A volcanic tuff near the Carboniferous–Permian boundary, Taiyuan Formation, North China: Radioisotopic dating and global correlation
A 66 cm thick volcanic ash fall tuff occurring within a thick coal deposit and containing a paleobotanical fossil lagerstätte in the Wuda coal district of North China has been dated as 298.34 ± 0.09 Ma. The fossil flora in the tuff indicates a latest Carboniferous to earliest Permian age and is thus...
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| Published in | Review of palaeobotany and palynology Vol. 294; p. 104244 |
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| Main Authors | , , , |
| Format | Journal Article |
| Language | English |
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Elsevier B.V
01.11.2021
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| Abstract | A 66 cm thick volcanic ash fall tuff occurring within a thick coal deposit and containing a paleobotanical fossil lagerstätte in the Wuda coal district of North China has been dated as 298.34 ± 0.09 Ma. The fossil flora in the tuff indicates a latest Carboniferous to earliest Permian age and is thus in agreement with the radioisotopic age of earliest Permian, Asselian, age. This bed supplies a well-defined position of the Carboniferous–Permian boundary near the northern edge of the North China Block. The tuff occurs in the top of the Taiyuan Formation and several meters below the base of the Shansi (=Shanxi) Formation. These beds were traditionally considered late Carboniferous to early Permian in age. Our results demonstrate that the Taiyuan Formation is time transgressive and its age has to be revised for the northern part of the North China Block.
•The tuff yielding the Permian “vegetational Pompeii” is dated as 298.34 ± 0.09 Ma.•The Taiyuan Formation in North China is time transgressive.•The Permo-Carboniferous boundary in North China can be well constrained now. |
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| AbstractList | A 66 cm thick volcanic ash fall tuff occurring within a thick coal deposit and containing a paleobotanical fossil lagerstätte in the Wuda coal district of North China has been dated as 298.34 ± 0.09 Ma. The fossil flora in the tuff indicates a latest Carboniferous to earliest Permian age and is thus in agreement with the radioisotopic age of earliest Permian, Asselian, age. This bed supplies a well-defined position of the Carboniferous–Permian boundary near the northern edge of the North China Block. The tuff occurs in the top of the Taiyuan Formation and several meters below the base of the Shansi (=Shanxi) Formation. These beds were traditionally considered late Carboniferous to early Permian in age. Our results demonstrate that the Taiyuan Formation is time transgressive and its age has to be revised for the northern part of the North China Block. A 66 cm thick volcanic ash fall tuff occurring within a thick coal deposit and containing a paleobotanical fossil lagerstätte in the Wuda coal district of North China has been dated as 298.34 ± 0.09 Ma. The fossil flora in the tuff indicates a latest Carboniferous to earliest Permian age and is thus in agreement with the radioisotopic age of earliest Permian, Asselian, age. This bed supplies a well-defined position of the Carboniferous–Permian boundary near the northern edge of the North China Block. The tuff occurs in the top of the Taiyuan Formation and several meters below the base of the Shansi (=Shanxi) Formation. These beds were traditionally considered late Carboniferous to early Permian in age. Our results demonstrate that the Taiyuan Formation is time transgressive and its age has to be revised for the northern part of the North China Block. •The tuff yielding the Permian “vegetational Pompeii” is dated as 298.34 ± 0.09 Ma.•The Taiyuan Formation in North China is time transgressive.•The Permo-Carboniferous boundary in North China can be well constrained now. |
| ArticleNumber | 104244 |
| Author | Shen, Shu-Zhong Schmitz, Mark D. Wang, Jun Pfefferkorn, Hermann W. |
| Author_xml | – sequence: 1 givenname: Mark D. surname: Schmitz fullname: Schmitz, Mark D. email: markschmitz@boisestate.edu organization: Department of Geosciences, Boise State University, 1910 University Drive, Boise, ID 83725, USA – sequence: 2 givenname: Hermann W. surname: Pfefferkorn fullname: Pfefferkorn, Hermann W. email: hpfeffer@sas.upenn.edu organization: Department of Earth and Environmental Sciences, University of Pennsylvania, Philadelphia, PA 19104-6316, USA – sequence: 3 givenname: Shu-Zhong surname: Shen fullname: Shen, Shu-Zhong email: szshen@nju.edu.cn organization: School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China – sequence: 4 givenname: Jun surname: Wang fullname: Wang, Jun email: jun.wang@nigpas.ac.cn organization: State Key Laboratory of Palaeobiology & Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, No. 39 East Beijing Road, Nanjing 210008, China |
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| SubjectTerms | Asselian age Biostratigraphy Carboniferous period Carboniferous–Permian boundary China coal flora fossils paleobotany Plant fossils Radioisotopic dating Taiyuan Formation tuff volcanic ash |
| Title | A volcanic tuff near the Carboniferous–Permian boundary, Taiyuan Formation, North China: Radioisotopic dating and global correlation |
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