Stratigraphy of Pleistocene glaciations in the St Elias Mountains, southwest Yukon, Canada

At least five Middle to Late Pleistocene advances of the northern Cordilleran Ice Sheet are preserved at Silver Creek, on the northeastern edge of the St Elias Mountains in southwest Yukon, Canada. Silver Creek is located 100 km up‐ice of the Marine Isotope Stage ( MIS ) 2 McConnell glacial limit of...

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Bibliographic Details
Published in:Boreas
Main Authors: Turner, Derek G., Ward, Brent C., Froese, Duane G., Lamothe, Michel, Bond, Jeffrey D., Bigelow, Nancy H.
Other Authors: National Sciences and Engineering Research Council of Canada, Yukon Geological Survey, Canadian Polar Commission's Northern Scientific Training Program
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2016
Subjects:
Canada
Silver Creek
Yukon
Ice Sheet
Tundra
Online Access:http://dx.doi.org/10.1111/bor.12172
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12172
https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12172
Description
Summary:At least five Middle to Late Pleistocene advances of the northern Cordilleran Ice Sheet are preserved at Silver Creek, on the northeastern edge of the St Elias Mountains in southwest Yukon, Canada. Silver Creek is located 100 km up‐ice of the Marine Isotope Stage ( MIS ) 2 McConnell glacial limit of the St Elias lobe. This site contains ~3 km of nearly continuous lateral exposure of glacial and non‐glacial sediments, including multiple tills separated by thick gravel, loess and tilted lake beds. Infrared‐stimulated luminescence ( IRSL ) and AMS radiocarbon dating constrain the glacial deposits to MIS 2, 4, either MIS 6 or mid‐ MIS 7, and two older Middle Pleistocene advances. This chronology and the tilt of the lake beds suggest Pleistocene uplift rates of up to 1.9 mm a −1 along the Denali Fault since MIS 7. The non‐glacial sediment consists of sand, gravel, loess and organic beds from MIS 7, MIS 3 and the early Holocene. The MIS 3 deposits date to between 30–36 14 C ka BP , making Silver Creek one of the few well‐constrained MIS 3‐aged sites in Yukon. This confirms that ice receded close to modern limits in MIS 3. Pollen and macrofossil analyses show that a meadow‐tundra to steppe‐tundra mosaic with abundant herbs and forbs and few shrubs or trees, dominated the environment at this time. The stratigraphy at Silver Creek provides a palaeoclimatic record since at least MIS 8 and comprises the oldest direct record of Pleistocene glaciation in southwest Yukon.

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