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Foraminifera: a tool for elucidating past and recent climate change in marine Arctic Canada

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dc.contributor.authorThiessen, Rabecca
dc.contributor.authorPieńkowski, Anna J.
dc.contributor.authorFurze, Mark F.A.
dc.contributor.authorCage, Alix
dc.contributor.authorCaouette, Alexandre
dc.contributor.authorCoates, Sina
dc.date.accessioned2017-11-30
dc.date.accessioned2022-05-28T00:38:03Z
dc.date.available2022-05-28T00:38:03Z
dc.date.issued2017
dc.descriptionPresented on December 11, 2017 at the International Arctic Change Conference held at Québec City Convention Centre, Québec.
dc.description.abstractOver the past five decades, polar regions such as the Canadian Arctic Archipelago (CAA) have experienced pronounced changes associated with recent climate warming, such as sea ice decline (ACIA, 2005; IPCC, 2007). Such relatively recent and open-ended environmental shifts have motivated research regarding past climate variability to understand how polar marine environments responded to previous high-magnitude changes such as glacial to interglacial transitions. MacEwan University's RAPIDE (Researching Arctic Palaeoceanographic Indicators of Deglacial Environments) program seeks to apply multiple sedimentological, stratigraphic, and micropalaeontological approaches to elucidate the timing and style of marine-based deglaciation and subsequent oceanographic evolution through the CAA.
dc.format.extent12.81 MB
dc.format.mimetypePDF
dc.identifier.urihttps://hdl.handle.net/20.500.14078/977
dc.languageEnglish
dc.language.isoen
dc.rightsAll Rights Reserved
dc.subjectCanadian Arctic Archipelago
dc.subjectdeglaciation
dc.subjectforaminifera
dc.titleForaminifera: a tool for elucidating past and recent climate change in marine Arctic Canadaen
dc.typeStudent Presentation
dspace.entity.type

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