Devonian Events and Biostratigraphy of South China

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Author: Bai Shun-liang et al
Language: English
Published on: 1999-01
Hardcover

In this research, the value of conodont studies is emphasized for biostratigraphy. From the base of the Emsian to the Lower Carboniferous. 53 conodont zones are recognized, which coincide with those of the international conodont zonation. Stage boundaries are defined by conodont-markers which had been ratified elsewhere by the International conmmission on Stratigraphy or Recommended by the subcommission on Devonian Stratigraphy, International Commission on Stratiigraphy. This zonation and definition fulfil the requirements of current international usage.



1.Stratigraphy, Sediment-Biofacies, Paleobathymetry, and Conodont CAI;
2.Carbon Stable Isotope & Strontinm as marker of mortality and paleosalinity
3.Ce/La Ration as Marker of Paleoredox;
4.Marker of Eustasy and Milankovitch Cyclicity;
5.Ni-Episode, Causes of Ni-Event and Mass Extinction;
6.Devonian-Carboniferous (D-C) Boundary;
7.Famennian, and the Frasnian-Famennian (F-F) Boundary;
8.Givetian-Frasnian (G-F) Boudary;
9.Eifelian-Givetian(E-G) Boundary;
10. Emsian-Eifelian(E-E) Boundary;
11. Basal Zlichovian;
12. Summary and Conclusions;
13. Systematic Paleontology, part 1.Conodontsand Miscellaneous;
14. Systematic Paleontology, Part 2. New Brachiopods Across the Eifelian-Givetian Boundary;
15. Systematic Paleontology, Part 3. Fauna across the F-F Boundary.




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