Botany A review of the plants of the Princeton chert (Eocene, British Columbia, Canada) Journal: Botany Manuscript ID cjb-2016-0079.R1 Manuscript Type: Review Date Submitted by the Author: 07-Jun-2016 Complete List of Authors: Pigg, Kathleen; Arizona State University, School of Life Sciences DeVore, Melanie; Georgia College and State University, Department of Biological &Draft Environmental Sciences Allenby Formation, Aquatic plants, Fossil monocots, Okanagan Highlands, Keyword: Permineralized floras https://mc06.manuscriptcentral.com/botany-pubs Page 1 of 75 Botany A review of the plants of the Princeton chert (Eocene, British Columbia, Canada) Kathleen B. Pigg , School of Life Sciences, Arizona State University, PO Box 874501, Tempe, AZ 85287-4501, USA Melanie L. DeVore , Department of Biological & Environmental Sciences, Georgia College & State University, 135 Herty Hall, Milledgeville, GA 31061 USA Corresponding author: Kathleen B. Pigg (email:
[email protected]) Draft 1 https://mc06.manuscriptcentral.com/botany-pubs Botany Page 2 of 75 A review of the plants of the Princeton chert (Eocene, British Columbia, Canada) Kathleen B. Pigg and Melanie L. DeVore Abstract The Princeton chert is one of the most completely studied permineralized floras of the Paleogene. Remains of over 30 plant taxa have been described in detail, along with a diverse assemblage of fungi that document a variety of ecological interactions with plants. As a flora of the Okanagan Highlands, the Princeton chert plants are an assemblage of higher elevation taxa of the latest early to early middle Eocene, with some components similar to those in the relatedDraft compression floras. However, like the well known floras of Clarno, Appian Way, the London Clay, and Messel, the Princeton chert provides an additional dimension of internal structure.