A review of paleobotanical studies of the Early Eocene Okanagan (Okanogan) Highlands floras of British Columbia, Canada, and Washington, USA
Author(s) -
David R. Greenwood,
Kathleen B. Pigg,
James F. Basinger,
Melanie L. DeVore
Publication year - 2016
Publication title -
canadian journal of earth sciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.525
H-Index - 75
eISSN - 1480-3313
pISSN - 0008-4077
DOI - 10.1139/cjes-2015-0177
Subject(s) - geology , archaeology , assemblage (archaeology) , paleontology , palynology , geological survey , geography , ecology , biology , pollen
The history of plant fossil collecting in the Okanagan (Okanogan) Highlands of British Columbia and northeastern Washington is closely intertwined with the history of geological surveys and mining activities from the 1870s onward. The first descriptions of fossil plants from British Columbia were published in 1870–1920 by J.W. Dawson, G.M. Dawson, and D.P. Penhallow. In the United States, fossil leaves and fish were first recognized at Republic, Washington, by miners in the early 1900s. Many early workers considered these floras to be of Oligocene or Miocene age. C.A. Arnold described Canadian occurrences of conifers and Azolla in the 1950s. Palynological studies in the 1960s by L.V. Hills, G.E. Rouse, and others and those of fossil fish by M.V.H. Wilson in the 1970–1980s provided the framework for paleobotanical research at several key localities. Permineralized plants were first described from the Princeton chert in the 1970s by C.N. Miller, J.F. Basinger, and others, followed by R.A. Stockey and her st...
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