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Volume 23 Issue 3
Jun 2012
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Journal of Earth Science  > 2012  >  23(3): 297-310.
Zhaokai Xu, Tiegang Li, Qingyun Nan, Xinke Yu, Anchun Li, Jinyong Choi. Paleoenvironmental Changes in the Northern Okinawa Trough since 25 ka BP: REE and Organic Carbon Evidence. Journal of Earth Science, 2012, 23(3): 297-310. doi: 10.1007/s12583-012-0254-5
Citation: Zhaokai Xu, Tiegang Li, Qingyun Nan, Xinke Yu, Anchun Li, Jinyong Choi. Paleoenvironmental Changes in the Northern Okinawa Trough since 25 ka BP: REE and Organic Carbon Evidence. Journal of Earth Science, 2012, 23(3): 297-310. doi: 10.1007/s12583-012-0254-5
shu

Paleoenvironmental Changes in the Northern Okinawa Trough since 25 ka BP: REE and Organic Carbon Evidence

doi: 10.1007/s12583-012-0254-5
  • 1.

    Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China

  • 2.

    Department of Oceanography, Kunsan National University, Kunsan 573-701, Korea

Funds:

the Open Fund of the Key Laboratory of Marine Geology and Environment, Chinese Academy of Sciences, the Innovative Program of Chinese Academy of Sciences KZCX2-YW-221

the National Basic Research Program of China 2007CB815903

the National Natural Science Foundation of China 41106043

the National Natural Science Foundation of China 40906038

More Information
  • Corresponding author: Tiegang Li, tgli@qdio.ac.cn
  • Received Date: 08 Nov 2010
  • Accepted Date: 30 Apr 2011
  • Publish Date: 01 Jun 2012
    Abstract
  • Paleoenvironmental changes in the northern Okinawa trough covering the last 25 ka were synthetically reconstructed using REE and organic carbon indices of core CSH1. Variations of these parameters revealed three distinct intervals of major sediment provenance changes that can be related to sea-level fluctuation and Tsushima Warm Current evolution. Interval 1 (16–24.7 ka BP) is characterized by dominantly fluvial discharge from the Changjiang (Yangtze River) and Huanghe (Yellow River) as well as high primary productivity. In Interval 2 (7.3–16 ka BP), the Changjiang and Huanghe mouths regressed with sea-level rising. The newly formed Tsushima Warm Current could carry some sediment loads of Taiwan to the study core, especially during its late phase (7.3–8.2 ka BP). Modern oceanographic conditions were finally established since the beginning of Interval 3, leading to more terrigenous contribution from Taiwan, whereas low sea-surface productivity in the study area.

     

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