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.     

Dissolution and growth of calcium oxalate monohydrate I. Effect of magnesium and pH

The rate of dissolution of calcium oxalate monohydrate and of a calcium oxalate renal stone was measured in 0.9% NaCl solution at different levels of magnesium concentration and pH. The growth of calcium oxalate obtained by chemical reaction between Ca²⁺ and oxalate ions at a concentration similar to that existing in normal urine was also investigated as a function of pH and magnesium concentration. It was found that both magnesium and pH exert a fine kinetic control on the precipitation and growth of calcium oxalate monohydrate. Magnesium had no effect on the dissolution. The possible role of magnesium and pH in calcium oxalate urolithiasis has been discussed in the light of previous reports and of the data presented in this study.     

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。     

Crystals in woody stems

Scanning electron microscopy has been used to examine the location and form of crystals in the stems of woody perennials. The results are discussed in relation to the effects of physical conditions and "impurities" upon crystal form. Infrared spectroscopy and X-ray diffraction have been used to establish the chemical identity of the crystals in a number of species which were chosen so as to provide a wide variation in form. Those from Populus deltoides and Polyalthia sp. consisted of calcium carbonate; those from ten other species consisted of hydrated calcium oxalate. The infrared spectra of the crystals from Dracaena fragrans, Terminalia balerica, Goniothalamus sp. and Combretum verticillatum were strongly indicative of calcium oxalate monohydrate, but in the other cases the degree of hydration of the oxalate was uncertain.     

Herbivory and Calcium Concentrations Affect Calcium Oxalate Crystal Formation in Leaves ofSida (Malvaceae)

Calcium oxalate crystals have potential roles in plants as partof a defence mechanism against herbivores and/or in accumulatingexcess calcium. To date, these potential roles have been studiedindependently. In this experimental study the effects of calciumlevels and herbivory on the production of calcium oxalate crystals(i.e. druse, spherical crystal aggregates) were examined inseedlings of Sida rhombifolia. Seedlings were subjected to threecalcium levels (low, normal or high) and an artificial herbivorytreatment. Calcium levels and herbivory both affected densityof crystals in leaves. Leaves from seedlings grown in low calciumhad a greater crystal density than those grown in high calcium.Leaves from seedlings subjected to herbivory had a greater crystaldensity than those from seedlings not subjected to herbivory.This study provides additional evidence that calcium oxalatecrystal production depends not only on calcium levels but canalso be influenced by external pressures such as herbivory.In addition to their physiological role in plants, these resultssuggest that calcium oxalate crystals can also act as a defencemechanism against herbivores. Copyright 2001 Annals of BotanyCompany Calcium concentrations, calcium oxalate crystals, herbivory, Malvaceae, Sida rhombifolia     

Evidence of formation of glushinskite as a biomineral in a Cactaceae species

The X-ray diffractometric and infrared spectroscopic investigation of crystalline material isolated from the Cactaceae species Opuntia ellisiana shows the presence of a very complex mineral composition, including whewellite (monohydrated calcium oxalate), opal (SiO2), calcite (CaCO3) and glushinskite (dihydrated magnesium oxalate). This is the first report of the presence of magnesium oxalate in plants.     

An X-ray Microanalysis Study of the Salt Glands and Intracellular Calcium Crystals of Tamarix

X-ray microprobe analyses of the secreted salts from glandsof 20 Tamarix aphylla (L.) Karst trees growing in alluvial soilsin the north western district of Victoria, Australia, show thatthe glands secrete a variety of elements including calcium,magnesium and sulphur. However, sodium, potassium and chloride,common ions reported to be secreted predominantly in other studies,are present in relatively low amounts in the secreted salts.Calcium, the major cationic element in the secretory productof the gland, was not detected in the symplasm of the secretoryand collecting cells or in the vacuoles of the collecting cells.Some evidence indicates that silicon may be secreted by theglands but further corroboratory data are required. Our resultssupport previous suggestions that the glands of Tamarix havea low level of selectivity. Large, spherical aggregates of calcium crystals were observedin the vacuoles of the mesophyll cells and quantitative X-raymicroanalysis suggested that the chemical composition of thecrystalline aggregates was CaSO₄, 2H₂O. The predominant elementsin the vacuolar sap were magnesium and sulphur, probably presentas MgSO₄, whereas the major elements in the cytoplasm were potassium,sulphur and phosphorus. In Tamarix aphylla the calcium contentof the leaf appears to be regulated by both the secretion ofcalcium salts from the leaf and by intracellular calcificationin mesophyll cells.Copyright 1994, 1999 Academic Press X-ray microanalysis, Tamarix, salt gland, secretion, salts, ions, calcium crystals, compartmentation     

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.     

Electron cytochemistry of oxalate-stimulated calcium uptake in microsomes from the smooth muscle of the pig stomach

Summary A microsomal fraction was isolated from the smooth muscle of the antrum of the pig stomach by differential centrifugation. Electron microscopy of the negatively stained material showed that this fraction is heterogeneous in composition. The microsomes accumulated calcium in the presence of ATP, magnesium and oxalate. The amount of calcium taken up per mg protein was in the same range as observed for other smooth muscle microsomal preparations. Although this amount is much smaller than that in the microsomal fraction of skeletal muscle, calcium oxalate crystals were formed in some vesicles, as occurs in the skeletal muscle fragmented sarcoplasmic reticulum. Through the presence of the calcium oxalate crystals, many of these vesicles acquired sufficient mass and density to allow them to be isolated by centrifugation. A purification of about 40 fold in terms of calcium content was reached.     

A calcium oxalate-secreting tissue in branchlets of the Casuarinaceae

Summary Deciduous branchlets of casuarina trees have an unusual calcium oxalate-secreting system in which the epidermal tissue deposits calcium oxalate crystals in cell walls of the branchlet surface. These prismatic crystals were identified by light and electron microscopy, histochemistry, and elemental X-ray analysis. This calcium oxalate-secreting tissue was found in all species of casuarinas examined, including three of the four genera of the Casuarinaceae:Allocasuarina sp.,Casuarina sp., andGymnostoma papuanum. Because crystals were present throughout the epidermis soon after it formed, the mechanism for their induction was likely to be different than that for calcium oxalate crystal idioblasts. Secreting cells had a complex endoplasmic reticulum that may be involved in the secretory process.Abbreviations EDS energy-dispersive X-ray spectroscopy - HPF/FS high pressure-frozen/freeze-substituted - SEM scanning electron microscopy - TEM transmission electron microscopy Dedicated to the memory of Professor John G. Torrey     

Precipitation of calcium, magnesium, strontium and barium in tissues of four acacia species (leguminosae: mimosoideae)

Precipitation of calcium in plants is common. There are abundant studies on the uptake and content of magnesium, strontium and barium, which have similar chemical properties to calcium, in comparison with those of calcium in plants, but studies on co-precipitation of these elements with calcium in plants are rare. In this study, we compared morphologies, distributional patterns, and elemental compositions of crystals in tissues of four Acacia species grown in the field as well as in the glasshouse. A comparison was also made of field-grown plants and glasshouse-grown plants, and of phyllodes of different ages for each species. Crystals of various morphologies and distributional patterns were observed in the four Acacia species studied. Magnesium, strontium and barium were precipitated together with calcium, mainly in phyllodes of the four Acacia species, and sometimes in branchlets and primary roots. These elements were most likely precipitated in forms of oxalate and sulfate in various tissues, including epidermis, mesophyll, parenchyma, sclerenchyma (fibre cells), pith, pith ray and cortex. In most cases, precipitation of calcium, magnesium, strontium and barium was biologically induced, and elements precipitated differed between soil types, plant species, and tissues within an individual plant; the precipitation was also related to tissue age. Formation of crystals containing these elements might play a role in regulating and detoxifying these elements in plants, and protecting the plants against herbivory.     

The Occurrence, Type and Location of Calcium Oxalate Crystals in the Leaves of Fourteen Species of Araceae

The occurrence, type and location of calcium oxalate crystalsin the leaves of 14 species belonging to the family Araceaewere studied by light microscopy. The Pizzolato test and theRubeanic acid-silver nitrate test, used to chemically identifyand locate the crystals in cross sections of laminae, showedthe presence of four types of crystals: druses, raphides, prismaticsand crystal sand. Styloids were not observed in any of the species.Crystals identified as calcium oxalate were observed in eachtissue layer of the leaf blade, druses occurring more frequentlyin the palisade mesophyll layers, raphides more often in thespongy mesophyll. Prismatics were sparse, occurring in the mesophyllof only two species. Specialized spindle-shaped crystal idioblasts,located in the spongy mesophyll in all cases, were observedin seven of the 14 aroids. Crystal sand and variations in crystalforms were most frequently observed to be calcium compoundsother than calcium oxalate. Crystals, calcium oxalate, idioblasts, Araceae     

草酸钙结晶在几种凤仙花属植物中的特征及其分类学意义

首次研究了7种凤仙花属(ImpatiensL.)植物茎的解剖学及细胞组织中草酸钙结晶的特征.结果表明,7种凤仙花属植物茎的解剖学结构非常近似,而茎中草酸钙结晶特征则差异显著,7种凤仙花属植物茎中均有草酸钙针晶,根据草酸钙结晶形态特征的不同,将针晶分为3种类型,即针晶束、针晶簇和散针晶.其中,黄金凤、长角凤仙花、锐齿凤仙花和红纹凤仙花有针晶束分布,而湖北凤仙花、紫花黄金凤和窄萼凤仙花则无针晶束分布,只有针晶簇或散针晶分布;此外,针晶的形态、长度、排列方式及丰富程度等在不同的物种中亦有差异.草酸钙结晶特征对凤仙花属植物的分类具有一定的科学意义.     

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.     

Functional Aspects of the Salt Glands of the Plumbaginaceae

X-ray microanalysis and diffuse reflectance infrared Fouriertransform spectrometry were used to determine the presence andratios of elements in salt secretions from salt glands of greenhouseand experimentally-manipulated leaves of five species of thePlumbaginaceae Sodium, magnesium, silica, sulphur, phosphorus,chloride, potassium, calcium and carbonate were detected insecretions of greenhouse-grown plants. The salt glands of excisedleaves challenged by solutions of KI, KCl, NaCl, Na₂SO₄, MgCl₂and MgSO₄ secreted principally the ions of the challenging solutions. Key words: Ion transport, secretion     

Comparative leaf anatomy of Salix species and hybrids

Epidermal features, mesophyll differentiation and calcium oxalate characteristics of 19 species and 12 hybrids of Salix are described. The species and hybrids can be distinguished by the presence or absence of the following epidermal features: striated cuticle; stomata; covering trichomes; beaded anticlinal walls, and diosmin-like njstals. In or near marginal teeth, glandular trichomes are present in all cases. The leaf veins of all specimens examined have calcium oxalate prism sheaths and, with the exception of S. herbacea , cluster crystals in some cells of the mesophyll. Most sprcies studied in the subgenus Salix show: both adaxial and abaxial stomata; striated cuticle metopllyll of palisade cells, with little or no spongy mesophyll, but with a well-defined hypodermis, and absence of thick-walled, sinuous trichomes. Characteristic features of the subgenus Caprisalix are: abaxial stomata only; epidermal crystals; smooth cuticle; mesophyll diflerentiated into palisade cells and spongy mesophyll and without a hypodermis, and trichomes more numerous and varied than those of the subgenus Salix . Leaves of the two species of the subgenus Chaemelia examined and those of S. lapponum , have predominantly anomocytic stomata, whereas all the other leaves studied have predominantly paracytic stomata. The anatomical features described, in conjunction with the morphologiral characters, enable the species and hybrids of Salix studied to be autheenticated.     

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.     

Effects of Chemical Speciation on the Mineralization of Organic Compounds by Microorganisms

The mineralization of 1.0 to 100 ng each of four complexing compounds—oxalate, citrate, nitrilotriacetate (NTA), and EDTA—per ml was tested in media prepared in accordance with equilibrium calculations by a computer program so that the H, Ca, Mg, Fe, or Al complex (chemical species) was predominant. Sewage microorganisms mineralized calcium citrate more rapidly than iron, aluminum, or hydrogen citrate, and magnesium citrate was degraded slowest. Aluminum, hydrogen, and iron oxalates were mineralized more rapidly than calcium oxalate, and magnesium oxalate was decomposed slowest. Sewage microorganisms mineralized calcium NTA but not aluminum, magnesium, hydrogen, or iron NTA or any of the EDTA complexes. Pseudomonas sp. mineralized calcium and iron citrates but had no activity on hydrogen, aluminum, or magnesium citrate. Pseudomonas pseudoalcaligenes mineralized calcium, iron, hydrogen, and aluminum citrates but had little activity on magnesium citrate. Pseudomonas alcaligenes used calcium, iron, hydrogen, and aluminum oxalates readily, but it used magnesium oxalate at a slower rate. Listeria sp. destroyed calcium NTA but had no effect on hydrogen, iron, or magnesium NTA. Increasing the Ca concentration in the medium enhanced the breakdown of NTA by Listeria sp. The different activities of the bacterial isolates were not a result of the toxicity of the complexes or the lack of availability of a nutrient element. NTA mineralization was not enhanced by the addition of Ca to Beebe Lake water, but it was enhanced when Ca and an NTA-degrading inoculum were added to water from an oligotrophic lake. The data show that chemical speciation influences the mineralization of organic compounds by naturally occurring microbial communities and by individual bacterial populations.     

Calcium oxalate crystals in fetal bovine serum: implications for cell culture, phagocytosis and biomineralization studies in vitro

Cell culture methods and models are key investigative tools for cell and molecular biology studies. Fetal bovine serum (FBS) is commonly used as an additive during cell culture since its constituents promote cell survival, proliferation and differentiation. Here we report that commercially available FBS from different major suppliers consistently contain precipitated, calcium oxalate crystals-either in the monohydrate (COM) or dihydrate (COD) form. Mineral structure and phase identification of the crystals were determined by X-ray diffraction, chemical composition by energy-dispersive X-ray microanalysis, and imaging and measurement of crystal growth steps by atomic force microscopy-all identified and confirmed crystallographic parameters for COM and COD. Proteins binding to the crystals were identified by immunoblotting, revealing the presence of osteopontin and fetuin-A (alpha(2)HS-glycoprotein)--known regulators of crystal growth found in serum. Macrophage cell cultures exposed to calcium oxalate crystals showed internalization of the crystals by phagocytosis in a process that induced disruption of cell-cell adhesion, release of reactive oxygen species and membrane damage, events that may be linked to the release of inflammatory cytokines by these cells into the culture media. In conclusion, calcium oxalate crystals found in commercially available FBS are toxic to cells, and their presence may confound results from in vitro studies where, amongst others, phagocytosis, biomineralization, renal cell and molecular biology, and drug and biomaterial testing are being examined.     

Crystals in tapetal cells of the Leguminosae

In a survey of the Leguminosae (167 species of 89 genera), calcium oxalate crystals were found in tapetal cells in all three subfamilies (84 species of 52 genera). Crystal form ranged from small scattered crystals to lens-like to various large prismatic types, and included the first report of styloid crystals in the Caesalpinioideae. Over half of the caesalpinioid and papilionoid legumes examined had crystals. Crystals were not common in the Mimosoideae, however, but this may be because of the small sample. The distribution of species with various crystal types, and of species lacking crystals, did not reveal any patterns that conform to the presently defined taxa. Crystals in tapetal cells have previously been reported only in the Commelinaceae and Labiatae.