Geochemical records of Taiwan-sourced sediments in the South China Sea linked to Holocene climate changes
详细信息 查看全文
- 作者：Jie Huang ; huangjie@qdio.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Shiming Wan ; Zhifang Xiong ; Debo Zhao ; Xiting Liu ; Anchun Li ; Tiegang Li
- 关键词：Geochemistry ; Chemical weathering ; Physical erosion ; Taiwan ; East Asian monsoon ; South China Sea
- 刊名：Palaeogeography, Palaeoclimatology, Palaeoecology
- 出版年：2016
- 出版时间：1 January 2016
- 年：2016
- 卷：441
- 期：part_P4
- 页码：871-881
- 全文大小：1525 K
文摘
- listitem" id="list_l0005">
- •
We present a variety of geochemical proxies of core KNG5.
- •
Core sediments were mainly derived from the Southwestern Taiwan Rivers.
- •
Taiwan belongs to a weathering-limited regime.
- •
Monsoon intensity is the primary control on the weathering intensity of Taiwan River sediments.
- •
Geochemical parameters are reliable proxies for climate changes in weathering-limited regimes.