Late Cretaceous radiolarians from a bentonitic-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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NRC Research Press (a division of Canadian Science Publishing)
2017
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Online Access: | http://hdl.handle.net/1807/82553 http://www.nrcresearchpress.com/doi/abs/10.1139/cjes-2017-0115 |
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ftunivtoronto:oai:localhost:1807/82553 2023-05-15T15:06:01+02:00 Late Cretaceous radiolarians from a bentonitic-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications Diaz, Juan F. Velez, Maria I. 2017-11-03 http://hdl.handle.net/1807/82553 http://www.nrcresearchpress.com/doi/abs/10.1139/cjes-2017-0115 unknown NRC Research Press (a division of Canadian Science Publishing) 0008-4077 http://hdl.handle.net/1807/82553 http://www.nrcresearchpress.com/doi/abs/10.1139/cjes-2017-0115 Article 2017 ftunivtoronto 2020-06-17T12:10:47Z 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). The accepted manuscript in pdf format is listed with the files at the bottom of this page. The presentation of the authors' names and (or) special characters in the title of the manuscript may differ slightly between what is listed on this page and what is listed in the pdf file of the accepted manuscript; that in the pdf file of the accepted manuscript is what was submitted by the author. Article in Journal/Newspaper Arctic Foraminifera* sverdrup basin University of Toronto: Research Repository T-Space Arctic Canada |
institution |
Open Polar |
collection |
University of Toronto: Research Repository T-Space |
op_collection_id |
ftunivtoronto |
language |
unknown |
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). The accepted manuscript in pdf format is listed with the files at the bottom of this page. The presentation of the authors' names and (or) special characters in the title of the manuscript may differ slightly between what is listed on this page and what is listed in the pdf file of the accepted manuscript; that in the pdf file of the accepted manuscript is what was submitted by the author. |
format |
Article in Journal/Newspaper |
author |
Diaz, Juan F. Velez, Maria I. |
spellingShingle |
Diaz, Juan F. Velez, Maria I. Late Cretaceous radiolarians from a bentonitic-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications |
author_facet |
Diaz, Juan F. Velez, Maria I. |
author_sort |
Diaz, Juan F. |
title |
Late Cretaceous radiolarians from a bentonitic-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications |
title_short |
Late Cretaceous radiolarians from a bentonitic-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications |
title_full |
Late Cretaceous radiolarians from a bentonitic-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications |
title_fullStr |
Late Cretaceous radiolarians from a bentonitic-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications |
title_full_unstemmed |
Late Cretaceous radiolarians from a bentonitic-rich interval at the base of the Niobrara Formation, southwestern Saskatchewan, Canada: biostratigraphic and paleoenvironmental implications |
title_sort |
late cretaceous radiolarians from a bentonitic-rich interval at the base of the niobrara formation, southwestern saskatchewan, canada: biostratigraphic and paleoenvironmental implications |
publisher |
NRC Research Press (a division of Canadian Science Publishing) |
publishDate |
2017 |
url |
http://hdl.handle.net/1807/82553 http://www.nrcresearchpress.com/doi/abs/10.1139/cjes-2017-0115 |
geographic |
Arctic Canada |
geographic_facet |
Arctic Canada |
genre |
Arctic Foraminifera* sverdrup basin |
genre_facet |
Arctic Foraminifera* sverdrup basin |
op_relation |
0008-4077 http://hdl.handle.net/1807/82553 http://www.nrcresearchpress.com/doi/abs/10.1139/cjes-2017-0115 |
_version_ |
1766337684620443648 |