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Volume 24 Issue 2
Apr 2013
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Journal of Earth Science  > 2013  >  24(2): 145-156.
Ito Tsuyoshi, Lei Zhang, Qinglai Feng, Matsuoka Atsushi. Guadalupian (Middle Permian) Radiolarian and Sponge Spicule Faunas from the Bancheng Formation of the Qinzhou Allochthon, South China. Journal of Earth Science, 2013, 24(2): 145-156. doi: 10.1007/s12583-013-0317-2
Citation: Ito Tsuyoshi, Lei Zhang, Qinglai Feng, Matsuoka Atsushi. Guadalupian (Middle Permian) Radiolarian and Sponge Spicule Faunas from the Bancheng Formation of the Qinzhou Allochthon, South China. Journal of Earth Science, 2013, 24(2): 145-156. doi: 10.1007/s12583-013-0317-2
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Guadalupian (Middle Permian) Radiolarian and Sponge Spicule Faunas from the Bancheng Formation of the Qinzhou Allochthon, South China

doi: 10.1007/s12583-013-0317-2
  • 1.

    State Key Laboratory for Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China

  • 2.

    Graduate School of Science and Technology, Niigata University, Niigata, 950-2181, Japan

  • 3.

    Department of Geology, Faculty of Science, Niigata University, Niigata, 950-2181, Japan

Funds:

the National Natural Science Foundation of China 40839903

the National Natural Science Foundation of China 40921062

the "111" Project B08030

the Niigata University's Scholarship Program for graduate school students conducting research abroad 

More Information
  • Corresponding author: Tsuyoshi Ito, i.t.110244@gmail.com
  • Received Date: 15 Apr 2012
  • Accepted Date: 06 Sep 2012
  • Publish Date: 01 Apr 2013
    Abstract
  • The Gujingling (古井岭) Section in Xiaodong (小董), Guangxi (广西) Zhuang Autonomous Region, China, consists of cherts and siliceous siltstones, which belongs to the Bancheng (板城) Formation of the Qinzhou (钦州) allochthon. Three successive radiolarian assemblage-zones related to the Guadalupian (Middle Permian) appear in the section in the following ascending order: Pseudoalbaillella sp. aff. Pseudoalbaillella longicornis-Pseudoalbaillella fusiformis, Follicucullus monacanthus, and Follicucullus scholasticus-Follicucullus porrectus. The radiolarian content in this section is generally greater than that of sponge spicules. The radiolarian fauna commonly consists of abundant Albaillellaria and spherical radiolaria with minor Latentifistularia and Entactinaria. The sponge fauna is composed mainly of hexactinellids with minor demosponges. These siliceous fossil faunal features, comparable with those in a deep basin of the western belt of the Phosphoria Basin in the western United States, indicate that the Bancheng Formation in the Gujingling Section was deposited in a basin deeper than 1 000 m. The siliceous siltstones in the section are characterized by inclusion of silt-sized quartz and no inclusion of sand-sized materials, suggesting that the Gujingling Section was located at least a few hundred kilometers from the South China Block in the Guadalupian.

     

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