Chinese Science Bulletin

, 54:1797

Discussion on the Neoproterozoic glaciations in the South China Block and their related paleolatitudes

Authors

    • State Key Laboratory of Lithospheric Evolution, Institute of Geology and GeophysicsChinese Academy of Sciences
  • XueLei Chu
    • State Key Laboratory of Lithospheric Evolution, Institute of Geology and GeophysicsChinese Academy of Sciences
  • LianJun Feng
    • State Key Laboratory of Lithospheric Evolution, Institute of Geology and GeophysicsChinese Academy of Sciences
Correspondence/Geology

DOI: 10.1007/s11434-009-0139-x

Cite this article as:
Zhang, Q., Chu, X. & Feng, L. Chin. Sci. Bull. (2009) 54: 1797. doi:10.1007/s11434-009-0139-x

Abstract

The Kaigas, Sturtian, Marinoan, and Gaskiers glaciations are widely recognized in Neoproterozoic. However, in the South China Block only the Jiangkou (Sturtian) and Nantuo (Marinoan) are symbolized by sedimentary records. The Kaigas, recorded by isotopic and chemical proxies, exhibited likely the nature of cold paleoclimate with local mountain glaciation. The correlation of the Doushantuo Formation with the Gaskiers is indicated by the carbon isotope excursion and the dated age from the interval, however the South China Block was then under non-glacial weather. With no paleomagnetic data, the position of the South China Block during the Sturtian glaciation cannot be determined. The paleolatitudes of the South China Block during the Kaigas and Nantuo glaciations are intermediate, even though the Nantuo was once rendered erratically deduced equatorial. In fact, the paleolatitudes of the South China Block during the Neoproterozoic glaciations are all likely at about 30°–40°.

Keywords

South China BlockNeoproterozoic glaciationspaleolatitudesKaigasSturtianMarinoanGaskiers

Copyright information

© Science in China Press and Springer-Verlag GmbH 2009