate crystals of calcium oxalate in a variety of shapes, sizes, amounts, and spatial locations. How and why many plants form crystals of calcium oxalate remain largely unknown. To gain insight into the regulatory mechanisms of crystal formation and function, we have initiated a mutant screen to identify the genetic determinants. Leaves from a chemically mutagenized Medicago truncatula population were visually screened for alterations in calcium oxalate crystal formation. Seven different classes of calcium oxalate defective mutants were identified that exhibited alterations in crystal nucleation, morphology, distribution and/or amount. Genetic analysis suggested that crystal formation is a complex process involving more than seven loci. Phenotypic analysis of a mutant that lacks crystals, cod 5, did not reveal any difference in plant growth and development compared with controls. This finding brings into question the hypothesized roles of calcium oxalate formation in supporting tissue structure and in regulating excess tissue calcium.     

Calcium Oxalate Crystals in Developing Seeds of Soybean

Young developing soybean seeds contain relatively large amountsof calcium oxalate (CaOx) monohydrate crystals. A test for Caand CaOx indicated that Ca deposits and crystals initially occurredin the funiculus, where a single vascular bundle enters theseed. Crystals formed in the integuments until the embryo enlargedenough to crush the inner portion of the inner integument. Crystalsthen appeared in the developing cotyledon tissues and embryoaxis. All crystals formed in cell vacuoles. Dense bodies andmembrane complexes were evident in the funiculus. In the innerintegument, cell vacuoles assumed the shape of the future crystals.This presumed predetermined crystal mould is reported here forthe first time for soybean seeds. As crystals in each tissuenear maturity, a wall forms around each crystal. This intracellularcrystal wall becomes contiguous with the cell wall. Integumentcrystals remain visible until the enlarging embryo crushes theinteguments; the crystals then disappear. A related study revealedthat the highest percent of oxalate by dry mass was reachedin the developing +16 d (post-fertilization) seeds, and thendecreased during late seed maturation. At +60 d, CaOx formationand disappearance are an integral part of developing soybeanseeds. Our results suggest that Ca deposits and crystals functionallyserve as Ca storage for the rapidly enlarging embryos. The oxalate,derived from one or more possible metabolic pathways, couldbe involved in seed storage protein synthesis. Copyright 2001Annals of Botany Company Calcium, crystals, development, Glycine max, ovule, oxalate, seed, soybean     

Calcium Oxalate Raphide Crystals and Crystalliferous Idioblasts in the Carpels of Ornithogalum caudatum

Crystalliferous idioblasts commonly are found in groups of twoor three cells in the peripheral region of the carpels Crystals,composed of calcium oxalate, usually are m well-organized bundleswhich develop within a matrix of protein and carbohydrate inthe vacuole of each idioblast The matrix occurs around and betweenindividual crystal chambers and contains spheres and tubules5.4 nm in diameter The matrix changes in character and locationwith age Crystals form within their own individual chambers,each comprised of a series of lamellae The number of lamellaeis variable The innermost lamella is different from the othersin that it is apparently continuous The other lamellae are platelikeand superficially resemble successive periderms. The lamellaemay begin and/or terminate abruptly or they may anastamose Eachlamella is composed of chains of spheres about 6 1 nm in diameterand is separated from adjacent lamellae by tubules 5.4 nm indiameter Both the crystals and slime body are absorbed duringlater stages of carpel maturation. Ornithogalum caudatum Ait carpel, calcium oxalate, idioblasts, ultrastructure     

ASSOCIATION OF FOUR DIFFERENT CALCIUM CRYSTALS IN THE ANTHER CONNECTIVE TISSUE AND HYPODERMAL STOMIUM OF CAPSICUM ANNUUM (SOLANACEAE) DURING MICROSPOROGENESIS

The anther connective tissue and hypodermal stomium between adjacent locules in the anthers of Capsicum annuum L. (Solanaceae) are the sites of formation of calcium salt crystals with four different habits. The spatial and temporal associations of these crystals and the idioblastic cells in which they form indicate that crystal sand occurs earliest in anther development near the single vascular strand, followed by spherulites and prismatic crystals farther out in the connective tissue, and finally druses occur in the hypodermal stomium. Both the druses and the crystal sand crystals are encased in crystal chambers and are associated with distinct membranes, whereas the spherulites and prismatic crystals are not bounded by any apparent membranes but they are surrounded by dense material that is rich in calcium and stains positively for polysaccharides and proteins. Quite often spherulites and prismatic crystals are observed within a single cell in contact with each other. X-ray diffraction of crystal preparations containing all four crystal habits and X-ray elemental analyses of single crystals, as well as visual observations and acid treatments, suggest that all four crystal habits consist of calcium oxalate. The hypodermal stomium and adjacent connective tissue degenerate at the pollen stage causing adjacent locules to fuse. Shortly afterward, each stomium epidermis splits open along the length of the anther releasing the pollen. It is suggested that the crystal idioblasts are involved in this process, possibly by a temporally orchestrated sequestration of calcium from both the cell cytoplasm and cell wall.