Palynological evidence for a warmer boreal climate in the Late Pliocene of the Yukon Territory, Canada

The Late Pliocene (3.6–2.6 Ma) was a period of significant global warmth, considered a potential analogue for future anthropogenic climate change. Newly discovered fine-grained sediments from between the gold-bearing lower and upper White Channel Gravels show the presence of a wetland or lake within...

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Bibliographic Details
Published in:Palynology
Main Authors: Pound, MJ, Lowther, RI, Peakall, J, Chapman, RJ, Salzmann, U
Format: Article in Journal/Newspaper
Language:English
Published: Taylor & Francis 2015
Subjects:
Online Access:https://eprints.whiterose.ac.uk/96052/
https://eprints.whiterose.ac.uk/96052/7/Pound_et_al_2015_AF.pdf
https://doi.org/10.1080/01916122.2014.940471