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Temporal constraints for the Late Wisconsinan deglaciation of western Canada using eolian dune luminescence chronologies from Alberta

Munyikwa, Kennedy, Rittenour, Tammy M., Feathers, James K.·2017·Palaeogeography, Palaeoclimatology, Palaeoecology

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Crossref · 10.1016/j.palaeo.2016.12.034

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  • Existing ages used to support the 14- to 15-ka time window for Ice-Free Corridor opening are largely based on dating methods with large uncertainties that include some lag between deglaciation and formation of the dated record, making them minimum-limiting ages.

    “existing ages used to support this time window are largely based on dating methods, many with large uncertainties, that include some lag between the time of deglaciation and the formation of the dated record (i.e., minimum-limiting ages) (26, 33).”
  • Luminescence ages on sand dunes in Alberta are even more problematic than the redeposited vole bone fragments for dating Ice-Free Corridor opening.

    “Luminescence ages on sand dunes in Alberta have been central to recent assessments of the age of the IFC (24, 26, 31–33), but these are even more problematic than the redeposited vole bone fragments.”
  • Assuming full bleaching, the oldest luminescence age would place the Ice-Free Corridor as open before 15.3 ± 1.3 ka for optically stimulated luminescence or 15.7 ± 1.6 ka for infrared stimulated luminescence.

    “This would place the IFC as open before 15.3 ± 1.3 ka for the optically stimulated luminescence method (33) or 15.7 ± 1.6 ka for the infrared stimulated luminescence method (40).”

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Authors
Munyikwa, K., Rittenour, T. M., & Feathers, J. K.
Venue
Palaeogeography, Palaeoclimatology, Palaeoecology
Publisher
Elsevier BV
Published
2017-03
Volume
470
Pages
147-165
ISSN
0031-0182
Cited by
34
References
2
Language
en
Funders
  • NSERC (342892)
  • Athabasca University (9902G)

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