Geosiphon pyriforme,a fungus forming endocytobiosis withNostoc (Cyanobacteria), is an ancestral member of the glomales: Evidence by SSU rRNA Analysis

Geosiphon pyriforme inhabiting the surface of humid soils represents the only known example of endocytobiosis between a fungus (Zygomycotina; macrosymbiont) and cyanobacteria (Nostoc; endosymbiont). In order to elucidate the taxonomical and evolutionary relationship ofGeosiphon pyriforme to fungi forming arbuscular mycorrhiza (AM fungi), the small-subunit (SSU) ribosomal RNA genes ofGeosiphon pyriforme andGlomus versiforme (Glomales; a typical AM fungus) were analyzed and aligned with SSU rRNA sequences of several Basidiomycetes, Ascomycetes, Chytridiomycetes, and Zygomycetes, together with all AM-fungal (Glomales) sequences published yet. The distinct group of the order Glomales, which includesGeosiphon, does not form a clade with any other group of Zygomycetes. Within the Glomales, two main lineages exist. One includes the families Gigasporaceae and Acaulosporaceae; the other one is represented by the genusGlomus, the members of which are very divergent.Glomus etunicatum andGeosiphon pyriforme both form independent lineages ancestral to the Glomales. The data provided by the present paper confirm clearly thatGeosiphon represents a fungus belonging to the Glomales. The question remains still open as to whether or notGeosiphon is to be placed within or outside the genusGlomus, since this genus is probably polyphyletic and not well defined yet.Geosiphon shows the ability of aGlomus-like fungus to form a “primitive” symbiosis with a unicellular photcautotrophic organism, in this case a cyanobacterium, leading to the conclusion that a hypothetical association of aGlomus-like fungus with a green alga as a step during the evolution of the land plants appears probable. Correspondence to: H. Gehrig     

The fungal bladders of the endocyanosisGeosiphon pyriforme,aGlomus-related fungus: cell wall permeability indicates a limiting pore radius of only 0.5 nm

Summary Geosiphon pyriforme, a consortium of aGlomiw-like fungus andNostoc spp., forms syncytial, up to 2 mm long bladders accommodating the endosymbiotic cyanobacteria. The bladders are bordered by an elastic cell wall and have a turgor of about 0.6 MPa, as measured by piercing them with oil filled microcapillaries within different osmolarities of sorbitol. In the presence of certain organic osmolytes in the surrounding medium, the bladders collapsed, i.e., showed cytorrhysis. We studied systematically the cytorrhytic effectivity of the diverse osmolytes in relation to their hydrodynamic molecule radii by a solute-exclusion method with living bladders and those which have been extracted by different methods. The results suggest that the cell wall of the bladders has an unusually small limiting pore size thus representing an effective diffusion barrier for glucose and is virtually impermeable for sucrose for at least 8 h. The pore radii of the cell wall are estimated to be about 0.5 nm. Na₂CO₃ extraction, frequently used to partially extract pectic substances from plant cell walls, strongly increases wall permeability. Electron microscopic observations show an electron-dense outer cell wall layer, perhaps responsible for the low permeability. The finding that the cell wall of theGeosiphon bladders represents an effective osmotic barrier provides not only new insights into the cell physiology ofGeosiphon but may also contribute more generally to a better understanding of the mechanisms of selectivity of transport across the cell walls of AM fungi.Abbreviations AM arbuscular mycorrhiza - DMSO dimethyl sulfoxyde - EDTA ethylenediaminetetraacetic acid - PEG polyethylene glycol - res Einstein-Stokes hydrodynamic radius     

Studies on initiation and development of the partner association inGeosiphon pyriforme (Kütz.) v. Wettstein,a unique endocytobiotic system of a fungus (Glomales) and the cyanobacteriumNostoc punctiforme (Kütz.) Hariot

Summary Phagocytosis ofNostoc filaments byGeosiphon, a fungus closely related to AM forming Glomales, was observed under light microscopes. Incorporation can only be performed ifNostoc primordia come into contact with growing hyphal tips of the fungus. The fungal wall just below the apex softens, and fungal cytoplasm is bulged out repeatedly covering the vegetativeNostoc cells but not the heterocytes. New heterocytes are differentiated by the internalised filament whose cells can increase up to ten times in volume after recovering from incorporation strain. TheNostoc cells are coated stepwise by short finger-shaped protuberances of the fungal hypha. These hernia-like outgrowths first remain separated, after 1 to 2 days they merge. Adjacent hyphal walls inside the complex covering disintegrate. Periphal fungal wall portions are united to form a smooth strong outer envelope. Internalisation is categorised as phagocytosis. The partnership is partly specific,Nostoc strains capable of living endocytobiotically are often partners in other symbioses besidesGeosiphon.Abbreviations AM arbuscular mycorrhiza (formerly VAM vesicular arbuscular mycorrhiza) - DIC differential interference contrast - LD light/dark Dedicated to Prof. Dr. Dr. h.c. Eberhard Schnepf on the occasion of his retirement     

Geosiphon pyriforme,an Endosymbiotic Consortium of a Fungus and a Cyanobacterium (Nostoc), Fixes Nitrogen

The bladders of Geosiphon pyriforme, an endosymbiotic consortium of a fungus and the cyanobacterium Nostoc punctiforme, show nitrogenase activity. This suggests that the organism is capable of nitrogen fixation.     

Molecular phylogeny,taxonomy, and evolution of Geosiphon pyriformis and arbuscular mycorrhizal fungi

Geosiphon pyriformis(Kütz.) v. Wettstein is the only known example of a fungus living in endocytobiotic association with a cyanobacterium. The close phylogenetic relationship of Geosiphonwith some arbuscular mycorrhizal fungi (AMF) and the phylogenetic position of Geosiphonare shown in detail. Comprehensive small subunit (SSU) rRNA sequence analyses allow the erection of a new, molecular phylogeny-based taxonomic system for the AMF, including Geosiphon (Geosiphonaceae). Within the recently described phylum Glomeromycota (with one class, Glomeromycetes), a system including four orders was proposed. The erection of several new families will also be necessary. Evolutionary implications are discussed, referring to different possibilities of the influence of AMF on the colonization of the terrestrial habitat by plants.     

Ultrastructure of hyphae and ascospores in the genus Eremascus eidam

Hyphae and ascospores of Eremascus fertilis and E. albus were studied in ultrathin sections. The lateral wall of the hyphae had a thick electron-light inner layer and a thin dark outer layer. The septa had a simple central pore with or without a plug, and there were Woronin bodies in the vicinity. The wall of the ascospores of E. fertilis showed a thick light inner layer and a thin dark outer layer. In the wall of the spores of E. albus a dark fibrillar layer was present between the light inner layer and the dark outer layer. The spores of this species germinated with a tube the wall of which was continuous with a newly formed layer inside the spore wall.This investigation was supported by the Netherlands Organization for the Advancement of Pure Research (Z. W. O.)     

Ambispora granatensis, a new arbuscular mycorrhizal fungus, associated with Asparagus officinalis in Andalucia (Spain)

A new dimorphic fungal species in the arbuscular mycorrhiza-forming Glomeromycota, Ambispora granatensis, was isolated from an agricultural site in the province of Granada (Andalucía, Spain) growing in the rhizosphere of Asparagus officinalis. It was propagated in pot cultures with Trifolium pratense and Sorghum vulgare. The fungus also colonized Ri T-DNA transformed Daucus carota roots but did not form spores in these root organ cultures. The spores of the acaulosporoid morph are 90-150 μm diam and hyaline to white to pale yellow. They have three walls and a papillae-like rough irregular surface on the outer surface of the outer wall. The irregular surface might become difficult to detect within a few hours in lactic acid-based mountings but are clearly visible in water. The structural central wall layer of the outer wall is only 0.8-1.5 μm thick. The glomoid spores are formed singly or in small, loose spore clusters of 2-10 spores. They are hyaline to pale yellow, (25)40-70 μm diam and have a bilayered spore wall without ornamentation. Nearly full length sequences of the 18S and the ITS regions of the ribosomal gene place the new fungus in a separate clade next to Ambispora fennica and Ambispora gerdemannii. The acaulosporoid spores of the new fungus can be distinguished easily from all other spores in genus Ambispora by the conspicuous thin outer wall.     

Characterization of theGeosiphon pyriforme symbiosome by affinity techniques: confocal laser scanning microscopy (CLSM) and electron microscopy

Summary Geosiphon pyriforme represents a photoautotrophic endosymbiosis of aGlomus-like fungus with the cyanobacteriumNostoc punctiforme. The fungus forms unicellular bladders of up to 2 mm in length and 0.5 mm in diameter growing on the soil surface and harboring the endosymbioticNostoc filaments. The cyanobacteria are located in a compartment (the symbiosome) bordered by a host membrane. The space between this symbiosome membrane (SM) and theNostoc cell wall is filled with an about 30–40 nm thick layer of amorphous material, which is present also in the regions of the symbiosome where noNostoc filaments are located. At these sites the amorphous material consists of a 20–30 nm thick layer separating the SM. The region between the SM and the cyanobacterium is defined as symbiosome space (SS). Fungal bladders, hyphae and free livingNostoc were analyzed by affinity techniques as well as the material occurring in the SS. FITC-coupled lectins with sugar specificity to -D-mannosyl/-D-glucosyl (Con A), N-acetyl--D-glucosamine oligomers (WGA), -L-fucosyl (UEA-I), -D-galactosyl (RCA-120), -D-galactosyl (BS-I-B₄), N-acetyl--D-galactosamine (HPA), and sialic acid (EBL) residues were tested. WGA binding and calcofluor white staining demonstrated that the bladder wall as well as the SS contain fibrillar chitin. Of the other lectins only Con A clearly labeled the symbiosome. On the contrary, the lectin binding properties of the slime produced by free livingNostoc-colonies indicate the presence of mannose, fucose, GalNAc, sialic acid, and galactose, while chitin or GlucNAc-oligomers could not be detected. The symbiosome was also investigated electron microscopically. WGA-gold binding confirmed the presence of chitin, while a slight PATAg reaction indicated some polysaccharidic molecules within the SS. Our results show that the amorphous material within the SS contains molecules typical of the fungal cell wall and suggest that the SM is related to the fungal plasma membrane. The applied lectins all bind to the hyphal surface, indicating a high molecular complexity. Mannosyl, -galactosyl, and sialic acid residues are strongly exposed at the outer cell wall layer, whereas GlucNAc, GalNAc, and -galactosyl residues seem to be present in smaller amounts. The symbiotic interface established between the fungus andNostoc inGeosiphon shows many similarities to that occurring between fungi and root cells in arbuscular mycorrhizas.Abbreviations AM arbuscular mycorrhiza - BS-I-B₄ Bandeiraea simplicifolia lectin I isolectin B₄ - CLSM confocal laser scanning microscopy - Con A Concanavalin A - EBL elderberry bark lectin I - FITC fluorescein isothiocyanate - HPA Helix pomatia agglutinin - PATAg periodic acid-thiocarbohydrazide-Ag proteinate - SM symbiosome membrane - SS symbiosome space - RCA-120 Ricinus communis agglutinin 120 - UEA-I Ulex europaeus agglutinin I - WGA wheat germ agglutinin Dedicated to Professor Dr. Peter Sitte at the occasion of his 65th birthday     

SPORE WALL ULTRASTRUCTURE OF PROTOSALVINIA

Protosalvinia is an enigmatic fossil which has been historically assigned to several major taxonomic groups. Stratigraphically, the fossil occurs in a narrow range of Upper Devonian sediments. Tetrads of spores are associated with shallow depressions on the surface of approximately 5% of the specimens collected from the Ohio Shale in Columbus, OH. Spores are approximately 250 μm in diameter and have a spore wall which is composed of at least two distinct layers. The outer layer is coarsely laminated in regions where adjacent spores are in contact. Individual laminar units are thinnest toward the inside and gradually thicker toward the surface of the spore. In non-contact regions, the outer layer is composed of globular units. The inner layer of the wall has little discernable structure except for the presence of a distinct suture beneath the proximal trilete mark. This firmly establishes the meiotic nature of these structures. Comparison with eggs and tetraspores of several extant phaeophycean algae shows little similarity.     

Ultrastructure of the ascospores of some species of the Torulaspora group

Development and germination of the ascospores in species of the Torulaspora group of yeasts have been described. Most species had warty spores which, in sections, showed a dark outer layer consisting of the outer unit membrane of the prospore wall and a layer underneath formed at an early stage of development of the spores. In mature spores the light inner layer of the wall was delimited at the outside by a thin dark layer. The warts often contained dark material. The ascospores of two Pichia and three Debaryomyces species were studied for comparison; they differed in sections from the Torulaspora spores. The taxonomic implications of the ultrastructural observations have been discussed.     

Polyamines stimulate hyphal branching and infection in the early stage of <Emphasis Type="Italic">Glomus etunicatum</Emphasis> colonization

Polyamines are known to strongly stimulate hyphal growth in arbuscular mycorrhizal fungi. The effect of the polyamines putrescine, spermidine and spermine on spore germination, hyphal elongation and branching by the AM fungus Glomus etunicatum was investigated in this study. The effect of spermine on infection and the development of the host and of daughter spores was further investigated using the dual monoaxenic culture system comprised of Gl. etunicatum fungal cultures in Ri T-DNA transformed carrot hairy roots. Spermidine and spermine showed positive effects on germination and all three polyamines significantly promoted hyphal growth. Hyphal branching was also strongly stimulated by treatment with polyamines, such as an increase in the number of branches. Infection during the early stages of the in vitro co-culture life cycle was enhanced in the presence of spermine, and daughter spores appeared at earlier timepoints compared to the control. Our results demonstrate that polyamines stimulate germination and hyphal branching in the early stage of AM fungal colonization. Moreover, results from the investigations conducted in the fungus-root co-culture suggest that polyamines may be involved in establishing the symbiotic relationship between root and fungus.     

Isolationin vitro ofStrongwellsea castrans [Fungi: Entomophthorales] a pathogen of adult cabbage root flies,Delia radicum [Dipt.: Anthomyiidae]

The entomogenous fungusStrongwellsea castrans was isolatedin vitro for the first time, by incubating conidia projected from infected cabbage root flies (Delia radicum) in a simple, semi-defined liquid medium comprising dextrose, yeast extract and lactalbumin hydrolysate buffered to pH 7. The fungus grew as long unitunicate hyphae. After transfer to a solid nutrient medium, multinucleate hyphal bodies were formed which developed a thick, laminated wall. Neither conidia nor resting spores developed in liquid or on solid media and the fungus survived successive sub-culturing only in liquid media. Using the API-ZYM system, tests on extracts on hyphae ofS. castrans were positive for 11 enzymes but there were no consistent differences in enzyme profiles betweenS. castrans and fungi of the related genusErynia.      

ULTRASTRUCTURE OF DISPERSED AND IN SITU SPECIMENS OF THE DEVONIAN SPORE RHABDOSPORITES LANGII: EVIDENCE FOR THE EVOLUTIONARY RELATIONSHIPS OF PROGYMNOSPERMS

Abstract: The spore Rhabdosporites (Triletes) langii (Eisenack) Richardson, 1960 is abundant and well preserved in Middle Devonian (Eifelian) ‘Middle Old Red Sandstone’ deposits from the Orcadian Basin, Scotland. Here it occurs as dispersed individual spores and in situ in isolated sporangia. This paper reports on a detailed light microscope (LM), scanning electron microscope (SEM) and transmission electron microscope (TEM) analysis of both dispersed and in situ spores. The dispersed spores are pseudosaccate with a thick walled inner body enclosed within an outer layer that was originally attached only over the proximal face. The inner body has lamellate/laminate ultrastructure consisting of fine lamellae that are continuous around the spore and parallel stacked. Towards the outer part of the inner body these group to form thicker laminate structures that are also continuous and parallel stacked. The outer layer has spongy ultrastructure. In situ spores preserved in the isolated sporangia are identical to the dispersed forms in terms of morphology, gross structure and wall ultrastructure. The sporangium wall is two‐layered. A thick coalified outer layer is cellular and represents the main sporangium wall. This layer is readily lost if oxidation is applied during processing. A thin inner layer is interpreted as a peritapetal membrane. This layer survives oxidation as a tightly adherent membranous covering of the spore mass. Ultrastructurally it consists of three layers, with the innermost layer composed of material similar to that comprising the outer layer of the spores. Based on the new LM, SEM and TEM information, consideration is given to spore wall formation. The inner body of the spores is interpreted as developing by centripetal accumulation of lamellae at the plasma membrane. The outer layer is interpreted as forming by accretion of sporopollenin units derived from a tapetum. The inner layer of the sporangium wall is considered to represent a peritapetal membrane formed from the remnants of this tapetum. The spore R. langii derives from aneurophytalean progymnosperms. In light of the new evidence on spore/sporangium characters, and hypotheses of spore wall development based on interpretation of these, the evolutionary relationships of the progymnosperms are considered in terms of their origins and relationship to the seed plants. It is concluded that there is a smooth evolutionary transition between Apiculiretusispora‐type spores of certain basal euphyllophytes, Rhabdosporites‐type spores of aneurophytalean progymnosperms and Geminospora‐/Contagisporites‐type spores of heterosporous archaeopteridalean progymnosperms. Prepollen of basal seed plants (hydrasperman, medullosan and callistophytalean pteridosperms) are easily derived from the spores of either homosporous or heterosporous progymnosperms. The proposed evolutionary transition was sequential with increasing complexity of the spore/pollen wall probably reflecting increasing sophistication of reproductive strategy. The pollen wall of crown group seed plants appears to incorporate a completely new developmental mechanism: tectum and infratectum initiation within a glycocalyx‐like Microspore Surface Coat. It is unclear when this feature evolved, but it appears likely that it was not present in the most basal stem group seed plants.     

Production of monoclonal antibodies against surface antigens of spores from arbuscular mycorrhizal fungi by an improved immunization and screening procedure

Monoclonal antibodies (mAbs) were produced against surface antigens of chlamydospores of arbuscular mycorrhizal (AM) fungi by immunizing mice with crushed or complete spores. The intrasplenic approach proved to be superior to the intraperitoneal method of immunization with regard to the amount of antigen required for the immune response. The hybridoma technology was combined with an improved screening procedure, applying an immunogold-silver staining technique to semi-thin sections of spores. In this way, mAbs to surface antigens on the outer wall could be selected. Two mAbs were raised against Glomus etunicatum and G. scintillans spores. Cross-reactivities of the antibodies to other structures of the fungus, to other species of Glomus and to other soil-borne fungi were tested with indirect immunofluorescent labelling. The mAbs did not react with non-AM fungi. One mAb (A5B1) selectively recognized G. etunicatum, another (D12F11) exhibited limited interspecies cross-reactivities. One further mAb (H8F7), which reacted with spores of all AM fungi but not with other fungi, was shown to be specific for Bacillus mycoides. The implications are discussed.     

Photosynthetic carbon assimilation in Geosiphon pyriforme (Kützing) F. v. Wettstein,an endosymbiotic association of fungus and cyanobacterium

Geosiphon pyriforme, an endosymbiotic association between a fungus and the cyanobacterium Nostoc, was shown by tracer studies to acquire carbon photosynthetically from CO₂ or bicarbonate. The organism also fixes inorganic carbon in darkness, at lower rates than in the light. The patterns of label distribution are indicative of the operation of the reductive pentose-phosphate pathway in the light and of the phosphoenolpyruvate-carboxylase reaction in the dark. The results are discussed in relation to the evolution of photoautotrophic endosymbiotic associations.This investigation has been supported by the Deutsche Forschungsgemeinschaft. We are indepted to Professor G.B. Feige (Institut für Pflanzenphysiologie, Universität Essen, FRG) for helpful discussion, Karin Faist for her excellent technical assitance and to Doris Schäfer for drawing the figures.     

Ultrastructure of the ascospores of the new yeast genus Sporopachydermia Rodrigues de Miranda

Development of the ascospores of Sporopachydermia lactativora and S. cereana was studied in ultrathin sections. The spores have a very thick wall consisting of a thin dark outer layer and a double light inner layer the outer part of which is very wide and often irregular. During germination, this part disappears, the outer dark layer breaks up and the inner part of the light layer remains around the protoplast during development to a vegetative cell.This investigation was supported by the Netherlands Organization for the Advancement of Pure Research (Z.W.O.).     

A structural comparison of cyst and germ tube wall inPhytophthora palmivora

Summary An electron microscopic analysis of germinating cysts ofPhytophthora palmivora involving freeze-etching, thin sectioning, and replica techniques reveals that both cyst and hyphal wall comprise a two-phase system with a fibrillar and an amorphous component. The cyst wall is fibrillar throughout with the fibrils tightly interwoven and embedded in an amorphous matrix on the internal side of the wall. The hyphal wall consists of a fibrillar inner layer with the fibrils lightly covered by some amorphous material and an amorphous outer layer devoid of any fibrillar material. Both cyst and germ tube walls are wholly or partially covered by a fluffy coat of variable thickness. In the zone of germ tube emergence cyst wall and germ tube wall overlap and are tightly apposed. Thus, the germ tube wall is not a simple extension of the cyst wall but a new structural entity separated from the cyst wall by a thin line of demarcation.     

Effect of Mannitol from Laminaria japonica, other Sugar Alcohols, and Marine Alga Polysaccharides on in vitro Hyphal Growth of Gigaspora margarita and Root Colonization of Trifoliate Orange

A compound that stimulated the growth of an arbuscular mycorrhizal (AM) fungus was isolated from 75% methyl alcohol (MeOH) extracts of a brown alga, Laminaria japonica Areschoug, using high-pressure liquid chromatography (HPLC). This compound (Compound 1) was identified as mannitol by HPLC and nuclear magnetic resonance (NMR) spectroscopy. Compound 1 and purchased polysaccharides (alginic acid, fucoidan, carrageenan and mannan from marine algae) were tested for in vitro hyphal growth of an AM fungus, Gigaspora margarita Becker and Hall. Compound 1 (50–500 mg L⁻¹) and carrageenan (1000 mg L⁻¹) significantly stimulated the hyphal growth of germinating spores of Gi. margarita. The application of 100 mg L⁻¹ of Compound 1 to trifoliate orange (Poncirus trifoliata Raf.) inoculated with Gi. margarita promoted root colonization and increased plant growth. These results suggest low concentrations of mannitol are among the reasons for enhanced hyphal growth and root colonization by the application of algal extracts. Other sugar alcohols (100–300 mg L⁻¹ of xylitol, sorbitol and meso-erythritol) also increased the hyphal growth of Gi. margarita.     

Otospora bareai, a new fungal species in the Glomeromycetes from a dolomitic shrub land in Sierra de Baza National Park (Granada, Spain)

A new fungal species of the Glomeromycetes was isolated from the rhizosphere of Pterocephalus spathulatus and Thymus granatensis, two rare endemic plants growing on dolomite in the Sierra de Baza (Granada, southern Spain). The fungus was propagated in pot cultures of Sorghum vulgare and Trifolium pratense for 4 y and it is described here on the basis of the spores found in nature and formed in pot cultures. Its brown spores (140-210 microm diam) form laterally on a persistent, brown stalk (=neck) of a sporiferous saccule. They have two walls without ornamentation: a brown, three- to four-layered outer wall and a hyaline two- to three-layered inner wall. The unique combination of spore formation and spore wall structure does not fit with any of the known fungal genera. Spore formation is similar to that of Acaulospora spp. and Archaeospora trappei, but Acaulospora spp. has three spore walls with a characteristic "beaded" wall, and the outer wall of Ar. trappei is simple, thin, hyaline and only bilayered. Spore wall structure of the new fungus is similar to that of Entrophospora infrequens, however this fungus forms its spores internally, inside the hyphal stalk of the sporiferous saccule. Molecular analyses of the small subunit of the ribosomal gene phylogenetically place the new fungus next to Diversispora spurca, which forms one-walled glomoid spores (i.e. terminally on hyphae). Based on these analyses we place the new fungus into a new genus in the family Diversisporaceae under the epithet Otospora bareai.     

Cytochemical evidence of a fungal cell wall alteration during infection of Eucalyptus roots by the ectomycorrhizal fungus Cenococcum geophilum

When the ectomycorrhizal fungus Cenococcum geophilum changes from a saprophytic to a symbiotic stage, its cell wall structure becomes simplified. The external hyphal wall layer which, in the saprophytic stage, is highly reactive to the Gomori-Swift test becomes poorly reactive and can no longer be distinguished from the internal wall layer in the Hartig net hyphae. The intensely stained external wall layer was also absent from pure cultures of Cenococcum geophilum grown on a medium with a low sugar content. This cell wall alteration could be due to a decrease in the amount of melanin or of melanin plus cystine-containing proteins. This change may be necessary for increased nutrient exchange between symbionts through hyphal walls.