Abstract
Glomeromycotan spores from the Lower Devonian Rhynie chert provide the first evidence for germination shields in fossil fungi and demonstrate that this complex mode of germination was in place in some fungi at least 400 million years ago. Moreover, they represent the first direct marker relative to the precise systematic position of an Early Devonian endomycorrhizal fungus. In extant fungi, germination shields occur exclusively in the genus Scutellospora (Glomeromycota: Diversisporales, Gigasporaceae). These structures are regarded as a derived feature within the phylum Glomeromycota, and hence their presence in the Rhynie chert suggests that major diversification within this group of fungi occurred before the Early Devonian.
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Acknowledgements
This study was supported in part by funds from the Alexander von Humboldt-Foundation (V-3.FLF-DEU/1064359 to M.K.) and the National Science Foundation (EAR-0542170 to T.N.T. and M.K.). We thank A. Schüßler and C. Walker for providing valuable information that contributed to this study and two anonymous reviewers for their insightful comments and suggestions.
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Scutellosporites Dotzler, M. Krings, T.N. Taylor and Agerer
Scutellosporites devonicus Dotzler, M. Krings, T.N. Taylor and Agerer
Stürmer 1998
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Dotzler, N., Krings, M., Taylor, T.N. et al. Germination shields in Scutellospora (Glomeromycota: Diversisporales, Gigasporaceae) from the 400 million-year-old Rhynie chert. Mycol Progress 5, 178–184 (2006). https://doi.org/10.1007/s11557-006-0511-z
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DOI: https://doi.org/10.1007/s11557-006-0511-z