The collapse of the Cordilleran-Laurentide ice saddle and early opening of the Mackenzie Valley, Northwest Territories, Canada, constrained by 10Be exposure dating
Deglaciation of the northwestern Laurentide Ice Sheet in the central Mackenzie Valley opened the northern portion of the deglacial Ice-Free Corridor between the Laurentide and Cordilleran ice sheets and a drainage route to the Arctic Ocean. In addition, ice sheet saddle collapse in this section of t...
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The Cryosphere
2022
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Online Access: | http://hdl.handle.net/1828/14691 https://doi.org/10.5194/tc-16-4865-2022 |
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ftuvicpubl:oai:dspace.library.uvic.ca:1828/14691 2023-05-15T15:02:05+02:00 The collapse of the Cordilleran-Laurentide ice saddle and early opening of the Mackenzie Valley, Northwest Territories, Canada, constrained by 10Be exposure dating Stoker, Benjamin J. Margold, Martin Gosse, John C. Hidy, Alan J. Monteath, Alistair J. Young, Joseph M. Gandy, Niall Gregoire, Lauren J. Norris, Sophie L. Froese, Duane 2022 application/pdf http://hdl.handle.net/1828/14691 https://doi.org/10.5194/tc-16-4865-2022 en eng The Cryosphere Stoker, B. J., Margold, M., Gosse, J. C., Hidy, A. J., Monteath, A. J., Young, J. M., . . . Froese, D. (2022). “The collapse of the Cordilleran-Laurentide ice saddle and early opening of the Mackenzie Valley, Northwest Territories, Canada, constrained by 10Be exposure dating.” The Cryosphere, 16, 4865-4886. https://doi.org/10.5195/tc- 16-4865-2022 https://doi.org/10.5194/tc-16-4865-2022 http://hdl.handle.net/1828/14691 Article 2022 ftuvicpubl https://doi.org/10.5194/tc-16-4865-2022 https://doi.org/10.5195/tc 2023-02-01T00:45:30Z Deglaciation of the northwestern Laurentide Ice Sheet in the central Mackenzie Valley opened the northern portion of the deglacial Ice-Free Corridor between the Laurentide and Cordilleran ice sheets and a drainage route to the Arctic Ocean. In addition, ice sheet saddle collapse in this section of the Laurentide Ice Sheet has been implicated as a mechanism for delivering substantial freshwater influx into the Arctic Ocean on centennial timescales. However, there is little empirical data to constrain the deglaciation chronology in the central Mackenzie Valley where the northern slopes of the ice saddle were located. Here, we present 30 new 10Be cosmogenic nuclide exposure dates across six sites, including two elevation transects, which constrain the timing and rate of thinning and retreat of the Laurentide Ice Sheet in the area. Our new 10Be dates indicate that the initial deglaciation of the eastern summits of the central Mackenzie Mountains began at ~ 15:8 ka (17.1–14.6 ka), ~ 1000 years earlier than in previous reconstructions. The main phase of ice saddle collapse occurred between ~ 14:9 and 13.6 ka, consistent with numerical modelling simulations, placing this event within the Bølling–Allerød interval (14.6–12.9 ka). Our new dates require a revision of ice margin retreat dynamics, with ice retreating more easterly rather than southward along the Mackenzie Valley. In addition, we quantify a total sea level rise contribution from the Cordilleran–Laurentide ice saddle region of ~ 11:2m between 16 and 13 ka. This research was supported by the Czech Science Foundation (grant no. 19-21216Y), the Swedish Research Council International Postdoctoral Fellowship (grant no. 637-2014- 483) awarded to Martin Margold, the Charles University Grant Agency project (GAUK project no. 122220) awarded to Benjamin J. Stoker, grants from the NRCan Polar Continental Shelf Program and the Natural Science and Engineering Research Council awarded to Duane Froese, and grants from the University of Alberta Northern Research Awards ... Article in Journal/Newspaper Arctic Arctic Ocean Ice Sheet Mackenzie mountains Mackenzie Valley Northwest Territories The Cryosphere University of Victoria (Canada): UVicDSpace Arctic Arctic Ocean Canada Mackenzie Valley ENVELOPE(-126.070,-126.070,52.666,52.666) Northwest Territories The Cryosphere 16 12 4865 4886 |
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Open Polar |
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University of Victoria (Canada): UVicDSpace |
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ftuvicpubl |
language |
English |
description |
Deglaciation of the northwestern Laurentide Ice Sheet in the central Mackenzie Valley opened the northern portion of the deglacial Ice-Free Corridor between the Laurentide and Cordilleran ice sheets and a drainage route to the Arctic Ocean. In addition, ice sheet saddle collapse in this section of the Laurentide Ice Sheet has been implicated as a mechanism for delivering substantial freshwater influx into the Arctic Ocean on centennial timescales. However, there is little empirical data to constrain the deglaciation chronology in the central Mackenzie Valley where the northern slopes of the ice saddle were located. Here, we present 30 new 10Be cosmogenic nuclide exposure dates across six sites, including two elevation transects, which constrain the timing and rate of thinning and retreat of the Laurentide Ice Sheet in the area. Our new 10Be dates indicate that the initial deglaciation of the eastern summits of the central Mackenzie Mountains began at ~ 15:8 ka (17.1–14.6 ka), ~ 1000 years earlier than in previous reconstructions. The main phase of ice saddle collapse occurred between ~ 14:9 and 13.6 ka, consistent with numerical modelling simulations, placing this event within the Bølling–Allerød interval (14.6–12.9 ka). Our new dates require a revision of ice margin retreat dynamics, with ice retreating more easterly rather than southward along the Mackenzie Valley. In addition, we quantify a total sea level rise contribution from the Cordilleran–Laurentide ice saddle region of ~ 11:2m between 16 and 13 ka. This research was supported by the Czech Science Foundation (grant no. 19-21216Y), the Swedish Research Council International Postdoctoral Fellowship (grant no. 637-2014- 483) awarded to Martin Margold, the Charles University Grant Agency project (GAUK project no. 122220) awarded to Benjamin J. Stoker, grants from the NRCan Polar Continental Shelf Program and the Natural Science and Engineering Research Council awarded to Duane Froese, and grants from the University of Alberta Northern Research Awards ... |
format |
Article in Journal/Newspaper |
author |
Stoker, Benjamin J. Margold, Martin Gosse, John C. Hidy, Alan J. Monteath, Alistair J. Young, Joseph M. Gandy, Niall Gregoire, Lauren J. Norris, Sophie L. Froese, Duane |
spellingShingle |
Stoker, Benjamin J. Margold, Martin Gosse, John C. Hidy, Alan J. Monteath, Alistair J. Young, Joseph M. Gandy, Niall Gregoire, Lauren J. Norris, Sophie L. Froese, Duane The collapse of the Cordilleran-Laurentide ice saddle and early opening of the Mackenzie Valley, Northwest Territories, Canada, constrained by 10Be exposure dating |
author_facet |
Stoker, Benjamin J. Margold, Martin Gosse, John C. Hidy, Alan J. Monteath, Alistair J. Young, Joseph M. Gandy, Niall Gregoire, Lauren J. Norris, Sophie L. Froese, Duane |
author_sort |
Stoker, Benjamin J. |
title |
The collapse of the Cordilleran-Laurentide ice saddle and early opening of the Mackenzie Valley, Northwest Territories, Canada, constrained by 10Be exposure dating |
title_short |
The collapse of the Cordilleran-Laurentide ice saddle and early opening of the Mackenzie Valley, Northwest Territories, Canada, constrained by 10Be exposure dating |
title_full |
The collapse of the Cordilleran-Laurentide ice saddle and early opening of the Mackenzie Valley, Northwest Territories, Canada, constrained by 10Be exposure dating |
title_fullStr |
The collapse of the Cordilleran-Laurentide ice saddle and early opening of the Mackenzie Valley, Northwest Territories, Canada, constrained by 10Be exposure dating |
title_full_unstemmed |
The collapse of the Cordilleran-Laurentide ice saddle and early opening of the Mackenzie Valley, Northwest Territories, Canada, constrained by 10Be exposure dating |
title_sort |
collapse of the cordilleran-laurentide ice saddle and early opening of the mackenzie valley, northwest territories, canada, constrained by 10be exposure dating |
publisher |
The Cryosphere |
publishDate |
2022 |
url |
http://hdl.handle.net/1828/14691 https://doi.org/10.5194/tc-16-4865-2022 |
long_lat |
ENVELOPE(-126.070,-126.070,52.666,52.666) |
geographic |
Arctic Arctic Ocean Canada Mackenzie Valley Northwest Territories |
geographic_facet |
Arctic Arctic Ocean Canada Mackenzie Valley Northwest Territories |
genre |
Arctic Arctic Ocean Ice Sheet Mackenzie mountains Mackenzie Valley Northwest Territories The Cryosphere |
genre_facet |
Arctic Arctic Ocean Ice Sheet Mackenzie mountains Mackenzie Valley Northwest Territories The Cryosphere |
op_relation |
Stoker, B. J., Margold, M., Gosse, J. C., Hidy, A. J., Monteath, A. J., Young, J. M., . . . Froese, D. (2022). “The collapse of the Cordilleran-Laurentide ice saddle and early opening of the Mackenzie Valley, Northwest Territories, Canada, constrained by 10Be exposure dating.” The Cryosphere, 16, 4865-4886. https://doi.org/10.5195/tc- 16-4865-2022 https://doi.org/10.5194/tc-16-4865-2022 http://hdl.handle.net/1828/14691 |
op_doi |
https://doi.org/10.5194/tc-16-4865-2022 https://doi.org/10.5195/tc |
container_title |
The Cryosphere |
container_volume |
16 |
container_issue |
12 |
container_start_page |
4865 |
op_container_end_page |
4886 |
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1766334072233132032 |