广西来宾二叠系瓜德鲁普统-乐平统界线蓬莱滩剖面沉积微相演变及其对生物灭绝事件的响应

黄俊亚, 张伟, 巴燕, 周红智, 杜保军, 宁勇. 2019. 广西来宾二叠系瓜德鲁普统-乐平统界线蓬莱滩剖面沉积微相演变及其对生物灭绝事件的响应. 沉积与特提斯地质, 39(3): 11-20.
引用本文: 黄俊亚, 张伟, 巴燕, 周红智, 杜保军, 宁勇. 2019. 广西来宾二叠系瓜德鲁普统-乐平统界线蓬莱滩剖面沉积微相演变及其对生物灭绝事件的响应. 沉积与特提斯地质, 39(3): 11-20.
HUANG Junya, ZHANG Wei, BA Yan, ZHOU Hongzhi, DU Baojun, NING Yong. 2019. Sedimentary microfacies and sedimentary responses to the biotic extinction events within the Penglaitan section at the Guadalupian-Lepingian (Permian) boundary in Laibin, Guangxi. Sedimentary Geology and Tethyan Geology, 39(3): 11-20.
Citation: HUANG Junya, ZHANG Wei, BA Yan, ZHOU Hongzhi, DU Baojun, NING Yong. 2019. Sedimentary microfacies and sedimentary responses to the biotic extinction events within the Penglaitan section at the Guadalupian-Lepingian (Permian) boundary in Laibin, Guangxi. Sedimentary Geology and Tethyan Geology, 39(3): 11-20.

广西来宾二叠系瓜德鲁普统-乐平统界线蓬莱滩剖面沉积微相演变及其对生物灭绝事件的响应

  • 基金项目:

    中国地质调查局(DD20179182)项目资助

详细信息
    作者简介: 黄俊亚(1961-),男,工程师。E-mail:yunzi90h@qq.com
  • 中图分类号: P512.2

Sedimentary microfacies and sedimentary responses to the biotic extinction events within the Penglaitan section at the Guadalupian-Lepingian (Permian) boundary in Laibin, Guangxi

  • 在中二叠世(瓜德鲁普世)末期发生了一次全球范围的生物灭绝事件,大约有34%的海洋无脊椎动物消失,同时发生了全球规模的海退事件。该事件在中国反应为东吴运动,致使华南大部分地区瓜德鲁普统-乐平统之交产生不整合。广西来宾地区位于扬子地台南缘,在中-晚二叠世时期处于滇黔桂盆地的东部。由于其独特的古地理位置,来宾地区发育了连续的中-晚二叠世海相沉积,是研究此次生物大灭绝和环境演变的绝佳位置。本文对广西来宾蓬莱滩瓜德鲁普统-乐平统(G-L)界线剖面沉积微相和生物化石进行了综合研究。研究表明,该剖面1~7层共发育5种主要的沉积微相组合,既礁基相组合、礁核相组合、覆礁相组合、礁滩相组合和深水斜坡相组合,生物礁发育于一个海退序列中。生物碎屑的丰度和类型在7a层突然急剧降低,与该剖面碳同位素的负偏和汞异常的出现一致,但实际上在这一层位只有个别牙形石和菊石消失,生物屑丰度的剧变并不能代表灭绝线,而是对海平面剧变的沉积响应。
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  • [1]

    Haq B U, Schutter S R. A chronology of Paleozoic sea-level changes[J]. Science, 2008, 322:64-68.

    [2]

    Chen Z Q, George A D, Yang W R. Effects of Middle-Late Permian sea-level changes and mass extinction on the formation of the Tieqiao skeletal mound in the Laibin area, South China[J]. Australian Journal of Earth Sciences, 2009, 56:745-763.

    [3]

    邱振,孙枢,王清晨,等. 瓜德鲁普统-乐平统全球界线层型剖面沉积相和层序地层[J]. 沉积学报,2014,32(3):429-441.

    [4]

    Wignall P B, Sun Y D, Bond D P G, et al. Volcanism, Mass Extinction, and Carbon Isotope Fluctuations in the Middle Permian of China[J]. Science, 2009, 324:1179-1182.

    [5]

    Jost A B, Mundil R, He B, et al. Constraining the cause of the end-Guadalupian extinction with coupled records of carbon and calcium isotopes[J]. Earth and Planetary Science Letters, 2014, 396:201-212.

    [6]

    Clapham M E, Shen S Z, Bottjer D J. The double mass extinction revisited:reassessing the severity, selectivity, and causes of the end-Guadalupian biotic crisis (Late Permian)[J]. Paleobiology, 2009, 35:32-50.

    [7]

    Flügel E, Wolfgang K. Patterns of Phanerozoic reef crises[C]. Tulsa:SEPM Special Publication, No. 72, 2002.691-733.

    [8]

    Huang Y G, Chen Z Q, Zhao L S, et al. Restoration of reef ecosystems following the Guadalupian-Lopingian boundary mass extinction:Evidence from the Laibin area, South China[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2019, 519:8-22.

    [9]

    Shen S Z, Wang Y, Henderson C M, et al. Biostratigraphy and lithofacies of the Permian System in the Laibin-Heshan area of Guangxi, South China[J]. Palaeoworld, 2007, 16:120-139.

    [10]

    Bond D P G, Hilton J, Wignall P B, et al. The Middle Permian (Capitanian) mass extinction on land and in the oceans[J]. Earth-Science Reviews, 2010, 102:100-116.

    [11]

    Zhang G J, Zhang X L, Li D D, et al. Widespread shoaling of sulfidic waters linked to the end-Guadalupian (Permian) mass extinction[J]. Geology, 2015, 43:1091-1094.

    [12]

    Wang X D, Sugiyama T. Middle Permian rugose corals from Laibin, Guangxi, South China[J]. Journal of Paleontology, 2001, 75:758-782.

    [13]

    Huang Y G, Chen Z Q, Zhao L S. Biotic responses to volatile volcanism and environmental stresses over the GuadalupianLopingian (Permian) transition[J]. Geology, 2019, 47:175-178.

    [14]

    Shen, S Z, Shi G R. Latest Guadalupian brachiopods from the Guadalupian/Lopingian boundary GSSP section at Penglaitan in Laibin, Guangxi, South China and implications for the timing of the pre-Lopingian crisis[J]. Palaeoworld, 2009, 18:152-161.

    [15]

    Ehiro M, Shen S Z. Permian ammonoid Kufengoceras from the uppermost Maokou Formation (earliest Wuchiapingian) at Penglaitan, Laibin Area, Guangxi Autonomous Region, South China[J]. Paleontological Research, 2008, 12:255-259.

    [16]

    Mei S L, Jin Y G, Wardlaw B R. Conodont succession of the Guadalupian-Lopingian boundary strata in Laibin of Guangxi, China and West Texas, USA[J]. Palaeoworld, 1998, 9:53-76.

    [17]

    韦雪梅,江增光,白玛曲宗,韦恒叶. 广西来宾蓬莱滩剖面瓜德鲁普统-乐平统(G-L)界线生境型及其意义[J]. 东华理工大学学报(自然科学版),2016,39(4):331-340.

    [18]

    Wang W, Cao CQ, Wang Y. The carbon isotope excursion on GSSP candidate section of Lopingian-Guadalupian boundary[J]. Earth and Planetary Science Letters, 2004, 220:57-67.

    [19]

    Wei H Y, Wei X M, Qiu Z, et al. Redox conditions across the G-L boundary in South China:Evidence from pyrite morphology and sulfur isotopic compositions[J]. Chemical Geology, 2016, 440:1-14.

    [20]

    王钦贤,童金南,宋海军,杨浩. 湖南慈利康家坪剖面二叠纪-三叠纪之交的生态系演变[J]. 中国科学(D辑:地球科学), 2009,39(9):1239-1247.

    [21]

    Jin Y G, Shen S Z, Henderson C M, et al. The Global Stratotype Section and Point (GSSP) for the boundary between the Capitanian and Wuchiapingian stage (Permian)[J]. Episodes, 2006, 29:253-262.

    [22]

    Qiu Z, Wang Q C, Zou C, et al. Transgressive-regressive sequences on the slope of an isolated carbonate platform (MiddleLate Permian, Laibin, South China)[J]. Facies, 2014, 60:327-345.

    [23]

    陈军,徐义刚. 二叠纪大火成岩省的环境与生物效应:进展与前瞻[J]. 矿物岩石地球化学通报,2017,36:374-393.

    [24]

    Zhang Z, Wang Y, Zheng Q F. Middle Permian smaller foraminifers from the Maokou Formation at the Tieqiao section, Guangxi, South China[J]. Palaeoworld, 2015, 24:263-276.

    [25]

    Chen B, Joachimski MM, Sun Y D, et al. Carbon and conodont apatite oxygen isotope records of Guadalupian-Lopingian boundary sections:Climatic or sea-level signal[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2011, 311:145-153.

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出版历程
收稿日期:  2019-07-17
修回日期:  2019-08-12
刊出日期:  2019-09-30

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