TRIASSIC FUNGUS FROM ANTARCTICA WITH POSSIBLE ASCOMYCETOUS AFFINITIES
Hyphae, sporocarps, and structures which appear to represent arthroconidia are described from silicified peat deposits of Triassic age from Antarctica. Sporocarps with a single ostiole possess a multilayered wall with internally produced aseptate appendages that ornament the sporocarp surface. The p...
Published in: | American Journal of Botany |
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Main Authors: | , |
Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
1988
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Subjects: | |
Online Access: | http://dx.doi.org/10.1002/j.1537-2197.1988.tb11223.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fj.1537-2197.1988.tb11223.x https://onlinelibrary.wiley.com/doi/pdf/10.1002/j.1537-2197.1988.tb11223.x http://api.wiley.com/onlinelibrary/chorus/v1/articles/10.1002%2Fj.1537-2197.1988.tb11223.x |
Summary: | Hyphae, sporocarps, and structures which appear to represent arthroconidia are described from silicified peat deposits of Triassic age from Antarctica. Sporocarps with a single ostiole possess a multilayered wall with internally produced aseptate appendages that ornament the sporocarp surface. The primitive features exhibited by this fungus, together with previously described sporocarps, provide evidence for the existence of a group of fungi that may be ancestral to modern Ascomycotina. |
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