Late Cretaceous radiolarians from a bentonite-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications

A radiolarian assemblage containing 11 species of both nasellarians and spumellarians was recovered from the Upper Cretaceous Niobrara Formation in southwestern Saskatchewan, Canada. This assemblage represents the first report of Coniacian radiolarians in the entire Western Interior Basin and one of...

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Published in:Canadian Journal of Earth Sciences
Main Authors: Diaz, Juan F., Velez, Maria I.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2018
Subjects:
Online Access:http://dx.doi.org/10.1139/cjes-2017-0115
http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2017-0115
http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2017-0115
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spelling crcansciencepubl:10.1139/cjes-2017-0115 2023-12-17T10:25:54+01:00 Late Cretaceous radiolarians from a bentonite-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications Diaz, Juan F. Velez, Maria I. 2018 http://dx.doi.org/10.1139/cjes-2017-0115 http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2017-0115 http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2017-0115 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 55, issue 3, page 321-329 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 2018 crcansciencepubl https://doi.org/10.1139/cjes-2017-0115 2023-11-19T13:39:37Z A radiolarian assemblage containing 11 species of both nasellarians and spumellarians was recovered from the Upper Cretaceous Niobrara Formation in southwestern Saskatchewan, Canada. This assemblage represents the first report of Coniacian radiolarians in the entire Western Interior Basin and one of the few reports for the Upper Cretaceous in North America. The presence of radiolarians and the partial disappearance of foraminifera in the only bentonitic interval in this formation suggest that high silica concentrations supplied by volcanic events favored ecological conditions for radiolarians to thrive and or enhanced their preservation before and after deposition. Correlation of this assemblage with other Upper Cretaceous radiolarian assemblages in North America shows a close affinity with the microfauna recovered in the Sverdrup Basin (Canadian Arctic). Article in Journal/Newspaper Arctic Foraminifera* sverdrup basin Canadian Science Publishing (via Crossref) Arctic Canada Canadian Journal of Earth Sciences 55 3 321 329
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic General Earth and Planetary Sciences
spellingShingle General Earth and Planetary Sciences
Diaz, Juan F.
Velez, Maria I.
Late Cretaceous radiolarians from a bentonite-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications
topic_facet General Earth and Planetary Sciences
description A radiolarian assemblage containing 11 species of both nasellarians and spumellarians was recovered from the Upper Cretaceous Niobrara Formation in southwestern Saskatchewan, Canada. This assemblage represents the first report of Coniacian radiolarians in the entire Western Interior Basin and one of the few reports for the Upper Cretaceous in North America. The presence of radiolarians and the partial disappearance of foraminifera in the only bentonitic interval in this formation suggest that high silica concentrations supplied by volcanic events favored ecological conditions for radiolarians to thrive and or enhanced their preservation before and after deposition. Correlation of this assemblage with other Upper Cretaceous radiolarian assemblages in North America shows a close affinity with the microfauna recovered in the Sverdrup Basin (Canadian Arctic).
format Article in Journal/Newspaper
author Diaz, Juan F.
Velez, Maria I.
author_facet Diaz, Juan F.
Velez, Maria I.
author_sort Diaz, Juan F.
title Late Cretaceous radiolarians from a bentonite-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications
title_short Late Cretaceous radiolarians from a bentonite-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications
title_full Late Cretaceous radiolarians from a bentonite-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications
title_fullStr Late Cretaceous radiolarians from a bentonite-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications
title_full_unstemmed Late Cretaceous radiolarians from a bentonite-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications
title_sort late cretaceous radiolarians from a bentonite-rich interval at the base of the niobrara formation, southwestern saskatchewan, canada: biostratigraphic and paleoenvironmental implications
publisher Canadian Science Publishing
publishDate 2018
url http://dx.doi.org/10.1139/cjes-2017-0115
http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2017-0115
http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2017-0115
geographic Arctic
Canada
geographic_facet Arctic
Canada
genre Arctic
Foraminifera*
sverdrup basin
genre_facet Arctic
Foraminifera*
sverdrup basin
op_source Canadian Journal of Earth Sciences
volume 55, issue 3, page 321-329
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/cjes-2017-0115
container_title Canadian Journal of Earth Sciences
container_volume 55
container_issue 3
container_start_page 321
op_container_end_page 329
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