Palynofloral evidence for terrestrial Middle Jurassic in the Moose River Basin, Ontario

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 Middl...

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Published in:Canadian Journal of Earth Sciences
Main Author: Norris, Geoffrey
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1977
Subjects:
Online Access:http://dx.doi.org/10.1139/e77-018
http://www.nrcresearchpress.com/doi/pdf/10.1139/e77-018
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spelling crcansciencepubl:10.1139/e77-018 2024-05-19T07:44:04+00:00 Palynofloral evidence for terrestrial Middle Jurassic in the Moose River Basin, Ontario Norris, Geoffrey 1977 http://dx.doi.org/10.1139/e77-018 http://www.nrcresearchpress.com/doi/pdf/10.1139/e77-018 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 14, issue 2, page 153-158 ISSN 0008-4077 1480-3313 journal-article 1977 crcansciencepubl https://doi.org/10.1139/e77-018 2024-04-25T06:52:02Z 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. Article in Journal/Newspaper Moose River Canadian Science Publishing Canadian Journal of Earth Sciences 14 2 153 158
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description 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.
format Article in Journal/Newspaper
author Norris, Geoffrey
spellingShingle Norris, Geoffrey
Palynofloral evidence for terrestrial Middle Jurassic in the Moose River Basin, Ontario
author_facet Norris, Geoffrey
author_sort Norris, Geoffrey
title Palynofloral evidence for terrestrial Middle Jurassic in the Moose River Basin, Ontario
title_short Palynofloral evidence for terrestrial Middle Jurassic in the Moose River Basin, Ontario
title_full Palynofloral evidence for terrestrial Middle Jurassic in the Moose River Basin, Ontario
title_fullStr Palynofloral evidence for terrestrial Middle Jurassic in the Moose River Basin, Ontario
title_full_unstemmed Palynofloral evidence for terrestrial Middle Jurassic in the Moose River Basin, Ontario
title_sort palynofloral evidence for terrestrial middle jurassic in the moose river basin, ontario
publisher Canadian Science Publishing
publishDate 1977
url http://dx.doi.org/10.1139/e77-018
http://www.nrcresearchpress.com/doi/pdf/10.1139/e77-018
genre Moose River
genre_facet Moose River
op_source Canadian Journal of Earth Sciences
volume 14, issue 2, page 153-158
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e77-018
container_title Canadian Journal of Earth Sciences
container_volume 14
container_issue 2
container_start_page 153
op_container_end_page 158
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