| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Department of Biological Sciences, University of Alberta, Edmonton, AB, T6G 2E9 Canada
| ABSTRACT |
|---|
|
|
|---|
Two new psychrophilic Pseudogymnoascus species with Geomyces anamorphs are described from a Sphagnum bog in Alberta, Canada. Pseudogymnoascus appendiculatus has long, branched, orange appendages and smooth, fusoid to ellipsoidal ascospores with a faint longitudinal rim. Pseudogymnoascus verrucosus has short, subhyaline appendages and warty peridial hyphae and ascospores, and both smooth to asperulate and irregularly warty conidia. Both species produce asci in chains, a feature that supports the distinction between this group and Myxotrichum, which produces asci singly. The discovery of species intermediate between Pseudogymnoascus and Gymnostellatospora, in having both ornamented ascospores and Geomyces anamorphs, prompted a re-evaluation of the genera. Sequence analysis of the internal transcribed spacer regions (ITS) of the nuclear ribosomal DNA indicates that the two genera remain distinct and comprise a monophyletic group. Pseudogymnoascus species have smooth to warty or lobate-reticulate ascospores while species of Gymnostellatospora have walnut-shaped spores with distinct longitudinal crests and striations. Anamorphs assignable to the form genus Geomyces are allied with both genera. A key is provided to the four species and varieties of Pseudogymnoascus.
Key words: Ascospore ornamentation, Geomyces, Gymnostellatospora, ITS sequences, Myxotrichaceae, phylogeny, Pseudogymnoascus
| INTRODUCTION |
|---|
|
|
|---|
The Myxotrichacaeae was placed in the Onygenales (Currah 1985
) but molecular data show it would be better disposed among the inoperculate discomycetes (Leotiomycetes) (Sugiyama et al 1999
, Mori et al 2000
, Gibas et al 2000). These data also suggest that Myxotrichum and Oidiodendron form a lineage separate from Pseudogymnoascus, Gymnostellatospora and Geomyces (Mori et al 2000
, Gibas et al 2002
).
During a survey of cellulose- and lignin-degrading fungi in a Sphagnum bog in the southern boreal forest of western Canada, numerous isolates assignable to Geomyces were obtained from bait blocks made of brown-rotted spruce that had been buried in the upper layers of the Sphagnum moss for 812 mo. Some of these isolates developed ascomata similar to those found in Pseudogymnoascus and Gymnostellatospora but their characteristics did not match any described species.
Two unique species were discerned: one with orange peridial hyphae, long, concolorous, branched appendages, ascospores with a faint longitudinal rim, and smooth to asperulate conidia; and a second with warty, red to red-brown peridial hyphae, short, unbranched appendages, irregularly ornamented ascospores, and smooth to asperulate and coarsely tuberculate conidia. Because these suites of character states suggested the new species might occupy intermediate positions between Pseudogymnoascus and Gymnostellatospora, we compared the nuclear ribosomal region of 24 isolates representing the two new species and 11 similar anamorphic or teleomorphic taxa in the Myxotrichaceae.
| MATERIALS AND METHODS |
|---|
|
|
|---|
|
DNA sequencing.
Three isolates of Pseudogymnoascus appendiculatus and two isolates of P. verrucosus were sequenced along with Geomyces asperulatus, G. pannorum, Geomyces sp., Gymnostellatospora alpina, Gy. canadensis, Gy. frigida, Gy. japonica, Gy. subnuda, and P. roseus var. roseus (TABLE I
). For outgroup comparison a sequence of Myxotrichum chartarum (AF062813
[GenBank]
) was obtained from GenBank.
Cultures were grown on OA overlaid with a cellophane membrane (Carmichael 1962
, Gibas et al 2002
). DNA extraction followed a modification of Cubero et al (1999)
and Gibas et al (2002)
. Approximately 100 mg of mycelium was scraped from the surface of the membrane and placed in a sterile 2 mL screw-cap microcentrifuge tube, containing acid-washed sand, a ceramic bead, and 750 µL CTAB extraction buffer (2% w/v cetyltrimethyl ammonium bromide, 1 M NaCl, 100 mM Tris, 20 mM EDTA). The mycelium was ground by centrifuging at least 2 min at maximum speed, then the entire mixture was transferred into a second tube and 1.5 µL ß-mercaptoethanol was added before incubating 2 h at 65 C. Seven hundred fifty µL of chloroform : isoamyl alcohol (24 : 1 v/v) was added, and the solution was mixed by inverting the tube about 20 times and centrifuging for 15 min at 10000 g at room temperature. The upper aqueous layer, containing crude DNA, was collected and purified with the QIAquick PCR purification kit (QIAGEN Inc, Mississauga, Ontario). Purified DNA was stored at 20 C.
The nuclear ribosomal region that includes the internal transcribed spacer (ITS) 1, 5.8S, and ITS2, was amplified with the primer pair NS1/ITS4 (White et al 1990
). PCR reactions were subjected to 30 cycles on a Perkin Elmer GeneAmp 9700 Thermal Cycler (PE Applied Biosystems, Foster City, California). Primers ITS1, ITS2, ITS3 and ITS4 were used to obtain sequence data for both strands using the BigDyeTM Terminator Cycle Sequencing Kit (Applied Biosystems) and run on an ABI 377 Automated Sequencer (Amersham Pharmacia Biotech Inc, Piscataway, New Jersey). Consensus sequences were obtained with the SequencherTM 4.0.2 (Gene Codes Corp., Ann Arbor, Michigan) and aligned manually by eye with Se-Al v 2.0a11 (University of Oxford). Phylogenetic analyses were run with PAUP (phylogenetic analysis using parsimony) v. 4.0b10 (Swofford 2002
) and the robustness of the resulting phylogenetic trees and inferred clades was tested with bootstrap analysis (Felsenstein 1985
) of 100 resamplings.
| TAXONOMY |
|---|
|
|
|---|
|
|
Ascomata fiunt in frigore 28 menses post incubationem, vel solitaria vel in globis, globosa ad subglobosa, primum alba, deinde aurantiaco-brunnea in maturitate, appendicibus inclusis 300650 µm diam. Hyphae peridiales aurantiaco-flavae, leves, septatae, crassiter tunicatae, 22.5 µm diam, ramosae, anastomosis reticuloperidium format. Appendices aurantiaco-flavae, crassiter tunicatae, septatae, dichotomose ramosae, leves, cum extremis fastigatis, 40120 µm longae. Asci octospori, hyalini, globosi ad subglobosi, deliquescentes, 57 µm diam. Ascosporae 2.55 x 1.52.5 µm, hyalinae, fusoideae ad ellipsoideae, crista longitudinalis et indistincta. Status anamorphosis a Geomyci. Conidiophora tenuiter distincta, erecta, hyalina, tenuiter et leviter tunicata, dendritica, verticillate ramosa. Conidia alba ad pallide alba. Conidia terminalia subglobosa ad late pyriformia, cicatrix basalis et prominens, levia ad minute asperulata, 2.53.5 x 1.52.5 µm. Conidia intercalaria subglobosa ad elongata et dolioformia, extremis vel magis vel minus truncatis, levia ad minute asperulata, 35 x 22.5 µm. Isolata ex ligno brunneo-putrefacto piceae marianae in sphagno palustro submersae.
Holotypus: Colonia exsiccata ex UAMH 10509 isolato ex ligno brunneo-putrefacto piceae marianae in sphagno palustro submersae.
Colonies on OA 4045 mm diam at 28 d at 15 C and 3847 mm diam at 5 C, appressed, white, producing a diffusible yellow pigment and a clear exudate; reverse yellow. Aerial conidia abundant, white. Colonies on CMA 3540 mm diam at 15 C and 3340 mm diam at 5 C, appressed, colorless, consisting of immersed, hyaline hyphae; reverse colorless. Aerial conidia sparse, patchy, white. Ascomata produced after 28 mo on CMA at 5 C and 15 C and after 3 mo on OA at 5 C. Ascomata solitary or in clusters, globose to subglobose, white at first, peridial hyphae and appendages becoming orange-brown at maturity (FIG. 1
), 200450 µm diam excluding appendages, 300650 µm diam including appendages (FIGS. 1
, 8
); centrum white. Peridial hyphae orange, smooth, septate, thick-walled, 22.5 µm diam, branched and anastomosed to form a reticuloperidium, giving rise to appendages (FIGS. 2
, 9
). Appendages orange, thick-walled, septate, thickened at each septum, branched, smooth, tapering toward apices, 40120 µm long (FIGS. 2
, 9
). Asci 8-spored, hyaline, globose to subglobose at maturity, deliquescent, 57 µm diam (FIGS. 3
, 12
). Immature asci subglobose to globose (FIGS. 11, 12
) or clavate (FIG. 10
), stipitate and borne singly (FIGS. 10, 12
), or sessile and borne in chains (FIG. 11
). Ascospores hyaline, fusoid to ellipsoidal, thick-walled, smooth or with an indistinct longitudinal rim (FIG. 4
, 13, 14
), 2.55 x 1.52.5 µm (FIGS. 4
, 13, 14
). Anamorph: Geomyces sp. (FIGS. 57
, 15, 16
). Conidia white to off-white en masse. Aleurioconidia terminal, subglobose to broadly pyriform with prominent truncate basal scars, hyaline, relatively thin-walled, smooth to minutely asperulate, 2.53.5 x 1.52.5 µm (FIGS. 5, 7
, 15, 16
). Intercalary arthroconidia subglobose to elongate and barrel-shaped with more or less truncate ends, hyaline, thin-walled, smooth to minutely asperulate, 35 x 22.5 µm (FIG. 6
). Conidia borne in long chains on undifferentiated hyphae (FIG. 6
), or verticillately branched conidiophores that are erect, hyaline, thin- and smooth-walled, 540 x 1.52.5 µm, with branches fragmenting basipetally into rhexolytically dehiscent arthroconidia or aleurioconidia (FIG. 5
). Conidiophores sometimes synnematous (FIGS. 7
, 16
).
Holotype: Dried culture of UAMH 10509 from brown-rotted black spruce wood under Sphagnum peat.
Other specimens: CANADA. ALBERTA: 5 km east of Perryvale (54°28'N, 113°16'W), Picea mariana-Sphagnum fuscum bog, ex brown-rotted wood bait block, 2002, A. Rice (UAMH 10510, UAMH 10511, UAMH 10512).
Pseudogymnoascus verrucosus Rice and Currah sp. nov. FIGS. 17
25
|
|
Ascomata fiunt in frigore post 68 menses, vel solitaria vel in globis, globosa ad subglobosa, primum alba, deinde rubra in maturitate, 150400 µm diam. Hyphae peridiales rubro-brunneae, septatae, crassiter tunicatae, 22.5 µm diam, crassiter asperulatae, alte ramosae; anastomosis reticuloperidium densum format. Appendices elongatae absunt, hyphae peridiales terminant in appendicibus nonnullis et distinctis, tumidis, subhyalinis, verrucosis, 510 x 34 µm. Asci octospori, hyalini, globosi ad subglobosi, deliquescentes, 58 µm diam. Ascosporae 35 x 23 µm, late fusoideae ad ellipsoideae, hyalinae, perispora irregulariter asperulata ad verrucosa. Status anamorphosis a Geomyci. Conidiophora tenuiter distincta, erecta, hyalina, tenuiter et leviter tunicata, dendritica, verticillate ramosa. Conidia alba, massiter ad pallide rosea. Conidia terminalia subglobosa ad late pyriformia, cicatrix basalis et prominens, asperulata ad irregulariter verrucosa in maturitate, 2.54 x 23 µm. Conidia intercalaria subglobosa ad elongata et dolioformia, extremis vel magis vel minus truncatis, asperulata ad irregulariter verrucosa, 2.55 x 23 µm. Isolata ex ligno brunneo-putrefacto piceae marianae in sphagno palustro submersae.
Holotypus: Colonia exsiccata ex UAMH 10579 isolata ex lingo brunneo-putrefacto piceae marianae in sphagno palustro submersae.
Colonies on OA 4045 mm diam at 28 d at 15 C, white, floccose, with a pale orange exudate; aerial hyphae and conidia abundant, white to off-white or pale gray; reverse orange. Colonies on CMA 4448 mm diam at 28 d and 15 C, appressed, colorless, consisting mostly of immersed, hyaline hyphae; reverse colorless. Aerial conidia sparse, concentrated in the center of the colony, initially white, becoming pink with age. Ascomata produced after 68 mo on CMA at 15 C. Ascomata solitary or clumped, globose to subglobose, red at maturity, 150400 µm diam. Peridial hyphae red brown (FIG. 17
), septate, thick-walled, 22.5 µm diam, coarsely asperulate, highly branched and anastomosing to form a dense reticuloperidium (FIGS. 17
, 21
). Distinct appendages absent, peridial hyphae with swollen, thin-walled, sub-hyaline, verruculose apices, 510 x 34 µm (FIG. 17
). Asci 8-spored, hyaline, globose to subglobose, solitary or borne in chains (FIG. 22
), deliquescent, 58 µm diam (FIGS. 18
, 22, 23
). Ascospores broadly fusoid to ellipsoidal, hyaline, thick-walled, irregularly asperulate to verruculose at maturity, 35 x 23 µm (FIGS. 23
). Anamorph: Geomyces sp. (FIGS. 19, 20
, 24, 25
). Conidia white to pale pink en masse. Aleurioconidia terminal, subglobose to broadly pyriform with a prominent truncate basal scar, relatively thick-walled, hyaline to lightly pigmented, asperulate (FIGS. 19
, 24
) or coarsely tuberculate (FIGS. 20
, 24, 25
) at maturity, 2.54 x 23 µm. Arthroconidia subglobose to elongate and barrel-shaped with more or less truncate ends, thickwalled, hyaline to lightly pigmented, asperulate or coarsely tuberculate at maturity, 2.55 x 23 µm (FIG. 25
). Conidiophores erect, hyaline, thin- and smooth-walled, dendritic with verticillate branching, 525 x 11.5 µm (FIG. 19
).
Holotype: Dried culture of UAMH 10579 from brown-rotted black spruce wood buried under Sphagnum peat.
Other specimen: CANADA. ALBERTA: 5 km east of Perryvale (54°28'N, 113°16'W), Picea mariana-Sphagnum fuscum bog, ex brown-rotted spruce wood bait, Jul 2002, A. Rice (UAMH 10580, paratype).
| KEY TO SPECIES OF PSEUDOGYMNOASCUS |
|---|
|
|
|---|
|
| RESULTS |
|---|
|
|
|---|
|
| DISCUSSION |
|---|
|
|
|---|
Raillo (1929)
erected Pseudogymnoascus (Gymnoascaceae) for two species (P. roseus and P. vinaceus Raillo) from soil in the Soviet Union. Two additional species were described from soil in the Soviet Union and Canada before 1980: P. caucasicus Cejp & Milko (Cejp and Milko 1966
) and P. bhatti Samson (Samson 1972
). All four have smooth ascospores and Geomyces anamorphs, characters considered diagnostic for the genus (Samson 1972
, Orr 1979
, Currah 1985
). Currah (1985)
considered the four names synonymous and gave priority to P. roseus. In 1982, P. dendroideus Locquin-Linard from cow dung in Algeria (Locquin-Linard 1982
) and P. alpinus Müller & von Arx from the rhizosphere of Erica carnea L. (Müller and von Arx 1982
) were described. Both had ridged ascospores and poorly developed anamorphs. Udagawa et al (1993)
erected Gymnostellatospora to accommodate species with ornamented ascospores and absent or poorly developed anamorphs. Between 1993 and 2000 five species were described from Japanese and Russian soils and from rotting wood in Canada: Gy. japonica Udagawa, Uchiyama & Kamiya (Udagawa et al 1993
), Gy. frigida Uchiyama, Kamiya & Udagawa (Uchiyama et al 1995
), Gy. canadensis Lumley, Sigler & Currah, Gy. subnuda Sigler, Lumley & Currah (Sigler et al 2000
), and Gy. parvula Udagawa & Uchiyama (Udagawa and Uchiyama 2000
). Udagawa (1997)
also transferred P. dendroideus and P. alpinus into Gymnostellatospora as Gy. dendroidea (Locquin-Linard) Udagawa and Gy. alpina (Müller & von Arx) Udagawa. The difference between Pseudogymnoascus and Gymnostellatospora was less distinct following the description of P. roseus var. ornatus with ornamented, rather than smooth, ascospores and a Geomyces anamorph (Udagawa and Uchiyama 1999
). Sigler et al (2000)
continued to regard the genera as distinct, despite the presence of ornamented ascospores in P. roseus var. ornatus and anamorphs in Gy. alpina, Gy. frigida and Gy. canadensis, noting that none of these anamorphs was a Geomyces state characteristic of Pseudogymnoascus and that the ascospores of P. roseus var. roseus lacked the longitudinal ridges and crests characteristic of Gymnostellatospora. They added the proviso that the species of Pseudogymnoascus and Gymnostellatospora represent a gradient of morphological types and recommended that DNA sequences should be compared among the species in both genera (Sigler et al 2000
).
DNA sequence analyses of the ITS 1, 5.8S, and ITS 2 regions of the nuclear ribosomal DNA (rDNA) region support Gymnostellatospora and Pseudogymnoascus as distinct and place most anamorphic Geomyces isolates sampled here in the Pseudogymnoascus clade although G. asperulatus was included among taxa in the Gymnostellatospora clade and one was in neither clade. The analyses suggest that presence of the distinct longitudinal ridges on ascospores continues to be a reliable morphological character in the definition of Gymnostellatospora.
Species-level relationships are reasonably well supported in Pseudogymnoascus, with P. appendiculatus, P. roseus and P. verrucosus appearing distinct and with P. roseus and P. verrucosus more closely related to each other than to P. appendiculatus. Bootstrap support for P. verrucosus was lower than that for P. appendiculatus and P. roseus although the sequences of the two isolates of P. verrucosus differed at less than 1% of bases. Consistent morphological differences, including the unique tuberculate conidia, further support conspecificity of the strains designated as P. verrucosus. The proximity of the two isolates in the bog also supports their close relationship; the isolates were recovered from bait blocks contained within the same 5 x 10 cm litter bag. The relationship of P. roseus var. ornatus to the type variety and to P. verrucosus cannot be assessed by molecular analyses because cultures are unavailable. Relationships among isolates of Geomyces are not well resolved but the group is clearly a polyphyletic assemblage. Resolution of species-level relationships in Gymnostellatospora awaits sampling of additional isolates.
Patterns of ascus development are rarely mentioned in descriptions of cleistothecial taxa, and the taxonomic importance of this character is unknown. In both new species asci develop asynchronously and in short chains. Tsuneda (1982)
also reported asynchronous ascus development in P. roseus, but this is the first report of catenate asci in the genus (Tsuneda 1982
, Udagawa and Uchiyama 1999
, Sigler et al 2000
). Ascus development in both differs when compared to Myxotrichum deflexum (Rosing 1985
) and M. arcticum (Tsuneda and Currah 2004
) in which asci arise individually from penultimate cells of croziers and develop more or less simultaneously. Tsuneda and Currah (2004)
suggested this pattern of ascus development in M. arcticum is more typical of leotiomycetous than plectomycetous species and supports placement of the Myxotrichaceae among the inoperculate discomycetes. The occurrence of catenate asci in both the Leotiomycetes (e.g. as shown here in Pseudogymnoascus) and in Euriotiomycetes (e.g. Tzean et al 1992) would suggest this feature is convergent in these lineages and that it confers some ecological or developmental advantage related to the cleistothecial form.
Myxotrichaceous fungi, including Geomyces and Oidiodendron species, were among the fungi most frequently isolated from Perryvale Bog (Rice and Currah 2002
, Rice et al 2006
) and their abundance suggests they may be important saprobes in this ecosystem. Most records of Myxotrichaceae are from soil, peat and decaying wood and other organic matter in cool, temperate environments (e.g. Barron 1962
, Barron and Booth 1966
, Udagawa et al 1994
, Hambleton et al 1998
, Udagawa and Uchiyama 1999
, Sigler et al 2000
, Rice and Currah 2006
). In vitro physiological studies of these fungi support the assertion that they are important saprobes in soil, decaying wood and peat in temperate and cool environments. Many are cellulolytic and psychrotolerant or psychrophilic (e.g. Currah 1985
, Udagawa et al 1993
, Uchiyama et al 1995
, Udagawa and Uchiyama 1999
, Sigler et al 2000
, Rice and Currah 2005
). Some species also degrade other plant and fungal residues, including polyphenolic compounds, pectin and chitin, that are common in peat, wood and organic soils. In addition to the saprobic habit, some members of the Myxotrichaceae, including P. roseus (Dalpé 1989
) have been shown to form ericoid mycorrhizal association in vitro and it is possible that at least some occupy a mycorrhizal role in peatlands. The two lineages traditionally included in the Myxotrichaceae are morphologically and ecologically similar, suggesting convergent evolution, possibly in response to a reliance on dispersal by arthropod vectors (Currah 1985
, 1994
; Greif and Currah 2003
).
| ACKNOWLEDGMENTS |
|---|
| FOOTNOTES |
|---|
1 Corresponding author. E-mail: r.currah{at}ualberta.ca
| LITERATURE CITED |
|---|
|
|
|---|
Barron GL. 1962. New species and new records of Oidiodendron. Can J Bot 40:589607.
, Booth C. 1966. A new species of Arachniotus with an Oidiodendron conidial state. Can J Bot 44:10571061.
Carmichael JW. 1962. Chrysosporium and some other aleuriosporic hyphomycetes. Can J Bot 40:11371173.
Cejp K, Milko AA. 1966. Genus Pseudogymnoascus Raillo (Gymnoascaceae).
eská Mykol 20:160163.
Cubero OF, Crespo A, Fatehi J, Bridge PD. 1999. DNA extraction and PCR amplification method suitable for fresh, herbarium-stored, lichenized, and other fungi. Plant Sys Evol 216:243249.[CrossRef]
Currah RS. 1985. Taxonomy of the Onygenales: Arthrodermataceae, Gymnoascaceae, Myxotrichaceae, and Onygenaceae. Mycotaxon 24:1216.
. 1994. Peridial morphology and evolution in the prototunicate ascomycetes. In: Hawksworth DL, ed. Ascomycete systematics: problems and perspectives in the Nineties. New York: Plenum Press. p 281294.
Dalpé Y. 1989. Ericoid mycorrhizal fungi in the Myxotrichaceae and Gymnoascaceae. New Phytol 113:523527.[CrossRef]
Felsenstein J. 1985. Confidence limits on phylogenies: an approach using the bootstrap. Evolution 39:783791.[CrossRef]
Gibas CFC, Sigler L, Summerbell RC, Currah RS. 2002. Phylogeny of the genus Arachnomyces and its anamorphs and the establishment of Arachnomycetales, a new eurotiomycete order in the Ascomycota. Stud Mycol 47:131139.
Greif MD, Currah RS. 2003. A functional interpretation of the role of the reticuloperidium in whole-ascoma dispersal by arthropods. Mycol Res 107:7781.[CrossRef][Medline]
Hambleton S, Egger KN, Currah RS. 1998. The genus Oidiodendron: species delimitation and phylogenetic relationships based on nuclear ribosomal DNA analysis. Mycologia 90:854869.[CrossRef]
Locquin-Linard M. 1982. Pseudogymnoascus dendroideus Locquin-Linard, nouvelle espèce de Gymnoascale (Ascomycètes) coprophile dAfrique du Nord. Cryptog, Mycol 3:409414.
Lumley TC, Gignac LD, Currah RS. 2001. Microfungus communities of white spruce and trembling aspen logs at different stages of decay in disturbed and undisturbed sites in the boreal mixedwood region of Alberta. Can J Bot 79:7692.[CrossRef]
Mori Y, Sato Y, Takamatsu S. 2000. Molecular phylogeny and radiation time of Erysiphales inferred from the nuclear ribosomal DNA sequences. Mycoscience 41: 437447.[CrossRef]
Müller E, von Arx JA. 1982. Pseudogymnoascus alpinus nov. spec. Sydowia 35:135137.
Orr GF. 1979. The genus Pseudogymnoascus. Mycotaxon 8:165173.
Raillo A. 1929. Beiträge zur Kenntnis der Boden-Pilze. Zentralblatt fur Bakteriologie und Parasitenkunde Jena Abt 2 78:515524.
Rice AV, Currah RS. 2002. New perspectives on the niche and holomorph of the myxotrichoid hyphomycete, Oidiodendron maius. Mycol Res 106:14631467.[CrossRef]
, . 2005. Oidiodendron: a survey of the named species and related anamorphs of Myxotrichum. Stud Mycol 53:83120.
, Tsuneda A, Currah RS. 2006. In vitro decomposition of Sphagnum by some microfungi resembles white rot of wood. FEMS Microbiol Ecol 56:372382.
Rosing WC. 1985. Fine structure of cleistothecia, asci, and ascospores of Myxotrichum deflexum. Mycologia 77:920926.[CrossRef]
Samson RA. 1972. Notes on Pseudogymnoascus, Gymnoascus, and related genera. Acta Botan Neerland 21:517527.
Sigler L, Lumley TC, Currah RS. 2000. New species and records of saprophytic ascomycetes (Myxotrichaceae) from decaying logs in the boreal forest. Mycoscience 41:495502.[CrossRef]
Sugiyama M, Ohara A, Mikawa T. 1999. Molecular phylogeny of onygenalean fungi based on small subunit ribosomal DNA (SSU rDNA) sequences. Mycoscience 40:251258.[CrossRef]
Swofford DL. 2002. PAUP*: phylogenetic analysis using parsimony (*and other methods), Version 4.0b10. Sunderland, Massachusetts: Sinauer Associates.
Tsuneda A. 1982. Scanning electron microscopy of Pseudogymnoascus roseus. Mycologia 74:844847.[CrossRef]
, Currah RS. 2004. Ascomatal morphogenesis in Myxotrichum arcticum supports the derivation of the Myxotrichaceae from a discomycetous ancestor. Mycologia 96:627635.
Tzeam SS, Chen JL, Shiu SH. 1992. Talaromyces unicus sp. nov. from Taiwan. Mycologia 84:739749.[CrossRef]
Uchiyama S, Kamiya S, Udagawa S. 1995. Five onygenalean fungi from Japan. Mycoscience 36:211220.[CrossRef]
Udagawa S. 1997. Taxonomic studies on Plectomycetes (cleistothecial ascomycetes). Trans Mycol Soc Jap 38: 143157.
, Uchiyama S. 1999. Taxonomic studies on new or critical fungi of non-pathogenic Onygenales 1. Mycoscience 40:277290.[CrossRef]
, . 2000. Two onygenalean fungi from Russian Far East soil. Mycoscience 41:217221.[CrossRef]
, , Kamiya S. 1993. Gymnostellatospora, a new genus of the Myxotrichaceae. Mycotaxon 48:157164.
, , . 1994. A new species of Myxotrichum with an Oidiodendron anamorph. Mycotaxon 52: 197205.
White TJ, Bruns TD, Lee SB, Taylor JW. 1990. Amplification and direct sequencing of fungal ribosomal RNA genes for phylogenetics. In: Innis MA, Gelfand DH, Sninsky JJ, White TJ, eds. PCR Protocols: a guide to the methods and applications. New York: Academic Press. p 315322.
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |