Abstract. 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 biota but also with abundant
thermophilic elements, such as crocodilians, and mesothermic taxodioid
conifers and angiosperms. The globally warm early Eocene was punctuated by
geologically brief hyperthermals such as the Paleocene–Eocene Thermal
Maximum (PETM), culminating in the Early Eocene Climatic Optimum (EECO),
during which the range of thermophilic plants such as palms extended into
the Arctic. Climate models have struggled to reproduce early Eocene Arctic
warm winters and high precipitation, with models invoking a variety of
mechanisms, from atmospheric CO2 levels that are unsupported by proxy
evidence to the role of an enhanced hydrological cycle, to reproduce winters
that experienced no direct solar energy input yet remained wet and above
freezing. Here, we provide new estimates of climate and compile existing
paleobotanical proxy data for upland and lowland midlatitude sites in
British Columbia, Canada, and northern Washington, USA, and from
high-latitude lowland sites in Alaska and the Canadian Arctic to compare
climatic regimes between the middle and high latitudes of the early
Eocene – spanning the PETM to the EECO – in the northern half of North
America. In addition, these data are used to reevaluate the latitudinal
temperature gradient in North America during the early Eocene and to provide
refined biome interpretations of these ancient forests based on climate and
physiognomic data.