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Volume 32 Issue 3
Jun 2021
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Article Contents
Hanxiao Li, Miaoyan Wang, Muhui Zhang, Paul B. Wignall, Manuel Rigo, Yanlong Chen, Xianlang Wu, Zhumin Ouyang, Baojin Wu, Zhaoyang Yi, Zaitian Zhang, Xulong Lai. First Records of Late Triassic Conodont Fauna and δ13Ccarb from the Dengdengqiao Section, Dangchang County, Gansu Province, Northwestern China. Journal of Earth Science, 2021, 32(3): 646-656. doi: 10.1007/s12583-021-1428-9
Citation: Hanxiao Li, Miaoyan Wang, Muhui Zhang, Paul B. Wignall, Manuel Rigo, Yanlong Chen, Xianlang Wu, Zhumin Ouyang, Baojin Wu, Zhaoyang Yi, Zaitian Zhang, Xulong Lai. First Records of Late Triassic Conodont Fauna and δ13Ccarb from the Dengdengqiao Section, Dangchang County, Gansu Province, Northwestern China. Journal of Earth Science, 2021, 32(3): 646-656. doi: 10.1007/s12583-021-1428-9

First Records of Late Triassic Conodont Fauna and δ13Ccarb from the Dengdengqiao Section, Dangchang County, Gansu Province, Northwestern China

doi: 10.1007/s12583-021-1428-9
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  • Corresponding author: Xulong Lai, xllai@cug.edu.cn
  • Received Date: 29 Oct 2020
  • Accepted Date: 03 Feb 2021
  • Publish Date: 01 Jun 2021
  • Based on a study of 49 conodont and 57 g eochemical 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.

     

  • Electronic Supplementary Material: Supplementary material (Table S1) is available in the online version of this article at https://doi.org/10.1007/s12583-021-1428-9.
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