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Mapes, Royal H., Boardman, Darwin R. (1988) The upper Paleozoic (Pennsylvanian-Permian) ammonoid Emilites. Journal of Paleontology, 62 (1) 69-75 doi:10.1017/s0022336000058893

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Reference TypeJournal (article/letter/editorial)
TitleThe upper Paleozoic (Pennsylvanian-Permian) ammonoid Emilites
JournalJournal of Paleontology
AuthorsMapes, Royal H.Author
Boardman, Darwin R.Author
Year1988 (January)Volume62
Issue1
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0022336000058893Search in ResearchGate
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Mindat Ref. ID414174Long-form Identifiermindat:1:5:414174:1
GUID0
Full ReferenceMapes, Royal H., Boardman, Darwin R. (1988) The upper Paleozoic (Pennsylvanian-Permian) ammonoid Emilites. Journal of Paleontology, 62 (1) 69-75 doi:10.1017/s0022336000058893
Plain TextMapes, Royal H., Boardman, Darwin R. (1988) The upper Paleozoic (Pennsylvanian-Permian) ammonoid Emilites. Journal of Paleontology, 62 (1) 69-75 doi:10.1017/s0022336000058893
In(1988, January) Journal of Paleontology Vol. 62 (1) Cambridge University Press (CUP)
Abstract/NotesFour species of Emilites are now known; these are E. incertus (Böse), E. plummeri Ruzhencev, E. brownwoodi n. sp., and E. bennisoni n. sp. Representatives of this genus may occur as early as Middle Pennsylvanian in North America to as late as Early Permian in the Soviet Union. All described taxa are from North America except E. plummeri, which is from the Soviet Union. Because Emilites is extremely rare in upper Paleozoic ammonoid assemblages, generic and species level phylogenetic relationships are poorly understood. Emilites is not considered to be a good generic-level zone indicator due to its relatively long time range and its rarity.


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