Picea banksii n. sp. Beaufort Formation (Tertiary), northwestern Banks Island, Arctic Canada

Picea cones of late Tertiary age, from northwestern Banks Island, Arctic Canada, are described and illustrated. Extremely good preservation allowed measurements on cone length and width, scale length and width, seed wing length, and bract length, width, and number of teeth. In addition, ratios such...

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Bibliographic Details
Published in:Canadian Journal of Botany
Main Authors: Hills, L. V., Ogilvie, R. T.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1970
Subjects:
Online Access:http://dx.doi.org/10.1139/b70-065
http://www.nrcresearchpress.com/doi/pdf/10.1139/b70-065
Description
Summary:Picea cones of late Tertiary age, from northwestern Banks Island, Arctic Canada, are described and illustrated. Extremely good preservation allowed measurements on cone length and width, scale length and width, seed wing length, and bract length, width, and number of teeth. In addition, ratios such as scale length to width; seed length to width; seed length to scale length; and bract length to scale length are calculated.Comparison is made with extant species of Picea and it is concluded that the fossil is most closely related to Picea glauca. It is suggested that a Picea glauca type was ancestral to many Northern Hemisphere spruce.