Palynofloras from the middle Early to early Middle Eocene Okanagan Highlands (northern
Washington State and southern British Columbia) are used to reconstruct vegetation across …

The late Early to early Middle Eocene Okanagan Highlands fossil sites, spanning∼ 1000 km
north–south (northeastern Washington State, southern British Columbia) provide an …

The fossil flora and depositional setting of the Early Eocene Falkland site in the southern
interior of British Columbia, Canada, is reported in detail for the first time, using a census …

Wetland plant communities persisted though much of the Pennsylvanian in Euramerica and
are the dominant coal forming vegetation in this region. Distribution of these floras show a …

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 …

The lower Cantwell Formation in Denali National Park, Alaska, is a Late Cretaceous high-
latitude fluvial succession that contains dinosaur and bird footprints, diverse invertebrate …

The Pennsylvanian lowlands of western Pangea are best known for their diverse wetland
floras of arborescent and herbaceous ferns, and arborescent horsetails and clubmosses. In …

The palaeobotanical record associated with the coal-bearing sequences of Euramerica has
historically been taken to epitomise Pennsylvanian (late Carboniferous) vegetation …

The early Eocene fossil localities of the Okanagan Highlands in British Columbia, Canada,
and Washington State, USA, span the Early Eocene Climatic Optimum, the warmest period …

The distribution and community ecology of Early Pennsylvanian (middle Bashkirian,
Langsettian) vegetation on a seasonally dry fluvial megafan is reconstructed from plant …