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Sponge spicules in phosphorites of the Early Cambrian Gezhongwu Formation, Zhijin, Guizhou
引用本文:YANG Ruidong,QIAN Yi,ZHANG Jie,ZHANG Weihu,JIANG Lijun,GAO Hui. Sponge spicules in phosphorites of the Early Cambrian Gezhongwu Formation, Zhijin, Guizhou[J]. 自然科学进展(英文版), 2004, 14(10): 896-902. DOI: 10.1080/10020070412331344521
作者姓名:YANG Ruidong  QIAN Yi  ZHANG Jie  ZHANG Weihu  JIANG Lijun  GAO Hui
作者单位:Guizhou University of Technology, Guiyang 550003, China,Institute of Geology and Paleontology, Chinese Academy of Sciences, Nanjing 210008, China,Guizhou University of Technology, Guiyang 550003, China,Guizhou University of Technology, Guiyang 550003, China,Guizhou University of Technology, Guiyang 550003, China,Guizhou University of Technology, Guiyang 550003, China
基金项目:国家重点研究项目,科技部资助项目,国家自然科学基金,中国博士后科学基金
摘    要:Phosphorites occurring at the bottom of the Cambrian system contain abundant small shelly fossils, which are the product of the first episode of life explosion in the Cambrian. It was previously reported that the small shelly fossils are dominated by hyolithids, olivooids, zhijinitids, conodontomorphs, yubelichitids, camenitids and algae, with minor amounts of sponge fossils. Large amounts of sponge spicules, diverse in form, have been found for the first time in the Gezhongwu Formation phosphorites at Shixing, Zhijin County, Guizhou Province, of which such spicules as diaxon-triactins, diaxon-tetractins, pentaxon-pentactins and hexon-hexactins account for 30%. These spicules constitute the sponge clastic phosphorites made up of sponge clastics. Meanwhile, it is also expected that the radiation and diversity of sponge animals started as early as in the earliest Early Cambrian. Habit and burying environment of sponge animal are discussed in the paper.

关 键 词:sponge animal   Gezhongwu Formation   Early Cambrian   Guizhou

Sponge spicules in phosphorites of the Early Cambrian Gezhongwu Formation, Zhijin, Guizhou
YANG Ruidong,QIAN Yi,ZHANG Jie,ZHANG Weihua,JIANG Lijun,GAO Hui. Sponge spicules in phosphorites of the Early Cambrian Gezhongwu Formation, Zhijin, Guizhou[J]. Progress in Natural Science, 2004, 14(10): 896-902. DOI: 10.1080/10020070412331344521
Authors:YANG Ruidong  QIAN Yi  ZHANG Jie  ZHANG Weihua  JIANG Lijun  GAO Hui
Affiliation:1. Guizhou University of Technology, Guiyang 550003, China
2. Institute of Geology and Paleontology, Chinese Academy of Sciences, Nanjing 210008, China
Abstract:Phosphorites occurring at the bottom of the Cambrian system contain abundant small shelly fossils, which are the product of the first episode of life explosion in the Cambrian. It was previously reported that the small shelly fossils are dominated by hyolithids, olivooids, zhijinitids, conodontomorphs, yubelichitids, camenitids and algae, with minor amounts of sponge fossils. Large amounts of sponge spicules, diverse in form, have been found for the first time in the Gezhongwu Formation phosphorites at Shixing, Zhijin County, Guizhou Province, of which such spicules as diaxon-triactins, diaxon-tetractins, pentaxon-pentactins and hexon-hexactins account for 30%. These spicules constitute the sponge clastic phosphorites made up of sponge clastics. Meanwhile, it is also expected that the radiation and diversity of sponge animals started as early as in the earliest Early Cambrian. Habit and burying environment of sponge animal are discussed in the paper.
Keywords:sponge animal  Gezhongwu Formation  Early Cambrian  Guizhou
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