A refined succession of Changhsingian and Griesbachian neogondolellid conodonts from the Meishan section, candidate of the global stratotype section and point of the Permian-Triassic boundary

107Citations
Citations of this article
24Readers
Mendeley users who have this article in their library.
Get full text

Abstract

A detailed study of new conodont collections from the Changxing Formation at the Meishan section has resulted in taxonomic refinement of several important neogondolellid species. Most of the previously erected species are much more strictly redefined, mainly based on the denticulation of the holotypes, and the stratigraphic ranges attributed to key conodont taxa are modified. Three new species and two new subspecies, all of which are form-species, are tentatively erected and described mainly for the purpose of taxonomic explanation. As a result of the taxonomic refinement, six neogondolellid conodont zones are recognized for the Changxing Formation and the Permian-Triassic boundary interval.

Cite

CITATION STYLE

APA

Mei, S., Zhang, K., & Wardlaw, B. R. (1998). A refined succession of Changhsingian and Griesbachian neogondolellid conodonts from the Meishan section, candidate of the global stratotype section and point of the Permian-Triassic boundary. In Palaeogeography, Palaeoclimatology, Palaeoecology (Vol. 143, pp. 213–226). Elsevier. https://doi.org/10.1016/S0031-0182(98)00112-6

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free