云贵水韭雌配子体发育及其濒危机制的研究

为了解云贵水韭(Isoetes yunguiensis)的生殖过程和濒危原因,采用人工培养获得其雌配子体,用半薄切片法观察雌配子体发育过程。结果表明,云贵水韭的大孢子萌发率约为26%;雌配子体异养,终生都在大孢子细胞壁内发育;颈卵器发育只有2枚颈沟细胞而无腹沟细胞。雌配子体发育停止在游离核时期、颈壁细胞数量偏少或排列紊乱、颈沟细胞异常、卵细胞凋亡等可能是导致生殖濒危的原因。同时,游离核是水韭生殖生物学研究和系统学研究的重要环节之一;缺失腹沟细胞可能是水韭类简化性进化的特征之一。     

Two new species ofIsoetes (Isoetaceae) from Jeju Island, South Korea

We name and describe two new species,Isoetes jejuensis and I.hallasanensis, from Jeju Island, South Korea. These taxa are compared with related species in East Asia, including I.coreana andI. sinensis. The rugulate megaspore ornamentation ofI. jejuensis differs from those otherIsoetes species. Furthermore,I. hallasanensis varies fromI. asiatica in its microspore ornamentation and chromosome number, although both species have an echinate megaspore ornamentation. These new species are tetraploid (2n = 44), whereasI. coreana is hexaploid (2n = 66).     

Different spore structures in sympatric Isoetes histrix populations and their relationship with gross morphology, chromosome number, and ribosomal nuclear ITS sequences

Traditionally, megaspores have supplied the most relevant character for the taxonomy of Isoetes at several systematic levels, including discriminant features usually used in species identification and diagnosis. Isoetes histrix Bory is a terrestrial circum-Mediterranean quillwort characterized by dark, shiny, and persistent phyllopodia with megaspore sporangia completely covered by a velum and tuberculate megaspores. Specimens of this species from Sardinian temporary wetlands showed the sympatric presence of two kinds of individuals with correlated variation in size, ornamentation, and radial ridges of megaspores, and in ornamentation of microspores. However, they showed the same diploid chromosome number (2n = 20), ITS ribotype, and macromorphological feature. No intermediate individuals, showing mixed characters of each spore types as well as malformed or aborted spores have been detected. These results suggest that the gene flow between both kinds of I. histrix plants is heavily restricted, if not limited at all. On the basis of the cytogenetic and molecular uniformity detected in I. histrix in this study, genomic incompatibilities do not seem to be the main reasons involved in the maintenance of the two kinds of I. histrix individuals. Prezygotic barriers involving changes in phenology (e.g. spore maturation) or differential gamete dispersal should be further assessed to gain insights in this topic. The presence of two kinds of individuals in I. histrix differing in significant spore features used in quillwort taxonomy, whatsoever the causes involved in its origin, could be the basis of an incipient differentiation process upon which selective pressures could ultimately lead to speciation.     

Micromorphology of outer exospore coatings in Selaginella megaspores

Variability of Selaginella megaspore microsculpture is defined and illustrated by means of SEM and TEM. Additional EDX analyses demonstrated that microsculpture elements in the investigated specimens are mainly formed by silica which may be removed by hydrofluoric acid. Our observations suggest that different proportions of sporopollenin/silica are present in the outer coating of at least some Selaginella megaspore walls. Pattern formation mechanisms as well as implications for terminology are discussed. On the basis of this investigation and using data available from the literature, it is argued that the sporoderm layers of Isoetes and Selaginella megaspores are probably homologous, supporting the consensual view.     

Diversity of exine structure in Upper Carboniferous (Westphalian) selaginellalean megaspores

Studies of wall structure in Mesozoic and Recent selaginellalean megaspores have been well documented. However, Palaeozoic examples have received minimal attention. The principal Palaeozoic megaspore genus of likely selaginellalean affinity is Triangulatisporites, extending from the Upper Devonian to the Upper Carboniferous. The particulate wall ultrastructure of a previously published Carboniferous (Duckmantian) megaspore assigned to this genus suggested that this form of wall construction may have been the ancestral wall structure of the group, an observation which posed difficulties in relating selaginellalean ultrastructure to that of other contemporaneous lycopsid megaspores. Subsequent investigation showed that the genus also contains more laminate exines similar to those of other extinct lycopsids and extant Selaginella species. Our new examples of Triangulatisporites ultrastructure from the Langsettian, Duckmantian and Westphalian D yield more information regarding early variation of wall structure within Carboniferous selaginellalean megaspores and suggest that a more laminate wall composition is at least as old as the particulate form. However, without further investigation of Lower Carboniferous forms, we are unable to state which is indeed ancestral. The laminate structure reported here and elsewhere is, none the less, more easily related to comparable ultrastructure in other groups of Carboniferous lycopsid megaspores and could suggest a link with such genera as Zonalesporites and early Lagenicula. This would be in keeping with current concepts regarding the most primitive ultrastructural type within lycopsid megaspore walls.     

ACHLAMYDOCARPON VARIUS COMB. NOV.: MORPHOLOGY AND REPRODUCTIVE BIOLOGY

Structurally preserved arborescent lycopsid fructifications are described from Pennsylvanian age strata in eastern Kentucky and southern Illinois. Achlamydocarpon varius comb. nov. is the name proposed for these cones and previously reported isolated megasporophylls described as Lepidostrobophyllum varius. The specimens range up to 3.5 cm long and represent cone apices. Megasporophylls are spirally arranged and attached to the cone axis at an acute angle. Megasporangia are large with a wall two cell layers thick. Each sporangium contains one large, presumably functional megaspore, and three smaller, abortive megaspores. Functional and abortive spores possess a prominent apical tuft (massa) that covers up to one-third of the proximal surface of the spore. Sporoderm ultrastructure is detailed together with a comparison of morphologically similar sporae dispersae megaspores. The possible function of the megaspore massa is discussed as it relates to the reproductive biology of the cone.     

Ultrastructure and affinity of Lower Carboniferous megaspores from the Moscow Basin, Russia

Ten megaspore species isolated from Moscow Basin lignites of Lower Carboniferous (Viséan) age have been studied by scanning and transmission electron microscopy (SEM and TEM). These species belong to seven megaspore genera: Lagenicula, Sublagenicula, Crassilagenicula, Setosisporites, Zonalesporites, Caudatosporites, and Cystosporites. Megaspores of the genus Caudatosporites have only been described previously from the Duckmantian (Westphalian B); a new species is duly erected. The ultrastructure of megaspore walls from the genera Crassilagenicula and Zonalesporites has not been previously described. This study also places them in context with other contemporaneous megaspores. The study shows that during the Viséan, in the Moscow Basin, megaspores expressed a similar wall ultrastructure despite large differences in external appearance. The genus Crassilagenicula may represent a group of megaspores from plants that had evolved from those bearing gulate megaspores here typified by Lagenicula acuminata, Setosisporites brevispinosus, and Sublagenicula hirsutoida. Zonalesporites brasserti also appears to show affinities to this group, and may be representative of a plant species in a transitional state between the Lagenicula bearing lycopsids and those more isoetalean in nature.     

Morphology and wall ultrastructure of some Middle Devonian dispersed megaspores from northern Poland

Specimens of dispersed Middle Devonian megaspores have been isolated from core samples from the Miastko 1 borehole in Western Pomerania. Comprehensive investigations using light, scanning and transmission electron microscopy supplement previous information on morphology and gross structure and provide data on spore wall ultrastructure of four megaspore species. Corystisporites acutispinosus is azonate; the inner layer is laminate, and the lumen is lined by a thick, laterally continuous lamina. The outer layer consists of small, tangentially aligned tabular elements that become wider, more extensive and irregularly arranged toward the outside. Coronispora variabilis is a coronate megaspore; the inner layer appears homogenous and is probably lamellate. The outer layer consists of elongate, cylindrical, branching elements that are overlaid within the proximal part of the body by a lamellate, compact, almost homogenous layer. Grandispora ciliata is pseudosaccate. The inner body is laminate with laminae thickening and becoming less continuous and less tightly packed toward the outside. The outermost region of the inner body and the innermost region of the outer envelope consist of tabular and cylindrical elongate units. The bulk of the outer wall is almost homogenous, and near the surface it is granular. Pomeranisporites subtriangularis is pseudozonate. The inner layer appears homogenous except for the presence of a single innermost lamina. The inner part of the outer layer may represent small tabular and cylindrical elements, and the outer part comprises folded laminae. The megaspores studied share numerous features of morphology and wall ultrastructure with the lycopsids, putative lycopsids, and some enigmatic Devonian plants.     

中国产3种水韭叶舌形态结构的比较研究

以中国产3种水韭的成熟叶片基部为实验材料,采用石蜡切片法,详细观察3种水韭的叶舌结构,建立各自叶舌的立体模型,探讨3种水韭间的亲缘关系,并比较了中国特产水韭与中亚及北美水韭的演化关系。结果显示:(1)3种水韭叶舌结构主要分为舌片、舌足和横带三部分。(2)中华水韭与东方水韭舌片均为三叉型,有主侧舌片之分,足角均为卵圆形,舌足与叶轴平行,而云贵水韭长鼻形,无主侧舌片之分,足角为三角形,舌足与叶轴有一定的角度。(3)中华水韭与云贵水韭的舌足侧面观为长椭圆形,东方水韭舌足侧面观为肾形。研究认为,中华水韭与东方水韭的亲缘关系较近,二者与云贵水韭亲缘关系较远;叶舌是水韭类的溯祖形态,其结构复杂,特征稳定,种间差异明显,应该作为水韭分类的重要依据。     

FURTHER OBSERVATIONS ON NATHORSTIANA (ISOETACEAE)

The patterns of root arrangement and stelar morphology in the Lower Cretaceous fossil Nathorstiana are essentially identical with those of extant Isoetes. These structural similarities imply a similar mode of development in both plants and are used to infer an Isoetes-like, linear, root-producing meristem along the lower end of the stele in Nathorstiana. The root-bearing base of Nathorstiana differs from that of Isoetes principally in two respects. In earlier developmental stages, the rooting base of Nathorstiana was unlobed and radially symmetrical, whereas Isoetes is originally bilobed. Unlike Isoetes, which lacks stelar elongation and sheds its root-bearing cortex at the periphery of the cortical lobes, the downward growth of the root-bearing base of Nathorstiana resulted in the accumulation of a substantial extent of axial root-bearing surface.     

Megaspore development in Selaginella. I. “Wicks”, their presence,ultrastructure, and presumed function

Summary Structures have been found in the locular space between the tapetal cells and megaspores in Selaginella argentea and S. kraussiana that enter the megaspore wall and extend to the plasma membrane of the megaspore cytoplasm. We have called these structures wicks. Unless special fixation procedures are used wicks are either very poorly preserved or not apparent. Wicks appear to be routes for the transport of materials from the tapetum to developing megaspores. The entry of the wicks into the megaspore wall and their passage throughout the wall implies that the megaspore wall of Selaginella is a three-dimensional mesh-work of inter-connecting spaces. Wicks have several macromolecular-sized subunits, and the results of our histochemical reactions indicated the presence of glycoprotein and/or mucopolysaccharide. X-ray microanalysis of the S. convoluta exospore showed that silicon is present in rod-shaped structures between units of the exospore in mature megaspores. Because of the size and form of the structures between the exospore units we consider that they are remnants of wicks stabilized by silicon.Present address:Cátedra de Palinologia, Museo de La Plata, Paseo del Bosque s/nro., 1900 La Plata, Argentina.     

The quillworts (Isoetes) of India: distribution, endemism and species radiation

The genus Isoetes L. in India is represented by 14species, of which eight species are recognized as being local endemics [confinedto one particular phyto-geographical division (PGD)] while the remaining sixoccur in more than one PGD and are described as endemic to a wider range. Thelocal endemic species are Isoetes dixitei,Isoetes panchganiensis and Isoetessahyadriensis in Western Ghats region; Isoetespantii, Isoetes bilaspurensis, Isoetesreticulata and Isoetes tuberculata inChotanagpur Malwa Vindhya Plateau and Isoetes debii innortheastern India. The wider endemic species are Isoetespanchananii, Isoetes sampathkumaranii,Isoetes rajasthanensis, Isoetesmahadevensis, Isoetes indica andIsoetes coromandelina. Our studies on the patterns ofendemism suggest that the radiation of quillworts advanced from dry lowlandareas to the rainy uplands and mountains. Isoetescoromandelina is the first Indian quillwort to colonize in lowlandsof the coastal zone (Coromandel), from where it spread to different parts of thesub-continent and gave rise to new species. Thus this species is a key Indianspecies which has played an important role in the radiation of quillwort in thecountry and appeared as the connecting link among the quillwort flora of variousPGDs. The centres of diversity for almost all the presently known Indianquillworts species are recognized.     

STUDIES ON FOSSIL AZOLLA: PRIMITIVE TYPES OF MEGASPORES AND MASSULAE FROM THE CRETACEOUS

Fossil Salviniaceae are described from the Claggett Shale and Judith River Formation, late Cretaceous (Campanian stage) of Montana. A new genus, Parazolla, from the Claggett Shale, has megaspores in which the swimming apparatus is composed of a number of elongate floats attached to the megaspore body and invested by coiled hairs. The floats separate at maturity. Massulae (bearing microspores) have simple hair-like glochidia, many of which are knobbed at their tips. Glochidia tend to resemble the perisporial hairs of the megaspore body. This resemblance provides fossil evidence of the homology of these two hair-like structures among living species of Azolla. In Azolla simplex from the Judith River Formation the megaspore has a single cap-like so-called columellate float. Massulae, which have anchor-shaped glochidia, are associated with these megaspores. A. simplex is the oldest species of Azolla and Parazolla the oldest member of the Salviniaceae so far found.     

A CONTRIBUTION TO THE EARLY TERTIARY FOSSIL RECORD OF THE SALVINIACEAE

Megaspores and massulae of Azolla, Azollopsis, and Salvinia are recorded from the Paleocene and Eocene of Montana and the Dakotas. Three new species of Azolla are described and two species of Azolla are redescribed. The columella of the floating apparatus of the megaspore apparatuses of Azolla appears to be a phylogenetic localization of the perispore around the megaspore. A new section of Azolla (section Kremastospora) is created for species whose megaspore apparatuses have many floats and whose massulae have hooked (anchor-shaped) glochidia. Salvinia preauriculata is based only on leaf remains from the Eocene of North America. Megaspores and massulae which probably are conspecific with the leaf remains are described. The megaspores and massulae of the fossil species are much smaller than those of the living species, S. auriculata, with which S. preauriculata has been compared. The similar size of the megaspores and massulae of the fossil species suggests a less specialized condition than in living species, where these two structures differ greatly in size. Azollopsis tomentosa, previously known from the late Cretaceous, has been found in the Eocene.     

Callose in cell walls during megasporogenesis in angiosperms

Summary Callose was detected by fluorescence microscopy in megasporogenesis in all investigated species with mono- and bisporic embryo-sac development. Callose occurs first in the meiotic prophase in the chalazal part of the megasporocyte wall and by the first meiotic metaphase the whole cell is enveloped in a callose-containing wall. Later, there is a marked decrease of callose fluorescence, usually at the chalazal end of the megasporocyte. In Oenothera, where the micropylar megaspore is active, decrease of fluorescence takes place at the micropylar pole of the megasporocyte. Callose appears centrifugally in the cell plates forming eventually the walls dividing the megaspores. It disappears from the walls of the megaspores during degeneration and differentiation.     

Micromorphological approach to the systematics of Mediterranean Isoëtes species (Isoëtaceae,Lycopodiophyta): analysis of the megaspore surface

Megaspore ornamentation is one of the few morphological characters used in the taxonomy of the genus Isoëtes. In the present work, we test the application of this character for distinguishing some Isoëtes species occurring in the Mediterranean: Isoëtes sicula, which according to some authors should be included as a variety in I. histrix, and the recently described I. todaroana, whose affinity with other taxa is currently unknown. Two additional species (I. duriei, I. velata) were also included in the analysis. The megaspores were studied using scanning electron microscopy combined with energy-dispersive X-ray spectroscopy and chemical treatment. In all species, the megaspore surface is covered by a siliceous coating; removal of this coating reveals an underlying three-dimensional network of fused rodlets. A unique pattern of this network occurs in I. sicula, supporting its separation from I. histrix. Comparison between the patterns observed in the examined Mediterranean species shows that I. todaroana is most similar to I. histrix.     

ULTRASTRUCTURAL STUDIES OF IN SITU DEVONIAN SPORES: BARINOPHYTON CITRULLIFORME

Each sporangium in the Upper Devonian taxon Barinophyton citrulliforme contains both microspores and megaspores. Microspores range up to 50 μm in diam and possess a homogeneous sporoderm characterized by an outer separable layer. The sporoderm of the megaspores (up to 900 μm) is constructed of sporopollenin units that are loosely arranged in the outer portion of the wall, and that give the megaspore wall a spongy organization. Ultrastructural evidence suggests that the small spores were not abortive megaspores, but that both spore types were functional. The spores of this plant, as well as other Devonian spores that show less dramatic size differences, are suggested as demonstrating a phase in the evolution of heterospory where sex determination was established in spores within the same sporangium prior to the evolution of micro- and megasporangia.     

Casparian Strips in the Leaf Intrastelar Canals of Isoetes duriei Bory, a Mediterranean Terrestrial Species

Anatomical observations, using light and fluorescence microscopy,were made on leaves of Isoetes duriei to verify the presenceof casparian bands around the intrastelar canals. This peculiaranatomical feature, previously reported for some Isoetes species,is confirmed. The possible role of this endodermis-like structure,in the transport of water due to root pressure or in the accumulationof certain metabolites, is discussed in relation to the ecologicaland anatomical features of the species. Copyright 2000 Annalsof Botany Company Isoetes duriei, Lycopsida, Mediterranean, leaf anatomy, endodermis, casparian strips, fluorescence microscopy     

Megaspores of an early Miocene aquatic lycopod (Isoetales) from Antarctica

The paucity of late Paleogene and Neogene floras from Antarctica limits our ability to understand the interplay between Antarctic climate evolution and the impact that glaciation had on the vegetation, in particular, how the vegetation changed from temperate Eocene forests, to today’s sparse vegetation. Fluvial and lacustrine strata deposited in a wet-based glacial sequence (Friis Hills, McMurdo Dry Valley sector, Transantarctic Mountains) have yielded abundant megaspores. These strata are early Miocene based on correlation with a volcanic ash dated at 19.76 ± 0.11 Ma. The megaspores are up to 736 µm in diameter with well-developed wing-like laesurae and equatorial zona. The morphology is consistent with extant Isoetes, and demonstrates the presence of Lycopsida and the Isoetaceae within Antarctic Miocene floras. Today, Isoetes is widespread from the Tropics to the Arctic such as Greenland (I. echinospora, I. lacustris) and from marginal marine (I. ekmanii) to high altitudinal environments (I. lechleri), though commonly associated with lacustrine or aquatic environments. The fossil spores occur in fluvial and lacustrine beds, suggesting the parent plants were aquatics. The occurrence together with mosses and Nothofagus leaves points to persistent vegetation in the early Miocene of Antarctica.