Way on the eastern shore of Vancouver Island. Three years later the ascomycete Margaretbarromyces dictyosporus was also described from the Appian Way site. Description The holotype of Quatsinoporites is a lone fragment of fruiting body by and deep, which was abraded by water transport before preservation in a calcareous nodule. The conk section has an average of three, 130 to 540 μm diameter tubes per millimeter. The fungus is composed of monomitic hyphae. Due to the abraded nature of the specimen the basidia and basidiospores are both unknown at this time. The specimen was studied by cutting the calcareous nodule into slices with a rock saw and using the cellulose acetate peel technique to create slides that were examined under stereo microscope.Quatsinoporites'' is placed in Hymenochaetaceae based on the structure of the poroid hymenophore, the presence of setae and monomitic hyphal system lacking clamp connections. This placement is tentative due to limited characters available in the fossil the lack of diagnostic features such as the basidiospores. References †Quatsinoporites †Quatsinoporites Prehistoric fungi Fossil taxa described in 2004 Flora of British Columbia Cretaceous fungi Monotypic Basidiomycota genera