Deepwater circulation variation in the South China Sea since the Last Glacial Maximum-Reference-Cited by-同舟云学术

Deepwater circulation variation in the South China Sea since the Last Glacial Maximum

Published:2016-08-19 Issue:16 Volume:43 Page:8590-8599
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Zheng Xufeng¹,Kao ShuhJi²,Chen Zhong¹,Menviel Laurie³,Chen Han⁴,Du Yan⁵,Wan Shiming⁶,Yan Hong⁷,Liu Zhonghui⁸,Zheng Liwei²,Wang Shuhong¹,Li Dawei²,Zhang Xu⁹

Affiliation:

1. Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology Chinese Academy of Sciences Guangzhou China

2. State Key Laboratory of Marine Environmental Science Xiamen University Xiamen China

3. Climate Change Research Centre, ARC Centre of Excellence for Climate System Science University of New South Wales Sydney Australia

4. Island Research Center State Oceanic Administration Fuzhou China

5. State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology Chinese Academy of Sciences Guangzhou China

6. Key Laboratory of Marine Geology and Environment Institute of Oceanology, Chinese Academy of Sciences (CAS) Qingdao China

7. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment Chinese Academy of Sciences Xi'an China

8. Department of Earth Sciences University of Hong Kong Hong Kong China

9. Alfred‐Wegener‐Institut Helmholtz‐Zentrumfür Polar‐ und Meeresforschung Bremerhaven Germany

Funder

National Natural Science Foundation of China

Australian Research Council

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL070342

Reference62 articles.

1. Timing of Millennial-Scale Climate Change in Antarctica and Greenland During the Last Glacial Period

2. Depositional characteristics and processes of alongslope currents related to a seamount on the northwestern margin of the Northwest Sub-Basin, South China Sea

3. Evidence for general instability of past climate from a 250-kyr ice-core record

4. A magnetic signature of bottom current erosion

5. Application of the anisotropy of magnetic susceptibility method as an indicator of bottom-water flow direction

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