Crystal macropatterns in leaves of Fagaceae and Nothofagaceae: a comparative study

Summary Crystal macropatterns in Fagaceae and Nothofagaceae were examined from cleared herbarium leaves (eight genera, 122 spp.) by polarizing microscopy. Prisms and druses dominate, but previously undescribed intermediate forms occur in 25 species of Fagaceae. Sixty-two species had only prisms associated with vein orders 1–4, but smallest orders 5 and 6 had few or no crystals. In mesophyll, 98 species had small druses in spongy parenchyma and larger but fewer druses in palisade parenchyma. Subfamily Fagoideae conformed closely to this macropattern, Castaneoideae less so. Six Castaneoideae species lacked vein crystals. Two Fagoideae species and seven Nothofagus species lacked mesophyll crystals. Druses with prominent cores occur throughout Fagaceae but none were seen in Nothofagaceae. Tabular presentation of results shows significant although overlapping trends from Fagoideae to Castaneoideae to Nothofagaceae, with the latter taxon deviating most from Fagaceae.     

Leaf anatomy ofDombeya andNesogordonia (Sterculiaceae), emphasizing epidermal and internal idioblasts

We studied leaf anatomy, using clearings, resin sections, and scanning electron microscopy, from mostly herbarium specimens of 123 species ofDombeya and 11 species ofNesogordonia (Sterculiaceae). Species were placed in seven idioblast categories, ranging from those without any to single and bicelled epidermal forms to multicelled nodules and single mesophyll idioblasts. Idioblast contents are possibly mucilaginous, but were not identified. In these two genera the range of foliar idioblast morphology surpasses that known previously for the entire family. Leaves are dorsiventral with mostly abaxial anomocytic stomata and typical palisade and spongy layers; paraveinal mesophyll is lacking. Miniature glandular (clavates, capitates) and nonglandular (mostly stellate) trichomes occur. Prismatic crystals predominate; epidermal prismatics and mesophyll druses are rare.     

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     

Calcium oxalate crystal types and trends in their distribution patterns in leaves ofPrunus (Rosaceae: Prunoideae)

Calcium oxalate crystal types and distribution within leaves ofPrunus sensu lato (Rosaceae; Prunoideae) were surveyed from mostly herbarium specimens (196 specimens of 131 species of all five subgenera usually recognized). Rehydrated samples were bleached, mounted unstained, and viewed microscopically between crossed polarizers. Six patterns were recognized based on crystal type and relative distribution around veins and in mesophyll. Druses predominate in four subgenera, but prismatics are most common in subgenus Padus. Prunophora and Amygdalus, considered to be the most advanced subgenera, have virtually only druses, which are almost always associated with veins. Cerasus and Laurocerasus, intermediate subgenera, have the greatest diversity of patterns, but few species with prismatics. A trend is evident from mostly mesophyll prismatics in Padus to fewer prismatics and more druses of mixed distribution in Laurocerasus and Cerasus, to mostly druses restricted to veins in Amygdalus and Prunophora.     

芋营养器官中的草酸钙晶体及其可能的生理作用

利用徒手切片,在光学显微镜下对芋(Colocasia esculenta(L.)Schott)营养器官中晶体的类型和分布进行了观察和研究,并用化学方法对晶体的化学成分进行了鉴定。结果表明,芋营养器官中的晶体为草酸钙结晶体,形态上可以分为针晶和簇晶两大类。含针晶束的异细胞有3种类型:含发射型草酸钙针晶束异细胞(存在于叶片、叶柄、块茎中),含大型草酸钙针晶束异细胞(存在于叶片、叶柄、块茎、块茎皮中),含大量草酸钙针晶的管状异细胞(仅存在于不定根中)。草酸钙针晶也有散乱分布于块茎和不定根中的。草酸钙簇晶在叶片、叶柄、块茎、块茎皮、不定根中均有分布,且叶片、叶柄、块茎皮中的簇晶比块茎和不定根中的尖锐。芋营养器官中的草酸钙晶体很可能是作为一种防御机制,防止动物的取食。     

虎掌（天南星科）中草酸钙晶体的形态和分布

在光学显微镜下对虎掌（Pinellia pedatisecta）营养器官和繁殖器官中晶体的类型和分布进行了观察和分析,探讨晶体的功能与作用机制。结果表明：（1）虎掌各个器官中都发现有晶体,且晶体类型有针晶、簇晶、砂晶和柱晶4种形态,其中针晶最为常见。（2）虎掌叶中的晶体大多以针晶状分布在叶片上表皮下的叶肉中,少数分布在叶下表皮下的叶肉中,其次砂晶和星芒状簇晶也在叶中较常见,叶中也有少量的柱晶。（3）虎掌的块茎中分布有大量的针晶束,在输导组织附近还有一些大的簇晶;虎掌的不定根中分布有不整齐的针晶和排列不规则的针晶束以及少量大的簇晶。（4）虎掌的佛焰苞中分布有针晶、簇晶和砂晶,且在佛焰苞中的针晶主要分布于上、下表皮之下的叶肉中,砂晶多分布在佛焰苞的上、下表皮上。（5）虎掌的花药壁中分布有针晶束,其方向和花药壁表面垂直,而花粉囊中只有小的簇晶。（6）虎掌的果皮和种皮上分布有大量的针晶。根据晶体在酸中的溶解性,虎掌体内所有晶体的化学成分都为草酸钙。研究认为,虎掌各个器官中的各种草酸钙晶体对于保护虎掌免受食草动物取食具有重要的作用。     

Crystal macropattern development in Prunus serotina (Rosaceae, Prunoideae) leaves

BACKGROUND AND AIMS: Prunus, subgenus Padus, exhibits two completely different calcium oxalate crystal macropatterns in mature leaves. Foliar macropattern development has been described previously in P. virginiana, representing one version. Prunus serotina, in the group exhibiting the second macropattern, is described here. The goal was to describe developmental details for comparison with P. virginiana, and to extend the sparse current knowledge of crystal macropatterns. METHODS: Leaves at various developmental stages were removed from local trees and from herbarium specimens. Early leaf stages and freehand leaf and stem sections were mounted directly in aqueous glycerine; larger leaves were processed whole or in representative pieces in household bleach, dehydrated in alcohol/xylol, and mounted in Permount. Crystals were detected microscopically between crossed polarizers. KEY RESULTS: Bud scales have a dense druse population. Druses appear first at the stipule tip and proliferate basipetally but soon stop forming; growing stipules therefore have a declining density of druses. Druses appear at the tip of leaves <1 mm long, then proliferate basipetally in the midrib. Lamina druses appear in the distal marginal teeth of leaves 3 cm long; from here they proliferate basipetally and towards midrib along major veins. In about two-thirds-grown leaves (6-9 cm length) druses are all adaxial to veins of most orders; a shift occurs then to formation of prisms, which appear first abaxial to, then all around, veins. Mature leaves have virtually all prisms encrusting all major veins, more sparsely along smaller minor veins. Late season leaves form epitactic crystals on existing prismatics. CONCLUSIONS: The developing and mature macropattern of P. serotina is almost the reverse of the pattern described previously in P. virginiana, and shows that two closely related species can develop radically different modes of crystallization. The few detailed macropattern studies to date reveal striking variations that indicate a new level of organization that must be integrated with the anatomical, physiological and molecular approaches that have been dominant so far.     

Calcium-induced patterns of calcium-oxalate crystals in isolated leaflets of Gleditsia triacanthos L. and Albizia julibrissin Durazz

For experimental induction of crystal cells (=crystal idioblasts) containing calcium-oxalate crystals, the lower epidermis was peeled from seedling leaflets of Gleditsia triacanthos L., exposing the crystal-free mesophyll and minor veins to the experimental solutions on which leaflets were floated for up to 10 d under continous light. On 0.3–2.0 mM Ca-acetate, increasing numbers of crystals, appearing 96 h after peeling, were induced. The pattern of crystal distribution changed with Ca²⁺-concentration ([Ca²⁺]): at low [Ca²⁺], crystals formed only in the non-green bundlesheath cells surrounding the veins, believed to have a relatively low Ca²⁺-extrusion capacity; at higher [Ca²⁺], crystals developed in up to 90% of the mesophyll cells, and at supraoptimal [Ca²⁺], large extracellular crystals formed on the tissue surface. By sequential treatments with solutions of different [Ca²⁺], the following three phases were identified in the induction of crystal cells: (1) during the initial 24-h period (adaptive aging), Ca²⁺ is not required and crystal induction is not possible; (2) during the following 48 h (induction period), exposure to 1–2 mM Ca-acetate induces the differentiation of mesophyll cells into crystal cells; (3) crystal growth begins 72 h after the start of induction. In intact leaflets of Albizia julibrissin Durazz., calcium-oxalate crystals are found exclusively in the bundle-sheath cells of the veins, but crystals were induced in the mesophyll of peeled leaflets floating on 1 mM Ca-acetate. Exposure to inductive [Ca²⁺] will thus trigger the differentiation of mature leaf cells into crystal cells; the spatial distribution of crystals is determined by the external [Ca²⁺] and by the structural and functional properties of the cells in the tissue.     

Leaf anatomical studies of Chamaecrista subsect. Baseophyllum (Leguminosae, Caesalpinioideae): new evidence for the up-ranking of the varieties to the species level

This study aims to determine whether morphoanatomical characters of the leaves of the species of Chamaecrista sect. Absus subsection Baseophyllum could be used to support an up-ranking of C. cytisoides varieties to the species level as previously defined by molecular studies. The significance of anatomical adaptive strategies to arid environments is also discussed. Standard light microscopy techniques and histochemical tests were used for both morphoanatomical and histochemical characterization of the leaves. All the species studied share a single-layered epidermis, actinodromous–camptodromous–brochidodromous type of venation, vascular bundles surrounded by layers of fibers bounded externally by a sheath of cells containing solitary crystals, enlarged tracheids at the vein endings, vascular petiole/rachis tissue with a parenchymatous pith, accessory vascular bundles, mucilage idioblasts and hypodermis in the mesophyll, colleters, and non-secretory trichomes. The position and type of stomata, type of mesophyll, number of palisade and spongy parenchyma layers, position of mucilage idioblasts in the mesophyll, and the number of accessory vascular bundles of petiole/rachis provided useful characters for discriminating the eight species of the subsect. Baseophyllum. Histochemical tests reveal the presence of total polysaccharides, pectins, mucilage and phenolic compounds in the idioblasts. Other xeromorphic characters such as thickened outer periclinal cell walls, compact mesophyll, mucilage idioblasts and hypodermis in the mesophyll may help enable the studied species to survive in exposed sunny areas.     

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.     

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     

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。     

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.     

Cellular ultrastructure and crystal development in Amorphophallus (Araceae)

Background and Aims: Species of Araceae accumulate calcium oxalate in the form ofcharacteristically grooved needle-shaped raphide crystals andmulti-crystal druses. This study focuses on the distributionand development of raphides and druses during leaf growth inten species of Amorphophallus (Araceae) in order to determinethe crystal macropatterns and the underlying ultrastructuralfeatures associated with formation of the unusual raphide groove. Methods: Transmission electron microscopy (TEM), scanning electron microscopy(SEM) and both bright-field and polarized-light microscopy wereused to study a range of developmental stages. Key Results: Raphide crystals are initiated very early in plant development.They are consistently present in most species and have a fairlyuniform distribution within mature tissues. Individual raphidesmay be formed by calcium oxalate deposition within individualcrystal chambers in the vacuole of an idioblast. Druse crystalsform later in the true leaves, and are absent from some species.Distribution of druses within leaves is more variable. Drusesinitially develop at leaf tips and then increase basipetallyas the leaf ages. Druse development may also be initiated incrystal chambers. Conclusions: The unusual grooved raphides in Amorphophallus species probablyresult from an unusual crystal chamber morphology. There aremultiple systems of transport and biomineralization of calciuminto the vacuole of the idioblast. Differences between raphideand druse idioblasts indicate different levels of cellular regulation.The relatively early development of raphides provides a defensivefunction in soft, growing tissues, and restricts build-up ofdangerously high levels of calcium in tissues that lack theability to adequately regulate calcium. The later developmentof druses could be primarily for calcium sequestration.     

Crystal diversity and macropatterns in leaves of Oleaceae

Oleaceae leaves surveyed from herbarium specimens of 240 species from 23 genera were rehydrated, bleached, processed into xylol, mounted unstained, and viewed microscopically between crossed polarizers. Occurrence of five crystal types and two variants (tiny acicular crystals and sphaerites) within one family is unusual. Number of crystal types within a single species was one (108 spp.), two (53 spp.), three (51 spp.), four (15 spp.), and five (6 spp.). Seven species lacked crystals. The tiny acicular crystal variant was most common (167 spp.), followed by prisms (67 spp.), raphides (65 spp.), druses (61 spp.), sphaerites variant (50 spp.), styloids (36 spp.), and crystal sand (21 spp.). Epidermal crystals were common (155 spp.), with epidermal crystals clustering at base of trichomes in 21 species. Jasminum was exceptional in having mostly druses and almost no crystals around vascular bundles. Most Oleaceae crystals are tiny, usually about 5 μm in length, except for larger styloids and raphides.     

New and unusual forms of calcium oxalate raphide crystals in the plant kingdom

Calcium oxalate crystals in higher plants occur in five major forms namely raphides, styloids, prisms, druses and crystal sand. The form, shape and occurrence of calcium oxalate crystals in plants are species- and tissue-specific, hence the presence or absence of a particular type of crystal can be used as a taxonomic character. So far, four different types of needle-like raphide crystals have been reported in plants. The present work describes two new and unusual forms of raphide crystals from the tubers of Dioscorea polystachya—six-sided needles with pointed ends (Type V) and four-sided needles with beveled ends (Type VI). Both of these new types of needles are distinct from the other four types by each having a surrounding membrane that envelopes a bundle of 10–20 closely packed thin crystalline sheets. The previously known four types of needles have solid or homogenous crystalline material, surrounded by a membrane or lamellate sheath called a crystal chamber. Only the Type VI crystals have beveled ends and the needles of the other five types have pointed ends.     

On the formation of the pattern of crystal idioblasts — in Canavalia ensiformis DC

Summary Light and electron-microscope observations were made of the crystal idioblasts in the leaves of Canavalia. The crystal-containing cells occur as pairs in which the crystals, nuclei, and the majority of the chloroplasts are symmetrically arranged with regard to the common wall. The chloroplasts are found in the cytoplasm along this wall.The crystals originate in a vacuole. The space in which the young crystal develops is delimited by a membrane. One to several additional membranes surround the crystal inside the vacuole. Numerous vesicles are distributed between these vacuolar membranes. Dense groups of tubules or fibrils are oriented toward a portion of the crystal surface, suggesting that the material forming the crystal might be transported to the surface by these structures.The cytoplasm of the young idioblasts contains many mitochondria and dictyosomes with associated vesicles. Concentrations of what is assumed to be protein are present in the cytoplasm. These protein accumulations are not seen in neighboring cells, suggesting that protein synthesis is especially high in the idioblasts.In older crystal cells, layers of wall material are deposited on the wall between the two crystals of the pair and towards the cell wall adjacent to the mesophyll. Not only does the original wall become thickened but a new wall develops at the border of the crystal vacuole. Eventually this wall material becomes continuous and the crystal becomes, on two sides, directly connected with the wall.     

Diversity and distribution of idioblasts producing calcium oxalate crystals in Dieffenbachia seguine (Araceae)

Although cells that synthesize crystals are known throughout the plant kingdom, their functional significance is still unknown. Mechanical support, mineral balance, waste sequestration, and protection against herbivores have all been proposed as crystal functions. To seek clues to their role(s), I systematically examined all organs except fruit of Dieffenbachia seguine (Araceae) for crystals. Crystals were found in nearly every organ. Raphides (long, slim, pointed crystals) were most common, but druses (crystal aggregates) and prisms were also found. Raphides varied in size by a factor of 10 and also in organization from tightly bundled to loosely organized. Biforines, a type of cell capable of expelling raphides, or biforine-like cells, were found in nearly all organs, but especially in leaves, spathes, and anthers. Different organs had different crystal complements, and characteristic crystals were found at specific locations, such as among pollen, along the undersides of leaf veins, and at root branch points. All crystals appeared to be composed of calcium oxalate, based on acid solubility. Possible roles of the crystals are discussed in light of these findings.     

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.