{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,6,21]],"date-time":"2026-06-21T04:59:20Z","timestamp":1782017960051,"version":"3.54.5"},"reference-count":27,"publisher":"Geological Society of America","issue":"4","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":[],"published-print":{"date-parts":[[2017,4,1]]},"abstract":"<jats:title>Abstract<\/jats:title>\n               <jats:p>Ice-marginal glaciated landscapes demarcate former boundaries of the continental ice sheets. Throughout circumpolar regions, permafrost has preserved relict ground ice and glacigenic sediments, delaying the sequence of postglacial landscape change that transformed temperate environments millennia earlier. Here we show that within 7 \u00d7 106 km2 of glaciated permafrost terrain, extensive landscapes remain poised for major climate-driven change. Across northwestern Canada, 60\u2013100-km-wide concentric swaths of thaw slump\u2013affected terrain delineate the maximum and recessional positions of the Laurentide Ice Sheet. These landscapes comprise \u223c17% of continuous permafrost terrain in a 1.27 \u00d7 106 km2 study area, indicating widespread preservation of late Pleistocene ground ice. These thaw slump, relict ground ice, and glacigenic terrain associations are also evident at the circumpolar scale. Recent intensification of thaw slumping across northwestern Canada has mobilized primary glacial sediments, triggering a cascade of fluvial, lacustrine, and coastal effects. These geologically significant processes, highlighted by the spatial distribution of thaw slumps and patterns of fluvial sediment mobilization, signal the climate-driven renewal of deglaciation and postglacial permafrost landscape evolution.<\/jats:p>","DOI":"10.1130\/g38626.1","type":"journal-article","created":{"date-parts":[[2017,2,8]],"date-time":"2017-02-08T01:25:19Z","timestamp":1486517119000},"page":"371-374","source":"Crossref","is-referenced-by-count":201,"title":["Climate-driven thaw of permafrost preserved glacial landscapes, northwestern Canada"],"prefix":"10.1130","volume":"45","author":[{"given":"Steven V.","family":"Kokelj","sequence":"first","affiliation":[{"name":"1Northwest Territories Geological Survey, Government of Northwest Territories (GNWT), Box 1320, Yellowknife, Northwest Territories X1A 2L9, Canada"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Trevor C.","family":"Lantz","sequence":"additional","affiliation":[{"name":"2School of Environmental Studies, University of Victoria, Box 1700, Victoria, British Columbia V8W 2Y2, Canada"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Jon","family":"Tunnicliffe","sequence":"additional","affiliation":[{"name":"3School of Environment, University of Auckland, Bag 92019, Auckland 1142, New Zealand"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Rebecca","family":"Segal","sequence":"additional","affiliation":[{"name":"2School of Environmental Studies, University of Victoria, Box 1700, Victoria, British Columbia V8W 2Y2, Canada"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Denis","family":"Lacelle","sequence":"additional","affiliation":[{"name":"4Department of Geography, Environment and Geomatics, University of Ottawa, 60 University, Ottawa, Ontario K1N 6N5, 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