Authors
April S Dalton, Martin Margold, Chris R Stokes, Lev Tarasov, Arthur S Dyke, Roberta S Adams, Serge Allard, Heather E Arends, Nigel Atkinson, John W Attig, Peter J Barnett, Robert L Barnett, Martin Batterson, Pascal Bernatchez, Harold W Borns Jr, Andy Breckenridge, Jason P Briner, Etienne Brouard, Janet E Campbell, Anders E Carlson, John J Clague, B Brandon Curry, Robert-André Daigneault, Hugo Dubé-Loubert, Don J Easterbrook, David A Franzi, Hannah G Friedrich, Svend Funder, Michelle S Gauthier, Angela S Gowan, Ken L Harris, Bernard Hétu, Tom S Hooyer, Carrie E Jennings, Mark D Johnson, Alan E Kehew, Samuel E Kelley, Daniel Kerr, Edward L King, Kristian K Kjeldsen, Alan R Knaeble, Patrick Lajeunesse, Thomas R Lakeman, Michel Lamothe, Phillip Larson, Martin Lavoie, Henry M Loope, Thomas V Lowell, Barbara A Lusardi, Lorraine Manz, Isabelle McMartin, F Chantel Nixon, Serge Occhietti, Michael A Parkhill, David JW Piper, Antonius G Pronk, Pierre JH Richard, John C Ridge, Martin Ross, Martin Roy, Allen Seaman, John Shaw, Rudolph R Stea, James T Teller, Woodrow B Thompson, L Harvey Thorleifson, Daniel J Utting, Jean J Veillette, Brent C Ward, Thomas K Weddle, Herbert E Wright Jr
Publication date
2020/4/15
Source
Quaternary Science Reviews
Volume
234
Pages
106223
Publisher
Pergamon
Description
The North American Ice Sheet Complex (NAISC; consisting of the Laurentide, Cordilleran and Innuitian ice sheets) was the largest ice mass to repeatedly grow and decay in the Northern Hemisphere during the Quaternary. Understanding its pattern of retreat following the Last Glacial Maximum is critical for studying many facets of the Late Quaternary, including ice sheet behaviour, the evolution of Holocene landscapes, sea level, atmospheric circulation, and the peopling of the Americas. Currently, the most up-to-date and authoritative margin chronology for the entire ice sheet complex is featured in two publications (Geological Survey of Canada Open File 1574 [Dyke et al., 2003]; ‘Quaternary Glaciations – Extent and Chronology, Part II’ [Dyke, 2004]). These often-cited datasets track ice margin recession in 36 time slices spanning 18 ka to 1 ka (all ages in uncalibrated radiocarbon years) using a combination of …
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