Redescubriendo a Polygala corifolia (Polygalaceae) después de 170 años de su descripción

Se reporta el redescubrimiento de Polygala corifolia Planch. and Triana después de 170 años de su primera y última colección. Polygala corifolia fue descrita con base en una única colección realizada en la Sabana de Bogotá en 1844. Debido a la ausencia de registros posteriores a su descripción, esta especie se consideraba extinta. El nuevo registro proviene de una nueva localidad en la zona de páramo del municipio de Yarumal, norte de Antioquia. La considerable transformación y las actividades agropecuarias evidenciadas en esta zona, hacen que la supervivencia de esta población y posiblemente de la especie sea poco probable.The rediscovery of Polygala corifolia Planch. and Triana 170 years after the first and last collection is reported. Polygala corifolia was described based on a single collection made in the Sabana de Bogota in 1844. Due to the absence of records after its description, this species was considered extinct. The new record comes from a new locality in the Páramo of the Yarumal municipality, north of Antioquia. The considerable transformation and agricultural activities evidenced in this area, makes unlikely the survival of this population and possibly of the species

Ontogeny of the sporangium, spore formation and cytochemistry in Colombian Lycopodials (Lycopodiaceae)

Studies on reproductive aspects of Lycopodiaceae are not very abundant in the scientific literature, and constitute essential information to support taxonomic and systematic relationships among the group. Here we present a detailed study of the ontogeny of sporangia and sporogenesis, and the chemical determination of several compounds generated during spore formation. The analyses were performed in 14 taxa of six genera of the family, Diphasiastrum, Diphasium, Huperzia (a genus which is treated here including Phlegmariurus), Lycopodiella, Lycopodium and Palhinhaea. Specimens were collected in three departments from the Colombian Andes between 1 454-3 677m altitude. Ontogeny was studied in small, 1cm long pieces of strobili and axis, which were fixed in glutaraldehyde or FAA, dehydrated in alcohol, embedded in LR White, sectioned in 0.2- 0.5μm and stained with toluidine blue (TBO), a metachromatic dye that allows to detect both sporopollenin and lignin or its precursors, during these processes. For other studies, paraplast plus-embedded sections (3-5μm) were stained with safranin-fast green and alcian blue-hematoxylin. Chemical tests were also conducted in sections of fresh sporangia at different stages of maturity using alcian blue (mucopolysaccharides), Lugol solution (starch), Sudan III (lipids), phloroglucinol (lignin) and orcein (chromosomes). Sections were observed with photonic microscope equipped with differential interference contrast (DIC) and fluorescence microscopy (for spore and sporangium walls unstained). Strobili and sporangia were dehydrated with 2.2 dimethoxypropane, critical point dried and coated with gold for scanning electron microscopy (SEM). Our results indicated that the ontogeny of sporangia and sporogenesis were very similar to the previously observed in Huperzia brevifolia. Cutinisation occurs in early stages of development of sporangium cell walls, but in their final stages walls become lignified. As for the sporoderm development, the exospore is the first layer formed, composed by sporopollenin. The endospore deposits as a thin inner layer composed of cellulose, pectin and carboxylated polysaccharides. The perispore, if present, deposits at last. Mucopolysaccharides were found on the sporocyte coat and its abundance in sporangial cavity persists up to the immature tetrads stage, and then disappears. The lipids were abundant in the sporocytes, tetrads and spores, representing the main source of energy of the latter. In contrast, starch is not detected in the spores, but is abundant in premeiotic sporocytes and immature tetrads, developmental stages of high cellular metabolic activity. Intrinsic fluorescence corroborates the presence of lignin and cutin in the sporangium wall, while the sporopollenin is restricted to the exospore. The transfusion cells and the perispore are not always present. However, the processes of ontogeny and sporogenesis are extremely similar throughout the taxa studied, suggesting that they represent conservative family traits, nonspecific or generic.Facultad de Ciencias Naturales y Muse

Ontogeny of the sporangium, spore formation and cytochemistry in Colombian Lycopodials (Lycopodiaceae)

Studies on reproductive aspects of Lycopodiaceae are not very abundant in the scientific literature, and constitute essential information to support taxonomic and systematic relationships among the group. Here we present a detailed study of the ontogeny of sporangia and sporogenesis, and the chemical determination of several compounds generated during spore formation. The analyses were performed in 14 taxa of six genera of the family, Diphasiastrum, Diphasium, Huperzia (a genus which is treated here including Phlegmariurus), Lycopodiella, Lycopodium and Palhinhaea. Specimens were collected in three departments from the Colombian Andes between 1 454-3 677m altitude. Ontogeny was studied in small, 1cm long pieces of strobili and axis, which were fixed in glutaraldehyde or FAA, dehydrated in alcohol, embedded in LR White, sectioned in 0.2- 0.5μm and stained with toluidine blue (TBO), a metachromatic dye that allows to detect both sporopollenin and lignin or its precursors, during these processes. For other studies, paraplast plus-embedded sections (3-5μm) were stained with safranin-fast green and alcian blue-hematoxylin. Chemical tests were also conducted in sections of fresh sporangia at different stages of maturity using alcian blue (mucopolysaccharides), Lugol solution (starch), Sudan III (lipids), phloroglucinol (lignin) and orcein (chromosomes). Sections were observed with photonic microscope equipped with differential interference contrast (DIC) and fluorescence microscopy (for spore and sporangium walls unstained). Strobili and sporangia were dehydrated with 2.2 dimethoxypropane, critical point dried and coated with gold for scanning electron microscopy (SEM). Our results indicated that the ontogeny of sporangia and sporogenesis were very similar to the previously observed in Huperzia brevifolia. Cutinisation occurs in early stages of development of sporangium cell walls, but in their final stages walls become lignified. As for the sporoderm development, the exospore is the first layer formed, composed by sporopollenin. The endospore deposits as a thin inner layer composed of cellulose, pectin and carboxylated polysaccharides. The perispore, if present, deposits at last. Mucopolysaccharides were found on the sporocyte coat and its abundance in sporangial cavity persists up to the immature tetrads stage, and then disappears. The lipids were abundant in the sporocytes, tetrads and spores, representing the main source of energy of the latter. In contrast, starch is not detected in the spores, but is abundant in premeiotic sporocytes and immature tetrads, developmental stages of high cellular metabolic activity. Intrinsic fluorescence corroborates the presence of lignin and cutin in the sporangium wall, while the sporopollenin is restricted to the exospore. The transfusion cells and the perispore are not always present. However, the processes of ontogeny and sporogenesis are extremely similar throughout the taxa studied, suggesting that they represent conservative family traits, nonspecific or generic.Facultad de Ciencias Naturales y Muse

Ontogeny of the sporangium, spore formation and cytochemistry in Colombian Lycopodials (Lycopodiaceae)

Studies on reproductive aspects of Lycopodiaceae are not very abundant in the scientific literature, and constitute essential information to support taxonomic and systematic relationships among the group. Here we present a detailed study of the ontogeny of sporangia and sporogenesis, and the chemical determination of several compounds generated during spore formation. The analyses were performed in 14 taxa of six genera of the family, Diphasiastrum, Diphasium, Huperzia (a genus which is treated here including Phlegmariurus), Lycopodiella, Lycopodium and Palhinhaea. Specimens were collected in three departments from the Colombian Andes between 1 454-3 677m altitude. Ontogeny was studied in small, 1cm long pieces of strobili and axis, which were fixed in glutaraldehyde or FAA, dehydrated in alcohol, embedded in LR White, sectioned in 0.2- 0.5μm and stained with toluidine blue (TBO), a metachromatic dye that allows to detect both sporopollenin and lignin or its precursors, during these processes. For other studies, paraplast plus-embedded sections (3-5μm) were stained with safranin-fast green and alcian blue-hematoxylin. Chemical tests were also conducted in sections of fresh sporangia at different stages of maturity using alcian blue (mucopolysaccharides), Lugol solution (starch), Sudan III (lipids), phloroglucinol (lignin) and orcein (chromosomes). Sections were observed with photonic microscope equipped with differential interference contrast (DIC) and fluorescence microscopy (for spore and sporangium walls unstained). Strobili and sporangia were dehydrated with 2.2 dimethoxypropane, critical point dried and coated with gold for scanning electron microscopy (SEM). Our results indicated that the ontogeny of sporangia and sporogenesis were very similar to the previously observed in Huperzia brevifolia. Cutinisation occurs in early stages of development of sporangium cell walls, but in their final stages walls become lignified. As for the sporoderm development, the exospore is the first layer formed, composed by sporopollenin. The endospore deposits as a thin inner layer composed of cellulose, pectin and carboxylated polysaccharides. The perispore, if present, deposits at last. Mucopolysaccharides were found on the sporocyte coat and its abundance in sporangial cavity persists up to the immature tetrads stage, and then disappears. The lipids were abundant in the sporocytes, tetrads and spores, representing the main source of energy of the latter. In contrast, starch is not detected in the spores, but is abundant in premeiotic sporocytes and immature tetrads, developmental stages of high cellular metabolic activity. Intrinsic fluorescence corroborates the presence of lignin and cutin in the sporangium wall, while the sporopollenin is restricted to the exospore. The transfusion cells and the perispore are not always present. However, the processes of ontogeny and sporogenesis are extremely similar throughout the taxa studied, suggesting that they represent conservative family traits, nonspecific or generic.Laboratorio de Estudios de Anatomía Vegetal Evolutiva y Sistemátic

The global abundance of tree palms

Aim: Palms are an iconic, diverse and often abundant component of tropical ecosys-tems that provide many ecosystem services. Being monocots, tree palms are evo-lutionarily, morphologically and physiologically distinct from other trees, and these differences have important consequences for ecosystem services (e.g., carbon se-questration and storage) and in terms of responses to climate change. We quanti-fied global patterns of tree palm relative abundance to help improve understanding of tropical forests and reduce uncertainty about these ecosystems under climate change.Location: Tropical and subtropical moist forests.Time period: Current.Major taxa studied: Palms (Arecaceae).Methods: We assembled a pantropical dataset of 2,548 forest plots (covering 1,191 ha) and quantified tree palm (i.e., ≥10 cm diameter at breast height) abundance relative to co-occurring non-palm trees. We compared the relative abundance of tree palms across biogeographical realms and tested for associations with palaeoclimate stability, current climate, edaphic conditions and metrics of forest structure.Results: On average, the relative abundance of tree palms was more than five times larger between Neotropical locations and other biogeographical realms. Tree palms were absent in most locations outside the Neotropics but present in >80% of Neotropical locations. The relative abundance of tree palms was more strongly asso-ciated with local conditions (e.g., higher mean annual precipitation, lower soil fertility, shallower water table and lower plot mean wood density) than metrics of long-term climate stability. Life-form diversity also influenced the patterns; palm assemblages outside the Neotropics comprise many non-tree (e.g., climbing) palms. Finally, we show that tree palms can influence estimates of above-ground biomass, but the mag-nitude and direction of the effect require additional work.Conclusions: Tree palms are not only quintessentially tropical, but they are also over-whelmingly Neotropical. Future work to understand the contributions of tree palms to biomass estimates and carbon cycling will be particularly crucial in Neotropical forests

The global abundance of tree palms

Aim Palms are an iconic, diverse and often abundant component of tropical ecosystems that provide many ecosystem services. Being monocots, tree palms are evolutionarily, morphologically and physiologically distinct from other trees, and these differences have important consequences for ecosystem services (e.g., carbon sequestration and storage) and in terms of responses to climate change. We quantified global patterns of tree palm relative abundance to help improve understanding of tropical forests and reduce uncertainty about these ecosystems under climate change. Location Tropical and subtropical moist forests. Time period Current. Major taxa studied Palms (Arecaceae). Methods We assembled a pantropical dataset of 2,548 forest plots (covering 1,191 ha) and quantified tree palm (i.e., ≥10 cm diameter at breast height) abundance relative to co‐occurring non‐palm trees. We compared the relative abundance of tree palms across biogeographical realms and tested for associations with palaeoclimate stability, current climate, edaphic conditions and metrics of forest structure. Results On average, the relative abundance of tree palms was more than five times larger between Neotropical locations and other biogeographical realms. Tree palms were absent in most locations outside the Neotropics but present in >80% of Neotropical locations. The relative abundance of tree palms was more strongly associated with local conditions (e.g., higher mean annual precipitation, lower soil fertility, shallower water table and lower plot mean wood density) than metrics of long‐term climate stability. Life‐form diversity also influenced the patterns; palm assemblages outside the Neotropics comprise many non‐tree (e.g., climbing) palms. Finally, we show that tree palms can influence estimates of above‐ground biomass, but the magnitude and direction of the effect require additional work. Conclusions Tree palms are not only quintessentially tropical, but they are also overwhelmingly Neotropical. Future work to understand the contributions of tree palms to biomass estimates and carbon cycling will be particularly crucial in Neotropical forests

Rediscovering Polygala corifolia (Polygalaceae) 170 years after its description

The rediscovery of Polygala corifolia Planch. & Triana 170 years after the first and last collection is reported. Polygala corifolia was described based on a single collection made in the Sabana de Bogota in 1844. Due to the absence of records after its description, this species was considered extinct. The new record comes from a new locality in the Páramo of the Yarumal municipality, north of Antioquia. The considerable transformation and agricultural activities evidenced in this area, makes unlikely the survival of this population and possibly of the species

Psittacanthus longerectus (Loranthaceae), a new showy species from Colombia

We describe Psittacanthus longerectus (Loranthaceae), a species so far only known from Antioquia (Colombia) and discuss the taxonomic affinities of the new species with P. acinarius and P. cyclophyllus. Psittacanthus longerectus is characterized by having cordate leaves, erect branches, and terminal inflorescences

Anatomía foliar comparativa de tres especies de Furcraea (Asparagaceae: Agavoideae)

RESUMEN El género neotropical Furcraea Vent. es ampliamente cultivado para la production de fibras conocidas como Fique o Cabuya. Se realizó un análisis histológico de las hojas de tres especies cultivadas en Colombia, con la finalidad de realizar la description comparativa entre ellas. Diferentes secciones de hojas listas para su cosecha fueron procesadas utilizando técnicas histológicas convencionales. Las tres especies presentaron características anatómicas comparativamente muy homogéneas dentro de las que resaltan: epidermis monoestratificada, cutícula gruesa, estomas encriptados, mesófilo no diferenciado, presencia de cristales de oxalato de calcio, fibras esclerenquimáticas de tipo septado asociadas a los haces vasculares o formando cordones y braquiesclereidas asociadas al margen foliar. Estas últimas varían ligeramente entre las especies estudiadas en el lumen, la forma de las punteaduras y el grado de lignificación, lo cual parece estar correlacionado con la dureza del margen foliar. Aparte de las braquiesclereidas, no se advierten suficientes caracteres histológicos que permitan la diferenciación clara entre los cultivares estudiados. Se discute también la anatomía de estas plantas en función de su metabolismo fotosintético

Ontogenia de los esporangios, formación y citoquímica de esporas en licopodios (Lycopodiaceae) colombianos

Studies on reproductive aspects of Lycopodiaceae are not very abundant in the scientific literature, and constitute essential information to support taxonomic and systematic relationships among the group. Here we present a detailed study of the ontogeny of sporangia and sporogenesis, and the chemical determination of several compounds generated during spore formation. The analyses were performed in 14 taxa of six genera of the family, Diphasiastrum, Diphasium, Huperzia (a genus which is treated here including Phlegmariurus), Lycopodiella, Lycopodium and Palhinhaea. Specimens were collected in three departments from the Colombian Andes between 1 454-3 677m altitude. Ontogeny was studied in small, 1cm long pieces of strobili and axis, which were fixed in glutaraldehyde or FAA, dehydrated in alcohol, embedded in LR White, sectioned in 0.2-0.5μm and stained with toluidine blue (TBO), a metachromatic dye that allows to detect both sporopollenin and lignin or its precursors, during these processes. For other studies, paraplast plus-embedded sections (3-5μm) were stained with safranin-fast green and alcian blue-hematoxylin. Chemical tests were also conducted in sections of fresh sporangia at different stages of maturity using alcian blue (mucopolysaccharides), Lugol solution (starch), Sudan III (lipids), phloroglucinol (lignin) and orcein (chromosomes). Sections were observed with photonic microscope equipped with differential interference contrast (DIC) and fluorescence microscopy (for spore and sporangium walls unstained). Strobili and sporangia were dehydrated with 2.2 dimethoxypropane, critical point dried and coated with gold for scanning electron microscopy (SEM). Our results indicated that the ontogeny of sporangia and sporogenesis were very similar to the previously observed in Huperzia brevifolia. Cutinisation occurs in early stages of development of sporangium cell walls, but in their final stages walls become lignified. As for the sporoderm development, the exospore is the first layer formed, composed by sporopollenin. The endospore deposits as a thin inner layer composed of cellulose, pectin and carboxylated polysaccharides. The perispore, if present, deposits at last. Mucopolysaccharides were found on the sporocyte coat and its abundance in sporangial cavity persists up to the immature tetrads stage, and then disappears. The lipids were abundant in the sporocytes, tetrads and spores, representing the main source of energy of the latter. In contrast, starch is not detected in the spores, but is abundant in premeiotic sporocytes and immature tetrads, developmental stages of high cellular metabolic activity. Intrinsic fluorescence corroborates the presence of lignin and cutin in the sporangium wall, while the sporopollenin is restricted to the exospore. The transfusion cells and the perispore are not always present. However, the processes of ontogeny and sporogenesis are extremely similar throughout the taxa studied, suggesting that they represent conservative family traits, nonspecific or generic.Los estudios sobre aspectos reproductivos no son muy abundantes en la literatura científica sobre los taxones de Lycopodiaceae y constituyen información esencial para apoyar la taxonomía y relaciones sistemáticas en el grupo. Por lo tanto, se presenta aquí un análisis detallado de la ontogenia de los esporangios y esporogénesis, así como determinaciones químicas de varios compuestos generados durante la formación de las esporas. Los análisis se llevaron a cabo en 14 taxones de seis géneros de la familia: Diphasiastrum, Diphasium, Huperzia (un género que se trata aquí, incluyendo Phlegmariurus), Lycopodiella, Lycopodium y Palhinhaea. Las muestras fueron recolectadas en tres departamentos de los Andes de Colombia entre 1 454-3 677m de altitud. La ontogenia se estudió en trozos de estróbilos y ejes, de 1cm de largo, que se fijaron en glutaraldehido o FAA, se deshidrataron en alcohol, se incluyeron en LR White, se seccionaron en cortes de 0.2-0.5μm y se colorearon con azul de toluidina (TBO), un colorante metacromático que permite detectar tanto esporopolenina como lignina o sus precursores. Para estudios adicionales, secciones de 3-5μm de material incluido en paraplast plus se colorearon con safranina-verde rápido y azul alcián-hematoxilina. Las pruebas químicas se llevaron a cabo en secciones de esporangios sin fijar en diferentes etapas de madurez utilizando azul alcián (mucopolisacáridos), solución de Lugol (almidón), Sudán III (lípidos), fluoroglucinol (lignina) y orceína (cromosomas). Las observaciones se efectuaron con microscopio fotónico equipado con contraste diferencial de interferencia (DIC) y microscopía de fluorescencia (para esporas y pared de los esporangios sin colorear). Para observaciones con microscopía electrónica de barrido (MEB), los estróbilos y esporangios se deshidrataron con 2,2 dimetoxipropano, se desecaron a punto crítico y se metalizaron con oro. Los resultados indican que la ontogenia de los esporangios y esporogénesis es muy similar a la observada previamente en Huperzia brevifolia. En las primeras etapas de desarrollo, las paredes celulares de la epidermis del esporangio se cutinizan y en las finales se lignifican. En el desarrollo del esporodermo, la primera capa que se forma es el exosporio, compuesto por esporopolenina. El endosporio es una capa interna delgada compuesta de celulosa, pectina y polisacáridos carboxilados. El perisporio, si está presente, es la última capa que se deposita. Los mucopolisacáridos se encontraron en la cubierta del esporocito, son abundantes en la cavidad esporangial hasta la etapa de tétradas inmaduras y luego desaparecen. Los lípidos son abundantes en esporocitos, tétradas y esporas, y representan la principal fuente de energía de estas. En contraste, el almidón no se detecta en las esporas pero es abundante en esporocitos premeióticos y tétradas inmaduras, ambos con gran actividad metabólica. La fluorescencia intrínseca corrobora la presencia de lignina y cutina en la pared del esporangio, mientras que la esporopolenina se limita al exosporio. Las células de transfusión y el perisporio no siempre están presentes. Sin embargo, los procesos de la ontogenia y esporogénesis son extremadamente similares en todos los taxones estudiados, lo que sugiere que representan rasgos típicos de familia, no específicos ni genéricos. 1Grupo de Estudios Botánicos y Docentes delInstituto de Biología, Universidad de Antioquia, calle 67 No. 53 -108, Medellín, Colombia; [email protected], [email protected] Grupo Ecología y Diversidad Vegetal, Departamento de Biología, Calle 13 # 100-00, Universidad del Valle, Sede Meléndez, Cali, Colombia