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Pyle, Leanne J., Barnes, Christopher R., Ji, Zailiang (2003) Conodont fauna and biostratigraphy of the Outram, Skoki, and Owen Creek Formations (Lower to Middle Ordovician), Wilcox Pass, Alberta, Canada. Journal of Paleontology, 77 (5) 958-976 doi:10.1017/s0022336000044796

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Reference TypeJournal (article/letter/editorial)
TitleConodont fauna and biostratigraphy of the Outram, Skoki, and Owen Creek Formations (Lower to Middle Ordovician), Wilcox Pass, Alberta, Canada
JournalJournal of Paleontology
AuthorsPyle, Leanne J.Author
Barnes, Christopher R.Author
Ji, ZailiangAuthor
Year2003 (September)Volume77
Issue5
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0022336000044796Search in ResearchGate
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Mindat Ref. ID419939Long-form Identifiermindat:1:5:419939:1
GUID0
Full ReferencePyle, Leanne J., Barnes, Christopher R., Ji, Zailiang (2003) Conodont fauna and biostratigraphy of the Outram, Skoki, and Owen Creek Formations (Lower to Middle Ordovician), Wilcox Pass, Alberta, Canada. Journal of Paleontology, 77 (5) 958-976 doi:10.1017/s0022336000044796
Plain TextPyle, Leanne J., Barnes, Christopher R., Ji, Zailiang (2003) Conodont fauna and biostratigraphy of the Outram, Skoki, and Owen Creek Formations (Lower to Middle Ordovician), Wilcox Pass, Alberta, Canada. Journal of Paleontology, 77 (5) 958-976 doi:10.1017/s0022336000044796
In(2003, September) Journal of Paleontology Vol. 77 (5) Cambridge University Press (CUP)
Abstract/NotesA collection of 60,886 conodonts was recovered from 141 samples of the Outram, Skoki and Owen Creek Formations (Lower to Middle Ordovician) that outcrop through the Wilcox Pass section, Jasper National Park, Alberta, Canada. This section representσ the standard reference section for the Lower-Middle Ordovician of the Southern Canadian Cordillera. The well preserved fauna is assigned to 75 species representing 48 genera. The species are representative of both the Midcontinent and Atlantic faunal realms, but dominantly the former. Nine Midcontinent Realm zones are recognized in the upwards shallowing carbonate platform succession including the Scolopodus subrex, Acodus kechikaensis, Oepikodus communis, Jumudontus gananda, Tripodus laevis, Histiodella altifrons, Histiodella sinuosa, Histiodella holodentata, and Phragmodus “pre-flexuosus” zones. Zones recognized that are characteristic of the Atlantic Realm include Paroistodus proteus, Paracordylodus gracilis, Oepikodus evae, Paroistodus originalis, and Microzarkodina flabellum. A new genus, Filodontus, is proposed for elements assigned previously to the form genus “Scolopodus” filosus. A new species, Leptochirognathus wilcoxi, is described and one new species, left in open nomenclature, is assigned to Rossodus?.


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