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.     

The intravacuolar organic matrix associated with calcium oxalate crystals in leaves of Vitis

In Vitis (grape) calcium oxalate crystals form in a needle-like morphology unique to plants, presenting an intriguing system of biological control over mineral formation. Crystals develop within an organic matrix which appears to provide control over the sites and forms of crystal deposition; however, little is known about the chemical nature of the matrix. A procedure has been developed to isolate crystals along with their associated intravacuolar matrix from leaves of grape, and studies have been initiated into the chemical composition of the matrix by characterizing elemental content, carbohydrates, and protein. The isolated matrix consisted of two structural phases, membrane chambers enclosing developing crystals, and a water-soluble phase surrounding the crystal chambers. Elemental analysis detected substantial calcium and potassium, as well as some iron in the water-soluble phase. Analysis of the water-soluble matrix by GC-MS showed that it contained an unusual polymer with novel glucuronic acid linkages. In addition, linkage analysis indicated 5-linked arabinans, arabinogalactan, and various mannosyl units typical of complex carbohydrates of N-linked glycoproteins. SDS—PAGE analysis of the water-soluble matrix and crystal chambers showed that each had distinct banding profiles in silver-stained gels, with prominent 60 and 70 kDa polypeptides in crystal chamber extracts. Demineralization studies provided direct evidence that the isolated matrix promotes crystal nucleation. The findings about the organic matrix associated with calcium oxalate crystals in grape are discussed in relation to crystal nucleation and growth and features shared with animal and microbial biomineralization systems.     

The Role of Druse and Raphide Calcium Oxalate Crystals in Tissue Calcium Regulation in Pistia stratiotes Leaves

Abstract: Ca oxalate crystal formation was examined in Pistia stratiotes L. leaves during excess Ca and Ca-deficient conditions. Pistia produces druse crystal idioblasts in the adaxial mesophyll and raphide idioblasts in the abaxial aerenchyma. Raphide crystals were previously found to grow bidirectionally, and here we show that Ca is incorporated along the entire surfaces of developing druse crystals, which are coated with membrane-bound microprojections. Leaves formed on plants grown on 0 Ca medium have fewer and smaller druse crystals than leaves formed under 5 mM Ca ("control") conditions, while raphide crystal formation is completely inhibited. When plants were moved from 0 to 15 mM ("high") Ca, the size and number of crystals in new leaves returned to (druse) or exceeded (raphide) control levels. High Ca also induced formation of druse, but not raphide, crystals in differentiating chlorenchyma cells. When plants were transferred from 15 mM Ca to 0 Ca, young druse crystals were preferentially partially dissolved. Oxalate oxidase, an enzyme that degrades oxalate, increased during Ca deficiency and was localized to the crystal surfaces. The more dynamic nature of druse crystals is not due to hydration form as both crystal types are shown to be monohydrate. Part of the difference may be because raphide idioblasts have developmental constraints that interfere with a more flexible response to changing Ca. These studies demonstrate that excess Ca can be stored as Ca oxalate, the Ca can be remobilized under certain conditions, and different forms of Ca oxalate have different roles in bulk Ca regulation.     

Biosynthesis of L-ascorbic acid and conversion of carbons 1 and 2 of L-ascorbic acid to oxalic acid occurs within individual calcium oxalate crystal idioblasts

L-Ascorbic acid (AsA) and its metabolic precursors give rise to oxalic acid (OxA) found in calcium oxalate crystals in specialized crystal idioblast cells in plants; however, it is not known if AsA and OxA are synthesized within the crystal idioblast cell or transported in from surrounding mesophyll cells. Isolated developing crystal idioblasts from Pistia stratiotes were used to study the pathway of OxA biosynthesis and to determine if idioblasts contain the entire path and are essentially independent in OxA synthesis. Idioblasts were supplied with various (14)C-labeled compounds and examined by micro-autoradiography for incorporation of (14)C into calcium oxalate crystals. [(14)C]OxA gave heavy labeling of crystals, indicating the isolated idioblasts are functional in crystal formation. Incubation with [1-(14)C]AsA also gave heavy labeling of crystals, whereas [6-(14)C]AsA gave no labeling. Labeled precursors of AsA (L-[1-(14)C]galactose; D-[1-(14)C]mannose) also resulted in crystal labeling, as did the ascorbic acid analog, D-[1-(14)C]erythorbic acid. Intensity of labeling of isolated idioblasts followed the pattern OxA > AsA (erythorbic acid) > L-galactose > D-mannose. Our results demonstrate that P. stratiotes crystal idioblasts synthesize the OxA used for crystal formation, the OxA is derived from the number 1 and 2 carbons of AsA, and the proposed pathway of ascorbic acid synthesis via D-mannose and L-galactose is operational in individual P. stratiotes crystal idioblasts. These results are discussed with respect to fine control of calcium oxalate precipitation and the concept of crystal idioblasts as independent physiological compartments.     

Calcium oxalate formation is a rapid and reversible process inLemna minor L.

Summary Lemna minor root tips form raphide Ca oxalate crystals in both the root cap and root proper. An in vivo system was developed to examine raphide crystal bundle formation in the root of intact plants. By increasing the exogenous Ca concentration, crystal bundle formation could be induced. Entire new crystal bundles could be formed within 30 minutes of an inductive stimulus. The process was reversible with recently formed crystal bundles being dissolved over a period of about 3 hours. Older, previously existing bundles were more resistant to dissolution. The calmodulin antagonists, chlorpromazine and trifluoperazine (300 M), prevented crystal formation and caused dissolution of some crystal bundles, even in the presence of exogenous Ca. When the antagonists were flushed out and replaced with fresh medium, crystals were formed in cells where dissolution had occurred under the influence of the antagonists. The Ca ionophore A 23187 (20 M) caused slow dissolution of crystal bundles, even in the presence of exogenous Ca. A model describing the control of and physiological significance of Ca oxalate formation in plants is presented and discussed with respect to the results obtained in this study.     

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.     

Calcium channels are involved in calcium oxalate crystal formation in specialized cells of Pistia stratiotes L

BACKGROUND AND AIMS: Pistia stratiotes produces large amounts of calcium (Ca) oxalate crystals in specialized cells called crystal idioblasts. The potential involvement of Ca(2+) channels in Ca oxalate crystal formation by crystal idioblasts was investigated. METHODS: Anatomical, ultrastructural and physiological analyses were used on plants, fresh or fixed tissues, or protoplasts. Ca(2+) uptake by protoplasts was measured with (45)Ca(2+), and the effect of Ca(2+) channel blockers studied in intact plants. Labelled Ca(2+) channel blockers and a channel protein antibody were used to determine if Ca(2+) channels were associated with crystal idioblasts. KEY RESULTS: (45)Ca(2+) uptake was more than two orders of magnitude greater for crystal idioblast protoplasts than mesophyll protoplasts, and idioblast number increased when medium Ca was increased. Plants grown on media containing 1-50 microM of the Ca(2+) channel blockers, isradipine, nifedipine or fluspirilene, showed almost complete inhibition of crystal formation. When fresh tissue sections were treated with the fluorescent dihydropyridine-type Ca(2+) channel blocker, DM-Bodipy-DHP, crystal idioblasts were intensely labelled compared with surrounding mesophyll, and the label appeared to be associated with the plasma membrane and the endoplasmic reticulum, which is shown to be abundant in idioblasts. An antibody to a mammalian Ca(2+) channel alpha1 subunit recognized a single band in a microsomal protein fraction but not soluble protein fraction on western blots, and it selectively and heavily labelled developing crystal idioblasts in tissue sections. CONCLUSIONS: The results demonstrate that Ca oxalate crystal idioblasts are enriched, relative to mesophyll cells, in dihydropyridine-type Ca(2+) channels and that the activity of these channels is important to transport and accumulation of Ca(2+) required for crystal formation.     

Characterization of histone (H1B) oxalate binding protein in experimental urolithiasis and bioinformatics approach to study its oxalate interaction

The rat kidney H1 oxalate binding protein was isolated and purified. Oxalate binds exclusively with H1B fraction of H1 histone. Oxalate binding activity is inhibited by lysine group modifiers such as 4',4'-diisothiostilbene-2,2-disulfonic acid (DIDS) and pyridoxal phosphate and reduced in presence of ATP and ADP. RNA has no effect on oxalate binding activity of H1B whereas DNA inhibits oxalate binding activity. Equilibrium dialysis method showed that H1B oxalate binding protein has two binding sites for oxalate, one with high affinity, other with low affinity. Histone H1B was modeled in silico using Modeller8v1 software tool since experimental structure is not available. In silico interaction studies predict that histone H1B-oxalate interaction take place through lysine121, lysine139, and leucine68. H1B oxalate binding protein is found to be a promoter of calcium oxalate crystal (CaOx) growth. A 10% increase in the promoting activity is observed in hyperoxaluric rat kidney H1B. Interaction of H1B oxalate binding protein with CaOx crystals favors the formation of intertwined calcium oxalate dehydrate (COD) crystals as studied by light microscopy. Intertwined COD crystals and aggregates of COD crystals were more pronounced in the presence of hyperoxalauric H1B.     

Peeping into Human Renal Calcium Oxalate Stone Matrix: Characterization of Novel Proteins Involved in the Intricate Mechanism of Urolithiasis

Background

The increasing number of patients suffering from urolithiasis represents one of the major challenges which nephrologists face worldwide today. For enhancing therapeutic outcomes of this disease, the pathogenic basis for the formation of renal stones is the need of hour. Proteins are found as major component in human renal stone matrix and are considered to have a potential role in crystal–membrane interaction, crystal growth and stone formation but their role in urolithiasis still remains obscure.

Methods

Proteins were isolated from the matrix of human CaOx containing kidney stones. Proteins having MW>3 kDa were subjected to anion exchange chromatography followed by molecular-sieve chromatography. The effect of these purified proteins was tested against CaOx nucleation and growth and on oxalate injured Madin–Darby Canine Kidney (MDCK) renal epithelial cells for their activity. Proteins were identified by Matrix-assisted laser desorption/ionization-time of flight (MALDI-TOF MS) followed by database search with MASCOT server. In silico molecular interaction studies with CaOx crystals were also investigated.

Results

Five proteins were identified from the matrix of calcium oxalate kidney stones by MALDI-TOF MS followed by database search with MASCOT server with the competence to control the stone formation process. Out of which two proteins were promoters, two were inhibitors and one protein had a dual activity of both inhibition and promotion towards CaOx nucleation and growth. Further molecular modelling calculations revealed the mode of interaction of these proteins with CaOx at the molecular level.

Conclusions

We identified and characterized Ethanolamine-phosphate cytidylyltransferase, Ras GTPase-activating-like protein, UDP-glucose:glycoprotein glucosyltransferase 2, RIMS-binding protein 3A, Macrophage-capping protein as novel proteins from the matrix of human calcium oxalate stone which play a critical role in kidney stone formation. Thus, these proteins having potential to modulate calcium oxalate crystallization will throw light on understanding and controlling urolithiasis in humans.     

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.     

Interactions between acidic matrix macromolecules and calcium phosphate ester crystals: relevance to carbonate apatite formation in biomineralization.

Control over crystal growth by acidic matrix macromolecules is an important process in the formation of many mineralized tissues. Earlier studies on the interactions between acidic macromolecules and carboxylate- and carbonate-containing crystals showed that the proteins recognize a specific stereochemical motif on the interacting plane. Here we show that a similar stereochemical motif is recognized by acidic mollusc shell macromolecules interacting with four different organic calcium phosphate-containing crystals. In addition, an acidic protein from vertebrate tooth dentin was also observed to recognize a similar structural motif in one of the crystals. The characteristic motif recognized is composed of rows of calcium ions and phosphates arranged in a plane defined by two free oxygens and a phosphorus atom emerging perpendicular to the affected face. These observations may have a direct bearing on the manner in which control over crystal growth is exerted on carbonate apatite crystals commonly found in vertebrate tissues.     

Characterization of two molluscan crystal-modulating biomineralization proteins and identification of putative mineral binding domains

Ethylenediamine-tetraacetic acid extracted water-soluble matrix proteins in molluscan shells secreted from the mantle epithelia are believed to control crystal nucleation, morphology, orientation, and phase of the deposited mineral. Previously, atomic force microscopy demonstrated that abalone nacre proteins bind to growing step edges and to specific crystallographic faces of calcite, suggesting that inhibition of calcite growth may be one of the molecular processes required for growth of the less thermodynamically stable aragonite phase. Previous experiments were done with protein mixtures. To elucidate the role of single proteins, we have characterized two proteins isolated from the aragonitic component of nacre of the red abalone, Haliotis rufescens. These proteins, purified by hydrophobic interaction chromatography, are designated AP7 and AP24 (aragonitic protein of molecular weight 7 kDa and 24 kDa, respectively). Degenerate oligonucleotide primers corresponding to N-terminal and internal peptide sequences were used to amplify cDNA clones by a polymerase chain reaction from a mantle cDNA library; the deduced primary amino acid sequences are presented. Preliminary crystal growth experiments demonstrate that protein fractions enriched in AP7 and AP24 produced CaCO(3) crystals with morphology distinct from crystals grown in the presence of the total mixture of soluble aragonite-specific proteins. Peptides corresponding to the first 30 residues of the N-terminal sequences of both AP7 and AP24 were generated. The synthetic peptides frustrate the progression of step edges of a growing calcite surface, indicating that sequence features within the N-termini of AP7 and AP24 include domains that interact with CaCO(3). CD analyses demonstrate that the N-terminal peptide sequences do not possess significant percentages of alpha-helix or beta-strand secondary structure in solution. Instead, in both the presence and absence of Ca(II), the peptides retain unfolded conformations that may facilitate protein-mineral interaction.     

Calcium Oxalate Deposits in Leaves of Corchorus olitorius as Related to Accumulation of Toxic Metals1

This study was to report and describe the formation of Ca oxalate crystals and to explore whether there is any correlation between their abundant formation and the ability of plant to uptake and accumulate high levels of toxic metals. Soil-grown Corchorus olitorius L. (Tiliaceae) seedlings were further grown in water culture in the presence of Cd, Pb, Cu, or Al (0–10 g/ml) for 20 days. Light and electron microscopic examinations revealed a large number of intracellular prismatic-shaped Ca oxalate crystals in both leaf and callus cells. Crystals were formed in the vacuole, a single large crystal being formed per cell. The crystal-containing cells differed in size and shape from crystal-free cells, they were rich in organelles, membranes, and vesicles and have dense cytoplasm, enlarged nucleus and modified starch-lacking plastids with few grana. These cells look highly active. Corchorus plants treated with Cd, Pb, Cu, and Al accumulated these metals to the levels several times higher than untreated plants. The contents of Pb, Cd, Al, and Cu in leaf tissues of plants grown in the presence of 5 g/ml of these metals were 10, 20, 25, and 40 times higher, respectively, than those in plants grown on media devoid of them. X-ray microanalysis of Ca oxalate crystals in leaves from plants exposed to 5 g/ml Cd, Pb, Al, or Cu indicated the incorporation only of Al into these crystals. Results of this paper suggest a possible contribution for Ca oxalate-crystal formation in sequestering and tolerance of at least some toxic metals.     

A new matrix protein family related to the nacreous layer formation of Pinctada fucata

We have isolated a new matrix protein family (N16) which is specific to the nacreous layer of the Japanese pearl oyster, Pinctada fucata, and have cloned and characterized the cDNAs coding for the components. Analysis of the deduced amino acid sequence revealed that N16 showed no definitive homology with other proteins. The in vitro studies of the crystallization clarified that N16 induced aragonite crystals when fixed on the substrate but inhibited crystal formation without it. The aragonite crystals showed platy morphology different from those formed inorganically, and long intervals of incubation resulted in crystalline layers highly similar to the nacreous layer.     

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.     

Calcium Oxalate Biomineralization by Piloderma fallax in Response to Various Levels of Calcium and Phosphorus

Piloderma fallax is an ectomycorrhizal fungus commonly associated with several conifer and hardwood species. We examined the formation of calcium oxalate crystals by P. fallax in response to calcium (0.0, 0.1, 0.5, 1, and 5 mM) and phosphorus (0.1 and 6 mM) additions in modified Melin-Norkrans agar medium. Both calcium and phosphorus supplementation significantly affected the amount of calcium oxalate formed. More calcium oxalate was formed at high P levels. Concentrations of soluble oxalate in the fungus and medium were higher at low P levels. There was a strong positive linear relationship between Ca level and calcium oxalate but only under conditions of phosphorus limitation. Calcium oxalate crystals were identified as the monohydrate form (calcium oxalate monohydrate [COM] whewellite) by X-ray diffraction analysis. Prismatic, styloid, and raphide forms of the crystals, characteristic COM, were observed on the surface of fungal hyphae by scanning electron microscopy. P. fallax may be capable of dissolving hyphal calcium oxalate under conditions of limited Ca. The biomineralization of calcium oxalate by fungi may be an important step in the translocation and cycling of Ca and P in soil.Many fungi from forest litter, including ectomycorrhizal fungi, exhibit calcium oxalate (CaOx) crystals on their hyphae. The ubiquity of CaOx crystals on fungal hyphae suggests that their formation may provide a selective advantage to the organism (4). CaOx formation is hypothesized to regulate intracellular pH and levels of oxalate and Ca and, hence, serves as a major sink for toxic amounts of Ca in soil and other environments (52, 53, 61). In plants, CaOx crystals have also been proposed to serve as a calcium source under conditions of calcium limitation (14, 18, 41), but such a process has yet to be established among fungi.CaOx on fungal hyphae is formed from soil-derived calcium and biologically synthesized oxalate. Oxalate released by ectomycorrhizae has been correlated with increased phosphorus bioavailability in the rhizosphere (V. Casarin, cited by Hinsinger in reference 25). The ability of oxalate to chelate metal ions makes it important in the solubilization and transport of metals in soil, the weathering and diagenesis of rocks and soil minerals (9, 23, 31, 57), and, consequently, the transport of nutrients. It is generally presumed that CaOx crystals form on the surface of fungal hyphae as a result of precipitation when released oxalic acid interacts with calcium cations (23, 43). However, the regularity of the CaOx crystals suggests that their formation is regulated and that they may be formed within the fungal hyphae at specific sites of origin (3, 5, 7).CaOx crystals vary in morphology, ranging from plates to raphides, druses, tetragonal bipyramids, and prisms. This variation in morphology can be seen among fungal genera and species (4). The crystals also usually occur either as CaOx monohydrate (COM; whewellite) (29) or CaOx dihydrate (weddellite) (3, 5, 28, 35, 60). Either crystal form or both may be present on fungal hyphae at the same time.In earlier studies (8, 9), we reported that Piloderma fallax is one of the major species of ectomycorrhizal fungi in subboreal forests. In addition, Piloderma sp. is found in temperate forest soils in association with conifer and hardwood species (34). Piloderma influences nutrient uptake and modifies mineral transformation in rock and soil systems (3, 33). In this study, we chose P. fallax because of (i) its ability to produce oxalate and form CaOx crystals (8, 56), (ii) its presence in many types of forest ecosystems, and (iii) its significant role in the breakdown and formation of soil minerals (9).The objective of this study was to quantify and characterize the formation of CaOx by P. fallax in response to various P and Ca levels in agar medium. We tested the hypothesis that P limitation will induce the production of oxalate and that increased concentrations of Ca will result in greater CaOx formation. This study also examined the dissolution of CaOx on P. fallax when it is grown on Ca-deficient medium and determined whether CaOx can serve as temporary Ca storage. Our study was conducted to add to knowledge of the ecological significance of CaOx, especially of its influence in biogeochemical cycling of P and Ca in soils.     

Morphologies and elemental compositions of calcium crystals in phyllodes and branchlets of Acacia robeorum (Leguminosae: Mimosoideae)

Background and Aims

Formation of calcium oxalate crystals is common in the plant kingdom, but biogenic formation of calcium sulfate crystals in plants is rare. We investigated the morphologies and elemental compositions of crystals found in phyllodes and branchlets of Acacia robeorum, a desert shrub of north-western Australia.

Methods

Morphologies of crystals in phyllodes and branchlets of A. robeorum were studied using scanning electron microscopy (SEM), and elemental compositions of the crystals were identified by energy-dispersive X-ray spectroscopy. Distributional patterns of the crystals were studied using optical microscopy together with SEM.

Key Results

According to the elemental compositions, the crystals were classified into three groups: (1) calcium oxalate; (2) calcium sulfate, which is a possible mixture of calcium sulfate and calcium oxalate with calcium sulfate being the major component; and (3) calcium sulfate · magnesium oxalate, presumably mixtures of calcium sulfate, calcium oxalate, magnesium oxalate and silica. The crystals were of various morphologies, including prisms, raphides, styloids, druses, crystal sand, spheres and clusters. Both calcium oxalate and calcium sulfate crystals were observed in almost all tissues, including mesophyll, parenchyma, sclerenchyma (fibre cells), pith, pith ray and cortex; calcium sulfate · magnesium oxalate crystals were only found in mesophyll and parenchyma cells in phyllodes.

Conclusions

The formation of most crystals was biologically induced, as confirmed by studying the crystals formed in the phyllodes from seedlings grown in a glasshouse. The crystals may have functions in removing excess calcium, magnesium and sulfur, protecting the plants against herbivory, and detoxifying aluminium and heavy metals.     

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 CRYSTALS IN THE GREEN ALGA SPIROGYRA SP. (ZYGNEMATALES, CHLOROPHYTA)

Specimens of an unidentified species of the freshwater green alga Spirogyra were found to have abundant cruciate cellular inclusions up to 34 micrometers long. A crystalline nature was shown by birefringence in polarized light. Despite their large size and complex shape, these inclusions did not occur free in the large central vacuole. Instead, they were associated with cytoplasmic strands that spanned the space between gyres of the parietal spiral chloroplasts and with strands that suspended the nucleus in a cytoplasmic embayment of the central vacuole. Some crystals moved directionally along the cytoplasmic strands, and their movement was arrested by cytochalasin B, suggesting that actin microfilaments had a role in crystal movement. Solubility tests showed that the inclusions were composed of calcium oxalate; they dissolved rapidly in weak hydrochloric acid without effervescence, but they were not soluble in concentrated acetic acid or sodium hypochlorite. A colorimetric enzymatic test for oxalate was used to demonstrate microscopically the presence of oxalate and to quantify the amounts. The calcium oxalate crystals were surrounded by a water-soluble organic matrix that retained the shape of the crystal even after demineralization. Scanning electron microscopy was used to examine the morphology of isolated crystals.