Several examples of mycoparasitism are described from the Lower Devoni
an (Siegenian) Rhynie chert. These fungal interactions include thick-w
alled chlamydospores and vesicles in which epibiotic fungi are attache
d to the outer surface of the spore. Other fossil spores are character
ized by mycoparasites developing between the layers of the spore wall
or within the lumen. The presence of callosities extending from the in
ner surface of some fossil spores demonstrates that the hosts were ali
ve when parasitized. This response by the mycohost is identical to tha
t found in certain modern mycoparasitic symbioses involving vesicular
arbuscular mycorrhizae that are parasitized by various aquatic fungi.
The presence of mycoparasitism in a 400-million-year-old ecosystem und
erscores the potential significance of the fungal genome early in the
evolution of other organisms.