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| 1 | The Global Stratotype Section and Point (GSSP) for the boundary between the Capitanian and Wuchiapingian Stage (Permian)显示文摘 | Yugan Jin Shuzhong Shen Charles M. Henderson Xiangdong Wang Wei Wang Yue Wang Changqun Cao Qinghua Shang | 2006 | Episodes2006，29，4： | 39 |
| 2 | Carbon isotope excursions across the Permian-Triassic boundary in the Meishan section, Zhejiang Province, China显示文摘Both gradual and sharp decrease in organic and carbonate carbon isotope values were detected across the Permian-Triassic boundary in the Meishan section, Changxing, Zhejiang Province, China. The gradual decrease in organic carbon isotope values started at the bottom of Bed 23, coinciding with the strong oscillations of total organic carbon (TOC) contents, indicates increasing fluxes from carbonate to organic carbon reservoir during this interval. A 2.3‰ sharp drop of inorganic carbon isotope values occurred at the uppermost part of Bed 24e. A 3.7‰ sharp drop of organic carbon isotope values occurred in Bed 26. The dramatic drop of inorganic carbon isotope value of 8‰ reported previously is not confirmed from the unweathered carbonate samples in Bed 27. The large-scale fluctuation of organic carbon isotope values in the Yinkeng Formation reflects different extent of mixing of marine and terrestrial organic matters. The gradual depletion and subsequent sharp drop of carbon isotopes near the | Changqun Cao Wei Wang Yugan Jin | 2002 | Chinese Science Bulletin2002，47，13： | 33 |
| 3 | The Global Boundary Stratotype Section and Point (GSSP) for the base of Changhsingian Stage (Upper Permian)显示文摘 | Yugan Jin Yue Wang Charles Henderson Bruce R. Wardlaw Shuzhong Shen Changqun Cao | 2006 | Episodes2006，29，3： | 24 |
| 4 | Chronostratigraphic Subdivision and Correlation of the Permian in China显示文摘Since the principle of multiple stratigraphic classification has been widely accepted by Chinese stratigraphers, various new Permian chronostratigraphic units have been proposed in China, and they need to be redefined. The establishment of a new global chronostratigraphic scheme of the Permian, compilation of Permian lithostratigraphic units and updating of Permian biostratigraphic sequences of China makes it possible to present a revised regional chronostratigraphic succession for the Permian System in China. This succession consists of three series and eight stages. The Chuanshanian Series includes two stages, the Zisongian and the Longlinian; the Yanghsinian (Yangxinian) Series is subdivided into the Chihsian (Qixiaan) and the Maokouan Subseries, of which the former comprises the Luodianian and the Xiangboan Stage, and the latter the Kufengian (Gufengian) and the Lengwuan Stage; the Lopingian (Lepingian) Series includes the Wuchiapingian (Wujiapingian) and the Changhsingian (Changxingian) Stage. | JIN Yugan SHANG Qinghau WANG Xiangdong WANG Yue SHENG Jinzhang | 1999 | Acta Geologica Sinica(English Edition)1999，73，2： | 14 |
| 5 | Zonation of Conodonts from the Maokouan-Wuchiapingian boundary strata, South China显示文摘 | Mei Shilong Jin Yugan Wardlaw B R | 1994 | Palaeoworld1994，4，： | 1 |
| 6 | Conodont succession of the Guadalupian-Lopingian boundary strata in Laibin of Guangxi, China and West Texas, USA显示文摘 | Mei Shilong Jin Yugan Wardlaw B R | 1998 | Palaeoworld1998，9，： | 1 |
| 7 | Proposal for the global stratotype section and point (GSSP) for the Guadalupian-Lopingian boundary显示文摘 | Jin Yugan Henderson C M Wardlaw B R | 2001 | Permophiles2001，39，： | 1 |
| 8 | Discuss the Age and Ancient Environment Characteristics of Hala’ alate Formation显示文摘 | WANG Yujing JIN Yugan JIANG Nayan | 1987 | Journal of Stratigraphy1987，11，1： | 1 |
| 9 | Late Permian magnetostratigraphy and its global correlation显示文摘A calibration among magnetic polarity sequence, biostratigraphy zonation and isotopicage reveals that the boundary between the Carboniferous-Permian reversed Polarity Superzone and Permian-Triassic Mixed Polarity Superzone occurs at the top of the wordian Stage of the Guadalupian Series and is dated as 265 Ma. The Late Permian magnetic polarity sequence integrates four polarity zones, corresponding to the Upper Guadalupian Series, the wuchiapingian Stage, and the Lower and the Upper Changhsingian Stage of the Lopingian Series. This reference magnetostratigraphy polarity sequence may serve as a useful guide to the chronostratigraphic correlation of Late Permian strata across major biogeographic and facies barriers. | Yugan Jin Qinghua Shang Changqun Cao | 2000 | Chinese Science Bulletin2000，45，8： | 1 |
| 10 | Pattern of marine mass extinction near the Permian- Triassic boundary in south China显示文摘 | Jin Yugan Wang Yue Wang Wei | 2000 | Science2000，289，： | 1 |
| 11 | The Lopingian Series of China and End-Permian Mass Extinction显示文摘The end-Permian mass extinction is the greatest bioevent in the geological history, which wiped out nearly 95% of the marine species and 75% of the terrestrial species,followed by a biological winter for more than five million years.The cause and the process of the end-Permian mass extinction remain an unsolved mystery in earth science and one of the most difficult and interesting scientific problems. | JIN Yugan SHEN Shuzhong WANG Xiangdong WANG Yue CAO Changqun | 2011 | Bulletin of the Chinese Academy of Sciences2011，25，2： | 0 |
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