Abstract The Taho Formation in western Shikoku Island, Japan, consists of Triassic carbonates that formed on a seamount the Panthalassic Ocean. In order to investigate stratigraphy and paleoceanography this carbonate succession, we analyzed biostratigraphy chemostratigraphy 17.6 m‐thick section upper at stratotype area Tahokamigumi, Seiyo City. This comprises bioclastic limestone containing biv...