Ulmus chuchuanus
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| Ulmus chuchuanus Temporal range: | |
|---|---|
| U. chuchuanus leaf | |
| Scientific classification | |
| Kingdom: | Plantae |
| Clade: | Tracheophytes |
| Clade: | Angiosperms |
| Clade: | Eudicots |
| Clade: | Rosids |
| Order: | Rosales |
| Family: | Ulmaceae |
| Genus: | Ulmus |
| Species: | †U. chuchuanus |
| Binomial name | |
| †Ulmus chuchuanus | |
| Synonyms | |
| |
Ulmus chuchuanus is an extinct species of flowering plant in the family Ulmaceae related to the modern elms. The species is known from fossil leaves and fruits found in early Eocene sites of northern Washington state, United States and central British Columbia, Canada.
Ulmus chuchuanus fossils have been identified from six locations in northwestern North America. The species redescription listed occurrences in the British Columbian Chu Chua Formation at Joseph Creek, the McAbee[1] and Falklands sites of the Traquille Formation around Cache Creek, and in Coldwater Beds at Quilchena. The most northerly of the sites known are the Driftwood Shales northeast of Smithers while the most southerly is of the Klondike Mountain Formation near Republic, Washington.[2]
The sites comprise the Eocene Okanagan Highlands fossil site system. The highlands, including the Eocene formations between Driftwood canyon and Republic, have been described as one of the "Great Canadian Lagerstätten"[3] based on the diversity, quality and unique nature of the paleofloral and paleofaunal biotas that are preserved. The highlands temperate biome preserved across a large transect of lakes recorded many of the earliest appearances of modern genera, while also documenting the last stands of ancient lines.[3] The warm temperate highland floras in association with downfaulted lacustrine basins and active volcanism are noted to have no exact modern equivalents. This is due to the more seasonally equitable conditions of the Early Eocene, resulting in much lower seasonal temperature shifts. However, the highlands have been compared to the upland ecological islands in the Virunga Mountains within the Albertine Rift of the African rift valley.[4]