By filling in the missing gaps present in geologic record, we can reconstruct past environmental conditions. This can be used to gain insight into the current climate threats today. No time in the past better mirrors current environmental conditions than the End-Permian. We intend to sample the Permian Triassic Boundary (PTr), of the Mino-Terrane, located in Central Japan to gain a better understanding of global conditions during the PTr. and verify results generated from Mount Jesmond.