Foraminiferal Evidence of Younger Dryas Age Cooling on the British Columbia Shelf

Cluster analysis of foraminifera from a ~12,000-9000 radiocarbon year old piston core from Goose Island Trough, Queen Charlotte Sound, indicates that a cold interval correlative with the Younger Dryas stadial occurred during a shallow water phase. The reduction in depth was caused by the passage acr...

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Bibliographic Details
Published in:Géographie physique et Quaternaire
Main Authors: Patterson, R. Timothy, Guilbault, Jean-Pierre, Thomson, Richard E., Luternauer, John L.
Format: Text
Language:English
Published: Les Presses de l'Université de Montréal 1995
Subjects:
Online Access:http://id.erudit.org/iderudit/033063ar
https://doi.org/10.7202/033063ar