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    全球古-中生代之交牙形石研究进展

    吴奎 童金南 李红军 田力 邹亚锐 梁蕾 赵璧

    吴奎, 童金南, 李红军, 田力, 邹亚锐, 梁蕾, 赵璧, 2022. 全球古-中生代之交牙形石研究进展. 地球科学, 47(3): 1012-1037. doi: 10.3799/dqkx.2021.196
    引用本文: 吴奎, 童金南, 李红军, 田力, 邹亚锐, 梁蕾, 赵璧, 2022. 全球古-中生代之交牙形石研究进展. 地球科学, 47(3): 1012-1037. doi: 10.3799/dqkx.2021.196
    Wu Kui, Tong Jinnan, Li Hongjun, Tian Li, Zou Yarui, Liang Lei, Zhao Bi, 2022. Advance in the Study of Global Conodont during the Palaeozoic-Mesozoic Upheavals. Earth Science, 47(3): 1012-1037. doi: 10.3799/dqkx.2021.196
    Citation: Wu Kui, Tong Jinnan, Li Hongjun, Tian Li, Zou Yarui, Liang Lei, Zhao Bi, 2022. Advance in the Study of Global Conodont during the Palaeozoic-Mesozoic Upheavals. Earth Science, 47(3): 1012-1037. doi: 10.3799/dqkx.2021.196

    全球古-中生代之交牙形石研究进展

    doi: 10.3799/dqkx.2021.196
    基金项目: 

    国家自然科学基金项目 42030513

    国家自然科学基金项目 41530104

    国家自然科学基金项目 41661134047

    国家自然科学基金项目 41602024

    国家自然科学基金项目 42102011

    湖北省自然科学基金项目 2021CFB276

    湖北省地质局专项 KJ2019-01

    湖北省地质局专项 KJ2021-3

    河北省自然科学基金青年项目 D2020403072

    古生物与地质环境演化湖北省重点实验室开放研究基金 PEL-202104

    详细信息
      作者简介:

      吴奎(1992-),男,工程师,博士,主要从事二叠纪-三叠纪之交牙形石研究. ORICD: 0000-0001-9996-8318. E-mail: kuiwu@cug.edu.cn

      通讯作者:

      童金南,E-mail: jntong@cug.edu.cn

    • 中图分类号: P52

    Advance in the Study of Global Conodont during the Palaeozoic-Mesozoic Upheavals

    • 摘要:

      古-中生代之交发生了许多重要的地质事件,包括“Pangea”大陆的解体、大火成岩省的喷发、晚古生代大冰期的消逝、极端高温事件、两次生物大灭绝以及迟缓的生物复苏等.牙形石作为该时期主要的标准化石,是进行地层对比以及生物与环境协同演化研究的重要依据.近些年,此阶段的牙形石相关研究取得了许多重要的进展,这些新的材料和技术手段上的突破,为人们进行高精度的地层对比、定量重建该时期地球的生物及环境演变起到了关键作用.本文系统地对该时期全球牙形石的研究,包括牙形石的生物学、地层学以及地球化学研究等进行了总结,也提出了部分亟待解决的问题.未来,随着更多技术手段的开发以及更多基础材料的发现,将加强研究人员对该时期牙形石演化的理解,必然也会在研究这段地质历史转折与突变期的古海洋、古环境、古生物过程中发挥更大的作用.

       

    • 图  1  二叠纪-早三叠世最早期牙形石带,包括40个可全球对比的牙形石带及35个地方性牙形石带(修改自Henderson, 2016)

      Fig.  1.  Permian-Earliest Triassic conodont zonation, including 40 global-correlative conodont zones and 35 regional conodont zones (modified from Henderson, 2016)

      图  2  早三叠世国际不同地区牙形石带

      Fig.  2.  Early Triassic global conodont zonation

      图  3  国际二叠纪-三叠纪年代地层划分及界线层型“金钉子”化石研究现状

      1.菊石“金钉子”; 2.有望以牙形石作为“金钉子”; 3.已确认的金钉子; 4.牙形石“金钉子”; 界线年龄引自2021年5月国际年代地层表

      Fig.  3.  Division of Permian-Triassic international chronostratigraphic units and locations of the GSSPs

      图  4  物种x在时间和空间上的分布

      修改自Guex et al. (1991); J(x)表示该物种x在地层中出现的集合,G表示物种x的生存范围,T表示物种在地质历史中存在的时间范围

      Fig.  4.  Tempo and space distributions of species x

      图  5  二叠纪牙形石氧同位素变化曲线(修改自Chen et al., 2013a)

      Fig.  5.  Permian conodont oxygen isotopes curves (modified from Chen et al., 2013a)

      图  6  蓬莱滩、铁桥剖面牙形石氧同位素变化曲线及海平面变化(修改自Chen et al., 2011)

      Fig.  6.  Conodont oxygen isotopes curves and sea level changes of the Penglaitan and Tieqiao sections (modified from Chen et al., 2011)

      图  7  早三叠世牙形石锶同位素、海水温度、氧化还原状态及海平面变化曲线(修改自Song et al., 2015)

      Fig.  7.  Sr isotpes, temperature, redox conditions of the sea water and sea level change during the Early Triassic (modified from Song et al., 2015)

      图  8  早三叠牙形石演化过程中“返祖现象”(修改自Guex, 2016)

      Fig.  8.  "Retrograde" evolution of the conodont during the Early Triassic (modified from Guex, 2016)

      a. "Neospathodus" arcucristatus; b. Protoclarkina crofri; c. Clarkina bitteri; d. C. meishanensis; e. C. krystyni; a'. Kashmirella timorensis; b'. Paragondolella regale; c'. P. excels

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