To the problem of stage subdivision of the Lower Cambrian

@article{Rozanov2008ToTP,
  title={To the problem of stage subdivision of the Lower Cambrian},
  author={Alexei Yu. Rozanov and V. V. Khomentovsky and Yu. Ya. Shabanov and G. A. Karlova and A. I. Varlamov and V. A. Luchinina and Tatyana V. Pegel and Yu. E. Demidenko and Pavel Yu. Parkhaev and Igor’ V. Korovnikov and N. A. Skorlotova},
  journal={Stratigraphy and Geological Correlation},
  year={2008},
  volume={16},
  pages={1-19}
}
It was a serious mistake when subdivision stratotypes had been disposed of in practice of constructing the General stratigraphic scale, because they cannot be substituted by the boundary stratotypes. A subdivision stratotype and respective GSSP are complementary parts characterizing any stratigraphic unit. The best candidates for stage stratotypes of the Lower Cambrian are certainly sections of the Lena-Aldan region in the Siberian platform, which have been studied in detail during many years… 
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Abstract A stage subdivision of the Cambrian System is proposed. In the lower series four stages are distinguished (the Tommotian, Atdabanian, Botomian, Tojohnian); in the middle series, two (the
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  • A. Rozanov
  • Geography, Environmental Science
    Journal of the Geological Society
  • 1992
In Siberia, the so-called Khailakh and Manykay Stages of ‘pre-Tommotian’ age are inferred to be partly coeval with the type Tommotian, and to be based on a misunderstanding about the control of
Pre-Tommotian age of the lower Pestrotsvet Formation in the Selinde section on the Siberian platform: carbon isotopic evidence
Carbon isotopic data from the Selinde section in the southeastern part of the Siberian platform area are correlated with the reference isotopic profile from the Lower Cambrian stratotype sections of
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