Fossil palms provide qualitative evidence of (sub-) tropical conditions and frost-free winters
in the geological past, including modern cold climate regions (eg, boreal, or polar climates) …

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 …

Early Eocene climates were globally warm, with ice-free conditions at both poles. Early
Eocene polar landmasses supported extensive forest ecosystems of a primarily temperate …

The biodiversity history on the Qinghai–Tibetan Plateau (QTP) has remained unclear for a
long time. Recent paleobotanical investigations provide opportunities for revealing the …

Abstract The McAbee Fossil Beds, in south-central British Columbia, Canada, provide a
record of forest ecosystems within a volcanically-active, upland landscape during the Early …

Detrital zircon U-Pb and Hf isotopic data from Ordovician to Devonian–Carboniferous
sedimentary rocks sampled from the Pearya terrane and adjacent areas, northern Ellesmere …

We examine the fossil weaver ants (Formicidae, Formicine, Oecophyllini) of the early
Eocene Okanagan Highlands fossil localities of British Columbia, Canada and Washington …

ABSTRACT During the Paleocene–Eocene, the Earth experienced the warmest conditions
of the Cenozoic and reduced equator-to-pole temperature gradients. Compared to low-and …

Palms (Arecaceae) are iconic plant fossils, providing evidence of warm climates in the
geological past in geographical areas that today support temperate, boreal or even polar …

Premise of research. Fossil fan palm fronds are well known from Eocene sites in the United
States; however, although they are also known from the Paleogene Huntingdon Formation …