The late Quaternary environmental evolution of marine Arctic Canada: Barrow Strait to Lancaster Sound

A marine sediment core from the east-central Canadian Arctic Archipelago (Core 86027-154; 74° 22.01′N 89° 51.26′W; 329 m water depth), studied by a multiproxy approach [lithostratigraphy, biogeochemistry, micropalaeontology (dinoflagellate cysts, other non-pollen palynomorphs, benthic and planktonic...

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Veröffentlicht in:	Quaternary science reviews 2014-05, Vol.91, p.184-203
Hauptverfasser:	Pieńkowski, Anna J., England, John H., Furze, Mark F.A., MacLean, Brian, Blasco, Steve
Format:	Artikel
Sprache:	eng
Schlagworte:	Deglaciation Environmental change Foraminifera Holocene Late Wisconsinan Neogloboquadrina pachyderma Northwest Passage Ostracoda Palaeoenvironment Portlandia Sea ice
Online-Zugang:	Volltext
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