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Atlantic water inflow in the early Holocene Northwest Passage marked by planktonic foraminifera (Neogloboquadrina pachyderma)

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dc.contributor.authorPieńkowski, Anna J.
dc.contributor.authorCage, Alix
dc.contributor.authorFurze, Mark F.A.
dc.contributor.authorFigueiredo Martins, Ana Sílvia de
dc.contributor.authorEngland, John H.
dc.contributor.authorMcLean, Brian
dc.contributor.authorBlasco, Steve
dc.date.accessioned2016-10-17
dc.date.accessioned2022-05-28T00:36:24Z
dc.date.available2022-05-28T00:36:24Z
dc.date.issued2015
dc.descriptionPresented on May 10–13, 2015 at the 45th International Arctic Workshop held on the campus of the University of Bergen, Norway.
dc.description.abstractFour marine piston cores from the central Canadian Arctic Archipelago (CAA), investigated for sedimentology, micropalaeontology, and biogeochemistry (52 AMS radiocarbon dates), uniformly show the prominent early Holocene (˜10 cal ka BP) appearance of planktonic foraminifera immediately following deglaciation.
dc.format.extent299.46 KB
dc.format.mimetypePDF
dc.identifier.urihttps://hdl.handle.net/20.500.14078/611
dc.languageEnglish
dc.language.isoen
dc.rightsAll Rights Reserved
dc.titleAtlantic water inflow in the early Holocene Northwest Passage marked by planktonic foraminifera (Neogloboquadrina pachyderma)en
dc.typePresentation
dspace.entity.type

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