A permineralized Early Cretaceous lycopsid from China and the evolution of crown clubmosses.

Lycopodiaceae are one of three surviving families of lycopsids, a lineage of vascular plants with a fossil history dating to at least the Early Devonian or perhaps the Late Silurian (c. 415 Ma). Many fossils have been linked to crown Lycopodiaceae, but the lack of well-preserved material has hindered definitive recognition of this group in the paleobotanical record. New, exceptionally well-preserved permineralized lycopsid fossils from the Early Cretaceous (125.6 ± 1.0 Ma) of Inner Mongolia, China, were examined in detail using acetate peel and micro-computed tomography techniques. The anatomy of extant Lycopodiaceae was analyzed for comparison using fluorescence microscopy. Phylogenetic relationships of the new fossil to extant Lycopodiaceae were evaluated using parsimony and maximum likelihood analyses. Lycopodicaulis oellgaardii gen. et sp. nov. provides the earliest unequivocal and best-documented evidence of crown Lycopodiaceae and Lycopodioideae, based on anatomically-preserved fossil material. Recognition of Lycopodicaulis in Asia during the Early Cretaceous indicates the presence of crown Lycopodiaceae at this time, and striking similarities of stem anatomy with extant species provide a framework for the understanding of the interaction of branching and vascular anatomy in crown-group lycopsids.

Virtual issue: Ecology and evolution of pteridophytes in the era of molecular genetics.

The past quarter-century has witnessed a revolution in our understanding of the phylogenetics, systematics, and ecology of pteridophytes (ferns and lycophytes), particularly due to the rapid accumulation of plastid sequence data and a renewed interest in the ecology of the sexual phase of the life cycle. We here compile 19 papers recently published in the Journal of Plant Research dealing with the biology of pteridophytes, grouped into six categories: (1) breeding systems, (2) species complexes and polyploidization, (3) fossil taxa, (4) gametophyte ecology, (5) systematics, (6) biodiversity. We hope this collection of papers will be of value to researchers interested in this fascinating group of plants.

An update and reassessment of fern and lycophyte diversity data in the Japanese Archipelago.

The fern and lycophyte flora of Japan comprising 721 native taxa (including subspecies and varieties) plus 371 interspecific hybrids was reassessed using a nearly comprehensively sampled distribution map at 10 km resolution vouchered by 216,687 specimens, up-to-date cytotaxonomic information covering 74% of the taxa, and an rbcL sequence dataset covering 97.9% of the taxa. Spatial distribution of species richness and phylogenetic diversity was visualized. Apomixis was observed in 11.0% of the native taxa whose reproductive modes are known. The number of sexually reproducing polyploid taxa (n = 199) is less than sexual diploids (n = 241), and 30 of them are evidently allopolyploid, in contrast with the low number of possible autopolyploids (n = 4). Apomictic taxa were found to have smaller latitudinal ranges than sexual taxa or taxa with multiple reproductive modes. A morphological character dataset in Lucid format is provided for taxonomic identification of the native taxa.

Quillworts from the Amazon: A multidisciplinary populational study on Isoetes serracarajensis and Isoetes cangae.

Isoetes are ancient quillworts members of the only genus of the order Isoetales. The genus is slow evolving but is resilient, and widespread worldwide. Two recently described species occur in the Eastern Brazilian Amazon, Isoetes serracarajensis and Isoetes cangae. They are found in the ironstone grasslands known as Canga. While I. serracarajensis is present mostly in seasonal water bodies, I. cangae is known to occur in a single permanent lake at the South mountain range. In this work, we undertake an extensive morphological, physiological and genetic characterization of both species to establish species boundaries and better understand the morphological and genetic features of these two species. Our results indicate that the morphological differentiation of the species is subtle and requires a quantitative assessment of morphological elements of the megaspore for diagnosis. We did not detect differences in microspore output, but morphological peculiarities may establish a reproductive barrier. Additionally, genetic analysis using DNA barcodes and whole chloroplast genomes indicate that although the plants are genetically very similar both approaches provide diagnostic characters. There was no indication of population structuring I. serracarajensis. These results set the basis for a deeper understanding of the evolution of the Isoetes genus.

Lilingostrobus chaloneri gen. et sp. nov., a Late Devonian woody lycopsid from Hunan, China.

Lycopsids are a minor component of current terrestrial herbaceous floras. However, lycopsid fossil diversity shows a great diversity and disparity including heterosporous woody plants, e.g. the giant isoetaleans that populated the extensive Pennsylvanian wetlands. The earliest known isoetaleans come from late Devonian localities from China. Here, we describe Lilingostrobus chaloneri gen. et sp. nov., a new isoetalean lycopsid from the Upper Devonian (Famennian) Xikuangshan Formation of China (Hunan Province, South China), which adds to the already impressive diversity of the Devonian lycopsids from China. Lilingostrobus shows an unusual combination of characters. This new plant is pseudoherbaceous, with a possible tufted habit, and consists of narrow axes with rare isotomies. The stem includes small quantities of secondary xylem. Each fertile axis bears one terminal strobilus comprising sporophylls ending in a very long upturned lamina. Microspores and putative megaspores have been found, but whether the plant has mono- or bisporangiate strobili is unknown. Importantly, our cladistic analysis identifies Lilingostrobus as a direct precursor of Isoetales, which provides new insights into the early evolution of lycopsids.

First insights on the biogeographical history of Phlegmariurus (Lycopodiaceae), with a focus on Madagascar.

We explored the biogeographical history of a group of spore-bearing plants focusing on Phlegmariurus (Lycopodiaceae), a genus of lycophytes comprising ca. 250 species. Given its wide distribution in the Southern Hemisphere, Phlegmariurus provides a good model to address questions about the biogeographical processes underlying southern distributions, notably in Madagascar and surrounding islands, also called the Western Indian Ocean (WIO). Our aims were (i) to discuss the systematics of the Malagasy species in the light of molecular phylogenetic results, (ii) to provide the first dating analysis focused on Phlegmariurus and (iii) to understand the relative role of vicariance, dispersal and diversification in the origin of the Malagasy Phlegmariurus species. The phylogenetic relationships were inferred based on three plastid DNA regions (rbcL, trnH-psbA and trnL+trnL-trnF) and on a dataset comprising 93 species, including 16 Malagasy species (80% of the total Malagasy diversity for the genus). Our results highlighted the need to combine Malagasy Huperzia species in Phlegmariurus, as well as the polyphyly of widely distributed species: Phlegmariurus phlegmaria, P. squarrosus and P. verticillatus with the Malagasy species not belonging with the types of P. phlegmaria or P. squarrosus. This led us to propose new circumscriptions of Phlegmariurus species, especially in the WIO. Our dating analysis, relying on fossil calibrations, showed that Phlegmariurus would have originated in the Late Cretaceous and diversified in the Early Eocene. The biogeographical analysis highlighted uncertainties about the biogeographical origins of Phlegmariurus: the genus would have started to diversify in an ancestral range covering at least the Neotropics and Australasia. Hypotheses on the biogeographical history of Phlegmariurus were discussed, especially the roles of long distance dispersal, migration via Antarctica and via the Boreotropics. Six long distance dispersal events over the last 40 Ma would explain the Malagasy species diversity of Phlegmariurus, in combination with an important in situ diversification starting in the Miocene.

Phylogenetic systematics, morphological evolution, and natural groups in neotropical Phlegmariurus (Lycopodiaceae).

The Neotropical clade of the lycophyte genus Phlegmariurus is comprised of an estimated 150 described species and exhibits exceptional morphological and ecological diversity. Because of their simple morphology, frequent convergent evolution, and the recentness of the group's diversification, the delimitation of species and species groups has remained challenging. Here, we present a robustly support phylogeny of Neotropical Phlegmariurus based on six chloroplast markers and ca. 70% of known species, and use ancestral character state reconstruction to investigate morphological evolution in the clade, and define natural species groups. The Neotropical species of Phlegmariurus form a clade that also includes a small number of Afro-Madagascan species. A morphologically and ecologically variable group of species from southeastern Brazil form a monophyletic group and represent a parallel radiation to principally Andean lineages. Species groups in Neotropical Phlegmariurus that were previously recognized based on morphology are not monophyletic. We find support for 11 morphologically cohesive and well-supported species groups. Morphological homoplasy is common in Phlegmariurus and complicates infrageneric classification of the Neotropical taxa. Our results provide a useful framework for identifying species groups and understanding patterns of morphological evolution in Neotropical Phlegmariurus. The radiation of the Brazilian species remains poorly understood and requires further study.

[Newly records of medicinal species in Jiangxi].

Seven species were reported as new records of Jiangxi province, which collected from Wugongshan region, including Huperzia kunmingensis(Lycopodiaceae), Hydrangea mangshanensis(Saxifragaceae), Itea glutinosa(Saxifragaceae), Stellaria monosperma var. japonica(Lycopodiaceae), Youngia pratti(Compositae), and Calanthe henryi(Orchidaceae), Collabium formosanum(Orchidaceae). Among these species, H. kunmingensis, H. mangshanensis, I. glutinosa, Y. pratti and C. henryi are endemic in China. C. henryi is stenotopic distribution in China and regarded as vulnerable endangered plant by IUCN. The report is of great significance to the plant diversity and floristic composition in Jiangxi. All the specimens examined are preserved in Jishou University (JIU) and Sun yat-sen University (SYS).

The Genus Diphasiastrum and Its Lycopodium Alkaloids.

The genus Diphasiastrum includes at least 23 species distributed primarily across the northern temperate and subarctic areas of the world. These plants produce an array of lycopodium alkaloids, and some species such as Diphasiastrum complanatum have been used in traditional medicine for ages for various conditions. Hybridization is common in this group of plants and they have always been a challenge for taxonomists and other scientists studying them. To date, 11 Diphasiastrum species have been reported to produce lycopodium alkaloids. In this review, reported alkaloids and their distribution patterns across these species along with taxonomical and bioactivity considerations are reviewed and discussed.

[Sporogenesis, sporoderm and mature spore ornamentation in Lycopodiaceae]. / Esporogénesis, esporodermo y ornamentación de esporas maduras en Lycopodiaceae.

Studies on reproductive aspects, spore morphology and ultrastructure of Lycopodiaceae are not very common in the scientific literature, and constitute essential information to support taxonomic and systematic relationships among the group. In order to complete existing information, adding new and broader contributions on these topics, a comparative analysis of the sporogenesis ultrastructure, with emphasis on cytological aspects of the sporocyte coat development, tapetum, monoplastidic and polyplastidic meiosis, sporoderm ontogeny and ornamentation of the mature spores, was carried out in 43 taxa of eight genera of the Lycopodiaceae: Austrolycopodium, Diphasium, Diphasiastrum, Huperzia (including Phlegmariurus), Lycopodium, Lycopodiella, Palhinhaea and Pseudolycopodiella growing in the Andes of Colombia and the Neotropics. For this study, the transmission elec- tron microscopy (TEM) samples were collected in Cauca and Valle del Cauca Departments, while most of the spores for scanning electron microscopy (SEM) analysis were obtained from herbarium samples. We followed standard preparation procedures for spore observation by TEM and SEM. Results showed that the sporocyte coat is largely composed by primary wall components; the sporocyte develop much of their metabolic activity in the production of their coat, which is retained until the spores release; protective functions for the diploid cells undergoing meiosis is postulated here for this layer. The abundance of dictyosomes in the sporocyte cytoplasm was related to the formation and development of the sporocyte coat. Besides microtubule activity, the membrane of sporocyte folds, associated with electrodense material, and would early determine the final patterns of spore ornamentation. Monoplastidic condition is common in Lycopodium s.l., whereas polyplastidic condition was observed in species of Huperzia and Lycopodiella s. l. In monoplastidic species, the tapetum presents abun- dant multivesicular bodies, while in polyplastidic species, the secretory activity of the tapetum is less intense. Sporoderm development is centripetal, exospore is the first formed layer, then the endospore and, if present, perispore is the final deposited layer. Adult spores of the Lycopodiaceae showed two patterns of ornamentation: negative or caviform (foveolate spores) and positive or muriform ornamentation, the latter with two subtypes (rugate and reticulate spores). The spores of Huperzia are characteristically foveolate, the rugate spores were found in a few species of Huperzia and in all of the Lycopodiella s. l. taxa studied, while Lycopodium s.l. spores bear reticulate ornamentation. Numerous ornamentation traits are diagnostic at the specific level. The types of ornamentation found do not support the recent extreme fragmentation of the family in several genera, but could match, a priori, with the idea of three subfamilies. The findings of sporogenesis, extremely similar in all taxa studied, point more to consider fewer genera, more comprehensive, than the recent, marked splitting of the family.

[Morphology and anatomy of caulinar axes, lycophylls and sporangia of Phlegmariurus phylicifolius: a contribution to the systematics of Neotropical Lycopodiaceae]. / Morfología y anatomía de ejes caulinares, licofilos y esporangios de Phlegmariurus phylicifolius: un aporte a la sistemática de las Lycopodiaceae neotropicales.

Phlegmariurus is the only genus of Lycopodiaceae with the species grouped in 22 informal groups. Species level relationships within Phlegmariurus are poorly understood and their circumscriptions require a thorough molecular and morphological review. A detailed study of morphology and anatomy of caulinar axes, lycophylls and sporangia of Phlegmariurus phylicifolius was carried out in order to contribute to the elucidation of species circumscription in the informal group Phlegmariurus phlegmaria. Small pieces of caulinar axes bearing trophophylls, sporophylls and sporangia were fixed, dehydrated, Histowax (paraffin) embedded, sectioned in a rotatory microtome, and stained using the common Safranin O-Fast Green technique; handmade cross sections were also made and stained with the same technique. P. phylicifolius includes slender, pendulous plants up to 40cm long. Shoots heterophyllous, in the basal divisions ca. 10-20(-25) mm in diameter including the trophophylls, then abruptly constricted to (1-) 1.5-2(-2.5) mm in diameter including the imbricate, reduced sporophylls. Trophophylls are borne in alternating whorls of three, or decussate, subdecussate, or alternate, widely spaced in alternate leaved caulinar axes portions, perpendicular to the caulinar axes to falcately ascending, lanceolate to linear-lanceolate, with flat to slightly revolute margins. Each lycophyll is supplied by a single central vascular bundle, connected to a protoxylem pole in the stele. At the site of leaf-trace departure, no leaf (lycophyll) gap is present. Caulinar axes excluding leaves 0.7-1.2 mm thick at the base, upward tapering to ca. 0.5 mm. Caulinar axes present unistratified epidermis and endodermis, the cortex is characterized by the presence of a trabecular structure of lisigenous origin formed in the parenchimatous tissue next to the endodermis. The vascular tissue occupies the central part of the caulinar axes, forming a plectostele ofsubradiate organization, with five poles ofprotoxylem. The epidermal cells present sinuous anticlinal walls; invaginations in the inner side of external periclinal wall of the epidermal cells could be probably adaptive morphological feature of a water deficient environment. Leaves of constricted terminal divi- sions are decussate, or subdecussate, continuously or discontinuously sporangiate, appressed, abaxially rounded to carinate, widely lanceolate to widely ovate or subcordate, acute to mucronate or cuspidate, shorter than the sporangia. Each sporangium originates from a group of epidermal cells, axilar to the sporophylls. The cell walls of epidermal cell of the sporangia are Huperzioideae type. The morphological studies of trophophylls contribute to confirm the differences between P. phylicifolius and P. subulatus.

Esporogénesis, esporodermo y ornamentaciónde esporas maduras en Lycopodiaceae / Sporogenesis, sporoderm and mature spore ornamentation in Lycopodiaceae

Studies on reproductive aspects, spore morphology and ultrastructure of Lycopodiaceae are not very common in the scientific literature, and constitute essential information to support taxonomic and systematic relationships among the group. In order to complete existing information, adding new and broader contributions on these topics, a comparative analysis of the sporogenesis ultrastructure, with emphasis on cytological aspects of the sporocyte coat development, tapetum, monoplastidic and polyplastidic meiosis, sporoderm ontogeny and ornamentation of the mature spores, was carried out in 43 taxa of eight genera of the Lycopodiaceae: Austrolycopodium, Diphasium, Diphasiastrum, Huperzia (including Phlegmariurus), Lycopodium, Lycopodiella, Palhinhaea and Pseudolycopodiella growing in the Andes of Colombia and the Neotropics. For this study, the transmission electron microscopy (TEM) samples were collected in Cauca and Valle del Cauca Departments, while most of the spores for scanning electron microscopy (SEM) analysis were obtained from herbarium samples. We followed standard preparation procedures for spore observation by TEM and SEM. Results showed that the sporocyte coat is largely composed by primary wall components; the sporocyte develop much of their metabolic activity in the production of their coat, which is retained until the spores release; protective functions for the diploid cells undergoing meiosis is postulated here for this layer. The abundance of dictyosomes in the sporocyte cytoplasm was related to the formation and development of the sporocyte coat. Besides microtubule activity, the membrane of sporocyte folds, associated with electrodense material, and would early determine the final patterns of spore ornamentation. Monoplastidic condition is common in Lycopodium s.l., whereas polyplastidic condition was observed in species of Huperzia and Lycopodiella s. l.. In monoplastidic species, the tapetum presents abundant multivesicular bodies, while in polyplastidic species, the secretory activity of the tapetum is less intense. Sporoderm development is centripetal, exospore is the first formed layer, then the endospore and, if present, perispore is the final deposited layer. Adult spores of the Lycopodiaceae showed two patterns of ornamentation: negative or caviform (foveolate spores) and positive or muriform ornamentation, the latter with two subtypes (rugate and reticulate spores). The spores of Huperzia are characteristically foveolate, the rugate spores were found in a few species of Huperzia and in all of the Lycopodiella s. l. taxa studied, while Lycopodium s.l. spores bear reticulate ornamentation. Numerous ornamentation traits are diagnostic at the specific level. The types of ornamentation found do not support the recent extreme fragmentation of the family in several genera, but could match, a priori, with the idea of three subfamilies. The findings of sporogenesis, extremely similar in all taxa studied, point more to consider fewer genera, more comprehensive, than the recent, markedsplitting of the family. Rev. Biol. Trop. 62 (3): 1161-1195. Epub 2014 September 01.

Estudios sobre aspectos reproductivos, morfología y ultraestructura de las esporas de Lycopodiaceae no son abundantes en la literatura científica y constituyen información esencial para apoyar las relaciones taxonómicas y sistemáticas en el grupo. Con el fin de completar la información existente, añadiendo contribuciones nuevas y más amplias sobre estos temas, se realizó un análisis comparado de la ultraestructura de la esporogénesis, con énfasis en aspectos citológicos que tienen que ver con la formación de la cubierta de los esporocitos, el tapete, las meiosis monoplastidial y poliplastidial, la ontogenia del esporodermo y la ornamentación de las esporas maduras en 43 táxones de ocho géneros de Lycopodiaceae: Austrolycopodium, Diphasium, Diphasiastrum, Huperzia (incluyendo Phlegmariurus), Lycopodium, Lycopodiella, Palhinhaea y Pseudolycopodiella que crecen en los Andes de Colombia y el Neotrópico. Para estudios con microscopía electrónica de trasmisión (MET) las muestras se recolectaron en los departamentos de Cauca y Valle del Cauca, mientras que la mayoría de las muestras para microscopía electrónica de barrido (MEB) provienen de material herborizado de colecciones. Para la observación de las muestras con MET y MEB se utilizaron protocolos estándar para el procesamiento de esporas. La cubierta de los esporocitos está formada por pared primaria; los esporocitos invierten gran parte de su actividad metabólica en la producción de esa cubierta, que es mantenida hasta la liberación de las esporas y tiene funciones de protección de las células que harán meiosis. La abundancia de dictiosomas en los esporocitos se relacionó con la formación y desarrollo de la cubierta. Además de la actividad de los microtúbulos, la presencia de sinuosidades y plegamientos asociados con material electro denso en la membrana de los esporocitos determinarían tempranamente los patrones de ornamentación de las esporas. La condición monoplastidial es común en Lycopodium s.l.y la poliplastidial se observó en Huperzia y Lycopodiella s. l. En especies monoplastidiales el tapete presenta abundantes cuerpos plurivesiculares, en las poliplastidiales la actividad secretora del tapete es menos intensa. El desarrollo del esporodermo es centrípeto, el exosporio se forma primero, seguido del endosporio y el perisporio, si está presente, se deposita de último. En las esporas adultas de Lycopodiaceae se encontraron dos patrones de ornamentación: negativo o caviforme (esporas foveoladas) y positivo o muriforme (esporas rugadas y reticuladas). Las esporas foveoladas son características de Huperzia; las rugadas de unas pocas especies de Huperzia y las especies de Lycopodiella s. l., mientras que las reticulada son típicas de Lycopodium s. l.. Numerosos caracteres de la ornamentación resultan diagnósticos en el nivel específico. Los tipos principales no apoyan la extrema fragmentación reciente de la familia en varios géneros, aunque podría coincidir, a priori, con la idea de tres subfamilias. Los hallazgos de la esporogénesis, extremadamente similar en todos los táxones estudiados, apuntan más a la unificación de los géneros en la familia que a su segregación.

Morfología y anatomía de ejes caulinares, licofilos y esporangios de Phlegmariurus phylicifolius: un aporte a la sistemática de las Lycopodiaceae neotropicales / Morphology and anatomy of caulinar axes, lycophylls and sporangia of Phlegmariurus phylicifolius: a contribution to the systematics of Neotropical Lycopodiaceae

Phlegmariurus is the only genus of Lycopodiaceae with the species grouped in 22 informal groups. Species level relationships within Phlegmariurus are poorly understood and their circumscriptions require a thorough molecular and morphological review. A detailed study of morphology and anatomy of caulinar axes, lycophylls and sporangia of Phlegmariurus phylicifolius was carried out in order to contribute to the elucidation of species circumscription in the informal group Phlegmariurus phlegmaria. Small pieces of caulinar axes bearing trophophylls, sporophylls and sporangia were fixed, dehydrated, Histowax (paraffin) embedded, sectioned in a rotatory microtome, and stained using the common Safranin O-Fast Green technique; handmade cross sections were also made and stained with the same technique. P. phylicifolius includes slender, pendulous plants up to 40cm long. Shoots heterophyllous, in the basal divisions ca. 10-20(-25)mm in diameter including the trophophylls, then abruptly constricted to (l-) 1.5-2(-2.5)mm in diameter including the imbricate, reduced sporophylls. Trophophylls are borne in alternating whorls of three, or decussate, subdecussate, or alternate, widely spaced in alternate leaved caulinar axes portions, perpendicular to the caulinar axes to falcately ascending, lanceolate to linear-lanceolate, with flat to slightly revolute margins. Each lycophyll is supplied by a single central vascular bundle, connected to a protoxylem pole in the stele. At the site of leaf-trace departure, no leaf (lycophyll) gap is present. Caulinar axes excluding leaves 0.7-1.2mm thick at the base, upward tapering to ca. 0.5mm. Caulinar axes present unistratified epidermis and endodermis, the cortex is characterized by the presence of a trabecular structure of lisigenous origin formed in the parenchimatous tissue next to the endodermis. The vascular tissue occupies the central part of the caulinar axes, forming a plectostele of subradiate organization, with five poles of protoxylem. The epidermal cells present sinuous anticlinal walls; invaginations in the inner side of external periclinal wall of the epidermal cells could be probably adaptive morphological feature of a water deficient environment. Leaves of constricted terminal divisions are decussate, or subdecussate, continuously or discontinuously sporangiate, appressed, abaxially rounded to carinate, widely lanceolate to widely ovate or subcordate, acute to mucronate or cuspidate, shorter than the sporangia. Each sporangium originates from a group of epidermal cells, axilar to the sporophylls. The cell walls of epidermal cell of the sporangia are Huperzioideae type. The morphological studies of trophophylls contribute to confirm the differences between P. phylicifolius and P. subulatus. Rev. Biol. Trop. 62 (3): 1217-1227. Epub 2014 September 01.

Phlegmariurus es el único género de Lycopodiaceae con las especies reunidas en 22 grupos informales. Las relaciones a nivel de especie dentro de Phlegmariurus están pobremente estudiadas y la circunscripción de las mismas requiere profundos exámenes moleculares y morfológicos. Se ha llevado a cabo un estudio detallado de la morfología y la anatomía de ejes caulinares, licofilos y esporangios de P. phylicifolius, con el fin de contribuir al esclarecimiento en la delimitación de las especies en el grupo Phlegmariurus phlegmaria. Segmentos de ejes caulinares con trofofilos, esporofilos y esporangios fueron fijados, deshidratados, incluidos en Histowax (parafina), cortados con un micrótomo rotatorio y coloreados usando la técnica tradicional Safranina O-Verde Rápido; además se hicieron cortes a mano alzada y se colorearon con la misma técnica. P. phylicifolius incluye plantas colgantes y péndulas de hasta 40cm de longitud. Los ejes son heterofilos, de aproximadamente 10-20(-25)mm de diámetro en las divisiones basales incluyendo los trofofilos, luego abruptamente reducidos a (l-) 1.5-2(-2.5)mm de diámetro incluyendo los esporofilos reducidos e imbricados. Los trofofilos están dispuestos en anillos alternantes de a tres, o decusados, subdecusados o alternos, dispuestos en forma espaciada en los ejes caulinares, perpendiculares al tallo hasta falcadamente ascendentes, lanceolados a lineal-lanceolados, con márgenes lisos o levemente revolutos. Cada licofilo está provisto de un haz vascular simple y central, conectado a un polo de protoxilema de la estela y sin laguna foliar. Los tallos poseen un ancho de 0.7-1.2mm en la base, excluyendo los licofilos, estrechándose hasta cerca de 0.5mm hacia el ápice. Los ejes caulinares presentan una epidermis uniestratificada y endodermis, la corteza se caracteriza por la presencia de una estructura trabecular de origen lisígeno formada en el tejido parenquimático próximo a la endodermis. El tejido vascular ocupa la parte central del eje caulinar, formando una plectostela de organización subradiada, con cinco polos de protoxilema. Las células epidérmicas presentan paredes anticlinales sinuosas; las invaginaciones en la cara interna de la pared periclinal externa podrían ser probablemente un característica morfológica adaptativa a un ambiente con períodos de sequía. Las hojas de las porciones apicales son decusadas o subdecusadas, con esporangio de disposición continua o discontinua, adpresas, abaxialmente redondeadas a carinadas, ampliamente lanceoladas a ovadas o subcordadas, ápice agudo a mucronado o cuspidado, más corto que el esporangio. Cada esporangio se origina de un grupo de células epidérmicas, en la axila de los esporofilos con el eje caulinar. Las paredes celulares de las células epidérmicas del esporangio son de tipo Huperzioideae. El estudio de la morfología de los trofofilos contribuye a confirmar las diferencias entre P. phylicifolius y P. subulatus.

[Ontogeny of the sporangium, spore formation and cytochemistry in Colombian Lycopodials (Lycopodiaceae)]. / 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 0.2-0.5 microm 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 (3-5 microm) 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.

Continuous morphological variation correlated with genome size indicates frequent introgressive hybridization among Diphasiastrum species (Lycopodiaceae) in Central Europe.

Introgressive hybridization is an important evolutionary process frequently contributing to diversification and speciation of angiosperms. Its extent in other groups of land plants has only rarely been studied, however. We therefore examined the levels of introgression in the genus Diphasiastrum, a taxonomically challenging group of Lycopodiophytes, using flow cytometry and numerical and geometric morphometric analyses. Patterns of morphological and cytological variation were evaluated in an extensive dataset of 561 individuals from 57 populations of six taxa from Central Europe, the region with the largest known taxonomic complexity. In addition, genome size values of 63 individuals from Northern Europe were acquired for comparative purposes. Within Central European populations, we detected a continuous pattern in both morphological variation and genome size (strongly correlated together) suggesting extensive levels of interspecific gene flow within this region, including several large hybrid swarm populations. The secondary character of habitats of Central European hybrid swarm populations suggests that man-made landscape changes might have enhanced unnatural contact of species, resulting in extensive hybridization within this area. On the contrary, a distinct pattern of genome size variation among individuals from other parts of Europe indicates that pure populations prevail outside Central Europe. All in all, introgressive hybridization among Diphasiastrum species in Central Europe represents a unique case of extensive interspecific gene flow among spore producing vascular plants that cause serious complications of taxa delimitation.

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

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 alciánhematoxilina. 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.

Trends and concepts in fern classification.

BACKGROUND AND AIMS: Throughout the history of fern classification, familial and generic concepts have been highly labile. Many classifications and evolutionary schemes have been proposed during the last two centuries, reflecting different interpretations of the available evidence. Knowledge of fern structure and life histories has increased through time, providing more evidence on which to base ideas of possible relationships, and classification has changed accordingly. This paper reviews previous classifications of ferns and presents ideas on how to achieve a more stable consensus. SCOPE: An historical overview is provided from the first to the most recent fern classifications, from which conclusions are drawn on past changes and future trends. The problematic concept of family in ferns is discussed, with a particular focus on how this has changed over time. The history of molecular studies and the most recent findings are also presented. KEY RESULTS: Fern classification generally shows a trend from highly artificial, based on an interpretation of a few extrinsic characters, via natural classifications derived from a multitude of intrinsic characters, towards more evolutionary circumscriptions of groups that do not in general align well with the distribution of these previously used characters. It also shows a progression from a few broad family concepts to systems that recognized many more narrowly and highly controversially circumscribed families; currently, the number of families recognized is stabilizing somewhere between these extremes. Placement of many genera was uncertain until the arrival of molecular phylogenetics, which has rapidly been improving our understanding of fern relationships. As a collective category, the so-called 'fern allies' (e.g. Lycopodiales, Psilotaceae, Equisetaceae) were unsurprisingly found to be polyphyletic, and the term should be abandoned. Lycopodiaceae, Selaginellaceae and Isoëtaceae form a clade (the lycopods) that is sister to all other vascular plants, whereas the whisk ferns (Psilotaceae), often included in the lycopods or believed to be associated with the first vascular plants, are sister to Ophioglossaceae and thus belong to the fern clade. The horsetails (Equisetaceae) are also members of the fern clade (sometimes inappropriately called 'monilophytes'), but, within that clade, their placement is still uncertain. Leptosporangiate ferns are better understood, although deep relationships within this group are still unresolved. Earlier, almost all leptosporangiate ferns were placed in a single family (Polypodiaceae or Dennstaedtiaceae), but these families have been redefined to narrower more natural entities. CONCLUSIONS: Concluding this paper, a classification is presented based on our current understanding of relationships of fern and lycopod clades. Major changes in our understanding of these families are highlighted, illustrating issues of classification in relation to convergent evolution and false homologies. Problems with the current classification and groups that still need study are pointed out. A summary phylogenetic tree is also presented. A new classification in which Aspleniaceae, Cyatheaceae, Polypodiaceae and Schizaeaceae are expanded in comparison with the most recent classifications is presented, which is a modification of those proposed by Smith et al. (2006, 2008) and Christenhusz et al. (2011). These classifications are now finding a wider acceptance and use, and even though a few amendments are made based on recently published results from molecular analyses, we have aimed for a stable family and generic classification of ferns.

Complete plastome sequences of Equisetum arvense and Isoetes flaccida: implications for phylogeny and plastid genome evolution of early land plant lineages.

BACKGROUND: Despite considerable progress in our understanding of land plant phylogeny, several nodes in the green tree of life remain poorly resolved. Furthermore, the bulk of currently available data come from only a subset of major land plant clades. Here we examine early land plant evolution using complete plastome sequences including two previously unexamined and phylogenetically critical lineages. To better understand the evolution of land plants and their plastomes, we examined aligned nucleotide sequences, indels, gene and nucleotide composition, inversions, and gene order at the boundaries of the inverted repeats. RESULTS: We present the plastome sequences of Equisetum arvense, a horsetail, and of Isoetes flaccida, a heterosporous lycophyte. Phylogenetic analysis of aligned nucleotides from 49 plastome genes from 43 taxa supported monophyly for the following clades: embryophytes (land plants), lycophytes, monilophytes (leptosporangiate ferns + Angiopteris evecta + Psilotum nudum + Equisetum arvense), and seed plants. Resolution among the four monilophyte lineages remained moderate, although nucleotide analyses suggested that P. nudum and E. arvense form a clade sister to A. evecta + leptosporangiate ferns. Results from phylogenetic analyses of nucleotides were consistent with the distribution of plastome gene rearrangements and with analysis of sequence gaps resulting from insertions and deletions (indels). We found one new indel and an inversion of a block of genes that unites the monilophytes. CONCLUSIONS: Monophyly of monilophytes has been disputed on the basis of morphological and fossil evidence. In the context of a broad sampling of land plant data we find several new pieces of evidence for monilophyte monophyly. Results from this study demonstrate resolution among the four monilophytes lineages, albeit with moderate support; we posit a clade consisting of Equisetaceae and Psilotaceae that is sister to the "true ferns," including Marattiaceae.

Occurrence and evolutionary origins of polyploids in the clubmoss genus Diphasiastrum (Lycopodiaceae).

Two polyploid taxa are commonly recognized in the genus Diphasiastrum, D. wightianum from Asia and D. zanclophyllum from South Africa and Madagascar. Here we present results from Feulgen DNA image densitometry analyses providing the first evidence for the polyploid origin of D. zanclophyllum. Also reported for the first time are data confirming that D. multispicatum and D. veitchii, representing the putative parent lineages of D. wightianum, are diploids. Phylogenetic analyses of the nuclear regions RPB2, LEAFY and LAMB4 reveal that putative tetraploid accessions are of allopolyploid origin. Diphasiastrum zanclophyllum shows close relationship to the North American taxon D. digitatum on the maternal side, but the paternal relationship is less clear. Two accessions from Asia, both inferred to be polyploid, have D. veitchii as the maternal parent, whereas the paternal paralogs show relationships to D. multispicatum and D. tristachyum, respectively. None of these parental combinations have previously been hypothesized.