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...
Published in: | Géographie physique et Quaternaire |
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Main Authors: | , , , |
Format: | Text |
Language: | English |
Published: |
Les Presses de l'Université de Montréal
1995
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Subjects: | |
Online Access: | http://id.erudit.org/iderudit/033063ar https://doi.org/10.7202/033063ar |