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
- 1 November 1998
- journal article
- Published by Elsevier BV in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 143 (4), 213-226
- https://doi.org/10.1016/s0031-0182(98)00112-6
Abstract
No abstract availableThis publication has 1 reference indexed in Scilit:
- A conodont-based high-resolution biostratigraphy for the Permo-Triassic boundary intervalPublished by Cambridge University Press (CUP) ,1992