Characterization of calcium oxalates generated as biominerals in cacti

The chemical composition and morphology of solid material isolated from various Cactaceae species have been analyzed. All of the tested specimens deposited high-purity calcium oxalate crystals in their succulent modified stems. These deposits occurred most frequently as round-shaped druses that sometimes coexist with abundant crystal sand in the tissue. The biominerals were identified either as CaC(2)O(4).2H(2)O (weddellite) or as CaC(2)O(4).H(2)O (whewellite). Seven different species from the Opuntioideae subfamily showed the presence of whewellite, and an equal number of species from the Cereoideae subfamily showed the deposition of weddellite. The chemical nature of these deposits was assessed by infrared spectroscopy. The crystal morphology of the crystals was visualized by both conventional light and scanning electron microscopy. Weddellite druses were made up of tetragonal crystallites, whereas those from whewellite were most often recognized by their acute points and general star-like shape. These studies clearly demonstrated that members from the main traditional subfamilies of the Cactaceae family could synthesize different chemical forms of calcium oxalate, suggesting a definite but different genetic control. The direct relationship established between a given Cactaceae species and a definite calcium oxalate biomineral seems to be a useful tool for plant identification and chemotaxonomy.     

Calcium oxalate and sulphate-containing structures on the thallial surface of the lichen Ramalina lacera: response to polluted air and simulated acid rain

The formation of calcium‐containing structures on the thallial surface of the lichen Ramalina lacera (With.) J.R. Laund. in response to air pollution and to simulated acid rain, was studied in in situ and transplanted thalli. In situ thalli were collected from an unpolluted site and transplanted to heavily polluted and less polluted sites for a 10 month period. Additional thalli were treated either with double distilled water or with simulated acid rain. Scanning electron microscopy and infrared spectrometry revealed that thallial surfaces of in situ R. lacera samples collected in unpolluted sites were covered with two kinds of calcium oxalate crystals: whewellite and weddellite. These aggregates of calcium oxalate crystals appear to disintegrate and provide a crystal layer on the thallial surface. Infrared spectroscopy of powder scraped from thallial surfaces of transplants, retrieved from non‐polluted sites, showed the presence of whewellite and weddellite, whereas powders obtained from thalli retrieved from polluted sites contained whewellite, weddellite and gypsum. It is suggested that a certain fraction of the gypsum detected in crater‐like structures in transplants from polluted sites and in thalli treated with simulated acid rain is endogenous and should be considered a biomineral.     

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.     

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 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.     

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.     

Oxalate patinas on ancient monuments: the biological hypothesis

Summary Whewellite and weddellite, calcium oxalate monohydrate and dihydrate respectively, have been found in the form of thin surface layers on limestone and marble monuments and artifacts of various historical periods at different sites. Experimental results indicate that the formation of both minerals must be attributed essentially to the action of oxalic acid secreted by microorganisms (lichens) which live and proliferate on the stone. Oxalic acid attacks the calcium carbonate of the stone surface giving rise to the precipitation of calcium oxalate.     

Distribution of peroxisomes and glycolate metabolism in relation to calcium oxalate formation in Lemna minor L

Calcium oxalate formation in Lemna minor L. occurs in structurally specialized cells called crystal idioblasts. Cytochemical and immunocytochemical protocols were employed to study the distribution of peroxisomes and the enzymes glycolate oxidase, glycine decarboxylase and ribulose 1,5-bisphosphate carboxylase-oxygenase (RuBisCO) in relation to synthesis of oxalate used for Ca oxalate formation. These enzymes are necessary for photorespiratory glycolate synthesis and metabolism. Using catalase cytochemistry, microbodies were found to exist in crystal idioblasts but were smaller and fewer than those found in mesophyll cells. Glycolate oxidase, which can oxidize glycolate to oxalate via glyoxylate, could not be found in microbodies of crystal idioblasts at any stage of development. This enzyme increased in amount in microbodies of mesophyll cells as they matured and could even be found in dense amorphous inclusions of mature cell peroxisomes. Glycine decarboxylase and RuBisCO could also be detected in increasing amount in mesophyll cells as they matured but could not be detected in idioblasts or were just detectable. Thus, Lemna idioblasts lack the machinery for synthesis of oxalate from glycolate. Based on these results and other available information, two general models for the generation and accumulation of oxalate used for Ca oxalate formation in crystal idioblasts are proposed. The biochemical specialization of crystal idioblasts indicated by this study is also discussed with respect to differentiation of cellular structure and function.     

Rock phosphate solubilization by abiotic and fungal-produced oxalic acid: reaction parameters and bioleaching potential

Oxalic acid-producing fungi play an important role in biogeochemical transformations of rocks and minerals and possess biotechnological potential for extraction of valuable elements from primary or waste ores and other solid matrices. This research investigates the extraction of phosphate from rock phosphate (RP) by oxalic acid. Reaction parameters were derived using pure oxalic acid solutions to solubilize RP. It was found that the oxalic acid concentration was the main factor driving reaction kinetics. Excess oxalic acid could retard the reaction due to calcium oxalate encrustation on RP surfaces. However, complete P extraction was reached at stoichiometric proportions of apatite and oxalic acid. This reaction reached completion after 168 h, although most of the P (up to 75%) was released in less than 1 h. Most of the Ca released from the apatite formed sparingly soluble calcium oxalate minerals, with a predominance of whewellite over weddellite. Bioleaching of RP employing biomass-free spent culture filtrates containing oxalic acid (100 mM) produced by Aspergillus niger extracted ~ 74% of the P contained in the RP. These findings contribute to a better understanding of the reaction between apatite and oxalic acid and provide insights for potential applications of this process for biotechnological production of phosphate fertilizer.     

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。     

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.     

Oxalic acid metabolism and calcium oxalate formation in Lemna minor L.

Abstract Axenic Lemna minor plants, which form numerous calcium oxalate crystals, were exposed to [¹⁴C]-glycolic acid, -glyoxylic acid, -oxalic acid and -ascorbic acid and prepared for microautoradiography by a technique that preserves only insoluble label to determine specifically the pathway leading to oxalic acid used for crystal formation. Label from glycolic, glyoxylic, and oxalic acids was incorporated into crystals. Label from oxalic acid was also found in starch when exposure to label was done in the light but not dark, while plastids specialized for lipid storage were heavily labelled under both conditions. Incorporation of label from glycolic and glyoxylic acids, but not oxalic acid, was inhibited in the presence of the glycolate oxidase inhibitors, αHPMS (2-pyridylhydroxy methanesulphonic acid) and mHBA (methyl 2-hydroxy-3-butynoic acid), and inhibition of labelling was not due to an effect on uptake. These studies show that the glycolate oxidase pathway to oxalic acid is operational in L. minor and that the product is available for crystal formation. Dark-grown plants form almost four times as many crystal cells (idioblasts) as do light-grown plants, indicating crystal formation is not in response to photorespiratory glycolate production. Label from [1-¹⁴C]ascorbic acid was also incorporated into crystals and labelling was inhibited by mHBA, indicating glycolic acid and/or glyoxylic acid are possible intermediates of ascorbic acid catabolism. The effect of nitrogen source on crystal formation was also investigated. Significantly more crystal idioblasts were formed, on a surface area basis, by plants grown on ammonium than by plants grown on nitrate nitrogen. When grown with mixed ammonium and nitrate, an intermediate number of crystal idioblasts were formed.     

Crystal morphology and carbon/carbon composition of solid oxalate in cacti

Morphology, crystal structure, and carbon isotopic composition of calcium oxalate from representative species from the family Cactaceae were determined using scanning electron microscopy, x-ray diffraction, and isotope ratio mass spectrometry. Crystals from one species in the Opuntieae tribe of the Cactaceae were druses with acute points composed of the monohydrate form of calcium oxalate (whewellite). Crystals from three species in the Cereeae tribe were the dihydrate form of calcium oxalate (weddellite) forming druses made up of tetragonal and isodiametric crystallites. The oxalate was relatively enriched in ¹³C isotope (-7.3 to - 8.7 ‰) compared with woody fibers (-13.3 to 14.1 ‰) from the same plants.     

Experimental calcium-oxalate crystal production and dissolution by selected wood-rot fungi

Twenty-six species of white-rotting Agaricomycotina fungi (Basidiomycota) were screened for their ability to produce calcium-oxalate (CaOx) crystals in vitro. Most were able to produce CaOx crystals in malt agar medium in the absence of additional calcium. In the same medium enriched with Ca²⁺, all the species produced CaOx crystals (weddellite or whewellite). Hyphae of four species (Ganoderma lucidum, Polyporus ciliatus, Pycnoporus cinnabarinus, and Trametes versicolor) were found coated with crystals (weddellite/whewellite). The production of CaOx crystals during the growth phase was confirmed by an investigation of the production kinetics for six of the species considered in the initial screening (Pleurotus citrinopileatus, Pleurotus eryngii, Pleurotus ostreatus, P. cinnabarinus, Trametes suaveolens, and T. versicolor). However, the crystals produced during the growth phase disappeared from the medium over time in four of the six species (P. citrinopileatus, P. eryngii, P. cinnabarinus, and T. suaveolens). For P. cinnabarinus, the disappearance of the crystals was correlated with a decrease in the total oxalate concentration measured in the medium from 0.65 ??g mm⁻² (at the maximum accumulation rate) to 0.30 ??g mm⁻². The decrease in the CaOx concentration was correlated with a change in mycelia morphology. The oxalate dissolution capability of all the species was also tested in a medium containing calcium oxalate as the sole source of carbon (modified Schlegel medium). Three species (Agaricus blazei, Pleurotus tuberregium, and P. ciliatus) presented a dissolution halo around the growth zone. This study shows that CaOx crystal production is a widespread phenomenon in white-rot fungi, and that an excess of Ca²⁺ can enhance CaOx crystal production. In addition, it shows that some white-rot fungal species are capable of dissolving CaOx crystals after growth has ceased. These results highlight a diversity of responses around the production or dissolution of calcium oxalate in white-rot fungi and reveal an unexpected potential importance of fungi on the oxalate cycle in the environment.     

CRYSTALLOGRAPHY OF THE TWO HYDRATES OF CRYSTALLINE CALCIUM OXALATE IN PLANTS

Crystal forms and crystal structure of the metastable polyhydrate (weddellite) and the stable monohydrate (whewellite) occurring in plant cells are described and their formation as well as their physiological bearing are discussed.     

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.     

First evidence for the presence of weddellite crystallites in Opuntia ficus indica parenchyma

Calcium oxalate crystallites occur very often in the plants tissues and their role is still poorly known. We report here the experimental protocol leading to the isolation of two forms of calcium oxalate crystallites differing in their hydration level in the parenchymal tissues of Opuntia ficus indica (Miller). Whereas the whewellite crystallites are habitual in all Opuntia species, the weddellite form has never been isolated from these species before, which is probably due to their small size (about 1 microm). We have identified these forms using X-ray diffraction and scanning electron microscopy.     

五种C4荒漠植物光合器官中含晶细胞的比较分析

 为了探讨荒漠植物适应干旱环境的机理, 选择光合器官发生很大变化的5种C₄荒漠植物进行了解剖结构的对比研究。结果表明, 这5种 植物中含晶细胞的数量、大小、形态和分布位置等存在差异。白梭梭(Haloxylon persicum)和梭梭(H. ammodendron)的同化枝普遍具有含晶细 胞; 沙拐枣(Calligonum mongolicum)的含晶细胞很少, 一般只分布在贮水组织或靠近栅栏组织处; 木本猪毛菜(Salsola arbuscula)的含晶细 胞也不多, 主要分布在栅栏组织和表皮细胞之间; 猪毛菜(S. collina)的含晶细胞更少, 仅在贮水组织中偶尔可见晶簇。比较梭梭、白梭梭和 沙拐枣同化枝不同部位的解剖结构发现, 梭梭同化枝基部含晶细胞最多, 中部次之, 顶部最少; 白梭梭同化枝顶部的含晶细胞数量较多, 中部 及基部较少; 沙拐枣同化枝顶部与基部的粘液细胞较多, 中部较少, 基部几乎没有栅栏组织, 而其维管组织较为发达。综合晶体的酸碱溶解性 及硝酸银组化分析结果, 并参照能谱仪的分析结果得知, 梭梭、白梭梭、沙拐枣和木本猪毛菜的叶片或同化枝中所含晶体的主要成分为草酸钙 。通过比较解剖结构发现, 梭梭和白梭梭的同化枝中含晶细胞最多, 其它3种植物的同化器官中含晶细胞较少, 而沙拐枣同化枝中有粘液细胞存 在。     

Cell and calcium oxalate crystal growth is coordinated to achieve high-capacity calcium regulation in plants

Summary Crystal idioblasts are cells which are specialized for accumulation of Ca²⁺ as a physiologically inactive, crystalline salt of oxalic acid. Using microautoradiographic, immunological, and ultrastructural techniques, the process of raphide crystal growth, and how crystal growth is coordinated with cell growth, was studied in idioblasts ofPistia stratiotes. Incorporation of⁴⁵Ca²⁺ directly demonstrated that, relative to surrounding mesophyll cells, crystal idioblasts act as high-capacity Ca²⁺ sinks, accumulating large amounts of Ca²⁺ within the vacuole as crystals. The pattern of addition of Ca²⁺ during crystal growth indicates a highly regulated process with bidirectional crystal growth. In very young idioblasts,⁴⁵Ca²⁺ is incorporated along the entire length of the needle-shaped raphide crystals, but as they mature incorporation only occurs at crystal tips in a bidirectional mode. At full maturity, the idioblast stops Ca²⁺ uptake, although the cells are still alive, demonstrating an ability to strictly regulate Ca transport processes at the plasma membrane. In situ hybridization for ribosomal RNA shows young idioblasts are extremely active cells, are more active than older idioblasts, and have higher general activity than surrounding mesophyll cells. Polarizing and scanning electron microscopy demonstrate that the crystal morphology changes as crystals develop and includes morphological polarity and an apparent nucleation point from which crystals grow bidirectionally. These results indicate a carefully regulated process of biomineralization in the vacuole. Finally, we show that the cytoskeleton is important in controlling the idioblast cell shape, but the regulation of crystal growth and morphology is under a different control mechanism.Abbreviation SEM scanning electron microscopy