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Ludvigsen, R., Chatterton, B. D. E. (1980) The ontogeny of Failleana and the origin of the Bumastinae (Trilobita) Geological Magazine, 117 (5) 471-478 doi:10.1017/s0016756800028582

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Reference TypeJournal (article/letter/editorial)
TitleThe ontogeny of Failleana and the origin of the Bumastinae (Trilobita)
JournalGeological Magazine
AuthorsLudvigsen, R.Author
Chatterton, B. D. E.Author
Year1980 (September)Volume117
Issue5
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800028582Search in ResearchGate
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Mindat Ref. ID251792Long-form Identifiermindat:1:5:251792:0
GUID0
Full ReferenceLudvigsen, R., Chatterton, B. D. E. (1980) The ontogeny of Failleana and the origin of the Bumastinae (Trilobita) Geological Magazine, 117 (5) 471-478 doi:10.1017/s0016756800028582
Plain TextLudvigsen, R., Chatterton, B. D. E. (1980) The ontogeny of Failleana and the origin of the Bumastinae (Trilobita) Geological Magazine, 117 (5) 471-478 doi:10.1017/s0016756800028582
In(1980, September) Geological Magazine Vol. 117 (5) Cambridge University Press (CUP)
Abstract/NotesSummaryThe metaprotaspid of the bumastine Failleana calva is similar to protaspids of scutelluids, whilst late meraspids and early holaspids of F. calva are similar to fully mature styginids. This suggests that the bumastines were derived from the styginids in the Early Ordovician and that the bumastines later gave rise to the scutelluids. Bumastus and similar Silurian trilobites are phyletic derivatives of Ordovician bumastines and not effaced scutelluids as claimed recently by Lane & Thomas. Revised diagnoses of Illaeninae and Bumastinae are presented.


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