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400 / Paleozoic
Paleopyrenomycites
Paleopyrenomycites devonicus
Tiny flask-shaped fruiting bodies inside plant tissue are among the oldest ascomycete evidence.
- Time range
- About 407 million years ago
- Final stage
- Early Devonian
- Geographic range
- Hot-spring wetland plant tissue · Scotland
01 / DEFINITION & ECOLOGY
What was Paleopyrenomycites?
Paleopyrenomycites (Paleopyrenomycites devonicus) was an extinct organism known from About 407 million years ago, with a range in Hot-spring wetland plant tissue · Scotland.
Life and ecology
Hyphae entered early land plants and formed perithecia containing spores.
02 / DISAPPEARANCE
Why did Paleopyrenomycites disappear?
Loss of the host and Rhynie ecosystem ended the form species.
03 / EVIDENCE
How do scientists know about Paleopyrenomycites?
Cellular chert preserves hyphae, cavities and spores; parasitic versus saprotrophic ecology remains uncertain.
04 / SOURCES & FURTHER READING
Check the source record
Use the scientific name to compare taxonomy, occurrence records and the fossil record. Database coverage and classifications may differ.
05 / REVISION HISTORY
How has this record changed?
- Verified authoritative entity sources and added three responsive reconstruction sizes.
- Initial bilingual species record published.
06 / CORRECTIONS & ADDITIONS