diversidad de inclusiones minerales en la subtribu oncidiinae (orchidaceae)

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ID: 167509
2010
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Abstract
Las inclusiones minerales en las plantas, han sido utilizadas como herramientas de diagnóstico en la identificación taxonómica. Se analizaron y compararon las inclusiones minerales en las hojas de 140 especies de Oncidiinae (Epidendroideae: Orchidaceae). Las secciones transversales de hojas se observaron para describir las inclusiones minerales con el apoyo de la microscopía de luz en campo claro, contraste de fases y polarización. Los cristales generalmente están presentes en las células del mesófilo, y sólo dos especies los presentan en las células epidérmicas. Se encontraron cristales de oxalato de calcio de diferentes formas y depósitos de dióxido de sílice en forma de estégmatos. Las formas cristalinas más comunes son rafidios, prismas y drusas. Sin embargo, algunas especies tienen cristales en arena, concéntricos o en placas radiales. En esta investigación se reportan las dos últimas por primera vez para Oncidiinae y también para Orchidaceae. Los estégmatos son cónicos con superficie rugosa, generalmente formando hileras a lo largo de las fibras. Comúnmente se presentan en los haces vasculares y en los haces de fibras abaxiales. Sin embargo, existen especies cuyos haces de fibras no tienen estégmatos, así como especies sin haces de fibras ni estégmatos. Se discute la importancia taxonómica de estas inclusiones minerales para los diferentes clados, géneros y/o especies de Oncidiinae.
Diversity of mineral inclusions in the subtribe Oncidiinae (Orchidaceae). Mineral inclusions in plants, of different chemical constitution and forms, have been studied in some plant groups and are currently used as diagnostic tools in taxonomic identifications. With the aim to identify their possible application in taxonomy, mineral inclusions in the leaves of 140 species of Oncidiinae (Orchidaceae) were analyzed and compared. Leave transversal sections were studied with the aid of clear field, phase contrast, and polarized light microscopy. Crystals commonly occured in mesophyll cells, and only in two species those were observed in epidermal cells. Several forms of calcium oxalate crystals and silicdioxide deposits in the form of stegmata were found. The most common crystalline forms were raphides, prisms and druses. Nevertheless, crystals like sands, and concentric and radial plates were also observed in few species. These crystalline forms of concentric and radial plates are reported for the first time in Oncidiinae and Orchidaceae. The stegmata are conical with rough surface, forming tiers along with fibers. Stegmata commonly occur in the vascular bundle sheath and in the abaxial or adaxial fiber bundles. However, few species do not have stegmata in fiber bundles and other species lack both. The taxonomic importance of these mineral inclusions is discussed for the different clades, genera or species within the subtribe Oncidiinae. Rev. Biol. Trop. 58 (2): 733-755. Epub 2010 June 02.
Reference Key
sandoval-zapotitla2010revistadiversidad Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors ;Estela Sandoval-Zapotitla;Teresa Terrazas;José Luís Villaseñor
Journal science journal of university of zakho
Year 2010
DOI
DOI not found
URL
http://www.scielo.sa.cr/scielo.php?script=sci_arttext&pid=S0034-77442010000200016
Keywords
leaf silica orchidaceae crystals

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