Conodonts and Carbon Isotopes during the Permian-Triassic Transition on the Napo Platform, South China
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://link.springer.com/content/pdf/10.1007/s12583-018-0884-3.pdf
Reference70 articles.
1. Bai, R. Y., Dai, X., Song, H. J., 2017. Conodont and Ammonoid Biostratigraphies around the Permian-Triassic Boundary from Jianzishan of South China. Journal of Earth Science, 28(4): 595–613. https://doi.org/10.1007/s12583-017-0754-4
2. Baresel, B., Bucher, H., Bagherpour, B., et al., 2017. Timing of Global Regression and Microbial Bloom Linked with the Permian-Triassic Boundary Mass Extinction: Implications for Driving Mechanisms. Scientific Reports, 7(1): 43630. https://doi.org/10.1038/srep43630
3. Baud, A., Richoz, S., Pruss, S., 2007. The Lower Triassic Anachronistic Carbonate Facies in Space and Time. Global and Planetary Change, 55(1/2/3): 81–89. https://doi.org/10.1016/j.gloplacha.2006.06.008
4. Brand, U., Blamey, N., Garbelli, C., et al., 2016. Methane Hydrate: Killer Cause of Earth’s Greatest Mass Extinction. Palaeoworld, 25(4): 496–507. https://doi.org/10.1016/j.palwor.2016.06.002
5. Brosse, M., Bucher, H., Bagherpour, B., et al., 2015. Conodonts from the Early Triassic Microbialite of Guangxi (South China): Implications for the Definition of the Base of the Triassic System. Palaeontology, 58(3): 563–584. https://doi.org/10.1111/pala.12162
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