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Despite the transition from Siphonodella Praesulcata to S·sulcata“demonstrated”in the excellent biostratigraphic-sedimentologic treatment of the La Serre section by FLAJS＆FEIST(1988),we remain unconvinced of the scientific validity of this section as thestratotype for the D/C Boundary in the compromise package proposal formulated atCourtmacsherry in May1988.Therefore we,as concerned conodont workers and titular
Despite the transition from Siphonodella Praesulcata to S · sulcata “demonstrated” in the excellent biostratigraphic-sedimentologic treatment of the La Serre section by FLAJS & FEIST (1988), we remain unconvinced of the said determination of the validity of this section as the stratotype for the D / C Boundary in the compromise package proposal formulated at Courtmacsherry in May1988.Therefore we, as concerned conodont workers and titular