A new genus, Planticonsortium (Mucoromycotina), and new combination (P. tenue), for the fine root endophyte, Glomus tenue (basionym Rhizophagus tenuis).

In 1977, the fine root endophyte, originally named Rhizophagus tenuis, was transferred into the genus Glomus as G. tenue, thus positioning the species with all other known arbuscular mycorrhizal fungi (Glomeromycota, Glomeromycotina). Recent molecular evidence, however, places it in a different subphylum, Mucoromycotina in the Mucoromycota. No suitable genus exists in the Mucoromycotina to accommodate G. tenue, so it is moved to Planticonsortium gen. nov. as P. tenue comb. nov.

Fine root endophytes under scrutiny: a review of the literature on arbuscule-producing fungi recently suggested to belong to the Mucoromycotina.

Fine root endophytes (FRE) are arbuscule-forming fungi presently considered as a single species-Glomus tenue in the Glomeromycota (Glomeromycotina)-but probably belong within the Mucoromycotina. Thus, FRE are the only known arbuscule-forming fungi not within the arbuscular mycorrhizal fungi (AMF; Glomeromycotina) as currently understood. Phylogenetic differences between FRE and AMF could reflect ecological differences. To synthesize current ecological knowledge, we reviewed the literature on FRE and identified 108 papers that noted the presence of FRE and, in some, the colonization levels for FRE or AMF (or both). We categorized these records by geographic region, host-plant family and environment (agriculture, moderate-natural, low-temperature, high-altitude and other) and determined their influence on the percentage of root length colonized by FRE in a meta-analysis. We found that FRE are globally distributed, with many observations from Poaceae, perhaps due to grasses being widely distributed. In agricultural environments, colonization by FRE often equalled or exceeded that of AMF, particularly in Australasia. In moderate-natural and high-altitude environments, average colonization by FRE (~10%) was lower than that of AMF (~35%), whereas in low-temperature environments, colonization was similar (~20%). Several studies suggested that FRE can enhance host-plant phosphorus uptake and growth, and may be more resilient than AMF to environmental stress in some host plants. Further research is required on the functioning of FRE in relation to the environment, host plant and co-occurring AMF and, in particular, to examine whether FRE are important for plant growth in stressful environments. Targeted molecular primers are urgently needed for further research on FRE.

Early cell evolution, eukaryotes, anoxia, sulfide, oxygen, fungi first (?), and a tree of genomes revisited.

Genomes contain evidence for the history of life and furthermore contain evidence for lateral gene transfer, which was an important part of that history. The geological record also contains evidence for the history of life, and newer findings indicates that the Earth's oceans were largely anoxic and highly sulfidic up until about 0.6 billion years ago. Eukaryotes, which fossil data indicate to have been in existence for at least 1.5 billion years, must have therefore spent much of their evolutionary history in oxygen-poor and sulfide-rich environments. Many eukaryotes still inhabit such environments today. Among eukaryotes, organelles also contain evidence for the history of life and have preserved abundant traces of their anaerobic past in the form of energy metabolic pathways. New views of eukaryote phylogeny suggest that fungi may be among the earliest-branching eukaryotes. From the standpoint of the fungal feeding habit (osmotrophy rather than phagotrophy) and from the standpoint of the diversity in their ATP-producing pathways, a eukaryotic tree with fungi first would make sense. Because of lateral gene transfer and endosymbiosis, branches in the tree of genomes intermingle and occasionally fuse, but the overall contours of cell history nonetheless seem sketchable and roughly correlateable with geological time.

First report of Basidiolum fimbriatum since 1861, with comments on its development, occurrence, distribution and relationship with other fungi.

An obscure parasitic fungus, Basidiolum fimbriatum, was found on Amoebidium parasiticum (Amoebidiales) associated with Caenis sp. (mayfly) nymphs, during a survey of gut fungi (Trichomycetes) from a small stream in northeastern Kansas, USA. The hindguts of the nymphs harboured a species of Legeriomycetaceae and Paramoebidium sp. This is the first report of the ectocommensal protozoan, A. parasiticum, associated with the gills of Caenidae (Ephemeroptera), and of B. fimbriatum in the 142 years since its original documentation from Wiesbaden, Germany. B. fimbriatum is recorded from two midwestern USA states (Kansas and Iowa) and the morphological and developmental features of the parasite on its host are compared with Cienkowski's original observations and interpretation. B. fimbriatum is characterized as a parasitic fungus possessing merosporangia that from on a simple pyriform thallus that penetrates and consumes its host via a haustorial network. The hypothesis that B. fimbriatum is most closely related to members of the order Zoopagales sensu Benjamin (1979) is proposed. The importance of future collections and molecular-based phylogenetic approaches to place this parasitic fungus within a current system of classification are highlighted.

Sooty moulds from European tertiary amber, with notes on the systematic position of Rosaria ('Cyanobacteria').

Sooty moulds are described and illustrated from European amber dating back to 22-54 Myr. All the fossils are fragments of superficial subicula composed of brown moniliform hyphae with markedly tapering distal ends. The subglobose cells are identical to those of extant Metacapnodium (Metacapnodiaceae, Capnodiales) species. Also other preserved features, like the type of apical growth, wide-angled branching and the production of two distinctive conidial states, supports a placement in this genus. The fossils demonstrate that Metacapnodium hyphae have remained unchanged for tens of millions of years. This confirms that hyphal morphology and conidial states should be accorded considerable classificatory significance in this group of fungi. The following nomenclatural change is made: Metacapnodium succinum comb. nov. (syn. Rosaria succina). The type specimen was initially described as a filamentous cyanobacterium, due to similarities with Rosaria ramosa. Also the systematic position of this attribute is shortly discussed.

Hyaloraphidium curvatum is not a green alga, but a lower fungus; Amoebidium parasiticum is not a fungus, but a member of the DRIPs.

The unicellular heterotrophic protist Hyaloraphidium is classified with a family of green algae, the Ankistrodesmaceae. The only species that exists in pure culture and that is available for taxonomic studies is H. curvatum. Comparative 18S ribosomal RNA sequence analyses showed that H. curvatum belongs to the fungi rather than to the algae. Within the fungi, H. curvatum preferentially clustered with Chytridiomycetes. Unlike Chytridiomycetes, H. curvatum propagates by autosporulation, and the presence of flagella has never been reported. Transmission electron microscopy indicated that H. curvatum in some respects resembles Chytridiomycetes, but no elements of a flagellar apparatus were detected. The habitus of H. curvatum is unlike that of other fungi except the trichomycete Amoebidium parasiticum. The cell wall sugar composition of H. curvatum was unique, but to some extent resembled that of A. parasiticum. However, H. curvatum and A. parasiticum are not closely related to each other according to 18S rRNA sequence data. Moreover, A. parasiticum clustered with protistan animals, the Mesomycetozoa (DRIPs). Combined molecular, ultrastructural and chemical data do not allow assignment of H. curvatum to any recognized clade of fungi. This suggests that H. curvatum may represent an independent evolutionary lineage within the fungi.