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TitleFaunal and archaeological remains as evidence of climate change in freezing caverns, Yukon Territory, Canada
AuthorLauriol, B; Prévost, C; Deschamps, É; Cinq-Mars, J; Labrecque, S
SourceArctic vol. 54, no. 2, 2001 p. 135-141, https://doi.org/10.14430/arctic772 (Open Access)
Year2001
Alt SeriesGeological Survey of Canada, Contribution Series 2000064
PublisherThe Arctic Institute of North America
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
ProvinceYukon
NTS117A; 117B; 117C; 117D
Lat/Long WENS-144.0000 -136.0000 70.0000 68.0000
Subjectsenvironmental geology; paleontology; surficial geology/geomorphology; Nature and Environment; karst topography; glaciers; biota; vegetation; faunas; paleoecology; climate effects; climate, arctic; climate; radiocarbon dating; Wisconsinian glacial stage; limestones; Holocene; ice; caves; Ogilvie Mountains; climate change; animals
Illustrationslocation maps; photographs; geological sketch maps; graphs; tables
ProgramNSERC Natural Sciences and Engineering Research Council of Canada
ProgramUniversity of Ottawa, Northern Research Funds
Released2001 01 01
AbstractAnimal and plant remains, some associated with prehistoric artefacts, were collected in freezing caverns (glacières) of northern Yukon Territory. Radiocarbon dates show that the oldest remains are Middle Wisconsinan (ca. 38 000 BP). The absence of material of Late Wisconsinan age likely indicates that the caves were infilled by ice during this cold period. Climate warming and ice melting during the Holocene allowed animals and prehistoric hunters to regularly visit these caves. Ice plugs were evidently smaller during the early Holocene than they are now.
GEOSCAN ID211499