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WANG KAIFA,JIANG HUI,FENG WENKE. 1987. DISCOVERY OF DIATOM ASSEMBLAGES FROM DEEP-SEA BASIN IN THE SOUTH CHINA SEA AND THEIR GEOLOGICAL IMPLICATION. Acta Oceanologica Sinica, (2):215－221
DISCOVERY OF DIATOM ASSEMBLAGES FROM DEEP-SEA BASIN IN THE SOUTH CHINA SEA AND THEIR GEOLOGICAL IMPLICATION
DISCOVERY OF DIATOM ASSEMBLAGES FROM DEEP-SEA BASIN IN THE SOUTH CHINA SEA AND THEIR GEOLOGICAL IMPLICATION
Received:September 25, 1985  Revised:February 28, 1986
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基金项目:Project supported by the Science Fund of the Chinese Academy of Sciences.
Author NameAffiliation
WANG KAIFA Department of Marine Geology, Tongji University, Shanghai 
JIANG HUI Department of Marine Geology, Tongji University, Shanghai 
FENG WENKE South China Sea Headquaters of Geological Survey, Ministry of Geology and Mineral Resources, Guangzhou 
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Abstract:
      Of the diatoms from sediments of the South China Sea, mainly composed of planktonic species of tropical and subtropical zones, 36 genera and 86 species are identified. Based on the changes in diatom numbers and the appearance of diatom assemblages, six diatom zones are distinguished in Core V1 reflecting six phases of paleoclimatc, paleo-watertemperature and paleogeography. According to the Quaternary climatic division, these zones represent hot weather and warm weather as a whole, and they are separately equal to postglacial period, the Holocene; Wurm glacial period; Riss-Wurm interglacial period; and Riss glacial period, the Late Pleistocene.
中文摘要:
      Of the diatoms from sediments of the South China Sea, mainly composed of planktonic species of tropical and subtropical zones, 36 genera and 86 species are identified. Based on the changes in diatom numbers and the appearance of diatom assemblages, six diatom zones are distinguished in Core V1 reflecting six phases of paleoclimatc, paleo-watertemperature and paleogeography. According to the Quaternary climatic division, these zones represent hot weather and warm weather as a whole, and they are separately equal to postglacial period, the Holocene; Wurm glacial period; Riss-Wurm interglacial period; and Riss glacial period, the Late Pleistocene.
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