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Volumn 329, Issue 5991, 2010, Pages 556-559

Decrease in the CO2 uptake capacity in an ice-free Arctic Ocean basin

(17)  Cai, Wei Jun a   Chen, Liqi b   Chen, Baoshan a   Gao, Zhongyong b   Lee, Sang H c   Chen, Jianfang d   Pierrot, Denis e,f   Sullivan, Kevin e,f   Wang, Yongchen a   Hu, Xinping a   Huang, Wei Jen a   Zhang, Yuanhui b   Xu, Suqing b   Murata, Akihiko g   Grebmeier, Jacqueline M h   Jones, E Peter i   Zhang, Haisheng d  


Author keywords

[No Author keywords available]

Indexed keywords

CARBON DIOXIDE; SEA WATER;

EID: 77955101803     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1189338     Document Type: Article
Times cited : (219)

References (26)
  • 26
    • 77955106334 scopus 로고    scopus 로고
    • We thank R. Wanninkhof, P. Yager, and N. Bates for discussions; J. Zhao for the salinity and temperature data; and H. Li and S. Gao for sample collection. Funding for the CHINARE CO2 survey and subsequent synthesis was provided by the Ministry of Science and Technology of China (2009DFA22920), the Natural Science Foundation of China (40531007), and the U.S. National Oceanic and Atmospheric Administration (NA05OAR4311161 and NA09OAR4310078) and NSF (ARC-0909330). The measurements for primary production of phytoplankton were funded by a Korean Arctic Research project (PM09020). We also thank the Chinese Arctic and Antarctic Administration and the Polar Research Institute of China for their support. We are grateful to the captain and crew of icebreaker Xuelong
    • We thank R. Wanninkhof, P. Yager, and N. Bates for discussions; J. Zhao for the salinity and temperature data; and H. Li and S. Gao for sample collection. Funding for the CHINARE CO2 survey and subsequent synthesis was provided by the Ministry of Science and Technology of China (2009DFA22920), the Natural Science Foundation of China (40531007), and the U.S. National Oceanic and Atmospheric Administration (NA05OAR4311161 and NA09OAR4310078) and NSF (ARC-0909330). The measurements for primary production of phytoplankton were funded by a Korean Arctic Research project (PM09020). We also thank the Chinese Arctic and Antarctic Administration and the Polar Research Institute of China for their support. We are grateful to the captain and crew of icebreaker Xuelong.


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