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A Paleogene flora from the upper Bonnet Plume Formation of northeast Yukon Territory, Canada
Philip J. Currie Dinosaur Museum.
Royal Ontario Museum.
Canadian Journal of Earth Sciences.
Uppsala universitet, Teknisk-naturvetenskapliga vetenskapsområdet, Geovetenskapliga sektionen, Institutionen för geovetenskaper. (Palaeobiology)
Vise andre og tillknytning
2012 (engelsk)Inngår i: Canadian journal of earth sciences (Print), ISSN 0008-4077, E-ISSN 1480-3313, Vol. 49, nr 3, s. 547-558Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Palaeontological exploration of the Bonnet Plume Basin in northwestern Yukon Territory, Canada, has revealed a Late Paleocene to Early Eocene macrofloral assemblage from a channel fill deposit. The flora is typified by cosmopolitan taxa and dominated by deciduous angiosperms, with the notable presence of ZizyphoidesEttingshausenia, and Corylites. Floras with a similar composition are known from Late Cretaceous through Early Eocene deposits in Alaska and the Canadian Arctic Archipelago, where they have been interpreted as evidence for warm, equable temperatures. This collection represents the most diverse known Paleogene plant macrofossil assemblage from the Yukon Territory and helps to expand our knowledge of ancient high-latitude floras.

sted, utgiver, år, opplag, sider
NRC Research Press, 2012. Vol. 49, nr 3, s. 547-558
HSV kategori
Forskningsprogram
Biologi med inriktning mot systematik
Identifikatorer
URN: urn:nbn:se:uu:diva-217209DOI: 10.1139/e11-073OAI: oai:DiVA.org:uu-217209DiVA, id: diva2:692532
Tilgjengelig fra: 2014-01-31 Laget: 2014-01-31 Sist oppdatert: 2017-12-06

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