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Late Quaternary marine records from High Arctic Canada: problems, solutions, and multiproxy perspectives

dc.contributor.authorPieńkowski, Anna J.
dc.contributor.authorFurze, Mark F.A.
dc.contributor.authorEngland, John H.
dc.contributor.authorMacLean, Brian
dc.contributor.authorVon Prause, Markus
dc.contributor.authorBlasco, Steve
dc.date.accessioned2014-10-10
dc.date.accessioned2022-05-27T01:13:17Z
dc.date.available2022-05-27T01:13:17Z
dc.date.issued2013
dc.descriptionPresented on April 8, 2013 at the European Geosciences Union General Assembly in Vienna, Austria.
dc.description.abstractThe Canadian Arctic Archipelago (= CAA) constitutes a significant geographic region within the Arctic Ocean Basin, influencing its oceanography, biology, ecology, and climate. Yet comparatively little is known about the long-term (post-Late Wisconsinan) environmental history of the marine channels of this region (the “Northwest Passage” = NWP). New marine data emerging from the central CAA extending back to regional deglaciation highlight the potential of multiproxy approaches in high-latitude settings.
dc.format.extent45.62 kb
dc.format.mimetypePDF
dc.identifier.urihttps://hdl.handle.net/20.500.14078/171
dc.languageEnglish
dc.language.isoen
dc.rightsAttribution (CC BY)
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subjectglaciation
dc.subjectCanadian Arctic Archipelago
dc.titleLate Quaternary marine records from High Arctic Canada: problems, solutions, and multiproxy perspectivesen
dc.typePresentation
dspace.entity.type

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