“…The lower formation is composed mainly of conglomerate, sandstone, and mudstone, with several intercalated tuff beds, of which one yields U-Pb ages of ca. 112.1 § 0.4 Ma (Kusuhashi et al, 2013). In 2006, a new terrestrial vertebrate fossil assemblage was found in a red mudstone of this formation, exposed in the bank of the Sasayama River at Kamitaki, Tamba City (Saegusa et al, 2008a(Saegusa et al, , 2008b.…”