Changes in Deep Water Oxygenation of the South China Sea Since the Last Glacial Period-Reference-Cited by-同舟云学术

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Changes in Deep Water Oxygenation of the South China Sea Since the Last Glacial Period

Published:2018-09-05 Issue:17 Volume:45 Page:9058-9066
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Li Gang¹^ORCID,Rashid Harunur²³,Zhong Lifeng⁴^ORCID,Xu Xing⁵,Yan Wen¹⁶,Chen Zhong¹

Affiliation:

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

2. Earth and Environmental Sciences; Memorial University of Newfoundland; St. John's Canada

3. Hadal Science and Technology Research Center; Shanghai Ocean University; Shanghai China

4. School of Marine Sciences; Sun Yat-Sen University; Guangzhou China

5. Guangzhou Marine Geological Survey; Ministry of Land and Resources; Guangzhou China

6. School of Marine Sciences; University of Chinese Academy of Sciences; Beijing China

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

Youth Innovation Promotion Association of the Chinese Academy of Sciences

Natural Science Foundation of Guangdong Province

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2018GL078568/fullpdf

Reference67 articles.

1. Mid-depth circulation in the Northwest Pacific during the last deglaciation: Evidence from foraminiferal radiocarbon ages;Ahagon;Geophysical Research Letters,2003

2. Limits on the ventilation rate for the Deep Ocean over the last 12000 years;Andree;Climate Dynamics,1986

3. The distribution of intermediate water in the western equatorial Pacific during January-February 1986;Bingham;Deep Sea Research Part I,1995

4. A deeper respired carbon pool in the glacial equatorial Pacific Ocean;Bradtmiller;Earth and Planetary Science Letters,2010

5. Ventilation of the glacial deep Pacific Ocean;Broecker;Science,2004

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