2 hyphae that typicallylack cross walls, so all the
nuclei are contained within a common cytoplasm (a
coenocytic mycelium);
3 the production of a thick-walled resting spore – the
zygospore– which if formed by a sexual process
involving the fusion of two gametangia;
4 the production of asexual sporesby cytoplasmic
cleavage within a sporangium;
5 a haploid genome.
Ecology and significance
The Zygomycota contains a diverse range of species,
with different types of behaviour, but for convenience
we start with the most familiar examples in the
Order Mucorales. This includes several common
species of the genera Mucor, Rhizopus, Phycomycesand
Thermomucor(a thermophilic fungus that can grow up
to about 60°C). All these fungi grow mainly as sapro-
trophs in soil, on animal dung, on composts in the case
of thermophilic species, or on various other substrates
such as over-ripe fruits. They grow rapidly, often cover-
ing an agar plate in 24 –36 hours, and they are among
the commonest fungi found on soil dilution plates. They
have been termed “sugar fungi”, to denote the fact that
they often depend on simple, soluble carbon nutrients.
However, some fruit-rotting species such as Rhizopus
stoloniferproduce pectic enzymes that can rapidly
liquefy apples and soft fruits (see Fig. 14.6). In addi-
tion, several species of Mortierelladegrade chitin by
producing chitinases (as also do several chytrids).
Chitin is a common and important polymer, because
it is a major component of fungal walls and of the
exoskeletons of insects and other invertebrates.
DIVERSITY OF FUNGI 23
Hypomyces
Neurospora
Ophiostoma
Blumeria
Eremascus
Eurotium
Morchella
Saccharomyces
Coprinus
Russula
Tremella
Tilletia
Gigaspora margarita
Scutellospora
Acaulospora (A)
Entrophospora
Glomus mosseae
Glomus intraradices
Glomus versiforme
Glomus etunicatum
Geosiphon pyriforme
A. gerdemannii
A. trappei
Glomus occultum
Mortierella
Endogone
Diphanoeca
Ichthyophanus
Dermocystis
400
90
290
240
400
460
0.01 substitutions/site
Zygomycota
and
outgroups
Glomeromycota
Basidio-mycota
Ascomycota
d e c f b a
Fig. 2.7A phylogenetic tree based on small subunit ribosomal RNA gene sequences. Triangle a indicates fossil spores
of the Ordovician (460 mya). Triangle b indicates fossil spores of presumed arbuscular mycorrhizal (AM) fungi from the
Rhynie chert (400 mya). Triangle c indicates a fossil clamp connection (Chapter 4) – the earliest evidence of
Basidiomycota (290 mya). Triangle d indicates Ascomycota from the Rhynie chert (400 mya). Triangle e indicates a gilled
mushroom in amber (90 mya). Triangle f indicates AM fungi of the Gigasporatype in the Triassic (about 240 mya). As
reference points, the “outgroups” are Diphanoeca(a choanoflagellate from which fungi are thought to have arisen),
and two early divergent forms of animals, Ichthyophanusand Dermocystis. (Courtesy of Redecker et al. 2000.)
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