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Solid Earth An interactive open-access journal of the European Geosciences Union

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doi:10.5194/se-2016-145
© Author(s) 2016. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
28 Oct 2016
Review status
A revision of this discussion paper was accepted for the journal Solid Earth (SE) and is expected to appear here in due course.
Precise age for the Permian-Triassic boundary in South China from high precision U-Pb geochronology and Bayesian age-depth modelling
Björn Baresel1, Hugo Bucher2, Morgane Brosse2, Fabrice Cordey3, Kuang Guodun4, and Urs Schaltegger1 1Department of Earth Sciences, University of Geneva, Geneva, 1205, Switzerland
2Paleontological Institute and Museum, Univer sity of Zurich, Zurich, 8006, Switzerland
3Laboratoire de Géologie de Lyon, CNRS-UMR 5265, Univer sité Claude Bernard Lyon 1, Villeurbanne, 69622, France
4Guangxi Bureau of Geology and Mineral Resources, Nanning, 530023, China
Abstract. This study is based on zircon U-Pb ages of 12 volcanic ash layers and volcanogenic sandstones from two marine sections with conformable formational Permian-Triassic boundaries (PTB) in the Nanpanjiang Basin (South China). Our dates of single, thermally annealed and chemically abraded zircons bracket the PTB in Dongpan and Penglaitan and provide the basis for a first proof-of-concept study utilizing a Bayesian chronology model comparing the three sections of Dongpan, Penglaitan and the Global Stratotype Section and Point (GSSP) Meishan. Our Bayesian modeling demonstrates that the formational boundaries in Dongpan (251.938 ± 0.029 Ma), Penglaitan (251.982 ± 0.031 Ma) and Meishan (251.956 ± 0.033 Ma) are synchronous within analytical uncertainty of ca. 30 ka. It also provides quantitative evidence that the ages of the paleontologically defined boundaries, based on conodont Unitary Associations zones in Meishan and on macrofaunas in Dongpan, are identical and coincide with the age of the formational boundaries. The age model also confirms the extreme condensation around the PTB in Meishan, which distorts the projection of any stratigraphic points or intervals onto other more expanded sections by means of Bayesian age-depth models. Dongpan and Penglaitan possess significantly higher sedimentation rates and thus offer a greater potential for high resolution studies of environmental proxies and correlations around the PTB than Meishan. This study highlights the power of high-resolution radio-isotopic ages that allow a robust intercalibration of patterns of biotic changes and fluctuating environmental proxies and will help recognizing their global, regional or local significance.

Citation: Baresel, B., Bucher, H., Brosse, M., Cordey, F., Guodun, K., and Schaltegger, U.: Precise age for the Permian-Triassic boundary in South China from high precision U-Pb geochronology and Bayesian age-depth modelling, Solid Earth Discuss., doi:10.5194/se-2016-145, in review, 2016.
Björn Baresel et al.
Björn Baresel et al.

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Short summary
This study re-evaluates the characterization of the Permian-Triassic boundary based on high-precision U-Pb geochronology from two basinal to slope depositional sections (Dongpan and Penglaitan) with conformable Permian-Triassic stage boundaries in the Nanpanjiang Basin, South China. Our new dates provide the basis for a first proof-of-concept study utilizing a Bayesian statistic age-depth chronology comparing these two sections with the Global Stratotype Section and Point at Meishan.
This study re-evaluates the characterization of the Permian-Triassic boundary based on...
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