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Chinese Science Bulletin 2009年第6期54卷 1058-1064页

作者： liu pengju yin chongyu gao linzhi tang feng chen shouming Institute of Geology Chinese Academy of Geological Sciences Beijing 100037 China

The Zhangcunping area is located at the north limb of the Huangling anticline in Yichang, Hubei Prov-ince. Here, the sedimentary succession of the Ediacaran Doushantuo Formation is similar with that in the Weng'an area, Guizhou Province. A large number of new microfossils (mainly acanthoacritarchs) from the Doushantuo Formation in this area are reported in this paper. The fossil assemblage shows similarity as the phosphatized biota of the Doushantuo Formation at Weng'an, Guizhou Province and the silicified biota of the Doushantuo Formation at the Yangtze Gorges, which suggests that the Zhangcunping area is a key for correlation of the Doushantuo Formation between the Weng'an area, Guizhou Province and the Yangtze Gorges. Besides, a new zircon SHRIMP U-Pb age (614.0±7.6 Ma) is first obtained from a horizon underneath the exposed surface in the middle of the Doushantuo Forma-tion in the Zhangcunping area. This age not only provides a new datum for subdivision of the Ediacaran Doushantuo Formation, but also indicates that the age of the exposed surface in the middle of the Doushantuo Formation in the Yangtze Platform should be posterior to 614.0±7.6 Ma. Due to the horizon of the Weng'an biota situated above the exposed surface, the age of the Weng'an biota should be pos-terior to 614.0±7.6 Ma as well.

关键词：锆石SHRIMP 陡山沱组微体化石湖北省年龄迪卡宜昌 Pb

Acanthomorph Biostratigraphic Succession of the Ediacaran Doushantuo Formation in the East Yangtze Gorges,South China

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Acta Geologica Sinica(English Edition) 2011年第2期85卷 283-295页

作者： yin chongyu liu pengju Stanley M. AWRAMIK chen shouming tang feng gao linzhi WANG Ziqiang Leigh A. RIEDMAN Institute of Geology Chinese Academy of Geological Sciences Beijing 100037 China Department of Earth Science University of California Santa Barbara CA 93106 USA School of Earth Sciences and Resources China University of Geosciences Beijing 100083 China

Large acanthomorphic acritarchs have been found in chert of the Ediacaran Doushantuo Formation at several localities in South China, including the East Yangtze Gorges of Hubei Province,Weng＇an area of Guizhou Province, and elsewhere. However, their potential for biostratigraphic subdivision and correlation of Ediacaran successions is limited by facies control, taphonomic biases,and taxonomic problems. In the Yangtze Gorges, the Doushantuo Formation is generally subdivided into four lithologic members. However, in the Weng＇an area, the Doushantuo Formation comprises just a lower and upper part separated by a mid-Doushantuo erosional surface. In the Yangtze Gorges at the Zhangcunping section, the Doushantuo succession is similar to that at Weng＇an. So far, the correlation between the Yangtze Gorges and Weng＇an area, and elsewhere has been an issue of debate. To resolvethe debate, we selected eight sections in the Yangtze Gorges area and systemically sampled chert nodules of the Doushantuo Formation, focusing in particular on the upper Doushantuo Formation. Our data confirm two different assemblages appearing separately in the second and third members, which are separated by a negative δ13C excursion （EN2）. The lower assemblage is characterized by Tianzhushania and a diverse suite of large acanthomorphic acritarchs. The upper assemblage is distinguished from the lower assemblage, by （1） absence of Tianzhushania; （2） occurrence of abundant,100-150 μm, smooth-walled spherical microfossils; （3） occurrence of highly diverse acanthomorphic acritarchs including species extending from the second member and new forms in this member; （4）occurrence of unnamed new forms of protist; and （5） occurrence of the tubular microfossil Sinocyclocylicus guizhouensis. Since the Tianzhushania-dominated assemblage is not present in Australia, it seems that only the upper acanthomorph assemblage is present and thus the lower Doushantuo acanthomorph assemblage is missing in Australia.

关键词： Acanthomorph biostratigraphic succession Ediacaran Doushantuo Formation the Yangtze Gorges South China

华南峡东地区埃迪卡拉(震旦)纪年代地层划分初探

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地质学报 2012年第6期86卷 849-866页

作者：刘鹏举尹崇玉陈寿铭李猛高林志唐烽中国地质科学院地质研究所国土资源部地层学与古生物学重点实验室北京100037

华南峡东地区埃迪卡拉纪地层连续,出露完整,化石丰富,顶、底界线清楚,是世界上同时代地层最具代表性的序列之一,也是解决埃迪卡拉纪年代地层划分、竞争相关界线层型剖面的最理想地区之一。根据近年来峡东地区埃迪卡拉系的同位素年代学... 详细信息

华南峡东地区埃迪卡拉纪地层连续,出露完整,化石丰富,顶、底界线清楚,是世界上同时代地层最具代表性的序列之一,也是解决埃迪卡拉纪年代地层划分、竞争相关界线层型剖面的最理想地区之一。根据近年来峡东地区埃迪卡拉系的同位素年代学、生物地层学和化学地层学等方面的研究积累,本文以生物地层序列(生物演化阶段)为基础标志,以碳稳定同位素组成的重要变化界面为辅助标志,对峡东地区埃迪卡拉纪地层进行年代地层的划分,提出2统5阶方案。下统名称建议用峡东统,下分九龙湾阶和陈家园子阶;上统名称建议用扬子统,下分吊崖坡阶、第四阶和第五阶。在此基础上,根据生物地层和碳稳定同位素地层学的特征,初步探讨了与其他地区埃迪卡拉系的对比关系。这一划分和对比方案只是目前研究的阶段性认识,更完整的划分对比意见还有待今后的进一步完善。

关键词：华南地区峡东地区埃迪卡拉纪震旦纪年代地层

湖北宜昌樟村坪埃迪卡拉系陡山沱组硅磷质结核中的微体化石

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地质学报 2010年第1期84卷 70-77页

作者：陈寿铭尹崇玉刘鹏举高林志唐烽王自强中国地质科学院地质研究所北京100037 中国地质大学北京100083

本文报道的微体化石产于湖北宜昌樟村坪万家沟剖面埃迪卡拉纪陡山沱组第10层的硅磷质结核中,化石组合包括疑源类Appendisphaera grandis、Ericiasphaera spjeldnaesii、Knollisphaeridium maxi mum、Leiosphaeridia tenuissi ma、Meghystrichosphaeridium perfectum、Tianzhushania polysiphonia、***、***;丝状蓝藻Oscillatoriopsis obtusa、Polytrichoides induviatus、***、Salome hubeiensis、Siphonophycustypicum;多细胞藻类Sarcinophycus palilloformis、Wengania minuta。该微体化石组合面貌与黄陵背斜东、南翼陡山沱组二段硅质结核中以大型具刺疑源类Tianzhushania为特征的组合相同,与贵州瓮安地区陡山沱组上磷块岩下部保存的微体化石组合面貌基本一致。

关键词：宜昌埃迪卡拉系陡山沱组微体化石

华北克拉通东部新元古代宏体化石生物地层序列

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地质论评 2009年第3期55卷 305-317页

作者：唐烽尹崇玉高林志刘鹏举王自强陈寿铭中国地质科学院地质研究所北京100037 中国地质科学院地层学及古生物学重点实验室北京100037 中国地质大学地球科学与资源学院北京100083

华北克拉通东部是中国晚前寒武纪地层出露最为完整、连续的地区,特别是华北克拉通东缘连续出露了新元古代自老至新的全部地层,是对比和衔接中国南、北方晚前寒武纪地层的关键地区。在该地区所发现和建立的宏体化石群——"龙凤山生物群"... 详细信息

华北克拉通东部是中国晚前寒武纪地层出露最为完整、连续的地区,特别是华北克拉通东缘连续出露了新元古代自老至新的全部地层,是对比和衔接中国南、北方晚前寒武纪地层的关键地区。在该地区所发现和建立的宏体化石群——"龙凤山生物群"、"辽南生物群"和"淮南生物群"可能是新元古代"南华大冰期"前后较为独特的生物群落,其中相当部分可能归属于多细胞后生动物和多细胞藻类,是地球早期生命景观的重要代表。因此,对这些新元古代早期生物群的研究将可能揭示比陡山沱期更早的多细胞后生动植物的演化面貌,在演化生物学上意义重大。近年来,在地调项目的资助下,开展了华北克拉通东部地区的新元古代年代地层及生物地层的研究。本文综合现有资料,详细记述了华北克拉通东部(燕山地区和辽南、徐淮地区)含宏体化石的新元古代地层及其宏体化石特征、组合面貌和生物地层序列。同时,依据宏体化石记录,探讨了中国新元古代地层的对比问题。

关键词：华北克拉通东部新元古代宏体化石生物地层序列地层对比