The conodont stratigraphy of a Guadalupian–Lopingian pelagic chert was examined.
A record of organic carbon isotopes from the same interval is presented.
未13C values in the Roadian–Wordian interval were relatively high.
未13C values gradually decreased during the Capitanian–Wuchiapingian interval.
The 未13C decrease can be correlated with excursions in other sections.