Silicon Distribution and Anatomy of the Grass Rhizome, with Special Reference to Miscanthus sacchariflorus (Maxim.) Hackel.

Rhizome anatomy is described for Miscanthus sacchariflorus (Maxim.)Hackel. Solid silica deposits, detected as elemental siliconby electron-probe microanalysis and energy-dispersive X-rayanalysis, are confined to cell walls of three concentric zonesconsisting of the uniseriate epidermis, and parenchyma layersaround the cortical air lacunae, and the central cavity, respectively.Si is localized in outer tangential walls of the epidermis,while occurring in all walls of nucleated, parenchyma cellsforming the two internal zones. In comparison, the root exhibitsonly one Si zone. Rhizome Si distribution more closely resemblesthat for Phragmites australis, than for related members of theAndropogoneae. P. australis similarly exhibits aerenchyma anda central cavity. Thus, internal anatomy may strongly influencesilicon distribution. A comparison of taxa of four tribes indicatesthat epidermal wall deposition is common, followed by specificinternal localization in up to three zones of perivascular tissues. Silicon accumulation occurs early in the epidermis of the youngapex of M. sacchariflorus, decreasing sharply across an internodetransection. In comparison, the oldest, basal internodes exhibitvery high Si X-ray counts in each of the three zones, the highestoccurring in the most internal zone around the central cavity.Early Si mobilization in the rhizome apex may resist shearingand abrasion during horizontal growth extension, while depositsbordering aerenchyma of older internodes may resist compression. Miscanthus sacchariflorus (Maxim.) Hackel, plume grass, rhizome, silicification, anatomy, aerenchyma     

Observations on the Distribution of Mineral Elements in the Leaf of Wheat (Triticum aestivum L.), with Particular Reference to Silicon

Wheat (Triticum aestivum L. cv. Wheaton) plants were grown inwater culture or in soil. Basal leaves (B) were harvested after3 weeks from the water culture plants, while flag leaves werecollected from soil-grown material at the time of inflorescenceemergence (E0) and 7 d after emergence (E + 7). Mineral distributionin bulk frozen leaves was investigated using SEM and X-ray microanalysis.The elements detected were silicon, phosphorus, chlorine, sulphur,potassium and calcium. Potassium was present in all cell typesat all harvests, chlorine was almost entirely confined to theadaxial and abaxial epidermi, while sulphur was only rarelydetected in the E0 and E + 7 leaves. Phosphorus was presentat higher levels in the E + 7 leaves than in the B or E0 leaves.At the B harvest calcium was confined to the adaxial epidermalcells, but in the E0 and E + 7 leaves it was present in bothepidermi. Silicon was, initially, mainly detected in the abaxialepidermal cells, but in older (E + 7) leaves it was presentin both epidermi and in some internal tissues. Mineral transportwithin the leaf and ionic environment at silica deposition sitesare discussed. Wheat, Triticum aestivum L., leaf, mineral distribution, X-ray microanalysis, silicon, calcium     

Silicon Deposition in the Inflorescence Bristles and Macrohairs of Setaria italica (L.) Beauv.

Silicon deposits in the inflorescence bristles subtending eachspikelet, and in the macrohairs of foxtail millet (Setaria italica(L.) Beauv.) were investigated using scanning electron microscopyand electron-probe microanalysis. High concentrations of silicon were detected in the pricklehairs which covered the bristles. In the unicellular macrohairscovering the inflorescence axis and its branches, silicon wasdeposited along the whole length of the hairs. The mechanisms by which silicification may have taken place,and the possibility that the bristles and macrohairs are involvedin the aetiology of oesophageal cancer in N. China are discussed. Setaria italica (L.) Beauv., foxtail millet, millet, silicon deposits, silicification, prickle hairs, scanning electron microscopy, electron-probe microanalysis     

Studies of Opaline Silica Deposits in the Leaf of Sieglingia decumbens L. 'Bernh.', using the Scanning Electron Microscope

Opaline silica deposits (phytoliths) of intracellular originwere photographed at magnifications up to 10⁴ diameters. Becauseof the great depth of focus of the scanning microscope the phytolithswere visible in three-dimensional aspect. They were solid witha possible porous internal structure, and some possessed diagonalstriae on the outer surface. The structural features revealedare related to phytolith models previously postulated from lightmicroscope studies, and to secondary cell-wall structure. Theporous internal structure is discussed in relation to possiblephysico-chemical formative processes.