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Norris, Geoffrey (1977) Palynofloral evidence for terrestrial Middle Jurassic in the Moose River Basin, Ontario. Canadian Journal of Earth Sciences, 14 (2) 153-158 doi:10.1139/e77-018

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Reference TypeJournal (article/letter/editorial)
TitlePalynofloral evidence for terrestrial Middle Jurassic in the Moose River Basin, Ontario
JournalCanadian Journal of Earth Sciences
AuthorsNorris, GeoffreyAuthor
Year1977 (February 1)Volume14
Issue2
PublisherCanadian Science Publishing
DOIdoi:10.1139/e77-018Search in ResearchGate
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Mindat Ref. ID475206Long-form Identifiermindat:1:5:475206:0
GUID0
Full ReferenceNorris, Geoffrey (1977) Palynofloral evidence for terrestrial Middle Jurassic in the Moose River Basin, Ontario. Canadian Journal of Earth Sciences, 14 (2) 153-158 doi:10.1139/e77-018
Plain TextNorris, Geoffrey (1977) Palynofloral evidence for terrestrial Middle Jurassic in the Moose River Basin, Ontario. Canadian Journal of Earth Sciences, 14 (2) 153-158 doi:10.1139/e77-018
In(1977, February) Canadian Journal of Earth Sciences Vol. 14 (2) Canadian Science Publishing
Abstract/Notes Miospore assemblages from a drill hole in the western Moose River Basin comprise 26 species, coniferalean pollen being numerically dominant. Some species are common to putative Middle Jurassic horizons in the western Canadian plains, and comparisons can also be made with the British and French Middle Jurassic. A large hiatus exists between the terrestrial Middle Jurassic sediments and overlying terrestrial Albian (Lower Cretaceous) strata comprising the Mattagami Formation, and may parallel a similar hiatus in southeast Saskatchewan.


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