Volume 35 Issue 2
Mar.  2010
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WANG Shan-shan, CAO Zhi-min, LAN Dong-zhao, ZHENG Zhi-chang, 2010. Geochemical Characteristics of Sediment of Pearl River Estuary and Its Paleoenvironmental Evolution. Earth Science, 35(2): 261-267. doi: 10.3799/dqkx.2010.026
Citation: WANG Shan-shan, CAO Zhi-min, LAN Dong-zhao, ZHENG Zhi-chang, 2010. Geochemical Characteristics of Sediment of Pearl River Estuary and Its Paleoenvironmental Evolution. Earth Science, 35(2): 261-267. doi: 10.3799/dqkx.2010.026

Geochemical Characteristics of Sediment of Pearl River Estuary and Its Paleoenvironmental Evolution

doi: 10.3799/dqkx.2010.026
  • Received Date: 2009-02-15
  • Publish Date: 2010-03-01
  • The trace metal elements and average grain size were determined for sediments of Pearl River Estuary and three important factors were identified using factor analysis method, which controls chemical compositions of sediments, such as catchment erosion, biogenic deposit, marine dominated condition. Moreover, further research indicates that the factor score curves of the three factors can be used to represent the changes of humidity, temperature and the hydrodynamics, respectively, which provides a good effective approach to paleoenviromental reconstruction. On the basis of the study, the evolution history of the regional climate and environment is evaluated and it is revealed that the basic climate succession in the region of Pearl River Delta is the cool-humid, cool-dry, warm-dry, warm-dry, warm-humid and warm-dry successively.

     

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