First Records of Late Triassic Conodont Fauna and δ13Ccarb from the Dengdengqiao Section, Dangchang County, Gansu Province, Northwestern China
Based on a study of 49 conodont and 57 geochemical samples from the Upper Triassic, carbonate-dominated Dengdengqiao Formation, Qinling Basin, China, the Carnian conodonts and carbon isotope records are first reported. Two genera and four species have been identified amongst 87 conodont elements: Mo...
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Abstract | Based on a study of 49 conodont and 57 geochemical samples from the Upper Triassic, carbonate-dominated Dengdengqiao Formation, Qinling Basin, China, the Carnian conodonts and carbon isotope records are first reported. Two genera and four species have been identified amongst 87 conodont elements:
Mosherella praebudaensis
,
Mo. longnanensis
sp. nov.,
Mo.
sp., and “
Misikella” longidentata
. The presence of
Mo. praebudaensis
indicates that the lower part (bed 2) of the formation is attributable to the Julian (lower Carnian) substage. A radiolarian fauna identified in a previous study belongs to the upper Carnian, but the sampling horizon is unclear. The δ
13
C
carb
curve shows a ∼1.8‰ negative excursion beginning from upper part of bed 3, but its stratigraphic location is uncertain. The Dengdengqiao Formation is clearly at least partly of Carnian age but could include younger strata. The abundant calcareous algae at the section is probably due to some transport rather than preserved in site. The unusual ecosystem with rare marine organisms may reflect long-term stressful and unfavorable conditions at Dengdengqiao. |
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AbstractList | Based on a study of 49 conodont and 57 geochemical samples from the Upper Triassic, carbonate-dominated Dengdengqiao Formation, Qinling Basin, China, the Carnian conodonts and carbon isotope records are first reported. Two genera and four species have been identified amongst 87 conodont elements:
Mosherella praebudaensis
,
Mo. longnanensis
sp. nov.,
Mo.
sp., and “
Misikella” longidentata
. The presence of
Mo. praebudaensis
indicates that the lower part (bed 2) of the formation is attributable to the Julian (lower Carnian) substage. A radiolarian fauna identified in a previous study belongs to the upper Carnian, but the sampling horizon is unclear. The δ
13
C
carb
curve shows a ∼1.8‰ negative excursion beginning from upper part of bed 3, but its stratigraphic location is uncertain. The Dengdengqiao Formation is clearly at least partly of Carnian age but could include younger strata. The abundant calcareous algae at the section is probably due to some transport rather than preserved in site. The unusual ecosystem with rare marine organisms may reflect long-term stressful and unfavorable conditions at Dengdengqiao. Based on a study of 49 conodont and 57 geochemical samples from the Upper Triassic, carbonate-dominated Dengdengqiao Formation, Qinling Basin, China, the Carnian conodonts and carbon isotope records are first reported. Two genera and four species have been identified amongst 87 conodont elements: Mosherella praebudaensis, Mo. longnanensis sp. nov., Mo. sp., and “Misikella” longidentata. The presence of Mo. praebudaensis indicates that the lower part (bed 2) of the formation is attributable to the Julian (lower Carnian) substage. A radiolarian fauna identified in a previous study belongs to the upper Carnian, but the sampling horizon is unclear. The δ13Ccarb curve shows a ∼1.8‰ negative excursion beginning from upper part of bed 3, but its stratigraphic location is uncertain. The Dengdengqiao Formation is clearly at least partly of Carnian age but could include younger strata. The abundant calcareous algae at the section is probably due to some transport rather than preserved in site. The unusual ecosystem with rare marine organisms may reflect long-term stressful and unfavorable conditions at Dengdengqiao. Based on a study of 49 conodont and 57 geochemical samples from the Upper Triassic, carbonate-dominated Dengdengqiao Formation, Qinling Basin, China, the Carnian conodonts and carbon isotope records are first reported. Two genera and four species have been identified amongst 87 conodont elements: Mosherella praebudaensis, Mo. longnanensis sp. nov., Mo. sp., and "Misikella" longidentata. The presence of Mo. praebudaensis indicates that the lower part (bed 2) of the formation is attributable to the Julian (lower Carnian) substage. A radiolarian fauna identified in a previous study belongs to the upper Carnian, but the sampling horizon is unclear. The δ13Ccarb curve shows a ~1.8‰ negative excursion beginning from upper part of bed 3, but its stratigraphic location is uncertain. The Dengdengqiao Formation is clearly at least partly of Carnian age but could include younger strata. The abundant calcareous algae at the section is probably due to some transport rather than preserved in site. The unusual ecosystem with rare marine organisms may reflect long-term stressful and unfavorable conditions at Dengdengqiao. |
Author | Wu, Xianlang Rigo, Manuel Lai, Xulong Wu, Baojin Zhang, Muhui Zhang, Zaitian Yi, Zhaoyang Li, Hanxiao Chen, Yanlong Wignall, Paul B. Wang, Miaoyan Ouyang, Zhumin |
AuthorAffiliation | School of Earth Sciences, China University of Geosciences, Wuhan 430074, China%School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China%School of Earth Sciences, China University of Geosciences, Wuhan 430074, China;State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China%School of Earth and Environment, University of Leeds, Leeds LS29JT, UK%Department of Geosciences, University of Padova, Via Gradenigo 6, 35131, Padova, Italy%Shaanxi Key Laboratory of Early Life and Environments, State Key Laboratory of Continental Dynamics and Department of Geology, Northwest University, Xi'an 710069, China%Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China%Wuhan Center of Geological Survey, Wuhan 430205, China;State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Acade |
AuthorAffiliation_xml | – name: School of Earth Sciences, China University of Geosciences, Wuhan 430074, China%School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China%School of Earth Sciences, China University of Geosciences, Wuhan 430074, China;State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China%School of Earth and Environment, University of Leeds, Leeds LS29JT, UK%Department of Geosciences, University of Padova, Via Gradenigo 6, 35131, Padova, Italy%Shaanxi Key Laboratory of Early Life and Environments, State Key Laboratory of Continental Dynamics and Department of Geology, Northwest University, Xi'an 710069, China%Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China%Wuhan Center of Geological Survey, Wuhan 430205, China;State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China |
Author_xml | – sequence: 1 givenname: Hanxiao orcidid: 0000-0001-6774-0618 surname: Li fullname: Li, Hanxiao organization: School of Earth Sciences, China University of Geosciences – sequence: 2 givenname: Miaoyan surname: Wang fullname: Wang, Miaoyan organization: School of Earth Sciences and Resources, China University of Geosciences – sequence: 3 givenname: Muhui surname: Zhang fullname: Zhang, Muhui organization: School of Earth Sciences, China University of Geosciences, State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences – sequence: 4 givenname: Paul B. surname: Wignall fullname: Wignall, Paul B. organization: School of Earth and Environment, University of Leeds – sequence: 5 givenname: Manuel surname: Rigo fullname: Rigo, Manuel organization: Department of Geosciences, University of Padova – sequence: 6 givenname: Yanlong surname: Chen fullname: Chen, Yanlong organization: Shaanxi Key Laboratory of Early Life and Environments, State Key Laboratory of Continental Dynamics and Department of Geology, Northwest University – sequence: 7 givenname: Xianlang surname: Wu fullname: Wu, Xianlang organization: School of Earth Sciences, China University of Geosciences – sequence: 8 givenname: Zhumin surname: Ouyang fullname: Ouyang, Zhumin organization: School of Earth Sciences, China University of Geosciences – sequence: 9 givenname: Baojin surname: Wu fullname: Wu, Baojin organization: School of Earth Sciences, China University of Geosciences – sequence: 10 givenname: Zhaoyang surname: Yi fullname: Yi, Zhaoyang organization: Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University – sequence: 11 givenname: Zaitian surname: Zhang fullname: Zhang, Zaitian organization: Wuhan Center of Geological Survey, State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences – sequence: 12 givenname: Xulong orcidid: 0000-0002-2837-0885 surname: Lai fullname: Lai, Xulong email: xllai@cug.edu.cn organization: School of Earth Sciences, China University of Geosciences, State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences |
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Copyright | China University of Geosciences (Wuhan) and Springer-Verlag GmbH Germany, Part of Springer Nature 2021 China University of Geosciences (Wuhan) and Springer-Verlag GmbH Germany, Part of Springer Nature 2021. Copyright © Wanfang Data Co. Ltd. All Rights Reserved. |
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Keywords | Late Triassic Qinling conodonts Julian |
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PublicationYear | 2021 |
Publisher | China University of Geosciences Springer Nature B.V School of Earth Sciences, China University of Geosciences, Wuhan 430074, China%School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China%School of Earth Sciences, China University of Geosciences, Wuhan 430074, China State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China%School of Earth and Environment, University of Leeds, Leeds LS29JT, UK%Department of Geosciences, University of Padova, Via Gradenigo 6, 35131, Padova, Italy%Shaanxi Key Laboratory of Early Life and Environments, State Key Laboratory of Continental Dynamics and Department of Geology, Northwest University, Xi'an 710069, China%Key Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking University, Beijing 100871, China%Wuhan Center of Geological Survey, Wuhan 430205, China |
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Snippet | Based on a study of 49 conodont and 57 geochemical samples from the Upper Triassic, carbonate-dominated Dengdengqiao Formation, Qinling Basin, China, the... |
SourceID | wanfang proquest crossref springer |
SourceType | Aggregation Database Publisher |
StartPage | 646 |
SubjectTerms | Algae Biogeosciences Carbon isotopes Carbonates Earth and Environmental Science Earth Sciences Fauna Geochemistry Geology Geotechnical Engineering & Applied Earth Sciences Identification Marine ecosystems Marine organisms New records New species Records Stratigraphy Triassic |
Title | First Records of Late Triassic Conodont Fauna and δ13Ccarb from the Dengdengqiao Section, Dangchang County, Gansu Province, Northwestern China |
URI | https://link.springer.com/article/10.1007/s12583-021-1428-9 https://www.proquest.com/docview/2537294493 https://d.wanfangdata.com.cn/periodical/dqkx-e202103013 |
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