Republica weatbrooki

Republica weatbrooki is known from a single location in the Eocene Okanagan Highlands, an outcrop of the Ypresian Klondike Mountain Formation in Republic. The holotype was recovered from the UWBM site B4131, which is designated the type locality, on May 24, 2006. Modern work on the fossil-bearing strata of the formation via radiometrically dating has given an estimated age in the Late Ypresian stage of the early Eocene, between at the youngest, with an oldest age estimate of , given based on detrital zircon isotopic data published in 2021. ==History and classification==

Republica weatbrooki was identified from only the type specimen, the holotype, number SR 06–59–08, which is a compression fossil preserved in the Stonerose Interpretive Center paleoentomological collection. The holotype was found at the Klondike Mountain Formations "B4131" locality, The fossil was described by paleontologist S. Bruce Archibald and entomologist Robert Cannings in 2021 and they coined the specific epithet weatbrooki as a patronym honoring Alex Weatbrook who found the fossil and donated it to Stonerose. They chose the genus name as a Latinized feminine form of the city name Republic. Modern Euphaeidae species are found in the Australasian, Indomalayan, and Palearctic biogeographic realms, while the known fossil record restricted to Europe and North America. ==Description==

The only known forewing is long and at its widest giving it a length to width ratio of 3.9, narrower than several other eodichromatines. The length between wing base and nodus is while the length to pterostigma is . The pterostigma is elongate, being long and only wide, and has slanted cell walls on both the basal and apical sides. Due to poor preservation of the finer venation of the wing, many of the delicate crossveins between more robust major veins are missing making total vein counts impossible from the holotype. The space between the Costa, which forms the frontal wing edge, and the Subcosta has at least 26 crossveins and likely more, all positioned between the Ax1 crossvein near the wing base and the nodus. Both the An isolated crossvein is present between the Ax1 and Ax2 veins of the other C-Sc space, both of which are distinctly more robust than any crossveins in the space. The wing was possibly slightly darkened across the basal region of the wing, with a lighter to hyaline window across the apical 1/3 of the wing surrounding a darkened tip area. However Archibald and Cannings noted the possibility of this "coloration" being a result of preservation artifacts and not coloration during life. ==Paleoenvironment==

The formation preserves an upland lake system surrounded by a mixed conifer–broadleaf forest with nearby volcanism. The pollen flora has notable elements of birch and golden larch, and distinct trace amounts of fir, spruce, cypress, and palm. ==References==