Taxonomic restudy of Early Darriwilian graptolites from the Yangtze region,
Chiadam and Alxa, has enabled a precise correlation of the Undulograptus a
ustrodentatus Zone (including two subzones) across the three regions, and w
ith the Darriwilian GSSP at Huangnitang in the Jiangshan-Changshan-Yushan (
JYC) area. Based on specimens from 17 localities in the Yangtze region, the
Exigraptus clavus and Undulograptus austrodentatus zones are recognised as
replacements respectively of the Undulograptus sinodentatus (Lower) and U.
austrodentatus (Upper) zones of Mu el al. (1979). The U. sinicus Subzone,
the upper subzone of the U, austrodentatus Zone, is also recognised from th
e Sichuan-Guizhou area of the Yangtze region, Two subzones of the U. austro
dentatus Zone have also been identified from the Chiadam region with more d
iverse graptolite fauna. The U. austrodentatus Zone fauna also occurs in th
e Alxa region. A general pattern of changing graptolite diversity from plat
form through basinal slope to deep basin is proposed, based on early Darriw
ilian bio- and lithofacies changes from the Yangtze Platform through the Ji
angnan belt to the Zhujiang basin. The graptolite diversity increased with
water depth and more off-shore setting. Key graptolite species are illustra
ted.