Evidence for Early Pleistocene glaciation from borecore stratigraphy in north-central Alberta, Canada
Pleistocene sediments collected in north-central Alberta, Canada, were subsampled and studied for paleomagnetic remanence characteristics. A magnetostratigraphy has been established for sediments previously assumed to represent multiple continental (Laurentide) glaciations but for which no geochrono...
Published in: | Canadian Journal of Earth Sciences |
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Online Access: | http://dx.doi.org/10.1139/cjes-2016-0175 http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2016-0175 http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2016-0175 |
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crcansciencepubl:10.1139/cjes-2016-0175 2024-09-15T18:12:30+00:00 Evidence for Early Pleistocene glaciation from borecore stratigraphy in north-central Alberta, Canada Andriashek, Laurence D. Barendregt, René W. 2017 http://dx.doi.org/10.1139/cjes-2016-0175 http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2016-0175 http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2016-0175 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 54, issue 4, page 445-460 ISSN 0008-4077 1480-3313 journal-article 2017 crcansciencepubl https://doi.org/10.1139/cjes-2016-0175 2024-07-25T04:10:08Z Pleistocene sediments collected in north-central Alberta, Canada, were subsampled and studied for paleomagnetic remanence characteristics. A magnetostratigraphy has been established for sediments previously assumed to represent multiple continental (Laurentide) glaciations but for which no geochronology was available. Based on the Quaternary record elsewhere in Alberta and Saskatchewan, it was thought that some of these sediments were deposited during pre-late Wisconsinan glaciations. The Quaternary sedimentary successions of north-central Alberta have a thickness up to 300 m within buried valleys and are composed of diamicts interbedded with glaciolacustrine and outwash sediments. Most of the sampled units are not accessible from outcrop, and their sedimentology and stratigraphy is derived from core data only. In 4 of 16 borecores sampled to date, diamict that correlates with the Bronson Lake Formation till is reversely magnetized, indicating an Early Pleistocene age. This formation is underlain by either Empress Formation sediments or Colorado Group shale, and is overlain by one or more normally magnetized glacigenic sedimentary units of the Bonnyville, Marie Creek, and Grand Centre formations, respectively. This new record of Early Pleistocene glaciation in north-central Alberta places the westernmost extent of earliest Laurentide ice at least 300 km farther west than its previously established limit in the Saskatoon and Regina regions of the Canadian Interior Plains, but still to the east of the maximum extent of the Late Wisconsinan (Late Pleistocene) Laurentide Ice Sheet, which extended into the foothills of the Alberta and Montana Rocky Mountains. Article in Journal/Newspaper Ice Sheet Canadian Science Publishing Canadian Journal of Earth Sciences 54 4 445 460 |
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Open Polar |
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Canadian Science Publishing |
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crcansciencepubl |
language |
English |
description |
Pleistocene sediments collected in north-central Alberta, Canada, were subsampled and studied for paleomagnetic remanence characteristics. A magnetostratigraphy has been established for sediments previously assumed to represent multiple continental (Laurentide) glaciations but for which no geochronology was available. Based on the Quaternary record elsewhere in Alberta and Saskatchewan, it was thought that some of these sediments were deposited during pre-late Wisconsinan glaciations. The Quaternary sedimentary successions of north-central Alberta have a thickness up to 300 m within buried valleys and are composed of diamicts interbedded with glaciolacustrine and outwash sediments. Most of the sampled units are not accessible from outcrop, and their sedimentology and stratigraphy is derived from core data only. In 4 of 16 borecores sampled to date, diamict that correlates with the Bronson Lake Formation till is reversely magnetized, indicating an Early Pleistocene age. This formation is underlain by either Empress Formation sediments or Colorado Group shale, and is overlain by one or more normally magnetized glacigenic sedimentary units of the Bonnyville, Marie Creek, and Grand Centre formations, respectively. This new record of Early Pleistocene glaciation in north-central Alberta places the westernmost extent of earliest Laurentide ice at least 300 km farther west than its previously established limit in the Saskatoon and Regina regions of the Canadian Interior Plains, but still to the east of the maximum extent of the Late Wisconsinan (Late Pleistocene) Laurentide Ice Sheet, which extended into the foothills of the Alberta and Montana Rocky Mountains. |
format |
Article in Journal/Newspaper |
author |
Andriashek, Laurence D. Barendregt, René W. |
spellingShingle |
Andriashek, Laurence D. Barendregt, René W. Evidence for Early Pleistocene glaciation from borecore stratigraphy in north-central Alberta, Canada |
author_facet |
Andriashek, Laurence D. Barendregt, René W. |
author_sort |
Andriashek, Laurence D. |
title |
Evidence for Early Pleistocene glaciation from borecore stratigraphy in north-central Alberta, Canada |
title_short |
Evidence for Early Pleistocene glaciation from borecore stratigraphy in north-central Alberta, Canada |
title_full |
Evidence for Early Pleistocene glaciation from borecore stratigraphy in north-central Alberta, Canada |
title_fullStr |
Evidence for Early Pleistocene glaciation from borecore stratigraphy in north-central Alberta, Canada |
title_full_unstemmed |
Evidence for Early Pleistocene glaciation from borecore stratigraphy in north-central Alberta, Canada |
title_sort |
evidence for early pleistocene glaciation from borecore stratigraphy in north-central alberta, canada |
publisher |
Canadian Science Publishing |
publishDate |
2017 |
url |
http://dx.doi.org/10.1139/cjes-2016-0175 http://www.nrcresearchpress.com/doi/full-xml/10.1139/cjes-2016-0175 http://www.nrcresearchpress.com/doi/pdf/10.1139/cjes-2016-0175 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Canadian Journal of Earth Sciences volume 54, issue 4, page 445-460 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/cjes-2016-0175 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
54 |
container_issue |
4 |
container_start_page |
445 |
op_container_end_page |
460 |
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1810450087065681920 |