Geology; v. 28; p. 623–626 (July 2000)

An error was found in the last paragraph of the section “Global Correlation.” The corrected paragraph is below.

The identification of archaeocyathan species Tumuliolythus macrospinosus and Archaelynthus macrospinosus near the top of a comparable Zhongyicun phosphorite bed, about 30 km east of our measured section (Luo et al., 1982), indicates that the C isotope peak in the Dahai Member is above the Tommotian. Because the lowest occurrence of archaeocyathan faunas has not yet been defined in southwest China, and the underlying Zhongyicun phosphogenesis may have removed parts of the primary C isotope...

You do not currently have access to this article.