Grünbach Formation

All remains have been found at a single locality, which is a thin marl seam in the Konstantin mining tunnel, within the Felbering Mine in the Neue Welt area north west of Muthmannsdorf in Lower Austria.^[3] The initial remains were discovered in 1859 after an ornithopod tooth was found in a piece of coal in a dump outside the mine by Professor Ferdinand Stoliczka, and the productive seam discovered thereafter. The first material was described by Emanuel Bunzel in 1871^[4] and then additional material was described by Harry Seeley in 1881.^[5] Due to mining activity in the area ceasing at the end of the 19th century, no additional remains have been recovered since.

Most of these specimens were recovered from mining dumps near Grünbach am Schneeberg in lower Austria. The flora of the formation is considered to represent that of a high humidity subtropical climate, typical of the Euro-Sinian phytogeographical region.^[11][12][13]