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McCracken, Alexander D., Nowlan, Godfrey S. (1989) Conodont paleontology and biostratigraphy of Ordovician carbonates and petroliferous carbonates on Southampton, Baffin, and Akpatok islands in the eastern Canadian Arctic. Canadian Journal of Earth Sciences, 26 (10) 1880-1903 doi:10.1139/e89-160

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Reference TypeJournal (article/letter/editorial)
TitleConodont paleontology and biostratigraphy of Ordovician carbonates and petroliferous carbonates on Southampton, Baffin, and Akpatok islands in the eastern Canadian Arctic
JournalCanadian Journal of Earth Sciences
AuthorsMcCracken, Alexander D.Author
Nowlan, Godfrey S.Author
Year1989 (October 1)Volume26
Issue10
PublisherCanadian Science Publishing
DOIdoi:10.1139/e89-160Search in ResearchGate
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Mindat Ref. ID480188Long-form Identifiermindat:1:5:480188:1
GUID0
Full ReferenceMcCracken, Alexander D., Nowlan, Godfrey S. (1989) Conodont paleontology and biostratigraphy of Ordovician carbonates and petroliferous carbonates on Southampton, Baffin, and Akpatok islands in the eastern Canadian Arctic. Canadian Journal of Earth Sciences, 26 (10) 1880-1903 doi:10.1139/e89-160
Plain TextMcCracken, Alexander D., Nowlan, Godfrey S. (1989) Conodont paleontology and biostratigraphy of Ordovician carbonates and petroliferous carbonates on Southampton, Baffin, and Akpatok islands in the eastern Canadian Arctic. Canadian Journal of Earth Sciences, 26 (10) 1880-1903 doi:10.1139/e89-160
In(1989, October) Canadian Journal of Earth Sciences Vol. 26 (10) Canadian Science Publishing
Abstract/Notes Carbonate and petroliferous carbonate units ("oil shales") on Southampton, Baffin, and Akpatok islands have yielded a total of 2277 conodonts, the more biostratigraphically useful of which indicate not all units are correlative. The Boas River "shale", the lower of the two petroliferous units on Southampton Island, overlies the Bad Cache Rapids Group and contains a diverse fauna, including elements of Amorphognathus ordovicicus Branson and Mehl. Previous reports have indicated the presence of Culumbodina penna Sweet, a species whose range only barely overlaps that of A. ordovicicus in the middle Maysvillian. Carbonate beds and bedding-plane surfaces of the higher Red Head Rapids Formation at Sixteen Mile Brook yielded A. ordovicicus faunas containing Aphelognathus cf. A. divergens Sweet. These beds are likely Richmondian, since A. divergens is known elsewhere only from Richmondian strata. A metasicula of "Glyptograptus" hudsoni Jackson, several natural conodont assemblages, and fused enigmatic coniform elements were also found at Sixteen Mile Brook.The petroliferous unit in unnamed strata at Amadjuak Lake on Baffin Island contains Belodina area Sweet, which is indicative of a late Edenian to early Maysvillian age. Conodonts from the petroliferous strata at Jordan River on Baffin Island suggest a Trentonian to early Maysvillian age. The conodonts recovered from unnamed strata on Akpatok Island are not very diagnostic but indicate an age range from Shermanian to Gamachian.


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