孙存礼, 黄冬保. 1995: 赣西南“阳岭砾岩”微古植物的发现及其时代探讨. 地质通报, (1).
    引用本文: 孙存礼, 黄冬保. 1995: 赣西南“阳岭砾岩”微古植物的发现及其时代探讨. 地质通报, (1).
    1995: THE DISCOVERY OF MICROPALEOPHYTES IN THE YANGLINGPSEPHYTE IN SOUTHWESTERN JIANGXI AND ITS AGE. Geological Bulletin of China, (1).
    Citation: 1995: THE DISCOVERY OF MICROPALEOPHYTES IN THE YANGLINGPSEPHYTE IN SOUTHWESTERN JIANGXI AND ITS AGE. Geological Bulletin of China, (1).

    赣西南“阳岭砾岩”微古植物的发现及其时代探讨

    THE DISCOVERY OF MICROPALEOPHYTES IN THE YANGLINGPSEPHYTE IN SOUTHWESTERN JIANGXI AND ITS AGE

    • 摘要: 首次在“阳岭砾岩”的夹层中,获大量微古植物及几丁虫化石,为其时代置于晚寒武世至早奥陶世提供了有力证据。另外,对含义不清的“阳岭砾岩”重新厘定了定义,作为“组”级的正式岩石地层单位。

       

      Abstract: Many fossil micropaleophytes and chitinozoans were collected for the first time froni inter-calations of the Yangling psephyte in southwestern Jiangxi, Which furnishes strong evidencefor assigning the age of the Yangling psephyte to Late Cambrian-Early Ordovician. Mean-while, the Yangling psephyte whose connotation was originally ambiguous and vague has beenredefined , and it is regarded as a formal formation-rank lithostratigraphic unit.

       

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