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Integrated Stratigraphy of the Lower and Middle Fernie Formation in Alberta and British Columbia, western Canada

Hall, R.; McNicoll, V.; Gröcke, D.R.; Craig, J.; Jonhston, K.

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Authors

R. Hall

V. McNicoll

J. Craig

K. Jonhston



Abstract

The lower and middle parts of the Fernie Formation in central-western Alberta and south-eastern British Columbia, ranging from Pliensbachian to ?Bathonian (Early to Middle Jurassic) in age, and consisting mainly of fossiliferous dark shales and black limestones, contain bentonitic clay horizons which have yielded radiometric ages using U-Pb analysis of zircon crystals. Here we report six new ages from the lowermost Red Deer Member (188.3 +1.5/-1 Ma); Highwood Member (ca. 173 Ma and 166.6 ± 0.2 Ma); and Grey Beds (167.0 ± 0.2 Ma, 165.6 ± 0.3 Ma, and 165.4 ± 0.3 Ma). Some of these bentonites are associated with ammonites and coccoliths which provide biostratigraphic constraints. Strontium and carbon and oxygen isotopes measured from belemnite rostra have been compared in two sections and the resulting curves are compared with those from western Europe.

Citation

Hall, R., McNicoll, V., Gröcke, D., Craig, J., & Jonhston, K. (2004). Integrated Stratigraphy of the Lower and Middle Fernie Formation in Alberta and British Columbia, western Canada. Rivista Italiana di Paleontologia e Stratigrafia, 110(1), 61-68. https://doi.org/10.13130/2039-4942/6264

Journal Article Type Article
Acceptance Date Sep 30, 2003
Publication Date Apr 1, 2004
Deposit Date May 19, 2015
Publicly Available Date Jan 26, 2017
Journal Rivista Italiana di Paleontologia e Stratigrafia
Electronic ISSN 2039-4942
Publisher Università degli Studi di Milano
Peer Reviewed Peer Reviewed
Volume 110
Issue 1
Pages 61-68
DOI https://doi.org/10.13130/2039-4942/6264
Public URL https://durham-repository.worktribe.com/output/1428399

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