Yenny Beltrán-Magos’s research while affiliated with National Autonomous University of Mexico and other places

Populations of the benthic diazotrophic cyanobacterium Hydrocoleum Kützing (1843) are widely distributed in coral reefs and lagoons of tropical oceans, where they contribute to benthic nitrogen fixation. We compared the morphological, molecular and physiological features of 31 freshwater and marine Hydrocoleum populations from geographically different localities and five specimens from herbaria. Our aims were to compare the features of Hydrocoleum with the morphologically and phylogenetically related genera Trichodesmium Ehrenberg ex Gomont 1892 and Blennothrix Kützing 1843, and to provide the basis for the validity of the genus Hydrocoleum. The Hydrocoleum populations were distributed over a wide range of sizes, showing no consistent inter-population grouping and leaving no gaps between groups that were traditionally attributed to different species. Transmission electron microscopy showed regular cell division rhythms in all Hydrocoleum populations with each cell division completed before the next one was initiated, similar to that described for Trichodesmium. In contrast, Blennothrix populations exhibited multiple initiation of cross-wall formation. Most Hydrocoleum populations fixed nitrogen at consistently higher nightly rates. The phylogenetic analysis of 16S rRNA and nifH gene sequences placed all morphologically distinct Hydrocoleum and Trichodesmium populations within a tight cluster. Neither of the analysed genes brought any further resolution of phenotypically and ecologically distinguished forms. However, freshwater morphospecies of Blennothrix together with the type species Blennothrix vermicularis Kützing were separated from the Trichodesmium/Hydrocoleum cluster, which further supported the genotypic distinction between the compared taxa, in addition to the fact that they also differ in morphology and ecology. We concluded that the genus Hydrocoleum possesses unique features that warrant its maintenance in the botanical classification system and that its introduction in bacteriological manuals as a valid cyanobacterial genus is acceptable.

Geochemical, mineralogical and microbiological data from four freshwater streams in central region of Mexico indicate the importance of Blennothrix ganeshii mats (Cyanobacteria, Oscillatoriales) in promoting the formation of calcium carbonate crystals. The streams were characterized by alkaline waters and relative physicochemical stability during three seasons (cold dry, warm dry and warm rainy). Calcification took the form of a thick, dense layer of calcium carbonate crystals surrounding the extracellular polymeric substances produced by B. ganeshii filaments, giving an appearance of micritic tubes (structures formed by crystallization in the spaces between filaments) along the sheath surfaces. The precipitate was analyzed using X-ray diffraction and energy dispersal X-ray spectrometry, and the calcite crystal habit was determined. The photosynthetic activity of cyanobacterial growth and the presence of abundant extracellular polymeric substances and epiphytic species promote the absorption of ions and mineral nucleation on the surface of the sediment and contribute to the formation of travertine in tropical regions.

García. 2013. Calcification of the filamentous cyanobacterium Blennothrix ganeshii in calcareous tropical streams of central Mexico region. Hidrobiológica 23 (1): 17-27. ABSTRACT Geochemical, mineralogical and microbiological data from four freshwater streams in central region of Mexico indicate the importance of Blennothrix ganeshii mats (Cyanobacteria, Oscillatoriales) in promoting the formation of calcium car-bonate crystals. The streams were characterized by alkaline waters and relative physicochemical stability during three seasons (cold dry, warm dry and warm rainy). Calcification took the form of a thick, dense layer of calcium carbonate crystals surrounding the extracellular polymeric substances produced by B. ganeshii filaments, giving an appearance of micritic tubes (structures formed by crystallization in the spaces between filaments) along the sheath surfaces. The precipitate was analyzed using X-ray diffraction and energy dispersal X-ray spectrometry, and the calcite crystal habit was determined. The photosynthetic activity of cyanobacterial growth and the presence of abundant extracellular polymeric substances and epiphytic species promote the absorption of ions and mineral nucleation on the surface of the sediment and contribute to the formation of travertine in tropical regions. RESUMEN Los datos geoquímicos, mineralógicos y microbiológicos en cuatro ríos de agua dulce de la región central de México, ponen de manifiesto la importancia de las matas de Blennothrix ganeshii (Cianobacteria, Oscillatoriales) como promo-toras de la formación de cristales de carbonato de calcio. Los ríos se caracterizaron por presentar aguas alcalinas y una relativa estabilidad fisicoquímica durante tres estaciones del año (seca fría, seca templada y lluviosa templada). La calcificación estuvo caracterizada como una densa y gruesa capa de cristales de carbonato de calcio que rodean el mucílago extracelular producido por los filamentos de B. ganeshii, dando la apariencia de tubos micríticos (estructuras formadas por un material cristalizado en las hendiduras existentes entre filamentos) a lo largo de la superficie de la vaina. El precipitado fue identificado como calcita por su hábito cristalino típico y por análisis de difracción de rayos-X y espectrometría de dispersión de energía de rayos X. La actividad fotosintética de los crecimientos de la cianobac-teria y la presencia de abundantes sustancias poliméricas extracelulares y especies epífitas promueven la absorción de iones y nucleación de minerales en la superficie del sedimento y contribuyen a la construcción de travertino en corrientes de regiones tropicales.

Geochemical, mineralogical and microbiological data from four freshwater streams in central region of Mexico indicate the importance of Blennothrix ganeshii mats (Cyanobacteria, Oscillatoriales) in promoting the formation of calcium carbonate crystals. The streams were characterized by alkaline waters and relative physicochemical stability during three seasons (cold dry, warm dry and warm rainy). Calcification took the form of a thick, dense layer of calcium carbonate crystals surrounding the extracellular polymeric substances produced by B. ganeshii filaments, giving an appearance of micritic tubes (structures formed by crystallization in the spaces between filaments) along the sheath surfaces. The precipitate was analyzed using X-ray diffraction and energy dispersal X-ray spectrometry, and the calcite crystal habit was determined. The photosynthetic activity of cyanobacterial growth and the presence of abundant extracellular polymeric substances and epiphytic species promote the absorption of ions and mineral nucleation on the surface of the sediment and contribute to the formation of travertine in tropical regions.

Beltrán-Magos, Y, J. Carmona, G. Vilaclara and M. Bojorge-García. 2013. Calcification of the filamentous cyanobacterium Blennothrix ganeshii in calcareous tropical streams of central Mexico region. Hidrobiológica 23 (1): XXX-XXX. ABSTRACT Geochemical, mineralogical and microbiological data from four freshwater streams in central region of Mexico indicate the importance of Blennothrix ganeshii mats (Cyanobacteria, Oscillatoriales) in promoting the formation of calcium car-bonate crystals. The streams were characterized by alkaline waters and relative physicochemical stability during three seasons (cold dry, warm dry and warm rainy). Calcification took the form of a thick, dense layer of calcium carbonate crystals surrounding the extracellular polymeric substances produced by B. ganeshii filaments, giving an appearance of micritic tubes (structures formed by crystallization in the spaces between filaments) along the sheath surfaces. The precipitate was analyzed using X-ray diffraction and energy dispersal X-ray spectrometry, and the calcite crystal habit was determined. The photosynthetic activity of cyanobacterial growth and the presence of abundant extracellular polymeric substances and epiphytic species promote the absorption of ions and mineral nucleation on the surface of the sediment and contribute to the formation of travertine in tropical regions. RESUMEN Los datos geoquímicos, mineralógicos y microbiológicos en cuatro ríos de agua dulce de la región central de México, ponen de manifiesto la importancia de las matas de Blennothrix ganeshii (Cianobacteria, Oscillatoriales) como promo-toras de la formación de cristales de carbonato de calcio. Los ríos se caracterizaron por presentar aguas alcalinas y una relativa estabilidad fisicoquímica durante tres estaciones del año (seca fría, seca templada y lluviosa templada). La calcificación estuvo caracterizada como una densa y gruesa capa de cristales de carbonato de calcio que rodean el mucílago extracelular producido por los filamentos de B. ganeshii, dando la apariencia de tubos micríticos (estructuras formadas por un material cristalizado en las hendiduras existentes entre filamentos) a lo largo de la superficie de la vaina. El precipitado fue identificado como calcita por su hábito cristalino típico y por análisis de difracción de rayos-X y espectrometría de dispersión de energía de rayos X. La actividad fotosintética de los crecimientos de la cianobac-teria y la presencia de abundantes sustancias poliméricas extracelulares y especies epífitas promueven la absorción de iones y nucleación de minerales en la superficie del sedimento y contribuyen a la construcción de travertino en corrientes de regiones tropicales.

Microhabitat was investigated in four populations of B. ganeshii in calcareous tropical streams in central Mexico to determine the distributional patterns and some of their controlling factors, as well as morphometric adaptations to varying conditions on scales of a few centimetres. Morphometric variations and their relation to physical variables (current velocity, depth, irradiance, and type of substratum) revealed some characteristics for each population and indicated particular adaptations: current velocity was negatively correlated with filament length, filament diameter and trichome width; irradiance was positively correlated with filament diameter and trichome width, number of false branches in a filament and percent cover; and predominant substratum was positively correlated with filament length and sheath thickness. The information here reported about the ecological distribution of B. ganeshii supplements the taxonomic knowledge with data about its environmental requirements, which are important for the taxonomy of the genus. Variations in microhabitat conditions and niche widths are the main contributors to the wide spatial and seasonal distribution of this Oscillatorian in central Mexican streams.