“…A recent study re-identified several ammonoid fossils from the type section of the Osawa Formation as Hellenites tchernyschewiensis , H. inopinatus , Neocolumbites grammi , N. insignis , Procolumbites ussuriensis , and P. subquadratus in its lower part; therefore, the lower Osawa Formation can be correlated to the N. insignis zone of South Primorye 60 . It is possible that Utatsu-Tatezaki, the other ichthyosauromorph-bearing “ Columbites – Subcolumbites zone” locality, which is the type locality of Utatsusaurus , also includes N. insignis (upper lower Spathian) and Subcolumbites (middle Spathian) subzones because no large missing parts have been recognized between the underlying Hiraiso Formation and Osawa Formation 32 , 61 , 62 . As evidenced by Smith et al 3 and this study, some medium (~ 2.5 m) to large (~ 5 m) ichthyopterygians were present during the early Spathian, shortly after the P–T boundary (approximately 3 Mys 53 ), thus, it is not surprising that lower Spathian marine reptiles exist among Japanese collections.…”