“…The sclerotium grains contain a remarkable amount of DHPQ (Kumada and Hurst, 1967;Sato, 1976b;Nakabayashi et al, 1982;Kumada, 1987), and DHPQ in the green fraction of humic acid (Pg) also originates from the C. geophilum sclerotium grains (Kumada and Hurst, 1967;Sato and Kumada, 1967;Sato, 1976b;Nakabayashi et al, 1982;Kumada, 1987). Moreover, both the sclerotium grains of C. geophilum (Trappe, 1969;Kumada, 1987;Massicotte et al, 1992;Watanabe et al, 2004Watanabe et al, , 2007Sakagami, 2010) and Pg (Kumada and Hurst, 1967;Sato, 1976a;Kumada, 1987;Watanabe et al, 1996) are found throughout the world. Thus, there is a strong possibility that DHPQ from C. geophilum is a major precursor of sedimentary perylene around the world.…”