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GONG Yunyun, JIANG Hanlu, NI Shengli. Sedimentary characteristics of the bioherm in Cambrian Changshan Formation in Jinzhou area, Liaoning Province[J]. GEOLOGY IN CHINA, 2018, 45(6): 1271-1288. DOI: 10.12029/gc20180616
Citation: GONG Yunyun, JIANG Hanlu, NI Shengli. Sedimentary characteristics of the bioherm in Cambrian Changshan Formation in Jinzhou area, Liaoning Province[J]. GEOLOGY IN CHINA, 2018, 45(6): 1271-1288. DOI: 10.12029/gc20180616
shu

Sedimentary characteristics of the bioherm in Cambrian Changshan Formation in Jinzhou area, Liaoning Province

  • School of Earth Resources and Sciences, China University of Geosciences, Beijing 100083, China

Funds: 

China Geological Survey Program 1212011121268

National Natural Science Foundation of China 41472090

National Natural Science Foundation of China 40472065

More Information
  • Author Bio:

    GONG Yunyun, female, born in 1989, doctor, mainly engages in the study of sedimentology and stratigraphy; E-mail:yunyungong@sina.com

  • Received Date: September 24, 2016
  • Revised Date: February 18, 2017
  • Available Online: September 25, 2023
    Graphical Abstract
    • Abstract

  • A bioherm 15m in thickness is exposed at the top of Cambrian Changshan Formation in Jinzhou area, Liaoning Province. Macroscopically, the bioherm is made up of thrombolite and leiolite, and microscopically, it is mainly composed of dense micrites and different kinds of grains. There are different types of grains, such as calcified microbes, benthic oolites, oncolites, bioclasts and clots, in the inner part of the bioherm, which indicates complex microfabric of the bioherm. The surface of trilobite skeletal clastics encrusted by micrites shows constructive and destructive micritization. Bioclasts dispersedly distributed within the dense micrite reflect relatively strong binding during the development of the bioherm. Large quantities of pyrite crystals existent in the dense micrites demonstrate that the formation of dense micrite was genetically related to heterotrophy-bacteria activities. Together with pyrite crystals, all kinds of grains within the bioherm reflect complex microbial activities during the formation of the bioherm, which provides not only prerequisite for the study of microbial sedimentation but also an important example and clue for the research on different types of grains within the bioherm.

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    • References (87)
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