全球古-中生代之交牙形石研究进展  

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

作　　者：吴奎 童金南 李红军 田力 邹亚锐 梁蕾 赵璧 Wu Kui;Tong Jinnan;Li Hongjun;Tian Li;Zou Yarui;Liang Lei;Zhao Bi(Hubei Institute of Geosciences,Wuhan 430034,China;State Key Laboratory of Biogeology and Environmental Geology,School of Earth Sciences,China University of Geosciences,Wuhan 430074,China;Hubei Key Laboratory for Paleontology and Geological Environment Evolution,Wuhan Center of China Geological Survey,Wuhan 430205,China;Institute of Paleontology,Hebei GEO University,Shijiazhuang 050031,China)

机构地区：[1]湖北省地质科学研究院,湖北武汉430034 [2]中国地质大学地球科学学院,生物地质与环境地质国家重点实验室,湖北武汉430074 [3]中国地质调查局武汉地质调查中心古生物与地质环境演化湖北省重点实验室,湖北武汉430205 [4]河北地质大学古生物研究院,河北石家庄050031

出　　处：《地球科学》2022年第3期1012-1037,共26页Earth Science

基　　金：国家自然科学基金项目(Nos.42030513,41530104,41661134047,41602024,42102011);湖北省自然科学基金项目(No.2021CFB276);湖北省地质局专项(Nos.KJ2019-01,KJ2021-3);河北省自然科学基金青年项目(No.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(No.PEL-202104)。

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.Numerous geological events took place during the Palaeozoic-Mesozoic upheavals, including breakup of the Pangea supercontinent, eruptions of large igneous provinces, ending of the Late Paleozoic Ice Age, extremely hot temperatures, two mass extinctions, and delayed ecosystem recovery. As the main index fossil of this interval, conodont is an important basis for stratigraphic correlation and the co-evolution history of organisms and the environment. In recent years, significant progress has been achieved through the study of Permian and Early Triassic conodonts and its related researches, which plays an important role in understanding the biotic and environment evolutions. The researches about Permian and Early Triassic conodonts have been summarized in this paper, including conodont biology, stratigraphy, and geochemistry. Moreover, some issues which have remained being overlooked or un-solved are also presented. In the future, the development of more technical approaches and the discoveries of more basic materials would be favored for more deep studies on the evolution of the conodont during this interval, which will further play an indispensable role in paleo-oceanic, paleo-environmental and paleontological studies during this transitional and mutational geologic history.

关 键 词：牙形石 晚二叠世 早三叠世 古环境 生物地层 地层学 

分 类 号：P52[天文地球—古生物学与地层学]