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Mamet, Bernard L., Nelson, Samuel J. (1984) Stratigraphic position of Carboniferous Macgowanella and Sinopora? pascuali, Canadian Cordillera. Canadian Journal of Earth Sciences, 21 (4) 500-501 doi:10.1139/e84-053

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Reference TypeJournal (article/letter/editorial)
TitleStratigraphic position of Carboniferous Macgowanella and Sinopora? pascuali, Canadian Cordillera
JournalCanadian Journal of Earth Sciences
AuthorsMamet, Bernard L.Author
Nelson, Samuel J.Author
Year1984 (April 1)Volume21
Issue4
PublisherCanadian Science Publishing
DOIdoi:10.1139/e84-053Search in ResearchGate
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Mindat Ref. ID478248Long-form Identifiermindat:1:5:478248:7
GUID0
Full ReferenceMamet, Bernard L., Nelson, Samuel J. (1984) Stratigraphic position of Carboniferous Macgowanella and Sinopora? pascuali, Canadian Cordillera. Canadian Journal of Earth Sciences, 21 (4) 500-501 doi:10.1139/e84-053
Plain TextMamet, Bernard L., Nelson, Samuel J. (1984) Stratigraphic position of Carboniferous Macgowanella and Sinopora? pascuali, Canadian Cordillera. Canadian Journal of Earth Sciences, 21 (4) 500-501 doi:10.1139/e84-053
In(1984, April) Canadian Journal of Earth Sciences Vol. 21 (4) Canadian Science Publishing
Abstract/Notes Microfossils associated with Carboniferous Macgowanella and Sinopora? pascuali allow more precise age determinations than previously determined. Macgowanella, a possible bryozoan holdfast, is represented by two species, M. tenuiradiata (Warren) and M. stellata (Warren), both from the Viséan (Upper Mississippian, Meramecian) Mount Head Formation of the southern Canadian Rocky Mountains. Microfossils indicate a correlation with upper Viséan Zone 14, equivalent to the lower upper Meramecian Marston/lower Opal members of the Mount Head Formation.The syringoporid coral Sinopora? pascuali is from near Kamloops, British Columbia. Microfossils support the Early Pennsylvanian date earlier assigned, correlating it with Zones 20 or 21, Bashkirian = Morrowan to basal Atokan.


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