A contiguous record of the SPICE event, sea‐level change and the first appearance of Fenghuangella laevis in Shandong Province, North China
2021; Wiley; Volume: 54; Issue: 5 Linguagem: Inglês
10.1111/let.12425
ISSN1502-3931
AutoresGuangying Ren, Fanwei Meng, Mikaela A. Pulsipher, James D. Schiffbauer, Jinliang Yuan, Yan Zhao, Ying Guo, Jian Gao, C.S. Chang,
Tópico(s)Evolution and Paleontology Studies
ResumoLethaiaVolume 54, Issue 5 p. 631-642 Original Article A contiguous record of the SPICE event, sea-level change and the first appearance of Fenghuangella laevis in Shandong Province, North China Guangying Ren, Guangying Ren gyren@lyu.edu.cn Institute of Geology and Paleontology, Linyi University, Linyi, 276000 China Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, 210008 ChinaSearch for more papers by this authorFanwei Meng, Corresponding Author Fanwei Meng fwmeng@nigpas.ac.cn Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, 210008 ChinaSearch for more papers by this authorMikaela A. Pulsipher, Mikaela A. Pulsipher mpbg6@mail.missouri.edu orcid.org/0000-0002-0992-6550 Department of Geological Sciences, University of Missouri, Columbia, Missouri, 65211 USASearch for more papers by this authorJames D. Schiffbauer, Corresponding Author James D. Schiffbauer schiffbauerj@missouri.edu orcid.org/0000-0003-4726-0355 Department of Geological Sciences, University of Missouri, Columbia, Missouri, 65211 USA X-ray Microanalysis Core, University of Missouri, Columbia, Missouri, 65211 USASearch for more papers by this authorJinliang Yuan, Jinliang Yuan yuanjl403@126.com Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, 210008 ChinaSearch for more papers by this authorYan Zhao, Yan Zhao zhaoyan@lyu.edu.cn Institute of Geology and Paleontology, Linyi University, Linyi, 276000 ChinaSearch for more papers by this authorYing Guo, Ying Guo guoying@lyu.edu.cn Institute of Geology and Paleontology, Linyi University, Linyi, 276000 ChinaSearch for more papers by this authorJian Gao, Jian Gao gaoeuler@aliyun.com Shanxi Key Laboratory of Early Life and Environment, State Key Laboratory of Continental Dynamics and Department of Geology, Northwest University, Xi'an, 710069 ChinaSearch for more papers by this authorChao Chang, Chao Chang changchao@nwu.edu.cn Shanxi Key Laboratory of Early Life and Environment, State Key Laboratory of Continental Dynamics and Department of Geology, Northwest University, Xi'an, 710069 ChinaSearch for more papers by this author Guangying Ren, Guangying Ren gyren@lyu.edu.cn Institute of Geology and Paleontology, Linyi University, Linyi, 276000 China Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, 210008 ChinaSearch for more papers by this authorFanwei Meng, Corresponding Author Fanwei Meng fwmeng@nigpas.ac.cn Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, 210008 ChinaSearch for more papers by this authorMikaela A. Pulsipher, Mikaela A. Pulsipher mpbg6@mail.missouri.edu orcid.org/0000-0002-0992-6550 Department of Geological Sciences, University of Missouri, Columbia, Missouri, 65211 USASearch for more papers by this authorJames D. Schiffbauer, Corresponding Author James D. Schiffbauer schiffbauerj@missouri.edu orcid.org/0000-0003-4726-0355 Department of Geological Sciences, University of Missouri, Columbia, Missouri, 65211 USA X-ray Microanalysis Core, University of Missouri, Columbia, Missouri, 65211 USASearch for more papers by this authorJinliang Yuan, Jinliang Yuan yuanjl403@126.com Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing, 210008 ChinaSearch for more papers by this authorYan Zhao, Yan Zhao zhaoyan@lyu.edu.cn Institute of Geology and Paleontology, Linyi University, Linyi, 276000 ChinaSearch for more papers by this authorYing Guo, Ying Guo guoying@lyu.edu.cn Institute of Geology and Paleontology, Linyi University, Linyi, 276000 ChinaSearch for more papers by this authorJian Gao, Jian Gao gaoeuler@aliyun.com Shanxi Key Laboratory of Early Life and Environment, State Key Laboratory of Continental Dynamics and Department of Geology, Northwest University, Xi'an, 710069 ChinaSearch for more papers by this authorChao Chang, Chao Chang changchao@nwu.edu.cn Shanxi Key Laboratory of Early Life and Environment, State Key Laboratory of Continental Dynamics and Department of Geology, Northwest University, Xi'an, 710069 ChinaSearch for more papers by this author First published: 10 May 2021 https://doi.org/10.1111/let.12425Read the full textAboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onFacebookTwitterLinked InRedditWechat Abstract Achieving accurate chronostratigraphical correlation between late Cambrian sections in North China and sections from elsewhere in the world has been a long-standing problem, largely owing to a lack of preserved or identified biostratigraphical marker fauna. Here, we examine trilobite occurrences, the sequence of facies and lithological change, and carbon and oxygen isotopes from the carbonate sequence of the Jiulongshan section, Shandong Province. Whereas regionally comparable sections are commonly unconformable coincident with the Kushan–Chaumitien formation boundary, we report the Steptoean Positive Isotopic Carbon Excursion (SPICE) event from an uninterrupted section recording a regressive–transgressive palaeoenvironmental fluctuation. Further, we place the onset and rise of the SPICE event within a high-resolution, trilobite biostratigraphical framework, reporting, for the first time, Fenghuangella laevis from Shandong Province. Although correlating trilobite biostratigraphical relationships from China to the rest of the world has long been burdened by the endemism of Chinese taxa, the base of the Fenghuangella biozone corresponds with the base of the globally recognized Glyptagnostus reticulatus biozone, thus better demarcating the base of the Paibian Stage in North China. Volume54, Issue5December 2021Pages 631-642 RelatedInformation
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