Clave polínica de las Ericaceae gallegas

Se ha realizado una clave polínica de las Ericaceae gallegas en relación a los caracteres morfológicos que fueron observados al microscópio óptico. Dicho estudio permitió diferenciar, desde un punto de vista polínico ocho especies y dos tipos (Erica cinerea y Vaccinium myrtillus) con cinco y dos especies respectivamente.

Contribución al conocimiento melitopalinológico de Sierra Morena

Sc ha estudiado al microscopio óptico el sedimento de once muestras de miel de diversas localidades del este de Sierra Morena. Se pone de manifiesto que, en este área, el néctar de flores es la principal fuenle de miel para Apis mellifera,siendo la mielada poco importante. Echium plantagineum, Lavandula stoechas y Eucalyptus camaldulensis son las principales fuentes de miel en este área, en tanto que Cistus ladanifer, C. albidus, Olea europaea y Quercus sp. lo son de polen.

Contribución al conocimiento del polen y de las semillas del género Spergularia en Andalucía occidental

Se estudia al microscopio óptico y al microscopio electrónico de barrido el polen y las semillas de los nueve taxones del género Spergularia representados en Andalucía occidental. El polen resulta ser variable en tamaño y morfología, por lo que su interés taxonómico es sólo relativo si se compara con el de las semillas, que constituyen un carácter útil para la separación de taxones. Se elabora una clave dicotómica para la separación de las especies en función de los caracteres estudiados.

Riella notarisii (Mont.) a Menorca

Se cita por primera vez en Baleares (Barranc d’Aljandar-Menorca) Riella notarisii (Mont.) Mont. Se hace referencia a su situación taxonómica actual. El estudio de las esporas al microscopio óptico y al microscopio electrónico de barrido ha hecho posible una descripción de las mismas. Se incluye un esquema de la especie y fotografías de las esporas.

On the microstructure, growth pattern and original porosity of belemnite rostra: insights from calcitic Jurassic belemnites

Calcitic belemnite rostra are usually employed to perform paleoenvironmental studies based on geochemical data. However, several questions, such as their original porosity and microstructure, remain open, despite they are essential to make accurate interpretations based on geochemical analyses.This paper revisits and enlightens some of these questions. Petrographic data demonstrate that calcite crystals of the rostrum solidum of belemnites grow from spherulites that successively develop along the apical line, resulting in a “regular spherulithic prismatic” microstructure. Radially arranged calcite crystals emerge and diverge from the spherulites: towards the apex, crystals grow until a new spherulite is formed; towards the external walls of the rostrum, the crystals become progressively bigger and prismatic. Adjacent crystals slightly vary in their c-axis orientation, resulting in undulose extinction. Concentric growth layering develops at different scales and is superimposed and traversed by a radial pattern, which results in the micro-fibrous texture that is observed in the calcite crystals in the rostra.Petrographic data demonstrate that single calcite crystals in the rostra have a composite nature, which strongly suggests that the belemnite rostra were originally porous. Single crystals consistently comprise two distinct zones or sectors in optical continuity: 1) the inner zone is fluorescent, has relatively low optical relief under transmitted light (TL) microscopy, a dark-grey color under backscatter electron microscopy (BSEM), a commonly triangular shape, a “patchy” appearance and relatively high Mg and Na contents; 2) the outer sector is non-fluorescent, has relatively high optical relief under TL, a light-grey color under BSEM and low Mg and Na contents. The inner and fluorescent sectors are interpreted to have formed first as a product of biologically controlled mineralization during belemnite skeletal growth and the non-fluorescent outer sectors as overgrowths of the former, filling the intra- and inter-crystalline porosity. This question has important implications for making paleoenvironmental and/or paleoclimatic interpretations based on geochemical analyses of belemnite rostra.Finally, the petrographic features of composite calcite crystals in the rostra also suggest the non-classical crystallization of belemnite rostra, as previously suggested by other authors.