Acer rousei was described from two complete fruit specimens which were recovered from outcrops of the early Eocene, Ypresian[2]Allenby Formation exposed near Princeton, British Columbia and an additional three fruits from the Ypresian[2]McAbee Fossil Beds near Cache Creek, British Columbia. The two Allenby Formation specimens were found at the Burke Museum of Natural History and Culture location UWBM B3389, known as the One Mile Creek locality. Both the Allenby Formation and the unnamed formation outcropping at the McAbee Fossil Beds preserve upland temperate floras that were first interpreted as being Microthermal,[1] although further study has shown them to be more mesothermal in nature.[2] The plant community preserved in the Allenby formation is a mixed conifer-broadleaf forest with large pollen elements of birch and golden larch, but also having notable traces of fir and spruce. In contrast the McAbee Fossil Beds site is mostly broadleaf pollen with alder and elm dominating, and may represent a successional forest involving multiple volcanic ash eruptions.[2] The species was known only from the McAbee Fossil Beds and Princeton fossil localities when first described. A. rousei is among a number of Acer species described from the Princeton and related sites by Wolfe and Tanai.[1]
The samaras of A. rousei have two indistinct flanges medially along the notably inflated nutlet. The overall shape of the nutlet is circular to elliptic with the average length of the samara up to 3.2 centimetres (1.3 in) and a wing width of 1.1 centimetres (0.43 in). The paired samaras of the species have a notably high attachment angle of 80° to 90°. While very similar in morphology to species in the modern section Palmata, A. rousei differs in the presence of the flanges on the nutlet and circular to elliptic outline of the nutlet. The wing venation of A. rousei is similar to the modern species A. spicatum and its closely related species. The similarities indicate A. rousei as a possible ancestor to the members of the section Palmata.[1]
^ abcdMoss, P. T.; Greenwood, D. R.; Archibald, S. B. (2005). "Regional and local vegetation community dynamics of the Eocene Okanagan Highlands (British Columbia – Washington State) from palynology". Canadian Journal of Earth Sciences. 42 (2): 187–204. Bibcode:2005CaJES..42..187M. doi:10.1139/E04-095.