Chitinozoans from the Telychian (Llandovery, Silurian) Shenxuanyi Member, upper Ningqiang Formation of the northwestern Yangtze Platform, China

Abstract Silurian strata are well-developed in the northwest margin of Yangtze Platform. A total of 117 densely spaced argillaceous samples were taken from the Shenxuanyi Member, upper Ningqiang Formation to the lowermost Chejiaba Formation of the Majia section in northern Sichuan Province. The main...

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Main Authors: Yangui Li, Chunbo Yan, Chuanshang Wang, Jörg Maletz, Yan Liang, Huazhou Yao, Haizhi Wu, Weixiong Chen, Jingqing Cheng, Zichen Fang, Xiaofeng Wang
Format: Article
Language:English
Published: SpringerOpen 2025-04-01
Series:Swiss Journal of Palaeontology
Subjects:
Online Access:https://doi.org/10.1186/s13358-025-00364-7
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author Yangui Li
Chunbo Yan
Chuanshang Wang
Jörg Maletz
Yan Liang
Huazhou Yao
Haizhi Wu
Weixiong Chen
Jingqing Cheng
Zichen Fang
Xiaofeng Wang
author_facet Yangui Li
Chunbo Yan
Chuanshang Wang
Jörg Maletz
Yan Liang
Huazhou Yao
Haizhi Wu
Weixiong Chen
Jingqing Cheng
Zichen Fang
Xiaofeng Wang
author_sort Yangui Li
collection DOAJ
description Abstract Silurian strata are well-developed in the northwest margin of Yangtze Platform. A total of 117 densely spaced argillaceous samples were taken from the Shenxuanyi Member, upper Ningqiang Formation to the lowermost Chejiaba Formation of the Majia section in northern Sichuan Province. The main aim of this study is to obtain chitinozoans to test whether Wenlock deposits are preserved here. A highly diverse and abundant chitinozoan assemblage is documented, including 21 species from six genera. This assemblage was then compared to contemporaneous chitinozoan assemblages reported from adjacent areas. This study proposes that Eisenackitina venusta (corresponds to the Pterospathodus celloni conodont Biozone) is of chronostratigraphical significance for discussing the Telychian of the Yangtze region. It is suggested that the Silurian upper red bed (lower part of the Shenxuanyi Member) in the study area is younger than the Xiushan Formation and can be correlated with the Huixingshao Formation of the Central Yangtze Platform. There are no index chitinozoan species near the Llandovery–Wenlock boundary that have been found in the upper part of the Shenxuanyi Member, and the updated chronostratigraphic framework suggests that it is Telychian-aged deposits.
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spelling doaj-art-02e92e34026644d585f16b652cec1bc32025-08-20T02:11:11ZengSpringerOpenSwiss Journal of Palaeontology1664-23761664-23842025-04-01144113310.1186/s13358-025-00364-7Chitinozoans from the Telychian (Llandovery, Silurian) Shenxuanyi Member, upper Ningqiang Formation of the northwestern Yangtze Platform, ChinaYangui Li0Chunbo Yan1Chuanshang Wang2Jörg Maletz3Yan Liang4Huazhou Yao5Haizhi Wu6Weixiong Chen7Jingqing Cheng8Zichen Fang9Xiaofeng Wang10College of Mining Engineering, Guizhou University of Engineering ScienceHubei Key Laboratory of Paleontology and Environmental Change, Wuhan Center of China Geological SurveyHubei Key Laboratory of Paleontology and Environmental Change, Wuhan Center of China Geological SurveyDepartment of Geosciences, FU BerlinState Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of SciencesHubei Key Laboratory of Paleontology and Environmental Change, Wuhan Center of China Geological SurveyCollege of Mining Engineering, Guizhou University of Engineering ScienceFoshan Geological Bureau of Guangdong Province, Guangdong GeologyHubei Center of Geological Disaster Control, Hubei Geological BureauHubei Key Laboratory of Paleontology and Environmental Change, Wuhan Center of China Geological SurveyHubei Key Laboratory of Paleontology and Environmental Change, Wuhan Center of China Geological SurveyAbstract Silurian strata are well-developed in the northwest margin of Yangtze Platform. A total of 117 densely spaced argillaceous samples were taken from the Shenxuanyi Member, upper Ningqiang Formation to the lowermost Chejiaba Formation of the Majia section in northern Sichuan Province. The main aim of this study is to obtain chitinozoans to test whether Wenlock deposits are preserved here. A highly diverse and abundant chitinozoan assemblage is documented, including 21 species from six genera. This assemblage was then compared to contemporaneous chitinozoan assemblages reported from adjacent areas. This study proposes that Eisenackitina venusta (corresponds to the Pterospathodus celloni conodont Biozone) is of chronostratigraphical significance for discussing the Telychian of the Yangtze region. It is suggested that the Silurian upper red bed (lower part of the Shenxuanyi Member) in the study area is younger than the Xiushan Formation and can be correlated with the Huixingshao Formation of the Central Yangtze Platform. There are no index chitinozoan species near the Llandovery–Wenlock boundary that have been found in the upper part of the Shenxuanyi Member, and the updated chronostratigraphic framework suggests that it is Telychian-aged deposits.https://doi.org/10.1186/s13358-025-00364-7Guangyuan CityNorthern Sichuan ProvinceBiostratigraphyLlandovery/Wenlock boundarySilurian upper red bed
spellingShingle Yangui Li
Chunbo Yan
Chuanshang Wang
Jörg Maletz
Yan Liang
Huazhou Yao
Haizhi Wu
Weixiong Chen
Jingqing Cheng
Zichen Fang
Xiaofeng Wang
Chitinozoans from the Telychian (Llandovery, Silurian) Shenxuanyi Member, upper Ningqiang Formation of the northwestern Yangtze Platform, China
Swiss Journal of Palaeontology
Guangyuan City
Northern Sichuan Province
Biostratigraphy
Llandovery/Wenlock boundary
Silurian upper red bed
title Chitinozoans from the Telychian (Llandovery, Silurian) Shenxuanyi Member, upper Ningqiang Formation of the northwestern Yangtze Platform, China
title_full Chitinozoans from the Telychian (Llandovery, Silurian) Shenxuanyi Member, upper Ningqiang Formation of the northwestern Yangtze Platform, China
title_fullStr Chitinozoans from the Telychian (Llandovery, Silurian) Shenxuanyi Member, upper Ningqiang Formation of the northwestern Yangtze Platform, China
title_full_unstemmed Chitinozoans from the Telychian (Llandovery, Silurian) Shenxuanyi Member, upper Ningqiang Formation of the northwestern Yangtze Platform, China
title_short Chitinozoans from the Telychian (Llandovery, Silurian) Shenxuanyi Member, upper Ningqiang Formation of the northwestern Yangtze Platform, China
title_sort chitinozoans from the telychian llandovery silurian shenxuanyi member upper ningqiang formation of the northwestern yangtze platform china
topic Guangyuan City
Northern Sichuan Province
Biostratigraphy
Llandovery/Wenlock boundary
Silurian upper red bed
url https://doi.org/10.1186/s13358-025-00364-7
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